Endangered and Threatened Wildlife and Plants; Endangered Status for Six West Texas Aquatic Invertebrate Species and Designation of Critical Habitat, 49601-49651 [2012-19829]
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Vol. 77
Thursday,
No. 159
August 16, 2012
Part III
Department of the Interior
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Fish and Wildlife Service
50 CFR Part 17
Endangered and Threatened Wildlife and Plants; Endangered Status for
Six West Texas Aquatic Invertebrate Species and Designation of Critical
Habitat; Proposed Rule
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Federal Register / Vol. 77, No. 159 / Thursday, August 16, 2012 / Proposed Rules
DEPARTMENT OF THE INTERIOR
Fish and Wildlife Service
50 CFR Part 17
[Docket No. FWS–R2–ES–2012–0029;
4500030113]
RIN 1018–AX70
Endangered and Threatened Wildlife
and Plants; Endangered Status for Six
West Texas Aquatic Invertebrate
Species and Designation of Critical
Habitat
Fish and Wildlife Service,
Interior.
ACTION: Proposed rule.
AGENCY:
We, the U.S. Fish and
Wildlife Service, propose to list as
endangered and propose critical habitat
for six west Texas aquatic invertebrate
species under the Endangered Species
Act. These actions are being taken as the
result of a court-approved settlement
agreement. These are proposed
regulations, and if finalized the effect of
these regulations will be to conserve the
species and protect their habitat under
the Endangered Species Act.
DATES: We will accept comments
received or postmarked on or before
October 15, 2012. We must receive
requests for public hearings, in writing,
at the address shown in FOR FURTHER
INFORMATION CONTACT by October 1,
2012.
SUMMARY:
You may submit comments
by one of the following methods:
(1) Electronically: Go to the Federal
eRulemaking Portal: https://
www.regulations.gov and search for
ADDRESSES:
FWS–R2–ES–2012–0029, which is the
docket number for this rulemaking.
(2) By hard copy: Submit by U.S. mail
or hand-delivery to: Public Comments
Processing, Attn: FWS–R2–ES–2012–
0029; Division of Policy and Directives
Management; U.S. Fish and Wildlife
Service; 4401 N. Fairfax Drive, MS
2042–PDM; Arlington, VA 22203.
We request that you send comments
only by the methods described above.
We will post all comments on https://
www.regulations.gov. This generally
means that we will post any personal
information you provide us (see the
Public Comments section below for
more information).
The coordinates, or plot points, or
both from which the critical habitat
maps are generated are included in the
administrative record for this
rulemaking and are available at (https://
www.fws.gov/southwest/es/
AustinTexas/), https://
www.regulations.gov at Docket No.
FWS–R2–ES–2012–0029, and at the
Austin Ecological Services Field Office
(see FOR FURTHER INFORMATION CONTACT).
Any additional tools or supporting
information that we may develop for
this rulemaking will also be available at
the Fish and Wildlife Service Web site
and Field Office set out above, and may
also be included in the preamble and/
or at https://www.regulations.gov.
FOR FURTHER INFORMATION CONTACT:
Adam Zerrenner, Field Supervisor, U.S.
Fish and Wildlife Service, Austin
Ecological Services Field Office, 10711
Burnet Road, Suite 200, Austin, TX
78758; by telephone 512–490–0057; or
by facsimile 512–490–0974. Persons
who use a telecommunications device
San Solomon Spring system (four springs) ....................
San Solomon Spring system (four springs) ....................
San Solomon Spring system (four springs) ....................
Diamond Y Spring system (two springs) ........................
Diamond Y Spring system (two springs) ........................
Diamond Y Spring system (two springs) ........................
Executive Summary
This document consists of proposed
rules to list six west Texas aquatic
invertebrate species as endangered and
propose critical habitat designations for
the six species. The six west Texas
aquatic invertebrate species are:
Phantom Cave snail (Pyrgulopsis
texana), Phantom springsnail (Tryonia
cheatumi), diminutive amphipod
(Gammarus hyalleloides), Diamond Y
Spring snail (Pseudotryonia
adamantina), Gonzales springsnail
(Tryonia circumstriata), and Pecos
amphipod (Gammarus pecos). The
current range for the first three species
is limited to spring outflows in the San
Solomon Springs system near
Balmorhea in Reeves and Jeff Davis
Counties, Texas. The current range of
the latter three species is restricted to
spring outflow areas within the
Diamond Y Spring system north of Fort
Stockton in Pecos County, Texas.
Why we need to publish a rule. Under
the Endangered Species Act, a species
may warrant protection through listing
if it is endangered or threatened
throughout all or a significant portion of
its range. In this proposal we are
explaining why these six species
warrant protection under the
Endangered Species Act. Five of the six
species of aquatic invertebrates are
currently identified as candidates for
listing based on threats to their habitat.
The table below summarizes the status
of each species:
Present range
Phantom Cave snail .............
Phantom Lake springsnail ...
diminutive amphipod ............
Diamond Y Spring snail .......
Gonzales springsnail ............
Pecos amphipod ..................
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Species
for the deaf (TDD) may call the Federal
Information Relay Service (FIRS) at
800–877–8339.
SUPPLEMENTARY INFORMATION:
These rules propose that all six of
these species should be listed as
endangered. We are proposing a listing
status of endangered for these six
species of aquatic invertebrates from
west Texas.
The Endangered Species Act provides
the basis for our action. Under the
Endangered Species Act, we can
determine that a species is endangered
or threatened based on any of five
factors: (A) The present or threatened
destruction, modification, or
curtailment of its habitat or range; (B)
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Status of species
common in a very restricted range.
very rare in a very restricted range.
common in a very restricted range.
very rare in a very restricted range.
very rare in a very restricted range.
common in a very restricted range
Overutilization for commercial,
recreational, scientific, or educational
purposes; (C) Disease or predation; (D)
The inadequacy of existing regulatory
mechanisms; or (E) Other natural or
manmade factors affecting its continued
existence. We are proposing that all six
species are endangered by the combined
effects of:
• Habitat loss and degradation of
aquatic resources, particularly the
current and ongoing decline in spring
flows that support the habitat of all the
species, and the potential for future
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water contamination at the Diamond Y
Spring system.
• Inadequate existing regulatory
mechanisms that allow significant
threats such as groundwater
withdrawal.
• Other natural or manmade factors,
including the presence of nonnative
snails and the small, reduced ranges of
the species.
These rules also propose designation
of critical habitat for each of the six
species. Under the Endangered Species
Act, we designate specific areas as
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critical habitat to foster conservation of
listed species. Future actions funded,
permitted, or otherwise carried out by
Federal agencies will be reviewed to
ensure they do not adversely modify
critical habitat. Critical habitat does not
affect private actions on private lands.
We are proposing the following areas in
49603
Texas as critical habitat for Phantom
Cave snail, Phantom springsnail, and
diminutive amphipod:
Size of unit in
hectares (acres)
Critical habitat unit
Land ownership by type
San Solomon Spring, Reeves County ......................................
Giffin Spring, Reeves County ...................................................
East Sandia Spring, Reeves County ........................................
Phantom Lake Spring, Jeff Davis County ................................
State—Texas Parks and Wildlife Department .........................
Private ......................................................................................
Private—The Nature Conservancy ..........................................
Federal—Bureau of Reclamation .............................................
1.8 (4.4)
0.7 (1.7)
1.2 (3.0)
0.02 (0.05)
Total ...................................................................................
...................................................................................................
3.7 (9.2)
Note: Area sizes may not sum due to rounding.
We are proposing the following areas
as critical habitat for Diamond Y Spring
snail, Gonzales springsnail, and Pecos
amphipod:
Size of unit in
hectares (acres)
Land ownership by type
Diamond Y Spring System, Pecos County ..............................
Private—The Nature Conservancy ..........................................
178.6 (441.4)
Total ...................................................................................
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Critical habitat unit
...................................................................................................
178.6 (441.4)
We are preparing an economic
analysis. We are preparing an economic
analysis of the proposed designations of
critical habitat to allow for
consideration of the economic impacts
of the proposed designations of critical
habitat. We will publish an
announcement and seek public
comments on the draft economic
analysis when it is completed.
We will request peer review of the
methods used in our proposal. We are
seeking comments from independent
specialists with scientific expertise in
these species or related fields. We have
invited these peer reviewers to comment
on the scientific information and
methods that we used in making this
proposal. Because we will consider all
comments and information received
during the comment period, our final
determinations may differ from this
proposal.
We are seeking public comment on
these proposed rules. Anyone is
welcome to comment on our proposal or
provide additional information on the
proposal that we can use in making a
final determination on the status of
these species. Please submit your
comments and materials concerning
these proposed rules by one of the
methods listed in the ADDRESSES
section. Within 1 year following the
publication of this proposal, we will
publish in the Federal Register a final
determination to list one or more of
these species as threatened or
endangered, or withdraw the proposals
if new information is provided that
supports that decision.
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Public Comments
We intend that any final action
resulting from these proposed rules will
be based on the best scientific and
commercial data available and be as
accurate and as effective as possible.
Therefore, we request comments or
information from the public, other
concerned governmental agencies,
Native American tribes, the scientific
community, industry, or any other
interested parties concerning these
proposed rules. We particularly seek
comments concerning:
(1) Biological, commercial trade, or
other relevant data concerning any
threats (or lack thereof) to this species
and regulations that may be addressing
those threats.
(2) Additional information concerning
the historical and current status, range,
distribution, and population size of this
species, including the locations of any
additional populations of this species.
(3) Any information on the biological
or ecological requirements of the
species, and ongoing conservation
measures for the species and its habitat.
(4) Current or planned activities in the
areas occupied by the species and
possible impacts of these activities on
this species.
(5) The reasons why we should or
should not designate habitat as ‘‘critical
habitat’’ under section 4 of the Act (16
U.S.C. 1531 et seq.) including whether
there are threats to the species from
human activity, the degree of which can
be expected to increase due to the
designation, and whether that increase
in threat outweighs the benefit of
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designation such that the designation of
critical habitat may not be prudent.
(6) Specific information on:
(a) The amount and distribution of
habitat for the six west Texas aquatic
invertebrates;
(b) What areas, that were occupied at
the time of listing (or are currently
occupied) and that contain features
essential to the conservation of the
species, should be included in the
designation and why;
(c) Special management
considerations or protection that may be
needed in critical habitat areas we are
proposing, including managing for the
potential effects of climate change; and
(d) What areas not occupied at the
time of listing are essential for the
conservation of the species and why.
(7) Land use designations and current
or planned activities in the subject areas
and their possible impacts on proposed
critical habitat.
(8) Information on the projected and
reasonably likely impacts of climate
change on the six west Texas aquatic
invertebrates and proposed critical
habitat.
(9) Any probable economic, national
security, or other relevant impacts of
designating any area that may be
included in the final designation; in
particular, any impacts on small entities
or families, and the benefits of including
or excluding areas that exhibit these
impacts.
(10) Whether any specific areas we are
proposing for critical habitat
designation should be considered for
exclusion under section 4(b)(2) of the
Act, and whether the benefits of
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potentially excluding any specific area
outweigh the benefits of including that
area under section 4(b)(2) of the Act.
(11) Whether the benefits of exclusion
outweigh the benefits of including the
area proposed as critical habitat around
San Solomon Spring at Balmorhea State
Park based on the existing habitat
conservation plan or other relevant
factors.
(12) Whether we could improve or
modify our approach to designating
critical habitat in any way to provide for
greater public participation and
understanding, or to better
accommodate public concerns and
comments.
Please note that submissions merely
stating support for or opposition to the
action under consideration without
providing supporting information,
although noted, will not be considered
in making a determination, as section
4(b)(1)(A) of the Act directs that
determinations as to whether any
species is a threatened or endangered
species must be made ‘‘solely on the
basis of the best scientific and
commercial data available.’’
You may submit your comments and
materials concerning these proposed
rules by one of the methods listed in the
ADDRESSES section. We request that you
send comments only by the methods
described in the ADDRESSES section.
If you submit information via https://
www.regulations.gov, your entire
submission—including any personal
identifying information—will be posted
on the Web site. If your submission is
made via a hardcopy that includes
personal identifying information, you
may request at the top of your document
that we withhold this information from
public review. However, we cannot
guarantee that we will be able to do so.
We will post all hardcopy submissions
on https://www.regulations.gov. Please
include sufficient information with your
comments to allow us to verify any
scientific or commercial information
you include.
Comments and materials we receive,
as well as supporting documentation we
used in preparing these proposed rules,
will be available for public inspection
on https://www.regulations.gov, or by
appointment, during normal business
hours, at the U.S. Fish and Wildlife
Service, Austin Ecological Services
Field Office (see FOR FURTHER
INFORMATION CONTACT).
Previous Federal Actions
We first proposed the Phantom Cave
snail and Phantom springsnail as
endangered species on April 28, 1976
(41 FR 17742). At that time, the
Phantom Cave snail (Pyrgulopsis
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texana) was referred to as the Reeves
County snail (Cochliopa texana), and
the Phantom springsnail was referred to
as the Cheatum’s snail. The proposal
was withdrawn on March 6, 1979 (44 FR
12382), following 1978 amendments to
the Act that made additional
requirements necessary for designating
critical habitat. Both species were added
as candidates for listing in the May 22,
1984, Notice of Review of Invertebrate
Wildlife for Listing as Endangered or
Threatened Species (49 FR 21664). At
that time they were categorized as
Category 2 Candidates, which meant
that we had information that proposed
listing is possibly appropriate, but
conclusive data on biological
vulnerability and threats was not
available to support a proposed rule at
the time. They remained so designated
in our subsequent annual Candidate
Notices of Review (54 FR 554, January
6, 1989; 56 FR 58804, November 21,
1991; and 59 FR 58982, November 15,
1994). In the February 28, 1996, Notice
(61 FR 7596), we discontinued the
designation of Category 2 species as
candidates, which removed these two
species from the candidate list.
Both species were then added back to
the candidate list on October 30, 2001
(66 FR 54808). Species on the candidate
list are those fish, wildlife, and plants
for which we have on file sufficient
information on biological vulnerability
and threats to support preparation of a
listing proposal, but for which
development of a listing regulation is
precluded by other higher priority
listing activities. Since 2001, the listing
priority number for both species has
been a 2, reflecting species with threats
that are both imminent and high in
magnitude in accordance with our
priority guidance published on
September 21, 1983 (48 FR 43098).
These two snails remained candidates
in subsequent Candidate Notices of
Review (67 FR 40657, June 13, 2002; 69
FR 24876, May 4, 2004). Both species
were also petitioned for listing on May
11, 2004, and were found to be
warranted for listing but precluded by
higher priority activities in subsequent
Candidate Notice of Reviews (70 FR
24870, May 11, 2005; 71 FR 53756,
September 12, 2006; 72 FR 69034,
December 6, 2007; 73 FR 75176,
December 10, 2008; 74 FR 57804,
November 9, 2009; and 75 FR 69222,
November 10, 2010). The October 26,
2011, Candidate Notice of Review (76
FR 66370) stated that we were working
on proposed listing rules for these
species.
We identified the Diamond Y Spring
snail and Gonzales springsnail as
candidates for listing in the January 6,
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1989, Endangered or Threatened
Wildlife and Plants, Annual Notice of
Review (54 FR 554). These snails were
designated as Category 1 candidates,
indicating we had substantial
information to support listing, but a
proposed rule was precluded by other
listing activities. These two species
were included in all of our subsequent
annual Candidate Notices of Review
even after discontinuing the candidate
categories (56 FR 58804, November 21,
1991, and 59 FR 58982, November 15,
1994). From 1996 to 1999 these two
species had a listing priority number of
5, reflecting species with high
magnitude but nonimminent threats (61
FR 7596, February 28, 1996; 62 FR
49398, September 19, 1997; and 64 FR
57534, October 25, 1999). In 2001 we
elevated the listing priority number
from 5 to 2 because of a new, imminent
threat associated with the introduction
of nonnative snails into the species’
habitat. A listing priority of 2 indicates
both high magnitude and imminent
threats. Both species have maintained a
listing priority of 2 since then (66 FR
54808, October 30, 2001; 67 FR 40657,
June 13, 2002; and 69 FR 24876, May 4,
2004). These two species were also
petitioned for listing on May 11, 2004,
and were found to be warranted for
listing but precluded by higher priority
activities in subsequent Candidate
Notice of Reviews (70 FR 24870, May
11, 2005; 71 FR 53756, September 12,
2006; 72 FR 69034, December 6, 2007;
73 FR 75176, December 10, 2008; 74 FR
57804, November 9, 2009; and 75 FR
69222, November 10, 2010). The
October 26, 2011, Candidate Notice of
Review (76 FR 66370) stated that we
were working on proposed listing rules
for these species.
We identified the diminutive
amphipod and Pecos amphipod as
Category 2 candidate species for listing
in the May 22, 1984, Notice of Review
of Invertebrate Wildlife for Listing as
Endangered or Threatened Species (49
FR 21664). They remained so designated
in our subsequent annual Candidate
Notices of Review (54 FR 554, January
6, 1989; 56 FR 58804, November 21,
1991; and 59 FR 58982, November 15,
1994). In the February 28, 1996, Notice
(61 FR 7596), we discontinued the
designation of Category 2 species as
candidates, which removed these two
species from the candidate list. The
diminutive amphipod was added back
to the candidate list on May 11, 2005
(70 FR 24870), and has remained a
candidate with a listing priority number
of 2 (reflecting both high-magnitude and
imminent threats) since that time (71 FR
53756, September 12, 2006; 72 FR
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69034, December 6, 2007; 73 FR 75176,
December 10, 2008; 74 FR 57804,
November 9, 2009; and 75 FR 69222,
November 10, 2010). The October 26,
2011, Candidate Notice of Review (76
FR 66370) stated that we were working
on a proposed listing rule for the
diminutive amphipod.
The Pecos amphipod was not
included in recent candidate notices
along with the other species in this
proposal because of taxonomic
uncertainties, which have since been
resolved. In the past it was unclear
whether this species range was limited
to Diamond Y Spring. Recent genetic
research has confirmed that the species
is endemic to Diamond Y Spring (see
full discussion below under Taxonomy,
Distribution, and Abundance of
Amphipods, Pecos Amphipod). The
Pecos amphipod was included in the
June 25, 2007, petition by WildEarth
Guardians to the Service seeking the
listing of 475 species in the
southwestern United States. On January
6, 2009, we published a partial 90-day
finding of the petition for listing 475
species which included a finding that
the petition did not present substantial
scientific or commercial information
indicating that the listing of the Pecos
amphipod may be warranted (74 FR
419). During our current review of the
other species endemic to the Diamond
Y Spring system, we reviewed the status
of the Pecos amphipod. Based on the
results of that review, we are proposing
to list it as endangered.
Background
We intend to discuss below only
those topics directly relevant to the
consideration of the listing of the six
west Texas aquatic invertebrates as
endangered and proposed critical
habitat designations. We have organized
this Background section into three
parts. The first part is a general
description of the two primary spring
systems where the six species occur.
The second part is a general description
of the life history and biology of the four
snail species, followed by specific
biological information on each of the
four snail species. The third part is a
general description of the life history
and biology of the two amphipod
species, followed by specific biological
information on each of the two
amphipod species.
Description of Chihuahuan Desert
Springs Inhabited by Invertebrate
Species
The six west Texas aquatic
invertebrate species (Phantom Cave
snail, Phantom springsnail, diminutive
amphipod, Diamond Y Spring snail,
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Gonzales springsnail, and Pecos
amphipod) occur within a relatively
small area of the Chihuahuan Desert of
the Pecos River drainage basin of west
Texas. The habitats of these species are
now isolated spring systems in
expansive carbonate (limestone)
deposit. The region includes a complex
of aquifers (underground water systems)
where the action of water on soluble
rocks (like limestone and dolomite) has
formed abundant ‘‘karst’’ features such
as sinkholes, caverns, springs, and
underground streams. These
hydrogeological formations provide
unique settings where a diverse
assemblage of flora and fauna has
evolved at the points where the aquifers
discharge waters to the surface through
spring openings. The isolated limestone
and gypsum springs, seeps, and
wetlands located in this part of west
Texas provide the only known habitats
for several endemic species of fish,
plants, mollusks, and crustaceans,
including the six endemic aquatic
invertebrate species addressed in these
proposed rules.
In the Chihuahuan Desert, springadapted aquatic species are distributed
in isolated, geographically separate
populations. They likely evolved into
distinct species from parent species that
once enjoyed a wider distribution
during wetter, cooler climates of the
Pleistocene epoch (about 10,000 to 2.5
million years before present). As ancient
lakes and streams dried during dry
periods (since the Late Pleistocene,
within about the last 100,000 years),
aquatic species in this region became
patchily distributed across the
landscape as geographically isolated
populations exhibiting a high degree of
endemism (species found only in a
particular region, area, or spring). Such
speciation through divergence has been
reported for these species (Gervasio et
al. 2004, p. 521; Brown et al. 2008, pp.
486–487; Seidel et al. 2009, p. 2304).
San Solomon Spring System
In these proposed rules we reference
the San Solomon Spring system to
include four different existing spring
outflows: San Solomon Spring, Giffin
Spring, Phantom Lake Spring, and East
Sandia Spring. The springs in this area
are also commonly referred to by some
authors as Toyah Basin springs or
Balmorhea area springs. All of the
springs historically drained into Toyah
Creek, an intermittent tributary of the
Pecos River that is now dry except
following large rainfall events. All four
springs are located in proximity to one
another; it is about 13 kilometers (km)
(8 miles (mi)) between the farthest two
(East Sandia Spring to Phantom Lake
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49605
Spring). Brune (1981, pp. 258–259, 382–
386) provides a brief overview of each
of these springs and documents their
declining flows during the early and
middle twentieth century.
The San Solomon Spring system is
located in the Chihuahuan Desert of
west Texas at the foothills of the Davis
Mountains near Balmorhea, Texas.
Phantom Lake Spring is in Jeff Davis
County (on the county boundary with
Reeves County), while the other major
springs in this system are in Reeves
County. In addition to being an
important habitat for rare aquatic fauna,
area springs have served for centuries as
an important source of irrigation water
for local farming communities. They are
all located near the small town of
Balmorhea (current population of less
than 500 people) in west Texas. The
area is very rural with no nearby
metropolitan centers. Land ownership
in the region is mainly private, except
as described below around the spring
openings, and land use is
predominantly dry-land ranching with
some irrigated farmland.
The base flows from all of these
springs are thought to ultimately
originate from a regional groundwater
flow system. Studies show that
groundwater moves through geologic
faults from the Salt Basin northwest of
the Apache and Delaware Mountains,
located 130 km (80 mi) or more to the
west of the springs (Sharp 2001, pp. 42–
45; Angle 2001, p. 247; Sharp et al.
2003, pp. 8–9; Chowdhury et al. 2004,
pp. 341–342; Texas Water Development
Board 2005, p. 106). The originating
groundwater and spring outflow are
moderately to highly mineralized and
appear to be of ancient origin, with the
water being estimated at 10,000 to
18,000 years old (Chowdhury et al.
2004, p. 340; Texas Water Development
Board 2005, p. 89). The Salt Basin
Bolson aquifer is part of the larger West
Texas Bolsons and is made up of
connected sub-basins underlying Wild
Horse, Michigan, Lobo, and Ryan Flats,
in the middle and southern Salt Basin
Valley in Texas (Angle, 2001, p. 242).
(The term bolson is of Spanish origin
and refers to a flat-floored desert valley
that drains to a playa or flat.) These
aquifers, which support the base flows
(flows not influenced by seasonal
rainfall events) of the San Solomon
Spring system, receive little to no
modern recharge from precipitation
(Scanlon et al. 2001, p. 28; Beach et al.
2004, pp. 6–9, 8–9). Studies of the
regional flow system indicate
groundwater may move from south to
north through the Salt Basin from Ryan
to Lobo to Wild Horse Flats before being
discharged through the Capitan
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Formation, into the Lower Cretaceous
rocks (older than Pleistocene) via large
geologic faults then exiting to the
surface at the springs (LaFave and Sharp
1987, pp. 7–12; Angle 2001, p. 247;
Sharp 2001, p. 42–45; Chowdhury et al.
2004, pp. 341–342; Beach et al. 2004,
Figure 4.1.13, p. 4–19, 4–53). Chemical
analysis and hydrogeological studies
support this hypothesis, and the water
elevations throughout these parts of the
Salt Basin Bolson aquifer are higher in
elevation than the discharge points at
the springs (Chowdhury et al. 2004, p.
342).
In contrast to the base flows, the
springs also respond with periodic
short-term increases in flow rates
following local, seasonal rainstorms
producing runoff events through
recharge areas from the Davis
Mountains located to the southwest of
the springs (White et al. 1941, pp. 112–
119; LaFave and Sharp 1987, pp. 11–12;
Chowdhury et al. 2004, p. 341). These
freshwater recharge events provide very
temporary increases in spring flows,
sometimes resulting in flow spikes
many times larger than the regular base
flows. The increased flows are shortlived until the local stormwater recharge
is drained away and spring flows return
to base flows supported by the distant
aquifers. Historically, many of the
springs in this spring system were likely
periodically interconnected following
storm events with water flowing
throughout the Toyah Creek watershed.
In recent times, however, manmade
structures altered the patterns of spring
outflows and stormwater runoff, largely
isolating the springs from one another
except through irrigation canals.
San Solomon Spring is by far the
largest single spring in the Toyah Basin
(Brune 1981, p. 384). The artesian
spring issues from the lower Cretaceous
limestone at an elevation of about 1,008
meters (m) (3,306 feet (ft)). Brune (1981,
p. 385) reported spring flows in the
range of 1.3 to 0.8 cubic meters per
second (cms) (46 to 28 cubic feet per
second (cfs)) between 1900 and 1978
indicating an apparent declining trend.
Texas Water Development Board (2005,
p. 84) studies reported an average flow
rate of about 0.85 cms (30 cfs) from data
between 1965 to 2001 with a calculated
slope showing a slight decline in
discharge.
San Solomon Spring now provides
the water for the large, unchlorinated,
flow-through swimming pool at
Balmorhea State Park and most of the
irrigation water for downstream
agricultural irrigation by the Reeves
County Water Improvement District No.
1 (District). The swimming pool is
concrete on the sides and natural
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substrates on the bottom and was
originally constructed in 1936.
Balmorhea State Park is owned and
managed by Texas Parks and Wildlife
Department and encompasses about 19
hectares (ha) (46 acres (ac)) located
about 6 km (4 mi) west of Balmorhea in
the historic community of Toyahvale.
The Park provides recreational
opportunities of camping, wildlife
viewing, and swimming and scuba
diving in the pool. The District holds
the water rights for the spring which is
channeled through an extensive system
of concrete-lined irrigation channels,
and much of the water is stored in
nearby Lake Balmorhea and delivered
through canals for flood irrigation on
farms down gradient (Simonds 1996, p.
2).
Balmorhea State Park’s primary
wildlife resource focus is on
conservation of the endemic aquatic
species that live in the outflow of San
Solomon Spring (Texas Parks and
Wildlife Department 1999, p. 1). Texas
Parks and Wildlife Department
´
maintains two constructed cienegas that
are flow-through, earth-lined pools in
the park to simulate more natural
aquatic habitat conditions for the
conservation of the rare species,
including the Phantom Cave snail,
Phantom springsnail, and diminutive
´
amphipods. (Cienega is a Spanish term
that describes a spring outflow that is a
permanently wet and marshy area.) San
Solomon Spring is also inhabited by two
federally listed fishes, Comanche
Springs pupfish (Cyprinodon elegans)
and Pecos gambusia (Gambusia nobilis).
No nonnative fishes are known to occur
in San Solomon Spring, but two
nonnative aquatic snails, red-rim
melania (Melanoides tuberculata) and
quilted melania (Tarebia granifera), do
occur in the spring outflows and are a
cause for concern for the native aquatic
invertebrate species.
Giffin Spring is on private property
less than 1.6 km (1.0 mi) west of
Balmorhea State Park, across State
Highway 17. The spring originates from
an elevation similar to San Solomon
Spring. Brune (1981, p. 385) reported
flow from Giffin Spring ranging from
0.07 to 0.17 cms (2.3 to 5.9 cfs) between
1919 and 1978, with a gradually
declining trend. During calendar year
2011, Giffin Spring flow rates were
recorded between 0.10 and 0.17 cms
(3.4 and 5.9 cfs) (U.S. Geological Survey
2012, p. 1). Giffin Spring water flows are
captured in irrigation earthen channels
for agricultural use. Giffin Spring is also
inhabited by the federally listed
Comanche springs pupfish and Pecos
gambusia, and the only nonnative
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aquatic species of concern there is the
red-rim melania.
Phantom Lake Spring is at the base of
the Davis Mountains about 6 km (4 mi)
west of Balmorhea State Park at an
elevation of 1,080 m (3,543 ft). The
outflow originates from a large crevice
on the side of a limestone outcrop cliff.
The 7-ha (17-ac) site around the spring
and cave opening is owned by the U.S.
Bureau of Reclamation. Prior to 1940 the
recorded flow of this spring was
regularly exceeding 0.5 cms (18 cfs).
Outflows after the 1940s were
immediately captured in concrete-lined
irrigation canals and provided water for
local crops before connecting to the
District’s canal system in Balmorhea
State Park. Flows declined steadily over
the next 70 years until ceasing
completely in about the year 2000
(Brune 1981, pp. 258–259; Allan 2000,
p. 51; Hubbs 2001, p. 306). The aquatic
habitat at the spring pool has been
maintained by a pumping system since
then. Phantom Lake Spring is also
inhabited by the two federally listed
fishes, Comanche Springs pupfish and
Pecos gambusia, and the only nonnative
aquatic species of concern there is the
red-rim melania.
East Sandia Spring is the smallest
spring in the system located in Reeves
County in the community of Brogado
approximately 3 km (2 mi) northeast of
the town of Balmorhea and 7.7 km (4.8
mi) northeast of Balmorhea State Park.
The spring is within a 97-ha (240-ac)
preserve owned and managed by The
Nature Conservancy—a private
nonprofit conservation organization
(Karges 2003, pp. 145–146). In contrast
to the other springs in the San Solomon
Spring system that are derived directly
from a deep underground regional flow
system, East Sandia Spring discharges
from alluvial sand and gravel from a
shallow groundwater source at an
elevation of 977 m (3,224 ft) (Brune
1981, p. 385; Schuster 1997, p. 92).
Water chemistry at East Sandia Spring
indicates it is not directly
hydrologically connected with the other
springs in the San Solomon Spring
system in the nearby area (Schuster
1997, pp. 92–93). Historically there was
an additional, smaller nearby spring
outlet called West Sandia Spring. Brune
(1981, pp. 385–386) reported the
combined flow of East and West Sandia
Springs as declining, with
measurements ranging from 0.09 to 0.02
cms (3.2 to 0.7 cfs) between 1932 and
1976. In 1976 outflow from East Sandia
was 0.01 cms (0.5 cfs) of the total 0.02
cms (0.7 cfs) of the two springs. In 1995
and 1996 Schuster (1997, p. 94) reported
flows from both springs ranging from
0.12 to 0.01 cms (4.07 cfs to 0.45 cfs),
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with an average of 0.05 cms (1.6 cfs).
The outflow waters from the spring
discharge to an irrigation canal within a
few hundred meters from its source.
East Sandia Spring is also inhabited by
two federally listed fishes, Comanche
Springs pupfish and Pecos gambusia, as
well as the federally endangered Pecos
assiminea (Assiminea pecos) snail and
the federally threatened Pecos
sunflower (Helianthus paradoxus). No
nonnative aquatic species of concern are
known from East Sandia Spring.
Historically there were other area
springs along Toyah Creek that were
part of the San Solomon Spring system.
Saragosa and Toyah Springs occurred in
the town of Balmorhea along Toyah
Creek. Brune (1981, p. 386) reported
historic base flows of about 0.2 cms (6
cfs) in the 1920s and 1940s, declining to
about 0.06 cms (2 cfs) in the 1950s and
1960s, and no flow was recorded in
1978. Brune (1981, p. 385) reported that
the flow from West Sandia Spring was
about 0.01 cms (0.2 cfs) in 1976, after
combined flows from East and West
Sandia Springs had exceeded 0.07 cms
(2.5 cfs) between the 1930s and early
1960s. The Texas Water Development
Board (2005, p. 12) reported West
Sandia and Saragosa Springs did not
discharge sufficient flow for
measurement. Karges (2003, p. 145)
indicated West Sandia has only
intermittent flow and harbors no aquatic
fauna. It is unconfirmed whether the six
aquatic invertebrates discussed in this
document occurred in these now dry
spring sites, but given their current
distribution in springs located upstream
and downstream of these historic
springs, we assume that they probably
did. However, because these springs
have been dry for many decades, they
no longer provide habitat for the aquatic
invertebrates.
Diamond Y Spring System
The Diamond Y Spring system is
within a tributary drainage flowing
northeast to the Pecos River. Diamond Y
Spring (previously called Willbank
Spring) is located about 80 km (50 mi)
due east of San Solomon Spring and
about 12 km (8 mi) north of the City of
Fort Stockton in Pecos County. The
Diamond Y Spring system is composed
of disjunct upper and lower
watercourses, separated by about 1 km
(0.6 mi) of dry stream channel.
The upper watercourse is about 1.5
km (0.9 mi) long and starts with the
Diamond Y Spring head pool, which
drains into a small spring outflow
channel. The channel enters a broad
valley and braids into numerous
wetland areas and is augmented by
numerous small seeps. The Diamond Y
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Spring outflow converges with the Leon
Creek drainage and flows through a
marsh-meadow, where it is then referred
to as Diamond Y Draw. All of the small
springs and seeps and their outflow
comprise the upper watercourse. These
lateral water features, often not mapped,
are spread across the flat, seasonally
wetted area along Diamond Y Draw.
Therefore, unlike other spring systems
that have a relatively small footprint,
aquatic habitat covers a relatively large
area along the Diamond Y draw.
The lower watercourse of Diamond Y
Draw has a smaller head pool spring,
referred to as Euphrasia Spring, with a
small outflow stream as well as several
isolated pools and associated seeps and
wetland areas. The total length of the
lower watercourse is about 1 km (0.6
mi) and has extended below the bridge
at State Highway 18 during wetter
seasons in the past. The upper
watercourse is only hydrologically
connected to the lower watercourse by
surface flows during rare large rainstorm
runoff events. The lower watercourse
also contains small springs and seeps
laterally separated from the main spring
outflow channels.
Virtually all of the Diamond Y Spring
area (both upper and lower
watercourses and the area in between)
occurs on the Diamond Y Spring
Preserve, which is owned and managed
by The Nature Conservancy. The
Diamond Y Spring Preserve is 1,603 ha
(3,962 ac) of contiguous land around
Diamond Y Draw. The surrounding
watershed and the land area over the
contributing aquifers are all privately
owned and managed as ranch land and
have been developed for oil and gas
extraction. In addition, a natural gas
processing plant is located within 0.8
km (0.5 mi) upslope of the headpool in
the upper watercourse of Diamond Y
Spring. Diamond Y Spring is also
inhabited by two federally listed fishes,
Leon Springs pupfish (Cyprinodon
bovinus) and Pecos gambusia, as well as
the federally endangered Pecos
assiminea snail and the federally
threatened Pecos sunflower. The only
nonnative species of concern at
Diamond Y Spring is the red-rim
melania, which is only known to occur
in the upper watercourse.
Studies by Boghici (1997, p. v)
indicate that the spring flow at Diamond
Y Spring originates chiefly from the
Rustler aquifer waters underlying the
Delaware Basin to the northwest of the
spring outlets (Boghici and Van
Broekhoven 2001, p. 219). The Rustler
aquifer underlies an area of
approximately 1,200 sq km (480 sq mi)
encompassing most of Reeves County
and parts of Culberson, Pecos, Loving,
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49607
and Ward Counties (Boghici and Van
Broekhoven 2001, p. 219). Much of the
water contains high total dissolved
solids (Boghici and Van Broekhoven
2001, p. 219) making it difficult for
agricultural or municipal use; therefore,
the aquifer has experienced only limited
pumping in the past (Mace 2001, pp. 7–
9).
Other springs in the area may have
once provided habitat for the aquatic
species but limited information is
generally available on historic
distribution of the invertebrates. Leon
Springs, a large spring that historically
occurred about 14 km (9 miles)
upstream along Leon Creek, historically
discharged about 0.7 cms (25 cfs) in
1920, 0.5 cms (18 cfs) in the 1930s, 0.4
cms (14 cfs) in the 1940s, and no
discharge from 1958 to 1971 (Brune
1981, p. 359). Nearby groundwater
pumping to irrigate farm lands began in
1946, which lowered the contributing
aquifer by 40 m (130 feet) by the 1970s
and resulted in the loss of the spring.
The only circumstantial evidence that
any of the three invertebrates that occur
in nearby Diamond Y Spring may have
occurred in Leon Springs is that the
spring is within the same drainage and
an endemic fish, Leon Springs pupfish,
once occurred in both Diamond Y and
Leon Springs.
Comanche Springs is another large
historic spring located in the City of
Fort Stockton. Prior to the 1950s, this
spring discharged more than 1.2 cms (42
cfs) (Brune 1981, p. 358) and provided
habitat for rare species of fishes and
invertebrates. As a result of groundwater
pumping for agriculture, the spring
ceased flowing by 1962 (Brune 1981, p.
358), eliminating all aquatic-dependent
plants and animals (Scudday 1977, pp.
515–518; Scudday 2003, pp. 135–136).
Although we do not have data
confirming that Comanche Springs was
inhabited by all of the Diamond Y
Spring species, there is evidence that at
least the two snails (Diamond Y Spring
snail and Gonzales springsnail)
occurred there at some time in the past
(see Taxonomy, Distribution,
Abundance, and Habitat of Snails,
below).
Life History and Biology of Snails
The background information
presented in this section applies to all
four species of snails in these proposed
rules: Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail,
and Gonzales springsnail. All four of
these snails are in the family
Hydrobiidae and are strictly aquatic
with respiration occurring through an
internal gill. These hydrobiid snails
(snails in the family Hydrobiidae)
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typically reproduce several times during
the spring to fall breeding season
(Brown 1991, p. 292) and are sexually
dimorphic (males and females are
shaped differently), with females being
characteristically larger and longer-lived
than males. Snails in the Pyrgulopsis
genus (Phantom Cave snail) reproduce
through laying a single small egg
capsule deposited on a hard surface
(Hershler 1998, p. 14). The other three
snail species are ovoviviparous,
meaning the larval stage is completed in
the egg capsule, and upon hatching, the
snails emerge into their adult form
(Brusca and Brusca 1990, p. 759;
Hershler and Sada 2002, p. 256). The
lifespan of most aquatic snails is
thought to be 9 to 15 months (Taylor
1985, p. 16; Pennak 1989, p. 552).
All of these snails are presumably
fine-particle feeders on detritus (organic
material from decomposing organisms)
and periphyton (mixture of algae and
other microbes attached to submerged
surfaces) associated with the substrates
(mud, rocks, and vegetation) (Allan
1995, p. 83; Hershler and Sada 2002, p.
256; Lysne et al. 2007, p. 649). Dundee
and Dundee (1969, p. 207) found
diatoms (a group of single-celled algae)
to be the primary component in the
digestive tract, indicating they are a
primary food source.
These hydrobiid snails from west
Texas occur in mainly flowing water
habitats such as small springs, seeps,
marshes, spring pools, and their
outflows. Proximity to spring vents,
where water emerges from the ground,
plays a key role in the life history of
springsnails. Many springsnail species
exhibit decreased abundance farther
away from spring vents, presumably due
to their need for stable water chemistry
(Hershler 1994, p. 68; Hershler 1998, p.
11; Hershler and Sada 2002, p. 256;
Martinez and Thome 2006, p. 14).
Several habitat parameters of springs,
such as temperature, substrate type,
dissolved carbon dioxide, dissolved
oxygen, conductivity, and water depth
have been shown to influence the
distribution and abundance of other
related species of springsnails (O’Brien
and Blinn 1999, pp. 231–232; Mladenka
and Minshall 2001, pp. 209–211;
Malcom et al. 2005, p. 75; Martinez and
Thome 2006, pp. 12–15; Lysne et al.
2007, p. 650). Dissolved salts such as
calcium carbonate may also be
important factors because they are
essential for shell formation (Pennak
1989, p. 552). Hydrobiid snails as a
group are considered sensitive to water
quality changes, and each species is
usually found within relatively narrow
habitat parameters (Sada 2008, p. 59).
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Native fishes have been shown to prey
upon these snails (Winemiller and
Anderson 1997, pp. 209–210; Brown et
al. 2008, p. 489), but it is unknown to
what degree predatory pressure may
play a role in controlling population
abundances or influencing habitat use.
There are currently no nonnative fishes
in the springs where the species occur,
so there is no unnatural predation
pressure from fish suspected.
Because of their small size and
dependence on water, significant
dispersal (in other words, movement
between spring systems) does not likely
occur, although on rare occasions
aquatic snails have been transported by
becoming attached to the feathers and
feet of migratory birds (Roscoe 1955, p.
66; Dundee et al. 1967, pp. 89–90). In
general, the species have little capacity
to move beyond their isolated aquatic
environments.
Taxonomy, Distribution, Abundance,
and Habitat of Snails
Phantom Cave Snail (Pyrgulopsis texana
Pilsbry 1935)
The Phantom Cave snail was first
described by Pilsbry (1935, pp. 91–92).
It is a very small snail, measuring only
0.98 to 1.27 millimeters (mm) (0.04 to
0.05 inches (in)) long (Dundee and
Dundee 1969, p. 207). Until 2010, the
species was placed in the genus
Cochliopa (Dundee and Dundee 1969, p.
209; Taylor 1987, p. 40). Hershler et al.
(2010, pp. 247–250) reviewed the
systematics of the species and
transferred Phantom Cave snail to the
genus Pyrgulopsis after morphological
and mitochondrial DNA analysis.
Hershler et al. (2010, p. 251) also noted
some minimal differences in shell size
(individuals were smaller at East Sandia
Spring) and mitochondrial DNA
sequence variation among populations
of Phantom Cave snails in different
springs. The low level of variation
(small differences) among the
populations did not support recognizing
different conservation units for the
species. Hershler et al. (2010, p. 251)
expected this small difference among
the populations because of their
proximity (separated by 6 to 13 km (4
to 8 mi)) and the past connectedness of
the aquatic habitats by Toyah Creek that
would have allowed mixing of the
populations before human alterations
and declining flows. Based on these
published studies we conclude that
Phantom Cave snail is a listable entity
under the Act.
The Phantom Cave snail only occurs
in the four remaining desert spring
outflow channels associated with the
San Solomon Spring system (San
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Solomon, Phantom, Giffin, and East
Sandia springs). Hershler et al. (2010, p.
250) did not include Giffin Spring in
this species distribution, but
unpublished data from Lang (2011, p. 5)
confirms that the species is also found
in Giffin Spring outflows as well as the
other three springs in the San Solomon
Spring system. The geographic extent of
the historic range for the Phantom Cave
snail was likely not larger than the
present range, but the species may have
occurred in additional small springs
contained within the current range of
the San Solomon Spring system, such as
Saragosa and Toyah Springs. It likely
also had a larger distribution within
Phantom Lake Spring and San Solomon
Spring before the habitat there was
modified and reduced in conversion of
spring outflow channels into irrigation
ditches.
Within its current, limited range,
Phantom Cave snails can exist in very
high densities. Dundee and Dundee
(1969, pp. 207) described the abundance
of the Phantom Cave snails at Phantom
Lake Spring in 1968 as persisting ‘‘in
such tremendous numbers that the
bottom and sides of the canal appear
black from the cover of snails.’’ Today
the snails are limited to the small pool
at the mouth of Phantom Cave and
cannot be found in the irrigation canal
downstream. At San Solomon Spring,
Taylor (1987, p. 41) reported the
Phantom Cave snail was abundant and
generally distributed in the canals from
1965 to 1981. Density data and simple
population size estimates based on
underwater observations indicate there
may be over 3.8 million individuals of
this species at San Solomon Spring
(Bradstreet 2011, p. 55). Lang (2011)
also reported very high densities (not
total population estimates) of Phantom
Cave snails (with ± standard deviations):
San Solomon Spring from 2009
sampling in the main canal, 71,740 per
sq m (6,672 per sq ft; ±47,229 per sq m,
±4,393 per sq ft); Giffin Spring at road
crossing in 2001, 4,518 per sq m (420
per sq ft; ±4,157 per sq m, ±387 per sq
ft); East Sandia Spring in 2009, 41,215
per sq m (3,832 per sq ft; ±30,587 per
sq m, ±2,845 per sq ft); and Phantom
Lake Spring in 2009, 1,378 per sq m
(128 per sq ft; ±626 per sq m, ±58 per
sq ft). From these data, it is evident that
when conditions are favorable Phantom
Cave snails can reach tremendous
population sizes in very small areas.
Phantom Cave snails are found
concentrated near the spring source
(Hershler et al. 2010, p. 250) and can
occur as far as a few hundred meters
downstream of a large spring outlet like
San Solomon Spring. Despite its
common name, it has not been found
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within Phantom Cave proper, but only
within the outflow of Phantom Lake
Spring. Bradstreet (2011, p. 55) found
the highest abundances of Phantom
Cave snails at San Solomon Spring
outflows in the high-velocity areas in
the irrigation canals and the lowest
abundances in the San Solomon
´
Cienega. The species was not collected
´
from the newest constructed cienega in
2010. Habitat of the species is found on
both soft and firm substrates on the
margins of spring outflows (Taylor 1987,
p. 41). They are also commonly found
attached to plants, particularly in dense
stands of submerged vegetation (Chara
sp.). Field and laboratory experiments
have suggested Phantom Cave snails
prefer substrates harder and larger in
size (Bradstreet 2011, p. 91).
Phantom Springsnail (Tryonia cheatumi
Pilsbry 1935)
The Phantom springsnail was first
described by Pilsbry (1935, p. 91) as
Potamopyrgus cheatumi. The species
was later included in the genus Lyrodes
and eventually placed in the genus
Tryonia (Taylor 1987, pp. 38–39). It is
a small snail measuring only 2.9 to 3.6
mm (0.11 to 0.14 in) long (Taylor 1987,
p. 39). Systematic studies of Tryonia
snails in the Family Hydrobiidae using
mitochondrial DNA sequences and
morphological characters confirms the
species is a ‘‘true Tryonia,’’ in other
words, it is appropriately classified in
the genus Tryonia (Hershler et al. 1999,
p. 383; Hershler 2001, p. 6; Hershler et
al. 2011, pp. 5–6). Based on these
published studies, we conclude that
Phantom springsnail is a listable entity
under the Act.
The Phantom springsnail only occurs
in the four remaining desert spring
outflow channels associated with the
San Solomon Spring system (San
Solomon, Phantom, Giffin, and East
Sandia springs) (Taylor 1987, p. 40;
Allan 2011, p. 1; Lang 2011, entire). The
historic range for the Phantom
springsnail was likely not larger than
present, but the species may have
occurred in other springs within the San
Solomon Spring system, such as
Saragosa and Toyah Springs. It likely
also had a wider distribution within
Phantom Lake Spring and San Solomon
Spring before the habitat there was
modified and reduced.
Within its current, limited range,
Phantom springsnails can have
moderate densities of abundance, but
have never been recorded as high as the
Phantom Cave snail. In the 1980s,
Taylor (1987, p. 40) described Phantom
springsnails as abundant in the outflow
ditch several hundred meters
downstream of Phantom Lake Spring.
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The snails are now limited to low
densities in the small pool at the mouth
of Phantom Cave and cannot be found
in the irrigation canal downstream as it
does not have water (Allan 2009, p. 1).
Density data and simple population size
estimates based on underwater
observations indicate there may be over
460,000 individuals of this species at
San Solomon Spring (Bradstreet 2011, p.
55). Lang (2011) reports the following
densities (not population estimates) of
Phantom springsnails (with ± standard
deviations): San Solomon Spring from
2009 sampling in the main canal, 11,681
per sq m (1,086 per sq ft; ±11,925 per
sq m, ±1,109 per sq ft); Giffin Spring at
road crossing in 2001, 3,857 per sq m
(358 per sq ft; ±6,110 per sq m, ±568 per
sq ft); East Sandia Spring in 2009,
65,845 per sq m (6,123 per sq ft; ±60,962
per sq m, ±5,669 per sq ft); and Phantom
Lake Spring in 2009, 31,462 per sq m
(2,926 per sq ft; ±20,251 per sq m,
±1,883 per sq ft). Phantom springsnails
can reach high population sizes in very
small areas with favorable conditions.
Phantom springsnails are usually
found concentrated near the spring
source but once occurred as far as a few
hundred meters downstream when
Phantom Lake Spring was a large
flowing spring (Dundee and Dundee
1969, p. 207; Taylor 1987, p. 40). The
species is most abundant in the
swimming pool at Balmorhea State Park,
but has not been found in either of the
´
constructed cienegas at the Park in 2010
and 2011 (Allan 2011, p. 3; Bradstreet
2011, pp. 55). The species is found on
both soft and firm substrates on the
margins of spring outflows (Taylor 1987,
p. 41), and they are also commonly
found attached to plants, particularly in
dense stands of submerged vegetation
(Chara sp.).
Diamond Y Spring Snail (Pseudotryonia
adamantina Taylor 1987)
The Diamond Y Spring snail was first
described by Taylor (1987, p. 41) as
Tryonia adamantina. It is a small snail
measuring only 2.9 to 3.6 mm (0.11 to
0.14 in) long (Taylor 1987, p. 41).
Systematic studies (Hershler et al.1999,
p. 377; Hershler 2001, pp. 7, 16) of these
snails have been conducted using
mitochondrial DNA sequences and
morphological characters. These
analyses resulted in the Diamond Y
Spring snail being reclassified into the
new genus Pseudotryonia (Hershler
2001, p. 16). Based on these published
studies, we conclude that Diamond Y
Spring snail is a listable entity under the
Act.
Taylor (1985, p. 1; 1987, p. 38) was
the earliest to document the distribution
and abundance of aquatic snails in the
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Diamond Y Spring system, referencing
surveys from 1968 to 1984. In 1968, the
Diamond Y Spring snail was considered
abundant in the outflow of Diamond Y
Spring in the upper watercourse for
about 1.6 km (1 mi) downstream of the
spring head pool, but by 1984 the
species was present in only areas along
stream margins (near the banks) (Taylor
1985, p. 1). Average density estimates in
1984 at 12 of 14 sampled sites in the
upper watercourse ranged from 500 to
93,700 individuals per sq m (50 to 8,700
per sq ft), with very low densities in the
upstream areas near the headspring
(Taylor 1985, p. 25). However, the
Diamond Y Spring snail was largely
absent from the headspring and main
spring flow channel where it had been
abundant in 1968 surveys (Taylor 1985,
p. 13). Instead it was most common in
small numbers along the outflow stream
margins and lateral springs (Taylor
1985, pp. 13–15). Over time, the
distribution of the Diamond Y Spring
snail in the upper watercourse has
continued to recede so that it is no
longer found in the outflow channel at
all but may be restricted to small lateral
spring seeps disconnected from the
main spring flow channel (Landye 2000,
p. 1; Echelle et al. 2001, pp. 24–25).
Surveys by Lang (2011, pp. 7–8) in 2001
and 2003 found only 2 and 7
individuals, respectively, in the outflow
channel of Diamond Y Spring.
Additional surveys in 2009 and 2010
(Ladd 2010, p. 18; Lang 2011, p. 12) did
not find Diamond Y Spring snails in the
upper watercourse. However, neither
researcher surveyed extensively in the
lateral spring seeps downstream from
the main spring outflow.
The Diamond Y Spring snail was not
previously reported from the lower
watercourse until first detected there in
2001 at the outflow of Euphrasia Spring
(Lang 2011, p. 6). It was confirmed there
again in 2009 (Lang 2011, p. 13) and
currently occurs within at least the first
50 m (160 feet) in the outflow channel
of Euphrasia Spring (Ladd 2010, p. 18).
Ladd (2010, p. 37) roughly estimated the
total number of Diamond Y Spring
snails in the lower watercourse to be
about 35,000 individuals with the
highest density reported as 2,500
individuals per sq m (230 per sq ft).
Lang (2011, p. 13) estimated densities of
Diamond Y Spring snails in 2009 at
16,695 per sq m (1,552 per sq ft; ±18,212
per sq m, ±1,694 per sq ft) in Euphrasia
Spring outflow, which suggests a much
larger population than that estimated by
Ladd (2010, p. 37).
In summary, the Diamond Y Spring
snail was historically common in the
upper watercourse and absent from the
lower watercourse. Currently it is very
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rare in the upper watercourse and
limited to small side seeps (and may be
extirpated), and it occurs in the lower
watercourse in the outflow of Euphrasia
Spring. The historic distribution of this
species may have been larger than the
present distribution. Other area springs
nearby such as Leon and Comanche
Springs may have harbored the species.
There is one collection of very old, dead
shells of the species that was made from
Comanche Springs in 1998
(Worthington 1998, unpublished data)
whose identification was recently
confirmed as Diamond Y Spring snail
(Hershler 2011, pers. comm.). However,
because these springs have been dry for
more than four decades and shells can
remain intact for thousands of years, it
is impossible to know how old the
shells might be. Therefore, we are
unable to confirm if the recent historic
distribution included Comanche
Springs.
Habitat of the species is primarily soft
substrates on the margins of small
springs, seeps, and marshes in shallow
flowing water associated with emergent
bulrush (Scirpus americanus) and
saltgrass (Distichlis spicata) (Taylor
1987, p. 38; Echelle et al. 2001, p. 5).
Gonzales Springsnail (Tryonia
circumstriata Leonard and Ho 1960)
The Gonzales springsnail was first
described as a late Pleistocene fossil
record, Calipyrgula circumstriata, from
the Pecos River near Independence
Creek in Terrell County, Texas (Leonard
and Ho 1960, p. 126). The snail from
Diamond Y Spring area was first
described as Tryonia stocktonensis by
Taylor (1987, p. 37). It is a small snail,
measuring only 3.0 to 3.7 mm (0.11 to
0.14 in) long. Systematic studies later
changed the name to Tryonia
circumstriata, integrating it with the
fossilized snails from the Pecos River
(Hershler 2001, p. 7), and confirming
the species as a ‘‘true Tryonia,’’ in other
words, it is appropriately classified in
the genus Tryonia (Hershler et al. 2011,
pp. 5–6). Based on these published
studies, we conclude that Gonzales
springsnail is a listable entity under the
Act.
Taylor (1985, pp. 18–19; 1987, p. 38)
found Gonzales springsnail only in the
first 27 m (90 ft) of the outflow from
Euphrasia Spring. The species has been
consistently found in this short stretch
of spring outflow channel since then
(Echelle et al. 2001, p. 20; Lang 2011,
pp. 6, 13). Ladd (2010, pp. 23–24)
reported that Gonzales springsnails no
longer occurred in the lower
watercourse and had been replaced by
Diamond Y Spring snails. However,
reevaluation of voucher specimens
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collected by Lang (2011, p. 13)
concurrently in 2009 with those by
Ladd (2010, p. 14) confirmed the species
is still present in the Euphrasia Spring
outflow channel of the lower
watercourse.
Gonzales springsnail was first
reported in the upper watercourse in
1991 during collections from one site in
the Diamond Y Spring outflow and one
small side seep near the spring head
(Fullington and Goodloe 1991, p. 3).
The species has since been collected
from this area (Lang 2011, pp. 7–9), and
Echelle et al. (2001, p. 20) found it to
be the most abundant snail for the first
430-m (1,400-ft) downstream from the
spring head. Ladd (2010, p. 18) also
found Gonzales springsnail in the
outflow of Diamond Y Spring, but only
from 125 to 422 m (410 to 1,384 ft)
downstream of the spring head (Ladd
2011, pers. comm.). The Gonzales
springsnail appears to have replaced the
Diamond Y Spring snail in some of the
habitat in the upper watercourse (Brown
2008, p. 489) since 1991.
Taylor (1985, p. 19) calculated
densities for Gonzales springsnails in
the outflow of Euphrasia Spring in the
range of 50,480 to 85,360 individuals
per sq m (4,690 to 7,930 individuals per
sq ft) and estimated the population size
in that 27-m (90-ft) stretch to be at least
162,000 individuals and estimated the
total population of over one million
individuals as a reasonable estimate.
Lang (2011, p. 13) estimated the density
of Gonzales springsnails in the
Euphrasia Spring outflow to be 3,086
individuals per sq m (287 per sq ft;
±5,061 per sq m, ±471per sq ft). Ladd
(2010, p. 37) estimated the population of
Gonzales springsnails in the upper
watercourse to be only about 11,000
individuals.
As with the Diamond Y Spring snail,
the historic distribution of the Gonzales
springsnail may have been larger than
the present distribution. Other area
springs nearby such as Leon and
Comanche Springs may have harbored
the species. There is one collection of
dead shells of the species that was made
from Comanche Springs in 1998
(Worthington 1998, unpublished data)
whose identification was recently
confirmed as Gonzales springsnail
(Hershler 2011, pers. comm.). However,
because these springs have been dry for
more than four decades and shells can
remain intact for thousands of years, it
is impossible to know how old the
shells might be. Therefore, we are
unable to confirm if the recent historic
distribution included Comanche
Springs.
Habitat of the species is primarily soft
substrates on the margins of small
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springs, seeps, and marshes in shallow
flowing water associated with emergent
bulrush and saltgrass (Taylor 1987, p.
38; Echelle et al. 2001, p. 5).
Life History, Biology, and Habitat of
Amphipods
The background information
presented here applies to both species of
amphipods in these proposed rules:
diminutive amphipod and Pecos
amphipod. These amphipods, in the
family Gammaridae, are small
freshwater inland crustaceans
sometimes referred to as freshwater
shrimp. Gammarids commonly inhabit
shallow, cool, well-oxygenated waters of
streams, ponds, ditches, sloughs, and
springs (Smith 2001, p. 574). These
bottom-dwelling amphipods feed on
algae, submergent vegetation, and
decaying organic matter (Smith 2001, p.
572). Amphipod eggs are held within a
marsupium (brood pouch) within the
female’s exoskeleton (Smith 2001, p.
573). Most amphipods complete their
life cycle in 1 year and breed from
February to October, depending on
water temperature (Smith 2001, p. 572).
Amphipods form breeding pairs that
remain attached for 1 to 7 days at or
near the substrate while continuing to
feed and swim (Bousfield 1989, p.
1721). They can produce from 15 to 50
offspring, forming a ‘‘brood.’’ Most
amphipods produce one brood, but
some species produce a series of broods
during the breeding season (Smith 2001,
p. 573).
These two species, diminutive
amphipod and Pecos amphipod, are part
of a related group of amphipods,
referred to as the Gammarus pecos
species complex, that are restricted to
desert spring systems from the Pecos
River Basin in southeast New Mexico
and west Texas (Cole 1985, p. 93; Lang
et al. 2003, p. 47; Gervasio et al. 2004,
p. 521). Similar to the snails, it is
thought that these freshwater
amphipods are derived from a
widespread ancestral marine amphipod
that was isolated inland during the
recession of the Late Cretaceous sea,
about 66 million years ago (Holsinger
1967, pp. 125–133; Lang et al. 2003, p.
47). They likely evolved into distinct
species during recent dry periods (since
the Late Pleistocene, about 100,000
years ago) through allopatric speciation
(that is, speciation by geographic
separation) following separation and
isolation in the remnant aquatic habitats
associated with springs (Gervasio et al.
2004, p. 528).
Amphipods in the Gammarus pecos
species complex only occur in desert
spring outflow channels on substrates,
often within interstitial spaces on and
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underneath rocks and within gravels
(Lang et al. 2003, p. 49) and are most
commonly found in microhabitats with
flowing water. They are also commonly
found in dense stands of submerged
vegetation (Cole 1976, p. 80). Because of
their affinity for constant water
temperatures, they are most common in
the immediate spring outflow channels,
usually only a few hundred meters
downstream of spring outlets.
Amphipods play important roles in
the processing of nutrients in aquatic
ecosystems and are also considered
sensitive to changes in aquatic habitat
conditions (for example, stream
velocities, light intensity, zooplankton
availability, and the presence of heavy
metals) and are often considered
ecological indicators of ecosystem
health and integrity (Covich and Thorpe
1991, pp. 672–673, 679; Lang et al.
2003, p. 48). Water chemistry
parameters, such as salinity, pH, and
temperature, are also key components to
amphipod habitats (Covich and Thorpe
1991, pp. 672–673).
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Taxonomy, Distribution, and
Abundance of Amphipods
Diminutive Amphipod (Gammarus
hyalleloides Cole 1976)
W.L. Minckley first collected the
diminutive amphipod from Phantom
Lake Spring in the San Solomon Spring
system in 1967, and the species was first
formally described by Cole (1976, pp.
80–85). The name comes from the
species being considered the smallest of
the known North American freshwater
Gammarus amphipods. Adults generally
range in length from 5 to 8 mm (0.20 to
0.24 in).
There has been some disparity in the
literature regarding the taxonomic
boundaries for the amphipods from the
San Solomon Spring system. In Cole’s
(1985, pp. 101–102) description of the
Gammarus pecos species complex of
amphipods based solely on
morphological measurements, he
considered the diminutive amphipod to
be endemic only to Phantom Lake
Spring, and amphipods from San
Solomon and Diamond Y Springs were
both considered to be the Pecos
amphipod (G. pecos). This study did not
include samples of amphipods from
East Sandia or Giffin Springs. However,
allozyme electrophoresis data on genetic
variation strongly support that the
populations from the San Solomon
Spring system form a distinct group
from the Pecos amphipod at Diamond Y
Spring (Gervasio et al. 2004, pp. 523–
530). Based on these data, we consider
the Pecos amphipod to be limited to the
Diamond Y Spring system.
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The results of these genetic studies
also suggested that the three Gammarus
amphipod populations from San
Solomon, Giffin, and East Sandia
Springs are a taxonomically unresolved
group differentiated from the
diminutive amphipod at Phantom Lake
Spring (Gervasio et al. 2004, pp. 523–
530). Further genetic analysis using
mitochondrial DNA (mtDNA) by Seidel
et al. (2009, p. 2309) also indicates that
the diminutive amphipod may be
limited to Phantom Lake Spring and the
Gammarus species at the other three
springs should be considered a new and
undescribed species. However, the
extent of genetic divergence measured
between these populations is not
definitive. For example, the 19-base pair
divergence between the population at
Phantom Lake Spring and the other San
Solomon Spring system populations
(Seidel et al. 2009, Figure 3, p. 2307)
represents about 1.7 percent mtDNA
sequence divergence (of the 1,100 base
pairs of the mitochondrial DNA
sequenced (using the cytochrome c
oxidase I (COI) gene). This is a relatively
low level of divergence to support
species separation, as a recent review of
a multitude of different animals (20,731
vertebrates and invertebrates) suggested
that the mean mtDNA distances (using
the COI gene) between subspecies is
3.78 percent (±0.16) divergence and
between species is 11.06 percent (±0.53)
divergence (Kartavtsev 2011, pp. 57–58).
Recent evaluations of species
boundaries of amphipods from China
suggest mtDNA genetic distances of at
least 4 percent were appropriate to
support species differentiation, and the
species they described all exceeded 15
percent divergence (Hou and Li 2010, p.
220). In addition, no species
descriptions using morphological or
ecological analysis have been completed
for these populations, which would be
important information in any taxonomic
revision (Hou and Li 2010, p. 216).
Therefore, the data available does not
currently support taxonomically
separating the amphipod population at
Phantom Lake Spring from the
populations at San Solomon, Giffin, and
East Sandia Springs into different
listable entities under the Act. So, for
the purposes of these proposed rules,
based on the best available scientific
information, we are including all four
populations of Gammarus amphipods
from the San Solomon Spring system as
part of the Gammarus hyalleloides
species (diminutive amphipod), and we
consider diminutive amphipod a
listable entity under the Act. We
recognize that the taxonomy of these
populations could change as additional
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information is collected and further
analyses are published.
The diminutive amphipod only
occurs in the four springs from the San
Solomon Spring system (Gervasio et al.
2004, pp. 520–522). There is no
available information that the species’
historic distribution was larger than the
present distribution, but other area
springs (such as Saragosa, Toyah, and
West Sandia Springs) may have
contained the species. However,
because these springs have been dry for
many decades, if the species historically
occurred there, they are now extirpated.
There is no opportunity to determine
the full extent of the historic
distribution of these amphipods because
of the lack of historic surveys and
collections.
Within its limited range, diminutive
amphipod can be very abundant. For
example, in May 2001, Lang et al. (2003,
p. 51) estimated mean densities at San
Solomon, Giffin, and East Sandia
Springs of 6,833 amphipods per sq m
(635 per sq ft; standard deviation ±5,416
per sq m, ±504 per sq ft); 1,167
amphipods per sq m (108 per sq ft; ±730
per sq m, ±68 per sq ft), and 4,625
amphipods per sq m (430 per sq ft; ±804
per sq m, ±75 per sq ft), respectively. In
2009 Lang (2011, p. 11) reported the
density at Phantom Lake Spring as 165
amphipods per sq m (15 per sq ft; ±165
per sq m, ±15 per sq ft).
Pecos Amphipod (Gammarus pecos
Cole and Bousfield 1970)
The Pecos amphipod was first
collected in 1964 from Diamond Y
Spring and was described by Cole and
Bousfield (1970, p. 89). Cole (1985, p.
101) analyzed morphological
characteristics of the Gammarus pecos
species complex and suggested the
Gammarus amphipod from San
Solomon Spring should also be
included as Pecos amphipod. However,
updated genetic analyses based on
allozymes (Gervasio et al. 2004, p. 526)
and mitochondrial DNA (Seidel et al.
2009, p. 2309) have shown that Pecos
amphipods are limited in distribution to
the Diamond Y Spring system. In
addition, Gervasio et al. (2004, pp. 523,
526) evaluated amphipods from three
different locations within the Diamond
Y Spring system and found no
significant differences in genetic
variation, indicating they all
represented a single species. Based on
these published studies, we conclude
that Pecos amphipod is a listable entity
under the Act.
The Pecos amphipod is generally
found in all the flowing water habitats
associated with the outflows of springs
and seeps in the Diamond Y Spring
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system (Echelle et al. 2001, p. 20; Lang
et al. 2003, p. 51; Allan 2011, p. 2; Lang
2011, entire). There is no available
information to determine if the species’
historic distribution was larger than the
present distribution. Other area springs,
such as Comanche and Leon Springs,
may have contained the same or similar
species of amphipod, but because these
springs have been dry for many decades
(Brune 1981, pp. 256–263, 382–386),
there is no opportunity to determine the
potential historic occurrence of
amphipods. Pecos amphipods are often
locally abundant, with reported mean
densities ranging from 2,208 individuals
per sq m (205 per sq ft; ±1,585 per sq
m, ±147 per sq ft) to 8,042 individuals
per sq m (748 per sq ft; ±7,229 per sq
m, ±672 per sq ft) (Lang et al. 2003, p.
51).
Summary of Factors Affecting the
Species
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Section 4 of the Act (16 U.S.C. 1533),
and its implementing regulations at 50
CFR part 424, set forth the procedures
for adding species to the Federal Lists
of Endangered and Threatened Wildlife
and Plants. Under section 4(a)(1) of the
Act, the Service determines whether a
species is endangered or threatened
because of any of the following five
factors: (A) The present or threatened
destruction, modification, or
curtailment of its habitat or range; (B)
overutilization for commercial,
recreational, scientific, or educational
purposes; (C) disease or predation; (D)
the inadequacy of existing regulatory
mechanisms; and (E) other natural or
manmade factors affecting its continued
existence. Listing actions may be
warranted based on any of the above
threat factors, singly or in combination.
Each of these factors is discussed below.
Based on the similarity in geographic
ranges and threats to habitats, we have
divided this analysis into two sections,
one covering the three species from the
San Solomon Spring system and then a
second analysis covering the three
species from the Diamond Y Spring
system. After each analysis we provide
proposed determinations for each
species.
San Solomon Spring Species—Phantom
Cave Snail, Phantom Springsnail, and
Diminutive Amphipod
The following analysis applies to the
three species that occur in the San
Solomon Spring system in Reeves and
Jeff Davis Counties, Texas: Phantom
Cave snail, Phantom Lake springsnail,
and diminutive amphipod.
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A. The Present or Threatened
Destruction, Modification, or
Curtailment of Their Habitat or Range
(San Solomon Spring Species)
The three species in the San Solomon
Spring system are threatened by the past
and future destruction of their habitat
and reduction in their range. The
discussion below evaluates the stressors
of: (1) Spring flow declines; (2) water
quality changes and contamination; and
(3) modification of spring channels.
Spring Flow Declines
The primary threat to the continued
existence of the San Solomon Spring
species is the degradation and potential
future loss of aquatic habitat (flowing
water from the spring outlets) due to the
decline of groundwater levels in the
aquifers that support spring surface
flows. Habitat for these species is
exclusively aquatic and completely
dependent on spring flows emerging to
the surface from underground aquifer
sources. Spring flows throughout the
San Solomon Spring system have and
continue to decline in flow rate, and as
spring flows decline, available aquatic
habitat is reduced and altered. If one
spring ceases to flow continually, all
habitats for the Phantom Cave snail,
Phantom Lake springsnail, and
diminutive amphipod are lost, and the
populations will be extirpated. If all of
the springs lose consistent surface
flows, all natural habitats for these
aquatic invertebrates will be gone, and
the species will become extinct.
The springs do not have to cease
flowing completely to have an adverse
effect on invertebrate populations. The
small size of the spring outflows at
Phantom, Giffin, and East Sandia
Springs makes them particularly
susceptible to changes in water
chemistry, increased water temperatures
during the summer and freezing in the
winter. Because these springs are small,
any reductions in the flow rates from
the springs can reduce the quantity and
quality of available habitat for the
species, which decreases the number of
individuals available and increases the
risk of extinction. Water temperatures
and chemical factors in springs, such as
dissolved oxygen and pH, do not
typically fluctuate to a large degree
(Hubbs 2001, p. 324), and invertebrates
are narrowly adapted to spring
conditions and are sensitive to changes
in water quality (Hershler 1998, p. 11;
Sada 2008, p. 69). Spring flow declines
can lead to the degradation and loss of
aquatic invertebrate habitat and present
a substantial threat to these species.
The precise reason for the declining
spring flows remains uncertain, but it is
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presumed to be related to a combination
of groundwater pumping, mainly for
agricultural irrigation, and a lack of
natural recharge to the supporting
aquifers due to limited rainfall and
geologic circumstances that prevent
recharge. In addition, future changes in
the regional climate are expected to
exacerbate declining flows. The San
Solomon Spring system historically may
have had a combined discharged of
about 2.8 cms (100 cfs) or 89 million
cubic meters per year (cmy) (72,000
acre-feet per year (afy)) (Beach et al.
2004, p. 4–53), while today the total
discharge is roughly one-third that
amount. Some smaller springs, such as
Saragosa, Toyah, and West Sandia
Springs have already ceased flowing
and likely resulted in the extirpation of
local populations of these species
(assuming they were present there
historically). The most dramatic recent
decline in flow rates have been observed
at Phantom Lake Spring, which is the
highest elevation spring in the system
and, not unexpectedly, was the first
large spring to cease flowing.
Phantom Lake Spring was a
´
historically large desert cienega with a
pond of water more than several acres
in size (Hubbs 2001, p. 307). The spring
outflow is at about 1,080 m (3,543 ft) in
elevation and previously provided
habitat for the endemic native aquatic
fauna. The outflow from Phantom Lake
Spring was originally isolated from the
other surface springs in the system, as
the spring discharge quickly recharged
back underground (Brune 1981, p. 258).
Human modifications to the spring
outflow captured and channeled the
spring water into a canal system for use
by local landowners and irrigation by
the local water users (Simonds 1996, p.
3). The outflow canal joins the main San
Solomon canal within Balmorhea State
Park. Despite the significant habitat
alterations, the native aquatic fauna
(including these three invertebrates)
have persisted, though in much reduced
numbers of total individuals, in the
small pool of water at the mouth of the
spring.
Flows from Phantom Lake Spring
have been steadily declining since
measurements were first taken in the
1930s (Brune 1981, p. 259). Discharge
data have been recorded from the spring
at least six to eight times per year since
the 1940s by the U.S. Geological Survey,
and the record shows a steady decline
of base flows from greater than 0.3 cms
(10 cfs) in the 1940s to 0 cms (0 cfs) in
1999 (Service 2009b, p. 23). The data
also show that the spring can have
short-term flow peaks resulting from
local rainfall events in the Davis
Mountains (Sharp et al. 1999, p. 4;
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Chowdhury et al. 2004, p. 341). These
flow peaks are from fast recharge of the
local aquifer system and discharge
through the springs. The flow peaks do
not come from direct surface water
runoff because the outflow spring is
within an extremely small surface
drainage basin that is not connected to
surface drainage basins from the Davis
Mountains upslope. However, after each
flow increase, the base flow has
returned to the same declining trend
within a few months.
Exploration of Phantom Cave by cave
divers has led to additional information
about the nature of the spring and its
supporting aquifer. Over 2,440 m (8,000
ft) of the underwater cave have been
mapped. Beyond the entrance, the cave
is a substantial conduit that transports
a large volume of water, in the 0.6 to 0.7
cms (20 to 25 cfs) range, generally from
the northwest to the southeast (Tucker
2009, p. 8), consistent with regional
flow pattern hypothesis (Chowdhury et
al. 2004, p. 319). The amount of water
measured is in the range of the rate of
flow at San Solomon Spring and, along
with water chemistry data (Chowdhury
et al. 2004, p. 340), confirms that the
groundwater flowing by Phantom Lake
Spring likely discharges at San Solomon
Spring. Tucker (2009, p. 8) recorded a
1-m (3-ft) decline in the water surface
elevation within the cave between 1996
and 2009 indicating a decline in the
amount of groundwater flowing through
Phantom Cave.
Phantom Lake Spring ceased flowing
in about 1999 (Allan 2000, p. 51;
Service 2009b, p. 23). All that remained
of the spring outflow habitat was a small
pool of water with about 37 sq m (400
sq ft) of wetted surface area. Hubbs
(2001, pp. 323–324) documented
changes in water quality (increased
temperature, decreased dissolved
oxygen, and decreased coefficient of
variation for pH, turbidity, ammonia,
and salinity) and fish community
structure at Phantom Lake Spring
following cessation of natural flows. In
May 2001, the U.S. Bureau of
Reclamation, in cooperation with the
Service, installed an emergency pump
system to bring water from within the
cave to the springhead in order to
prevent complete drying of the pool and
loss of the federally listed endangered
fishes and candidate invertebrates that
occur there. Habitat for the San
Solomon Spring system invertebrates
continues to be maintained at Phantom
Lake Spring, and in 2011 the small pool
was enlarged, nearly doubling the
amount of aquatic habitat available for
the species (Service 2012, entire).
The three San Solomon Spring
species have maintained minimal
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populations at Phantom Lake Spring
despite the habitat being drastically
modified from its original state and
being maintained by a pump system
since 2000. However, because the
habitat is sustained with a pump
system, the risk of extirpation of these
populations continues to be extremely
high from the potential for a pump
failure or some unforeseen event. For
example, the pump system failed
several times during 2008, resulting in
stagnant pools and near drying
conditions, placing severe stress on the
invertebrate populations (Allan 2008,
pp. 1–2). Substantial efforts were
implemented in 2011 to improve the
reliability of the pump system and the
quality of the habitat (Service 2012, pp.
5–9). However, because the habitat is
completely maintained by artificial
means, the potential loss of the
invertebrate population will continue to
be an imminent threat of high
magnitude to the populations at
Phantom Lake Spring.
Although long-term data for San
Solomon Spring flows are limited, they
appear to have declined somewhat over
the history of record, though not as
severely as Phantom Lake Spring
(Schuster 1997, pp. 86–90; Sharp et al.
1999, p. 4). Some recent declines in
overall flow have likely occurred due to
drought conditions and declining
aquifer levels (Sharp et al. 2003, p. 7).
San Solomon Spring discharges are
usually in the 0.6 to 0.8 cms (25 to 30
cfs) range (Ashworth et al. 1997, p. 3;
Schuster 1997, p. 86) and are consistent
with the theory that the water bypassing
Phantom Lake Spring discharges at San
Solomon Spring.
In Giffin Spring, Brune (1981, pp.
384–385) documented a gradual decline
in flow between the 1930s and 1970s,
but the discharge has remained
relatively constant since that time, with
outflow of about 0.08 to 0.1 cms (3 to
4 cfs) (Ashworth et al. 1997, p. 3; U.S.
Geological Survey 2012, p. 2). Although
the flow rates from Giffin Spring appear
to be steady in recent years, its small
size makes the threat of spring flow loss
imminent and of high magnitude
because even a small decline in flow
rate may have substantial impacts on
the habitat provided by the spring flow.
Also, it would only take a small decline
in spring flow rates to result in
desiccation of the spring.
Brune (1981, p. 385) noted that flows
from Sandia Springs (combining East
and West Sandia Springs) were
declining up until 1976. East Sandia
may be very susceptible to over
pumping of the local aquifer in the
nearby area that supports the small
spring. Measured discharges in 1995
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and 1996 ranged from 0.013 to 0.12 cms
(0.45 to 4.07 cfs) (Schuster 1997, p. 94).
Like the former springs of West Sandia
and Saragosa, which also originated in
shallow aquifers and previously ceased
flowing (Ashworth et al. 1997, p. 3),
East Sandia Spring’s very small volume
of water makes it particularly at risk of
failure from any local changes in
groundwater conditions.
The exact causes for the decline in
flow from the San Solomon Spring
system are unknown. Some of the
possible reasons, which are likely acting
together, include groundwater pumping
of the Salt Basin Bolson aquifer areas
west of the springs, long-term climatic
changes, or changes in the geologic
structure that permits regional
interbasin flow of groundwater (Sharp et
al. 1999, p. 4; Sharp et al. 2003, p. 7).
Studies indicate that the base flows
originate from ancient waters to the
west (Chadhury et al. 2004, p. 340) and
that many of the aquifers in west Texas
receive little to no recharge from
precipitation (Scanlon et al. 2001, p. 28)
and are influenced by regional
groundwater flow patterns (Sharp 2001,
p. 41).
Ashworth et al. (1997, entire)
provided a brief study to examine the
cause of declining spring flows in the
San Solomon Spring system. They
concluded that declines in spring flows
in the 1990s were more likely the result
of diminished recharge due to the
extended dry period rather than from
groundwater pumpage (Ashworth et al.
1997, p. 5). Although possibly a factor,
drought is unlikely the only reason for
the declines because the drought of
record in the 1950s had no measurable
effect on the overall flow trend at
Phantom Lake Spring (Allan 2000, p. 51;
Sharp 2001, p. 49) and because the
contributing aquifer receives virtually
no recharge from most precipitation
events (Beach et al. 2004, pp. 6–9, 8–9).
Also, Ashworth et al. (1997, entire) did
not consider the effects of the regional
flow system in relation to the declining
spring flows. Further, an assessment of
the springs near Balmorhea by Sharp
(2001, p. 49) concluded that irrigation
pumpage since 1945 has caused many
springs in the area to cease flowing,
lowering water-table elevations and
creating a cone of depression in the area
(that is, a lowering of the groundwater
elevation around pumping areas).
The Texas Water Development Board
(2005, entire) completed a
comprehensive study to ascertain the
potential causes of spring flow declines
in the San Solomon Spring system,
including a detailed analysis of historic
regional groundwater pumping trends.
The study was unable to quantify direct
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correlations between changes in
groundwater pumping in the
surrounding counties and spring flow
decline over time at Phantom Lake
Spring (Texas Water Development
Board 2005, p. 93). However, they
suggested that because of the large
distance between the source
groundwater and the springs and the
long travel time for the water to reach
the spring outlets, any impacts of
pumping are likely to be reflected much
later in time (Texas Water Development
Board 2005, p. 92). The authors did
conclude that groundwater pumping
will impact groundwater levels and
spring flow rates if it is occurring
anywhere along the flow path system
(Texas Water Development Board 2005,
p. 92).
Groundwater pumping for irrigated
agriculture has had a measurable effect
on groundwater levels in the areas that
likely support the spring flows at the
San Solomon Spring system. For
example, between the 1950s and 2000
the Salt Basin Bolson aquifer in Lobo
Flat fell in surface elevation in the range
of 15 to 30 m (50 to near 100 ft), and
in Wild Horse Flat from 6 to 30 m (20
to 50 ft) (Angle 2001, p. 248; Beach et
al. 2004, p. 4–9). Beach et al. (2004, p.
4–10) found significant pumping,
especially in the Wild Horse Flat area,
locally influences flow patterns in the
aquifer system. The relationship of
regional flow exists because Wild Horse
Flat is located in the lowest part of the
hydraulically connected Salt Basin
Bolson aquifer, and next highest is
Lobo, followed by Ryan Flat, which is
at the highest elevations (Beach et al.
2004, p. 9–32). This means that water
withdrawn from any southern part of
the basin (Ryan and Lobo Flats) may
affect the volume of water discharging
out of Wild Horse Flat toward the
springs. Because these bolson aquifers
have little to no direct recharge from
precipitation (Beach et al. 2004, pp. 6–
9, 8–9), these groundwater declines can
be expected to permanently reduce the
amount of water available for discharge
in the springs in the San Solomon
Spring system. This is evidenced by the
marked decline of groundwater flow out
of the Wild Horse Flat toward the
southeast (the direction of the springs)
(Beach et al. 2004, p. 9–27). Based on
this information, it appears reasonable
that past and future groundwater
withdrawals in the Salt Basin Bolson
aquifers are likely one of the causes of
decreased spring flows in the San
Solomon Spring system.
Groundwater pumping withdrawals
in Culberson, Jeff Davis, and Presidio
Counties in the Salt Basin Bolson
aquifer are expected to continue in the
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future mainly to support irrigated
agriculture (Region F Water Planning
Group 2010, pp. 2–16–2–19) and will
result in continued lowering of the
groundwater levels in the Salt Basin
Bolson aquifer. The latest plans from
Groundwater Management Area 4 (the
planning group covering the relevant
portion of the Salt Basin Bolson aquifer)
expect over 69 million cubic m (56,000
af) of groundwater pumping per year for
the next 50 years, resulting in an
average drawdown of 22 to 24 m (72 to
78 feet) in the West Texas Bolsons (Salt
Basin) aquifer by 2060 (Adams 2010, p.
2; Oliver 2010, p. 7). There have been
no studies evaluating the effects of this
level of anticipated drawdown on spring
flows. The aquifer in the Wild Horse
Flat area (the likely spring source) can
range from 60 to 300 m (200 to 1,000 ft)
thick. So although it is impossible to
determine precisely, we anticipate the
planned level of groundwater
drawdown will likely result in
continued future declines in spring flow
rates in the San Solomon Spring system.
Another reason that spring flows may
be declining is from an increase in the
frequency and duration of local and
regional drought associated with
climatic changes. The term ‘‘climate’’
refers to the mean and variability of
different types of weather conditions
over time, with 30 years being a typical
period for such measurements, although
shorter or longer periods also may be
used (IPCC 2007a, p. 78). The term
‘‘climate change’’ thus refers to a change
in the mean or variability of one or more
measures of climate (e.g., temperature or
precipitation) that persists for an
extended period, typically decades or
longer, whether the change is due to
natural variability, human activity, or
both (IPCC 2007a, p. 78).
Although the bulk of spring flows
appear to originate from ancient water
sources with limited recent recharge,
any decreases in regional precipitation
patterns due to prolonged drought will
further stress groundwater availability
and increase the risk of diminishment or
drying of the springs. Drought affects
both surface and groundwater resources
and can lead to diminished water
quality (Woodhouse and Overpeck
1998, p. 2693) in addition to reducing
groundwater quantities. Lack of rainfall
may also indirectly affect aquifer levels
by resulting in an increase in
groundwater pumping to offset water
shortages from low precipitation (Mace
and Wade 2008, p. 665).
Recent drought conditions may be
indicative of more common future
conditions. The current, multiyear
drought in the western United States,
including the Southwest, is the most
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severe drought recorded since 1900
(Overpeck and Udall 2010, p. 1642). In
2011, Texas experienced the worst
annual drought since recordkeeping
began in 1895 (NOAA 2012, p. 4), and
only one other year since 1550 (the year
1789) was as dry as 2011 based on treering climate reconstruction (NOAA
2011, pp. 20–22). In addition, numerous
climate change models predict an
overall decrease in annual precipitation
in the southwestern United States and
northern Mexico.
Future global climate change may
result in increased magnitude of
droughts and further contribute to
impacts on the aquatic habitat from
reduction of spring flows. There is high
confidence that many semi-arid areas
like the western United States will
suffer a decrease in water resources due
to ongoing climate change (IPCC 2007b,
p. 7; Karl et al. 2009, pp. 129–131), as
a result of less annual mean
precipitation. Milly et al. (2005, p. 347)
also project a 10 to 30 percent decrease
in precipitation in mid-latitude western
North America by the year 2050 based
on an ensemble of 12 climate models.
Even under lower greenhouse gas
emission scenarios, recent projections
forecast a 10 percent decline in
precipitation in western Texas by 2080
to 2099 (Karl et al. 2009, pp. 129–130).
Assessments of climate change in west
Texas suggest that the area is likely to
become warmer and at least slightly
drier (Texas Water Development Board
2008, pp. 22–25).
The potential effects of future climate
change could reduce overall water
availability in this region of western
Texas and compound the stressors
associated with declining flows from the
San Solomon Spring system. As a result
of the effects of increased drought,
spring flows could decline indirectly as
a result of increased pumping of
groundwater to accommodate human
needs for additional water supplies
(Mace and Wade 2008, p. 664; Texas
Water Development Board 2012c, p.
231).
In conclusion, the Phantom Cave
snail, Phantom springsnail, and
diminutive amphipod all face
significant threats from the current and
future loss of habitat associated with
declining spring flows. Some springs in
the San Solomon Spring system have
already gone dry, and aquatic habitat at
Phantom Lake Spring has not yet been
lost only because of the maintenance of
a pumping system. While the sources of
the stress of declining spring flows are
not known for certain, the best available
scientific information indicates that it is
the result of a combination of factors
including past and current groundwater
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pumping, the complex hydrogeologic
conditions that produce these springs
(ancient waters from a regional flow
system), and climatic changes
(decreased precipitation and recharge).
The threat of habitat loss from declining
spring flows affects all four of the
remaining populations, as all are at risk
of future loss from declining spring
flows. All indications are that the source
of this threat will persist into the future
and will result in continued degradation
of the species’ habitats, putting the
Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
at a high risk of extinction.
Water Quality Changes and
Contamination
Another potential factor that could
impact habitat of the San Solomon
Spring species is the potential
degradation of water quality from point
and nonpoint pollutant sources. This
can occur either directly into surface
water or indirectly through
contamination of groundwater that
discharges into spring run habitats used
by the species. The primary threat for
contamination in these springs comes
from herbicide and pesticide use in
nearby agricultural areas. There are no
oil and gas operations in the area
around the San Solomon Spring system.
These aquatic invertebrates are
sensitive to water contamination.
Hydrobiid snails as a group are
considered sensitive to water quality
changes, and each species is usually
found within relatively narrow habitat
parameters (Sada 2008, p. 59).
Amphipods generally do not tolerate
habitat desiccation (drying), standing
water, sedimentation, or other adverse
environmental conditions; they are
considered very sensitive to habitat
degradation (Covich and Thorpe 1991,
pp. 676–677).
The exposure of the spring habitats to
pollutants is limited because most of the
nearby agricultural activity mainly
occurs in downstream areas where
herbicide or pesticide use would not
likely come into contact with the
species or their habitat in upstream
spring outlets. To ensure these
pollutants do not affect these spring
outflow habitats, their use has been
limited in an informal protected area in
the outflows of San Solomon and Giffin
Springs (Service 2004, pp. 20–21). This
area was developed in cooperation with
the U.S. Environmental Protection
Agency and the Texas Department of
Agriculture. While there are more
agriculture activities far upstream in the
aquifer source area, there is no
information indicating concerns about
contaminants from those sources.
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In addition, Texas Parks and Wildlife
Department completed a Habitat
Conservation Plan and received an
incidental take permit (Service 2009a,
entire) in 2009 under section 10(a)(1)(B)
(U.S.C. 1539(a)(1)(B)) of the Act for
management activities at Balmorhea
State Park (Texas Parks and Wildlife
Department 1999, entire). The three
aquatic invertebrate candidate species
from the San Solomon Spring system
were all included as covered species in
the permit (Service 2009a, pp. 20–22).
This permit authorizes ‘‘take’’ of the
invertebrates (which were candidates at
the time of issuance) in the State Park
for ongoing management activities while
minimizing impacts to the aquatic
species. The activities included in the
Habitat Conservation Plan are a part of
Texas Parks and Wildlife Department’s
operation and maintenance of the State
Park, including the drawdowns
associated with cleaning the swimming
pool and vegetation management within
´
the refuge canal and cienega. The
Habitat Conservation Plan also calls for
restrictions and guidelines for chemical
use in and near aquatic habitats to avoid
and minimize impacts to the three
aquatic invertebrate species (Service
2009a, pp. 9, 29–32).
Because the use of potential
pollutants is very limited within the
range of the San Solomon Spring
species, at this time we do not find that
the Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
are at a heightened risk of extinction
from water quality changes or
contamination.
Modification of Spring Channels
´
The natural cienega habitats of the
San Solomon Spring system have been
heavily altered over time primarily to
accommodate agricultural irrigation.
Most significant was the draining of
wetland areas and the modification of
spring outlets to develop the water
resources for human use. San Solomon
and Phantom Lake Springs have been
altered the most severely through
capture and diversion of the spring
outlets into concrete irrigation canals.
Giffin Spring appears to have been
dredged in the past, and the outflow is
now immediately captured in highbanked, earthen-lined canals. The
outflow of East Sandia Spring does not
appear to have been altered in an
appreciable way, but it may have been
minimally channelized to connect the
spring flow to the irrigation canals.
The Reeves County Water
Improvement District No. 1 maintains
an extensive system of about 100 km (60
mi) of irrigation canals that now provide
only minimal aquatic habitat for the
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49615
invertebrate species near the spring
sources. Most of the canals are concretelined with high water velocities and
little natural substrate available. Many
of the canals are also regularly
dewatered as part of the normal water
management operations. Before the
canals were constructed, the suitable
habitat areas around the spring
openings, particularly at San Solomon
Spring, were much larger in size. The
conversion of the natural aquatic mosaic
of habitats into linear irrigation canals
represents a past impact resulting in
significant habitat loss and an increase
in the overall risk of extinction by
lowering the amount of habitat available
to the species and, therefore, lowering
the overall number of individuals in the
populations affected. These reductions
in population size result in an increase
in the risk of extirpation of local
populations and, ultimately, the
extinction of the species as a whole.
Because the physical conditions of the
spring channels have changed
dramatically in the past, the species are
now at a greater risk of extinction
because of the alterations to the
ecosystem and the overall lower number
of individuals likely making up the
populations.
A number of efforts have been
undertaken at Balmorhea State Park to
conserve and maintain aquatic habitats
at some of the spring sites to conserve
habitat for the native aquatic species.
First, a refuge canal encircling the
historic motel was built in 1974 to
create habitat for the endangered fishes,
Comanche Springs pupfish and Pecos
gambusia (Garrett 2003, p. 153).
Although the canal was concrete-lined,
it had slower moderate water velocities,
and natural substrates covered the wide
concrete bottom and provided usable
habitat for the aquatic invertebrates.
Second, the 1-ha (2.5-ac) San Solomon
´
Cienega was built in 1996 to create an
additional flow-through pond of water
for habitat of the native aquatic species
(Garrett 2003, pp. 153–154). Finally,
during 2009 and 2010, a portion of the
deteriorating 1974 refuge canal was
removed and relocated away from the
motel. The wetted area was expanded to
´
create a new, larger cienega habitat. This
was intended to provide additional
natural habitat for the federally listed
endangered fishes and candidate
invertebrates (Service 2009c, p. 3;
Lockwood 2010, p. 3). All of these
efforts have been generally successful in
providing additional habitat areas for
the aquatic invertebrates, although
neither the snails nor amphipods have
´
been shown to use the newest cienega
pond to date (Allan 2011, p. 3).
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At Phantom Lake Spring, a pupfish
refuge canal was built in 1993 (Young
et al. 1993, pp. 1–3) to increase the
available aquatic habitat that had been
destroyed by the irrigation canal.
Winemiller and Anderson (1997, pp.
204–213) showed that the refuge canal
was used by endangered fish species
when water was available. Stomach
analysis of the endangered pupfish from
Phantom Lake Spring showed that the
Phantom Cave snail and diminutive
amphipod were a part of the fish’s diet
(Winemiller and Anderson 1997, pp.
209–210), indicating that the
invertebrates also used the refuge canal.
The refuge canal was constructed for a
design flow down to about 0.01 cms (0.5
cfs), which at the time of construction
was the lowest flow ever recorded out
of Phantom Lake Spring. The
subsequent loss of spring flow
eliminated the usefulness of the refuge
canal because the canal went dry
beginning in about 2000.
All the water for the remaining spring
head pool at Phantom Lake Spring is
being provided by a pump system to
bring water from about 23 m (75 ft)
within the cave out to the surface. The
small outflow pool was enlarged in 2011
(U.S. Bureau of Reclamation 2011, p. 1;
Service 2012, entire) to encompass
about 75 sq m (800 sq ft) of wetted area.
In 2011, the pool was relatively stable
and all three of the San Solomon Spring
invertebrates were present (Allan 2011,
p. 3; Service 2012, p. 9).
In summary, the modifications to the
natural spring channels at San Solomon,
Phantom Lake, and Giffin Springs
represent activities that occurred in the
past and resulted in a deterioration of
the available habitat for the Phantom
Cave snail, Phantom springsnail, and
diminutive amphipod. Actions by
conservation agencies over the past few
decades have mitigated the impacts of
those actions by restoring some natural
functions to the outflow channels.
While additional impacts from
modifications are not likely to occur in
the future because of land ownership by
conservation entities at three of the four
spring sites, the past modifications have
contributed to the endangerment of
these species by reducing the overall
quantity of available habitat and,
therefore, reducing the number of
individuals of each species that can
inhabit the spring outflows. The lower
the overall number of individuals of
each species and the lower the amount
of available habitat, the greater the risk
of extinction. Therefore, the
modification of spring channels
contributes to increased risk of
extinction in the future as a
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consequence of the negative impacts of
the past actions.
Other Conservation Efforts
All four of these springs in the San
Solomon Spring system are inhabited by
two fishes federally listed as
endangered—Comanche Springs
pupfish (Service 1981, pp. 1–2) and
Pecos gambusia (Service 1983, p. 4).
Critical habitat has not been designated
for either species. In addition, East
Sandia Spring is also inhabited by the
federally threatened Pecos sunflower
(Service 2005, p. 4) and the federally
endangered Pecos assiminea snail
(Service 2010, p. 5). Both the Pecos
sunflower and the Pecos assiminea snail
also have critical habitat designated at
East Sandia Spring (73 FR 17762, April
1, 2008; 76 FR 33036, June 7, 2011,
respectively).
The Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
have been afforded some protection
indirectly in the past due to the
presence of these other listed species in
the same locations. Management and
protection of the spring habitats by
Texas Parks and Wildlife Department at
San Solomon Spring, U.S. Bureau of
Reclamation at Phantom Lake Spring,
and The Nature Conservancy at East
Sandia Spring have benefited the
aquatic invertebrates. However, the
primary threat from the loss of habitat
due to declining spring flows related to
groundwater changes have not been
abated by the Federal listing of the fish
or other species. Therefore, the
conservation efforts provided by the
concomitant occurrence of species
already listed under the Act have not
prevented the past and ongoing habitat
loss, nor is it expected to prevent future
habitat loss.
Summary of Factor A
Based on our evaluation of the best
available information, we conclude that
the present and future destruction and
modification of the habitat of the
Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
is a significant threat. Some of these
impacts occurred in the past from the
loss of natural spring flows at several
springs likely within the historic range.
The impacts are occurring now and are
likely to continue in the future
throughout the current range as
groundwater levels decline and increase
the possibility of the loss of additional
springs. As additional springs are lost,
the number of populations will decline
and further increase the risk of
extinction of these species. The sources
of this threat are not confirmed but are
presumed to include a combination of
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factors associated with groundwater
pumping, hydrogeologic structure of the
supporting groundwater, and climatic
changes. The risk of extinction is also
heightened by the past alteration of
spring channels reducing the available
habitat and the number of individuals in
each population.
B. Overutilization for Commercial,
Recreational, Scientific, or Educational
Purposes (San Solomon Spring Species)
There are very few people who are
interested in or study springsnails and
amphipods, and those who do are
sensitive to their rarity and endemism.
Consequently, collection for scientific or
educational purposes is very limited.
There are no known commercial or
recreational uses of these invertebrates.
For these reasons we conclude that
overutilization for commercial,
recreational, scientific, or educational
purposes is currently not a threat to the
Phantom Lake snail, Phantom
springsnail, and diminutive amphipod,
and we have no indication that these
factors will affect these species in the
future.
C. Disease or Predation (San Solomon
Spring Species)
The San Solomon Spring species are
not known to be affected by any disease.
These invertebrates are likely natural
prey species for fishes and crayfishes
that occur in their habitats. Native snails
and amphipods have been found as
small proportions of the diets of native
fishes at San Solomon and Phantom
Lake Springs (Winemiller and Anderson
1997, p. 201; Hargrave 2010, p. 10), and
crayfish are a known predator of snails
(Hershler 1998, p. 14). Bradstreet (2011,
p. 98) assumed that snails at San
Solomon Spring were prey for both
fishes and crayfishes and suspected that
the native snails may be more
susceptible than the nonnative snails
because of their small body size and
thinner shells. In addition, Ladd and
Rogowski (2012, p. 289) suggested that
the nonnative red-rim melania
(Melanoides tuberculata) may prey
upon native snail eggs of a different
species. However, our knowledge of
such predation is very limited, and the
extent to which the predation might
affect native springsnails is unknown.
For more discussion about red-rim
melania see ‘‘Factor E. Other Natural or
Manmade Factors Affecting Its
Continued Existence.’’ We are not aware
of any other information indicating that
the San Solomon Spring species are
affected by disease or predation factors.
For these reasons we conclude that
disease or predation are not significant
threats to the Phantom Lake snail,
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Phantom springsnail, and diminutive
amphipod, and we have no indication
that these factors will affect these
species more severely in the future.
D. The Inadequacy of Existing
Regulatory Mechanisms (San Solomon
Spring Species)
Under this factor, we examine
whether existing regulatory mechanisms
are inadequate to address the threats to
the species discussed under Factors A
and E. Section 4(b)(1)(A) of the
Endangered Species Act requires the
Service to take into account ‘‘those
efforts, if any, being made by any State
or foreign nation, or any political
subdivision of a State or foreign nation,
to protect such species * * *.’’ We
interpret this language to require the
Service to consider relevant Federal,
State, and Tribal laws or regulations that
may minimize any of the threats we
describe in threat analyses under the
other four factors, or otherwise enhance
conservation of the species. An example
would be the terms and conditions
attached to a grazing permit that
describe how a permittee will manage
livestock on a BLM allotment. They are
nondiscretionary and enforceable, and
are considered a regulatory mechanism
under this analysis. Other examples
include State governmental actions
enforced under a State statute or
constitution, or Federal action under
statute.
Having evaluated the significance of
the threat as mitigated by any such
conservation efforts, we analyze under
Factor D the extent to which existing
regulatory mechanisms are inadequate
to address the specific threats to the
species. Regulatory mechanisms, if they
exist, may reduce or eliminate the
impacts from one or more identified
threats. In this section, we review
existing State and Federal regulatory
mechanisms to determine whether they
effectively reduce or remove threats to
the three San Solomon Spring species.
Texas laws provide no specific
protection for these invertebrate species,
as they are not listed as threatened or
endangered by the Texas Parks and
Wildlife Department. However, even if
they were listed by the State, those
regulations (Title 31 Part 2 of Texas
Administrative Code) would only
prohibit the taking, possession,
transportation, or sale of any animal
species without the issuance of a
permit. The State makes no provision
for the protection of the habitat of listed
species, which is the main threat to
these aquatic invertebrates.
Some protection for the habitat of this
species is provided with the land
ownership of the springs by Federal
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(Phantom Lake Spring owned by the
U.S. Bureau of Reclamation) and State
(San Solomon Spring owned by Texas
Parks and Wildlife Department)
agencies, and by The Nature
Conservancy (East Sandia Spring).
However, this land ownership only
protects the spring outflow channels
and provides no protection for
maintaining groundwater levels to
ensure continuous spring flows.
In the following discussion, we
evaluate the existing local regulations
related to groundwater management
within areas that might provide indirect
benefits to the species’ habitats through
management of groundwater levels.
Local Groundwater Regulations
One regulatory mechanism that could
provide some protection to the spring
flows for these species comes from local
groundwater conservation districts.
Groundwater in Texas is generally
governed by the rule of capture unless
there is a groundwater district in place.
The rule of capture allows a landowner
to produce as much groundwater as he
or she chooses, as long as the water is
not wasted (Mace 2001, p. 11). However,
local groundwater conservation districts
have been established throughout much
of Texas and are now the preferred
method for groundwater management in
the State (Texas Water Development
Board 2012, pp. 23–258). Groundwater
districts ‘‘may regulate the location and
production of wells, with certain
voluntary and mandatory exemptions’’
(Texas Water Development Board 2012,
p. 27).
There are currently four local
groundwater districts in the area west of
the springs (Texas Water Development
Board 2011, p. 1) that could possibly
manage groundwater to protect spring
flows in the San Solomon Spring
system. The Culberson County
Groundwater Conservation District
covers the southwestern portion of
Culberson County and was confirmed
(established by the Texas legislature and
approved by local voters) in 1998. The
Jeff Davis County Underground Water
Conservation District covers all of Jeff
Davis County and was confirmed in
1993. The Presidio County Underground
Water Conservation District covers all of
Presidio County and was confirmed in
1999. The Hudspeth County
Underground Water District No. 1
covers the northwest portion of
Hudspeth County and was confirmed in
1957. This area of Hudspeth County
manages the Bone Spring-Victoria Peak
aquifer (Hudspeth County Underground
Water District No. 1 2007, p. 1), which
is not known to contribute water to the
regional flow that supplies the San
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Solomon Spring system (Ashworth
2001, pp. 143–144). Therefore, we will
not further consider that groundwater
district.
In 2010 the Groundwater Management
Area 4 established ‘‘desired future
conditions’’ for the aquifers occurring
within the five-county area of west
Texas (Adams 2010, entire; Texas Water
Development Board 2012a, entire).
These projected conditions are
important because they guide the plans
for water use of groundwater within
groundwater conservation districts in
order to attain the desired future
condition of each aquifer they manage
(Texas Water Development Board 2012c,
p. 23). In the following discussion we
review the plans and desired future
conditions for the groundwater
conservation districts in Culberson, Jeff
Davis, and Presidio Counties relative to
the potential regulation of groundwater
for maintaining spring flows and abating
future declines in the San Solomon
Spring system.
The Culberson County Groundwater
Conservation District seeks to
implement water management strategies
to ‘‘prevent the extreme decline of water
levels for the benefit of all water right
owners, the economy, our citizens, and
the environment of the territory inside
the district’’ (Culberson County
Groundwater Conservation District
2007, p. 1). The missions of Jeff Davis
County Underground Water District and
Presidio County Underground Water
Conservation District are to ‘‘strive to
develop, promote, and implement water
conservation and management strategies
to protect water resources for the benefit
of the citizens, economy, and
environment of the District’’ (Jeff Davis
County Underground Water
Conservation District 2008, p. 1;
Presidio County Underground Water
Conservation District 2009, p. 1).
However, all three management plans
specifically exclude addressing natural
resources issues as a goal because, ‘‘The
District has no documented occurrences
of endangered or threatened species
dependent upon groundwater
resources’’ (Culberson County
Groundwater Conservation District
2007, p. 10; Jeff Davis County
Underground Water Conservation
District 2008, p. 19; Presidio County
Underground Water Conservation
District 2009, p. 14). This lack of
acknowledgement of the relationship of
the groundwater resources under the
Districts’ management to the
conservation of the spring flow habitat
at the San Solomon Spring system
prevents any direct benefits of their
management plans for the three aquatic
invertebrates.
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We also considered the desired future
condition of the relevant aquifer that
supports San Solomon Spring system
flows. The Culberson County
Groundwater Conservation District
manages the groundwater where the
bulk of groundwater pumping occurs in
the Salt Basin Bolson aquifer (part of the
West Texas Bolson, the source of the
water for the San Solomon Spring
system) (Oliver 2010, p. 7). The desired
future condition for aquifers within the
Culberson County Groundwater
Conservation District area includes a 24m (78-ft) drawdown for the West Texas
Bolsons (Salt Basin Bolson aquifer in
Wild Horse Flat) to accommodate an
average annual groundwater pumping of
46 million cm (38,000 af) (Adams 2010,
p. 2; Oliver 2010, p. 7). The desired
future condition for the West Texas
Bolsons for Jeff Davis County
Underground Water Conservation
District includes a 72-ft (22-m)
drawdown over the next 50 years to
accommodate an average annual
groundwater pumping of 10 million cm
(8,075 af) (Adams 2010, p. 2; Oliver
2010, p. 7). The desired future condition
for the West Texas Bolsons for Presidio
County Underground Water District also
includes a 72-ft (22-m) drawdown over
the next 50 years to accommodate an
average annual groundwater pumping of
12 million cm (9,793 af) (Adams 2010,
p. 2; Oliver 2010, p. 7). These
drawdowns are based on analysis using
groundwater availability models
developed for the Texas Water
Development Board (Beach et al. 2004,
p. 10–6–10–8; Oliver 2010, entire). We
expect that these groundwater districts
will use their district rules to regulate
water withdrawals in such a way as to
implement these desired future
conditions.
The Salt Basin Bolson aquifer in the
Wild Horse Flat area (the likely spring
source) can range from 60 to 300 m (200
to 1,000 ft) thick. So although it is
impossible to determine precisely, we
anticipate the planned level of
groundwater drawdown will likely
result in continued future declines in
spring flow rates in the San Solomon
Spring system. Therefore, we expect
that continued drawdown of the
aquifers as identified in the desired
future conditions will contribute to
ongoing and future spring flow declines.
Based on these desired future
conditions from the groundwater
conservation districts, we conclude that
the regulatory mechanisms available to
the groundwater districts directing
future groundwater withdrawal rates
from the aquifers that support spring
flows in the San Solomon Spring system
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are inadequate to protect against
ongoing and future modification of
habitat for the Phantom Cave snail,
Phantom springsnail, and diminutive
amphipod.
Summary of Factor D
Although there are some regulatory
mechanisms in place, such as the
existence of groundwater conservation
districts, we find that the mechanisms
are not serving to alleviate or limit the
salient threats to the Phantom Cave
snail, Phantom springsnail, or
diminutive amphipod. We, therefore,
conclude that these existing regulatory
mechanisms are inadequate to
sufficiently reduce the identified threats
to the Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
now and in the future.
E. Other Natural or Manmade Factors
Affecting Their Continued Existence
(San Solomon Spring Species)
We considered three other factors that
may be affecting the continued
existence of the San Solomon Spring
species: nonnative snails, other
nonnative species, and the small,
reduced ranges of the three San
Solomon Spring species.
Nonnative Snails
Another factor that may be impacting
the San Solomon Spring species is the
presence of two nonnative snails that
occur in a portion of their range. The
red-rim melania and quilted melania
both occur at San Solomon Spring, and
the red-rim melania also occurs at
Phantom Lake and Giffin Springs (Allan
2011, p. 1; Bradstreet 2011, pp. 4–5;
Lang 2011, pp. 4–5, 11). Both species
are native to Africa and Asia and have
been imported into the United States as
aquarium species. They are now
established in various locations across
the southern and western portions of the
United States (Bradstreet 2011, pp. 4–5;
U.S. Geological Survey 2009, p. 2;
Benson 2012, p. 2).
The red-rim melania was first
reported from Phantom Lake Spring
during the 1990s (Fullington 1993, p. 2;
McDermott 2000, pp. 14–15) and was
first reported from Giffin Spring in 2001
(Lang 2011, pp. 4–5). The species has
been at San Solomon Spring for some
time longer (Texas Parks and Wildlife
Department 1999, p. 14), but it is not
found in East Sandia Spring (Lang 2011,
p. 10; Allan 2011, p. 1). Bradstreet
reported the red-rim melania in all of
the habitats throughout San Solomon
Spring at moderate densities compared
to other snails, with a total population
estimate of about 390,000 snails (±
350,000) (Bradstreet 2011, pp. 45–55).
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Lang (2011, pp. 4–5) also found
moderate densities of red-rim melania at
Giffin Spring in both the headspring
area and downstream spring run area.
The quilted melania was first reported
as being at San Solomon Spring in 1999
(Texas Parks and Wildlife Department
1999, p. 14) from observations in 1995
(Bowles 2012, pers. comm.). It was later
collected in 2001 (Lang 2011, p. 4), but
not identified until Bradstreet (2011, p.
4) confirmed its presence there. The
species is not found in any other springs
in the San Solomon Spring system, but
occurs in all habitats throughout San
Solomon Spring at moderate densities
compared to other snails, with a total
population estimate of about 840,000
snails (±1,070,000) (Bradstreet 2011, pp.
45–55).
The mechanism and extent of
potential effects of the two nonnative
snails on the native invertebrates have
not been studied directly. However,
because both nonnative snails occur in
relatively high abundances, it is
reasonable to presume that they are
likely competing for space and food
resources in the limited habitats in
which they occur. Rader et al. (2003, pp.
651–655) reviewed the biology and
possible impacts of red-rim melania and
suggested that the species had already
displaced some native springsnails in
spring systems of the Bonneville Basin
of Utah. Appleton et al. (2009, entire)
reviewed the biology and possible
impacts of the quilted melania and
found potentially significant impacts
likely to occur to the native benthic
invertebrate community in aquatic
systems in South Africa. Currently, East
Sandia Spring has remained free of
nonnative snails, but their invasion
there is a continuing concern (Bradstreet
2011, p. 95). We conclude that these two
snails may be having some negative
effects on the Phantom Cave snail,
Phantom springsnail, and diminutive
amphipod based on a potential for
competition for spaces and food
resources.
Other Nonnative Species
A potential future threat to these
species comes from the possible
introduction of additional nonnative
species into their habitat. In general,
introduced species are a serious threat
to native aquatic species (Williams et al.
1989, p. 18; Lodge et al. 2000, p. 7). The
threat is particularly elevated at San
Solomon Spring where the public access
to the habitat is prolific by the
thousands of visitors to the Balmorhea
State Park who swim in the spring
outflow pool. Unfortunately, people will
sometimes release nonnative species
into natural waters, intentionally or
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unintentionally, without understanding
the potential impacts to native species.
In spite of regulations that do not permit
it, visitors to the Park may release
nonnative species into the outflow
waters of San Solomon Spring. This is
presumably how the two nonnative
snails became established there.
Nonnative fishes are sometimes seen
and removed from the water by Park
personnel (Texas Parks and Wildlife
Department 1999, pp. 46–47). The Park
makes some effort to minimize the risk
of nonnative species introductions by
prohibiting fishing (so no live bait is
released) and by taking measures to
educate visitors about the prohibition of
releasing species into the water (Texas
Parks and Wildlife Department 1999,
pp. 48). In spite of these efforts, there is
an ongoing risk, which cannot be fully
determined, that novel and destructive
nonnative species could be introduced
in the future. This risk is much lower at
the other three springs in the San
Solomon Spring system because of the
lack of public access to these sites.
We conclude that the future
introduction of any nonnative species
represents an ongoing concern to the
aquatic invertebrates, however, the
immediacy of this happening is
relatively low because it is only a future
possibility. In addition, the severity of
the impact is also relatively low because
it is most likely to occur only at San
Solomon Spring and the actual effects of
any nonnative species on the Phantom
Cave snail, Phantom springsnail, and
diminutive amphipod are unknown at
this time.
Small, Reduced Range
One important factor that contributes
to the high risk of extinction for these
species is their naturally small range
that has been reduced from past
destruction of their habitat. While the
overall extent of geographic range of the
species has not changed, the number
and distribution of local populations
within their range has likely been
reduced when other small springs
within the San Solomon Spring system
(such as Saragosa, Toyah, and West
Sandia Springs) ceased to flow (Brune
1981, p. 386; Karges 2003, p. 145).
These species are now currently limited
to four small spring outflow areas, with
the populations at Phantom Lake Spring
in imminent threat of loss.
The geographically small range with
only four populations of these
invertebrate species increases the risk of
extinction from any effects associated
with other threats or stochastic events.
When species are limited to small,
isolated habitats, they are more likely to
become extinct due to a local event that
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negatively affects the populations
(Shepard 1993, pp. 354–357; McKinney
1997, p. 497; Minckley and Unmack
2000, pp. 52–53). In addition, the
species are restricted to aquatic habitats
in small spring systems and have
minimal mobility and no other habitats
available for colonization, so it is
unlikely their range will ever expand
beyond the current extent. This
situation makes the magnitude of
impact of any possible threat very high.
In other words, the resulting effects of
any of the threat factors under
consideration here, even if they are
relatively small on a temporal or
geographic scale, could result in
complete extinction of the species.
While the small, reduced range does not
represent an independent threat to these
species, it does substantially increase
the risk of extinction from the effects of
other threats, including those addressed
in this analysis and those that could
occur in the future from unknown
sources.
Summary of Factor E
The potential impacts of these
nonnative snails and any future
introductions of other nonnative species
on the Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
are largely unknown with the current
available information. But the nonnative
snails are presumed to have some
negative consequences to the native
snails through competition for space
and resources. The effects on the
diminutive amphipod are even less
clear, but competition could still be
occurring. These nonnative snails have
likely been co-occurring for at least 20
years at three of the four known
locations for these species, and there is
currently nothing preventing the
invasion of the species into East Sandia
Spring. Considering the best available
information, we conclude that the
presence of these two nonnative snails
and the potential future introductions of
nonnative species currently represent a
low-intensity threat to the Phantom
Cave snail, Phantom Lake springsnail,
and diminutive amphipod. In addition,
the small, reduced ranges of these
species limit the number of available
populations and increase the risk of
extinction from other threats. In
combination with the past and future
threats from habitat modification and
loss, these factors contribute to the
increased risk of extinction to the three
native species.
Proposed Determination—San Solomon
Spring Species
We have carefully assessed the best
scientific and commercial information
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available regarding the past, present,
and future threats to the Phantom Cave
snail, Phantom springsnail, and
diminutive amphipod. We find the
species are in danger of extinction due
to the current and ongoing modification
and destruction of their habitat and
range (Factor A) from the ongoing and
future decline in spring flows, and
historic modification of spring channels.
The most significant factor threatening
these species is a result of historic and
future declines in regional groundwater
levels that have caused some springs to
cease flowing and threatens the
remaining springs with the same fate.
We did not find any significant threats
to the species under Factors B or C. We
found that existing regulatory
mechanisms are inadequate to provide
protection to the species through
groundwater management by
groundwater conservation districts
(Factor D) from existing and future
threats. Finally, two nonnative snails
occur in portions of the species’ range
that could be another factor negatively
affecting the species (Factor E). The
severity of the impact from these
nonnative snails or other future
introductions of nonnative species is
not known, but such introductions may
contribute to the risk of extinction from
the threats to habitat through reducing
the abundance of the three aquatic
invertebrates through competition for
space and resources. The small, reduced
ranges (Factor E) of these species, when
coupled with the presence of additional
threats, also put them at a heightened
risk of extinction.
The elevated risk of extinction of the
Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
is a result of the cumulative nature of
the stressors on the species and their
habitats. For example, the past
reduction in available habitat through
modification of spring channels resulted
in a lower number of individuals
contributing to the sizes of the
populations. In addition, the loss of
other small springs that may have been
inhabited by the species reduced the
number of populations that would
contribute to the species’ overall
viability. In this diminished state, the
species are also facing future risks from
the impacts of continuing declining
spring flows, exacerbated by potential
extended future droughts resulting from
global climate change, and potential
effects from nonnative species. All of
these factors contribute together to
heighten the risk of extinction and lead
to our finding that the Phantom Cave
snail, Phantom springsnail, and
diminutive amphipod are in danger of
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extinction throughout all of their ranges
and warrant listing as endangered
species.
The Act defines an endangered
species as any species that is ‘‘in danger
of extinction throughout all or a
significant portion of its range’’ and a
threatened species as any species ‘‘that
is likely to become endangered
throughout all or a significant portion of
its range within the foreseeable future.’’
We have carefully assessed the best
scientific and commercial information
available regarding the past, present,
and future threats to the species, and
have determined that the Phantom Cave
snail, Phantom springsnail, and
diminutive amphipod all meet the
definition of endangered species under
the Act. Significant threats are occurring
now and in the foreseeable future, at a
high intensity, and across the species’
entire range, placing them on the brink
of extinction at the present time.
Because the threats are placing the
species in danger of extinction now and
not only in the foreseeable future, we
have determined that they meet the
definition of endangered species rather
than threatened species. Therefore, on
the basis of the best available scientific
and commercial information, we
propose listing the Phantom Cave snail,
Phantom springsnail, and diminutive
amphipod as endangered species in
accordance with sections 3(6) and
4(a)(1) of the Act.
Under the Act and our implementing
regulations, a species may warrant
listing if it is threatened or endangered
throughout all or a significant portion of
its range. The species proposed for
listing in this rule are highly restricted
within their range, and the threats occur
throughout their range. Therefore, we
assessed the status of the species
throughout their entire range. The
threats to the survival of the species
occur throughout the species’ range and
are not restricted to any particular
significant portion of that range.
Accordingly, our assessment and
proposed determination applies to the
species throughout their entire range.
Diamond Y Spring Species—Diamond Y
Spring Snail, Gonzales Springsnail, and
Pecos Amphipod
The following five-factor analysis
applies to the three species that occur in
the Diamond Y Spring system in Pecos
County, Texas: Diamond Y Spring snail,
Gonzales springsnail, and Pecos
amphipod.
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A. The Present or Threatened
Destruction, Modification, or
Curtailment of Their Habitat or Range
(Diamond Y Spring Species)
Spring Flow Decline
The primary threat to the continued
existence of the Diamond Y Spring
species is the degradation and potential
future loss of aquatic habitat (flowing
water from the spring outlets) due to the
decline of groundwater levels in the
aquifers that support spring surface
flows. Habitat for these species is
exclusively aquatic and completely
dependent upon spring outflows. Spring
flows in the Diamond Y Spring system
appear to have declined in flow rate
over time, and as spring flows decline
available aquatic habitat is reduced and
altered. When a spring ceases to flow
continually, all habitats for these
species are lost, and the populations
will be extirpated. When all of the
springs lose consistent surface flows, all
natural habitats for these aquatic
invertebrates will be gone, and the
species will become extinct. We know
springs in this area can fail due to
groundwater pumping, because larger
nearby springs, such as Comanche and
Leon Springs have already ceased
flowing and likely resulted in the
extirpation of local populations of these
species (assuming they were present
historically).
The springs do not have to cease
flowing completely to have an adverse
effect on invertebrate populations. The
small size of the spring outflows in the
Diamond Y Spring system makes them
particularly susceptible to changes in
water chemistry, increased water
temperatures, and freezing. Because
these springs are small, any reductions
in the flow rates from the springs can
reduce the available habitat for the
species, decreasing the number of
individuals and increasing the risk of
extinction. Water temperatures and
chemical factors such as dissolved
oxygen in springs do not typically
fluctuate (Hubbs 2001, p. 324);
invertebrates are narrowly adapted to
spring conditions and are sensitive to
changes in water quality (Hershler 1998,
p. 11). Spring flow declines can lead to
the degradation and loss of aquatic
invertebrate habitat and present a
substantial threat to the species.
There have been no regular recordings
of spring flow discharge at Diamond Y
Spring to quantify any trends in spring
flow. The total flow rates are very low,
as Veni (1991, p. 86) estimated total
discharge from the upper watercourse at
0.05 to .08 cms (2 to 3 cfs) and from the
lower watercourse at 0.04 to 0.05 cms (1
to 2 cfs). The nature of the system with
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many diffuse and unconfined small
springs and seeps makes the estimates
of water quantity discharging from the
spring system difficult to obtain.
However, many authors (Veni 1991, p.
86; Echelle et al. 2001, p. 28; Karges
2003, pp. 144–145) have described the
reductions in available surface waters
observed compared to older
descriptions of the area (Kennedy 1977,
p. 93; Hubbs et al. 1978, p. 489; Taylor
1985, pp. 4, 15, 21). The amount of
aquatic habitat may vary to some degree
based on annual and seasonal
conditions, but the overall trend in the
reduction in the amount of surface
water over the last several decades is
apparent.
A clear example of the loss in aquatic
habitat comes from Kennedy’s (1977, p.
93) description of one of his study sites
in 1974. Station 2 was called a ‘‘very
large pool’’ near Leon Creek of about
1,500 to 2,500 sq m (16,000 to 27,000 sq
ft) with shallow depths of 0.5 to 0.6 m
(1.6 to 2.0 ft), with a small 2-m (6.6-ft)
deep depression in the center. Today
very little open water is found in this
area, only marshy soils with occasional
trickles of surface flow. This slow loss
of aquatic habitat has occurred
throughout the system over time and
represents a substantial threat to the
continued existence of the Diamond Y
Spring snail, Gonzales springsnail, and
the Pecos amphipod.
The precise reason for the declining
spring flows remains uncertain, but it is
presumed to be related to a combination
of groundwater pumping, mainly for
agricultural irrigation, and a lack of
natural recharge to the supporting
aquifers. In addition, future changes in
the regional climate are expected to
exacerbate declining flows.
Initial studies of the Diamond Y
Spring system suggested that the
Edwards-Trinity aquifer was the
primary source of flows (Veni 1991, p.
86). However, later studies seem to
confirm that the Rustler aquifer is
instead more likely the chief source of
water (Boghici 1997, p. 107). The
Rustler aquifer is one of the less-studied
aquifers in Texas and encompasses most
of Reeves County and parts of
Culberson, Pecos, Loving, and Ward
Counties in the Delaware Basin of west
Texas (Boghici and Van Broekhoven
2001, pp. 209–210). The Rustler strata
are thought to be between 75 to 200 m
(250 to 670 ft) thick (Boghici and Van
Broekhoven 2001, p. 207). Very little
recharge to the aquifer likely comes
from precipitation in the Rustler Hills in
Culberson County, but most of it may be
contributed by cross-formational flows
from old water from deeper aquifer
formations (Boghici and Van
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Broekhoven 2001, pp. 218–219).
Groundwater planning for the Rustler
aquifer anticipates no annual recharge
(Middle Pecos Groundwater
Conservation District 2010b, p. 18).
Historic pumping from the Rustler
aquifer in Pecos County may have
contributed to declining spring flows, as
withdrawals of up to 9 million cm
(7,500 af) in 1958 were recorded, with
estimates from 1970 to 1997 suggesting
groundwater use averaged between
430,000 cm (350 af) to 2 million cm
(1,550 af) per year (Boghici and Van
Broekhoven 2001, p. 218). As a result,
declines in water levels in Pecos County
wells in the Rustler aquifer from the
mid-1960s through the late 1970s of up
to 30 m (100 ft) have been recorded
(Boghici and Van Broekhoven 2001, p.
213). We assume that groundwater
pumping has had some impacts on
spring flows of the Diamond Y Spring
system in the past; however, they have
not yet been substantial enough to cause
the main springs to cease flowing.
Future groundwater withdrawals may
further impact spring flow rates if they
occur in areas of the Rustler Aquifer that
affect the spring source areas.
Groundwater pumping withdrawals in
Pecos County are expected to continue
in the future mainly to support irrigated
agriculture (Region F Water Planning
Group 2011, pp. 2-16–2-19) and will
result in continued lowering of the
groundwater levels in the Rustler
aquifer. The latest plans from
Groundwater Management Area 3 (the
planning group covering the relevant
portion of the Rustler Aquifer) allows
for a groundwater withdrawal in the
Rustler Aquifer not to exceed 90 m (300
ft) in the year 2060 (Middle Pecos
Groundwater Conservation District
2010a, p. 2). This level of drawdown
will accommodate 12.9 million cm
(10,508 af) of annual withdrawals by
pumping (Middle Pecos Groundwater
Conservation District 2010b, p. 15). This
level of pumping would be 30 times
more than the long-term average and
could result in an extensive reduction in
the available groundwater in the aquifer
based on the total thickness of the
Rustler strata. Therefore, we anticipate
this level of groundwater drawdown
may contribute to continued declines in
spring flow rates in the Diamond Y
Spring system.
Another factor possibly contributing
to declining spring flows is climatic
changes that may increase the frequency
and duration of local and regional
drought. The term ‘‘climate’’ refers to
the mean and variability of different
types of weather conditions over time,
with 30 years being a typical period for
such measurements, although shorter or
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longer periods also may be used (IPCC
2007a, p. 78). The term ‘‘climate
change’’ thus refers to a change in the
mean or variability of one or more
measures of climate (e.g., temperature or
precipitation) that persists for an
extended period, typically decades or
longer, whether the change is due to
natural variability, human activity, or
both (IPCC 2007a, p. 78).
Although the bulk of spring flows
probably originates from water sources
with limited recent recharge, any
decreases in regional precipitation
patterns due to prolonged drought will
further stress groundwater availability
and increase the risk of diminishment or
drying of the springs. Drought affects
both surface and groundwater resources
and can lead to diminished water
quality (Woodhouse and Overpeck
1998, p. 2693; MacRae et al. 2001, pp.
4, 10) in addition to reducing
groundwater quantities. Lack of rainfall
may also indirectly affect aquifer levels
by resulting in an increase in
groundwater pumping to offset water
shortages from low precipitation (Mace
and Wade 2008, p. 665).
Recent drought conditions may be
indicative of more common future
conditions. The current, multiyear
drought in the western United States,
including the Southwest, is the most
severe drought recorded since 1900
(Overpeck and Udall 2010, p. 1642). In
2011, Texas experienced the worst
annual drought since recordkeeping
began in 1895 (NOAA 2012, p. 4), and
only 1 other year since 1550 (the year
1789) was as dry as 2011 based on treering climate reconstruction (NOAA
2011, pp. 20–22). In addition, numerous
climate change models predict an
overall decrease in annual precipitation
in the southwestern United States and
northern Mexico.
Future global climate change may
result in increased severity of droughts
and further contribute to impacts on the
aquatic habitat from reduction of spring
flows. There is high confidence that
many semiarid areas like the western
United States will suffer a decrease in
water resources due to ongoing climate
change (IPCC 2007b, p. 7; Karl et al.
2009, pp. 129–131), as a result of less
annual mean precipitation. Milly et al.
(2005, p. 347) also project a 10 to 30
percent decrease in precipitation in
mid-latitude western North America by
the year 2050 based on an ensemble of
12 climate models. Even under lower
greenhouse gas emission scenarios,
recent projections forecast a 10 percent
decline in precipitation in western
Texas by 2080 to 2099 (Karl et al. 2009,
pp. 129–130). Assessments of climate
change in west Texas suggest that the
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area is likely to become warmer and at
least slightly drier (Texas Water
Development Board 2008, pp. 22–25).
The potential effects of future climate
change could reduce overall water
availability in this region of western
Texas and compound the stressors
associated with declining flows from the
Diamond Y Spring system. As a result
of the effects of increased drought,
spring flows could decline indirectly as
a result of increased pumping of
groundwater to accommodate human
needs for additional water supplies
(Mace and Wade 2008, p. 664; Texas
Water Development Board 2012c, p.
231).
In conclusion, the Diamond Y Spring
snail, Gonzales springsnail, and Pecos
amphipod are in danger of extinction
because of the past and expected future
loss of habitat associated with declining
spring flows. Some nearby springs have
already gone dry. While the sources of
the stress of declining spring flows are
not known for certain, the best available
scientific information would indicate
that it is the result of a combination of
factors including past and current
groundwater pumping and climatic
changes (decreased precipitation and
recharge). The threat of habitat loss from
declining spring flows affects all the
entire range of all three species, as all
are at risk of future loss due to declining
spring flows. All indications are that the
source of this threat will persist into the
future and will result in continued
degradation of the species’ habitats,
placing them at a high risk of extinction.
Water Quality Changes and
Contamination
Another potential factor that could
impact habitat of the Diamond Y Spring
species is the potential degradation of
water quality from point pollutant
sources. This can occur either directly
into surface water or indirectly through
contamination of groundwater that
discharges into spring run habitats used
by the species. The primary threat for
contamination in these springs comes
from activities related to oil and gas
exploration, extraction, transportation,
and processing.
Oil and gas activities are a source of
significant threat to the Diamond Y
Spring species because of the potential
groundwater or surface water
contamination from pollutants (Veni
1991, p. 83; Fullington 1991, p. 6). The
Diamond Y Spring system is within an
active oil and gas extraction field that
has been operational for many decades.
In 1990, there were 45 active and
plugged wells within the Diamond Y
Preserve and an estimated 800 to 1,000
wells perforated the aquifers within the
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springs’ drainage basins (Veni 1991, p.
83). At this time there are still many
active wells located within about 100 m
(about 300 ft) of surface waters. In
addition, a natural gas processing plant,
known as the Gomez Plant, is located
within 0.8 km (0.5 mi) upslope of
Diamond Y Spring. Oil and gas
pipelines cross the habitat, and many oil
extraction wells are located near the
occupied habitat. Oil and gas drilling
also occurs throughout the area of
supporting groundwater providing
another potential source of
contamination through the groundwater
supply. The Gomez Plant, which
collects and processes natural gas is
located about 350 m (1,100 feet) up
gradient from the head pool of Diamond
Y Spring (Hoover 2011, p. 1). Taylor
(1985, p. 15) suggested that an
unidentified groundwater pollutant may
have been responsible for reductions in
abundance of Diamond Y Spring snail
in the headspring and outflow of
Diamond Y Spring, although there never
were any follow-up studies done to
investigate the presumption. The
potential for an event catastrophic to the
Diamond Y Spring species from a
contaminant spill or leak is possible at
any time (Veni 1991, p. 83).
As an example of the possibility for
spills, in 1992 approximately 10,600
barrels of crude oil were released from
a 15-cm (6-in) pipeline that traverses
Leon Creek above its confluence with
Diamond Y Draw. The oil was from a
pipeline, which ruptured at a point
several hundred feet away from the
Leon Creek channel. The spill site itself
is about 1.6 km (1 mi) overland from
Diamond Y Spring. The pipeline was
operated at the time of the spill by the
Texas-New Mexico Pipeline Company,
but ownership has since been
transferred to several other companies.
The Texas Railroad Commission has
been responsible for overseeing cleanup
of the spill site. Remediation of the site
initially involved aboveground land
farming of contaminated soil and rock
strata to allow microbial degradation. In
later years, remediation efforts focused
on vacuuming oil residues from the
surface of groundwater exposed by
trenches dug at the spill site. No
impacts on the rare fauna of Diamond Y
Springs have been observed, but no
specific monitoring of the effects of the
spill was undertaken (Industrial
Economics, Inc. 2005, p. 4–12).
If a contaminant were to leak into the
habitat of the species from any of the
various sources, the effects of the
contamination could result in death to
exposed individuals, reductions in food
availability, or other ecological impacts
(such as long-term alteration to water or
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soil chemistry and the microorganisms
that serve as the base of food web in the
aquatic ecosystem). The effects of a
surface spill or leak might be contained
to a local area and only affect a portion
of the populations; however, an event
that contaminated the groundwater
could impact both the upper and lower
watercourses and eliminate the entire
range of all three species. There is
currently no regular monitoring of the
water quality occurring for these species
or their habitats, so it is unlikely that
the effects would be detected quickly to
allow for a timely response.
These invertebrates are sensitive to
water contamination. Hydrobiid snails
as a group are considered sensitive to
water quality changes, and each species
is usually found within relatively
narrow habitat parameters (Sada 2008,
p. 59). Taylor (1985, p. 15) suggested
that an unidentified groundwater
pollutant may have been responsible for
reductions in abundance of Diamond Y
Spring snails in the headspring and
outflow of Diamond Y Spring, although
no follow-up studies were ever
conducted to investigate the
presumption. Additionally, amphipods
generally do not tolerate habitat
desiccation (drying), standing water,
sedimentation, or other adverse
environmental conditions; they are
considered very sensitive to habitat
degradation (Covich and Thorpe 1991,
pp. 676–677).
Several conservation measures have
been implemented in the past to reduce
the potential for a contamination event.
In the 1970s the U.S. Department of
Agriculture, Natural Resources
Conservation Service (then the Soil
Conservation Service) built a small berm
encompassing the south side of
Diamond Y Spring to prevent a surface
spill from the Gomez Plant from
reaching the spring head. After The
Nature Conservancy purchased the
Diamond Y Springs Preserve in 1990, oil
and gas companies undertook a number
of conservation measures to minimize
the potential for contamination of the
aquatic habitats. These measures
included decommissioning buried
corrodible metal pipelines and replacing
them with synthetic surface lines,
installing emergency shut-off valves,
building berms around oil pad sites, and
removing abandoned oil pad sites and
their access roads that had been
impeding surface water flow (Karges
2003, p. 144).
Presently, there is no evidence of
habitat destruction or modification due
to groundwater or surface water
contamination from leaks or spills, and
no major spills affecting the habitat have
been reported in the past (Veni 1991, p.
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83). However, the potential for future
adverse effects from a catastrophic event
is an ongoing threat of high severity of
potential impact but not immediate.
Modification of Spring Channels
The spring outflow channels in the
Diamond Y Spring system have
remained mostly intact. The main subtle
changes in the past were a result of
some cattle grazing before The Nature
Conservancy discontinued livestock use
in 2000, and roads and well pads that
were constructed in the spring outflow
areas. Most of these structures were
removed by the oil and gas industry
following The Nature Conservancy’s
ownership in 1990. Several caliche
(hard calcium carbonate material) roads
still cross the spring outflows with
small culverts used to pass the restricted
flows.
A recent concern has been raised
regarding the encroachment of bulrush
into the spring channels. Bulrush is an
emergent plant that grows in dense
stands along the margins of spring
channels. (An emergent plant is one
rooted in shallow water and having
most of its vegetative growth above the
water.) When flow levels decline,
reducing water depths and velocities,
bulrush can become very dense and
dominate the wetted channel. In 1998,
bulrush made up 39 percent (± 33
percent) of the plant species in the
wetted marsh areas of the Diamond Y
Draw (Van Auken et al. 2007, p. 54).
Observations by Itzkowitz (2008, p. 5;
2010, pp. 13–14) found that bulrush
were increasing in density at several
locations within the upper and lower
watercourses in Diamond Y Draw
resulting in the loss of open water
habitats. Itzkowitz (2010, pp. 13–14)
also noted a positive response by
bulrush following a controlled fire for
grassland management.
In addition to water level declines,
the bulrush encroachment may have
been aided by a small flume that was
installed in 2000 about 100 m (300 ft)
downstream of the springhead pool at
Diamond Y Spring (Service 1999, p. 2).
The purpose of the flume was to
facilitate spring flow monitoring, but the
instrumentation was not maintained.
The flume remains in place and is now
being used for flow measurements by
the U.S. Geological Survey. The
installation of the flume may have
slightly impounded the water upstream
creating shallow, slow overflow areas
along the bank promoting bulrush
growth. This potential effect of the
action was not foreseen (Service 1999,
p. 3). Whether or not the flume was the
cause, the area upstream of it is now
overgrown with bulrush, and the two
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snails have not been found in this
section for some time.
There are several ways in which
dense bulrush stands may alter habitat
for the invertebrates. Bulrush grows to
a height of about 0.7 m (2 ft) tall in very
dense stands. Dense bulrush thickets
will result in increased shading of the
water surface, which is likely to reduce
the algae and other food sources for the
invertebrates. In addition, the stems will
slow the water velocity, and the root
masses will collect sediments and alter
the substrates in the stream. These small
changes in habitat conditions may result
in proportionally large areas of the
spring outflow channels being
unsuitable for use by the invertebrates,
particularly the springsnails. Supporting
this idea is the reported distributions of
the snails that found them in highest
abundance in areas with more open
flowing water not dominated by bulrush
(Allan 2011, p. 2). The impacts of dense
bulrush stands as a result of declining
spring flow rates may be negatively
affecting the distribution and abundance
of the invertebrates within the Diamond
Y Spring system.
Another recent impact to spring
channels comes from disturbance by
feral hogs (Sus scrofa). These species
have been released or escaped from
domestic livestock and have become
free-ranging over time (Mapston 2005, p.
6). They have been in Texas for about
300 years and occur throughout the
State. The area around Diamond Y
Spring has not previously been reported
as within their distribution (Mapston
2005, p. 5), but they have now been
confirmed there (Allan 2011, p. 2). The
feral hogs prefer wet and marshy areas
and damage spring channels by creating
wallows, muddy depressions used to
keep cool and coat themselves with
mud (Mapston 2005, p. 15). In 2011,
wallows were observed in spring
channels formerly inhabited by the
invertebrates in both the upper and
lower watercourses at the Diamond Y
Preserve (Allan 2011, p. 2). The
alterations in the spring channels
caused by the wallows make the
affected area uninhabitable by the
invertebrates. The effects of feral hog
wallows are limited to small areas but
act as another stressor on the very
limited habitat of these three Diamond
Y Spring species.
Some protection for the spring
channel habitats for the Diamond Y
Spring species is provided with the
ownership and management of the
Diamond Y Spring Preserve by The
Nature Conservancy (Karges 2003, pp.
143–144). Their land stewardship efforts
ensure that intentional or direct impacts
to the spring channel habitats will not
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occur. However, land ownership by The
Nature Conservancy provides limited
ability to prevent changes such as
increases in bulrush or to control feral
hogs. Moreover, the Nature Conservancy
can provide little protection from the
main threats to this species—the loss of
necessary groundwater levels to ensure
adequate spring flows or contamination
of groundwater from oil and gas
activities (Taylor 1985, p. 21; Karges
2003, pp. 144–145).
In summary, the modifications to the
natural spring channels at the Diamond
Y Spring system represent activities that
are occurring now and will likely
continue in the future through the
continued encroachment of bulrush as
spring flows continue to decline and
through the effects of feral hog wallows.
Conservation actions over the past two
decades have removed and minimized
some past impacts to spring channels by
removing livestock and rehabilitating
former oil pads and access roads. While
additional direct modifications are not
likely to occur in the future because of
land ownership by The Nature
Conservancy, future modifications from
bulrush encroachment and feral hog
wallows contribute to the suite of
threats to the species’ habitat by
reducing the overall quantity of
available habitat and, therefore,
reducing the number of individuals of
each species that can inhabit the
springs. The lower the overall number
of individuals of each species and the
less available habitat, the greater the risk
of extinction. Therefore, the
modification of spring channels
contributes to increased risk of
extinction in the future as a
consequence of ongoing and future
impacts.
Other Conservation Efforts
The Diamond Y Spring system is
inhabited by two fishes federally listed
as endangered—Leon Springs pupfish
(Service 1985, pp. 3) and Pecos
gambusia (Service 1983, p. 4). In
addition, the area is also inhabited by
the federally threatened Pecos
sunflower (Service 2005, p. 4) and the
federally endangered Pecos assiminea
snail (Service 2010, p. 5). Critical
habitat has not been designated for
Pecos gambusia. The Diamond Y Spring
has been designated as critical habitat
for Leon Springs pupfish, Pecos
sunflower, and Pecos assiminea snail
(45 FR 54678, August 15, 1980; 73 FR
17762, April 1, 2008; 76 FR 33036, June
7, 2011, respectively).
The three Diamond Y Spring species
have been afforded some protection
indirectly in the past due to the
presence of these other listed species in
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the same locations. Management and
protection of the spring habitats by
Texas Parks and Wildlife Department,
The Nature Conservancy, and the
Service has benefited the aquatic
invertebrates (Karges 2007, pp. 19–20).
However, the primary threat from the
loss of habitat due to declining spring
flows related to groundwater changes
have not been abated by the Federal
listing of the fish or other species.
Therefore, the conservation efforts
provided by the concomitant occurrence
of species already listed under the Act
have not prevented past and current
habitat loss, nor are they expected to do
so in the future.
Summary of Factor A
Based on our evaluation of the best
available information, we conclude that
the present and future destruction and
modification of the habitat of the
Diamond Y Spring snail, Gonzales
springsnail, and Pecos amphipod is a
significant threat. These impacts in the
past have come from the loss of natural
spring flows at several springs likely
within the historic range, and the future
threat of the loss of additional springs
as groundwater levels are likely to
decline in the future. As springs decline
throughout the small range of these
species, the number of individuals and
populations will decline and continue
to increase the risk of extinction of these
species. The sources of this threat are
not confirmed but are presumed to
include a combination of factors
associated with groundwater pumping
and climatic changes. The potential for
a spill of contaminants from oil and gas
operations presents a constant future
threat to the quality of the aquatic
habitat. Finally, the risk of extinction is
heightened by the ongoing and future
modification of spring channels, which
reduces the number of individuals in
each population, from the encroachment
of bulrush and the presence of feral
hogs.
B. Overutilization for Commercial,
Recreational, Scientific, or Educational
Purposes (Diamond Y Spring Species)
There are very few people who are
interested in or study springsnails and
amphipods, and those who do are
sensitive to their rarity and endemism.
Consequently, collection for scientific or
educational purposes is very limited.
There are no known commercial or
recreational uses of these invertebrates.
For these reasons we conclude that
overutilization for commercial,
recreational, scientific, or educational
purposes are not a threat to the
Diamond Y Spring snail, Gonzales
springsnail, and Pecos amphipod, and
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we have no indication that these factors
will affect these species in the future.
C. Disease or Predation (Diamond Y
Spring Species)
The Diamond Y Spring species are not
known to be affected by any disease.
These invertebrates are likely natural
prey species for fishes that occur in
their habitats. There are no known
nonnative predatory fishes within their
spring habitats, but there are crayfish,
which are known to prey on snails
(Hershler 1998, p. 14). Ladd and
Rogowski (2012, p. 289) suggested that
the nonnative red-rim melania may prey
upon different species of native snail
eggs. However, the evidence of such
predation is very limited, and the extent
to which the predation might affect
native snails is unknown. For more
discussion about red-rim melania, see
‘‘Factor E. Other Natural or Manmade
Factors Affecting Its Continued
Existence (Diamond Y Spring Species).’’
We are not aware of any other
information indicating that the Diamond
Y Spring species are affected by disease
or predation. For these reasons we
conclude that neither disease nor
predation are threats to the Diamond Y
Spring snail, Gonzales springsnail, and
Pecos amphipod, and we have no
indication that these factors will affect
these species in the future.
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D. The Inadequacy of Existing
Regulatory Mechanisms (Diamond Y
Spring Species)
Under this factor, we examine
whether existing regulatory mechanisms
are inadequate to address the threats to
the species discussed under the other
four factors. Section 4(b)(1)(A) of the
Endangered Species Act requires the
Service to take into account ‘‘those
efforts, if any, being made by any State
or foreign nation, or any political
subdivision of a State or foreign nation,
to protect such species * * * .’’ We
interpret this language to require the
Service to consider relevant Federal,
State, and Tribal laws and regulations
that may minimize any of the threats we
describe in threat analyses under the
other four factors, or otherwise enhance
conservation of the species. An example
would be the terms and conditions
attached to a grazing permit that
describe how a permittee will manage
livestock on a BLM allotment. They are
nondiscretionary and enforceable, and
are considered a regulatory mechanism
under this analysis. Other examples
include State governmental actions
enforced under a State statute or
constitution, or Federal action under
statute.
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Having evaluated the significance of
the threat as mitigated by any such
conservation efforts, we analyze under
Factor D the extent to which existing
regulatory mechanisms are inadequate
to address the specific threats to the
species. Regulatory mechanisms, if they
exist, may reduce or eliminate the
impacts from one or more identified
threats. In this section, we review
existing State and Federal regulatory
mechanisms to determine whether they
effectively reduce or remove threats to
the three San Solomon Spring species.
Texas laws provide no specific
protection for these invertebrate species,
as they are not listed as threatened or
endangered by the Texas Parks and
Wildlife Department. However, even if
they were listed by the State, those
regulations (Title 31 Part 2 of Texas
Administrative Code) would only
prohibit the taking, possession,
transportation, or sale of any animal
species without the issuance of a
permit. The State makes no provision
for the protection of the habitat of listed
species, which is the main threat to
these aquatic invertebrates.
Some protection for the habitat of this
species is provided with the land
ownership of the springs by The Nature
Conservancy. However, this land
ownership only protects the spring
outflow channels and provides no
protection for maintaining groundwater
levels to ensure continuous spring
flows.
In the following discussion we
evaluate the local regulations related to
groundwater management within areas
that might provide indirect benefits to
the species’ habitats through
management of groundwater
withdrawals, and Texas regulations for
oil and gas activities.
Local Groundwater Regulations
One regulatory mechanism that could
provide some protection to the spring
flows for these species comes from local
groundwater conservation districts.
Groundwater in Texas is generally
governed by the rule of capture unless
there is a groundwater district in place.
The rule of capture allows a landowner
to produce as much groundwater as he
or she chooses, as long as the water is
not wasted (Mace 2001, p. 11). However,
local groundwater conservation districts
have been established throughout much
of Texas and are now the preferred
method for groundwater management in
the State (Texas Water Development
Board 2012, pp. 23–258). Groundwater
districts ‘‘may regulate the location and
production of wells, with certain
voluntary and mandatory exemptions’’
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(Texas Water Development Board 2012,
p. 27).
There is currently one local
groundwater district in the area (Texas
Water Development Board 2011, p. 1)
that could possibly manage groundwater
to protect spring flows in the Diamond
Y Spring system. The Middle Pecos
Groundwater Conservation District
covers all of Pecos County and was
confirmed in 2002. The Middle Pecos
County Groundwater Conservation
District seeks to implement water
management strategies to ‘‘help
maintain a sustainable, adequate,
reliable, cost effective and high quality
source of groundwater to promote the
vitality, economy and environment of
the District’’ (Middle Pecos
Groundwater Conservation District
2010b, p. 1). However, the management
plan provides no objectives to maintain
spring flow at Diamond Y Spring or to
otherwise conserve the three aquatic
invertebrates. This lack of
acknowledgement of the relationship
between the groundwater resources
under the Districts’ management to the
conservation of the spring flow habitat
at the Diamond Y Spring system limits
any direct benefits of the management
plan for the three aquatic invertebrates.
In 2010 the Groundwater Management
Area 3 established ‘‘desired future
conditions’’ for the aquifers occurring
within a six-county area of west Texas
(Texas Water Development Board
2012b, entire). These projected
conditions are important because they
guide the plans for water use of
groundwater within groundwater
conservation districts in order to attain
the desired future condition of each
aquifer they manage (Texas Water
Development Board 2012c, p. 23). The
latest plans from Groundwater
Management Area 3 (the planning group
covering the relevant portion of the
Rustler aquifer) allows for a
groundwater withdrawal in the Rustler
aquifer not to exceed a 90 m (300 ft)
drawdown in the year 2060 (Middle
Pecos Groundwater Conservation
District 2010a, p. 2). The Rustler strata
are thought to be between only about 75
and 200 m (250 and 670 ft) thick. This
level of drawdown will accommodate
12.9 million cm (10,508 af) of annual
withdrawals by pumping (Middle Pecos
Groundwater Conservation District
2010b, p. 15; Williams 2010, pp. 3–5).
We expect that the groundwater district
will use their district rules to regulate
water withdrawals in such a way as to
implement these desired future
conditions.
We expect that continued drawdown
of the Rustler aquifer as identified in the
desired future conditions will
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contribute to ongoing and future spring
flow declines. Based on these desired
future conditions from the groundwater
conservation district, we find that the
regulatory mechanisms directing future
groundwater withdrawal rates from the
aquifer that supports spring flows in the
Diamond Y Spring system are
inadequate to protect against ongoing
and future modification of habitat for
the Diamond Y Spring snail, Gonzales
springsnail, and Pecos amphipod.
Texas Regulations for Oil and Gas
Activities
The Railroad Commission of Texas
has regulations that govern many
activities by the oil and gas industries
to minimize the opportunity for the
release of contaminants into the surface
water or groundwater in Texas (Texas
Administrative Code, Title 16.
Economic Regulation, Part 1). While the
many regulations in place may be
effective at reducing the risk of
contaminant releases, they cannot
remove the threat of a catastrophic event
that could lead to the extinction of the
aquatic invertebrates. Therefore,
because of the inherent risk associated
with oil and gas activities in proximity
to the habitats of the three Diamond Y
Spring species, and the severe
consequences to the species of any
contamination, Texas regulations for oil
and gas activities cannot remove or
alleviate the threats associated with
water contamination from an oil or gas
spill.
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Summary of Factor D
Although there are regulatory
mechanisms in place, such as the
existence of a local groundwater
conservation district and State
regulations of oil and gas operations, we
find that the mechanisms are not
serving to alleviate or limit the threats
to the Diamond Y Spring snail, Gonzales
springsnail, or Pecos amphipod. We,
therefore, conclude that these
mechanisms are inadequate to
sufficiently reduce the identified threats
to these species.
E. Other Natural or Manmade Factors
Affecting Their Continued Existence
(Diamond Y Spring Species)
We considered four other factors that
may be affecting the continued
existence of the Diamond Y Spring
species: nonnative fish management,
nonnative snail, other nonnative
species, and the small, reduced ranges
of the three Diamond Y Spring species.
Nonnative Fish Management
Another source of potential impacts to
these species comes from the indirect
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effect of management to control
nonnative fishes in Diamond Y Spring.
One of the major threats to the
endangered Leon Springs pupfish,
which is also endemic to the Diamond
Y Spring system, is hybridization with
the introduced, nonnative sheepshead
minnow (Cyprinodon variegatus). On
two separate occasions efforts to
eradicate the sheepshead minnow have
incorporated the use of fish toxicants in
the upper watercourse to kill and
remove all the fish and restock with
pure Leon Springs pupfish. The first
time was in the 1970s when the
chemical rotenone was used (Hubbs et
al. 1978, pp. 489–490) with no
documented conservation efforts or
monitoring for the invertebrate
community.
A second restoration effort was made
in 1998 when the fish toxicant
Antimycin A was used (Echelle et al.
2001, pp. 9–10) in the upper
watercourse. In that effort, actions were
taken to preserve some invertebrates
(holding them in tanks) during the
treatment, and an intense monitoring
effort was conducted to measure the
distribution and abundance of the
invertebrates immediately before and for
1 year after the chemical treatment
(Echelle et al. 2001, p. 14). The results
suggested that the Antimycin A had an
immediate and dramatic negative effect
on Pecos amphipods; however, their
abundance returned to pretreatment
levels within 7 months (Echelle et al.
2001, p. 23). Gonzales springsnail also
showed a decline in abundance that
persisted during the 1 year of
monitoring following the treatment at
both treated and untreated sites (Echelle
et al. 2001, pp. 23, 51).
There is no information available on
the impacts of the initial rotenone
treatment, but we suspect that, like the
later Antimycin A treatment, there were
at least short-term effects on the
individuals of the Diamond Y Spring
species. Both of these chemicals kill fish
and other gill-breathing animals (like
the three invertebrates) by inhibiting
their use of oxygen at the cellular level
(U.S. Army Corps of Engineers 2009, p.
2). Both chemicals are active for only a
short time, degrade quickly in the
environment, and are not toxic beyond
the initial application. The long-term
effects of these impacts are uncertain,
but the available information indicates
that the Gonzales springsnail may have
responded negatively over at least 1
year. This action was limited to the
upper watercourse populations, and the
effects were likely short-term in nature.
The use of fish toxicants represents
past stressors that are no longer directly
affecting the species but may have some
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lasting consequences to the distribution
and abundance of the snails. Currently
the Gonzales springsnail occurs in this
area of the upper watercourse in a very
narrow stretch of the outflow channel
from Diamond Y Spring, and the
Diamond Y Spring snail may no longer
occur in this stretch. Whether or not the
application of the fish toxicants
influenced these changes in distribution
and the current status of the Gonzales
springsnail is unknown. However, there
is some possibility that these actions
could have contributed to the current
absence of the Diamond Y Spring snail
from this reach and the restricted
distribution of the Gonzales springsnail
that now occurs in this reach. These
actions only occurred in the past, and
we do not anticipate them occurring
again in the future. If the sheepshead
minnow were to invade this habitat
again, we do not expect that chemical
treatment would be used due to a
heightened concern about conservation
of the invertebrates. Therefore, we
consider this threat relatively
insignificant because it was not severe
in its impact on the species, and it is not
likely to occur again in the future.
Nonnative Snail
Another factor that may be impacting
the Diamond Y Spring species is the
presence of the nonnative red-rim
melania, an invertebrate species native
to Africa and Asia that has been
imported as an aquarium species and is
now established in various locations
across the southern and western
portions of the United States (Benson
2012, p. 2).
The red-rim melania became
established in Diamond Y Spring in the
mid 1990s (Echelle et al. 2001, p. 15;
McDermott 2000, p. 15). The exotic
snail is now the most abundant snail in
the Diamond Y Spring system (Ladd
2010, p. 18). It only occurs in the first
270 m (890 ft) of the upper watercourse
of the Diamond Y Spring system, and it
has not been detected in the lower
watercourse (Echelle et al. 2001, p. 26;
Ladd 2010, p. 22).
The mechanism and extent of
potential effects of this nonnative snail
on the native invertebrates have not
been studied directly. However, because
the snail occurs in relatively high
abundances, it is reasonable to presume
that it is likely competing for space and
food resources in the limited habitats
within which they occur. Rader et al.
(2003, pp. 651–655) reviewed the
biology and possible impacts of red-rim
melania and suggested that the species
had already displaced some native
springsnails in spring systems of the
Bonneville Basin of Utah. In the upper
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watercourse where the red-rim melania
occurs, only the Gonzales springsnail
occurs there now in very low abundance
in the area of overlap, and the Diamond
Y Spring snail does not occur in this
reach any longer (Ladd 2010, p. 19).
The potential impacts of the red-rim
melania on the three aquatic
invertebrate species in the Diamond Y
Spring system are largely unknown with
the current available information, but
the nonnative snail is presumed to have
some negative consequences to the
native snails through competition for
space and resources. The effects on the
Pecos amphipod is even less clear, but
competition could still be occurring.
The red-rim melania has been present in
the upper watercourse since the mid
1990s, and there is currently nothing
preventing the invasion of the species
into Euphrasia Spring in the lower
watercourse by an incidental human
introduction or downstream transport
during a flood. Considering the best
available information, we conclude that
the presence of this nonnative snail
represents a moderate threat to the
Diamond Y Spring snail, Gonzales
springsnail, and Pecos amphipod.
Other Nonnative Species
A potential future threat to these
species comes from the possible
introduction of additional nonnative
species into their habitat. In general,
introduced species are a serious threat
to native aquatic species (Williams et al.
1989, p. 18; Lodge et al. 2000, p. 7). The
threat is moderated by the limited
public access to the habitat on The
Nature Conservancy’s preserve.
Unfortunately, the limited access did
not prevent the introduction of the
nonnative sheepshead minnow on two
separate occasions (Echelle et al. 2001,
p. 4). In addition, invertebrates could be
inadvertently moved by biologists
conducting studies in multiple spring
sites (Echelle et al. 2001, p. 26).
While the introduction of any future
nonnative species could represent a
threat to the aquatic invertebrates, the
likelihood of this happening is
relatively low because it is only a future
possibility. In addition the extent of the
impacts of any future nonnative species
on the Diamond Y Spring snail,
Gonzales springsnail, and Pecos
amphipod are unknown at this time.
Small, Reduced Range
One important factor that contributes
to the high risk of extinction for these
species is their naturally small range
that has likely been reduced from past
destruction of their habitat. The overall
geographic range of the species may
have been reduced from the loss of
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Comanche Springs (where the snails
once occurred and likely the Pecos
amphipod did as well) and from Leon
Springs (if they historically occurred
there). And within the Diamond Y
Spring system, their distribution has
been reduced as flows from small
springs and seeps have declined and
reduced the amount of wetted areas in
the spring outflow. These species are
now currently limited to two small
spring outflow areas.
The geographically small range and
only two proximate populations of these
invertebrate species increases the risk of
extinction from any effects associated
with other threats or stochastic events.
When species are limited to small,
isolated habitats, they are more likely to
become extinct due to a local event that
negatively effects the populations
(Shepard 1993, pp. 354–357; McKinney
1997, p. 497; Minckley and Unmack
2000, pp. 52–53). In addition, the
species are restricted to aquatic habitats
in small spring systems and have
minimal mobility and no other habitats
available for colonization, so it is
unlikely their range will ever expand
beyond the current extent. This
situation makes the severity of impact of
any possible separate threat very high.
In other words, the resulting effects of
any of the threat factors under
consideration here, even if they are
relatively small on a temporal or
geographic scale, could result in
complete extinction of the species.
While the small, reduced range does not
represent an independent threat to these
species, it does substantially increase
the risk of extinction from the effects of
other threats, including those addressed
in this analysis, and those that could
occur in the future from unknown
sources.
Summary of Factor E
We considered four additional
stressors as other natural or manmade
factors that may be affecting these
species. The effects from management
actions to control nonnative fish species
are considered low because they
occurred in the past, with limited
impact, and we do not expect them to
occur in the future. The potential
impacts of the nonnative snail red-rim
melania and any future introductions of
other nonnative species on the Phantom
Cave snail, Phantom springsnail, and
diminutive amphipod are largely
unknown with the current available
information. But the nonnative snail is
presumed to have some negative
consequences to the native snails
through competition for space and
resources. The effects on the Pecos
amphipod are even less clear, but
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competition could still be occurring.
These nonnative snails have likely been
co-occurring for up to 20 years at one of
the two known locations for these
species, and there is currently nothing
preventing the invasion of the species
into Euphrasia Spring by an incidental
human introduction or downstream
transport during a flood. Considering
the best available information, we
conclude that the presence of the
nonnative snail and the potential future
introductions of nonnative species
represent a low magnitude threat to the
Diamond Y Spring snail, Gonzales
springsnail, and Pecos amphipod. In
addition, the effects of the small,
reduced ranges of these species limits
the number of available populations and
increases the risk of extinction from
other threats. In combination with the
past and future threats from habitat
modification and loss, these factors
contribute to the increased risk of
extinction to the three native species.
Proposed Determination—Diamond Y
Spring Species
We have carefully assessed the best
scientific and commercial information
available regarding the past, present,
and future threats to the Diamond Y
Spring snail, Gonzales springsnail, and
Pecos amphipod. We find the species
are in danger of extinction due to the
current and ongoing modification and
destruction of their habitat and range
(Factor A) from the ongoing and future
decline in spring flows, ongoing and
future modification of spring channels,
and threats of future water
contamination from oil and gas
activities. The most significant factor
threatening these species is a result of
historic and future declines in regional
groundwater levels that have caused the
spring system to have reduced surface
aquatic habitat and threaten the
remaining habitat with the same fate.
We did not find any significant threats
to the species under Factors B or C. We
found that existing regulatory
mechanisms that could provide
protection to the species through
groundwater management by
groundwater conservation districts and
Texas regulations of the oil and gas
activities (Factor D) are inadequate to
protect the species from existing and
future threats. Finally, the past
management actions for nonnative
fishes, the persistence of the nonnative
red-rim melania, and the future
introductions of other nonnative species
are other factors that have or could
negatively affect the species (Factor E).
The severity of the impact from the redrim melania is not known, but it and
future introductions may contribute to
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the risk of extinction from the threats to
habitat by reducing the abundance of
the three aquatic invertebrates through
competition for space and resources.
The small, reduced ranges (Factor E) of
these species, when coupled with the
presence of additional threats, also put
them at a heightened risk of extinction.
The elevated risk of extinction of the
Diamond Y Spring snail, Gonzales
springsnail, and Pecos amphipod is a
result of the cumulative nature of the
stressors on the species and their
habitats. For example, the past
reduction in available habitat from
declining surface water in the Diamond
Y Spring system results in lower
numbers of individuals contributing to
the sizes of the populations. In addition,
the loss of other spring systems that may
have been inhabited by these species
reduced the number of populations that
would contribute to the species’ overall
viability. In this diminished state, the
species are also facing future risks from
the impacts of continuing declining
spring flows, exacerbated by potential
extended future droughts resulting from
global climate change, and potential
effects from nonnative species. All of
these factors contribute together to
heighten the risk of extinction and lead
to our finding that the Diamond Y
Spring snail, Gonzales springsnail, and
Pecos amphipod are in danger of
extinction throughout all of their ranges
and warrant listing as endangered
species.
The Act defines an endangered
species as any species that is ‘‘in danger
of extinction throughout all or a
significant portion of its range’’ and a
threatened species as any species ‘‘that
is likely to become endangered
throughout all or a significant portion of
its range within the foreseeable future.’’
We have carefully assessed the best
scientific and commercial information
available regarding the past, present,
and future threats to the species, and
have determined that the Diamond Y
Spring snail, Gonzales springsnail, and
Pecos amphipod all meet the definition
of endangered under the Act. They do
not meet the definition of threatened
species, because significant threats are
occurring now and in the foreseeable
future, at a high magnitude, and across
the species’ entire range, placing them
on the brink of extinction at the present
time. Because the threats are placing the
species on the brink of extinction now
and not only in the foreseeable future,
we have determined that they meet the
definition of endangered species rather
than threatened species. Therefore, on
the basis of the best available scientific
and commercial information, we
propose listing the Diamond Y Spring
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snail, Gonzales springsnail, and Pecos
amphipod as endangered species in
accordance with sections 3(6) and
4(a)(1) of the Act.
Under the Act and our implementing
regulations, a species may warrant
listing if it is threatened or endangered
throughout all or a significant portion of
its range. The species proposed for
listing in this rule are highly restricted
in their range, and the threats occur
throughout their ranges. Therefore, we
assessed the status of these species
throughout their entire ranges. The
threats to the survival of these species
occur throughout the species’ ranges
and are not restricted to any particular
significant portion of their ranges.
Accordingly, our assessments and
proposed determinations apply to these
species throughout their entire ranges.
Available Conservation Measures
Conservation measures provided to
species listed as endangered or
threatened under the Act include
recognition, recovery actions,
requirements for Federal protection, and
prohibitions against certain practices.
Recognition through listing results in
public awareness and conservation by
Federal, state, tribal, and local agencies,
private organizations, and individuals.
The Act encourages cooperation with
the States and requires that recovery
actions be carried out for all listed
species. The protection required by
Federal agencies and the prohibitions
against certain activities are discussed,
in part, below.
The primary purpose of the Act is the
conservation of endangered and
threatened species and the ecosystems
upon which they depend. The ultimate
goal of such conservation efforts is the
recovery of these listed species, so that
they no longer need the protective
measures of the Act. Subsection 4(f) of
the Act requires the Service to develop
and implement recovery plans for the
conservation of endangered and
threatened species. The recovery
planning process involves the
identification of actions that are
necessary to halt or reverse the species’
decline by addressing the threats to its
survival and recovery. The goal of this
process is to restore listed species to a
point where they are secure, selfsustaining, and functioning components
of their ecosystems.
Recovery planning includes the
development of a recovery outline
shortly after a species is listed,
preparation of a draft and final recovery
plan, and revisions to the plan as
significant new information becomes
available. The recovery outline guides
the immediate implementation of urgent
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49627
recovery actions and describes the
process to be used to develop a recovery
plan. The recovery plan identifies sitespecific management actions that will
achieve recovery of the species,
measurable criteria that determine when
a species may be downlisted or delisted,
and methods for monitoring recovery
progress. Recovery plans also establish
a framework for agencies to coordinate
their recovery efforts and provide
estimates of the cost of implementing
recovery tasks. Recovery teams
(comprising species experts, Federal
and State agencies, nongovernmental
organizations, and stakeholders) are
often established to develop recovery
plans. When completed, the recovery
outline, draft recovery plan, and the
final recovery plan will be available on
our Web site (https://www.fws.gov/
endangered), or from our Austin
Ecological Services Field Office (see FOR
FURTHER INFORMATION CONTACT).
Implementation of recovery actions
generally requires the participation of a
broad range of partners, including other
Federal agencies, States, Tribes,
nongovernmental organizations,
businesses, and private landowners.
Examples of recovery actions include
habitat restoration (e.g., restoration of
native vegetation), research, captive
propagation and reintroduction, and
outreach and education. The recovery of
many listed species cannot be
accomplished solely on Federal lands
because their range may occur primarily
or solely on non-Federal lands. To
achieve recovery of these species
requires cooperative conservation efforts
on private, State, and Tribal lands.
If these species are listed, funding for
recovery actions will be available from
a variety of sources, including Federal
budgets, State programs, and cost share
grants for non-Federal landowners, the
academic community, and
nongovernmental organizations. In
addition, pursuant to section 6 of the
Act, the State of Texas would be eligible
for Federal funds to implement
management actions that promote the
protection and recovery of these species.
Information on our grant programs that
are available to aid species recovery can
be found at:
https://www.fws.gov/grants.
Although the six aquatic invertebrates
are only proposed for listing under the
Act at this time, please let us know if
you are interested in participating in
recovery efforts for this species.
Additionally, we invite you to submit
any new information on this species
whenever it becomes available and any
information you may have for recovery
planning purposes (see FOR FURTHER
INFORMATION CONTACT).
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Section 7(a) of the Act requires
Federal agencies to evaluate their
actions with respect to any species that
is proposed or listed as endangered or
threatened and with respect to its
critical habitat, if any is designated.
Regulations implementing this
interagency cooperation provision of the
Act are codified at 50 CFR part 402.
Section 7(a)(4) of the Act requires
Federal agencies to confer with the
Service on any action that is likely to
jeopardize the continued existence of a
species proposed for listing or result in
destruction or adverse modification of
proposed critical habitat. If a species is
listed subsequently, section 7(a)(2) of
the Act requires Federal agencies to
ensure that activities they authorize,
fund, or carry out are not likely to
jeopardize the continued existence of
the species or destroy or adversely
modify its critical habitat. If a Federal
action may affect a listed species or its
critical habitat, the responsible Federal
agency must enter into formal
consultation with the Service.
Federal agency actions within the
species habitat that may require
conference or consultation or both as
described in the preceding paragraph
include management and any other
landscape altering activities on Federal
lands administered by the U.S. Bureau
of Reclamation; issuance of section 404
Clean Water Act permits by the Army
Corps of Engineers; construction and
management of gas pipeline and power
line rights-of-way by the Federal Energy
Regulatory Commission; and
construction and maintenance of roads
or highways by the Federal Highway
Administration.
The Act and its implementing
regulations set forth a series of general
prohibitions and exceptions that apply
to all endangered wildlife. The
prohibitions of section 9(a)(2) of the Act,
codified at 50 CFR 17.21 for endangered
wildlife, in part, make it illegal for any
person subject to the jurisdiction of the
United States to take (includes harass,
harm, pursue, hunt, shoot, wound, kill,
trap, capture, or collect; or to attempt
any of these), import, export, ship in
interstate commerce in the course of
commercial activity, or sell or offer for
sale in interstate or foreign commerce
any listed species. Under the Lacey Act
(18 U.S.C. 42–43; 16 U.S.C. 3371–3378),
it is also illegal to possess, sell, deliver,
carry, transport, or ship any such
wildlife that has been taken illegally.
Certain exceptions apply to agents of the
Service and State conservation agencies.
We may issue permits to carry out
otherwise prohibited activities
involving endangered and threatened
wildlife species under certain
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circumstances. Regulations governing
permits are codified at 50 CFR 17.22 for
endangered species, and at 17.32 for
threatened species. With regard to
endangered wildlife, a permit must be
issued for the following purposes: for
scientific purposes, to enhance the
propagation or survival of the species,
and for incidental take in connection
with otherwise lawful activities.
It is our policy, as published in the
Federal Register on July 1, 1994 (59 FR
34272), to identify to the maximum
extent practicable at the time a species
is listed, those activities that would or
would not constitute a violation of
section 9 of the Act. The intent of this
policy is to increase public awareness of
the effect of a proposed listing on
proposed and ongoing activities within
the range of species proposed for listing.
The following activities could
potentially result in a violation of
section 9 of the Act; this list is not
comprehensive:
(1) Unauthorized collecting, handling,
possessing, selling, delivering, carrying,
or transporting of the species, including
import or export across State lines and
international boundaries, except for
properly documented antique
specimens of these taxa at least 100
years old, as defined by section 10(h)(1)
of the Act;
(2) Introduction into the habitat of the
six west Texas aquatic invertebrate
species of nonnative species that
compete with or prey upon any of the
six west Texas aquatic invertebrate
species;
(3) The unauthorized release of
biological control agents that attack any
life stage of these species;
(4) Unauthorized modification of the
springs or spring outflows inhabited by
the six west Texas aquatic invertebrates;
and
(5) Unauthorized discharge of
chemicals or fill material into any
waters in which these species are
known to occur.
Questions regarding whether specific
activities would constitute a violation of
section 9 of the Act should be directed
to the Austin Ecological Services Office
(see FOR FURTHER INFORMATION CONTACT).
Critical Habitat
Prudency Determination
Section 4 of the Act, as amended, and
implementing regulations (50 CFR
424.12), require that, to the maximum
extent prudent and determinable, the
Secretary designate critical habitat at the
time the species is determined to be
endangered or threatened. Our
regulations at 50 CFR 424.12(a)(1) state
that the designation of critical habitat is
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not prudent when one or both of the
following situations exist: (1) The
species is threatened by taking or other
activity and the identification of critical
habitat can be expected to increase the
degree of threat to the species; or (2) the
designation of critical habitat would not
be beneficial to the species.
There is no indication that the six
species of west Texas invertebrates are
threatened by collection and there are
no likely increases in the degree of
threats to the species if critical habitat
were designated. These species are not
targets of collection and the areas
proposed for designation either have
restricted public access or are already
readily open to the public (i.e.,
Balmorhea State Park). None of the
threats identified to the species are
associated with human access to the
sites, with the possible exception of the
potential for introducing nonnative
species at San Solomon Spring in
Balmorhea State Park. This threat, or
any other identified threat, is not
expected to increase as a result of
critical habitat designation because the
San Solomon Spring swimming pool is
already heavily visited, the Balmorhea
State Park take proactive measures to
prevent introduction of non-native
species, and the designation of critical
habitat will not change the situation.
In the absence of finding that the
designation of critical habitat would
increase threats to a species, if there are
any benefits to a critical habitat
designation, then a prudent finding is
warranted. The potential benefits of
critical habitat to the six west Texas
invertebrates include: (1) Triggering
consultation under section 7 of the Act,
in new areas for actions in which there
may be a Federal nexus where it would
not otherwise occur, because, for
example, Federal agencies were not
aware of the potential impacts of an
action on the species; (2) focusing
conservation activities on the most
essential features and areas; (3)
providing educational benefits to State
or county governments or private
entities; and (4) preventing people from
causing inadvertent harm to the species.
Therefore, because we have determined
that the designation of critical habitat
will not likely increase the degree of
threat to any of the six species and may
provide some measure of benefit, we
find that designation of critical habitat
is prudent for the Phantom Cave snail,
Phantom springsnail, diminutive
amphipod, Diamond Y Spring snail,
Gonzales springsnail, and Pecos
amphipod.
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Background
It is our intent to discuss below only
those topics directly relevant to the
designation of critical habitat for six
aquatic invertebrates in this section of
the proposed rules.
Critical habitat is defined in section 3
of the Act as:
(1) The specific areas within the
geographical area occupied by the
species, at the time it is listed in
accordance with the Act, on which are
found those physical or biological
features;
(a) Essential to the conservation of the
species; and
(b) Which may require special
management considerations or
protection; and
(2) Specific areas outside the
geographical area occupied by the
species at the time it is listed, upon a
determination that such areas are
essential for the conservation of the
species.
Conservation, as defined under
section 3 of the Act, means to use and
the use of all methods and procedures
that are necessary to bring an
endangered or threatened species to the
point at which the measures provided
pursuant to the Act are no longer
necessary. Such methods and
procedures include, but are not limited
to, all activities associated with
scientific resources management such as
research, census, law enforcement,
habitat acquisition and maintenance,
propagation, live trapping, and
transplantation, and, in the
extraordinary case where population
pressures within a given ecosystem
cannot be otherwise relieved, may
include regulated taking.
Critical habitat receives protection
under section 7 of the Act through the
requirement that Federal agencies
ensure, in consultation with the Service,
that any action they authorize, fund, or
carry out is not likely to result in the
destruction or adverse modification of
critical habitat. The designation of
critical habitat does not affect land
ownership or establish a refuge,
wilderness, reserve, preserve, or other
conservation area. Such designation
does not allow the government or public
to access private lands. Such
designation does not require
implementation of restoration, recovery,
or enhancement measures by nonFederal landowners. Where a landowner
requests Federal agency funding or
authorization for an action that may
affect a listed species or critical habitat,
the consultation requirements of section
7(a)(2) of the Act would apply, but even
in the event of a destruction or adverse
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modification finding, the obligation of
the Federal action agency and the
landowner is not to restore or recover
the species, but to implement
reasonable and prudent alternatives to
avoid destruction or adverse
modification of critical habitat.
Under the first prong of the Act’s
definition of critical habitat, areas
within the geographic area occupied by
the species at the time it was listed are
included in a critical habitat designation
if they contain physical or biological
features (1) which are essential to the
conservation of the species and (2)
which may require special management
considerations or protection. For these
areas, critical habitat designations
identify, to the extent known using the
best scientific and commercial data
available, those physical or biological
features that are essential to the
conservation of the species (such as
space, food, cover, and protected
habitat). In identifying those physical
and biological features within an area,
we focus on the principal biological or
physical constituent elements (primary
constituent elements such as roost sites,
nesting grounds, seasonal wetlands,
water quality, tide, soil type) that are
essential to the conservation of the
species. Primary constituent elements
are the elements of physical or
biological features that, when laid out in
the appropriate quantity and spatial
arrangement to provide for a species’
life-history processes, are essential to
the conservation of the species.
Under the second prong of the Act’s
definition of critical habitat, we can
designate critical habitat in areas
outside the geographic area occupied by
the species at the time it is listed, upon
a determination that such areas are
essential for the conservation of the
species. For example, an area currently
occupied by the species but that was not
occupied at the time of listing may be
essential to the conservation of the
species and may be included in the
critical habitat designation. We
designate critical habitat in areas
outside the geographic area occupied by
a species only when a designation
limited to its range would be inadequate
to ensure the conservation of the
species.
Section 4 of the Act requires that we
designate critical habitat on the basis of
the best scientific data available.
Further, our Policy on Information
Standards Under the Endangered
Species Act (published in the Federal
Register on July 1, 1994 (59 FR 34271)),
the Information Quality Act (section 515
of the Treasury and General
Government Appropriations Act for
Fiscal Year 2001 (Pub. L. 106–554; H.R.
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49629
5658)), and our associated Information
Quality Guidelines, provide criteria,
establish procedures, and provide
guidance to ensure that our decisions
are based on the best scientific data
available. They require our biologists, to
the extent consistent with the Act and
with the use of the best scientific data
available, to use primary and original
sources of information as the basis for
recommendations to designate critical
habitat.
When we are determining which areas
should be designated as critical habitat,
our primary source of information is
generally the information developed
during the listing process for the
species. Additional information sources
may include the recovery plan for the
species, articles in peer-reviewed
journals, conservation plans developed
by States and counties, scientific status
surveys and studies, biological
assessments, other unpublished
materials, or experts’ opinions or
personal knowledge.
Habitat is dynamic, and species may
move from one area to another over
time. We recognize that critical habitat
designated at a particular point in time
may not include all of the habitat areas
that we may later determine are
necessary for the recovery of the
species. For these reasons, a critical
habitat designation does not signal that
habitat outside the designated area is
unimportant or may not be needed for
recovery of the species. Areas that are
important to the conservation of the
species, both inside and outside the
critical habitat designation, will
continue to be subject to: (1)
Conservation actions implemented
under section 7(a)(1) of the Act, (2)
regulatory protections afforded by the
requirement in section 7(a)(2) of the Act
for Federal agencies to ensure their
actions are not likely to jeopardize the
continued existence of any endangered
or threatened species, and (3) the
prohibitions of section 9 of the Act if
actions occurring in these areas may
affect the species. Federally funded or
permitted projects affecting listed
species outside their designated critical
habitat areas may still result in jeopardy
findings in some cases. These
protections and conservation tools will
continue to contribute to recovery of
this species. Similarly, critical habitat
designations made on the basis of the
best available information at the time of
designation will not control the
direction and substance of future
recovery plans, habitat conservation
plans, or other species conservation
planning efforts if new information
available at the time of these planning
efforts calls for a different outcome.
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Physical or Biological Features
In accordance with section 3(5)(A)(i)
and 4(b)(1)(A) of the Act and regulations
at 50 CFR 424.12, in determining which
areas within the geographic area
occupied by the species at the time of
listing to designate as critical habitat,
we consider the physical or biological
features that are essential to the
conservation of the species and which
may require special management
considerations or protection. These
include, but are not limited to:
(1) Space for individual and
population growth and for normal
behavior;
(2) Food, water, air, light, minerals, or
other nutritional or physiological
requirements;
(3) Cover or shelter;
(4) Sites for breeding, reproduction, or
rearing (or development) of offspring;
and
(5) Habitats that are protected from
disturbance or are representative of the
historical, geographic, and ecological
distributions of a species.
We derive the specific physical or
biological features required for the
Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive
amphipod, and Pecos amphipod from
studies of the species’ habitat, ecology,
and life history as described below. We
have determined that the following
physical or biological features are
essential for the Phantom Cave snail,
Phantom springsnail, Diamond Y Spring
snail, Gonzales springsnail, diminutive
amphipod, and Pecos amphipod.
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Space for Individual and Population
Growth and for Normal Behavior
The aquatic environment associated
with spring outflow channels and
marshes provide the habitat for
Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive
amphipod, and Pecos amphipod growth
and normal behavior. The areas must
contain permanent flowing water to
provide for the biological needs of the
species. Each of the species completes
all of their life-history functions in the
water and cannot exist for any time
outside of the aquatic environment.
Several habitat parameters of springs,
such as temperature, dissolved carbon
dioxide, dissolved oxygen, conductivity,
substrate type, and water depth have
been shown to influence the
distribution and abundance of other
related species of springsnails (O’Brien
and Blinn 1999, pp. 231–232; Mladenka
and Minshall 2001, pp. 209–211;
Malcom et al. 2005, p. 75; Martinez and
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Thome 2006, pp. 12–15; Lysne et al.
2007, p. 650). Dissolved salts such as
calcium carbonate may also be
important factors because they are
essential for shell formation for the
snails (Pennak 1989, p. 552). Salinity
levels are also relevant, particularly at
Diamond Y Spring because elevated
salinity levels (3 to 6 parts per thousand
(Hubbs 2001, p. 314) of dissolved salts)
may prevent other more freshwateradapted species from competing with
the native species adapted to higher
salinity levels.
The six invertebrates inhabit springs
and spring-fed aquatic habitats with low
variability in water temperatures. For
example, Hubbs (2001, pp. 311–312,
314–315) reported that the spring
outflow temperatures had very low
variability with average readings of 20
degrees Celsius (°C) (68 degrees
Fahrenheit (°F)) at Diamond Y Spring
and 19°C (66 °F) at East Sandia Spring
with a range between 11 and 25 °C (52
to 77 °F). Spring measurements from
2001 to 2003 at the four springs in the
San Solomon Spring complex found
water temperatures ranging from 17 to
27 °C (63 to 81 °F) (Texas Water
Development Board 2005, p. 38).
Proximity to spring vents, where water
emerges from the ground, plays a key
role in the life history of the six west
Texas aquatic invertebrates. For
example, many springsnail species
exhibit decreased abundance farther
away from spring vents, presumably due
to their need for stable water chemistry
(Hershler 1994, p. 68; Hershler 1998, p.
11; Hershler and Sada 2002, p. 256;
Martinez and Thome 2006, p. 14).
The six west Texas aquatic
invertebrates are sensitive to water
contamination. Hydrobiid snails as a
group are considered sensitive to water
quality changes, and each species is
usually found within relatively narrow
habitat parameters (Sada 2008, p. 59).
Taylor (1985, p. 15) suggested that an
unidentified groundwater pollutant may
have been responsible for reductions in
abundance of Diamond Y Spring snail
in the headspring and outflow of
Diamond Y Spring, although no followup studies have been conducted to
investigate the presumption.
Additionally, amphipods generally do
not tolerate habitat desiccation (drying),
standing water, sedimentation, or other
adverse environmental conditions; they
are considered very sensitive to habitat
degradation (Covich and Thorpe 1991,
pp. 676–677).
All six species are most commonly
found in flowing water, presumably
where dissolved oxygen levels are
higher. The species are often found in
moderate flowing water along the spring
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outflow margins rather than in central
channels. Water depths where the
species occur are generally very
shallow, usually less than 1 m (3 ft)
deep. An exception to this is the bottom
of the San Solomon Spring pool where,
because of the construction of the
swimming pool, water depths are much
greater, exceeding 5 m (15 ft). In San
Solomon, Giffin, and Phantom Lake
Springs, the habitats for the species are
limited to the spring outflow channels
because past alteration of the system
(building of ditches) has eliminated any
small spring openings. However, at
Diamond Y Spring (and to a limited
extent, East Sandia Spring) the spring
outflows have not been severely
modified so that small springs, seeps,
and marshes still provide diffuse
shallow flowing water habitat associated
with emergent bulrush and saltgrass
(Taylor 1987, p. 38; Echelle et al. 2001,
p. 5). While these areas are more
difficult to map, measure, and survey,
these small springs and seeps are
important habitat for the three
invertebrate species at Diamond Y
Spring as long as they provide flowing
water.
Therefore, based on the information
above, we identify permanent, flowing,
unpolluted water (free from
contamination) within natural
temperature variations, emerging from
the ground and flowing on the surface,
to be a physical or biological feature
necessary for these species.
Food, Water, Air, Light, Minerals, or
Other Nutritional or Physiological
Requirements
Invertebrates in small spring
ecosystems depend on food from two
sources: that which grows in or on the
substrate (aquatic and attached plants
and algae) and that which falls or is
blown into the system (primarily
leaves). Water is also the medium
necessary to provide the algae, detritus
(dead or partially decayed plant
materials or animals), bacteria, and
submergent vegetation on which all six
species depend as a food resource.
Abundant sunlight is necessary to
promote the growth of algae upon which
all six west Texas aquatic invertebrates
feed.
All four snails are presumably fineparticle feeders on detritus (organic
material from decomposing organisms)
and periphyton (mixture of algae and
other microbes attached to submerged
surfaces) associated with the substrates
(mud, rocks, and vegetation) (Allan
1995, p. 83; Hershler and Sada 2002, p.
256; Lysne et al. 2007, p. 649). Dundee
and Dundee (1969, p. 207) found
diatoms (a group of single-celled algae)
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to be the primary component in the
digestive tract of the Phantom Cave
snail and Phantom springsnail,
indicating diatoms are a primary food
source. Spring ecosystems occupied by
these snail species must support the
periphyton upon which springsnails
graze. Additionally, submergent
vegetation contributes the necessary
nutrients, detritus, and bacteria on
which these species forage.
Amphipods are omnivorous, feeding
on algae, submergent vegetation, and
decaying organic matter (Smith 2001, p.
572). Both species of amphipod are
often found in beds of submerged
aquatic plants (Cole 1976, p. 80),
indicating that they probably feed on a
surface film of algae, diatoms, bacteria,
and fungi (Smith 2001, p. 572). Young
amphipods depend on microbial foods,
such as algae and bacteria, associated
with aquatic plants (Covich and Thorp
1991, p. 677).
Therefore, based on the information
above, we identify the presence of
abundant food, consisting of algae,
bacteria, decaying organic material, and
submergent vegetation that contributes
the necessary nutrients, detritus, and
bacteria on which these species forage
to be a physical or biological feature for
these species.
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Sites for Cover or Shelter and for
Breeding, Reproduction, or Rearing (or
Development) of Offspring
The six west Texas aquatic
invertebrates occur across a wide range
of substrate types. The Phantom Cave
snail is most commonly attached to hard
surfaces, especially large algae-covered
rocks, submerged vegetation, or even
concrete walls of the irrigation ditches,
and found in areas of higher water
velocities (Bradstreet 2011, pp. 73, 91).
The other springsnails may also be
attached to hard surfaces but will also
often be found in the softer substrate at
the margins of the stream flows.
Suitable substrates for egg laying by the
snails are typically firm, characterized
by cobble, gravel, sand, woody debris,
and aquatic vegetation. These substrates
increase productivity by providing
suitable egg-laying sites for the snails.
The amphipods, in the absence of
predatory fishes, will swim over any
open substrate on the channel bottom,
but in circumstances where fishes are
abundant they may be found in greater
abundance underneath large rocks,
embedded in gravels, or associated with
submerged vegetation. Amphipods do
not lay eggs upon a surface; instead, the
eggs are held within a marsupium
(brood pouch) within the female’s
exoskeleton.
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Therefore, based on the information
above, we identify substrates that
include cobble, gravel, pebble, sand,
silt, and aquatic vegetation, for
breeding, egg laying, maturing, feeding,
and escape from predators to be a
physical or biological feature for these
species.
Habitats Protected From Disturbance or
Representative of the Historical,
Geographic, and Ecological
Distributions of the Species
The Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive
amphipod, and Pecos amphipod have a
very restricted geographic distribution.
Endemic species whose populations
exhibit a high degree of isolation are
extremely susceptible to extinction from
both random and nonrandom
catastrophic natural or human-caused
events. Therefore, it is essential to
maintain the spring systems in which
they are currently found and upon
which these species depend. Adequate
spring sites, free of inappropriate
disturbance, must exist to promote
population expansion and viability.
This means protection from disturbance
caused by water depletion, water
contamination, springhead alteration, or
nonnative species. These species must,
at a minimum, sustain their current
distributions if ecological representation
of these species is to be ensured.
As discussed above (see Factor E:
Other Natural or Manmade Factors
Affecting Its Continued Existence),
introduced species are a moderate threat
to native aquatic species (Williams et al.
1989, p. 18; Lodge et al. 2000, p. 7),
including the six west Texas aquatic
invertebrates. The red-rim melania
already competes with all six species
where they occur, and the quilted
melania has been introduced into
habitats occupied by the San Solomon
Spring species. Feral hogs cause local
spring channel destruction within the
Diamond Y Spring system. Because the
distribution of the Phantom Cave snail,
Phantom springsnail, Diamond Y Spring
snail, Gonzales springsnail, diminutive
amphipod, and Pecos amphipod is so
limited, and their habitat so restricted,
introduction of additional nonnative
species into their habitat could be
devastating.
Therefore, based on the information
above, we identify either an absence of
nonnative predators and competitors or
nonnative predators and competitors at
low population levels to be a physical
or biological feature necessary for these
species.
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Primary Constituent Elements
Under the Act and its implementing
regulations, we are required to identify
the physical or biological features
essential to the conservation of the
Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive
amphipod, and Pecos amphipod in
areas occupied at the time of listing,
focusing on the features’ primary
constituent elements. We consider
primary constituent elements to be the
elements of physical or biological
features that provide for a species’ lifehistory processes and are essential to
the conservation of the species.
Based on our current knowledge of
the physical or biological features and
habitat characteristics required to
sustain the species’ life-history
processes, we determine that the
primary constituent elements specific to
the Phantom Cave snail, Phantom
springsnail, diminutive amphipod,
Diamond Y Spring snail, Gonzales
springsnail, and Pecos amphipod are
springs and spring-fed aquatic systems
that contain:
a. Permanent, flowing, unpolluted
water (free from contamination)
emerging from the ground and flowing
on the surface;
b. Water temperatures that vary
between 11 and 27 °C (52 to 81 °F) with
natural seasonal and diurnal variations
slightly above and below that range;
c. Substrates that include cobble,
gravel, pebble, sand, silt, and aquatic
vegetation, for breeding, egg laying,
maturing, feeding, and escape from
predators;
d. Abundant food, consisting of algae,
bacteria, decaying organic material, and
submergent vegetation that contributes
the necessary nutrients, detritus, and
bacteria on which these species forage;
and
e. Either an absence of nonnative
predators and competitors or nonnative
predators and competitors at low
population levels.
With this proposed designation of
critical habitat, we intend to identify the
physical or biological features essential
to the conservation of the species,
through the identification of the
appropriate quantity and spatial
arrangement of the primary constituent
elements sufficient to support the lifehistory processes of the species. All
units and subunits proposed to be
designated as critical habitat are
currently occupied by the Phantom
Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales
springsnail, diminutive amphipod, and
Pecos amphipod and contain the
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primary constituent elements in the
appropriate quantity and spatial
arrangement sufficient to support the
life history needs of the species.
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Special Management Considerations or
Protection
When designating critical habitat, we
assess whether the specific areas within
the geographic area occupied by the
species at the time of listing contain
features that are essential to the
conservation of the species and which
may require special management
considerations or protection. The
features essential to the conservation of
the Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive
amphipod, and Pecos amphipod may
require special management
considerations or protection to reduce
threats, such as reducing or eliminating
water in suitable or occupied habitat
through drought or groundwater
pumping; introducing pollutants to
levels unsuitable for the species; and
introducing nonnative species into the
inhabited spring systems such that
suitable habitat is reduced or
eliminated. Special management
considerations or protection are
required within critical habitat areas to
address these threats (See Summary of
Factors Affecting the Species).
Management activities that could
ameliorate these threats include
management of groundwater levels to
ensure the springs remain flowing (all
spring sites), managing oil and gas
activities to eliminate the threat of
groundwater or surface water
contamination (Diamond Y Spring),
maintaining the pump within Phantom
Lake Spring to ensure consistent flow,
managing existing nonnative species,
red-rim melania, quilted melania, and
feral hogs (San Solomon, Giffin,
Phantom Lake, and Diamond Y
Springs), and preventing the
introduction of additional nonnative
species (all spring sites).
Criteria Used To Identify Critical
Habitat
As required by section 4(b)(2) of the
Act, we use the best scientific data
available to designate critical habitat.
We review available information
pertaining to the habitat requirements of
the species. In accordance with the Act
and its implementing regulation at 50
CFR 424.12(e), we consider whether
designating additional areas—outside
those currently occupied as well as
those occupied at the time of listing—
are necessary to ensure the conservation
of the species. We are not currently
proposing to designate any areas outside
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the geographic area occupied by the
species because none of the historically
occupied areas (or those that may have
been occupied) were found to be
essential for the conservation of the
species (see discussion below).
We relied on information from
knowledgeable biologists and
recommendations contained in state
wildlife resource reports (Dundee and
Dundee 1969, entire; Cole and Bousfield
1970, entire; Cole 1976, entire; Cole
1985, entire; Taylor 1985, entire; Henry
1992, entire; Bowles and Arsuffi 1993,
entire; Seidel et al. 2009, entire;
Hershler et al. 2010, entire; Ladd 2010,
entire; Allan 2011, entire; Bradstreet
2011, entire; Hershler 2011, p. 1) in
making this determination. We also
reviewed the available literature
pertaining to habitat requirements,
historic localities, and current localities
for these species. This includes regional
geographic information system (GIS)
coverages.
Areas Occupied at the Time of Listing
For the purpose of designating critical
habitat for the Phantom Cave snail,
Phantom springsnail, Diamond Y Spring
snail, Gonzales springsnail, diminutive
amphipod, and Pecos amphipod, we
defined the occupied area based on the
most recent surveys available, which
includes the Diamond Y and San
Solomon Spring systems. We then
evaluated whether these areas contain
the primary constituent elements for the
species and whether they require
special management. Next we
considered areas historically occupied,
but not currently occupied. While the
west Texas aquatic invertebrates may
have inhabited other springs in the area
(such as Saragosa and Toyah Springs,
for the San Solomon Spring species, and
Leon and Comanche Springs for the
Diamond Y Spring species), we only
have confirmation that the Diamond Y
Spring snail and Gonzales springsnail
occurred in Comanche Spring at some
point in the past. We evaluated these
areas to determine whether they were
essential for the conservation of the
species.
To determine if currently occupied
areas contain the primary constituent
elements, we assessed the life-history
components of the species as they relate
to habitat. All of the west Texas aquatic
invertebrate species require unpolluted
spring water in the springheads and
spring outflows; periphyton and
decaying organic material for food; a
combination of soft and hard substrates
for maturation, feeding, egg laying by
snails, and escape from predators; and
absence of nonnative predators and
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competitors (see discussion on Physical
or Biological Features).
Areas Unoccupied at the Time of Listing
To determine if the sites that may
have been historically occupied by the
Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive
amphipod, and Pecos amphipod are
essential for their conservation, we
considered: (1) The importance of the
site to the overall status of the species
to prevent extinction and contribute to
future recovery of each species; (2)
whether the area could be restored to
contain the necessary physical and
biological features to support the
species; and (3) whether a population of
the species could be reestablished at the
site.
The Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
occur in the San Solomon Spring
system, which includes San Solomon
Spring, Giffin Spring, East Sandia
Spring, and Phantom Spring. These
species may have occurred in other
springs within the system, including
Saragosa, Toyah, and West Sandia
Springs. These springs now lack water
flow and the physical or biological
features necessary to support the San
Solomon Spring system invertebrates—
mainly the lack of flowing water. We do
not foresee these features being
restorable to the point where
populations of the Phantom Cave snail,
Phantom springsnail, and diminutive
amphipod could be reestablished. These
springs are not restorable because we do
not foresee an opportunity for
groundwater levels to rise sufficiently in
the future to restore permanent spring
flows because the supporting aquifers
are of ancient origin and do not receive
substantial modern recharge. Therefore,
even if current pumping activities were
to be managed for the benefit of spring
flows, it is doubtful that aquifer levels
would rise sufficiently to provide
restoration of permanent aquatic habitat
at these sites. For these reasons, we are
not proposing Saragosa Spring, Toyah
Spring, or West Sandia Spring or any
other unoccupied areas as critical
habitat for the San Solomon Spring
system invertebrates.
The Diamond Y Spring snail,
Gonzales springsnail, and Pecos
amphipod occur in the Diamond Y
Spring system. The Diamond Y Spring
snail and Gonzales springsnail
historically occurred at Comanche
Spring, and the Pecos amphipod may
have occurred there as well. All three
species may have occurred at Leon
Spring. Both Comanche Spring and
Leon Spring, which have aquifer
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sources that may be different or more
localized than that of Diamond Y
Spring, are dry or nearly so and have
been altered to such a degree that they
no longer contain the physical or
biological features necessary to support
the Diamond Y Spring invertebrates—
mainly the lack of flowing water.
Natural flow conditions from these
springs do not appear to be restorable to
the point where populations of the
Diamond Y Spring snail, Gonzales
springsnail, and Pecos amphipod could
be reestablished. For these reasons, we
are not proposing Leon Spring or
Comanche Spring as critical habitat for
the Diamond Y Spring invertebrates.
Mapping
For the areas we are proposing as
critical habitat, we plotted the known
occurrences of the Phantom Cave snail,
Phantom springsnail, Diamond Y Spring
snail, Gonzales springsnail, diminutive
amphipod, and Pecos amphipod in
springheads and spring outflows on
2010 aerial photography from U.S.
Department of Agriculture, National
Agriculture Imagery Program base maps
using ArcMap (Environmental Systems
Research Institute, Inc.), a computer
geographic information system (GIS)
program. We drew the boundaries
around the water features that make up
the critical habitat in each area. Other
than at San Solomon Spring, there are
no known developed areas such as
buildings, paved areas, and other
structures that lack the biological
features for the springsnail within the
proposed critical habitat areas.
When determining proposed critical
habitat boundaries, we made every
effort to avoid including developed
areas such as lands covered by
buildings, pavement, and other
structures because such lands lack
physical or biological features for the
species. The scale of the maps we
prepared under the parameters for
publication within the Code of Federal
Regulations may not reflect the
exclusion of such developed lands
within Balmorhea State Park at San
Solomon Spring. Any such lands left
inside critical habitat boundaries shown
on the maps of these proposed rules
(such as the asphalt and concrete-paved
dry surfaces in Balmorhea State Park)
have been excluded by text in these
proposed rules and are not proposed for
designation as critical habitat.
Therefore, if the critical habitat is
finalized as proposed, a Federal action
involving these lands would not trigger
section 7 consultation with respect to
critical habitat and the requirement of
no adverse modification unless the
specific action would affect the physical
or biological features in the adjacent
critical habitat.
Summary
We are proposing for designation of
critical habitat lands that we have
determined are occupied at the time of
listing and contain sufficient elements
of physical or biological features to
support life-history processes essential
for the conservation of the species.
Units were proposed for designation
based on sufficient elements of physical
49633
or biological features being present to
support the Phantom Cave snail,
Phantom springsnail, Diamond Y Spring
snail, Gonzales springsnail, diminutive
amphipod, and Pecos amphipod lifehistory processes. Some units contain
all of the identified elements of physical
or biological features and supported
multiple life-history processes. Some
segments contained only some elements
of the physical or biological features
necessary to support the Phantom Cave
snail, Phantom springsnail, Diamond Y
Spring snail, Gonzales springsnail,
diminutive amphipod, and Pecos
amphipod particular use of that habitat.
Proposed Critical Habitat Designation
We are proposing four areas as critical
habitat for the Phantom Cave snail,
Phantom springsnail, and diminutive
amphipod. We are proposing one area as
critical habitat for the Diamond Y
Spring snail, Gonzales springsnail, and
Pecos amphipod. The critical habitat
areas we describe below constitute our
current best assessment of areas that
meet the definition of critical habitat for
the species. The five areas we propose
as critical habitat are: (1) San Solomon
Spring, (2) Giffin Spring, (3) East Sandia
Spring, (4) Phantom Lake Spring, and
(5) the Diamond Y Spring System.
Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
all occur in the first 4 units and they are
listed in Table 1. Diamond Y Spring
snail, Gonzales springsnail, and Pecos
amphipod occur in the Diamond Y
Spring Unit and it is listed in Table 2.
TABLE 1—PROPOSED CRITICAL HABITAT UNITS FOR PHANTOM CAVE SNAIL, PHANTOM SPRINGSNAIL, AND DIMINUTIVE
AMPHIPOD
[Area estimates reflect all land within critical habitat unit boundaries]
Size of unit in
hectares
(acres)
Critical habitat unit
Land ownership by type
San Solomon Spring ................................................................
Giffin Spring .............................................................................
East Sandia Spring ..................................................................
Phantom Lake Spring ..............................................................
State—Texas Parks and Wildlife Department ........................
Private .....................................................................................
Private—The Nature Conservancy .........................................
Federal—Bureau of Reclamation ............................................
1.8 (4.4)
0.7 (1.7)
1.2 (3.0)
0.02 (0.05)
Total ..................................................................................
..................................................................................................
3.7 (9.2)
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Note: Area sizes may not sum due to rounding.
TABLE 2—PROPOSED CRITICAL HABITAT UNIT FOR DIAMOND Y SPRING SNAIL, GONZALES SPRINGSNAIL, AND PECOS
AMPHIPOD
[Area estimate reflects all land within critical habitat unit boundaries]
Size of unit in
hectares
(acres)
Critical habitat unit
Land ownership by type
Diamond Y Spring System ......................................................
Private—The Nature Conservancy .........................................
178.6 (441.4)
Total ..................................................................................
..................................................................................................
178.6 (441.4)
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minimize impacts resulting from these
threats.
We present brief descriptions of all
units, and reasons why they meet the
definition of critical habitat below.
San Solomon Spring Unit
The San Solomon Spring Unit
consists of 1.8 ha (4.4 ac) that is
currently occupied by the Phantom
Cave snail, Phantom springsnail, and
diminutive amphipod and contains all
of the features essential to the
conservation of these species. It is
located in Reeves County, near
Balmorhea, Texas. San Solomon Spring
provides the water for the large
swimming pool at Balmorhea State Park,
which is owned and managed by Texas
Parks and Wildlife Department. The
proposed designation includes all
springs, seeps, and outflows of San
Solomon Spring, including the part of
the concrete-lined pool that has a
natural substrate bottom and irrigation
´
ditch, and two constructed cienegas.
While the ditches do not provide all of
the physical or biological features (such
as submerged vegetation), there are
sufficient features (including natural
substrates on the ditch bottoms) to
provide for the life-history processes of
the species. Habitat in this unit is
threatened by future declining spring
flows due to drought or groundwater
withdrawals, the presence of nonnative
snails, and the introduction of other
nonnative species. Therefore, the
primary constituent elements in this
unit may require special management
considerations or protection to
minimize impacts resulting from these
threats.
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Giffin Spring Unit
Giffin Spring Unit consists of 0.7 ha
(1.7 ac) that is currently occupied by the
Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
and contains all of the features essential
to the conservation of these species. It
is located on private property in Reeves
County, near Balmorhea, Texas, and its
waters are captured in irrigation earthen
channels for agricultural use. The
proposed designation includes all
springs, seeps, sinkholes, and outflows
of Giffin Spring. The unit contains most
all of the identified physical and
biological features. Habitat in this unit
is threatened by declining spring flows
due to drought or groundwater
withdrawals, the presence of nonnative
snails, the introduction of other
nonnative species, and further
modification of spring outflow
channels. Therefore, the primary
constituent elements in this unit may
require special management
considerations or protection to
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East Sandia Spring Unit
East Sandia Spring consists of 1.2 ha
(3.0 ac) that is currently occupied by the
Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
and contains all of the features essential
to the conservation of these species.
This unit is included within a preserve
owned and managed by The Nature
Conservancy (Karges 2003, p. 145) in
Reeves County just east of Balmorhea,
Texas. The proposed designation
includes the springhead itself and
surrounding seeps and outflows. The
unit contains all of the identified
physical and biological features. Habitat
in this unit is threatened by declining
spring flows due to drought or
groundwater withdrawals, the
introduction of nonnative species, and
modification of spring outflow
channels. Therefore, the primary
constituent elements in this unit may
require special management
considerations or protection to
minimize impacts resulting from these
threats.
Phantom Lake Spring Unit
Phantom Lake Spring consists of a
small pool about 0.02 ha (0.05 ac) in
size that is currently occupied by the
Phantom Cave snail, Phantom
springsnail, and diminutive amphipod
and contains the features essential to the
conservation of these species. Phantom
Lake Spring is owned by the U.S.
Bureau of Reclamation about 6 km (4
mi) west of Balmorhea State Park in Jeff
Davis County, Texas. The proposed
designation includes only the
springhead pool. The physical or
biological features of the habitat at
Phantom Lake Spring have been
maintained since 2000 by a pumping
system and subsequent reconstruction
of the spring pool. Although artificially
maintained, the site continues to
provide sufficient physical or biological
features to provide for all the life-history
processes of the three invertebrate
species. Habitat in this unit is
threatened by future declining spring
flows due to drought or groundwater
withdrawals, the presence of nonnative
snails, and the introduction of other
nonnative species. Therefore, the
primary constituent elements in this
unit may require special management
considerations or protection to
minimize impacts resulting from these
threats.
Diamond Y Spring Unit
Diamond Y Spring Unit consists of
178.6 ha (441.4 ac) that is currently
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occupied by the Diamond Y Spring
snail, Gonzales springsnail, and Pecos
amphipod and contains all of the
features essential to the conservation of
these species. Diamond Y Spring and
surrounding lands are owned and
managed by The Nature Conservancy.
The proposed designation includes the
Diamond Y Spring and approximately
6.8 km (4.2 mi) of its outflow, including
both upper and lower watercourses,
ending at approximately 0.8 km (0.5 mi)
downstream of the State Highway 18
bridge crossing. Also included in this
proposed unit is approximately 0.8 km
(0.5 mi) of Leon Creek upstream of the
confluence with Diamond Y Draw. The
boundaries of this unit extend out
laterally beyond the mapped spring
outflow channels to incorporate any and
all small springs and seeps that may not
be mapped or surveyed but are expected
to contain the species and the necessary
physical or biological features. The unit
contains all of the identified physical
and biological features. Habitat in this
unit is threatened by declining spring
flows due to drought or groundwater
withdrawals, subsurface drilling and
other oil and gas activities that could
contaminate surface drainage or aquifer
water, the presence of nonnative snails
and feral hogs, the introduction of other
nonnative species, and modification of
spring outflow channels. Therefore, the
primary constituent elements in this
unit may require special management
considerations or protection to
minimize impacts resulting from these
threats.
Effects of Critical Habitat Designation
Section 7 Consultation
Section 7(a)(2) of the Act requires
Federal agencies, including the Service,
to ensure that any action they fund,
authorize, or carry out is not likely to
jeopardize the continued existence of
any endangered species or threatened
species or result in the destruction or
adverse modification of designated
critical habitat of such species. In
addition, section 7(a)(4) of the Act
requires Federal agencies to confer with
the Service on any agency action that is
likely to jeopardize the continued
existence of any species proposed to be
listed under the Act or result in the
destruction or adverse modification of
proposed critical habitat.
Decisions by the 5th and 9th Circuit
Courts of Appeals have invalidated our
regulatory definition of ‘‘destruction or
adverse modification’’ (50 CFR 402.02)
(see Gifford Pinchot Task Force v. U.S.
Fish and Wildlife Service, 378 F. 3d
1059 (9th Cir. 2004) and Sierra Club v.
U.S. Fish and Wildlife Service et al., 245
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F.3d 434, 442 (5th Cir. 2001)), and we
do not rely on this regulatory definition
when analyzing whether an action is
likely to destroy or adversely modify
critical habitat. Under the statutory
provisions of the Act, we determine
destruction or adverse modification on
the basis of whether, with
implementation of the proposed Federal
action, the affected critical habitat
would continue to serve its intended
conservation role for the species.
If a Federal action may affect a listed
species or its critical habitat, the
responsible Federal agency (action
agency) must enter into consultation
with us. Examples of actions that are
subject to the section 7 consultation
process are actions on State, tribal,
local, or private lands that require a
Federal permit (such as a permit from
the U.S. Army Corps of Engineers under
section 404 of the Clean Water Act (33
U.S.C. 1251 et seq.) or a permit from the
Service under section 10 of the Act) or
that involve some other Federal action
(such as funding from the Federal
Highway Administration, Federal
Aviation Administration, or the Federal
Emergency Management Agency).
Federal actions not affecting listed
species or critical habitat, and actions
on State, tribal, local, or private lands
that are not federally funded or
authorized, do not require section 7
consultation.
As a result of section 7 consultation,
we document compliance with the
requirements of section 7(a)(2) through
our issuance of:
(1) A concurrence letter for Federal
actions that may affect, but are not
likely to adversely affect, listed species
or critical habitat; or
(2) A biological opinion for Federal
actions that may affect, or are likely to
adversely affect, listed species or critical
habitat.
When we issue a biological opinion
concluding that a project is likely to
jeopardize the continued existence of a
listed species and/or destroy or
adversely modify critical habitat, we
provide reasonable and prudent
alternatives to the project, if any are
identifiable, that would avoid the
likelihood of jeopardy and/or
destruction or adverse modification of
critical habitat. We define ‘‘reasonable
and prudent alternatives’’ (at 50 CFR
402.02) as alternative actions identified
during consultation that:
(1) Can be implemented in a manner
consistent with the intended purpose of
the action,
(2) Can be implemented consistent
with the scope of the Federal agency’s
legal authority and jurisdiction,
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(3) Are economically and
technologically feasible, and
(4) Would, in the Director’s opinion,
avoid the likelihood of jeopardizing the
continued existence of the listed species
and/or avoid the likelihood of
destroying or adversely modifying
critical habitat.
Reasonable and prudent alternatives
can vary from slight project
modifications to extensive redesign or
relocation of the project. Costs
associated with implementing a
reasonable and prudent alternative are
similarly variable.
Regulations at 50 CFR 402.16 require
Federal agencies to reinitiate
consultation on previously reviewed
actions in instances where we have
listed a new species or subsequently
designated critical habitat that may be
affected and the Federal agency has
retained discretionary involvement or
control over the action (or the agency’s
discretionary involvement or control is
authorized by law). Consequently,
Federal agencies sometimes may need to
request reinitiation of consultation with
us on actions for which formal
consultation has been completed, if
those actions with discretionary
involvement or control may affect
subsequently listed species or
designated critical habitat.
Application of the ‘‘Adverse
Modification’’ Standard
The key factor related to the adverse
modification determination is whether,
with implementation of the proposed
Federal action, the affected critical
habitat would continue to serve its
intended conservation role for the
species. Activities that may destroy or
adversely modify critical habitat are
those that alter the physical or
biological features to an extent that
appreciably reduces the conservation
value of critical habitat for the Phantom
Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales
springsnail, diminutive amphipod, and
Pecos amphipod. As discussed above,
the role of critical habitat is to support
the life-history needs of the species and
provide for the conservation of the
species.
Section 4(b)(8) of the Act requires us
to briefly evaluate and describe, in any
proposed or final regulation that
designates critical habitat, activities
involving a Federal action that may
destroy or adversely modify such
habitat, or that may be affected by such
designation.
Activities that may affect critical
habitat, when carried out, funded, or
authorized by a Federal agency, should
result in consultation for the Phantom
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49635
Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales
springsnail, diminutive amphipod, and
Pecos amphipod. These activities
include, but are not limited to:
(1) Actions that would reduce the
quantity of water flow within the spring
systems proposed as critical habitat.
(2) Actions that would contaminate or
cause significant degradation of water
quality within the spring systems
proposed as critical habitat, including
surface drainage water or aquifer water
quality.
(3) Actions that would modify the
springheads or outflow channels within
the spring systems proposed as critical
habitat.
(4) Actions that would reduce or alter
the availability of aquatic substrates
within the spring systems that are
proposed as critical habitat.
(5) Actions that would reduce the
occurrence of native aquatic periphyton
within the spring systems proposed as
critical habitat.
(6) Actions that would introduce,
promote, or maintain nonnative
predators and competitors within the
spring systems proposed as critical
habitat.
Exemptions
Application of Section 4(a)(3) of the Act
The National Defense Authorization
Act for Fiscal Year 2004 (Pub. L. 108–
136) amended the Act to limit areas
eligible for designation as critical
habitat on some Department of Defense
lands. There are no Department of
Defense lands within or near the
proposed critical habitat designation, so
section 4(a)(3)(B)(i) of the Act does not
apply.
Exclusions
Application of Section 4(b)(2) of the Act
Section 4(b)(2) of the Act states that
the Secretary shall designate and make
revisions to critical habitat on the basis
of the best available scientific data after
taking into consideration the economic
impact, national security impact, and
any other relevant impact of specifying
any particular area as critical habitat.
The Secretary may exclude an area from
critical habitat if he determines that the
benefits of such exclusion outweigh the
benefits of specifying such area as part
of the critical habitat, unless he
determines, based on the best scientific
data available, that the failure to
designate such area as critical habitat
will result in the extinction of the
species. In making that determination,
the statute on its face, as well as the
legislative history, are clear that the
Secretary has broad discretion regarding
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which factor(s) to use and how much
weight to give to any factor.
Under section 4(b)(2) of the Act, we
may exclude an area from designated
critical habitat based on economic
impacts, impacts on national security,
or any other relevant impacts. In
considering whether to exclude a
particular area from the designation, we
identify the benefits of including the
area in the designation, identify the
benefits of excluding the area from the
designation, and evaluate whether the
benefits of exclusion outweigh the
benefits of inclusion. If the analysis
indicates that the benefits of exclusion
outweigh the benefits of inclusion, the
Secretary may exercise his discretion to
exclude the area only if such exclusion
would not result in the extinction of the
species.
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Exclusions Based on Economic Impacts
Under section 4(b)(2) of the Act, we
consider the economic impacts of
specifying any particular area as critical
habitat. In order to consider economic
impacts, we are preparing an analysis of
the economic impacts of the proposed
critical habitat designation and related
factors. Potential land use sectors that
may be affected by critical habitat
designation include oil and gas
development near the Diamond Y
Spring system and agriculture (irrigated
lands using groundwater withdrawals)
at both spring systems. We also consider
any social impacts that might occur
because of the designation.
We will announce the availability of
the draft economic analysis as soon as
it is completed, at which time we will
seek public review and comment. At
that time, copies of the draft economic
analysis will be available for
downloading from the Internet at
https://www.regulations.gov, or by
contacting the Austin Ecological
Services Field Office directly (see FOR
FURTHER INFORMATION CONTACT section).
During the development of a final
designation, we will consider economic
impacts, public comments, and other
new information, and areas may be
excluded from the final critical habitat
designation under section 4(b)(2) of the
Act and our implementing regulations at
50 CFR 424.19.
Exclusions Based on National Security
Impacts
Under section 4(b)(2) of the Act, we
consider whether there are lands owned
or managed by the Department of
Defense where a national security
impact might exist. In preparing this
proposal, we have determined that the
lands within the proposed designation
of critical habitat for the Phantom Cave
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snail, Phantom springsnail, Diamond Y
Spring snail, Gonzales springsnail,
diminutive amphipod, and Pecos
amphipod are not owned or managed by
the Department of Defense, and,
therefore, we anticipate no impact on
national security. Consequently, the
Secretary does not propose to exert his
discretion to exclude any areas from the
final designation based on impacts on
national security.
Exclusions Based on Other Relevant
Impacts
Under section 4(b)(2) of the Act, we
consider any other relevant impacts, in
addition to economic impacts and
impacts on national security. We
consider a number of factors, including
whether the landowners have developed
any habitat conservation plans or other
management plans for the area, or
whether there are conservation
partnerships that would be encouraged
by designation of, or exclusion from,
critical habitat. In addition, we look at
any tribal issues, and consider the
government-to-government relationship
of the United States with tribal entities.
We also consider any social impacts that
might occur because of the designation.
We are not proposing any exclusions
at this time from the proposed critical
habitat designation under section 4(b)(2)
of the Act based on partnerships,
management, or protection afforded by
cooperative management efforts.
However, we are considering excluding
the San Solomon Spring Unit that is
currently covered under a habitat
conservation plan with Texas Parks and
Wildlife Department for the Phantom
Cave snail, Phantom springsnail, and
diminutive amphipod for management
activities at Balmorhea State Park. This
permit authorizes ‘‘take’’ of the
invertebrates (which were candidates at
the time of issuance) in the State Park
for ongoing management activities while
minimizing impacts to the aquatic
species. The activities included in the
habitat conservation plan are a part of
Texas Parks and Wildlife Department’s
operation and maintenance of the State
Park, including the drawdowns
associated with cleaning the swimming
pool and vegetation management within
´
the refuge canal and cienega. The
habitat conservation plan also calls for
restrictions and guidelines for chemical
use in and near aquatic habitats to avoid
and minimize impacts to the three
aquatic invertebrate species (Service
2009a, pp. 9, 29–32). The habitat
conservation plan, however, provides
no protection from the main threat to
this critical habitat unit—future
declining spring flows due to drought or
groundwater withdrawals. In these
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proposed rules, we are seeking input
from the public as to whether or not the
Secretary should exclude the area
within this habitat conservation plan or
other such areas under management that
benefit the Phantom Cave snail,
Phantom springsnail, Diamond Y Spring
snail, Gonzales springsnail, diminutive
amphipod, and Pecos amphipod from
the final critical habitat designation.
(Please see the Public Comments section
of this document for instructions on
how to submit comments).
Peer Review
In accordance with our joint policy on
peer review published in the Federal
Register on July 1, 1994 (59 FR 34270),
we will seek the expert opinions of at
least three appropriate and independent
specialists regarding these proposed
rules. The purpose of peer review is to
ensure that our critical habitat
designation is based on scientifically
sound data, assumptions, and analyses.
We have invited these peer reviewers to
comment during this public comment
period on our specific assumptions and
conclusions in these proposed
designations of critical habitat.
We will consider all comments and
information received during this
comment period on these proposed
rules during our preparation of a final
determination. Accordingly, the final
decision may differ from this proposal.
Public Hearings
Section 4(b)(5) of the Act provides for
one or more public hearings on this
proposal, if requested. Requests must be
received within 45 days after the date of
publication of these proposed rules in
the Federal Register. Such requests
must be sent to the address shown in
FOR FURTHER INFORMATION CONTACT. We
will schedule public hearings on this
proposal, if any are requested, and
announce the dates, times, and places of
those hearings, as well as how to obtain
reasonable accommodations, in the
Federal Register and local newspapers
at least 15 days before the hearing.
Required Determinations
Regulatory Planning and Review—
Executive Orders 12866 and 13563
Executive Order 12866 provides that
the Office of Information and Regulatory
Affairs (OIRA) will review all significant
rules. The Office of Information and
Regulatory Affairs has determined that
this rule is not significant.
Executive Order 13563 reaffirms the
principles of E.O. 12866 while calling
for improvements in the nation’s
regulatory system to promote
predictability, to reduce uncertainty,
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and to use the best, most innovative,
and least burdensome tools for
achieving regulatory ends. The
executive order directs agencies to
consider regulatory approaches that
reduce burdens and maintain flexibility
and freedom of choice for the public
where these approaches are relevant,
feasible, and consistent with regulatory
objectives. E.O. 13563 emphasizes
further that regulations must be based
on the best available science and that
the rulemaking process must allow for
public participation and an open
exchange of ideas. We have developed
this rule in a manner consistent with
these requirements.
Regulatory Flexibility Act (5 U.S.C. 601
et seq.)
Under the Regulatory Flexibility Act
(RFA; 5 U.S.C. 601 et seq.) as amended
by the Small Business Regulatory
Enforcement Fairness Act (SBREFA) of
1996 (5 U.S.C 801 et seq.), whenever an
agency must publish a notice of
rulemaking for any proposed or final
rule, it must prepare and make available
for public comment a regulatory
flexibility analysis that describes the
effects of the rule on small entities
(small businesses, small organizations,
and small government jurisdictions).
However, no regulatory flexibility
analysis is required if the head of the
agency certifies the rule will not have a
significant economic impact on a
substantial number of small entities.
The SBREFA amended the RFA to
require Federal agencies to provide a
certification statement of the factual
basis for certifying that the rule will not
have a significant economic impact on
a substantial number of small entities.
At this time, we lack the available
economic information necessary to
provide an adequate factual basis for the
required RFA finding. Therefore, we
defer the RFA finding until completion
of the draft economic analysis prepared
under section 4(b)(2) of the Act and
Executive Order 12866. This draft
economic analysis will provide the
required factual basis for the RFA
finding. Upon completion of the draft
economic analysis, we will announce
availability of the draft economic
analysis of the proposed designation in
the Federal Register and reopen the
public comment period for the proposed
designation. We will include with this
announcement, as appropriate, an initial
regulatory flexibility analysis or a
certification that the rule will not have
a significant economic impact on a
substantial number of small entities
accompanied by the factual basis for
that determination. We have concluded
that deferring the RFA finding until
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completion of the draft economic
analysis is necessary to meet the
purposes and requirements of the RFA.
Deferring the RFA finding in this
manner will ensure that we make a
sufficiently informed determination
based on adequate economic
information and provide the necessary
opportunity for public comment.
Energy Supply, Distribution, or Use—
Executive Order 13211
Executive Order 13211 (Actions
Concerning Regulations That
Significantly Affect Energy Supply,
Distribution, or Use) requires agencies
to prepare Statements of Energy Effects
when undertaking certain actions. We
do not expect the designation of this
proposed critical habitat to significantly
affect energy supplies, distribution, or
use due to the small amount of habitat
we are proposing for designation and
the lack of Federal activities that would
be affected by the designation.
Therefore, this action is not a significant
energy action, and no Statement of
Energy Effects is required. However, we
will further evaluate this issue as we
conduct our economic analysis, and
review and revise this assessment as
necessary.
Unfunded Mandates Reform Act (2
U.S.C. 1501 et seq.)
In accordance with the Unfunded
Mandates Reform Act (2 U.S.C. 1501 et
seq.), we make the following findings:
(1) This rule will not produce a
Federal mandate. In general, a Federal
mandate is a provision in legislation,
statute, or regulation that would impose
an enforceable duty upon State, local, or
tribal governments, or the private sector,
and includes both ‘‘Federal
intergovernmental mandates’’ and
‘‘Federal private sector mandates.’’
These terms are defined in 2 U.S.C.
658(5)-(7). ‘‘Federal intergovernmental
mandate’’ includes a regulation that
‘‘would impose an enforceable duty
upon State, local, or tribal governments’’
with two exceptions. It excludes ‘‘a
condition of Federal assistance.’’ It also
excludes ‘‘a duty arising from
participation in a voluntary Federal
program,’’ unless the regulation ‘‘relates
to a then-existing Federal program
under which $500,000,000 or more is
provided annually to State, local, and
tribal governments under entitlement
authority,’’ if the provision would
‘‘increase the stringency of conditions of
assistance’’ or ‘‘place caps upon, or
otherwise decrease, the Federal
Government’s responsibility to provide
funding,’’ and the State, local, or tribal
governments ‘‘lack authority’’ to adjust
accordingly. At the time of enactment,
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these entitlement programs were:
Medicaid; Aid to Families with
Dependent Children work programs;
Child Nutrition; Food Stamps; Social
Services Block Grants; Vocational
Rehabilitation State Grants; Foster Care,
Adoption Assistance, and Independent
Living; Family Support Welfare
Services; and Child Support
Enforcement. ‘‘Federal private sector
mandate’’ includes a regulation that
‘‘would impose an enforceable duty
upon the private sector, except (i) a
condition of Federal assistance or (ii) a
duty arising from participation in a
voluntary Federal program.’’
The designation of critical habitat
does not impose a legally binding duty
on non-Federal Government entities or
private parties. Under the Act, the only
regulatory effect is that Federal agencies
must ensure that their actions do not
destroy or adversely modify critical
habitat under section 7. While nonFederal entities that receive Federal
funding, assistance, or permits, or that
otherwise require approval or
authorization from a Federal agency for
an action, may be indirectly impacted
by the designation of critical habitat, the
legally binding duty to avoid
destruction or adverse modification of
critical habitat rests squarely on the
Federal agency. Furthermore, to the
extent that non-Federal entities are
indirectly impacted because they
receive Federal assistance or participate
in a voluntary Federal aid program, the
Unfunded Mandates Reform Act would
not apply, nor would critical habitat
shift the costs of the large entitlement
programs listed above onto State
governments.
(2) We do not believe that this rule
will significantly or uniquely affect
small governments because the land
proposed for designation is either
privately owned or owned by U.S.
Bureau of Reclamation or the State of
Texas. None of these government
entities fit the definition of ‘‘small
governmental jurisdiction.’’ Therefore, a
Small Government Agency Plan is not
required. However, we will further
evaluate this issue as we conduct our
economic analysis, and review and
revise this assessment if appropriate.
Takings—Executive Order 12630
In accordance with Executive Order
12630 (Government Actions and
Interference with Constitutionally
Protected Private Property Rights), we
will analyze the potential takings
implications of designating critical
habitat for the Phantom Cave snail,
Phantom springsnail, Diamond Y Spring
snail, Gonzales springsnail, diminutive
amphipod, and Pecos amphipod in a
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takings implications assessment. Critical
habitat designation does not affect
landowner actions that do not require
Federal funding or permits, nor does it
preclude development of habitat
conservation programs or issuance of
incidental take permits to permit actions
that do require Federal funding or
permits to go forward. The takings
implications assessment will analyze
whether this proposed designation of
critical habitat for the Phantom Cave
snail, Phantom springsnail, Diamond Y
Spring snail, Gonzales springsnail,
diminutive amphipod, and Pecos
amphipod poses significant takings
implications for lands within or affected
by the designation.
Federalism—Executive Order 13132
In accordance with Executive Order
13132 (Federalism), these proposed
rules do not have significant Federalism
effects. A Federalism assessment is not
required. In keeping with Department of
the Interior and Department of
Commerce policy, we requested
information from, and coordinated
development of, these proposed critical
habitat designations with appropriate
State resource agencies in Texas. The
designation of critical habitat in areas
currently occupied by the Phantom
Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales
springsnail, diminutive amphipod, and
Pecos amphipod imposes no additional
restrictions to those currently in place
and, therefore, has little incremental
impact on State and local governments
and their activities. The designation
may have some benefit to these
governments because the areas that
contain the physical or biological
features essential to the conservation of
the species are more clearly defined,
and the elements of the features of the
habitat necessary to the conservation of
the species are specifically identified.
This information does not alter where
and what federally sponsored activities
may occur. However, it may assist local
governments in long-range planning
(rather than having them wait for caseby-case section 7 consultations to
occur).
Where State and local governments
require approval or authorization from a
Federal agency for actions that may
affect critical habitat, consultation
under section 7(a)(2) would be required.
While non-Federal entities that receive
Federal funding, assistance, or permits,
or that otherwise require approval or
authorization from a Federal agency for
an action, may be indirectly impacted
by the designation of critical habitat, the
legally binding duty to avoid
destruction or adverse modification of
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critical habitat rests squarely on the
Federal agency.
Civil Justice Reform—Executive Order
12988
In accordance with Executive Order
12988 (Civil Justice Reform), the Office
of the Solicitor has determined that the
rule does not unduly burden the judicial
system and that it meets the
requirements of sections 3(a) and 3(b)(2)
of the Order. We have proposed
designating critical habitat in
accordance with the provisions of the
Act. These proposed rules use standard
mapping technology and identify the
elements of physical or biological
features essential to the conservation of
the Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive
amphipod, and Pecos amphipod within
the designated areas to assist the public
in understanding the habitat needs of
the species.
Paperwork Reduction Act of 1995 (44
U.S.C. 3501 et seq.)
This rule does not contain any new
collections of information that require
approval by OMB under the Paperwork
Reduction Act of 1995 (44 U.S.C. 3501
et seq.). This rule will not impose
recordkeeping or reporting requirements
on State or local governments,
individuals, businesses, or
organizations. An agency may not
conduct or sponsor, and a person is not
required to respond to, a collection of
information unless it displays a
currently valid OMB control number.
National Environmental Policy Act (42
U.S.C. 4321 et seq.)
We have determined that
environmental assessments and
environmental impact statements, as
defined under the authority of the
National Environmental Policy Act
(NEPA; 42 U.S.C. 4321 et seq.), need not
be prepared in connection with listing
a species as endangered or threatened
under the Endangered Species Act. We
published a notice outlining our reasons
for this determination in the Federal
Register on October 25, 1983 (48 FR
49244).
It is our position that, outside the
jurisdiction of the U.S. Court of Appeals
for the Tenth Circuit, we do not need to
prepare environmental analyses
pursuant to NEPA in connection with
designating critical habitat under the
Endangered Species Act. We published
a notice outlining our reasons for this
determination in the Federal Register
on October 25, 1983 (48 FR 49244). This
position was upheld by the U.S. Court
of Appeals for the Ninth Circuit
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(Douglas County v. Babbitt, 48 F.3d
1495 (9th Cir. 1995), cert. denied 516
U.S. 1042 (1996)). The range of the
Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive
amphipod, and Pecos amphipod does
not occur in the Tenth Circuit, so a
NEPA analysis will not be conducted.
Clarity of the Rule
We are required by Executive Orders
12866 and 12988 and by the
Presidential Memorandum of June 1,
1998, to write all rules in plain
language. This means that each rule we
publish must:
(1) Be logically organized;
(2) Use the active voice to address
readers directly;
(3) Use clear language rather than
jargon;
(4) Be divided into short sections and
sentences; and
(5) Use lists and tables wherever
possible.
If you feel that we have not met these
requirements, send us comments by one
of the methods listed in the ADDRESSES
section. To better help us revise the
rule, your comments should be as
specific as possible. For example, you
should tell us the numbers of the
sections or paragraphs that are unclearly
written, which sections or sentences are
too long, the sections where you feel
lists or tables would be useful, etc.
Government-to-Government
Relationship with Tribes
In accordance with the President’s
memorandum of April 29, 1994
(Government-to-Government Relations
with Native American Tribal
Governments; 59 FR 22951), Executive
Order 13175 (Consultation and
Coordination with Indian Tribal
Governments), and the Department of
the Interior’s manual at 512 DM 2, we
readily acknowledge our responsibility
to communicate meaningfully with
recognized Federal Tribes on a
government-to-government basis. In
accordance with Secretarial Order 3206
of June 5, 1997 (American Indian Tribal
Rights, Federal-Tribal Trust
Responsibilities, and the Endangered
Species Act), we readily acknowledge
our responsibilities to work directly
with tribes in developing programs for
healthy ecosystems, to acknowledge that
tribal lands are not subject to the same
controls as Federal public lands, to
remain sensitive to Indian culture, and
to make information available to tribes.
We determined that there are no tribal
lands within or near the current or
historic ranges of the Phantom Cave
snail, Phantom springsnail, Diamond Y
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Spring snail, Gonzales springsnail,
diminutive amphipod, and Pecos
amphipod that contain the features
essential for conservation of the species.
Therefore, we are not proposing to
designate critical habitat on tribal lands.
List of Subjects in 50 CFR Part 17
References Cited
A complete list of references cited in
this rulemaking is available on the
Internet at https://www.regulations.gov at
Docket No. FWS–R2–ES–2012–0029 and
upon request from the Austin Ecological
Services Field Office (see FOR FURTHER
INFORMATION CONTACT).
Proposed Regulation Promulgation
Endangered and threatened species,
Exports, Imports, Reporting and
recordkeeping requirements,
Transportation.
Accordingly, we propose to amend
part 17, subchapter B of chapter I, title
50 of the Code of Federal Regulations,
as set forth below:
1. The authority citation for part 17
continues to read as follows:
Historic range
*
Scientific name
*
*
*
(h) * * *
*
*
Authority: 16 U.S.C. 1361–1407; 16 U.S.C.
1531–1544; 16 U.S.C. 4201–4245; Pub. L. 99–
625, 100 Stat. 3500; unless otherwise noted.
Species
Common name
§ 17.11 Endangered and threatened
wildlife.
*
PART 17—[AMENDED]
Authors
The primary authors of this package
are the staff members of the Southwest
Region of the Service.
2. In § 17.11(h) add entries for ‘‘Snail,
Diamond Y Spring’’, ‘‘Snail, Phantom
Cave’’, ‘‘Springsnail, Gonzales’’, and
‘‘Springsnail, Phantom’’ under
‘‘SNAILS’’ and ‘‘Amphipod,
diminutive’’ and ‘‘Amphipod, Pecos’’
under ‘‘CRUSTACEANS’’ to the List of
Endangered and Threatened Wildlife in
alphabetical order to read as follows:
*
*
Vertebrate
population where
endangered or
threatened
*
When
listed
Status
*
Critical
habitat
Special
rules
*
SNAILS:
*
*
Snail, Diamond Y Spring ..........
*
Pseudotryonia adamantina .....
*
U.S.A. (TX) .......
*
NA .......................
E .......
.............
17.95(f)
NA
*
*
Snail, Phantom Cave ...............
*
Pyrgulopsis texana .................
*
U.S.A. (TX) .......
*
NA .......................
*
E .......
.............
*
17.95(f)
NA
*
*
Springsnail, Gonzales ..............
*
Tryonia circumstriata ..............
*
U.S.A. (TX) .......
*
NA .......................
E .......
.............
17.95(f)
NA
*
*
Springsnail, Phantom ...............
*
Tryonia cheatumi ....................
*
U.S.A. (TX) .......
*
NA .......................
E .......
.............
17.95(f)
NA
U.S.A. (TX) .......
NA .......................
E .......
*
*
Amphipod, Pecos .....................
*
Gammarus pecos ...................
*
U.S.A. (TX) .......
*
NA .......................
E .......
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*
3. Amend § 17.95 by:
a. In paragraph (f), adding an entry for
‘‘Diamond Y Spring snail
(Pseudotryonia adamantina) and
Gonzales springsnail (Tryonia
circumstriata)’’ followed by an entry for
‘‘Phantom Cave snail (Pyrgulopsis
texana) and Phantom springsnail
(Tryonia cheatumi)’’ after the entry for
‘‘Interrupted Rocksnail (Leptoxis
foremani)’’, to read as follows:
b. In paragraph (h), adding an entry
for ‘‘Diminutive amphipod (Gammarus
hyalleloides)’’ and an entry for ‘‘Pecos
amphipod (Gammarus pecos)’’ in the
same alphabetical order that these
species appear in the table at § 17.11(h),
to read as follows.
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*
*
§ 17.95
Critical habitat—fish and wildlife.
*
*
*
*
(f) Clams and Snails.
*
*
*
*
*
Diamond Y Spring snail (Pseudotryonia
adamantina) and Gonzales springsnail
(Tryonia circumstriata)
(1) A critical habitat unit is depicted
for Pecos County, Texas, on the map
below.
(2) Within this area, the primary
constituent elements of the physical or
biological features essential to the
conservation of Diamond Y Spring snail
and Gonzales springsnail are springs
and spring-fed aquatic systems that
contain:
(i) Permanent, flowing, unpolluted
water (free from contamination)
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*
Sfmt 4702
*
.............
17.95(h)
.............
*
17.95(h) NA
*
*
*
*
*
Gammarus hyalleloides ..........
*
*
*
*
*
*
CRUSTACEANS:
Amphipod, diminutive ...............
*
*
*
*
NA
*
emerging from the ground and flowing
on the surface;
(ii) Water temperatures that vary
between 11 and 27 °C (52 to 81 °F) with
natural seasonal and diurnal variations
slightly above and below that range;
(iii) Substrates that include cobble,
gravel, pebble, sand, silt, and aquatic
vegetation, for breeding, egg laying,
maturing, feeding, and escape from
predators;
(iv) Abundant food, consisting of
algae, bacteria, decaying organic
material, and submergent vegetation
that contributes the necessary nutrients,
detritus, and bacteria on which these
species forage; and
(v) Either an absence of nonnative
predators and competitors or nonnative
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predators and competitors at low
population levels.
(3) Critical habitat does not include
manmade structures (such as buildings,
aqueducts, runways, roads, and other
paved areas) and the land on which they
are located existing within the legal
boundaries on the effective date of this
rule.
(4) Critical habitat map unit. Data
layers defining the map unit were
created on 2010 aerial photography from
U.S. Department of Agriculture,
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National Agriculture Imagery Program
base maps using ArcMap
(Environmental Systems Research
Institute, Inc.), a computer geographic
information system (GIS) program. The
maps in this entry, as modified by any
accompanying regulatory text, establish
the boundaries of the critical habitat
designation. The coordinates or plot
points or both on which each map is
based are available to the public at the
Service’s internet site, (https://
www.fws.gov/southwest/es/
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AustinTexas/), Regulations.gov (https://
www.regulations.gov at Docket No.
FWS–R2–ES–2012–0029) and at the
field office responsible for this
designation. You may obtain field office
location information by contacting one
of the Service regional offices, the
addresses of which are listed at 50 CFR
2.2.
(5) Diamond Y Spring Unit, Pecos
County, Texas. Map of Diamond Y
Spring Unit follows:
BILLING CODE 4310–55–P
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Phantom Cave snail (Pyrgulopsis
texana) and Phantom springsnail
(Tryonia cheatumi)
(1) Critical habitat units are depicted
for Jeff Davis County and Reeves
County, Texas, on the maps below.
(2) Within these areas, the primary
constituent elements of the physical or
biological features essential to the
conservation of Phantom Cave snail and
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Phantom springsnail are springs and
spring-fed aquatic systems that contain:
(i) Permanent, flowing, unpolluted
water (free from contamination)
emerging from the ground and flowing
on the surface;
(ii) Water temperatures that vary
between 11 and 27 °C (52 to 81 °F) with
natural seasonal and diurnal variations
slightly above and below that range;
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49641
(iii) Substrates that include cobble,
gravel, pebble, sand, silt, and aquatic
vegetation, for breeding, egg laying,
maturing, feeding, and escape from
predators;
(iv) Abundant food, consisting of
algae, bacteria, decaying organic
material, and submergent vegetation
that contributes the necessary nutrients,
detritus, and bacteria on which these
species forage; and
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(v) Either an absence of nonnative
predators and competitors or nonnative
predators and competitors at low
population levels.
(3) Critical habitat does not include
manmade structures (such as buildings,
aqueducts, runways, roads, and other
paved areas) and the land on which they
are located existing within the legal
boundaries on the effective date of this
rule.
(4) Critical habitat map units. Data
layers defining map units were created
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on 2010 aerial photography from U.S.
Department of Agriculture, National
Agriculture Imagery Program base maps
using ArcMap (Environmental Systems
Research Institute, Inc.), a computer
geographic information system (GIS)
program. The maps in this entry, as
modified by any accompanying
regulatory text, establish the boundaries
of the critical habitat designation. The
coordinates or plot points or both on
which each map is based are available
to the public at the Service’s Internet
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site (https://www.fws.gov/southwest/es/
AustinTexas/), Regulations.gov (https://
www.regulations.gov at Docket No.
FWS–R2–ES–2012–0029) and at the
field office responsible for this
designation. You may obtain field office
location information by contacting one
of the Service regional offices, the
addresses of which are listed at 50 CFR
2.2.
(5) San Solomon Spring Unit, Reeves
County, Texas. Map of San Solomon
Spring Unit follows:
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provided at subparagraph (5) of this
entry.
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(7) East Sandia Spring Unit, Jeff Davis
County, Texas. Map of East Sandia
Spring Unit follows:
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(6) Giffin Spring Unit, Reeves County,
Texas. Map of Giffin Spring Unit is
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(8) Phantom Lake Spring Unit, Jeff
Davis County, Texas. Map of Phantom
Lake Spring Unit follows:
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*
*
*
*
*
(h) Crustaceans.
Diminutive amphipod (Gammarus
hyalleloides)
(1) Critical habitat units are depicted
for Jeff Davis County and Reeves
County, Texas, on the maps below.
(2) Within these areas, the primary
constituent elements of the physical or
biological features essential to the
conservation of diminutive amphipod
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are springs and spring-fed aquatic
systems that contain:
(i) Permanent, flowing, unpolluted
water (free from contamination)
emerging from the ground and flowing
on the surface;
(ii) Water temperatures that vary
between 11 and 27 °C (52 to 81 °F) with
natural seasonal and diurnal variations
slightly above and below that range;
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49645
(iii) Substrates that include cobble,
gravel, pebble, sand, silt, and aquatic
vegetation, for breeding, maturing,
feeding, and escape from predators;
(iv) Abundant food, consisting of
algae, bacteria, decaying organic
material, and submergent vegetation
that contributes the necessary nutrients,
detritus, and bacteria on which these
species forage; and
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(v) Either an absence of nonnative
predators and competitors or nonnative
predators and competitors at low
population levels.
(3) Critical habitat does not include
manmade structures (such as buildings,
aqueducts, runways, roads, and other
paved areas) and the land on which they
are located existing within the legal
boundaries on the effective date of this
rule.
(4) Critical habitat map units. Data
layers defining map units were created
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on 2010 aerial photography from U.S.
Department of Agriculture, National
Agriculture Imagery Program base maps
using ArcMap (Environmental Systems
Research Institute, Inc.), a computer
geographic information system (GIS)
program. The maps in this entry, as
modified by any accompanying
regulatory text, establish the boundaries
of the critical habitat designation. The
coordinates or plot points or both on
which each map is based are available
to the public at the Service’s Internet
PO 00000
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Sfmt 4702
site (https://www.fws.gov/southwest/es/
AustinTexas/), Regulations.gov (https://
www.regulations.gov at Docket No.
FWS–R2–ES–2012–0029) and at the
field office responsible for this
designation. You may obtain field office
location information by contacting one
of the Service regional offices, the
addresses of which are listed at 50 CFR
2.2.
(5) San Solomon Spring Unit, Reeves
County, Texas. Map of San Solomon
Spring Unit follows:
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(6) Giffin Spring Unit, Reeves County,
Texas. Map of Giffin Spring Unit is
provided at paragraph (5) of this entry.
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(7) East Sandia Spring Unit, Jeff Davis
County, Texas. Map of East Sandia
Spring Unit follows:
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(8) Phantom Lake Spring Unit, Jeff
Davis County, Texas. Map of Phantom
Lake Spring Unit follows:
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Pecos amphipod (Gammarus pecos)
(1) The critical habitat unit is
depicted for Pecos County, Texas, on
the map below.
(2) Within this area, the primary
constituent elements of the physical or
biological features essential to the
conservation of Pecos amphipod are
springs and spring-fed aquatic systems
that contain:
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(i) Permanent, flowing, unpolluted
water (free from contamination)
emerging from the ground and flowing
on the surface;
(ii) Water temperatures that vary
between 11 and 27 °C (52 to 81 °F) with
natural seasonal and diurnal variations
slightly above and below that range;
(iii) Substrates that include cobble,
gravel, pebble, sand, silt, and aquatic
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49649
vegetation, for breeding, maturing,
feeding, and escape from predators;
(iv) Abundant food, consisting of
algae, bacteria, decaying organic
material, and submergent vegetation
that contributes the necessary nutrients,
detritus, and bacteria on which these
species forage; and
(v) Either an absence of nonnative
predators and competitors or nonnative
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49650
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predators and competitors at low
population levels.
(3) Critical habitat does not include
manmade structures (such as buildings,
aqueducts, runways, roads, and other
paved areas) and the land on which they
are located existing within the legal
boundaries on the effective date of this
rule.
(4) Critical habitat map units. Data
layers defining map units were created
on 2010 aerial photography from U.S.
Department of Agriculture, National
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Agriculture Imagery Program base maps
using ArcMap (Environmental Systems
Research Institute, Inc.), a computer
geographic information system (GIS)
program. The maps in this entry, as
modified by any accompanying
regulatory text, establish the boundaries
of the critical habitat designation. The
coordinates or plot points or both on
which each map is based are available
to the public at the Service’s Internet
site (https://www.fws.gov/southwest/es/
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AustinTexas/), Regulations.gov (https://
www.regulations.gov at Docket No.
FWS–R2–ES–2012–0029) and at the
field office responsible for this
designation. You may obtain field office
location information by contacting one
of the Service regional offices, the
addresses of which are listed at 50 CFR
2.2.
(5) Diamond Y Spring Unit, Pecos
County, Texas. Map of Diamond Y
Spring Unit follows:
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*
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Dated: August 2, 2012.
Eileen Sobeck,
Deputy Assistant Secretary for Fish and
Wildlife and Parks.
*
[FR Doc. 2012–19829 Filed 8–15–12; 8:45 am]
BILLING CODE 4310–55–C
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49651
Agencies
[Federal Register Volume 77, Number 159 (Thursday, August 16, 2012)]
[Proposed Rules]
[Pages 49601-49651]
From the Federal Register Online via the Government Printing Office [www.gpo.gov]
[FR Doc No: 2012-19829]
[[Page 49601]]
Vol. 77
Thursday,
No. 159
August 16, 2012
Part III
Department of the Interior
-----------------------------------------------------------------------
Fish and Wildlife Service
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50 CFR Part 17
Endangered and Threatened Wildlife and Plants; Endangered Status for
Six West Texas Aquatic Invertebrate Species and Designation of Critical
Habitat; Proposed Rule
Federal Register / Vol. 77 , No. 159 / Thursday, August 16, 2012 /
Proposed Rules
[[Page 49602]]
-----------------------------------------------------------------------
DEPARTMENT OF THE INTERIOR
Fish and Wildlife Service
50 CFR Part 17
[Docket No. FWS-R2-ES-2012-0029; 4500030113]
RIN 1018-AX70
Endangered and Threatened Wildlife and Plants; Endangered Status
for Six West Texas Aquatic Invertebrate Species and Designation of
Critical Habitat
AGENCY: Fish and Wildlife Service, Interior.
ACTION: Proposed rule.
-----------------------------------------------------------------------
SUMMARY: We, the U.S. Fish and Wildlife Service, propose to list as
endangered and propose critical habitat for six west Texas aquatic
invertebrate species under the Endangered Species Act. These actions
are being taken as the result of a court-approved settlement agreement.
These are proposed regulations, and if finalized the effect of these
regulations will be to conserve the species and protect their habitat
under the Endangered Species Act.
DATES: We will accept comments received or postmarked on or before
October 15, 2012. We must receive requests for public hearings, in
writing, at the address shown in FOR FURTHER INFORMATION CONTACT by
October 1, 2012.
ADDRESSES: You may submit comments by one of the following methods:
(1) Electronically: Go to the Federal eRulemaking Portal: https://www.regulations.gov and search for FWS-R2-ES-2012-0029, which is the
docket number for this rulemaking.
(2) By hard copy: Submit by U.S. mail or hand-delivery to: Public
Comments Processing, Attn: FWS-R2-ES-2012-0029; Division of Policy and
Directives Management; U.S. Fish and Wildlife Service; 4401 N. Fairfax
Drive, MS 2042-PDM; Arlington, VA 22203.
We request that you send comments only by the methods described
above. We will post all comments on https://www.regulations.gov. This
generally means that we will post any personal information you provide
us (see the Public Comments section below for more information).
The coordinates, or plot points, or both from which the critical
habitat maps are generated are included in the administrative record
for this rulemaking and are available at (https://www.fws.gov/southwest/es/AustinTexas/), https://www.regulations.gov at Docket No. FWS-R2-ES-
2012-0029, and at the Austin Ecological Services Field Office (see FOR
FURTHER INFORMATION CONTACT). Any additional tools or supporting
information that we may develop for this rulemaking will also be
available at the Fish and Wildlife Service Web site and Field Office
set out above, and may also be included in the preamble and/or at
https://www.regulations.gov.
FOR FURTHER INFORMATION CONTACT: Adam Zerrenner, Field Supervisor, U.S.
Fish and Wildlife Service, Austin Ecological Services Field Office,
10711 Burnet Road, Suite 200, Austin, TX 78758; by telephone 512-490-
0057; or by facsimile 512-490-0974. Persons who use a
telecommunications device for the deaf (TDD) may call the Federal
Information Relay Service (FIRS) at 800-877-8339.
SUPPLEMENTARY INFORMATION:
Executive Summary
This document consists of proposed rules to list six west Texas
aquatic invertebrate species as endangered and propose critical habitat
designations for the six species. The six west Texas aquatic
invertebrate species are: Phantom Cave snail (Pyrgulopsis texana),
Phantom springsnail (Tryonia cheatumi), diminutive amphipod (Gammarus
hyalleloides), Diamond Y Spring snail (Pseudotryonia adamantina),
Gonzales springsnail (Tryonia circumstriata), and Pecos amphipod
(Gammarus pecos). The current range for the first three species is
limited to spring outflows in the San Solomon Springs system near
Balmorhea in Reeves and Jeff Davis Counties, Texas. The current range
of the latter three species is restricted to spring outflow areas
within the Diamond Y Spring system north of Fort Stockton in Pecos
County, Texas.
Why we need to publish a rule. Under the Endangered Species Act, a
species may warrant protection through listing if it is endangered or
threatened throughout all or a significant portion of its range. In
this proposal we are explaining why these six species warrant
protection under the Endangered Species Act. Five of the six species of
aquatic invertebrates are currently identified as candidates for
listing based on threats to their habitat. The table below summarizes
the status of each species:
------------------------------------------------------------------------
Species Present range Status of species
------------------------------------------------------------------------
Phantom Cave snail.......... San Solomon Spring common in a very
system (four restricted range.
springs).
Phantom Lake springsnail.... San Solomon Spring very rare in a very
system (four restricted range.
springs).
diminutive amphipod......... San Solomon Spring common in a very
system (four restricted range.
springs).
Diamond Y Spring snail...... Diamond Y Spring very rare in a very
system (two restricted range.
springs).
Gonzales springsnail........ Diamond Y Spring very rare in a very
system (two restricted range.
springs).
Pecos amphipod.............. Diamond Y Spring common in a very
system (two restricted range
springs).
------------------------------------------------------------------------
These rules propose that all six of these species should be listed
as endangered. We are proposing a listing status of endangered for
these six species of aquatic invertebrates from west Texas.
The Endangered Species Act provides the basis for our action. Under
the Endangered Species Act, we can determine that a species is
endangered or threatened based on any of five factors: (A) The present
or threatened destruction, modification, or curtailment of its habitat
or range; (B) Overutilization for commercial, recreational, scientific,
or educational purposes; (C) Disease or predation; (D) The inadequacy
of existing regulatory mechanisms; or (E) Other natural or manmade
factors affecting its continued existence. We are proposing that all
six species are endangered by the combined effects of:
Habitat loss and degradation of aquatic resources,
particularly the current and ongoing decline in spring flows that
support the habitat of all the species, and the potential for future
water contamination at the Diamond Y Spring system.
Inadequate existing regulatory mechanisms that allow
significant threats such as groundwater withdrawal.
Other natural or manmade factors, including the presence
of nonnative snails and the small, reduced ranges of the species.
These rules also propose designation of critical habitat for each
of the six species. Under the Endangered Species Act, we designate
specific areas as
[[Page 49603]]
critical habitat to foster conservation of listed species. Future
actions funded, permitted, or otherwise carried out by Federal agencies
will be reviewed to ensure they do not adversely modify critical
habitat. Critical habitat does not affect private actions on private
lands. We are proposing the following areas in Texas as critical
habitat for Phantom Cave snail, Phantom springsnail, and diminutive
amphipod:
------------------------------------------------------------------------
Size of unit in
Critical habitat unit Land ownership by type hectares (acres)
------------------------------------------------------------------------
San Solomon Spring, Reeves State--Texas Parks and 1.8 (4.4)
County. Wildlife Department.
Giffin Spring, Reeves County.. Private............... 0.7 (1.7)
East Sandia Spring, Reeves Private--The Nature 1.2 (3.0)
County. Conservancy.
Phantom Lake Spring, Jeff Federal--Bureau of 0.02 (0.05)
Davis County. Reclamation.
-----------------------------------------
Total..................... ...................... 3.7 (9.2)
------------------------------------------------------------------------
Note: Area sizes may not sum due to rounding.
We are proposing the following areas as critical habitat for
Diamond Y Spring snail, Gonzales springsnail, and Pecos amphipod:
------------------------------------------------------------------------
Size of unit in
Critical habitat unit Land ownership by type hectares (acres)
------------------------------------------------------------------------
Diamond Y Spring System, Pecos Private--The Nature 178.6 (441.4)
County. Conservancy.
-----------------------------------------
Total..................... ...................... 178.6 (441.4)
------------------------------------------------------------------------
We are preparing an economic analysis. We are preparing an economic
analysis of the proposed designations of critical habitat to allow for
consideration of the economic impacts of the proposed designations of
critical habitat. We will publish an announcement and seek public
comments on the draft economic analysis when it is completed.
We will request peer review of the methods used in our proposal. We
are seeking comments from independent specialists with scientific
expertise in these species or related fields. We have invited these
peer reviewers to comment on the scientific information and methods
that we used in making this proposal. Because we will consider all
comments and information received during the comment period, our final
determinations may differ from this proposal.
We are seeking public comment on these proposed rules. Anyone is
welcome to comment on our proposal or provide additional information on
the proposal that we can use in making a final determination on the
status of these species. Please submit your comments and materials
concerning these proposed rules by one of the methods listed in the
ADDRESSES section. Within 1 year following the publication of this
proposal, we will publish in the Federal Register a final determination
to list one or more of these species as threatened or endangered, or
withdraw the proposals if new information is provided that supports
that decision.
Public Comments
We intend that any final action resulting from these proposed rules
will be based on the best scientific and commercial data available and
be as accurate and as effective as possible. Therefore, we request
comments or information from the public, other concerned governmental
agencies, Native American tribes, the scientific community, industry,
or any other interested parties concerning these proposed rules. We
particularly seek comments concerning:
(1) Biological, commercial trade, or other relevant data concerning
any threats (or lack thereof) to this species and regulations that may
be addressing those threats.
(2) Additional information concerning the historical and current
status, range, distribution, and population size of this species,
including the locations of any additional populations of this species.
(3) Any information on the biological or ecological requirements of
the species, and ongoing conservation measures for the species and its
habitat.
(4) Current or planned activities in the areas occupied by the
species and possible impacts of these activities on this species.
(5) The reasons why we should or should not designate habitat as
``critical habitat'' under section 4 of the Act (16 U.S.C. 1531 et
seq.) including whether there are threats to the species from human
activity, the degree of which can be expected to increase due to the
designation, and whether that increase in threat outweighs the benefit
of designation such that the designation of critical habitat may not be
prudent.
(6) Specific information on:
(a) The amount and distribution of habitat for the six west Texas
aquatic invertebrates;
(b) What areas, that were occupied at the time of listing (or are
currently occupied) and that contain features essential to the
conservation of the species, should be included in the designation and
why;
(c) Special management considerations or protection that may be
needed in critical habitat areas we are proposing, including managing
for the potential effects of climate change; and
(d) What areas not occupied at the time of listing are essential
for the conservation of the species and why.
(7) Land use designations and current or planned activities in the
subject areas and their possible impacts on proposed critical habitat.
(8) Information on the projected and reasonably likely impacts of
climate change on the six west Texas aquatic invertebrates and proposed
critical habitat.
(9) Any probable economic, national security, or other relevant
impacts of designating any area that may be included in the final
designation; in particular, any impacts on small entities or families,
and the benefits of including or excluding areas that exhibit these
impacts.
(10) Whether any specific areas we are proposing for critical
habitat designation should be considered for exclusion under section
4(b)(2) of the Act, and whether the benefits of
[[Page 49604]]
potentially excluding any specific area outweigh the benefits of
including that area under section 4(b)(2) of the Act.
(11) Whether the benefits of exclusion outweigh the benefits of
including the area proposed as critical habitat around San Solomon
Spring at Balmorhea State Park based on the existing habitat
conservation plan or other relevant factors.
(12) Whether we could improve or modify our approach to designating
critical habitat in any way to provide for greater public participation
and understanding, or to better accommodate public concerns and
comments.
Please note that submissions merely stating support for or
opposition to the action under consideration without providing
supporting information, although noted, will not be considered in
making a determination, as section 4(b)(1)(A) of the Act directs that
determinations as to whether any species is a threatened or endangered
species must be made ``solely on the basis of the best scientific and
commercial data available.''
You may submit your comments and materials concerning these
proposed rules by one of the methods listed in the ADDRESSES section.
We request that you send comments only by the methods described in the
ADDRESSES section.
If you submit information via https://www.regulations.gov, your
entire submission--including any personal identifying information--will
be posted on the Web site. If your submission is made via a hardcopy
that includes personal identifying information, you may request at the
top of your document that we withhold this information from public
review. However, we cannot guarantee that we will be able to do so. We
will post all hardcopy submissions on https://www.regulations.gov.
Please include sufficient information with your comments to allow us to
verify any scientific or commercial information you include.
Comments and materials we receive, as well as supporting
documentation we used in preparing these proposed rules, will be
available for public inspection on https://www.regulations.gov, or by
appointment, during normal business hours, at the U.S. Fish and
Wildlife Service, Austin Ecological Services Field Office (see FOR
FURTHER INFORMATION CONTACT).
Previous Federal Actions
We first proposed the Phantom Cave snail and Phantom springsnail as
endangered species on April 28, 1976 (41 FR 17742). At that time, the
Phantom Cave snail (Pyrgulopsis texana) was referred to as the Reeves
County snail (Cochliopa texana), and the Phantom springsnail was
referred to as the Cheatum's snail. The proposal was withdrawn on March
6, 1979 (44 FR 12382), following 1978 amendments to the Act that made
additional requirements necessary for designating critical habitat.
Both species were added as candidates for listing in the May 22, 1984,
Notice of Review of Invertebrate Wildlife for Listing as Endangered or
Threatened Species (49 FR 21664). At that time they were categorized as
Category 2 Candidates, which meant that we had information that
proposed listing is possibly appropriate, but conclusive data on
biological vulnerability and threats was not available to support a
proposed rule at the time. They remained so designated in our
subsequent annual Candidate Notices of Review (54 FR 554, January 6,
1989; 56 FR 58804, November 21, 1991; and 59 FR 58982, November 15,
1994). In the February 28, 1996, Notice (61 FR 7596), we discontinued
the designation of Category 2 species as candidates, which removed
these two species from the candidate list.
Both species were then added back to the candidate list on October
30, 2001 (66 FR 54808). Species on the candidate list are those fish,
wildlife, and plants for which we have on file sufficient information
on biological vulnerability and threats to support preparation of a
listing proposal, but for which development of a listing regulation is
precluded by other higher priority listing activities. Since 2001, the
listing priority number for both species has been a 2, reflecting
species with threats that are both imminent and high in magnitude in
accordance with our priority guidance published on September 21, 1983
(48 FR 43098). These two snails remained candidates in subsequent
Candidate Notices of Review (67 FR 40657, June 13, 2002; 69 FR 24876,
May 4, 2004). Both species were also petitioned for listing on May 11,
2004, and were found to be warranted for listing but precluded by
higher priority activities in subsequent Candidate Notice of Reviews
(70 FR 24870, May 11, 2005; 71 FR 53756, September 12, 2006; 72 FR
69034, December 6, 2007; 73 FR 75176, December 10, 2008; 74 FR 57804,
November 9, 2009; and 75 FR 69222, November 10, 2010). The October 26,
2011, Candidate Notice of Review (76 FR 66370) stated that we were
working on proposed listing rules for these species.
We identified the Diamond Y Spring snail and Gonzales springsnail
as candidates for listing in the January 6, 1989, Endangered or
Threatened Wildlife and Plants, Annual Notice of Review (54 FR 554).
These snails were designated as Category 1 candidates, indicating we
had substantial information to support listing, but a proposed rule was
precluded by other listing activities. These two species were included
in all of our subsequent annual Candidate Notices of Review even after
discontinuing the candidate categories (56 FR 58804, November 21, 1991,
and 59 FR 58982, November 15, 1994). From 1996 to 1999 these two
species had a listing priority number of 5, reflecting species with
high magnitude but nonimminent threats (61 FR 7596, February 28, 1996;
62 FR 49398, September 19, 1997; and 64 FR 57534, October 25, 1999). In
2001 we elevated the listing priority number from 5 to 2 because of a
new, imminent threat associated with the introduction of nonnative
snails into the species' habitat. A listing priority of 2 indicates
both high magnitude and imminent threats. Both species have maintained
a listing priority of 2 since then (66 FR 54808, October 30, 2001; 67
FR 40657, June 13, 2002; and 69 FR 24876, May 4, 2004). These two
species were also petitioned for listing on May 11, 2004, and were
found to be warranted for listing but precluded by higher priority
activities in subsequent Candidate Notice of Reviews (70 FR 24870, May
11, 2005; 71 FR 53756, September 12, 2006; 72 FR 69034, December 6,
2007; 73 FR 75176, December 10, 2008; 74 FR 57804, November 9, 2009;
and 75 FR 69222, November 10, 2010). The October 26, 2011, Candidate
Notice of Review (76 FR 66370) stated that we were working on proposed
listing rules for these species.
We identified the diminutive amphipod and Pecos amphipod as
Category 2 candidate species for listing in the May 22, 1984, Notice of
Review of Invertebrate Wildlife for Listing as Endangered or Threatened
Species (49 FR 21664). They remained so designated in our subsequent
annual Candidate Notices of Review (54 FR 554, January 6, 1989; 56 FR
58804, November 21, 1991; and 59 FR 58982, November 15, 1994). In the
February 28, 1996, Notice (61 FR 7596), we discontinued the designation
of Category 2 species as candidates, which removed these two species
from the candidate list. The diminutive amphipod was added back to the
candidate list on May 11, 2005 (70 FR 24870), and has remained a
candidate with a listing priority number of 2 (reflecting both high-
magnitude and imminent threats) since that time (71 FR 53756, September
12, 2006; 72 FR
[[Page 49605]]
69034, December 6, 2007; 73 FR 75176, December 10, 2008; 74 FR 57804,
November 9, 2009; and 75 FR 69222, November 10, 2010). The October 26,
2011, Candidate Notice of Review (76 FR 66370) stated that we were
working on a proposed listing rule for the diminutive amphipod.
The Pecos amphipod was not included in recent candidate notices
along with the other species in this proposal because of taxonomic
uncertainties, which have since been resolved. In the past it was
unclear whether this species range was limited to Diamond Y Spring.
Recent genetic research has confirmed that the species is endemic to
Diamond Y Spring (see full discussion below under Taxonomy,
Distribution, and Abundance of Amphipods, Pecos Amphipod). The Pecos
amphipod was included in the June 25, 2007, petition by WildEarth
Guardians to the Service seeking the listing of 475 species in the
southwestern United States. On January 6, 2009, we published a partial
90-day finding of the petition for listing 475 species which included a
finding that the petition did not present substantial scientific or
commercial information indicating that the listing of the Pecos
amphipod may be warranted (74 FR 419). During our current review of the
other species endemic to the Diamond Y Spring system, we reviewed the
status of the Pecos amphipod. Based on the results of that review, we
are proposing to list it as endangered.
Background
We intend to discuss below only those topics directly relevant to
the consideration of the listing of the six west Texas aquatic
invertebrates as endangered and proposed critical habitat designations.
We have organized this Background section into three parts. The first
part is a general description of the two primary spring systems where
the six species occur. The second part is a general description of the
life history and biology of the four snail species, followed by
specific biological information on each of the four snail species. The
third part is a general description of the life history and biology of
the two amphipod species, followed by specific biological information
on each of the two amphipod species.
Description of Chihuahuan Desert Springs Inhabited by Invertebrate
Species
The six west Texas aquatic invertebrate species (Phantom Cave
snail, Phantom springsnail, diminutive amphipod, Diamond Y Spring
snail, Gonzales springsnail, and Pecos amphipod) occur within a
relatively small area of the Chihuahuan Desert of the Pecos River
drainage basin of west Texas. The habitats of these species are now
isolated spring systems in expansive carbonate (limestone) deposit. The
region includes a complex of aquifers (underground water systems) where
the action of water on soluble rocks (like limestone and dolomite) has
formed abundant ``karst'' features such as sinkholes, caverns, springs,
and underground streams. These hydrogeological formations provide
unique settings where a diverse assemblage of flora and fauna has
evolved at the points where the aquifers discharge waters to the
surface through spring openings. The isolated limestone and gypsum
springs, seeps, and wetlands located in this part of west Texas provide
the only known habitats for several endemic species of fish, plants,
mollusks, and crustaceans, including the six endemic aquatic
invertebrate species addressed in these proposed rules.
In the Chihuahuan Desert, spring-adapted aquatic species are
distributed in isolated, geographically separate populations. They
likely evolved into distinct species from parent species that once
enjoyed a wider distribution during wetter, cooler climates of the
Pleistocene epoch (about 10,000 to 2.5 million years before present).
As ancient lakes and streams dried during dry periods (since the Late
Pleistocene, within about the last 100,000 years), aquatic species in
this region became patchily distributed across the landscape as
geographically isolated populations exhibiting a high degree of
endemism (species found only in a particular region, area, or spring).
Such speciation through divergence has been reported for these species
(Gervasio et al. 2004, p. 521; Brown et al. 2008, pp. 486-487; Seidel
et al. 2009, p. 2304).
San Solomon Spring System
In these proposed rules we reference the San Solomon Spring system
to include four different existing spring outflows: San Solomon Spring,
Giffin Spring, Phantom Lake Spring, and East Sandia Spring. The springs
in this area are also commonly referred to by some authors as Toyah
Basin springs or Balmorhea area springs. All of the springs
historically drained into Toyah Creek, an intermittent tributary of the
Pecos River that is now dry except following large rainfall events. All
four springs are located in proximity to one another; it is about 13
kilometers (km) (8 miles (mi)) between the farthest two (East Sandia
Spring to Phantom Lake Spring). Brune (1981, pp. 258-259, 382-386)
provides a brief overview of each of these springs and documents their
declining flows during the early and middle twentieth century.
The San Solomon Spring system is located in the Chihuahuan Desert
of west Texas at the foothills of the Davis Mountains near Balmorhea,
Texas. Phantom Lake Spring is in Jeff Davis County (on the county
boundary with Reeves County), while the other major springs in this
system are in Reeves County. In addition to being an important habitat
for rare aquatic fauna, area springs have served for centuries as an
important source of irrigation water for local farming communities.
They are all located near the small town of Balmorhea (current
population of less than 500 people) in west Texas. The area is very
rural with no nearby metropolitan centers. Land ownership in the region
is mainly private, except as described below around the spring
openings, and land use is predominantly dry-land ranching with some
irrigated farmland.
The base flows from all of these springs are thought to ultimately
originate from a regional groundwater flow system. Studies show that
groundwater moves through geologic faults from the Salt Basin northwest
of the Apache and Delaware Mountains, located 130 km (80 mi) or more to
the west of the springs (Sharp 2001, pp. 42-45; Angle 2001, p. 247;
Sharp et al. 2003, pp. 8-9; Chowdhury et al. 2004, pp. 341-342; Texas
Water Development Board 2005, p. 106). The originating groundwater and
spring outflow are moderately to highly mineralized and appear to be of
ancient origin, with the water being estimated at 10,000 to 18,000
years old (Chowdhury et al. 2004, p. 340; Texas Water Development Board
2005, p. 89). The Salt Basin Bolson aquifer is part of the larger West
Texas Bolsons and is made up of connected sub-basins underlying Wild
Horse, Michigan, Lobo, and Ryan Flats, in the middle and southern Salt
Basin Valley in Texas (Angle, 2001, p. 242). (The term bolson is of
Spanish origin and refers to a flat-floored desert valley that drains
to a playa or flat.) These aquifers, which support the base flows
(flows not influenced by seasonal rainfall events) of the San Solomon
Spring system, receive little to no modern recharge from precipitation
(Scanlon et al. 2001, p. 28; Beach et al. 2004, pp. 6-9, 8-9). Studies
of the regional flow system indicate groundwater may move from south to
north through the Salt Basin from Ryan to Lobo to Wild Horse Flats
before being discharged through the Capitan
[[Page 49606]]
Formation, into the Lower Cretaceous rocks (older than Pleistocene) via
large geologic faults then exiting to the surface at the springs
(LaFave and Sharp 1987, pp. 7-12; Angle 2001, p. 247; Sharp 2001, p.
42-45; Chowdhury et al. 2004, pp. 341-342; Beach et al. 2004, Figure
4.1.13, p. 4-19, 4-53). Chemical analysis and hydrogeological studies
support this hypothesis, and the water elevations throughout these
parts of the Salt Basin Bolson aquifer are higher in elevation than the
discharge points at the springs (Chowdhury et al. 2004, p. 342).
In contrast to the base flows, the springs also respond with
periodic short-term increases in flow rates following local, seasonal
rainstorms producing runoff events through recharge areas from the
Davis Mountains located to the southwest of the springs (White et al.
1941, pp. 112-119; LaFave and Sharp 1987, pp. 11-12; Chowdhury et al.
2004, p. 341). These freshwater recharge events provide very temporary
increases in spring flows, sometimes resulting in flow spikes many
times larger than the regular base flows. The increased flows are
short-lived until the local stormwater recharge is drained away and
spring flows return to base flows supported by the distant aquifers.
Historically, many of the springs in this spring system were likely
periodically interconnected following storm events with water flowing
throughout the Toyah Creek watershed. In recent times, however, manmade
structures altered the patterns of spring outflows and stormwater
runoff, largely isolating the springs from one another except through
irrigation canals.
San Solomon Spring is by far the largest single spring in the Toyah
Basin (Brune 1981, p. 384). The artesian spring issues from the lower
Cretaceous limestone at an elevation of about 1,008 meters (m) (3,306
feet (ft)). Brune (1981, p. 385) reported spring flows in the range of
1.3 to 0.8 cubic meters per second (cms) (46 to 28 cubic feet per
second (cfs)) between 1900 and 1978 indicating an apparent declining
trend. Texas Water Development Board (2005, p. 84) studies reported an
average flow rate of about 0.85 cms (30 cfs) from data between 1965 to
2001 with a calculated slope showing a slight decline in discharge.
San Solomon Spring now provides the water for the large,
unchlorinated, flow-through swimming pool at Balmorhea State Park and
most of the irrigation water for downstream agricultural irrigation by
the Reeves County Water Improvement District No. 1 (District). The
swimming pool is concrete on the sides and natural substrates on the
bottom and was originally constructed in 1936. Balmorhea State Park is
owned and managed by Texas Parks and Wildlife Department and
encompasses about 19 hectares (ha) (46 acres (ac)) located about 6 km
(4 mi) west of Balmorhea in the historic community of Toyahvale. The
Park provides recreational opportunities of camping, wildlife viewing,
and swimming and scuba diving in the pool. The District holds the water
rights for the spring which is channeled through an extensive system of
concrete-lined irrigation channels, and much of the water is stored in
nearby Lake Balmorhea and delivered through canals for flood irrigation
on farms down gradient (Simonds 1996, p. 2).
Balmorhea State Park's primary wildlife resource focus is on
conservation of the endemic aquatic species that live in the outflow of
San Solomon Spring (Texas Parks and Wildlife Department 1999, p. 1).
Texas Parks and Wildlife Department maintains two constructed
ci[eacute]negas that are flow-through, earth-lined pools in the park to
simulate more natural aquatic habitat conditions for the conservation
of the rare species, including the Phantom Cave snail, Phantom
springsnail, and diminutive amphipods. (Ci[eacute]nega is a Spanish
term that describes a spring outflow that is a permanently wet and
marshy area.) San Solomon Spring is also inhabited by two federally
listed fishes, Comanche Springs pupfish (Cyprinodon elegans) and Pecos
gambusia (Gambusia nobilis). No nonnative fishes are known to occur in
San Solomon Spring, but two nonnative aquatic snails, red-rim melania
(Melanoides tuberculata) and quilted melania (Tarebia granifera), do
occur in the spring outflows and are a cause for concern for the native
aquatic invertebrate species.
Giffin Spring is on private property less than 1.6 km (1.0 mi) west
of Balmorhea State Park, across State Highway 17. The spring originates
from an elevation similar to San Solomon Spring. Brune (1981, p. 385)
reported flow from Giffin Spring ranging from 0.07 to 0.17 cms (2.3 to
5.9 cfs) between 1919 and 1978, with a gradually declining trend.
During calendar year 2011, Giffin Spring flow rates were recorded
between 0.10 and 0.17 cms (3.4 and 5.9 cfs) (U.S. Geological Survey
2012, p. 1). Giffin Spring water flows are captured in irrigation
earthen channels for agricultural use. Giffin Spring is also inhabited
by the federally listed Comanche springs pupfish and Pecos gambusia,
and the only nonnative aquatic species of concern there is the red-rim
melania.
Phantom Lake Spring is at the base of the Davis Mountains about 6
km (4 mi) west of Balmorhea State Park at an elevation of 1,080 m
(3,543 ft). The outflow originates from a large crevice on the side of
a limestone outcrop cliff. The 7-ha (17-ac) site around the spring and
cave opening is owned by the U.S. Bureau of Reclamation. Prior to 1940
the recorded flow of this spring was regularly exceeding 0.5 cms (18
cfs). Outflows after the 1940s were immediately captured in concrete-
lined irrigation canals and provided water for local crops before
connecting to the District's canal system in Balmorhea State Park.
Flows declined steadily over the next 70 years until ceasing completely
in about the year 2000 (Brune 1981, pp. 258-259; Allan 2000, p. 51;
Hubbs 2001, p. 306). The aquatic habitat at the spring pool has been
maintained by a pumping system since then. Phantom Lake Spring is also
inhabited by the two federally listed fishes, Comanche Springs pupfish
and Pecos gambusia, and the only nonnative aquatic species of concern
there is the red-rim melania.
East Sandia Spring is the smallest spring in the system located in
Reeves County in the community of Brogado approximately 3 km (2 mi)
northeast of the town of Balmorhea and 7.7 km (4.8 mi) northeast of
Balmorhea State Park. The spring is within a 97-ha (240-ac) preserve
owned and managed by The Nature Conservancy--a private nonprofit
conservation organization (Karges 2003, pp. 145-146). In contrast to
the other springs in the San Solomon Spring system that are derived
directly from a deep underground regional flow system, East Sandia
Spring discharges from alluvial sand and gravel from a shallow
groundwater source at an elevation of 977 m (3,224 ft) (Brune 1981, p.
385; Schuster 1997, p. 92). Water chemistry at East Sandia Spring
indicates it is not directly hydrologically connected with the other
springs in the San Solomon Spring system in the nearby area (Schuster
1997, pp. 92-93). Historically there was an additional, smaller nearby
spring outlet called West Sandia Spring. Brune (1981, pp. 385-386)
reported the combined flow of East and West Sandia Springs as
declining, with measurements ranging from 0.09 to 0.02 cms (3.2 to 0.7
cfs) between 1932 and 1976. In 1976 outflow from East Sandia was 0.01
cms (0.5 cfs) of the total 0.02 cms (0.7 cfs) of the two springs. In
1995 and 1996 Schuster (1997, p. 94) reported flows from both springs
ranging from 0.12 to 0.01 cms (4.07 cfs to 0.45 cfs),
[[Page 49607]]
with an average of 0.05 cms (1.6 cfs). The outflow waters from the
spring discharge to an irrigation canal within a few hundred meters
from its source. East Sandia Spring is also inhabited by two federally
listed fishes, Comanche Springs pupfish and Pecos gambusia, as well as
the federally endangered Pecos assiminea (Assiminea pecos) snail and
the federally threatened Pecos sunflower (Helianthus paradoxus). No
nonnative aquatic species of concern are known from East Sandia Spring.
Historically there were other area springs along Toyah Creek that
were part of the San Solomon Spring system. Saragosa and Toyah Springs
occurred in the town of Balmorhea along Toyah Creek. Brune (1981, p.
386) reported historic base flows of about 0.2 cms (6 cfs) in the 1920s
and 1940s, declining to about 0.06 cms (2 cfs) in the 1950s and 1960s,
and no flow was recorded in 1978. Brune (1981, p. 385) reported that
the flow from West Sandia Spring was about 0.01 cms (0.2 cfs) in 1976,
after combined flows from East and West Sandia Springs had exceeded
0.07 cms (2.5 cfs) between the 1930s and early 1960s. The Texas Water
Development Board (2005, p. 12) reported West Sandia and Saragosa
Springs did not discharge sufficient flow for measurement. Karges
(2003, p. 145) indicated West Sandia has only intermittent flow and
harbors no aquatic fauna. It is unconfirmed whether the six aquatic
invertebrates discussed in this document occurred in these now dry
spring sites, but given their current distribution in springs located
upstream and downstream of these historic springs, we assume that they
probably did. However, because these springs have been dry for many
decades, they no longer provide habitat for the aquatic invertebrates.
Diamond Y Spring System
The Diamond Y Spring system is within a tributary drainage flowing
northeast to the Pecos River. Diamond Y Spring (previously called
Willbank Spring) is located about 80 km (50 mi) due east of San Solomon
Spring and about 12 km (8 mi) north of the City of Fort Stockton in
Pecos County. The Diamond Y Spring system is composed of disjunct upper
and lower watercourses, separated by about 1 km (0.6 mi) of dry stream
channel.
The upper watercourse is about 1.5 km (0.9 mi) long and starts with
the Diamond Y Spring head pool, which drains into a small spring
outflow channel. The channel enters a broad valley and braids into
numerous wetland areas and is augmented by numerous small seeps. The
Diamond Y Spring outflow converges with the Leon Creek drainage and
flows through a marsh-meadow, where it is then referred to as Diamond Y
Draw. All of the small springs and seeps and their outflow comprise the
upper watercourse. These lateral water features, often not mapped, are
spread across the flat, seasonally wetted area along Diamond Y Draw.
Therefore, unlike other spring systems that have a relatively small
footprint, aquatic habitat covers a relatively large area along the
Diamond Y draw.
The lower watercourse of Diamond Y Draw has a smaller head pool
spring, referred to as Euphrasia Spring, with a small outflow stream as
well as several isolated pools and associated seeps and wetland areas.
The total length of the lower watercourse is about 1 km (0.6 mi) and
has extended below the bridge at State Highway 18 during wetter seasons
in the past. The upper watercourse is only hydrologically connected to
the lower watercourse by surface flows during rare large rainstorm
runoff events. The lower watercourse also contains small springs and
seeps laterally separated from the main spring outflow channels.
Virtually all of the Diamond Y Spring area (both upper and lower
watercourses and the area in between) occurs on the Diamond Y Spring
Preserve, which is owned and managed by The Nature Conservancy. The
Diamond Y Spring Preserve is 1,603 ha (3,962 ac) of contiguous land
around Diamond Y Draw. The surrounding watershed and the land area over
the contributing aquifers are all privately owned and managed as ranch
land and have been developed for oil and gas extraction. In addition, a
natural gas processing plant is located within 0.8 km (0.5 mi) upslope
of the headpool in the upper watercourse of Diamond Y Spring. Diamond Y
Spring is also inhabited by two federally listed fishes, Leon Springs
pupfish (Cyprinodon bovinus) and Pecos gambusia, as well as the
federally endangered Pecos assiminea snail and the federally threatened
Pecos sunflower. The only nonnative species of concern at Diamond Y
Spring is the red-rim melania, which is only known to occur in the
upper watercourse.
Studies by Boghici (1997, p. v) indicate that the spring flow at
Diamond Y Spring originates chiefly from the Rustler aquifer waters
underlying the Delaware Basin to the northwest of the spring outlets
(Boghici and Van Broekhoven 2001, p. 219). The Rustler aquifer
underlies an area of approximately 1,200 sq km (480 sq mi) encompassing
most of Reeves County and parts of Culberson, Pecos, Loving, and Ward
Counties (Boghici and Van Broekhoven 2001, p. 219). Much of the water
contains high total dissolved solids (Boghici and Van Broekhoven 2001,
p. 219) making it difficult for agricultural or municipal use;
therefore, the aquifer has experienced only limited pumping in the past
(Mace 2001, pp. 7-9).
Other springs in the area may have once provided habitat for the
aquatic species but limited information is generally available on
historic distribution of the invertebrates. Leon Springs, a large
spring that historically occurred about 14 km (9 miles) upstream along
Leon Creek, historically discharged about 0.7 cms (25 cfs) in 1920, 0.5
cms (18 cfs) in the 1930s, 0.4 cms (14 cfs) in the 1940s, and no
discharge from 1958 to 1971 (Brune 1981, p. 359). Nearby groundwater
pumping to irrigate farm lands began in 1946, which lowered the
contributing aquifer by 40 m (130 feet) by the 1970s and resulted in
the loss of the spring. The only circumstantial evidence that any of
the three invertebrates that occur in nearby Diamond Y Spring may have
occurred in Leon Springs is that the spring is within the same drainage
and an endemic fish, Leon Springs pupfish, once occurred in both
Diamond Y and Leon Springs.
Comanche Springs is another large historic spring located in the
City of Fort Stockton. Prior to the 1950s, this spring discharged more
than 1.2 cms (42 cfs) (Brune 1981, p. 358) and provided habitat for
rare species of fishes and invertebrates. As a result of groundwater
pumping for agriculture, the spring ceased flowing by 1962 (Brune 1981,
p. 358), eliminating all aquatic-dependent plants and animals (Scudday
1977, pp. 515-518; Scudday 2003, pp. 135-136). Although we do not have
data confirming that Comanche Springs was inhabited by all of the
Diamond Y Spring species, there is evidence that at least the two
snails (Diamond Y Spring snail and Gonzales springsnail) occurred there
at some time in the past (see Taxonomy, Distribution, Abundance, and
Habitat of Snails, below).
Life History and Biology of Snails
The background information presented in this section applies to all
four species of snails in these proposed rules: Phantom Cave snail,
Phantom springsnail, Diamond Y Spring snail, and Gonzales springsnail.
All four of these snails are in the family Hydrobiidae and are strictly
aquatic with respiration occurring through an internal gill. These
hydrobiid snails (snails in the family Hydrobiidae)
[[Page 49608]]
typically reproduce several times during the spring to fall breeding
season (Brown 1991, p. 292) and are sexually dimorphic (males and
females are shaped differently), with females being characteristically
larger and longer-lived than males. Snails in the Pyrgulopsis genus
(Phantom Cave snail) reproduce through laying a single small egg
capsule deposited on a hard surface (Hershler 1998, p. 14). The other
three snail species are ovoviviparous, meaning the larval stage is
completed in the egg capsule, and upon hatching, the snails emerge into
their adult form (Brusca and Brusca 1990, p. 759; Hershler and Sada
2002, p. 256). The lifespan of most aquatic snails is thought to be 9
to 15 months (Taylor 1985, p. 16; Pennak 1989, p. 552).
All of these snails are presumably fine-particle feeders on
detritus (organic material from decomposing organisms) and periphyton
(mixture of algae and other microbes attached to submerged surfaces)
associated with the substrates (mud, rocks, and vegetation) (Allan
1995, p. 83; Hershler and Sada 2002, p. 256; Lysne et al. 2007, p.
649). Dundee and Dundee (1969, p. 207) found diatoms (a group of
single-celled algae) to be the primary component in the digestive
tract, indicating they are a primary food source.
These hydrobiid snails from west Texas occur in mainly flowing
water habitats such as small springs, seeps, marshes, spring pools, and
their outflows. Proximity to spring vents, where water emerges from the
ground, plays a key role in the life history of springsnails. Many
springsnail species exhibit decreased abundance farther away from
spring vents, presumably due to their need for stable water chemistry
(Hershler 1994, p. 68; Hershler 1998, p. 11; Hershler and Sada 2002, p.
256; Martinez and Thome 2006, p. 14). Several habitat parameters of
springs, such as temperature, substrate type, dissolved carbon dioxide,
dissolved oxygen, conductivity, and water depth have been shown to
influence the distribution and abundance of other related species of
springsnails (O'Brien and Blinn 1999, pp. 231-232; Mladenka and
Minshall 2001, pp. 209-211; Malcom et al. 2005, p. 75; Martinez and
Thome 2006, pp. 12-15; Lysne et al. 2007, p. 650). Dissolved salts such
as calcium carbonate may also be important factors because they are
essential for shell formation (Pennak 1989, p. 552). Hydrobiid snails
as a group are considered sensitive to water quality changes, and each
species is usually found within relatively narrow habitat parameters
(Sada 2008, p. 59).
Native fishes have been shown to prey upon these snails (Winemiller
and Anderson 1997, pp. 209-210; Brown et al. 2008, p. 489), but it is
unknown to what degree predatory pressure may play a role in
controlling population abundances or influencing habitat use. There are
currently no nonnative fishes in the springs where the species occur,
so there is no unnatural predation pressure from fish suspected.
Because of their small size and dependence on water, significant
dispersal (in other words, movement between spring systems) does not
likely occur, although on rare occasions aquatic snails have been
transported by becoming attached to the feathers and feet of migratory
birds (Roscoe 1955, p. 66; Dundee et al. 1967, pp. 89-90). In general,
the species have little capacity to move beyond their isolated aquatic
environments.
Taxonomy, Distribution, Abundance, and Habitat of Snails
Phantom Cave Snail (Pyrgulopsis texana Pilsbry 1935)
The Phantom Cave snail was first described by Pilsbry (1935, pp.
91-92). It is a very small snail, measuring only 0.98 to 1.27
millimeters (mm) (0.04 to 0.05 inches (in)) long (Dundee and Dundee
1969, p. 207). Until 2010, the species was placed in the genus
Cochliopa (Dundee and Dundee 1969, p. 209; Taylor 1987, p. 40).
Hershler et al. (2010, pp. 247-250) reviewed the systematics of the
species and transferred Phantom Cave snail to the genus Pyrgulopsis
after morphological and mitochondrial DNA analysis. Hershler et al.
(2010, p. 251) also noted some minimal differences in shell size
(individuals were smaller at East Sandia Spring) and mitochondrial DNA
sequence variation among populations of Phantom Cave snails in
different springs. The low level of variation (small differences) among
the populations did not support recognizing different conservation
units for the species. Hershler et al. (2010, p. 251) expected this
small difference among the populations because of their proximity
(separated by 6 to 13 km (4 to 8 mi)) and the past connectedness of the
aquatic habitats by Toyah Creek that would have allowed mixing of the
populations before human alterations and declining flows. Based on
these published studies we conclude that Phantom Cave snail is a
listable entity under the Act.
The Phantom Cave snail only occurs in the four remaining desert
spring outflow channels associated with the San Solomon Spring system
(San Solomon, Phantom, Giffin, and East Sandia springs). Hershler et
al. (2010, p. 250) did not include Giffin Spring in this species
distribution, but unpublished data from Lang (2011, p. 5) confirms that
the species is also found in Giffin Spring outflows as well as the
other three springs in the San Solomon Spring system. The geographic
extent of the historic range for the Phantom Cave snail was likely not
larger than the present range, but the species may have occurred in
additional small springs contained within the current range of the San
Solomon Spring system, such as Saragosa and Toyah Springs. It likely
also had a larger distribution within Phantom Lake Spring and San
Solomon Spring before the habitat there was modified and reduced in
conversion of spring outflow channels into irrigation ditches.
Within its current, limited range, Phantom Cave snails can exist in
very high densities. Dundee and Dundee (1969, pp. 207) described the
abundance of the Phantom Cave snails at Phantom Lake Spring in 1968 as
persisting ``in such tremendous numbers that the bottom and sides of
the canal appear black from the cover of snails.'' Today the snails are
limited to the small pool at the mouth of Phantom Cave and cannot be
found in the irrigation canal downstream. At San Solomon Spring, Taylor
(1987, p. 41) reported the Phantom Cave snail was abundant and
generally distributed in the canals from 1965 to 1981. Density data and
simple population size estimates based on underwater observations
indicate there may be over 3.8 million individuals of this species at
San Solomon Spring (Bradstreet 2011, p. 55). Lang (2011) also reported
very high densities (not total population estimates) of Phantom Cave
snails (with standard deviations): San Solomon Spring from
2009 sampling in the main canal, 71,740 per sq m (6,672 per sq ft;
47,229 per sq m, 4,393 per sq ft); Giffin
Spring at road crossing in 2001, 4,518 per sq m (420 per sq ft; 4,157 per sq m, 387 per sq ft); East Sandia Spring in
2009, 41,215 per sq m (3,832 per sq ft; 30,587 per sq m,
2,845 per sq ft); and Phantom Lake Spring in 2009, 1,378
per sq m (128 per sq ft; 626 per sq m, 58 per
sq ft). From these data, it is evident that when conditions are
favorable Phantom Cave snails can reach tremendous population sizes in
very small areas.
Phantom Cave snails are found concentrated near the spring source
(Hershler et al. 2010, p. 250) and can occur as far as a few hundred
meters downstream of a large spring outlet like San Solomon Spring.
Despite its common name, it has not been found
[[Page 49609]]
within Phantom Cave proper, but only within the outflow of Phantom Lake
Spring. Bradstreet (2011, p. 55) found the highest abundances of
Phantom Cave snails at San Solomon Spring outflows in the high-velocity
areas in the irrigation canals and the lowest abundances in the San
Solomon Ci[eacute]nega. The species was not collected from the newest
constructed ci[eacute]nega in 2010. Habitat of the species is found on
both soft and firm substrates on the margins of spring outflows (Taylor
1987, p. 41). They are also commonly found attached to plants,
particularly in dense stands of submerged vegetation (Chara sp.). Field
and laboratory experiments have suggested Phantom Cave snails prefer
substrates harder and larger in size (Bradstreet 2011, p. 91).
Phantom Springsnail (Tryonia cheatumi Pilsbry 1935)
The Phantom springsnail was first described by Pilsbry (1935, p.
91) as Potamopyrgus cheatumi. The species was later included in the
genus Lyrodes and eventually placed in the genus Tryonia (Taylor 1987,
pp. 38-39). It is a small snail measuring only 2.9 to 3.6 mm (0.11 to
0.14 in) long (Taylor 1987, p. 39). Systematic studies of Tryonia
snails in the Family Hydrobiidae using mitochondrial DNA sequences and
morphological characters confirms the species is a ``true Tryonia,'' in
other words, it is appropriately classified in the genus Tryonia
(Hershler et al. 1999, p. 383; Hershler 2001, p. 6; Hershler et al.
2011, pp. 5-6). Based on these published studies, we conclude that
Phantom springsnail is a listable entity under the Act.
The Phantom springsnail only occurs in the four remaining desert
spring outflow channels associated with the San Solomon Spring system
(San Solomon, Phantom, Giffin, and East Sandia springs) (Taylor 1987,
p. 40; Allan 2011, p. 1; Lang 2011, entire). The historic range for the
Phantom springsnail was likely not larger than present, but the species
may have occurred in other springs within the San Solomon Spring
system, such as Saragosa and Toyah Springs. It likely also had a wider
distribution within Phantom Lake Spring and San Solomon Spring before
the habitat there was modified and reduced.
Within its current, limited range, Phantom springsnails can have
moderate densities of abundance, but have never been recorded as high
as the Phantom Cave snail. In the 1980s, Taylor (1987, p. 40) described
Phantom springsnails as abundant in the outflow ditch several hundred
meters downstream of Phantom Lake Spring. The snails are now limited to
low densities in the small pool at the mouth of Phantom Cave and cannot
be found in the irrigation canal downstream as it does not have water
(Allan 2009, p. 1). Density data and simple population size estimates
based on underwater observations indicate there may be over 460,000
individuals of this species at San Solomon Spring (Bradstreet 2011, p.
55). Lang (2011) reports the following densities (not population
estimates) of Phantom springsnails (with standard
deviations): San Solomon Spring from 2009 sampling in the main canal,
11,681 per sq m (1,086 per sq ft; 11,925 per sq m, 1,109 per sq ft); Giffin Spring at road crossing in 2001, 3,857
per sq m (358 per sq ft; 6,110 per sq m, 568
per sq ft); East Sandia Spring in 2009, 65,845 per sq m (6,123 per sq
ft; 60,962 per sq m, 5,669 per sq ft); and
Phantom Lake Spring in 2009, 31,462 per sq m (2,926 per sq ft; 20,251 per sq m, 1,883 per sq ft). Phantom
springsnails can reach high population sizes in very small areas with
favorable conditions.
Phantom springsnails are usually found concentrated near the spring
source but once occurred as far as a few hundred meters downstream when
Phantom Lake Spring was a large flowing spring (Dundee and Dundee 1969,
p. 207; Taylor 1987, p. 40). The species is most abundant in the
swimming pool at Balmorhea State Park, but has not been found in either
of the constructed ci[eacute]negas at the Park in 2010 and 2011 (Allan
2011, p. 3; Bradstreet 2011, pp. 55). The species is found on both soft
and firm substrates on the margins of spring outflows (Taylor 1987, p.
41), and they are also commonly found attached to plants, particularly
in dense stands of submerged vegetation (Chara sp.).
Diamond Y Spring Snail (Pseudotryonia adamantina Taylor 1987)
The Diamond Y Spring snail was first described by Taylor (1987, p.
41) as Tryonia adamantina. It is a small snail measuring only 2.9 to
3.6 mm (0.11 to 0.14 in) long (Taylor 1987, p. 41). Systematic studies
(Hershler et al.1999, p. 377; Hershler 2001, pp. 7, 16) of these snails
have been conducted using mitochondrial DNA sequences and morphological
characters. These analyses resulted in the Diamond Y Spring snail being
reclassified into the new genus Pseudotryonia (Hershler 2001, p. 16).
Based on these published studies, we conclude that Diamond Y Spring
snail is a listable entity under the Act.
Taylor (1985, p. 1; 1987, p. 38) was the earliest to document the
distribution and abundance of aquatic snails in the Diamond Y Spring
system, referencing surveys from 1968 to 1984. In 1968, the Diamond Y
Spring snail was considered abundant in the outflow of Diamond Y Spring
in the upper watercourse for about 1.6 km (1 mi) downstream of the
spring head pool, but by 1984 the species was present in only areas
along stream margins (near the banks) (Taylor 1985, p. 1). Average
density estimates in 1984 at 12 of 14 sampled sites in the upper
watercourse ranged from 500 to 93,700 individuals per sq m (50 to 8,700
per sq ft), with very low densities in the upstream areas near the
headspring (Taylor 1985, p. 25). However, the Diamond Y Spring snail
was largely absent from the headspring and main spring flow channel
where it had been abundant in 1968 surveys (Taylor 1985, p. 13).
Instead it was most common in small numbers along the outflow stream
margins and lateral springs (Taylor 1985, pp. 13-15). Over time, the
distribution of the Diamond Y Spring snail in the upper watercourse has
continued to recede so that it is no longer found in the outflow
channel at all but may be restricted to small lateral spring seeps
disconnected from the main spring flow channel (Landye 2000, p. 1;
Echelle et al. 2001, pp. 24-25). Surveys by Lang (2011, pp. 7-8) in
2001 and 2003 found only 2 and 7 individuals, respectively, in the
outflow channel of Diamond Y Spring. Additional surveys in 2009 and
2010 (Ladd 2010, p. 18; Lang 2011, p. 12) did not find Diamond Y Spring
snails in the upper watercourse. However, neither researcher surveyed
extensively in the lateral spring seeps downstream from the main spring
outflow.
The Diamond Y Spring snail was not previously reported from the
lower watercourse until first detected there in 2001 at the outflow of
Euphrasia Spring (Lang 2011, p. 6). It was confirmed there again in
2009 (Lang 2011, p. 13) and currently occurs within at least the first
50 m (160 feet) in the outflow channel of Euphrasia Spring (Ladd 2010,
p. 18). Ladd (2010, p. 37) roughly estimated the total number of
Diamond Y Spring snails in the lower watercourse to be about 35,000
individuals with the highest density reported as 2,500 individuals per
sq m (230 per sq ft). Lang (2011, p. 13) estimated densities of Diamond
Y Spring snails in 2009 at 16,695 per sq m (1,552 per sq ft; 18,212 per sq m, 1,694 per sq ft) in Euphrasia Spring
outflow, which suggests a much larger population than that estimated by
Ladd (2010, p. 37).
In summary, the Diamond Y Spring snail was historically common in
the upper watercourse and absent from the lower watercourse. Currently
it is very
[[Page 49610]]
rare in the upper watercourse and limited to small side seeps (and may
be extirpated), and it occurs in the lower watercourse in the outflow
of Euphrasia Spring. The historic distribution of this species may have
been larger than the present distribution. Other area springs nearby
such as Leon and Comanche Springs may have harbored the species. There
is one collection of very old, dead shells of the species that was made
from Comanche Springs in 1998 (Worthington 1998, unpublished data)
whose identification was recently confirmed as Diamond Y Spring snail
(Hershler 2011, pers. comm.). However, because these springs have been
dry for more than four decades and shells can remain intact for
thousands of years, it is impossible to know how old the shells might
be. Therefore, we are unable to confirm if the recent historic
distribution included Comanche Springs.
Habitat of the species is primarily soft substrates on the margins
of small springs, seeps, and marshes in shallow flowing water
associated with emergent bulrush (Scirpus americanus) and saltgrass
(Distichlis spicata) (Taylor 1987, p. 38; Echelle et al. 2001, p. 5).
Gonzales Springsnail (Tryonia circumstriata Leonard and Ho 1960)
The Gonzales springsnail was first described as a late Pleistocene
fossil record, Calipyrgula circumstriata, from the Pecos River near
Independence Creek in Terrell County, Texas (Leonard and Ho 1960, p.
126). The snail from Diamond Y Spring area was first described as
Tryonia stocktonensis by Taylor (1987, p. 37). It is a small snail,
measuring only 3.0 to 3.7 mm (0.11 to 0.14 in) long. Systematic studies
later changed the name to Tryonia circumstriata, integrating it with
the fossilized snails from the Pecos River (Hershler 2001, p. 7), and
confirming the species as a ``true Tryonia,'' in other words, it is
appropriately classified in the genus Tryonia (Hershler et al. 2011,
pp. 5-6). Based on these published studies, we conclude that Gonzales
springsnail is a listable entity under the Act.
Taylor (1985, pp. 18-19; 1987, p. 38) found Gonzales springsnail
only in the first 27 m (90 ft) of the outflow from Euphrasia Spring.
The species has been consistently found in this short stretch of spring
outflow channel since then (Echelle et al. 2001, p. 20; Lang 2011, pp.
6, 13). Ladd (2010, pp. 23-24) reported that Gonzales springsnails no
longer occurred in the lower watercourse and had been replaced by
Diamond Y Spring snails. However, reevaluation of voucher specimens
collected by Lang (2011, p. 13) concurrently in 2009 with those by Ladd
(2010, p. 14) confirmed the species is still present in the Euphrasia
Spring outflow channel of the lower watercourse.
Gonzales springsnail was first reported in the upper watercourse in
1991 during collections from one site in the Diamond Y Spring outflow
and one small side seep near the spring head (Fullington and Goodloe
1991, p. 3). The species has since been collected from this area (Lang
2011, pp. 7-9), and Echelle et al. (2001, p. 20) found it to be the
most abundant snail for the first 430-m (1,400-ft) downstream from the
spring head. Ladd (2010, p. 18) also found Gonzales springsnail in the
outflow of Diamond Y Spring, but only from 125 to 422 m (410 to 1,384
ft) downstream of the spring head (Ladd 2011, pers. comm.). The
Gonzales springsnail appears to have replaced the Diamond Y Spring
snail in some of the habitat in the upper watercourse (Brown 2008, p.
489) since 1991.
Taylor (1985, p. 19) calculated densities for Gonzales springsnails
in the outflow of Euphrasia Spring in the range of 50,480 to 85,360
individuals per sq m (4,690 to 7,930 individuals per sq ft) and
estimated the population size in that 27-m (90-ft) stretch to be at
least 162,000 individuals and estimated the total population of over
one million individuals as a reasonable estimate. Lang (2011, p. 13)
estimated the density of Gonzales springsnails in the Euphrasia Spring
outflow to be 3,086 individuals per sq m (287 per sq ft; 5,061 per sq m, 471per sq ft). Ladd (2010, p. 37)
estimated the population of Gonzales springsnails in the upper
watercourse to be only about 11,000 individuals.
As with the Diamond Y Spring snail, the historic distribution of
the Gonzales springsnail may have been larger than the present
distribution. Other area springs nearby such as Leon and Comanche
Springs may have harbored the species. There is one collection of dead
shells of the species that was made from Comanche Springs in 1998
(Worthington 1998, unpublished data) whose identification was recently
confirmed as Gonzales springsnail (Hershler 2011, pers. comm.).
However, because these springs have been dry for more than four decades
and shells can remain intact for thousands of years, it is impossible
to know how old the shells might be. Therefore, we are unable to
confirm if the recent historic distribution included Comanche Springs.
Habitat of the species is primarily soft substrates on the margins
of small springs, seeps, and marshes in shallow flowing water
associated with emergent bulrush and saltgrass (Taylor 1987, p. 38;
Echelle et al. 2001, p. 5).
Life History, Biology, and Habitat of Amphipods
The background information presented here applies to both species
of amphipods in these proposed rules: diminutive amphipod and Pecos
amphipod. These amphipods, in the family Gammaridae, are small
freshwater inland crustaceans sometimes referred to as freshwater
shrimp. Gammarids commonly inhabit shallow, cool, well-oxygenated
waters of streams, ponds, ditches, sloughs, and springs (Smith 2001, p.
574). These bottom-dwelling amphipods feed on algae, submergent
vegetation, and decaying organic matter (Smith 2001, p. 572). Amphipod
eggs are held within a marsupium (brood pouch) within the female's
exoskeleton (Smith 2001, p. 573). Most amphipods complete their life
cycle in 1 year and breed from February to October, depending on water
temperature (Smith 2001, p. 572). Amphipods form breeding pairs that
remain attached for 1 to 7 days at or near the substrate while
continuing to feed and swim (Bousfield 1989, p. 1721). They can produce
from 15 to 50 offspring, forming a ``brood.'' Most amphipods produce
one brood, but some species produce a series of broods during the
breeding season (Smith 2001, p. 573).
These two species, diminutive amphipod and Pecos amphipod, are part
of a related group of amphipods, referred to as the Gammarus pecos
species complex, that are restricted to desert spring systems from the
Pecos River Basin in southeast New Mexico and west Texas (Cole 1985, p.
93; Lang et al. 2003, p. 47; Gervasio et al. 2004, p. 521). Similar to
the snails, it is thought that these freshwater amphipods are derived
from a widespread ancestral marine amphipod that was isolated inland
during the recession of the Late Cretaceous sea, about 66 million years
ago (Holsinger 1967, pp. 125-133; Lang et al. 2003, p. 47). They likely
evolved into distinct species during recent dry periods (since the Late
Pleistocene, about 100,000 years ago) through allopatric speciation
(that is, speciation by geographic separation) following separation and
isolation in the remnant aquatic habitats associated with springs
(Gervasio et al. 2004, p. 528).
Amphipods in the Gammarus pecos species complex only occur in
desert spring outflow channels on substrates, often within interstitial
spaces on and
[[Page 49611]]
underneath rocks and within gravels (Lang et al. 2003, p. 49) and are
most commonly found in microhabitats with flowing water. They are also
commonly found in dense stands of submerged vegetation (Cole 1976, p.
80). Because of their affinity for constant water temperatures, they
are most common in the immediate spring outflow channels, usually only
a few hundred meters downstream of spring outlets.
Amphipods play important roles in the processing of nutrients in
aquatic ecosystems and are also considered sensitive to changes in
aquatic habitat conditions (for example, stream velocities, light
intensity, zooplankton availability, and the presence of heavy metals)
and are often considered ecological indicators of ecosystem health and
integrity (Covich and Thorpe 1991, pp. 672-673, 679; Lang et al. 2003,
p. 48). Water chemistry parameters, such as salinity, pH, and
temperature, are also key components to amphipod habitats (Covich and
Thorpe 1991, pp. 672-673).
Taxonomy, Distribution, and Abundance of Amphipods
Diminutive Amphipod (Gammarus hyalleloides Cole 1976)
W.L. Minckley first collected the diminutive amphipod from Phantom
Lake Spring in the San Solomon Spring system in 1967, and the species
was first formally described by Cole (1976, pp. 80-85). The name comes
from the species being considered the smallest of the known North
American freshwater Gammarus amphipods. Adults generally range in
length from 5 to 8 mm (0.20 to 0.24 in).
There has been some disparity in the literature regarding the
taxonomic boundaries for the amphipods from the San Solomon Spring
system. In Cole's (1985, pp. 101-102) description of the Gammarus pecos
species complex of amphipods based solely on morphological
measurements, he considered the diminutive amphipod to be endemic only
to Phantom Lake Spring, and amphipods from San Solomon and Diamond Y
Springs were both considered to be the Pecos amphipod (G. pecos). This
study did not include samples of amphipods from East Sandia or Giffin
Springs. However, allozyme electrophoresis data on genetic variation
strongly support that the populations from the San Solomon Spring
system form a distinct group from the Pecos amphipod at Diamond Y
Spring (Gervasio et al. 2004, pp. 523-530). Based on these data, we
consider the Pecos amphipod to be limited to the Diamond Y Spring
system.
The results of these genetic studies also suggested that the three
Gammarus amphipod populations from San Solomon, Giffin, and East Sandia
Springs are a taxonomically unresolved group differentiated from the
diminutive amphipod at Phantom Lake Spring (Gervasio et al. 2004, pp.
523-530). Further genetic analysis using mitochondrial DNA (mtDNA) by
Seidel et al. (2009, p. 2309) also indicates that the diminutive
amphipod may be limited to Phantom Lake Spring and the Gammarus species
at the other three springs should be considered a new and undescribed
species. However, the extent of genetic divergence measured between
these populations is not definitive. For example, the 19-base pair
divergence between the population at Phantom Lake Spring and the other
San Solomon Spring system populations (Seidel et al. 2009, Figure 3, p.
2307) represents about 1.7 percent mtDNA sequence divergence (of the
1,100 base pairs of the mitochondrial DNA sequenced (using the
cytochrome c oxidase I (COI) gene). This is a relatively low level of
divergence to support species separation, as a recent review of a
multitude of different animals (20,731 vertebrates and invertebrates)
suggested that the mean mtDNA distances (using the COI gene) between
subspecies is 3.78 percent (0.16) divergence and between
species is 11.06 percent (0.53) divergence (Kartavtsev
2011, pp. 57-58).
Recent evaluations of species boundaries of amphipods from China
suggest mtDNA genetic distances of at least 4 percent were appropriate
to support species differentiation, and the species they described all
exceeded 15 percent divergence (Hou and Li 2010, p. 220). In addition,
no species descriptions using morphological or ecological analysis have
been completed for these populations, which would be important
information in any taxonomic revision (Hou and Li 2010, p. 216).
Therefore, the data available does not currently support taxonomically
separating the amphipod population at Phantom Lake Spring from the
populations at San Solomon, Giffin, and East Sandia Springs into
different listable entities under the Act. So, for the purposes of
these proposed rules, based on the best available scientific
information, we are including all four populations of Gammarus
amphipods from the San Solomon Spring system as part of the Gammarus
hyalleloides species (diminutive amphipod), and we consider diminutive
amphipod a listable entity under the Act. We recognize that the
taxonomy of these populations could change as additional information is
collected and further analyses are published.
The diminutive amphipod only occurs in the four springs from the
San Solomon Spring system (Gervasio et al. 2004, pp. 520-522). There is
no available information that the species' historic distribution was
larger than the present distribution, but other area springs (such as
Saragosa, Toyah, and West Sandia Springs) may have contained the
species. However, because these springs have been dry for many decades,
if the species historically occurred there, they are now extirpated.
There is no opportunity to determine the full extent of the historic
distribution of these amphipods because of the lack of historic surveys
and collections.
Within its limited range, diminutive amphipod can be very abundant.
For example, in May 2001, Lang et al. (2003, p. 51) estimated mean
densities at San Solomon, Giffin, and East Sandia Springs of 6,833
amphipods per sq m (635 per sq ft; standard deviation 5,416
per sq m, 504 per sq ft); 1,167 amphipods per sq m (108 per
sq ft; 730 per sq m, 68 per sq ft), and 4,625
amphipods per sq m (430 per sq ft; 804 per sq m, 75 per sq ft), respectively. In 2009 Lang (2011, p. 11) reported
the density at Phantom Lake Spring as 165 amphipods per sq m (15 per sq
ft; 165 per sq m, 15 per sq ft).
Pecos Amphipod (Gammarus pecos Cole and Bousfield 1970)
The Pecos amphipod was first collected in 1964 from Diamond Y
Spring and was described by Cole and Bousfield (1970, p. 89). Cole
(1985, p. 101) analyzed morphological characteristics of the Gammarus
pecos species complex and suggested the Gammarus amphipod from San
Solomon Spring should also be included as Pecos amphipod. However,
updated genetic analyses based on allozymes (Gervasio et al. 2004, p.
526) and mitochondrial DNA (Seidel et al. 2009, p. 2309) have shown
that Pecos amphipods are limited in distribution to the Diamond Y
Spring system. In addition, Gervasio et al. (2004, pp. 523, 526)
evaluated amphipods from three different locations within the Diamond Y
Spring system and found no significant differences in genetic
variation, indicating they all represented a single species. Based on
these published studies, we conclude that Pecos amphipod is a listable
entity under the Act.
The Pecos amphipod is generally found in all the flowing water
habitats associated with the outflows of springs and seeps in the
Diamond Y Spring
[[Page 49612]]
system (Echelle et al. 2001, p. 20; Lang et al. 2003, p. 51; Allan
2011, p. 2; Lang 2011, entire). There is no available information to
determine if the species' historic distribution was larger than the
present distribution. Other area springs, such as Comanche and Leon
Springs, may have contained the same or similar species of amphipod,
but because these springs have been dry for many decades (Brune 1981,
pp. 256-263, 382-386), there is no opportunity to determine the
potential historic occurrence of amphipods. Pecos amphipods are often
locally abundant, with reported mean densities ranging from 2,208
individuals per sq m (205 per sq ft; 1,585 per sq m, 147 per sq ft) to 8,042 individuals per sq m (748 per sq ft;
7,229 per sq m, 672 per sq ft) (Lang et al.
2003, p. 51).
Summary of Factors Affecting the Species
Section 4 of the Act (16 U.S.C. 1533), and its implementing
regulations at 50 CFR part 424, set forth the procedures for adding
species to the Federal Lists of Endangered and Threatened Wildlife and
Plants. Under section 4(a)(1) of the Act, the Service determines
whether a species is endangered or threatened because of any of the
following five factors: (A) The present or threatened destruction,
modification, or curtailment of its habitat or range; (B)
overutilization for commercial, recreational, scientific, or
educational purposes; (C) disease or predation; (D) the inadequacy of
existing regulatory mechanisms; and (E) other natural or manmade
factors affecting its continued existence. Listing actions may be
warranted based on any of the above threat factors, singly or in
combination. Each of these factors is discussed below.
Based on the similarity in geographic ranges and threats to
habitats, we have divided this analysis into two sections, one covering
the three species from the San Solomon Spring system and then a second
analysis covering the three species from the Diamond Y Spring system.
After each analysis we provide proposed determinations for each
species.
San Solomon Spring Species--Phantom Cave Snail, Phantom Springsnail,
and Diminutive Amphipod
The following analysis applies to the three species that occur in
the San Solomon Spring system in Reeves and Jeff Davis Counties, Texas:
Phantom Cave snail, Phantom Lake springsnail, and diminutive amphipod.
A. The Present or Threatened Destruction, Modification, or Curtailment
of Their Habitat or Range (San Solomon Spring Species)
The three species in the San Solomon Spring system are threatened
by the past and future destruction of their habitat and reduction in
their range. The discussion below evaluates the stressors of: (1)
Spring flow declines; (2) water quality changes and contamination; and
(3) modification of spring channels.
Spring Flow Declines
The primary threat to the continued existence of the San Solomon
Spring species is the degradation and potential future loss of aquatic
habitat (flowing water from the spring outlets) due to the decline of
groundwater levels in the aquifers that support spring surface flows.
Habitat for these species is exclusively aquatic and completely
dependent on spring flows emerging to the surface from underground
aquifer sources. Spring flows throughout the San Solomon Spring system
have and continue to decline in flow rate, and as spring flows decline,
available aquatic habitat is reduced and altered. If one spring ceases
to flow continually, all habitats for the Phantom Cave snail, Phantom
Lake springsnail, and diminutive amphipod are lost, and the populations
will be extirpated. If all of the springs lose consistent surface
flows, all natural habitats for these aquatic invertebrates will be
gone, and the species will become extinct.
The springs do not have to cease flowing completely to have an
adverse effect on invertebrate populations. The small size of the
spring outflows at Phantom, Giffin, and East Sandia Springs makes them
particularly susceptible to changes in water chemistry, increased water
temperatures during the summer and freezing in the winter. Because
these springs are small, any reductions in the flow rates from the
springs can reduce the quantity and quality of available habitat for
the species, which decreases the number of individuals available and
increases the risk of extinction. Water temperatures and chemical
factors in springs, such as dissolved oxygen and pH, do not typically
fluctuate to a large degree (Hubbs 2001, p. 324), and invertebrates are
narrowly adapted to spring conditions and are sensitive to changes in
water quality (Hershler 1998, p. 11; Sada 2008, p. 69). Spring flow
declines can lead to the degradation and loss of aquatic invertebrate
habitat and present a substantial threat to these species.
The precise reason for the declining spring flows remains
uncertain, but it is presumed to be related to a combination of
groundwater pumping, mainly for agricultural irrigation, and a lack of
natural recharge to the supporting aquifers due to limited rainfall and
geologic circumstances that prevent recharge. In addition, future
changes in the regional climate are expected to exacerbate declining
flows. The San Solomon Spring system historically may have had a
combined discharged of about 2.8 cms (100 cfs) or 89 million cubic
meters per year (cmy) (72,000 acre-feet per year (afy)) (Beach et al.
2004, p. 4-53), while today the total discharge is roughly one-third
that amount. Some smaller springs, such as Saragosa, Toyah, and West
Sandia Springs have already ceased flowing and likely resulted in the
extirpation of local populations of these species (assuming they were
present there historically). The most dramatic recent decline in flow
rates have been observed at Phantom Lake Spring, which is the highest
elevation spring in the system and, not unexpectedly, was the first
large spring to cease flowing.
Phantom Lake Spring was a historically large desert ci[eacute]nega
with a pond of water more than several acres in size (Hubbs 2001, p.
307). The spring outflow is at about 1,080 m (3,543 ft) in elevation
and previously provided habitat for the endemic native aquatic fauna.
The outflow from Phantom Lake Spring was originally isolated from the
other surface springs in the system, as the spring discharge quickly
recharged back underground (Brune 1981, p. 258). Human modifications to
the spring outflow captured and channeled the spring water into a canal
system for use by local landowners and irrigation by the local water
users (Simonds 1996, p. 3). The outflow canal joins the main San
Solomon canal within Balmorhea State Park. Despite the significant
habitat alterations, the native aquatic fauna (including these three
invertebrates) have persisted, though in much reduced numbers of total
individuals, in the small pool of water at the mouth of the spring.
Flows from Phantom Lake Spring have been steadily declining since
measurements were first taken in the 1930s (Brune 1981, p. 259).
Discharge data have been recorded from the spring at least six to eight
times per year since the 1940s by the U.S. Geological Survey, and the
record shows a steady decline of base flows from greater than 0.3 cms
(10 cfs) in the 1940s to 0 cms (0 cfs) in 1999 (Service 2009b, p. 23).
The data also show that the spring can have short-term flow peaks
resulting from local rainfall events in the Davis Mountains (Sharp et
al. 1999, p. 4;
[[Page 49613]]
Chowdhury et al. 2004, p. 341). These flow peaks are from fast recharge
of the local aquifer system and discharge through the springs. The flow
peaks do not come from direct surface water runoff because the outflow
spring is within an extremely small surface drainage basin that is not
connected to surface drainage basins from the Davis Mountains upslope.
However, after each flow increase, the base flow has returned to the
same declining trend within a few months.
Exploration of Phantom Cave by cave divers has led to additional
information about the nature of the spring and its supporting aquifer.
Over 2,440 m (8,000 ft) of the underwater cave have been mapped. Beyond
the entrance, the cave is a substantial conduit that transports a large
volume of water, in the 0.6 to 0.7 cms (20 to 25 cfs) range, generally
from the northwest to the southeast (Tucker 2009, p. 8), consistent
with regional flow pattern hypothesis (Chowdhury et al. 2004, p. 319).
The amount of water measured is in the range of the rate of flow at San
Solomon Spring and, along with water chemistry data (Chowdhury et al.
2004, p. 340), confirms that the groundwater flowing by Phantom Lake
Spring likely discharges at San Solomon Spring. Tucker (2009, p. 8)
recorded a 1-m (3-ft) decline in the water surface elevation within the
cave between 1996 and 2009 indicating a decline in the amount of
groundwater flowing through Phantom Cave.
Phantom Lake Spring ceased flowing in about 1999 (Allan 2000, p.
51; Service 2009b, p. 23). All that remained of the spring outflow
habitat was a small pool of water with about 37 sq m (400 sq ft) of
wetted surface area. Hubbs (2001, pp. 323-324) documented changes in
water quality (increased temperature, decreased dissolved oxygen, and
decreased coefficient of variation for pH, turbidity, ammonia, and
salinity) and fish community structure at Phantom Lake Spring following
cessation of natural flows. In May 2001, the U.S. Bureau of
Reclamation, in cooperation with the Service, installed an emergency
pump system to bring water from within the cave to the springhead in
order to prevent complete drying of the pool and loss of the federally
listed endangered fishes and candidate invertebrates that occur there.
Habitat for the San Solomon Spring system invertebrates continues to be
maintained at Phantom Lake Spring, and in 2011 the small pool was
enlarged, nearly doubling the amount of aquatic habitat available for
the species (Service 2012, entire).
The three San Solomon Spring species have maintained minimal
populations at Phantom Lake Spring despite the habitat being
drastically modified from its original state and being maintained by a
pump system since 2000. However, because the habitat is sustained with
a pump system, the risk of extirpation of these populations continues
to be extremely high from the potential for a pump failure or some
unforeseen event. For example, the pump system failed several times
during 2008, resulting in stagnant pools and near drying conditions,
placing severe stress on the invertebrate populations (Allan 2008, pp.
1-2). Substantial efforts were implemented in 2011 to improve the
reliability of the pump system and the quality of the habitat (Service
2012, pp. 5-9). However, because the habitat is completely maintained
by artificial means, the potential loss of the invertebrate population
will continue to be an imminent threat of high magnitude to the
populations at Phantom Lake Spring.
Although long-term data for San Solomon Spring flows are limited,
they appear to have declined somewhat over the history of record,
though not as severely as Phantom Lake Spring (Schuster 1997, pp. 86-
90; Sharp et al. 1999, p. 4). Some recent declines in overall flow have
likely occurred due to drought conditions and declining aquifer levels
(Sharp et al. 2003, p. 7). San Solomon Spring discharges are usually in
the 0.6 to 0.8 cms (25 to 30 cfs) range (Ashworth et al. 1997, p. 3;
Schuster 1997, p. 86) and are consistent with the theory that the water
bypassing Phantom Lake Spring discharges at San Solomon Spring.
In Giffin Spring, Brune (1981, pp. 384-385) documented a gradual
decline in flow between the 1930s and 1970s, but the discharge has
remained relatively constant since that time, with outflow of about
0.08 to 0.1 cms (3 to 4 cfs) (Ashworth et al. 1997, p. 3; U.S.
Geological Survey 2012, p. 2). Although the flow rates from Giffin
Spring appear to be steady in recent years, its small size makes the
threat of spring flow loss imminent and of high magnitude because even
a small decline in flow rate may have substantial impacts on the
habitat provided by the spring flow. Also, it would only take a small
decline in spring flow rates to result in desiccation of the spring.
Brune (1981, p. 385) noted that flows from Sandia Springs
(combining East and West Sandia Springs) were declining up until 1976.
East Sandia may be very susceptible to over pumping of the local
aquifer in the nearby area that supports the small spring. Measured
discharges in 1995 and 1996 ranged from 0.013 to 0.12 cms (0.45 to 4.07
cfs) (Schuster 1997, p. 94). Like the former springs of West Sandia and
Saragosa, which also originated in shallow aquifers and previously
ceased flowing (Ashworth et al. 1997, p. 3), East Sandia Spring's very
small volume of water makes it particularly at risk of failure from any
local changes in groundwater conditions.
The exact causes for the decline in flow from the San Solomon
Spring system are unknown. Some of the possible reasons, which are
likely acting together, include groundwater pumping of the Salt Basin
Bolson aquifer areas west of the springs, long-term climatic changes,
or changes in the geologic structure that permits regional interbasin
flow of groundwater (Sharp et al. 1999, p. 4; Sharp et al. 2003, p. 7).
Studies indicate that the base flows originate from ancient waters to
the west (Chadhury et al. 2004, p. 340) and that many of the aquifers
in west Texas receive little to no recharge from precipitation (Scanlon
et al. 2001, p. 28) and are influenced by regional groundwater flow
patterns (Sharp 2001, p. 41).
Ashworth et al. (1997, entire) provided a brief study to examine
the cause of declining spring flows in the San Solomon Spring system.
They concluded that declines in spring flows in the 1990s were more
likely the result of diminished recharge due to the extended dry period
rather than from groundwater pumpage (Ashworth et al. 1997, p. 5).
Although possibly a factor, drought is unlikely the only reason for the
declines because the drought of record in the 1950s had no measurable
effect on the overall flow trend at Phantom Lake Spring (Allan 2000, p.
51; Sharp 2001, p. 49) and because the contributing aquifer receives
virtually no recharge from most precipitation events (Beach et al.
2004, pp. 6-9, 8-9). Also, Ashworth et al. (1997, entire) did not
consider the effects of the regional flow system in relation to the
declining spring flows. Further, an assessment of the springs near
Balmorhea by Sharp (2001, p. 49) concluded that irrigation pumpage
since 1945 has caused many springs in the area to cease flowing,
lowering water-table elevations and creating a cone of depression in
the area (that is, a lowering of the groundwater elevation around
pumping areas).
The Texas Water Development Board (2005, entire) completed a
comprehensive study to ascertain the potential causes of spring flow
declines in the San Solomon Spring system, including a detailed
analysis of historic regional groundwater pumping trends. The study was
unable to quantify direct
[[Page 49614]]
correlations between changes in groundwater pumping in the surrounding
counties and spring flow decline over time at Phantom Lake Spring
(Texas Water Development Board 2005, p. 93). However, they suggested
that because of the large distance between the source groundwater and
the springs and the long travel time for the water to reach the spring
outlets, any impacts of pumping are likely to be reflected much later
in time (Texas Water Development Board 2005, p. 92). The authors did
conclude that groundwater pumping will impact groundwater levels and
spring flow rates if it is occurring anywhere along the flow path
system (Texas Water Development Board 2005, p. 92).
Groundwater pumping for irrigated agriculture has had a measurable
effect on groundwater levels in the areas that likely support the
spring flows at the San Solomon Spring system. For example, between the
1950s and 2000 the Salt Basin Bolson aquifer in Lobo Flat fell in
surface elevation in the range of 15 to 30 m (50 to near 100 ft), and
in Wild Horse Flat from 6 to 30 m (20 to 50 ft) (Angle 2001, p. 248;
Beach et al. 2004, p. 4-9). Beach et al. (2004, p. 4-10) found
significant pumping, especially in the Wild Horse Flat area, locally
influences flow patterns in the aquifer system. The relationship of
regional flow exists because Wild Horse Flat is located in the lowest
part of the hydraulically connected Salt Basin Bolson aquifer, and next
highest is Lobo, followed by Ryan Flat, which is at the highest
elevations (Beach et al. 2004, p. 9-32). This means that water
withdrawn from any southern part of the basin (Ryan and Lobo Flats) may
affect the volume of water discharging out of Wild Horse Flat toward
the springs. Because these bolson aquifers have little to no direct
recharge from precipitation (Beach et al. 2004, pp. 6-9, 8-9), these
groundwater declines can be expected to permanently reduce the amount
of water available for discharge in the springs in the San Solomon
Spring system. This is evidenced by the marked decline of groundwater
flow out of the Wild Horse Flat toward the southeast (the direction of
the springs) (Beach et al. 2004, p. 9-27). Based on this information,
it appears reasonable that past and future groundwater withdrawals in
the Salt Basin Bolson aquifers are likely one of the causes of
decreased spring flows in the San Solomon Spring system.
Groundwater pumping withdrawals in Culberson, Jeff Davis, and
Presidio Counties in the Salt Basin Bolson aquifer are expected to
continue in the future mainly to support irrigated agriculture (Region
F Water Planning Group 2010, pp. 2-16-2-19) and will result in
continued lowering of the groundwater levels in the Salt Basin Bolson
aquifer. The latest plans from Groundwater Management Area 4 (the
planning group covering the relevant portion of the Salt Basin Bolson
aquifer) expect over 69 million cubic m (56,000 af) of groundwater
pumping per year for the next 50 years, resulting in an average
drawdown of 22 to 24 m (72 to 78 feet) in the West Texas Bolsons (Salt
Basin) aquifer by 2060 (Adams 2010, p. 2; Oliver 2010, p. 7). There
have been no studies evaluating the effects of this level of
anticipated drawdown on spring flows. The aquifer in the Wild Horse
Flat area (the likely spring source) can range from 60 to 300 m (200 to
1,000 ft) thick. So although it is impossible to determine precisely,
we anticipate the planned level of groundwater drawdown will likely
result in continued future declines in spring flow rates in the San
Solomon Spring system.
Another reason that spring flows may be declining is from an
increase in the frequency and duration of local and regional drought
associated with climatic changes. The term ``climate'' refers to the
mean and variability of different types of weather conditions over
time, with 30 years being a typical period for such measurements,
although shorter or longer periods also may be used (IPCC 2007a, p.
78). The term ``climate change'' thus refers to a change in the mean or
variability of one or more measures of climate (e.g., temperature or
precipitation) that persists for an extended period, typically decades
or longer, whether the change is due to natural variability, human
activity, or both (IPCC 2007a, p. 78).
Although the bulk of spring flows appear to originate from ancient
water sources with limited recent recharge, any decreases in regional
precipitation patterns due to prolonged drought will further stress
groundwater availability and increase the risk of diminishment or
drying of the springs. Drought affects both surface and groundwater
resources and can lead to diminished water quality (Woodhouse and
Overpeck 1998, p. 2693) in addition to reducing groundwater quantities.
Lack of rainfall may also indirectly affect aquifer levels by resulting
in an increase in groundwater pumping to offset water shortages from
low precipitation (Mace and Wade 2008, p. 665).
Recent drought conditions may be indicative of more common future
conditions. The current, multiyear drought in the western United
States, including the Southwest, is the most severe drought recorded
since 1900 (Overpeck and Udall 2010, p. 1642). In 2011, Texas
experienced the worst annual drought since recordkeeping began in 1895
(NOAA 2012, p. 4), and only one other year since 1550 (the year 1789)
was as dry as 2011 based on tree-ring climate reconstruction (NOAA
2011, pp. 20-22). In addition, numerous climate change models predict
an overall decrease in annual precipitation in the southwestern United
States and northern Mexico.
Future global climate change may result in increased magnitude of
droughts and further contribute to impacts on the aquatic habitat from
reduction of spring flows. There is high confidence that many semi-arid
areas like the western United States will suffer a decrease in water
resources due to ongoing climate change (IPCC 2007b, p. 7; Karl et al.
2009, pp. 129-131), as a result of less annual mean precipitation.
Milly et al. (2005, p. 347) also project a 10 to 30 percent decrease in
precipitation in mid-latitude western North America by the year 2050
based on an ensemble of 12 climate models. Even under lower greenhouse
gas emission scenarios, recent projections forecast a 10 percent
decline in precipitation in western Texas by 2080 to 2099 (Karl et al.
2009, pp. 129-130). Assessments of climate change in west Texas suggest
that the area is likely to become warmer and at least slightly drier
(Texas Water Development Board 2008, pp. 22-25).
The potential effects of future climate change could reduce overall
water availability in this region of western Texas and compound the
stressors associated with declining flows from the San Solomon Spring
system. As a result of the effects of increased drought, spring flows
could decline indirectly as a result of increased pumping of
groundwater to accommodate human needs for additional water supplies
(Mace and Wade 2008, p. 664; Texas Water Development Board 2012c, p.
231).
In conclusion, the Phantom Cave snail, Phantom springsnail, and
diminutive amphipod all face significant threats from the current and
future loss of habitat associated with declining spring flows. Some
springs in the San Solomon Spring system have already gone dry, and
aquatic habitat at Phantom Lake Spring has not yet been lost only
because of the maintenance of a pumping system. While the sources of
the stress of declining spring flows are not known for certain, the
best available scientific information indicates that it is the result
of a combination of factors including past and current groundwater
[[Page 49615]]
pumping, the complex hydrogeologic conditions that produce these
springs (ancient waters from a regional flow system), and climatic
changes (decreased precipitation and recharge). The threat of habitat
loss from declining spring flows affects all four of the remaining
populations, as all are at risk of future loss from declining spring
flows. All indications are that the source of this threat will persist
into the future and will result in continued degradation of the
species' habitats, putting the Phantom Cave snail, Phantom springsnail,
and diminutive amphipod at a high risk of extinction.
Water Quality Changes and Contamination
Another potential factor that could impact habitat of the San
Solomon Spring species is the potential degradation of water quality
from point and nonpoint pollutant sources. This can occur either
directly into surface water or indirectly through contamination of
groundwater that discharges into spring run habitats used by the
species. The primary threat for contamination in these springs comes
from herbicide and pesticide use in nearby agricultural areas. There
are no oil and gas operations in the area around the San Solomon Spring
system.
These aquatic invertebrates are sensitive to water contamination.
Hydrobiid snails as a group are considered sensitive to water quality
changes, and each species is usually found within relatively narrow
habitat parameters (Sada 2008, p. 59). Amphipods generally do not
tolerate habitat desiccation (drying), standing water, sedimentation,
or other adverse environmental conditions; they are considered very
sensitive to habitat degradation (Covich and Thorpe 1991, pp. 676-677).
The exposure of the spring habitats to pollutants is limited
because most of the nearby agricultural activity mainly occurs in
downstream areas where herbicide or pesticide use would not likely come
into contact with the species or their habitat in upstream spring
outlets. To ensure these pollutants do not affect these spring outflow
habitats, their use has been limited in an informal protected area in
the outflows of San Solomon and Giffin Springs (Service 2004, pp. 20-
21). This area was developed in cooperation with the U.S. Environmental
Protection Agency and the Texas Department of Agriculture. While there
are more agriculture activities far upstream in the aquifer source
area, there is no information indicating concerns about contaminants
from those sources.
In addition, Texas Parks and Wildlife Department completed a
Habitat Conservation Plan and received an incidental take permit
(Service 2009a, entire) in 2009 under section 10(a)(1)(B) (U.S.C.
1539(a)(1)(B)) of the Act for management activities at Balmorhea State
Park (Texas Parks and Wildlife Department 1999, entire). The three
aquatic invertebrate candidate species from the San Solomon Spring
system were all included as covered species in the permit (Service
2009a, pp. 20-22). This permit authorizes ``take'' of the invertebrates
(which were candidates at the time of issuance) in the State Park for
ongoing management activities while minimizing impacts to the aquatic
species. The activities included in the Habitat Conservation Plan are a
part of Texas Parks and Wildlife Department's operation and maintenance
of the State Park, including the drawdowns associated with cleaning the
swimming pool and vegetation management within the refuge canal and
ci[eacute]nega. The Habitat Conservation Plan also calls for
restrictions and guidelines for chemical use in and near aquatic
habitats to avoid and minimize impacts to the three aquatic
invertebrate species (Service 2009a, pp. 9, 29-32).
Because the use of potential pollutants is very limited within the
range of the San Solomon Spring species, at this time we do not find
that the Phantom Cave snail, Phantom springsnail, and diminutive
amphipod are at a heightened risk of extinction from water quality
changes or contamination.
Modification of Spring Channels
The natural ci[eacute]nega habitats of the San Solomon Spring
system have been heavily altered over time primarily to accommodate
agricultural irrigation. Most significant was the draining of wetland
areas and the modification of spring outlets to develop the water
resources for human use. San Solomon and Phantom Lake Springs have been
altered the most severely through capture and diversion of the spring
outlets into concrete irrigation canals. Giffin Spring appears to have
been dredged in the past, and the outflow is now immediately captured
in high-banked, earthen-lined canals. The outflow of East Sandia Spring
does not appear to have been altered in an appreciable way, but it may
have been minimally channelized to connect the spring flow to the
irrigation canals.
The Reeves County Water Improvement District No. 1 maintains an
extensive system of about 100 km (60 mi) of irrigation canals that now
provide only minimal aquatic habitat for the invertebrate species near
the spring sources. Most of the canals are concrete-lined with high
water velocities and little natural substrate available. Many of the
canals are also regularly dewatered as part of the normal water
management operations. Before the canals were constructed, the suitable
habitat areas around the spring openings, particularly at San Solomon
Spring, were much larger in size. The conversion of the natural aquatic
mosaic of habitats into linear irrigation canals represents a past
impact resulting in significant habitat loss and an increase in the
overall risk of extinction by lowering the amount of habitat available
to the species and, therefore, lowering the overall number of
individuals in the populations affected. These reductions in population
size result in an increase in the risk of extirpation of local
populations and, ultimately, the extinction of the species as a whole.
Because the physical conditions of the spring channels have changed
dramatically in the past, the species are now at a greater risk of
extinction because of the alterations to the ecosystem and the overall
lower number of individuals likely making up the populations.
A number of efforts have been undertaken at Balmorhea State Park to
conserve and maintain aquatic habitats at some of the spring sites to
conserve habitat for the native aquatic species. First, a refuge canal
encircling the historic motel was built in 1974 to create habitat for
the endangered fishes, Comanche Springs pupfish and Pecos gambusia
(Garrett 2003, p. 153). Although the canal was concrete-lined, it had
slower moderate water velocities, and natural substrates covered the
wide concrete bottom and provided usable habitat for the aquatic
invertebrates. Second, the 1-ha (2.5-ac) San Solomon Ci[eacute]nega was
built in 1996 to create an additional flow-through pond of water for
habitat of the native aquatic species (Garrett 2003, pp. 153-154).
Finally, during 2009 and 2010, a portion of the deteriorating 1974
refuge canal was removed and relocated away from the motel. The wetted
area was expanded to create a new, larger ci[eacute]nega habitat. This
was intended to provide additional natural habitat for the federally
listed endangered fishes and candidate invertebrates (Service 2009c, p.
3; Lockwood 2010, p. 3). All of these efforts have been generally
successful in providing additional habitat areas for the aquatic
invertebrates, although neither the snails nor amphipods have been
shown to use the newest ci[eacute]nega pond to date (Allan 2011, p. 3).
[[Page 49616]]
At Phantom Lake Spring, a pupfish refuge canal was built in 1993
(Young et al. 1993, pp. 1-3) to increase the available aquatic habitat
that had been destroyed by the irrigation canal. Winemiller and
Anderson (1997, pp. 204-213) showed that the refuge canal was used by
endangered fish species when water was available. Stomach analysis of
the endangered pupfish from Phantom Lake Spring showed that the Phantom
Cave snail and diminutive amphipod were a part of the fish's diet
(Winemiller and Anderson 1997, pp. 209-210), indicating that the
invertebrates also used the refuge canal. The refuge canal was
constructed for a design flow down to about 0.01 cms (0.5 cfs), which
at the time of construction was the lowest flow ever recorded out of
Phantom Lake Spring. The subsequent loss of spring flow eliminated the
usefulness of the refuge canal because the canal went dry beginning in
about 2000.
All the water for the remaining spring head pool at Phantom Lake
Spring is being provided by a pump system to bring water from about 23
m (75 ft) within the cave out to the surface. The small outflow pool
was enlarged in 2011 (U.S. Bureau of Reclamation 2011, p. 1; Service
2012, entire) to encompass about 75 sq m (800 sq ft) of wetted area. In
2011, the pool was relatively stable and all three of the San Solomon
Spring invertebrates were present (Allan 2011, p. 3; Service 2012, p.
9).
In summary, the modifications to the natural spring channels at San
Solomon, Phantom Lake, and Giffin Springs represent activities that
occurred in the past and resulted in a deterioration of the available
habitat for the Phantom Cave snail, Phantom springsnail, and diminutive
amphipod. Actions by conservation agencies over the past few decades
have mitigated the impacts of those actions by restoring some natural
functions to the outflow channels. While additional impacts from
modifications are not likely to occur in the future because of land
ownership by conservation entities at three of the four spring sites,
the past modifications have contributed to the endangerment of these
species by reducing the overall quantity of available habitat and,
therefore, reducing the number of individuals of each species that can
inhabit the spring outflows. The lower the overall number of
individuals of each species and the lower the amount of available
habitat, the greater the risk of extinction. Therefore, the
modification of spring channels contributes to increased risk of
extinction in the future as a consequence of the negative impacts of
the past actions.
Other Conservation Efforts
All four of these springs in the San Solomon Spring system are
inhabited by two fishes federally listed as endangered--Comanche
Springs pupfish (Service 1981, pp. 1-2) and Pecos gambusia (Service
1983, p. 4). Critical habitat has not been designated for either
species. In addition, East Sandia Spring is also inhabited by the
federally threatened Pecos sunflower (Service 2005, p. 4) and the
federally endangered Pecos assiminea snail (Service 2010, p. 5). Both
the Pecos sunflower and the Pecos assiminea snail also have critical
habitat designated at East Sandia Spring (73 FR 17762, April 1, 2008;
76 FR 33036, June 7, 2011, respectively).
The Phantom Cave snail, Phantom springsnail, and diminutive
amphipod have been afforded some protection indirectly in the past due
to the presence of these other listed species in the same locations.
Management and protection of the spring habitats by Texas Parks and
Wildlife Department at San Solomon Spring, U.S. Bureau of Reclamation
at Phantom Lake Spring, and The Nature Conservancy at East Sandia
Spring have benefited the aquatic invertebrates. However, the primary
threat from the loss of habitat due to declining spring flows related
to groundwater changes have not been abated by the Federal listing of
the fish or other species. Therefore, the conservation efforts provided
by the concomitant occurrence of species already listed under the Act
have not prevented the past and ongoing habitat loss, nor is it
expected to prevent future habitat loss.
Summary of Factor A
Based on our evaluation of the best available information, we
conclude that the present and future destruction and modification of
the habitat of the Phantom Cave snail, Phantom springsnail, and
diminutive amphipod is a significant threat. Some of these impacts
occurred in the past from the loss of natural spring flows at several
springs likely within the historic range. The impacts are occurring now
and are likely to continue in the future throughout the current range
as groundwater levels decline and increase the possibility of the loss
of additional springs. As additional springs are lost, the number of
populations will decline and further increase the risk of extinction of
these species. The sources of this threat are not confirmed but are
presumed to include a combination of factors associated with
groundwater pumping, hydrogeologic structure of the supporting
groundwater, and climatic changes. The risk of extinction is also
heightened by the past alteration of spring channels reducing the
available habitat and the number of individuals in each population.
B. Overutilization for Commercial, Recreational, Scientific, or
Educational Purposes (San Solomon Spring Species)
There are very few people who are interested in or study
springsnails and amphipods, and those who do are sensitive to their
rarity and endemism. Consequently, collection for scientific or
educational purposes is very limited. There are no known commercial or
recreational uses of these invertebrates. For these reasons we conclude
that overutilization for commercial, recreational, scientific, or
educational purposes is currently not a threat to the Phantom Lake
snail, Phantom springsnail, and diminutive amphipod, and we have no
indication that these factors will affect these species in the future.
C. Disease or Predation (San Solomon Spring Species)
The San Solomon Spring species are not known to be affected by any
disease. These invertebrates are likely natural prey species for fishes
and crayfishes that occur in their habitats. Native snails and
amphipods have been found as small proportions of the diets of native
fishes at San Solomon and Phantom Lake Springs (Winemiller and Anderson
1997, p. 201; Hargrave 2010, p. 10), and crayfish are a known predator
of snails (Hershler 1998, p. 14). Bradstreet (2011, p. 98) assumed that
snails at San Solomon Spring were prey for both fishes and crayfishes
and suspected that the native snails may be more susceptible than the
nonnative snails because of their small body size and thinner shells.
In addition, Ladd and Rogowski (2012, p. 289) suggested that the
nonnative red-rim melania (Melanoides tuberculata) may prey upon native
snail eggs of a different species. However, our knowledge of such
predation is very limited, and the extent to which the predation might
affect native springsnails is unknown. For more discussion about red-
rim melania see ``Factor E. Other Natural or Manmade Factors Affecting
Its Continued Existence.'' We are not aware of any other information
indicating that the San Solomon Spring species are affected by disease
or predation factors. For these reasons we conclude that disease or
predation are not significant threats to the Phantom Lake snail,
[[Page 49617]]
Phantom springsnail, and diminutive amphipod, and we have no indication
that these factors will affect these species more severely in the
future.
D. The Inadequacy of Existing Regulatory Mechanisms (San Solomon Spring
Species)
Under this factor, we examine whether existing regulatory
mechanisms are inadequate to address the threats to the species
discussed under Factors A and E. Section 4(b)(1)(A) of the Endangered
Species Act requires the Service to take into account ``those efforts,
if any, being made by any State or foreign nation, or any political
subdivision of a State or foreign nation, to protect such species * *
*.'' We interpret this language to require the Service to consider
relevant Federal, State, and Tribal laws or regulations that may
minimize any of the threats we describe in threat analyses under the
other four factors, or otherwise enhance conservation of the species.
An example would be the terms and conditions attached to a grazing
permit that describe how a permittee will manage livestock on a BLM
allotment. They are nondiscretionary and enforceable, and are
considered a regulatory mechanism under this analysis. Other examples
include State governmental actions enforced under a State statute or
constitution, or Federal action under statute.
Having evaluated the significance of the threat as mitigated by any
such conservation efforts, we analyze under Factor D the extent to
which existing regulatory mechanisms are inadequate to address the
specific threats to the species. Regulatory mechanisms, if they exist,
may reduce or eliminate the impacts from one or more identified
threats. In this section, we review existing State and Federal
regulatory mechanisms to determine whether they effectively reduce or
remove threats to the three San Solomon Spring species.
Texas laws provide no specific protection for these invertebrate
species, as they are not listed as threatened or endangered by the
Texas Parks and Wildlife Department. However, even if they were listed
by the State, those regulations (Title 31 Part 2 of Texas
Administrative Code) would only prohibit the taking, possession,
transportation, or sale of any animal species without the issuance of a
permit. The State makes no provision for the protection of the habitat
of listed species, which is the main threat to these aquatic
invertebrates.
Some protection for the habitat of this species is provided with
the land ownership of the springs by Federal (Phantom Lake Spring owned
by the U.S. Bureau of Reclamation) and State (San Solomon Spring owned
by Texas Parks and Wildlife Department) agencies, and by The Nature
Conservancy (East Sandia Spring). However, this land ownership only
protects the spring outflow channels and provides no protection for
maintaining groundwater levels to ensure continuous spring flows.
In the following discussion, we evaluate the existing local
regulations related to groundwater management within areas that might
provide indirect benefits to the species' habitats through management
of groundwater levels.
Local Groundwater Regulations
One regulatory mechanism that could provide some protection to the
spring flows for these species comes from local groundwater
conservation districts. Groundwater in Texas is generally governed by
the rule of capture unless there is a groundwater district in place.
The rule of capture allows a landowner to produce as much groundwater
as he or she chooses, as long as the water is not wasted (Mace 2001, p.
11). However, local groundwater conservation districts have been
established throughout much of Texas and are now the preferred method
for groundwater management in the State (Texas Water Development Board
2012, pp. 23-258). Groundwater districts ``may regulate the location
and production of wells, with certain voluntary and mandatory
exemptions'' (Texas Water Development Board 2012, p. 27).
There are currently four local groundwater districts in the area
west of the springs (Texas Water Development Board 2011, p. 1) that
could possibly manage groundwater to protect spring flows in the San
Solomon Spring system. The Culberson County Groundwater Conservation
District covers the southwestern portion of Culberson County and was
confirmed (established by the Texas legislature and approved by local
voters) in 1998. The Jeff Davis County Underground Water Conservation
District covers all of Jeff Davis County and was confirmed in 1993. The
Presidio County Underground Water Conservation District covers all of
Presidio County and was confirmed in 1999. The Hudspeth County
Underground Water District No. 1 covers the northwest portion of
Hudspeth County and was confirmed in 1957. This area of Hudspeth County
manages the Bone Spring-Victoria Peak aquifer (Hudspeth County
Underground Water District No. 1 2007, p. 1), which is not known to
contribute water to the regional flow that supplies the San Solomon
Spring system (Ashworth 2001, pp. 143-144). Therefore, we will not
further consider that groundwater district.
In 2010 the Groundwater Management Area 4 established ``desired
future conditions'' for the aquifers occurring within the five-county
area of west Texas (Adams 2010, entire; Texas Water Development Board
2012a, entire). These projected conditions are important because they
guide the plans for water use of groundwater within groundwater
conservation districts in order to attain the desired future condition
of each aquifer they manage (Texas Water Development Board 2012c, p.
23). In the following discussion we review the plans and desired future
conditions for the groundwater conservation districts in Culberson,
Jeff Davis, and Presidio Counties relative to the potential regulation
of groundwater for maintaining spring flows and abating future declines
in the San Solomon Spring system.
The Culberson County Groundwater Conservation District seeks to
implement water management strategies to ``prevent the extreme decline
of water levels for the benefit of all water right owners, the economy,
our citizens, and the environment of the territory inside the
district'' (Culberson County Groundwater Conservation District 2007, p.
1). The missions of Jeff Davis County Underground Water District and
Presidio County Underground Water Conservation District are to ``strive
to develop, promote, and implement water conservation and management
strategies to protect water resources for the benefit of the citizens,
economy, and environment of the District'' (Jeff Davis County
Underground Water Conservation District 2008, p. 1; Presidio County
Underground Water Conservation District 2009, p. 1). However, all three
management plans specifically exclude addressing natural resources
issues as a goal because, ``The District has no documented occurrences
of endangered or threatened species dependent upon groundwater
resources'' (Culberson County Groundwater Conservation District 2007,
p. 10; Jeff Davis County Underground Water Conservation District 2008,
p. 19; Presidio County Underground Water Conservation District 2009, p.
14). This lack of acknowledgement of the relationship of the
groundwater resources under the Districts' management to the
conservation of the spring flow habitat at the San Solomon Spring
system prevents any direct benefits of their management plans for the
three aquatic invertebrates.
[[Page 49618]]
We also considered the desired future condition of the relevant
aquifer that supports San Solomon Spring system flows. The Culberson
County Groundwater Conservation District manages the groundwater where
the bulk of groundwater pumping occurs in the Salt Basin Bolson aquifer
(part of the West Texas Bolson, the source of the water for the San
Solomon Spring system) (Oliver 2010, p. 7). The desired future
condition for aquifers within the Culberson County Groundwater
Conservation District area includes a 24-m (78-ft) drawdown for the
West Texas Bolsons (Salt Basin Bolson aquifer in Wild Horse Flat) to
accommodate an average annual groundwater pumping of 46 million cm
(38,000 af) (Adams 2010, p. 2; Oliver 2010, p. 7). The desired future
condition for the West Texas Bolsons for Jeff Davis County Underground
Water Conservation District includes a 72-ft (22-m) drawdown over the
next 50 years to accommodate an average annual groundwater pumping of
10 million cm (8,075 af) (Adams 2010, p. 2; Oliver 2010, p. 7). The
desired future condition for the West Texas Bolsons for Presidio County
Underground Water District also includes a 72-ft (22-m) drawdown over
the next 50 years to accommodate an average annual groundwater pumping
of 12 million cm (9,793 af) (Adams 2010, p. 2; Oliver 2010, p. 7).
These drawdowns are based on analysis using groundwater availability
models developed for the Texas Water Development Board (Beach et al.
2004, p. 10-6-10-8; Oliver 2010, entire). We expect that these
groundwater districts will use their district rules to regulate water
withdrawals in such a way as to implement these desired future
conditions.
The Salt Basin Bolson aquifer in the Wild Horse Flat area (the
likely spring source) can range from 60 to 300 m (200 to 1,000 ft)
thick. So although it is impossible to determine precisely, we
anticipate the planned level of groundwater drawdown will likely result
in continued future declines in spring flow rates in the San Solomon
Spring system. Therefore, we expect that continued drawdown of the
aquifers as identified in the desired future conditions will contribute
to ongoing and future spring flow declines. Based on these desired
future conditions from the groundwater conservation districts, we
conclude that the regulatory mechanisms available to the groundwater
districts directing future groundwater withdrawal rates from the
aquifers that support spring flows in the San Solomon Spring system are
inadequate to protect against ongoing and future modification of
habitat for the Phantom Cave snail, Phantom springsnail, and diminutive
amphipod.
Summary of Factor D
Although there are some regulatory mechanisms in place, such as the
existence of groundwater conservation districts, we find that the
mechanisms are not serving to alleviate or limit the salient threats to
the Phantom Cave snail, Phantom springsnail, or diminutive amphipod.
We, therefore, conclude that these existing regulatory mechanisms are
inadequate to sufficiently reduce the identified threats to the Phantom
Cave snail, Phantom springsnail, and diminutive amphipod now and in the
future.
E. Other Natural or Manmade Factors Affecting Their Continued Existence
(San Solomon Spring Species)
We considered three other factors that may be affecting the
continued existence of the San Solomon Spring species: nonnative
snails, other nonnative species, and the small, reduced ranges of the
three San Solomon Spring species.
Nonnative Snails
Another factor that may be impacting the San Solomon Spring species
is the presence of two nonnative snails that occur in a portion of
their range. The red-rim melania and quilted melania both occur at San
Solomon Spring, and the red-rim melania also occurs at Phantom Lake and
Giffin Springs (Allan 2011, p. 1; Bradstreet 2011, pp. 4-5; Lang 2011,
pp. 4-5, 11). Both species are native to Africa and Asia and have been
imported into the United States as aquarium species. They are now
established in various locations across the southern and western
portions of the United States (Bradstreet 2011, pp. 4-5; U.S.
Geological Survey 2009, p. 2; Benson 2012, p. 2).
The red-rim melania was first reported from Phantom Lake Spring
during the 1990s (Fullington 1993, p. 2; McDermott 2000, pp. 14-15) and
was first reported from Giffin Spring in 2001 (Lang 2011, pp. 4-5). The
species has been at San Solomon Spring for some time longer (Texas
Parks and Wildlife Department 1999, p. 14), but it is not found in East
Sandia Spring (Lang 2011, p. 10; Allan 2011, p. 1). Bradstreet reported
the red-rim melania in all of the habitats throughout San Solomon
Spring at moderate densities compared to other snails, with a total
population estimate of about 390,000 snails ( 350,000)
(Bradstreet 2011, pp. 45-55). Lang (2011, pp. 4-5) also found moderate
densities of red-rim melania at Giffin Spring in both the headspring
area and downstream spring run area.
The quilted melania was first reported as being at San Solomon
Spring in 1999 (Texas Parks and Wildlife Department 1999, p. 14) from
observations in 1995 (Bowles 2012, pers. comm.). It was later collected
in 2001 (Lang 2011, p. 4), but not identified until Bradstreet (2011,
p. 4) confirmed its presence there. The species is not found in any
other springs in the San Solomon Spring system, but occurs in all
habitats throughout San Solomon Spring at moderate densities compared
to other snails, with a total population estimate of about 840,000
snails (1,070,000) (Bradstreet 2011, pp. 45-55).
The mechanism and extent of potential effects of the two nonnative
snails on the native invertebrates have not been studied directly.
However, because both nonnative snails occur in relatively high
abundances, it is reasonable to presume that they are likely competing
for space and food resources in the limited habitats in which they
occur. Rader et al. (2003, pp. 651-655) reviewed the biology and
possible impacts of red-rim melania and suggested that the species had
already displaced some native springsnails in spring systems of the
Bonneville Basin of Utah. Appleton et al. (2009, entire) reviewed the
biology and possible impacts of the quilted melania and found
potentially significant impacts likely to occur to the native benthic
invertebrate community in aquatic systems in South Africa. Currently,
East Sandia Spring has remained free of nonnative snails, but their
invasion there is a continuing concern (Bradstreet 2011, p. 95). We
conclude that these two snails may be having some negative effects on
the Phantom Cave snail, Phantom springsnail, and diminutive amphipod
based on a potential for competition for spaces and food resources.
Other Nonnative Species
A potential future threat to these species comes from the possible
introduction of additional nonnative species into their habitat. In
general, introduced species are a serious threat to native aquatic
species (Williams et al. 1989, p. 18; Lodge et al. 2000, p. 7). The
threat is particularly elevated at San Solomon Spring where the public
access to the habitat is prolific by the thousands of visitors to the
Balmorhea State Park who swim in the spring outflow pool.
Unfortunately, people will sometimes release nonnative species into
natural waters, intentionally or
[[Page 49619]]
unintentionally, without understanding the potential impacts to native
species. In spite of regulations that do not permit it, visitors to the
Park may release nonnative species into the outflow waters of San
Solomon Spring. This is presumably how the two nonnative snails became
established there. Nonnative fishes are sometimes seen and removed from
the water by Park personnel (Texas Parks and Wildlife Department 1999,
pp. 46-47). The Park makes some effort to minimize the risk of
nonnative species introductions by prohibiting fishing (so no live bait
is released) and by taking measures to educate visitors about the
prohibition of releasing species into the water (Texas Parks and
Wildlife Department 1999, pp. 48). In spite of these efforts, there is
an ongoing risk, which cannot be fully determined, that novel and
destructive nonnative species could be introduced in the future. This
risk is much lower at the other three springs in the San Solomon Spring
system because of the lack of public access to these sites.
We conclude that the future introduction of any nonnative species
represents an ongoing concern to the aquatic invertebrates, however,
the immediacy of this happening is relatively low because it is only a
future possibility. In addition, the severity of the impact is also
relatively low because it is most likely to occur only at San Solomon
Spring and the actual effects of any nonnative species on the Phantom
Cave snail, Phantom springsnail, and diminutive amphipod are unknown at
this time.
Small, Reduced Range
One important factor that contributes to the high risk of
extinction for these species is their naturally small range that has
been reduced from past destruction of their habitat. While the overall
extent of geographic range of the species has not changed, the number
and distribution of local populations within their range has likely
been reduced when other small springs within the San Solomon Spring
system (such as Saragosa, Toyah, and West Sandia Springs) ceased to
flow (Brune 1981, p. 386; Karges 2003, p. 145). These species are now
currently limited to four small spring outflow areas, with the
populations at Phantom Lake Spring in imminent threat of loss.
The geographically small range with only four populations of these
invertebrate species increases the risk of extinction from any effects
associated with other threats or stochastic events. When species are
limited to small, isolated habitats, they are more likely to become
extinct due to a local event that negatively affects the populations
(Shepard 1993, pp. 354-357; McKinney 1997, p. 497; Minckley and Unmack
2000, pp. 52-53). In addition, the species are restricted to aquatic
habitats in small spring systems and have minimal mobility and no other
habitats available for colonization, so it is unlikely their range will
ever expand beyond the current extent. This situation makes the
magnitude of impact of any possible threat very high. In other words,
the resulting effects of any of the threat factors under consideration
here, even if they are relatively small on a temporal or geographic
scale, could result in complete extinction of the species. While the
small, reduced range does not represent an independent threat to these
species, it does substantially increase the risk of extinction from the
effects of other threats, including those addressed in this analysis
and those that could occur in the future from unknown sources.
Summary of Factor E
The potential impacts of these nonnative snails and any future
introductions of other nonnative species on the Phantom Cave snail,
Phantom springsnail, and diminutive amphipod are largely unknown with
the current available information. But the nonnative snails are
presumed to have some negative consequences to the native snails
through competition for space and resources. The effects on the
diminutive amphipod are even less clear, but competition could still be
occurring. These nonnative snails have likely been co-occurring for at
least 20 years at three of the four known locations for these species,
and there is currently nothing preventing the invasion of the species
into East Sandia Spring. Considering the best available information, we
conclude that the presence of these two nonnative snails and the
potential future introductions of nonnative species currently represent
a low-intensity threat to the Phantom Cave snail, Phantom Lake
springsnail, and diminutive amphipod. In addition, the small, reduced
ranges of these species limit the number of available populations and
increase the risk of extinction from other threats. In combination with
the past and future threats from habitat modification and loss, these
factors contribute to the increased risk of extinction to the three
native species.
Proposed Determination--San Solomon Spring Species
We have carefully assessed the best scientific and commercial
information available regarding the past, present, and future threats
to the Phantom Cave snail, Phantom springsnail, and diminutive
amphipod. We find the species are in danger of extinction due to the
current and ongoing modification and destruction of their habitat and
range (Factor A) from the ongoing and future decline in spring flows,
and historic modification of spring channels. The most significant
factor threatening these species is a result of historic and future
declines in regional groundwater levels that have caused some springs
to cease flowing and threatens the remaining springs with the same
fate. We did not find any significant threats to the species under
Factors B or C. We found that existing regulatory mechanisms are
inadequate to provide protection to the species through groundwater
management by groundwater conservation districts (Factor D) from
existing and future threats. Finally, two nonnative snails occur in
portions of the species' range that could be another factor negatively
affecting the species (Factor E). The severity of the impact from these
nonnative snails or other future introductions of nonnative species is
not known, but such introductions may contribute to the risk of
extinction from the threats to habitat through reducing the abundance
of the three aquatic invertebrates through competition for space and
resources. The small, reduced ranges (Factor E) of these species, when
coupled with the presence of additional threats, also put them at a
heightened risk of extinction.
The elevated risk of extinction of the Phantom Cave snail, Phantom
springsnail, and diminutive amphipod is a result of the cumulative
nature of the stressors on the species and their habitats. For example,
the past reduction in available habitat through modification of spring
channels resulted in a lower number of individuals contributing to the
sizes of the populations. In addition, the loss of other small springs
that may have been inhabited by the species reduced the number of
populations that would contribute to the species' overall viability. In
this diminished state, the species are also facing future risks from
the impacts of continuing declining spring flows, exacerbated by
potential extended future droughts resulting from global climate
change, and potential effects from nonnative species. All of these
factors contribute together to heighten the risk of extinction and lead
to our finding that the Phantom Cave snail, Phantom springsnail, and
diminutive amphipod are in danger of
[[Page 49620]]
extinction throughout all of their ranges and warrant listing as
endangered species.
The Act defines an endangered species as any species that is ``in
danger of extinction throughout all or a significant portion of its
range'' and a threatened species as any species ``that is likely to
become endangered throughout all or a significant portion of its range
within the foreseeable future.'' We have carefully assessed the best
scientific and commercial information available regarding the past,
present, and future threats to the species, and have determined that
the Phantom Cave snail, Phantom springsnail, and diminutive amphipod
all meet the definition of endangered species under the Act.
Significant threats are occurring now and in the foreseeable future, at
a high intensity, and across the species' entire range, placing them on
the brink of extinction at the present time. Because the threats are
placing the species in danger of extinction now and not only in the
foreseeable future, we have determined that they meet the definition of
endangered species rather than threatened species. Therefore, on the
basis of the best available scientific and commercial information, we
propose listing the Phantom Cave snail, Phantom springsnail, and
diminutive amphipod as endangered species in accordance with sections
3(6) and 4(a)(1) of the Act.
Under the Act and our implementing regulations, a species may
warrant listing if it is threatened or endangered throughout all or a
significant portion of its range. The species proposed for listing in
this rule are highly restricted within their range, and the threats
occur throughout their range. Therefore, we assessed the status of the
species throughout their entire range. The threats to the survival of
the species occur throughout the species' range and are not restricted
to any particular significant portion of that range. Accordingly, our
assessment and proposed determination applies to the species throughout
their entire range.
Diamond Y Spring Species--Diamond Y Spring Snail, Gonzales Springsnail,
and Pecos Amphipod
The following five-factor analysis applies to the three species
that occur in the Diamond Y Spring system in Pecos County, Texas:
Diamond Y Spring snail, Gonzales springsnail, and Pecos amphipod.
A. The Present or Threatened Destruction, Modification, or Curtailment
of Their Habitat or Range (Diamond Y Spring Species)
Spring Flow Decline
The primary threat to the continued existence of the Diamond Y
Spring species is the degradation and potential future loss of aquatic
habitat (flowing water from the spring outlets) due to the decline of
groundwater levels in the aquifers that support spring surface flows.
Habitat for these species is exclusively aquatic and completely
dependent upon spring outflows. Spring flows in the Diamond Y Spring
system appear to have declined in flow rate over time, and as spring
flows decline available aquatic habitat is reduced and altered. When a
spring ceases to flow continually, all habitats for these species are
lost, and the populations will be extirpated. When all of the springs
lose consistent surface flows, all natural habitats for these aquatic
invertebrates will be gone, and the species will become extinct. We
know springs in this area can fail due to groundwater pumping, because
larger nearby springs, such as Comanche and Leon Springs have already
ceased flowing and likely resulted in the extirpation of local
populations of these species (assuming they were present historically).
The springs do not have to cease flowing completely to have an
adverse effect on invertebrate populations. The small size of the
spring outflows in the Diamond Y Spring system makes them particularly
susceptible to changes in water chemistry, increased water
temperatures, and freezing. Because these springs are small, any
reductions in the flow rates from the springs can reduce the available
habitat for the species, decreasing the number of individuals and
increasing the risk of extinction. Water temperatures and chemical
factors such as dissolved oxygen in springs do not typically fluctuate
(Hubbs 2001, p. 324); invertebrates are narrowly adapted to spring
conditions and are sensitive to changes in water quality (Hershler
1998, p. 11). Spring flow declines can lead to the degradation and loss
of aquatic invertebrate habitat and present a substantial threat to the
species.
There have been no regular recordings of spring flow discharge at
Diamond Y Spring to quantify any trends in spring flow. The total flow
rates are very low, as Veni (1991, p. 86) estimated total discharge
from the upper watercourse at 0.05 to .08 cms (2 to 3 cfs) and from the
lower watercourse at 0.04 to 0.05 cms (1 to 2 cfs). The nature of the
system with many diffuse and unconfined small springs and seeps makes
the estimates of water quantity discharging from the spring system
difficult to obtain. However, many authors (Veni 1991, p. 86; Echelle
et al. 2001, p. 28; Karges 2003, pp. 144-145) have described the
reductions in available surface waters observed compared to older
descriptions of the area (Kennedy 1977, p. 93; Hubbs et al. 1978, p.
489; Taylor 1985, pp. 4, 15, 21). The amount of aquatic habitat may
vary to some degree based on annual and seasonal conditions, but the
overall trend in the reduction in the amount of surface water over the
last several decades is apparent.
A clear example of the loss in aquatic habitat comes from Kennedy's
(1977, p. 93) description of one of his study sites in 1974. Station 2
was called a ``very large pool'' near Leon Creek of about 1,500 to
2,500 sq m (16,000 to 27,000 sq ft) with shallow depths of 0.5 to 0.6 m
(1.6 to 2.0 ft), with a small 2-m (6.6-ft) deep depression in the
center. Today very little open water is found in this area, only marshy
soils with occasional trickles of surface flow. This slow loss of
aquatic habitat has occurred throughout the system over time and
represents a substantial threat to the continued existence of the
Diamond Y Spring snail, Gonzales springsnail, and the Pecos amphipod.
The precise reason for the declining spring flows remains
uncertain, but it is presumed to be related to a combination of
groundwater pumping, mainly for agricultural irrigation, and a lack of
natural recharge to the supporting aquifers. In addition, future
changes in the regional climate are expected to exacerbate declining
flows.
Initial studies of the Diamond Y Spring system suggested that the
Edwards-Trinity aquifer was the primary source of flows (Veni 1991, p.
86). However, later studies seem to confirm that the Rustler aquifer is
instead more likely the chief source of water (Boghici 1997, p. 107).
The Rustler aquifer is one of the less-studied aquifers in Texas and
encompasses most of Reeves County and parts of Culberson, Pecos,
Loving, and Ward Counties in the Delaware Basin of west Texas (Boghici
and Van Broekhoven 2001, pp. 209-210). The Rustler strata are thought
to be between 75 to 200 m (250 to 670 ft) thick (Boghici and Van
Broekhoven 2001, p. 207). Very little recharge to the aquifer likely
comes from precipitation in the Rustler Hills in Culberson County, but
most of it may be contributed by cross-formational flows from old water
from deeper aquifer formations (Boghici and Van
[[Page 49621]]
Broekhoven 2001, pp. 218-219). Groundwater planning for the Rustler
aquifer anticipates no annual recharge (Middle Pecos Groundwater
Conservation District 2010b, p. 18).
Historic pumping from the Rustler aquifer in Pecos County may have
contributed to declining spring flows, as withdrawals of up to 9
million cm (7,500 af) in 1958 were recorded, with estimates from 1970
to 1997 suggesting groundwater use averaged between 430,000 cm (350 af)
to 2 million cm (1,550 af) per year (Boghici and Van Broekhoven 2001,
p. 218). As a result, declines in water levels in Pecos County wells in
the Rustler aquifer from the mid-1960s through the late 1970s of up to
30 m (100 ft) have been recorded (Boghici and Van Broekhoven 2001, p.
213). We assume that groundwater pumping has had some impacts on spring
flows of the Diamond Y Spring system in the past; however, they have
not yet been substantial enough to cause the main springs to cease
flowing.
Future groundwater withdrawals may further impact spring flow rates
if they occur in areas of the Rustler Aquifer that affect the spring
source areas. Groundwater pumping withdrawals in Pecos County are
expected to continue in the future mainly to support irrigated
agriculture (Region F Water Planning Group 2011, pp. 2-16-2-19) and
will result in continued lowering of the groundwater levels in the
Rustler aquifer. The latest plans from Groundwater Management Area 3
(the planning group covering the relevant portion of the Rustler
Aquifer) allows for a groundwater withdrawal in the Rustler Aquifer not
to exceed 90 m (300 ft) in the year 2060 (Middle Pecos Groundwater
Conservation District 2010a, p. 2). This level of drawdown will
accommodate 12.9 million cm (10,508 af) of annual withdrawals by
pumping (Middle Pecos Groundwater Conservation District 2010b, p. 15).
This level of pumping would be 30 times more than the long-term average
and could result in an extensive reduction in the available groundwater
in the aquifer based on the total thickness of the Rustler strata.
Therefore, we anticipate this level of groundwater drawdown may
contribute to continued declines in spring flow rates in the Diamond Y
Spring system.
Another factor possibly contributing to declining spring flows is
climatic changes that may increase the frequency and duration of local
and regional drought. The term ``climate'' refers to the mean and
variability of different types of weather conditions over time, with 30
years being a typical period for such measurements, although shorter or
longer periods also may be used (IPCC 2007a, p. 78). The term ``climate
change'' thus refers to a change in the mean or variability of one or
more measures of climate (e.g., temperature or precipitation) that
persists for an extended period, typically decades or longer, whether
the change is due to natural variability, human activity, or both (IPCC
2007a, p. 78).
Although the bulk of spring flows probably originates from water
sources with limited recent recharge, any decreases in regional
precipitation patterns due to prolonged drought will further stress
groundwater availability and increase the risk of diminishment or
drying of the springs. Drought affects both surface and groundwater
resources and can lead to diminished water quality (Woodhouse and
Overpeck 1998, p. 2693; MacRae et al. 2001, pp. 4, 10) in addition to
reducing groundwater quantities. Lack of rainfall may also indirectly
affect aquifer levels by resulting in an increase in groundwater
pumping to offset water shortages from low precipitation (Mace and Wade
2008, p. 665).
Recent drought conditions may be indicative of more common future
conditions. The current, multiyear drought in the western United
States, including the Southwest, is the most severe drought recorded
since 1900 (Overpeck and Udall 2010, p. 1642). In 2011, Texas
experienced the worst annual drought since recordkeeping began in 1895
(NOAA 2012, p. 4), and only 1 other year since 1550 (the year 1789) was
as dry as 2011 based on tree-ring climate reconstruction (NOAA 2011,
pp. 20-22). In addition, numerous climate change models predict an
overall decrease in annual precipitation in the southwestern United
States and northern Mexico.
Future global climate change may result in increased severity of
droughts and further contribute to impacts on the aquatic habitat from
reduction of spring flows. There is high confidence that many semiarid
areas like the western United States will suffer a decrease in water
resources due to ongoing climate change (IPCC 2007b, p. 7; Karl et al.
2009, pp. 129-131), as a result of less annual mean precipitation.
Milly et al. (2005, p. 347) also project a 10 to 30 percent decrease in
precipitation in mid-latitude western North America by the year 2050
based on an ensemble of 12 climate models. Even under lower greenhouse
gas emission scenarios, recent projections forecast a 10 percent
decline in precipitation in western Texas by 2080 to 2099 (Karl et al.
2009, pp. 129-130). Assessments of climate change in west Texas suggest
that the area is likely to become warmer and at least slightly drier
(Texas Water Development Board 2008, pp. 22-25).
The potential effects of future climate change could reduce overall
water availability in this region of western Texas and compound the
stressors associated with declining flows from the Diamond Y Spring
system. As a result of the effects of increased drought, spring flows
could decline indirectly as a result of increased pumping of
groundwater to accommodate human needs for additional water supplies
(Mace and Wade 2008, p. 664; Texas Water Development Board 2012c, p.
231).
In conclusion, the Diamond Y Spring snail, Gonzales springsnail,
and Pecos amphipod are in danger of extinction because of the past and
expected future loss of habitat associated with declining spring flows.
Some nearby springs have already gone dry. While the sources of the
stress of declining spring flows are not known for certain, the best
available scientific information would indicate that it is the result
of a combination of factors including past and current groundwater
pumping and climatic changes (decreased precipitation and recharge).
The threat of habitat loss from declining spring flows affects all the
entire range of all three species, as all are at risk of future loss
due to declining spring flows. All indications are that the source of
this threat will persist into the future and will result in continued
degradation of the species' habitats, placing them at a high risk of
extinction.
Water Quality Changes and Contamination
Another potential factor that could impact habitat of the Diamond Y
Spring species is the potential degradation of water quality from point
pollutant sources. This can occur either directly into surface water or
indirectly through contamination of groundwater that discharges into
spring run habitats used by the species. The primary threat for
contamination in these springs comes from activities related to oil and
gas exploration, extraction, transportation, and processing.
Oil and gas activities are a source of significant threat to the
Diamond Y Spring species because of the potential groundwater or
surface water contamination from pollutants (Veni 1991, p. 83;
Fullington 1991, p. 6). The Diamond Y Spring system is within an active
oil and gas extraction field that has been operational for many
decades. In 1990, there were 45 active and plugged wells within the
Diamond Y Preserve and an estimated 800 to 1,000 wells perforated the
aquifers within the
[[Page 49622]]
springs' drainage basins (Veni 1991, p. 83). At this time there are
still many active wells located within about 100 m (about 300 ft) of
surface waters. In addition, a natural gas processing plant, known as
the Gomez Plant, is located within 0.8 km (0.5 mi) upslope of Diamond Y
Spring. Oil and gas pipelines cross the habitat, and many oil
extraction wells are located near the occupied habitat. Oil and gas
drilling also occurs throughout the area of supporting groundwater
providing another potential source of contamination through the
groundwater supply. The Gomez Plant, which collects and processes
natural gas is located about 350 m (1,100 feet) up gradient from the
head pool of Diamond Y Spring (Hoover 2011, p. 1). Taylor (1985, p. 15)
suggested that an unidentified groundwater pollutant may have been
responsible for reductions in abundance of Diamond Y Spring snail in
the headspring and outflow of Diamond Y Spring, although there never
were any follow-up studies done to investigate the presumption. The
potential for an event catastrophic to the Diamond Y Spring species
from a contaminant spill or leak is possible at any time (Veni 1991, p.
83).
As an example of the possibility for spills, in 1992 approximately
10,600 barrels of crude oil were released from a 15-cm (6-in) pipeline
that traverses Leon Creek above its confluence with Diamond Y Draw. The
oil was from a pipeline, which ruptured at a point several hundred feet
away from the Leon Creek channel. The spill site itself is about 1.6 km
(1 mi) overland from Diamond Y Spring. The pipeline was operated at the
time of the spill by the Texas-New Mexico Pipeline Company, but
ownership has since been transferred to several other companies. The
Texas Railroad Commission has been responsible for overseeing cleanup
of the spill site. Remediation of the site initially involved
aboveground land farming of contaminated soil and rock strata to allow
microbial degradation. In later years, remediation efforts focused on
vacuuming oil residues from the surface of groundwater exposed by
trenches dug at the spill site. No impacts on the rare fauna of Diamond
Y Springs have been observed, but no specific monitoring of the effects
of the spill was undertaken (Industrial Economics, Inc. 2005, p. 4-12).
If a contaminant were to leak into the habitat of the species from
any of the various sources, the effects of the contamination could
result in death to exposed individuals, reductions in food
availability, or other ecological impacts (such as long-term alteration
to water or soil chemistry and the microorganisms that serve as the
base of food web in the aquatic ecosystem). The effects of a surface
spill or leak might be contained to a local area and only affect a
portion of the populations; however, an event that contaminated the
groundwater could impact both the upper and lower watercourses and
eliminate the entire range of all three species. There is currently no
regular monitoring of the water quality occurring for these species or
their habitats, so it is unlikely that the effects would be detected
quickly to allow for a timely response.
These invertebrates are sensitive to water contamination. Hydrobiid
snails as a group are considered sensitive to water quality changes,
and each species is usually found within relatively narrow habitat
parameters (Sada 2008, p. 59). Taylor (1985, p. 15) suggested that an
unidentified groundwater pollutant may have been responsible for
reductions in abundance of Diamond Y Spring snails in the headspring
and outflow of Diamond Y Spring, although no follow-up studies were
ever conducted to investigate the presumption. Additionally, amphipods
generally do not tolerate habitat desiccation (drying), standing water,
sedimentation, or other adverse environmental conditions; they are
considered very sensitive to habitat degradation (Covich and Thorpe
1991, pp. 676-677).
Several conservation measures have been implemented in the past to
reduce the potential for a contamination event. In the 1970s the U.S.
Department of Agriculture, Natural Resources Conservation Service (then
the Soil Conservation Service) built a small berm encompassing the
south side of Diamond Y Spring to prevent a surface spill from the
Gomez Plant from reaching the spring head. After The Nature Conservancy
purchased the Diamond Y Springs Preserve in 1990, oil and gas companies
undertook a number of conservation measures to minimize the potential
for contamination of the aquatic habitats. These measures included
decommissioning buried corrodible metal pipelines and replacing them
with synthetic surface lines, installing emergency shut-off valves,
building berms around oil pad sites, and removing abandoned oil pad
sites and their access roads that had been impeding surface water flow
(Karges 2003, p. 144).
Presently, there is no evidence of habitat destruction or
modification due to groundwater or surface water contamination from
leaks or spills, and no major spills affecting the habitat have been
reported in the past (Veni 1991, p. 83). However, the potential for
future adverse effects from a catastrophic event is an ongoing threat
of high severity of potential impact but not immediate.
Modification of Spring Channels
The spring outflow channels in the Diamond Y Spring system have
remained mostly intact. The main subtle changes in the past were a
result of some cattle grazing before The Nature Conservancy
discontinued livestock use in 2000, and roads and well pads that were
constructed in the spring outflow areas. Most of these structures were
removed by the oil and gas industry following The Nature Conservancy's
ownership in 1990. Several caliche (hard calcium carbonate material)
roads still cross the spring outflows with small culverts used to pass
the restricted flows.
A recent concern has been raised regarding the encroachment of
bulrush into the spring channels. Bulrush is an emergent plant that
grows in dense stands along the margins of spring channels. (An
emergent plant is one rooted in shallow water and having most of its
vegetative growth above the water.) When flow levels decline, reducing
water depths and velocities, bulrush can become very dense and dominate
the wetted channel. In 1998, bulrush made up 39 percent (
33 percent) of the plant species in the wetted marsh areas of the
Diamond Y Draw (Van Auken et al. 2007, p. 54). Observations by
Itzkowitz (2008, p. 5; 2010, pp. 13-14) found that bulrush were
increasing in density at several locations within the upper and lower
watercourses in Diamond Y Draw resulting in the loss of open water
habitats. Itzkowitz (2010, pp. 13-14) also noted a positive response by
bulrush following a controlled fire for grassland management.
In addition to water level declines, the bulrush encroachment may
have been aided by a small flume that was installed in 2000 about 100 m
(300 ft) downstream of the springhead pool at Diamond Y Spring (Service
1999, p. 2). The purpose of the flume was to facilitate spring flow
monitoring, but the instrumentation was not maintained. The flume
remains in place and is now being used for flow measurements by the
U.S. Geological Survey. The installation of the flume may have slightly
impounded the water upstream creating shallow, slow overflow areas
along the bank promoting bulrush growth. This potential effect of the
action was not foreseen (Service 1999, p. 3). Whether or not the flume
was the cause, the area upstream of it is now overgrown with bulrush,
and the two
[[Page 49623]]
snails have not been found in this section for some time.
There are several ways in which dense bulrush stands may alter
habitat for the invertebrates. Bulrush grows to a height of about 0.7 m
(2 ft) tall in very dense stands. Dense bulrush thickets will result in
increased shading of the water surface, which is likely to reduce the
algae and other food sources for the invertebrates. In addition, the
stems will slow the water velocity, and the root masses will collect
sediments and alter the substrates in the stream. These small changes
in habitat conditions may result in proportionally large areas of the
spring outflow channels being unsuitable for use by the invertebrates,
particularly the springsnails. Supporting this idea is the reported
distributions of the snails that found them in highest abundance in
areas with more open flowing water not dominated by bulrush (Allan
2011, p. 2). The impacts of dense bulrush stands as a result of
declining spring flow rates may be negatively affecting the
distribution and abundance of the invertebrates within the Diamond Y
Spring system.
Another recent impact to spring channels comes from disturbance by
feral hogs (Sus scrofa). These species have been released or escaped
from domestic livestock and have become free-ranging over time (Mapston
2005, p. 6). They have been in Texas for about 300 years and occur
throughout the State. The area around Diamond Y Spring has not
previously been reported as within their distribution (Mapston 2005, p.
5), but they have now been confirmed there (Allan 2011, p. 2). The
feral hogs prefer wet and marshy areas and damage spring channels by
creating wallows, muddy depressions used to keep cool and coat
themselves with mud (Mapston 2005, p. 15). In 2011, wallows were
observed in spring channels formerly inhabited by the invertebrates in
both the upper and lower watercourses at the Diamond Y Preserve (Allan
2011, p. 2). The alterations in the spring channels caused by the
wallows make the affected area uninhabitable by the invertebrates. The
effects of feral hog wallows are limited to small areas but act as
another stressor on the very limited habitat of these three Diamond Y
Spring species.
Some protection for the spring channel habitats for the Diamond Y
Spring species is provided with the ownership and management of the
Diamond Y Spring Preserve by The Nature Conservancy (Karges 2003, pp.
143-144). Their land stewardship efforts ensure that intentional or
direct impacts to the spring channel habitats will not occur. However,
land ownership by The Nature Conservancy provides limited ability to
prevent changes such as increases in bulrush or to control feral hogs.
Moreover, the Nature Conservancy can provide little protection from the
main threats to this species--the loss of necessary groundwater levels
to ensure adequate spring flows or contamination of groundwater from
oil and gas activities (Taylor 1985, p. 21; Karges 2003, pp. 144-145).
In summary, the modifications to the natural spring channels at the
Diamond Y Spring system represent activities that are occurring now and
will likely continue in the future through the continued encroachment
of bulrush as spring flows continue to decline and through the effects
of feral hog wallows. Conservation actions over the past two decades
have removed and minimized some past impacts to spring channels by
removing livestock and rehabilitating former oil pads and access roads.
While additional direct modifications are not likely to occur in the
future because of land ownership by The Nature Conservancy, future
modifications from bulrush encroachment and feral hog wallows
contribute to the suite of threats to the species' habitat by reducing
the overall quantity of available habitat and, therefore, reducing the
number of individuals of each species that can inhabit the springs. The
lower the overall number of individuals of each species and the less
available habitat, the greater the risk of extinction. Therefore, the
modification of spring channels contributes to increased risk of
extinction in the future as a consequence of ongoing and future
impacts.
Other Conservation Efforts
The Diamond Y Spring system is inhabited by two fishes federally
listed as endangered--Leon Springs pupfish (Service 1985, pp. 3) and
Pecos gambusia (Service 1983, p. 4). In addition, the area is also
inhabited by the federally threatened Pecos sunflower (Service 2005, p.
4) and the federally endangered Pecos assiminea snail (Service 2010, p.
5). Critical habitat has not been designated for Pecos gambusia. The
Diamond Y Spring has been designated as critical habitat for Leon
Springs pupfish, Pecos sunflower, and Pecos assiminea snail (45 FR
54678, August 15, 1980; 73 FR 17762, April 1, 2008; 76 FR 33036, June
7, 2011, respectively).
The three Diamond Y Spring species have been afforded some
protection indirectly in the past due to the presence of these other
listed species in the same locations. Management and protection of the
spring habitats by Texas Parks and Wildlife Department, The Nature
Conservancy, and the Service has benefited the aquatic invertebrates
(Karges 2007, pp. 19-20). However, the primary threat from the loss of
habitat due to declining spring flows related to groundwater changes
have not been abated by the Federal listing of the fish or other
species. Therefore, the conservation efforts provided by the
concomitant occurrence of species already listed under the Act have not
prevented past and current habitat loss, nor are they expected to do so
in the future.
Summary of Factor A
Based on our evaluation of the best available information, we
conclude that the present and future destruction and modification of
the habitat of the Diamond Y Spring snail, Gonzales springsnail, and
Pecos amphipod is a significant threat. These impacts in the past have
come from the loss of natural spring flows at several springs likely
within the historic range, and the future threat of the loss of
additional springs as groundwater levels are likely to decline in the
future. As springs decline throughout the small range of these species,
the number of individuals and populations will decline and continue to
increase the risk of extinction of these species. The sources of this
threat are not confirmed but are presumed to include a combination of
factors associated with groundwater pumping and climatic changes. The
potential for a spill of contaminants from oil and gas operations
presents a constant future threat to the quality of the aquatic
habitat. Finally, the risk of extinction is heightened by the ongoing
and future modification of spring channels, which reduces the number of
individuals in each population, from the encroachment of bulrush and
the presence of feral hogs.
B. Overutilization for Commercial, Recreational, Scientific, or
Educational Purposes (Diamond Y Spring Species)
There are very few people who are interested in or study
springsnails and amphipods, and those who do are sensitive to their
rarity and endemism. Consequently, collection for scientific or
educational purposes is very limited. There are no known commercial or
recreational uses of these invertebrates. For these reasons we conclude
that overutilization for commercial, recreational, scientific, or
educational purposes are not a threat to the Diamond Y Spring snail,
Gonzales springsnail, and Pecos amphipod, and
[[Page 49624]]
we have no indication that these factors will affect these species in
the future.
C. Disease or Predation (Diamond Y Spring Species)
The Diamond Y Spring species are not known to be affected by any
disease. These invertebrates are likely natural prey species for fishes
that occur in their habitats. There are no known nonnative predatory
fishes within their spring habitats, but there are crayfish, which are
known to prey on snails (Hershler 1998, p. 14). Ladd and Rogowski
(2012, p. 289) suggested that the nonnative red-rim melania may prey
upon different species of native snail eggs. However, the evidence of
such predation is very limited, and the extent to which the predation
might affect native snails is unknown. For more discussion about red-
rim melania, see ``Factor E. Other Natural or Manmade Factors Affecting
Its Continued Existence (Diamond Y Spring Species).'' We are not aware
of any other information indicating that the Diamond Y Spring species
are affected by disease or predation. For these reasons we conclude
that neither disease nor predation are threats to the Diamond Y Spring
snail, Gonzales springsnail, and Pecos amphipod, and we have no
indication that these factors will affect these species in the future.
D. The Inadequacy of Existing Regulatory Mechanisms (Diamond Y Spring
Species)
Under this factor, we examine whether existing regulatory
mechanisms are inadequate to address the threats to the species
discussed under the other four factors. Section 4(b)(1)(A) of the
Endangered Species Act requires the Service to take into account
``those efforts, if any, being made by any State or foreign nation, or
any political subdivision of a State or foreign nation, to protect such
species * * * .'' We interpret this language to require the Service to
consider relevant Federal, State, and Tribal laws and regulations that
may minimize any of the threats we describe in threat analyses under
the other four factors, or otherwise enhance conservation of the
species. An example would be the terms and conditions attached to a
grazing permit that describe how a permittee will manage livestock on a
BLM allotment. They are nondiscretionary and enforceable, and are
considered a regulatory mechanism under this analysis. Other examples
include State governmental actions enforced under a State statute or
constitution, or Federal action under statute.
Having evaluated the significance of the threat as mitigated by any
such conservation efforts, we analyze under Factor D the extent to
which existing regulatory mechanisms are inadequate to address the
specific threats to the species. Regulatory mechanisms, if they exist,
may reduce or eliminate the impacts from one or more identified
threats. In this section, we review existing State and Federal
regulatory mechanisms to determine whether they effectively reduce or
remove threats to the three San Solomon Spring species.
Texas laws provide no specific protection for these invertebrate
species, as they are not listed as threatened or endangered by the
Texas Parks and Wildlife Department. However, even if they were listed
by the State, those regulations (Title 31 Part 2 of Texas
Administrative Code) would only prohibit the taking, possession,
transportation, or sale of any animal species without the issuance of a
permit. The State makes no provision for the protection of the habitat
of listed species, which is the main threat to these aquatic
invertebrates.
Some protection for the habitat of this species is provided with
the land ownership of the springs by The Nature Conservancy. However,
this land ownership only protects the spring outflow channels and
provides no protection for maintaining groundwater levels to ensure
continuous spring flows.
In the following discussion we evaluate the local regulations
related to groundwater management within areas that might provide
indirect benefits to the species' habitats through management of
groundwater withdrawals, and Texas regulations for oil and gas
activities.
Local Groundwater Regulations
One regulatory mechanism that could provide some protection to the
spring flows for these species comes from local groundwater
conservation districts. Groundwater in Texas is generally governed by
the rule of capture unless there is a groundwater district in place.
The rule of capture allows a landowner to produce as much groundwater
as he or she chooses, as long as the water is not wasted (Mace 2001, p.
11). However, local groundwater conservation districts have been
established throughout much of Texas and are now the preferred method
for groundwater management in the State (Texas Water Development Board
2012, pp. 23-258). Groundwater districts ``may regulate the location
and production of wells, with certain voluntary and mandatory
exemptions'' (Texas Water Development Board 2012, p. 27).
There is currently one local groundwater district in the area
(Texas Water Development Board 2011, p. 1) that could possibly manage
groundwater to protect spring flows in the Diamond Y Spring system. The
Middle Pecos Groundwater Conservation District covers all of Pecos
County and was confirmed in 2002. The Middle Pecos County Groundwater
Conservation District seeks to implement water management strategies to
``help maintain a sustainable, adequate, reliable, cost effective and
high quality source of groundwater to promote the vitality, economy and
environment of the District'' (Middle Pecos Groundwater Conservation
District 2010b, p. 1). However, the management plan provides no
objectives to maintain spring flow at Diamond Y Spring or to otherwise
conserve the three aquatic invertebrates. This lack of acknowledgement
of the relationship between the groundwater resources under the
Districts' management to the conservation of the spring flow habitat at
the Diamond Y Spring system limits any direct benefits of the
management plan for the three aquatic invertebrates.
In 2010 the Groundwater Management Area 3 established ``desired
future conditions'' for the aquifers occurring within a six-county area
of west Texas (Texas Water Development Board 2012b, entire). These
projected conditions are important because they guide the plans for
water use of groundwater within groundwater conservation districts in
order to attain the desired future condition of each aquifer they
manage (Texas Water Development Board 2012c, p. 23). The latest plans
from Groundwater Management Area 3 (the planning group covering the
relevant portion of the Rustler aquifer) allows for a groundwater
withdrawal in the Rustler aquifer not to exceed a 90 m (300 ft)
drawdown in the year 2060 (Middle Pecos Groundwater Conservation
District 2010a, p. 2). The Rustler strata are thought to be between
only about 75 and 200 m (250 and 670 ft) thick. This level of drawdown
will accommodate 12.9 million cm (10,508 af) of annual withdrawals by
pumping (Middle Pecos Groundwater Conservation District 2010b, p. 15;
Williams 2010, pp. 3-5). We expect that the groundwater district will
use their district rules to regulate water withdrawals in such a way as
to implement these desired future conditions.
We expect that continued drawdown of the Rustler aquifer as
identified in the desired future conditions will
[[Page 49625]]
contribute to ongoing and future spring flow declines. Based on these
desired future conditions from the groundwater conservation district,
we find that the regulatory mechanisms directing future groundwater
withdrawal rates from the aquifer that supports spring flows in the
Diamond Y Spring system are inadequate to protect against ongoing and
future modification of habitat for the Diamond Y Spring snail, Gonzales
springsnail, and Pecos amphipod.
Texas Regulations for Oil and Gas Activities
The Railroad Commission of Texas has regulations that govern many
activities by the oil and gas industries to minimize the opportunity
for the release of contaminants into the surface water or groundwater
in Texas (Texas Administrative Code, Title 16. Economic Regulation,
Part 1). While the many regulations in place may be effective at
reducing the risk of contaminant releases, they cannot remove the
threat of a catastrophic event that could lead to the extinction of the
aquatic invertebrates. Therefore, because of the inherent risk
associated with oil and gas activities in proximity to the habitats of
the three Diamond Y Spring species, and the severe consequences to the
species of any contamination, Texas regulations for oil and gas
activities cannot remove or alleviate the threats associated with water
contamination from an oil or gas spill.
Summary of Factor D
Although there are regulatory mechanisms in place, such as the
existence of a local groundwater conservation district and State
regulations of oil and gas operations, we find that the mechanisms are
not serving to alleviate or limit the threats to the Diamond Y Spring
snail, Gonzales springsnail, or Pecos amphipod. We, therefore, conclude
that these mechanisms are inadequate to sufficiently reduce the
identified threats to these species.
E. Other Natural or Manmade Factors Affecting Their Continued Existence
(Diamond Y Spring Species)
We considered four other factors that may be affecting the
continued existence of the Diamond Y Spring species: nonnative fish
management, nonnative snail, other nonnative species, and the small,
reduced ranges of the three Diamond Y Spring species.
Nonnative Fish Management
Another source of potential impacts to these species comes from the
indirect effect of management to control nonnative fishes in Diamond Y
Spring. One of the major threats to the endangered Leon Springs
pupfish, which is also endemic to the Diamond Y Spring system, is
hybridization with the introduced, nonnative sheepshead minnow
(Cyprinodon variegatus). On two separate occasions efforts to eradicate
the sheepshead minnow have incorporated the use of fish toxicants in
the upper watercourse to kill and remove all the fish and restock with
pure Leon Springs pupfish. The first time was in the 1970s when the
chemical rotenone was used (Hubbs et al. 1978, pp. 489-490) with no
documented conservation efforts or monitoring for the invertebrate
community.
A second restoration effort was made in 1998 when the fish toxicant
Antimycin A was used (Echelle et al. 2001, pp. 9-10) in the upper
watercourse. In that effort, actions were taken to preserve some
invertebrates (holding them in tanks) during the treatment, and an
intense monitoring effort was conducted to measure the distribution and
abundance of the invertebrates immediately before and for 1 year after
the chemical treatment (Echelle et al. 2001, p. 14). The results
suggested that the Antimycin A had an immediate and dramatic negative
effect on Pecos amphipods; however, their abundance returned to
pretreatment levels within 7 months (Echelle et al. 2001, p. 23).
Gonzales springsnail also showed a decline in abundance that persisted
during the 1 year of monitoring following the treatment at both treated
and untreated sites (Echelle et al. 2001, pp. 23, 51).
There is no information available on the impacts of the initial
rotenone treatment, but we suspect that, like the later Antimycin A
treatment, there were at least short-term effects on the individuals of
the Diamond Y Spring species. Both of these chemicals kill fish and
other gill-breathing animals (like the three invertebrates) by
inhibiting their use of oxygen at the cellular level (U.S. Army Corps
of Engineers 2009, p. 2). Both chemicals are active for only a short
time, degrade quickly in the environment, and are not toxic beyond the
initial application. The long-term effects of these impacts are
uncertain, but the available information indicates that the Gonzales
springsnail may have responded negatively over at least 1 year. This
action was limited to the upper watercourse populations, and the
effects were likely short-term in nature.
The use of fish toxicants represents past stressors that are no
longer directly affecting the species but may have some lasting
consequences to the distribution and abundance of the snails. Currently
the Gonzales springsnail occurs in this area of the upper watercourse
in a very narrow stretch of the outflow channel from Diamond Y Spring,
and the Diamond Y Spring snail may no longer occur in this stretch.
Whether or not the application of the fish toxicants influenced these
changes in distribution and the current status of the Gonzales
springsnail is unknown. However, there is some possibility that these
actions could have contributed to the current absence of the Diamond Y
Spring snail from this reach and the restricted distribution of the
Gonzales springsnail that now occurs in this reach. These actions only
occurred in the past, and we do not anticipate them occurring again in
the future. If the sheepshead minnow were to invade this habitat again,
we do not expect that chemical treatment would be used due to a
heightened concern about conservation of the invertebrates. Therefore,
we consider this threat relatively insignificant because it was not
severe in its impact on the species, and it is not likely to occur
again in the future.
Nonnative Snail
Another factor that may be impacting the Diamond Y Spring species
is the presence of the nonnative red-rim melania, an invertebrate
species native to Africa and Asia that has been imported as an aquarium
species and is now established in various locations across the southern
and western portions of the United States (Benson 2012, p. 2).
The red-rim melania became established in Diamond Y Spring in the
mid 1990s (Echelle et al. 2001, p. 15; McDermott 2000, p. 15). The
exotic snail is now the most abundant snail in the Diamond Y Spring
system (Ladd 2010, p. 18). It only occurs in the first 270 m (890 ft)
of the upper watercourse of the Diamond Y Spring system, and it has not
been detected in the lower watercourse (Echelle et al. 2001, p. 26;
Ladd 2010, p. 22).
The mechanism and extent of potential effects of this nonnative
snail on the native invertebrates have not been studied directly.
However, because the snail occurs in relatively high abundances, it is
reasonable to presume that it is likely competing for space and food
resources in the limited habitats within which they occur. Rader et al.
(2003, pp. 651-655) reviewed the biology and possible impacts of red-
rim melania and suggested that the species had already displaced some
native springsnails in spring systems of the Bonneville Basin of Utah.
In the upper
[[Page 49626]]
watercourse where the red-rim melania occurs, only the Gonzales
springsnail occurs there now in very low abundance in the area of
overlap, and the Diamond Y Spring snail does not occur in this reach
any longer (Ladd 2010, p. 19).
The potential impacts of the red-rim melania on the three aquatic
invertebrate species in the Diamond Y Spring system are largely unknown
with the current available information, but the nonnative snail is
presumed to have some negative consequences to the native snails
through competition for space and resources. The effects on the Pecos
amphipod is even less clear, but competition could still be occurring.
The red-rim melania has been present in the upper watercourse since the
mid 1990s, and there is currently nothing preventing the invasion of
the species into Euphrasia Spring in the lower watercourse by an
incidental human introduction or downstream transport during a flood.
Considering the best available information, we conclude that the
presence of this nonnative snail represents a moderate threat to the
Diamond Y Spring snail, Gonzales springsnail, and Pecos amphipod.
Other Nonnative Species
A potential future threat to these species comes from the possible
introduction of additional nonnative species into their habitat. In
general, introduced species are a serious threat to native aquatic
species (Williams et al. 1989, p. 18; Lodge et al. 2000, p. 7). The
threat is moderated by the limited public access to the habitat on The
Nature Conservancy's preserve. Unfortunately, the limited access did
not prevent the introduction of the nonnative sheepshead minnow on two
separate occasions (Echelle et al. 2001, p. 4). In addition,
invertebrates could be inadvertently moved by biologists conducting
studies in multiple spring sites (Echelle et al. 2001, p. 26).
While the introduction of any future nonnative species could
represent a threat to the aquatic invertebrates, the likelihood of this
happening is relatively low because it is only a future possibility. In
addition the extent of the impacts of any future nonnative species on
the Diamond Y Spring snail, Gonzales springsnail, and Pecos amphipod
are unknown at this time.
Small, Reduced Range
One important factor that contributes to the high risk of
extinction for these species is their naturally small range that has
likely been reduced from past destruction of their habitat. The overall
geographic range of the species may have been reduced from the loss of
Comanche Springs (where the snails once occurred and likely the Pecos
amphipod did as well) and from Leon Springs (if they historically
occurred there). And within the Diamond Y Spring system, their
distribution has been reduced as flows from small springs and seeps
have declined and reduced the amount of wetted areas in the spring
outflow. These species are now currently limited to two small spring
outflow areas.
The geographically small range and only two proximate populations
of these invertebrate species increases the risk of extinction from any
effects associated with other threats or stochastic events. When
species are limited to small, isolated habitats, they are more likely
to become extinct due to a local event that negatively effects the
populations (Shepard 1993, pp. 354-357; McKinney 1997, p. 497; Minckley
and Unmack 2000, pp. 52-53). In addition, the species are restricted to
aquatic habitats in small spring systems and have minimal mobility and
no other habitats available for colonization, so it is unlikely their
range will ever expand beyond the current extent. This situation makes
the severity of impact of any possible separate threat very high. In
other words, the resulting effects of any of the threat factors under
consideration here, even if they are relatively small on a temporal or
geographic scale, could result in complete extinction of the species.
While the small, reduced range does not represent an independent threat
to these species, it does substantially increase the risk of extinction
from the effects of other threats, including those addressed in this
analysis, and those that could occur in the future from unknown
sources.
Summary of Factor E
We considered four additional stressors as other natural or manmade
factors that may be affecting these species. The effects from
management actions to control nonnative fish species are considered low
because they occurred in the past, with limited impact, and we do not
expect them to occur in the future. The potential impacts of the
nonnative snail red-rim melania and any future introductions of other
nonnative species on the Phantom Cave snail, Phantom springsnail, and
diminutive amphipod are largely unknown with the current available
information. But the nonnative snail is presumed to have some negative
consequences to the native snails through competition for space and
resources. The effects on the Pecos amphipod are even less clear, but
competition could still be occurring. These nonnative snails have
likely been co-occurring for up to 20 years at one of the two known
locations for these species, and there is currently nothing preventing
the invasion of the species into Euphrasia Spring by an incidental
human introduction or downstream transport during a flood. Considering
the best available information, we conclude that the presence of the
nonnative snail and the potential future introductions of nonnative
species represent a low magnitude threat to the Diamond Y Spring snail,
Gonzales springsnail, and Pecos amphipod. In addition, the effects of
the small, reduced ranges of these species limits the number of
available populations and increases the risk of extinction from other
threats. In combination with the past and future threats from habitat
modification and loss, these factors contribute to the increased risk
of extinction to the three native species.
Proposed Determination--Diamond Y Spring Species
We have carefully assessed the best scientific and commercial
information available regarding the past, present, and future threats
to the Diamond Y Spring snail, Gonzales springsnail, and Pecos
amphipod. We find the species are in danger of extinction due to the
current and ongoing modification and destruction of their habitat and
range (Factor A) from the ongoing and future decline in spring flows,
ongoing and future modification of spring channels, and threats of
future water contamination from oil and gas activities. The most
significant factor threatening these species is a result of historic
and future declines in regional groundwater levels that have caused the
spring system to have reduced surface aquatic habitat and threaten the
remaining habitat with the same fate. We did not find any significant
threats to the species under Factors B or C. We found that existing
regulatory mechanisms that could provide protection to the species
through groundwater management by groundwater conservation districts
and Texas regulations of the oil and gas activities (Factor D) are
inadequate to protect the species from existing and future threats.
Finally, the past management actions for nonnative fishes, the
persistence of the nonnative red-rim melania, and the future
introductions of other nonnative species are other factors that have or
could negatively affect the species (Factor E). The severity of the
impact from the red-rim melania is not known, but it and future
introductions may contribute to
[[Page 49627]]
the risk of extinction from the threats to habitat by reducing the
abundance of the three aquatic invertebrates through competition for
space and resources. The small, reduced ranges (Factor E) of these
species, when coupled with the presence of additional threats, also put
them at a heightened risk of extinction.
The elevated risk of extinction of the Diamond Y Spring snail,
Gonzales springsnail, and Pecos amphipod is a result of the cumulative
nature of the stressors on the species and their habitats. For example,
the past reduction in available habitat from declining surface water in
the Diamond Y Spring system results in lower numbers of individuals
contributing to the sizes of the populations. In addition, the loss of
other spring systems that may have been inhabited by these species
reduced the number of populations that would contribute to the species'
overall viability. In this diminished state, the species are also
facing future risks from the impacts of continuing declining spring
flows, exacerbated by potential extended future droughts resulting from
global climate change, and potential effects from nonnative species.
All of these factors contribute together to heighten the risk of
extinction and lead to our finding that the Diamond Y Spring snail,
Gonzales springsnail, and Pecos amphipod are in danger of extinction
throughout all of their ranges and warrant listing as endangered
species.
The Act defines an endangered species as any species that is ``in
danger of extinction throughout all or a significant portion of its
range'' and a threatened species as any species ``that is likely to
become endangered throughout all or a significant portion of its range
within the foreseeable future.'' We have carefully assessed the best
scientific and commercial information available regarding the past,
present, and future threats to the species, and have determined that
the Diamond Y Spring snail, Gonzales springsnail, and Pecos amphipod
all meet the definition of endangered under the Act. They do not meet
the definition of threatened species, because significant threats are
occurring now and in the foreseeable future, at a high magnitude, and
across the species' entire range, placing them on the brink of
extinction at the present time. Because the threats are placing the
species on the brink of extinction now and not only in the foreseeable
future, we have determined that they meet the definition of endangered
species rather than threatened species. Therefore, on the basis of the
best available scientific and commercial information, we propose
listing the Diamond Y Spring snail, Gonzales springsnail, and Pecos
amphipod as endangered species in accordance with sections 3(6) and
4(a)(1) of the Act.
Under the Act and our implementing regulations, a species may
warrant listing if it is threatened or endangered throughout all or a
significant portion of its range. The species proposed for listing in
this rule are highly restricted in their range, and the threats occur
throughout their ranges. Therefore, we assessed the status of these
species throughout their entire ranges. The threats to the survival of
these species occur throughout the species' ranges and are not
restricted to any particular significant portion of their ranges.
Accordingly, our assessments and proposed determinations apply to these
species throughout their entire ranges.
Available Conservation Measures
Conservation measures provided to species listed as endangered or
threatened under the Act include recognition, recovery actions,
requirements for Federal protection, and prohibitions against certain
practices. Recognition through listing results in public awareness and
conservation by Federal, state, tribal, and local agencies, private
organizations, and individuals. The Act encourages cooperation with the
States and requires that recovery actions be carried out for all listed
species. The protection required by Federal agencies and the
prohibitions against certain activities are discussed, in part, below.
The primary purpose of the Act is the conservation of endangered
and threatened species and the ecosystems upon which they depend. The
ultimate goal of such conservation efforts is the recovery of these
listed species, so that they no longer need the protective measures of
the Act. Subsection 4(f) of the Act requires the Service to develop and
implement recovery plans for the conservation of endangered and
threatened species. The recovery planning process involves the
identification of actions that are necessary to halt or reverse the
species' decline by addressing the threats to its survival and
recovery. The goal of this process is to restore listed species to a
point where they are secure, self-sustaining, and functioning
components of their ecosystems.
Recovery planning includes the development of a recovery outline
shortly after a species is listed, preparation of a draft and final
recovery plan, and revisions to the plan as significant new information
becomes available. The recovery outline guides the immediate
implementation of urgent recovery actions and describes the process to
be used to develop a recovery plan. The recovery plan identifies site-
specific management actions that will achieve recovery of the species,
measurable criteria that determine when a species may be downlisted or
delisted, and methods for monitoring recovery progress. Recovery plans
also establish a framework for agencies to coordinate their recovery
efforts and provide estimates of the cost of implementing recovery
tasks. Recovery teams (comprising species experts, Federal and State
agencies, nongovernmental organizations, and stakeholders) are often
established to develop recovery plans. When completed, the recovery
outline, draft recovery plan, and the final recovery plan will be
available on our Web site (https://www.fws.gov/endangered), or from our
Austin Ecological Services Field Office (see FOR FURTHER INFORMATION
CONTACT).
Implementation of recovery actions generally requires the
participation of a broad range of partners, including other Federal
agencies, States, Tribes, nongovernmental organizations, businesses,
and private landowners. Examples of recovery actions include habitat
restoration (e.g., restoration of native vegetation), research, captive
propagation and reintroduction, and outreach and education. The
recovery of many listed species cannot be accomplished solely on
Federal lands because their range may occur primarily or solely on non-
Federal lands. To achieve recovery of these species requires
cooperative conservation efforts on private, State, and Tribal lands.
If these species are listed, funding for recovery actions will be
available from a variety of sources, including Federal budgets, State
programs, and cost share grants for non-Federal landowners, the
academic community, and nongovernmental organizations. In addition,
pursuant to section 6 of the Act, the State of Texas would be eligible
for Federal funds to implement management actions that promote the
protection and recovery of these species. Information on our grant
programs that are available to aid species recovery can be found at:
https://www.fws.gov/grants.
Although the six aquatic invertebrates are only proposed for
listing under the Act at this time, please let us know if you are
interested in participating in recovery efforts for this species.
Additionally, we invite you to submit any new information on this
species whenever it becomes available and any information you may have
for recovery planning purposes (see FOR FURTHER INFORMATION CONTACT).
[[Page 49628]]
Section 7(a) of the Act requires Federal agencies to evaluate their
actions with respect to any species that is proposed or listed as
endangered or threatened and with respect to its critical habitat, if
any is designated. Regulations implementing this interagency
cooperation provision of the Act are codified at 50 CFR part 402.
Section 7(a)(4) of the Act requires Federal agencies to confer with the
Service on any action that is likely to jeopardize the continued
existence of a species proposed for listing or result in destruction or
adverse modification of proposed critical habitat. If a species is
listed subsequently, section 7(a)(2) of the Act requires Federal
agencies to ensure that activities they authorize, fund, or carry out
are not likely to jeopardize the continued existence of the species or
destroy or adversely modify its critical habitat. If a Federal action
may affect a listed species or its critical habitat, the responsible
Federal agency must enter into formal consultation with the Service.
Federal agency actions within the species habitat that may require
conference or consultation or both as described in the preceding
paragraph include management and any other landscape altering
activities on Federal lands administered by the U.S. Bureau of
Reclamation; issuance of section 404 Clean Water Act permits by the
Army Corps of Engineers; construction and management of gas pipeline
and power line rights-of-way by the Federal Energy Regulatory
Commission; and construction and maintenance of roads or highways by
the Federal Highway Administration.
The Act and its implementing regulations set forth a series of
general prohibitions and exceptions that apply to all endangered
wildlife. The prohibitions of section 9(a)(2) of the Act, codified at
50 CFR 17.21 for endangered wildlife, in part, make it illegal for any
person subject to the jurisdiction of the United States to take
(includes harass, harm, pursue, hunt, shoot, wound, kill, trap,
capture, or collect; or to attempt any of these), import, export, ship
in interstate commerce in the course of commercial activity, or sell or
offer for sale in interstate or foreign commerce any listed species.
Under the Lacey Act (18 U.S.C. 42-43; 16 U.S.C. 3371-3378), it is also
illegal to possess, sell, deliver, carry, transport, or ship any such
wildlife that has been taken illegally. Certain exceptions apply to
agents of the Service and State conservation agencies.
We may issue permits to carry out otherwise prohibited activities
involving endangered and threatened wildlife species under certain
circumstances. Regulations governing permits are codified at 50 CFR
17.22 for endangered species, and at 17.32 for threatened species. With
regard to endangered wildlife, a permit must be issued for the
following purposes: for scientific purposes, to enhance the propagation
or survival of the species, and for incidental take in connection with
otherwise lawful activities.
It is our policy, as published in the Federal Register on July 1,
1994 (59 FR 34272), to identify to the maximum extent practicable at
the time a species is listed, those activities that would or would not
constitute a violation of section 9 of the Act. The intent of this
policy is to increase public awareness of the effect of a proposed
listing on proposed and ongoing activities within the range of species
proposed for listing. The following activities could potentially result
in a violation of section 9 of the Act; this list is not comprehensive:
(1) Unauthorized collecting, handling, possessing, selling,
delivering, carrying, or transporting of the species, including import
or export across State lines and international boundaries, except for
properly documented antique specimens of these taxa at least 100 years
old, as defined by section 10(h)(1) of the Act;
(2) Introduction into the habitat of the six west Texas aquatic
invertebrate species of nonnative species that compete with or prey
upon any of the six west Texas aquatic invertebrate species;
(3) The unauthorized release of biological control agents that
attack any life stage of these species;
(4) Unauthorized modification of the springs or spring outflows
inhabited by the six west Texas aquatic invertebrates; and
(5) Unauthorized discharge of chemicals or fill material into any
waters in which these species are known to occur.
Questions regarding whether specific activities would constitute a
violation of section 9 of the Act should be directed to the Austin
Ecological Services Office (see FOR FURTHER INFORMATION CONTACT).
Critical Habitat
Prudency Determination
Section 4 of the Act, as amended, and implementing regulations (50
CFR 424.12), require that, to the maximum extent prudent and
determinable, the Secretary designate critical habitat at the time the
species is determined to be endangered or threatened. Our regulations
at 50 CFR 424.12(a)(1) state that the designation of critical habitat
is not prudent when one or both of the following situations exist: (1)
The species is threatened by taking or other activity and the
identification of critical habitat can be expected to increase the
degree of threat to the species; or (2) the designation of critical
habitat would not be beneficial to the species.
There is no indication that the six species of west Texas
invertebrates are threatened by collection and there are no likely
increases in the degree of threats to the species if critical habitat
were designated. These species are not targets of collection and the
areas proposed for designation either have restricted public access or
are already readily open to the public (i.e., Balmorhea State Park).
None of the threats identified to the species are associated with human
access to the sites, with the possible exception of the potential for
introducing nonnative species at San Solomon Spring in Balmorhea State
Park. This threat, or any other identified threat, is not expected to
increase as a result of critical habitat designation because the San
Solomon Spring swimming pool is already heavily visited, the Balmorhea
State Park take proactive measures to prevent introduction of non-
native species, and the designation of critical habitat will not change
the situation.
In the absence of finding that the designation of critical habitat
would increase threats to a species, if there are any benefits to a
critical habitat designation, then a prudent finding is warranted. The
potential benefits of critical habitat to the six west Texas
invertebrates include: (1) Triggering consultation under section 7 of
the Act, in new areas for actions in which there may be a Federal nexus
where it would not otherwise occur, because, for example, Federal
agencies were not aware of the potential impacts of an action on the
species; (2) focusing conservation activities on the most essential
features and areas; (3) providing educational benefits to State or
county governments or private entities; and (4) preventing people from
causing inadvertent harm to the species. Therefore, because we have
determined that the designation of critical habitat will not likely
increase the degree of threat to any of the six species and may provide
some measure of benefit, we find that designation of critical habitat
is prudent for the Phantom Cave snail, Phantom springsnail, diminutive
amphipod, Diamond Y Spring snail, Gonzales springsnail, and Pecos
amphipod.
[[Page 49629]]
Background
It is our intent to discuss below only those topics directly
relevant to the designation of critical habitat for six aquatic
invertebrates in this section of the proposed rules.
Critical habitat is defined in section 3 of the Act as:
(1) The specific areas within the geographical area occupied by the
species, at the time it is listed in accordance with the Act, on which
are found those physical or biological features;
(a) Essential to the conservation of the species; and
(b) Which may require special management considerations or
protection; and
(2) Specific areas outside the geographical area occupied by the
species at the time it is listed, upon a determination that such areas
are essential for the conservation of the species.
Conservation, as defined under section 3 of the Act, means to use
and the use of all methods and procedures that are necessary to bring
an endangered or threatened species to the point at which the measures
provided pursuant to the Act are no longer necessary. Such methods and
procedures include, but are not limited to, all activities associated
with scientific resources management such as research, census, law
enforcement, habitat acquisition and maintenance, propagation, live
trapping, and transplantation, and, in the extraordinary case where
population pressures within a given ecosystem cannot be otherwise
relieved, may include regulated taking.
Critical habitat receives protection under section 7 of the Act
through the requirement that Federal agencies ensure, in consultation
with the Service, that any action they authorize, fund, or carry out is
not likely to result in the destruction or adverse modification of
critical habitat. The designation of critical habitat does not affect
land ownership or establish a refuge, wilderness, reserve, preserve, or
other conservation area. Such designation does not allow the government
or public to access private lands. Such designation does not require
implementation of restoration, recovery, or enhancement measures by
non-Federal landowners. Where a landowner requests Federal agency
funding or authorization for an action that may affect a listed species
or critical habitat, the consultation requirements of section 7(a)(2)
of the Act would apply, but even in the event of a destruction or
adverse modification finding, the obligation of the Federal action
agency and the landowner is not to restore or recover the species, but
to implement reasonable and prudent alternatives to avoid destruction
or adverse modification of critical habitat.
Under the first prong of the Act's definition of critical habitat,
areas within the geographic area occupied by the species at the time it
was listed are included in a critical habitat designation if they
contain physical or biological features (1) which are essential to the
conservation of the species and (2) which may require special
management considerations or protection. For these areas, critical
habitat designations identify, to the extent known using the best
scientific and commercial data available, those physical or biological
features that are essential to the conservation of the species (such as
space, food, cover, and protected habitat). In identifying those
physical and biological features within an area, we focus on the
principal biological or physical constituent elements (primary
constituent elements such as roost sites, nesting grounds, seasonal
wetlands, water quality, tide, soil type) that are essential to the
conservation of the species. Primary constituent elements are the
elements of physical or biological features that, when laid out in the
appropriate quantity and spatial arrangement to provide for a species'
life-history processes, are essential to the conservation of the
species.
Under the second prong of the Act's definition of critical habitat,
we can designate critical habitat in areas outside the geographic area
occupied by the species at the time it is listed, upon a determination
that such areas are essential for the conservation of the species. For
example, an area currently occupied by the species but that was not
occupied at the time of listing may be essential to the conservation of
the species and may be included in the critical habitat designation. We
designate critical habitat in areas outside the geographic area
occupied by a species only when a designation limited to its range
would be inadequate to ensure the conservation of the species.
Section 4 of the Act requires that we designate critical habitat on
the basis of the best scientific data available. Further, our Policy on
Information Standards Under the Endangered Species Act (published in
the Federal Register on July 1, 1994 (59 FR 34271)), the Information
Quality Act (section 515 of the Treasury and General Government
Appropriations Act for Fiscal Year 2001 (Pub. L. 106-554; H.R. 5658)),
and our associated Information Quality Guidelines, provide criteria,
establish procedures, and provide guidance to ensure that our decisions
are based on the best scientific data available. They require our
biologists, to the extent consistent with the Act and with the use of
the best scientific data available, to use primary and original sources
of information as the basis for recommendations to designate critical
habitat.
When we are determining which areas should be designated as
critical habitat, our primary source of information is generally the
information developed during the listing process for the species.
Additional information sources may include the recovery plan for the
species, articles in peer-reviewed journals, conservation plans
developed by States and counties, scientific status surveys and
studies, biological assessments, other unpublished materials, or
experts' opinions or personal knowledge.
Habitat is dynamic, and species may move from one area to another
over time. We recognize that critical habitat designated at a
particular point in time may not include all of the habitat areas that
we may later determine are necessary for the recovery of the species.
For these reasons, a critical habitat designation does not signal that
habitat outside the designated area is unimportant or may not be needed
for recovery of the species. Areas that are important to the
conservation of the species, both inside and outside the critical
habitat designation, will continue to be subject to: (1) Conservation
actions implemented under section 7(a)(1) of the Act, (2) regulatory
protections afforded by the requirement in section 7(a)(2) of the Act
for Federal agencies to ensure their actions are not likely to
jeopardize the continued existence of any endangered or threatened
species, and (3) the prohibitions of section 9 of the Act if actions
occurring in these areas may affect the species. Federally funded or
permitted projects affecting listed species outside their designated
critical habitat areas may still result in jeopardy findings in some
cases. These protections and conservation tools will continue to
contribute to recovery of this species. Similarly, critical habitat
designations made on the basis of the best available information at the
time of designation will not control the direction and substance of
future recovery plans, habitat conservation plans, or other species
conservation planning efforts if new information available at the time
of these planning efforts calls for a different outcome.
[[Page 49630]]
Physical or Biological Features
In accordance with section 3(5)(A)(i) and 4(b)(1)(A) of the Act and
regulations at 50 CFR 424.12, in determining which areas within the
geographic area occupied by the species at the time of listing to
designate as critical habitat, we consider the physical or biological
features that are essential to the conservation of the species and
which may require special management considerations or protection.
These include, but are not limited to:
(1) Space for individual and population growth and for normal
behavior;
(2) Food, water, air, light, minerals, or other nutritional or
physiological requirements;
(3) Cover or shelter;
(4) Sites for breeding, reproduction, or rearing (or development)
of offspring; and
(5) Habitats that are protected from disturbance or are
representative of the historical, geographic, and ecological
distributions of a species.
We derive the specific physical or biological features required for
the Phantom Cave snail, Phantom springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive amphipod, and Pecos amphipod from
studies of the species' habitat, ecology, and life history as described
below. We have determined that the following physical or biological
features are essential for the Phantom Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales springsnail, diminutive amphipod, and
Pecos amphipod.
Space for Individual and Population Growth and for Normal Behavior
The aquatic environment associated with spring outflow channels and
marshes provide the habitat for Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail, Gonzales springsnail, diminutive
amphipod, and Pecos amphipod growth and normal behavior. The areas must
contain permanent flowing water to provide for the biological needs of
the species. Each of the species completes all of their life-history
functions in the water and cannot exist for any time outside of the
aquatic environment.
Several habitat parameters of springs, such as temperature,
dissolved carbon dioxide, dissolved oxygen, conductivity, substrate
type, and water depth have been shown to influence the distribution and
abundance of other related species of springsnails (O'Brien and Blinn
1999, pp. 231-232; Mladenka and Minshall 2001, pp. 209-211; Malcom et
al. 2005, p. 75; Martinez and Thome 2006, pp. 12-15; Lysne et al. 2007,
p. 650). Dissolved salts such as calcium carbonate may also be
important factors because they are essential for shell formation for
the snails (Pennak 1989, p. 552). Salinity levels are also relevant,
particularly at Diamond Y Spring because elevated salinity levels (3 to
6 parts per thousand (Hubbs 2001, p. 314) of dissolved salts) may
prevent other more freshwater-adapted species from competing with the
native species adapted to higher salinity levels.
The six invertebrates inhabit springs and spring-fed aquatic
habitats with low variability in water temperatures. For example, Hubbs
(2001, pp. 311-312, 314-315) reported that the spring outflow
temperatures had very low variability with average readings of 20
degrees Celsius ([deg]C) (68 degrees Fahrenheit ([deg]F)) at Diamond Y
Spring and 19[deg]C (66 [deg]F) at East Sandia Spring with a range
between 11 and 25 [deg]C (52 to 77[emsp14][deg]F). Spring measurements
from 2001 to 2003 at the four springs in the San Solomon Spring complex
found water temperatures ranging from 17 to 27 [deg]C (63 to
81[emsp14][deg]F) (Texas Water Development Board 2005, p. 38).
Proximity to spring vents, where water emerges from the ground, plays a
key role in the life history of the six west Texas aquatic
invertebrates. For example, many springsnail species exhibit decreased
abundance farther away from spring vents, presumably due to their need
for stable water chemistry (Hershler 1994, p. 68; Hershler 1998, p. 11;
Hershler and Sada 2002, p. 256; Martinez and Thome 2006, p. 14).
The six west Texas aquatic invertebrates are sensitive to water
contamination. Hydrobiid snails as a group are considered sensitive to
water quality changes, and each species is usually found within
relatively narrow habitat parameters (Sada 2008, p. 59). Taylor (1985,
p. 15) suggested that an unidentified groundwater pollutant may have
been responsible for reductions in abundance of Diamond Y Spring snail
in the headspring and outflow of Diamond Y Spring, although no follow-
up studies have been conducted to investigate the presumption.
Additionally, amphipods generally do not tolerate habitat desiccation
(drying), standing water, sedimentation, or other adverse environmental
conditions; they are considered very sensitive to habitat degradation
(Covich and Thorpe 1991, pp. 676-677).
All six species are most commonly found in flowing water,
presumably where dissolved oxygen levels are higher. The species are
often found in moderate flowing water along the spring outflow margins
rather than in central channels. Water depths where the species occur
are generally very shallow, usually less than 1 m (3 ft) deep. An
exception to this is the bottom of the San Solomon Spring pool where,
because of the construction of the swimming pool, water depths are much
greater, exceeding 5 m (15 ft). In San Solomon, Giffin, and Phantom
Lake Springs, the habitats for the species are limited to the spring
outflow channels because past alteration of the system (building of
ditches) has eliminated any small spring openings. However, at Diamond
Y Spring (and to a limited extent, East Sandia Spring) the spring
outflows have not been severely modified so that small springs, seeps,
and marshes still provide diffuse shallow flowing water habitat
associated with emergent bulrush and saltgrass (Taylor 1987, p. 38;
Echelle et al. 2001, p. 5). While these areas are more difficult to
map, measure, and survey, these small springs and seeps are important
habitat for the three invertebrate species at Diamond Y Spring as long
as they provide flowing water.
Therefore, based on the information above, we identify permanent,
flowing, unpolluted water (free from contamination) within natural
temperature variations, emerging from the ground and flowing on the
surface, to be a physical or biological feature necessary for these
species.
Food, Water, Air, Light, Minerals, or Other Nutritional or
Physiological Requirements
Invertebrates in small spring ecosystems depend on food from two
sources: that which grows in or on the substrate (aquatic and attached
plants and algae) and that which falls or is blown into the system
(primarily leaves). Water is also the medium necessary to provide the
algae, detritus (dead or partially decayed plant materials or animals),
bacteria, and submergent vegetation on which all six species depend as
a food resource. Abundant sunlight is necessary to promote the growth
of algae upon which all six west Texas aquatic invertebrates feed.
All four snails are presumably fine-particle feeders on detritus
(organic material from decomposing organisms) and periphyton (mixture
of algae and other microbes attached to submerged surfaces) associated
with the substrates (mud, rocks, and vegetation) (Allan 1995, p. 83;
Hershler and Sada 2002, p. 256; Lysne et al. 2007, p. 649). Dundee and
Dundee (1969, p. 207) found diatoms (a group of single-celled algae)
[[Page 49631]]
to be the primary component in the digestive tract of the Phantom Cave
snail and Phantom springsnail, indicating diatoms are a primary food
source. Spring ecosystems occupied by these snail species must support
the periphyton upon which springsnails graze. Additionally, submergent
vegetation contributes the necessary nutrients, detritus, and bacteria
on which these species forage.
Amphipods are omnivorous, feeding on algae, submergent vegetation,
and decaying organic matter (Smith 2001, p. 572). Both species of
amphipod are often found in beds of submerged aquatic plants (Cole
1976, p. 80), indicating that they probably feed on a surface film of
algae, diatoms, bacteria, and fungi (Smith 2001, p. 572). Young
amphipods depend on microbial foods, such as algae and bacteria,
associated with aquatic plants (Covich and Thorp 1991, p. 677).
Therefore, based on the information above, we identify the presence
of abundant food, consisting of algae, bacteria, decaying organic
material, and submergent vegetation that contributes the necessary
nutrients, detritus, and bacteria on which these species forage to be a
physical or biological feature for these species.
Sites for Cover or Shelter and for Breeding, Reproduction, or Rearing
(or Development) of Offspring
The six west Texas aquatic invertebrates occur across a wide range
of substrate types. The Phantom Cave snail is most commonly attached to
hard surfaces, especially large algae-covered rocks, submerged
vegetation, or even concrete walls of the irrigation ditches, and found
in areas of higher water velocities (Bradstreet 2011, pp. 73, 91). The
other springsnails may also be attached to hard surfaces but will also
often be found in the softer substrate at the margins of the stream
flows. Suitable substrates for egg laying by the snails are typically
firm, characterized by cobble, gravel, sand, woody debris, and aquatic
vegetation. These substrates increase productivity by providing
suitable egg-laying sites for the snails.
The amphipods, in the absence of predatory fishes, will swim over
any open substrate on the channel bottom, but in circumstances where
fishes are abundant they may be found in greater abundance underneath
large rocks, embedded in gravels, or associated with submerged
vegetation. Amphipods do not lay eggs upon a surface; instead, the eggs
are held within a marsupium (brood pouch) within the female's
exoskeleton.
Therefore, based on the information above, we identify substrates
that include cobble, gravel, pebble, sand, silt, and aquatic
vegetation, for breeding, egg laying, maturing, feeding, and escape
from predators to be a physical or biological feature for these
species.
Habitats Protected From Disturbance or Representative of the
Historical, Geographic, and Ecological Distributions of the Species
The Phantom Cave snail, Phantom springsnail, Diamond Y Spring
snail, Gonzales springsnail, diminutive amphipod, and Pecos amphipod
have a very restricted geographic distribution. Endemic species whose
populations exhibit a high degree of isolation are extremely
susceptible to extinction from both random and nonrandom catastrophic
natural or human-caused events. Therefore, it is essential to maintain
the spring systems in which they are currently found and upon which
these species depend. Adequate spring sites, free of inappropriate
disturbance, must exist to promote population expansion and viability.
This means protection from disturbance caused by water depletion, water
contamination, springhead alteration, or nonnative species. These
species must, at a minimum, sustain their current distributions if
ecological representation of these species is to be ensured.
As discussed above (see Factor E: Other Natural or Manmade Factors
Affecting Its Continued Existence), introduced species are a moderate
threat to native aquatic species (Williams et al. 1989, p. 18; Lodge et
al. 2000, p. 7), including the six west Texas aquatic invertebrates.
The red-rim melania already competes with all six species where they
occur, and the quilted melania has been introduced into habitats
occupied by the San Solomon Spring species. Feral hogs cause local
spring channel destruction within the Diamond Y Spring system. Because
the distribution of the Phantom Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales springsnail, diminutive amphipod, and
Pecos amphipod is so limited, and their habitat so restricted,
introduction of additional nonnative species into their habitat could
be devastating.
Therefore, based on the information above, we identify either an
absence of nonnative predators and competitors or nonnative predators
and competitors at low population levels to be a physical or biological
feature necessary for these species.
Primary Constituent Elements
Under the Act and its implementing regulations, we are required to
identify the physical or biological features essential to the
conservation of the Phantom Cave snail, Phantom springsnail, Diamond Y
Spring snail, Gonzales springsnail, diminutive amphipod, and Pecos
amphipod in areas occupied at the time of listing, focusing on the
features' primary constituent elements. We consider primary constituent
elements to be the elements of physical or biological features that
provide for a species' life-history processes and are essential to the
conservation of the species.
Based on our current knowledge of the physical or biological
features and habitat characteristics required to sustain the species'
life-history processes, we determine that the primary constituent
elements specific to the Phantom Cave snail, Phantom springsnail,
diminutive amphipod, Diamond Y Spring snail, Gonzales springsnail, and
Pecos amphipod are springs and spring-fed aquatic systems that contain:
a. Permanent, flowing, unpolluted water (free from contamination)
emerging from the ground and flowing on the surface;
b. Water temperatures that vary between 11 and 27 [deg]C (52 to
81[emsp14][deg]F) with natural seasonal and diurnal variations slightly
above and below that range;
c. Substrates that include cobble, gravel, pebble, sand, silt, and
aquatic vegetation, for breeding, egg laying, maturing, feeding, and
escape from predators;
d. Abundant food, consisting of algae, bacteria, decaying organic
material, and submergent vegetation that contributes the necessary
nutrients, detritus, and bacteria on which these species forage; and
e. Either an absence of nonnative predators and competitors or
nonnative predators and competitors at low population levels.
With this proposed designation of critical habitat, we intend to
identify the physical or biological features essential to the
conservation of the species, through the identification of the
appropriate quantity and spatial arrangement of the primary constituent
elements sufficient to support the life-history processes of the
species. All units and subunits proposed to be designated as critical
habitat are currently occupied by the Phantom Cave snail, Phantom
springsnail, Diamond Y Spring snail, Gonzales springsnail, diminutive
amphipod, and Pecos amphipod and contain the
[[Page 49632]]
primary constituent elements in the appropriate quantity and spatial
arrangement sufficient to support the life history needs of the
species.
Special Management Considerations or Protection
When designating critical habitat, we assess whether the specific
areas within the geographic area occupied by the species at the time of
listing contain features that are essential to the conservation of the
species and which may require special management considerations or
protection. The features essential to the conservation of the Phantom
Cave snail, Phantom springsnail, Diamond Y Spring snail, Gonzales
springsnail, diminutive amphipod, and Pecos amphipod may require
special management considerations or protection to reduce threats, such
as reducing or eliminating water in suitable or occupied habitat
through drought or groundwater pumping; introducing pollutants to
levels unsuitable for the species; and introducing nonnative species
into the inhabited spring systems such that suitable habitat is reduced
or eliminated. Special management considerations or protection are
required within critical habitat areas to address these threats (See
Summary of Factors Affecting the Species). Management activities that
could ameliorate these threats include management of groundwater levels
to ensure the springs remain flowing (all spring sites), managing oil
and gas activities to eliminate the threat of groundwater or surface
water contamination (Diamond Y Spring), maintaining the pump within
Phantom Lake Spring to ensure consistent flow, managing existing
nonnative species, red-rim melania, quilted melania, and feral hogs
(San Solomon, Giffin, Phantom Lake, and Diamond Y Springs), and
preventing the introduction of additional nonnative species (all spring
sites).
Criteria Used To Identify Critical Habitat
As required by section 4(b)(2) of the Act, we use the best
scientific data available to designate critical habitat. We review
available information pertaining to the habitat requirements of the
species. In accordance with the Act and its implementing regulation at
50 CFR 424.12(e), we consider whether designating additional areas--
outside those currently occupied as well as those occupied at the time
of listing--are necessary to ensure the conservation of the species. We
are not currently proposing to designate any areas outside the
geographic area occupied by the species because none of the
historically occupied areas (or those that may have been occupied) were
found to be essential for the conservation of the species (see
discussion below).
We relied on information from knowledgeable biologists and
recommendations contained in state wildlife resource reports (Dundee
and Dundee 1969, entire; Cole and Bousfield 1970, entire; Cole 1976,
entire; Cole 1985, entire; Taylor 1985, entire; Henry 1992, entire;
Bowles and Arsuffi 1993, entire; Seidel et al. 2009, entire; Hershler
et al. 2010, entire; Ladd 2010, entire; Allan 2011, entire; Bradstreet
2011, entire; Hershler 2011, p. 1) in making this determination. We
also reviewed the available literature pertaining to habitat
requirements, historic localities, and current localities for these
species. This includes regional geographic information system (GIS)
coverages.
Areas Occupied at the Time of Listing
For the purpose of designating critical habitat for the Phantom
Cave snail, Phantom springsnail, Diamond Y Spring snail, Gonzales
springsnail, diminutive amphipod, and Pecos amphipod, we defined the
occupied area based on the most recent surveys available, which
includes the Diamond Y and San Solomon Spring systems. We then
evaluated whether these areas contain the primary constituent elements
for the species and whether they require special management. Next we
considered areas historically occupied, but not currently occupied.
While the west Texas aquatic invertebrates may have inhabited other
springs in the area (such as Saragosa and Toyah Springs, for the San
Solomon Spring species, and Leon and Comanche Springs for the Diamond Y
Spring species), we only have confirmation that the Diamond Y Spring
snail and Gonzales springsnail occurred in Comanche Spring at some
point in the past. We evaluated these areas to determine whether they
were essential for the conservation of the species.
To determine if currently occupied areas contain the primary
constituent elements, we assessed the life-history components of the
species as they relate to habitat. All of the west Texas aquatic
invertebrate species require unpolluted spring water in the springheads
and spring outflows; periphyton and decaying organic material for food;
a combination of soft and hard substrates for maturation, feeding, egg
laying by snails, and escape from predators; and absence of nonnative
predators and competitors (see discussion on Physical or Biological
Features).
Areas Unoccupied at the Time of Listing
To determine if the sites that may have been historically occupied
by the Phantom Cave snail, Phantom springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive amphipod, and Pecos amphipod are
essential for their conservation, we considered: (1) The importance of
the site to the overall status of the species to prevent extinction and
contribute to future recovery of each species; (2) whether the area
could be restored to contain the necessary physical and biological
features to support the species; and (3) whether a population of the
species could be reestablished at the site.
The Phantom Cave snail, Phantom springsnail, and diminutive
amphipod occur in the San Solomon Spring system, which includes San
Solomon Spring, Giffin Spring, East Sandia Spring, and Phantom Spring.
These species may have occurred in other springs within the system,
including Saragosa, Toyah, and West Sandia Springs. These springs now
lack water flow and the physical or biological features necessary to
support the San Solomon Spring system invertebrates--mainly the lack of
flowing water. We do not foresee these features being restorable to the
point where populations of the Phantom Cave snail, Phantom springsnail,
and diminutive amphipod could be reestablished. These springs are not
restorable because we do not foresee an opportunity for groundwater
levels to rise sufficiently in the future to restore permanent spring
flows because the supporting aquifers are of ancient origin and do not
receive substantial modern recharge. Therefore, even if current pumping
activities were to be managed for the benefit of spring flows, it is
doubtful that aquifer levels would rise sufficiently to provide
restoration of permanent aquatic habitat at these sites. For these
reasons, we are not proposing Saragosa Spring, Toyah Spring, or West
Sandia Spring or any other unoccupied areas as critical habitat for the
San Solomon Spring system invertebrates.
The Diamond Y Spring snail, Gonzales springsnail, and Pecos
amphipod occur in the Diamond Y Spring system. The Diamond Y Spring
snail and Gonzales springsnail historically occurred at Comanche
Spring, and the Pecos amphipod may have occurred there as well. All
three species may have occurred at Leon Spring. Both Comanche Spring
and Leon Spring, which have aquifer
[[Page 49633]]
sources that may be different or more localized than that of Diamond Y
Spring, are dry or nearly so and have been altered to such a degree
that they no longer contain the physical or biological features
necessary to support the Diamond Y Spring invertebrates--mainly the
lack of flowing water. Natural flow conditions from these springs do
not appear to be restorable to the point where populations of the
Diamond Y Spring snail, Gonzales springsnail, and Pecos amphipod could
be reestablished. For these reasons, we are not proposing Leon Spring
or Comanche Spring as critical habitat for the Diamond Y Spring
invertebrates.
Mapping
For the areas we are proposing as critical habitat, we plotted the
known occurrences of the Phantom Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales springsnail, diminutive amphipod, and
Pecos amphipod in springheads and spring outflows on 2010 aerial
photography from U.S. Department of Agriculture, National Agriculture
Imagery Program base maps using ArcMap (Environmental Systems Research
Institute, Inc.), a computer geographic information system (GIS)
program. We drew the boundaries around the water features that make up
the critical habitat in each area. Other than at San Solomon Spring,
there are no known developed areas such as buildings, paved areas, and
other structures that lack the biological features for the springsnail
within the proposed critical habitat areas.
When determining proposed critical habitat boundaries, we made
every effort to avoid including developed areas such as lands covered
by buildings, pavement, and other structures because such lands lack
physical or biological features for the species. The scale of the maps
we prepared under the parameters for publication within the Code of
Federal Regulations may not reflect the exclusion of such developed
lands within Balmorhea State Park at San Solomon Spring. Any such lands
left inside critical habitat boundaries shown on the maps of these
proposed rules (such as the asphalt and concrete-paved dry surfaces in
Balmorhea State Park) have been excluded by text in these proposed
rules and are not proposed for designation as critical habitat.
Therefore, if the critical habitat is finalized as proposed, a Federal
action involving these lands would not trigger section 7 consultation
with respect to critical habitat and the requirement of no adverse
modification unless the specific action would affect the physical or
biological features in the adjacent critical habitat.
Summary
We are proposing for designation of critical habitat lands that we
have determined are occupied at the time of listing and contain
sufficient elements of physical or biological features to support life-
history processes essential for the conservation of the species. Units
were proposed for designation based on sufficient elements of physical
or biological features being present to support the Phantom Cave snail,
Phantom springsnail, Diamond Y Spring snail, Gonzales springsnail,
diminutive amphipod, and Pecos amphipod life-history processes. Some
units contain all of the identified elements of physical or biological
features and supported multiple life-history processes. Some segments
contained only some elements of the physical or biological features
necessary to support the Phantom Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales springsnail, diminutive amphipod, and
Pecos amphipod particular use of that habitat.
Proposed Critical Habitat Designation
We are proposing four areas as critical habitat for the Phantom
Cave snail, Phantom springsnail, and diminutive amphipod. We are
proposing one area as critical habitat for the Diamond Y Spring snail,
Gonzales springsnail, and Pecos amphipod. The critical habitat areas we
describe below constitute our current best assessment of areas that
meet the definition of critical habitat for the species. The five areas
we propose as critical habitat are: (1) San Solomon Spring, (2) Giffin
Spring, (3) East Sandia Spring, (4) Phantom Lake Spring, and (5) the
Diamond Y Spring System. Phantom Cave snail, Phantom springsnail, and
diminutive amphipod all occur in the first 4 units and they are listed
in Table 1. Diamond Y Spring snail, Gonzales springsnail, and Pecos
amphipod occur in the Diamond Y Spring Unit and it is listed in Table
2.
Table 1--Proposed Critical Habitat Units for Phantom Cave Snail, Phantom
Springsnail, and Diminutive Amphipod
[Area estimates reflect all land within critical habitat unit
boundaries]
------------------------------------------------------------------------
Land ownership by Size of unit in
Critical habitat unit type hectares (acres)
------------------------------------------------------------------------
San Solomon Spring............ State--Texas Parks 1.8 (4.4)
and Wildlife
Department.
Giffin Spring................. Private.............. 0.7 (1.7)
East Sandia Spring............ Private--The Nature 1.2 (3.0)
Conservancy.
Phantom Lake Spring........... Federal--Bureau of 0.02 (0.05)
Reclamation.
------------------
Total..................... ..................... 3.7 (9.2)
------------------------------------------------------------------------
Note: Area sizes may not sum due to rounding.
Table 2--Proposed Critical Habitat Unit for Diamond Y Spring Snail,
Gonzales Springsnail, and Pecos Amphipod
[Area estimate reflects all land within critical habitat unit
boundaries]
------------------------------------------------------------------------
Land ownership by Size of unit in
Critical habitat unit type hectares (acres)
------------------------------------------------------------------------
Diamond Y Spring System....... Private--The Nature 178.6 (441.4)
Conservancy.
Total..................... ..................... 178.6 (441.4)
------------------------------------------------------------------------
[[Page 49634]]
We present brief descriptions of all units, and reasons why they
meet the definition of critical habitat below.
San Solomon Spring Unit
The San Solomon Spring Unit consists of 1.8 ha (4.4 ac) that is
currently occupied by the Phantom Cave snail, Phantom springsnail, and
diminutive amphipod and contains all of the features essential to the
conservation of these species. It is located in Reeves County, near
Balmorhea, Texas. San Solomon Spring provides the water for the large
swimming pool at Balmorhea State Park, which is owned and managed by
Texas Parks and Wildlife Department. The proposed designation includes
all springs, seeps, and outflows of San Solomon Spring, including the
part of the concrete-lined pool that has a natural substrate bottom and
irrigation ditch, and two constructed ci[eacute]negas. While the
ditches do not provide all of the physical or biological features (such
as submerged vegetation), there are sufficient features (including
natural substrates on the ditch bottoms) to provide for the life-
history processes of the species. Habitat in this unit is threatened by
future declining spring flows due to drought or groundwater
withdrawals, the presence of nonnative snails, and the introduction of
other nonnative species. Therefore, the primary constituent elements in
this unit may require special management considerations or protection
to minimize impacts resulting from these threats.
Giffin Spring Unit
Giffin Spring Unit consists of 0.7 ha (1.7 ac) that is currently
occupied by the Phantom Cave snail, Phantom springsnail, and diminutive
amphipod and contains all of the features essential to the conservation
of these species. It is located on private property in Reeves County,
near Balmorhea, Texas, and its waters are captured in irrigation
earthen channels for agricultural use. The proposed designation
includes all springs, seeps, sinkholes, and outflows of Giffin Spring.
The unit contains most all of the identified physical and biological
features. Habitat in this unit is threatened by declining spring flows
due to drought or groundwater withdrawals, the presence of nonnative
snails, the introduction of other nonnative species, and further
modification of spring outflow channels. Therefore, the primary
constituent elements in this unit may require special management
considerations or protection to minimize impacts resulting from these
threats.
East Sandia Spring Unit
East Sandia Spring consists of 1.2 ha (3.0 ac) that is currently
occupied by the Phantom Cave snail, Phantom springsnail, and diminutive
amphipod and contains all of the features essential to the conservation
of these species. This unit is included within a preserve owned and
managed by The Nature Conservancy (Karges 2003, p. 145) in Reeves
County just east of Balmorhea, Texas. The proposed designation includes
the springhead itself and surrounding seeps and outflows. The unit
contains all of the identified physical and biological features.
Habitat in this unit is threatened by declining spring flows due to
drought or groundwater withdrawals, the introduction of nonnative
species, and modification of spring outflow channels. Therefore, the
primary constituent elements in this unit may require special
management considerations or protection to minimize impacts resulting
from these threats.
Phantom Lake Spring Unit
Phantom Lake Spring consists of a small pool about 0.02 ha (0.05
ac) in size that is currently occupied by the Phantom Cave snail,
Phantom springsnail, and diminutive amphipod and contains the features
essential to the conservation of these species. Phantom Lake Spring is
owned by the U.S. Bureau of Reclamation about 6 km (4 mi) west of
Balmorhea State Park in Jeff Davis County, Texas. The proposed
designation includes only the springhead pool. The physical or
biological features of the habitat at Phantom Lake Spring have been
maintained since 2000 by a pumping system and subsequent reconstruction
of the spring pool. Although artificially maintained, the site
continues to provide sufficient physical or biological features to
provide for all the life-history processes of the three invertebrate
species. Habitat in this unit is threatened by future declining spring
flows due to drought or groundwater withdrawals, the presence of
nonnative snails, and the introduction of other nonnative species.
Therefore, the primary constituent elements in this unit may require
special management considerations or protection to minimize impacts
resulting from these threats.
Diamond Y Spring Unit
Diamond Y Spring Unit consists of 178.6 ha (441.4 ac) that is
currently occupied by the Diamond Y Spring snail, Gonzales springsnail,
and Pecos amphipod and contains all of the features essential to the
conservation of these species. Diamond Y Spring and surrounding lands
are owned and managed by The Nature Conservancy. The proposed
designation includes the Diamond Y Spring and approximately 6.8 km (4.2
mi) of its outflow, including both upper and lower watercourses, ending
at approximately 0.8 km (0.5 mi) downstream of the State Highway 18
bridge crossing. Also included in this proposed unit is approximately
0.8 km (0.5 mi) of Leon Creek upstream of the confluence with Diamond Y
Draw. The boundaries of this unit extend out laterally beyond the
mapped spring outflow channels to incorporate any and all small springs
and seeps that may not be mapped or surveyed but are expected to
contain the species and the necessary physical or biological features.
The unit contains all of the identified physical and biological
features. Habitat in this unit is threatened by declining spring flows
due to drought or groundwater withdrawals, subsurface drilling and
other oil and gas activities that could contaminate surface drainage or
aquifer water, the presence of nonnative snails and feral hogs, the
introduction of other nonnative species, and modification of spring
outflow channels. Therefore, the primary constituent elements in this
unit may require special management considerations or protection to
minimize impacts resulting from these threats.
Effects of Critical Habitat Designation
Section 7 Consultation
Section 7(a)(2) of the Act requires Federal agencies, including the
Service, to ensure that any action they fund, authorize, or carry out
is not likely to jeopardize the continued existence of any endangered
species or threatened species or result in the destruction or adverse
modification of designated critical habitat of such species. In
addition, section 7(a)(4) of the Act requires Federal agencies to
confer with the Service on any agency action that is likely to
jeopardize the continued existence of any species proposed to be listed
under the Act or result in the destruction or adverse modification of
proposed critical habitat.
Decisions by the 5th and 9th Circuit Courts of Appeals have
invalidated our regulatory definition of ``destruction or adverse
modification'' (50 CFR 402.02) (see Gifford Pinchot Task Force v. U.S.
Fish and Wildlife Service, 378 F. 3d 1059 (9th Cir. 2004) and Sierra
Club v. U.S. Fish and Wildlife Service et al., 245
[[Page 49635]]
F.3d 434, 442 (5th Cir. 2001)), and we do not rely on this regulatory
definition when analyzing whether an action is likely to destroy or
adversely modify critical habitat. Under the statutory provisions of
the Act, we determine destruction or adverse modification on the basis
of whether, with implementation of the proposed Federal action, the
affected critical habitat would continue to serve its intended
conservation role for the species.
If a Federal action may affect a listed species or its critical
habitat, the responsible Federal agency (action agency) must enter into
consultation with us. Examples of actions that are subject to the
section 7 consultation process are actions on State, tribal, local, or
private lands that require a Federal permit (such as a permit from the
U.S. Army Corps of Engineers under section 404 of the Clean Water Act
(33 U.S.C. 1251 et seq.) or a permit from the Service under section 10
of the Act) or that involve some other Federal action (such as funding
from the Federal Highway Administration, Federal Aviation
Administration, or the Federal Emergency Management Agency). Federal
actions not affecting listed species or critical habitat, and actions
on State, tribal, local, or private lands that are not federally funded
or authorized, do not require section 7 consultation.
As a result of section 7 consultation, we document compliance with
the requirements of section 7(a)(2) through our issuance of:
(1) A concurrence letter for Federal actions that may affect, but
are not likely to adversely affect, listed species or critical habitat;
or
(2) A biological opinion for Federal actions that may affect, or
are likely to adversely affect, listed species or critical habitat.
When we issue a biological opinion concluding that a project is
likely to jeopardize the continued existence of a listed species and/or
destroy or adversely modify critical habitat, we provide reasonable and
prudent alternatives to the project, if any are identifiable, that
would avoid the likelihood of jeopardy and/or destruction or adverse
modification of critical habitat. We define ``reasonable and prudent
alternatives'' (at 50 CFR 402.02) as alternative actions identified
during consultation that:
(1) Can be implemented in a manner consistent with the intended
purpose of the action,
(2) Can be implemented consistent with the scope of the Federal
agency's legal authority and jurisdiction,
(3) Are economically and technologically feasible, and
(4) Would, in the Director's opinion, avoid the likelihood of
jeopardizing the continued existence of the listed species and/or avoid
the likelihood of destroying or adversely modifying critical habitat.
Reasonable and prudent alternatives can vary from slight project
modifications to extensive redesign or relocation of the project. Costs
associated with implementing a reasonable and prudent alternative are
similarly variable.
Regulations at 50 CFR 402.16 require Federal agencies to reinitiate
consultation on previously reviewed actions in instances where we have
listed a new species or subsequently designated critical habitat that
may be affected and the Federal agency has retained discretionary
involvement or control over the action (or the agency's discretionary
involvement or control is authorized by law). Consequently, Federal
agencies sometimes may need to request reinitiation of consultation
with us on actions for which formal consultation has been completed, if
those actions with discretionary involvement or control may affect
subsequently listed species or designated critical habitat.
Application of the ``Adverse Modification'' Standard
The key factor related to the adverse modification determination is
whether, with implementation of the proposed Federal action, the
affected critical habitat would continue to serve its intended
conservation role for the species. Activities that may destroy or
adversely modify critical habitat are those that alter the physical or
biological features to an extent that appreciably reduces the
conservation value of critical habitat for the Phantom Cave snail,
Phantom springsnail, Diamond Y Spring snail, Gonzales springsnail,
diminutive amphipod, and Pecos amphipod. As discussed above, the role
of critical habitat is to support the life-history needs of the species
and provide for the conservation of the species.
Section 4(b)(8) of the Act requires us to briefly evaluate and
describe, in any proposed or final regulation that designates critical
habitat, activities involving a Federal action that may destroy or
adversely modify such habitat, or that may be affected by such
designation.
Activities that may affect critical habitat, when carried out,
funded, or authorized by a Federal agency, should result in
consultation for the Phantom Cave snail, Phantom springsnail, Diamond Y
Spring snail, Gonzales springsnail, diminutive amphipod, and Pecos
amphipod. These activities include, but are not limited to:
(1) Actions that would reduce the quantity of water flow within the
spring systems proposed as critical habitat.
(2) Actions that would contaminate or cause significant degradation
of water quality within the spring systems proposed as critical
habitat, including surface drainage water or aquifer water quality.
(3) Actions that would modify the springheads or outflow channels
within the spring systems proposed as critical habitat.
(4) Actions that would reduce or alter the availability of aquatic
substrates within the spring systems that are proposed as critical
habitat.
(5) Actions that would reduce the occurrence of native aquatic
periphyton within the spring systems proposed as critical habitat.
(6) Actions that would introduce, promote, or maintain nonnative
predators and competitors within the spring systems proposed as
critical habitat.
Exemptions
Application of Section 4(a)(3) of the Act
The National Defense Authorization Act for Fiscal Year 2004 (Pub.
L. 108-136) amended the Act to limit areas eligible for designation as
critical habitat on some Department of Defense lands. There are no
Department of Defense lands within or near the proposed critical
habitat designation, so section 4(a)(3)(B)(i) of the Act does not
apply.
Exclusions
Application of Section 4(b)(2) of the Act
Section 4(b)(2) of the Act states that the Secretary shall
designate and make revisions to critical habitat on the basis of the
best available scientific data after taking into consideration the
economic impact, national security impact, and any other relevant
impact of specifying any particular area as critical habitat. The
Secretary may exclude an area from critical habitat if he determines
that the benefits of such exclusion outweigh the benefits of specifying
such area as part of the critical habitat, unless he determines, based
on the best scientific data available, that the failure to designate
such area as critical habitat will result in the extinction of the
species. In making that determination, the statute on its face, as well
as the legislative history, are clear that the Secretary has broad
discretion regarding
[[Page 49636]]
which factor(s) to use and how much weight to give to any factor.
Under section 4(b)(2) of the Act, we may exclude an area from
designated critical habitat based on economic impacts, impacts on
national security, or any other relevant impacts. In considering
whether to exclude a particular area from the designation, we identify
the benefits of including the area in the designation, identify the
benefits of excluding the area from the designation, and evaluate
whether the benefits of exclusion outweigh the benefits of inclusion.
If the analysis indicates that the benefits of exclusion outweigh the
benefits of inclusion, the Secretary may exercise his discretion to
exclude the area only if such exclusion would not result in the
extinction of the species.
Exclusions Based on Economic Impacts
Under section 4(b)(2) of the Act, we consider the economic impacts
of specifying any particular area as critical habitat. In order to
consider economic impacts, we are preparing an analysis of the economic
impacts of the proposed critical habitat designation and related
factors. Potential land use sectors that may be affected by critical
habitat designation include oil and gas development near the Diamond Y
Spring system and agriculture (irrigated lands using groundwater
withdrawals) at both spring systems. We also consider any social
impacts that might occur because of the designation.
We will announce the availability of the draft economic analysis as
soon as it is completed, at which time we will seek public review and
comment. At that time, copies of the draft economic analysis will be
available for downloading from the Internet at https://www.regulations.gov, or by contacting the Austin Ecological Services
Field Office directly (see FOR FURTHER INFORMATION CONTACT section).
During the development of a final designation, we will consider
economic impacts, public comments, and other new information, and areas
may be excluded from the final critical habitat designation under
section 4(b)(2) of the Act and our implementing regulations at 50 CFR
424.19.
Exclusions Based on National Security Impacts
Under section 4(b)(2) of the Act, we consider whether there are
lands owned or managed by the Department of Defense where a national
security impact might exist. In preparing this proposal, we have
determined that the lands within the proposed designation of critical
habitat for the Phantom Cave snail, Phantom springsnail, Diamond Y
Spring snail, Gonzales springsnail, diminutive amphipod, and Pecos
amphipod are not owned or managed by the Department of Defense, and,
therefore, we anticipate no impact on national security. Consequently,
the Secretary does not propose to exert his discretion to exclude any
areas from the final designation based on impacts on national security.
Exclusions Based on Other Relevant Impacts
Under section 4(b)(2) of the Act, we consider any other relevant
impacts, in addition to economic impacts and impacts on national
security. We consider a number of factors, including whether the
landowners have developed any habitat conservation plans or other
management plans for the area, or whether there are conservation
partnerships that would be encouraged by designation of, or exclusion
from, critical habitat. In addition, we look at any tribal issues, and
consider the government-to-government relationship of the United States
with tribal entities. We also consider any social impacts that might
occur because of the designation.
We are not proposing any exclusions at this time from the proposed
critical habitat designation under section 4(b)(2) of the Act based on
partnerships, management, or protection afforded by cooperative
management efforts. However, we are considering excluding the San
Solomon Spring Unit that is currently covered under a habitat
conservation plan with Texas Parks and Wildlife Department for the
Phantom Cave snail, Phantom springsnail, and diminutive amphipod for
management activities at Balmorhea State Park. This permit authorizes
``take'' of the invertebrates (which were candidates at the time of
issuance) in the State Park for ongoing management activities while
minimizing impacts to the aquatic species. The activities included in
the habitat conservation plan are a part of Texas Parks and Wildlife
Department's operation and maintenance of the State Park, including the
drawdowns associated with cleaning the swimming pool and vegetation
management within the refuge canal and ci[eacute]nega. The habitat
conservation plan also calls for restrictions and guidelines for
chemical use in and near aquatic habitats to avoid and minimize impacts
to the three aquatic invertebrate species (Service 2009a, pp. 9, 29-
32). The habitat conservation plan, however, provides no protection
from the main threat to this critical habitat unit--future declining
spring flows due to drought or groundwater withdrawals. In these
proposed rules, we are seeking input from the public as to whether or
not the Secretary should exclude the area within this habitat
conservation plan or other such areas under management that benefit the
Phantom Cave snail, Phantom springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive amphipod, and Pecos amphipod from the
final critical habitat designation. (Please see the Public Comments
section of this document for instructions on how to submit comments).
Peer Review
In accordance with our joint policy on peer review published in the
Federal Register on July 1, 1994 (59 FR 34270), we will seek the expert
opinions of at least three appropriate and independent specialists
regarding these proposed rules. The purpose of peer review is to ensure
that our critical habitat designation is based on scientifically sound
data, assumptions, and analyses. We have invited these peer reviewers
to comment during this public comment period on our specific
assumptions and conclusions in these proposed designations of critical
habitat.
We will consider all comments and information received during this
comment period on these proposed rules during our preparation of a
final determination. Accordingly, the final decision may differ from
this proposal.
Public Hearings
Section 4(b)(5) of the Act provides for one or more public hearings
on this proposal, if requested. Requests must be received within 45
days after the date of publication of these proposed rules in the
Federal Register. Such requests must be sent to the address shown in
FOR FURTHER INFORMATION CONTACT. We will schedule public hearings on
this proposal, if any are requested, and announce the dates, times, and
places of those hearings, as well as how to obtain reasonable
accommodations, in the Federal Register and local newspapers at least
15 days before the hearing.
Required Determinations
Regulatory Planning and Review--Executive Orders 12866 and 13563
Executive Order 12866 provides that the Office of Information and
Regulatory Affairs (OIRA) will review all significant rules. The Office
of Information and Regulatory Affairs has determined that this rule is
not significant.
Executive Order 13563 reaffirms the principles of E.O. 12866 while
calling for improvements in the nation's regulatory system to promote
predictability, to reduce uncertainty,
[[Page 49637]]
and to use the best, most innovative, and least burdensome tools for
achieving regulatory ends. The executive order directs agencies to
consider regulatory approaches that reduce burdens and maintain
flexibility and freedom of choice for the public where these approaches
are relevant, feasible, and consistent with regulatory objectives. E.O.
13563 emphasizes further that regulations must be based on the best
available science and that the rulemaking process must allow for public
participation and an open exchange of ideas. We have developed this
rule in a manner consistent with these requirements.
Regulatory Flexibility Act (5 U.S.C. 601 et seq.)
Under the Regulatory Flexibility Act (RFA; 5 U.S.C. 601 et seq.) as
amended by the Small Business Regulatory Enforcement Fairness Act
(SBREFA) of 1996 (5 U.S.C 801 et seq.), whenever an agency must publish
a notice of rulemaking for any proposed or final rule, it must prepare
and make available for public comment a regulatory flexibility analysis
that describes the effects of the rule on small entities (small
businesses, small organizations, and small government jurisdictions).
However, no regulatory flexibility analysis is required if the head of
the agency certifies the rule will not have a significant economic
impact on a substantial number of small entities. The SBREFA amended
the RFA to require Federal agencies to provide a certification
statement of the factual basis for certifying that the rule will not
have a significant economic impact on a substantial number of small
entities.
At this time, we lack the available economic information necessary
to provide an adequate factual basis for the required RFA finding.
Therefore, we defer the RFA finding until completion of the draft
economic analysis prepared under section 4(b)(2) of the Act and
Executive Order 12866. This draft economic analysis will provide the
required factual basis for the RFA finding. Upon completion of the
draft economic analysis, we will announce availability of the draft
economic analysis of the proposed designation in the Federal Register
and reopen the public comment period for the proposed designation. We
will include with this announcement, as appropriate, an initial
regulatory flexibility analysis or a certification that the rule will
not have a significant economic impact on a substantial number of small
entities accompanied by the factual basis for that determination. We
have concluded that deferring the RFA finding until completion of the
draft economic analysis is necessary to meet the purposes and
requirements of the RFA. Deferring the RFA finding in this manner will
ensure that we make a sufficiently informed determination based on
adequate economic information and provide the necessary opportunity for
public comment.
Energy Supply, Distribution, or Use--Executive Order 13211
Executive Order 13211 (Actions Concerning Regulations That
Significantly Affect Energy Supply, Distribution, or Use) requires
agencies to prepare Statements of Energy Effects when undertaking
certain actions. We do not expect the designation of this proposed
critical habitat to significantly affect energy supplies, distribution,
or use due to the small amount of habitat we are proposing for
designation and the lack of Federal activities that would be affected
by the designation. Therefore, this action is not a significant energy
action, and no Statement of Energy Effects is required. However, we
will further evaluate this issue as we conduct our economic analysis,
and review and revise this assessment as necessary.
Unfunded Mandates Reform Act (2 U.S.C. 1501 et seq.)
In accordance with the Unfunded Mandates Reform Act (2 U.S.C. 1501
et seq.), we make the following findings:
(1) This rule will not produce a Federal mandate. In general, a
Federal mandate is a provision in legislation, statute, or regulation
that would impose an enforceable duty upon State, local, or tribal
governments, or the private sector, and includes both ``Federal
intergovernmental mandates'' and ``Federal private sector mandates.''
These terms are defined in 2 U.S.C. 658(5)-(7). ``Federal
intergovernmental mandate'' includes a regulation that ``would impose
an enforceable duty upon State, local, or tribal governments'' with two
exceptions. It excludes ``a condition of Federal assistance.'' It also
excludes ``a duty arising from participation in a voluntary Federal
program,'' unless the regulation ``relates to a then-existing Federal
program under which $500,000,000 or more is provided annually to State,
local, and tribal governments under entitlement authority,'' if the
provision would ``increase the stringency of conditions of assistance''
or ``place caps upon, or otherwise decrease, the Federal Government's
responsibility to provide funding,'' and the State, local, or tribal
governments ``lack authority'' to adjust accordingly. At the time of
enactment, these entitlement programs were: Medicaid; Aid to Families
with Dependent Children work programs; Child Nutrition; Food Stamps;
Social Services Block Grants; Vocational Rehabilitation State Grants;
Foster Care, Adoption Assistance, and Independent Living; Family
Support Welfare Services; and Child Support Enforcement. ``Federal
private sector mandate'' includes a regulation that ``would impose an
enforceable duty upon the private sector, except (i) a condition of
Federal assistance or (ii) a duty arising from participation in a
voluntary Federal program.''
The designation of critical habitat does not impose a legally
binding duty on non-Federal Government entities or private parties.
Under the Act, the only regulatory effect is that Federal agencies must
ensure that their actions do not destroy or adversely modify critical
habitat under section 7. While non-Federal entities that receive
Federal funding, assistance, or permits, or that otherwise require
approval or authorization from a Federal agency for an action, may be
indirectly impacted by the designation of critical habitat, the legally
binding duty to avoid destruction or adverse modification of critical
habitat rests squarely on the Federal agency. Furthermore, to the
extent that non-Federal entities are indirectly impacted because they
receive Federal assistance or participate in a voluntary Federal aid
program, the Unfunded Mandates Reform Act would not apply, nor would
critical habitat shift the costs of the large entitlement programs
listed above onto State governments.
(2) We do not believe that this rule will significantly or uniquely
affect small governments because the land proposed for designation is
either privately owned or owned by U.S. Bureau of Reclamation or the
State of Texas. None of these government entities fit the definition of
``small governmental jurisdiction.'' Therefore, a Small Government
Agency Plan is not required. However, we will further evaluate this
issue as we conduct our economic analysis, and review and revise this
assessment if appropriate.
Takings--Executive Order 12630
In accordance with Executive Order 12630 (Government Actions and
Interference with Constitutionally Protected Private Property Rights),
we will analyze the potential takings implications of designating
critical habitat for the Phantom Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales springsnail, diminutive amphipod, and
Pecos amphipod in a
[[Page 49638]]
takings implications assessment. Critical habitat designation does not
affect landowner actions that do not require Federal funding or
permits, nor does it preclude development of habitat conservation
programs or issuance of incidental take permits to permit actions that
do require Federal funding or permits to go forward. The takings
implications assessment will analyze whether this proposed designation
of critical habitat for the Phantom Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales springsnail, diminutive amphipod, and
Pecos amphipod poses significant takings implications for lands within
or affected by the designation.
Federalism--Executive Order 13132
In accordance with Executive Order 13132 (Federalism), these
proposed rules do not have significant Federalism effects. A Federalism
assessment is not required. In keeping with Department of the Interior
and Department of Commerce policy, we requested information from, and
coordinated development of, these proposed critical habitat
designations with appropriate State resource agencies in Texas. The
designation of critical habitat in areas currently occupied by the
Phantom Cave snail, Phantom springsnail, Diamond Y Spring snail,
Gonzales springsnail, diminutive amphipod, and Pecos amphipod imposes
no additional restrictions to those currently in place and, therefore,
has little incremental impact on State and local governments and their
activities. The designation may have some benefit to these governments
because the areas that contain the physical or biological features
essential to the conservation of the species are more clearly defined,
and the elements of the features of the habitat necessary to the
conservation of the species are specifically identified. This
information does not alter where and what federally sponsored
activities may occur. However, it may assist local governments in long-
range planning (rather than having them wait for case-by-case section 7
consultations to occur).
Where State and local governments require approval or authorization
from a Federal agency for actions that may affect critical habitat,
consultation under section 7(a)(2) would be required. While non-Federal
entities that receive Federal funding, assistance, or permits, or that
otherwise require approval or authorization from a Federal agency for
an action, may be indirectly impacted by the designation of critical
habitat, the legally binding duty to avoid destruction or adverse
modification of critical habitat rests squarely on the Federal agency.
Civil Justice Reform--Executive Order 12988
In accordance with Executive Order 12988 (Civil Justice Reform),
the Office of the Solicitor has determined that the rule does not
unduly burden the judicial system and that it meets the requirements of
sections 3(a) and 3(b)(2) of the Order. We have proposed designating
critical habitat in accordance with the provisions of the Act. These
proposed rules use standard mapping technology and identify the
elements of physical or biological features essential to the
conservation of the Phantom Cave snail, Phantom springsnail, Diamond Y
Spring snail, Gonzales springsnail, diminutive amphipod, and Pecos
amphipod within the designated areas to assist the public in
understanding the habitat needs of the species.
Paperwork Reduction Act of 1995 (44 U.S.C. 3501 et seq.)
This rule does not contain any new collections of information that
require approval by OMB under the Paperwork Reduction Act of 1995 (44
U.S.C. 3501 et seq.). This rule will not impose recordkeeping or
reporting requirements on State or local governments, individuals,
businesses, or organizations. An agency may not conduct or sponsor, and
a person is not required to respond to, a collection of information
unless it displays a currently valid OMB control number.
National Environmental Policy Act (42 U.S.C. 4321 et seq.)
We have determined that environmental assessments and environmental
impact statements, as defined under the authority of the National
Environmental Policy Act (NEPA; 42 U.S.C. 4321 et seq.), need not be
prepared in connection with listing a species as endangered or
threatened under the Endangered Species Act. We published a notice
outlining our reasons for this determination in the Federal Register on
October 25, 1983 (48 FR 49244).
It is our position that, outside the jurisdiction of the U.S. Court
of Appeals for the Tenth Circuit, we do not need to prepare
environmental analyses pursuant to NEPA in connection with designating
critical habitat under the Endangered Species Act. We published a
notice outlining our reasons for this determination in the Federal
Register on October 25, 1983 (48 FR 49244). This position was upheld by
the U.S. Court of Appeals for the Ninth Circuit (Douglas County v.
Babbitt, 48 F.3d 1495 (9th Cir. 1995), cert. denied 516 U.S. 1042
(1996)). The range of the Phantom Cave snail, Phantom springsnail,
Diamond Y Spring snail, Gonzales springsnail, diminutive amphipod, and
Pecos amphipod does not occur in the Tenth Circuit, so a NEPA analysis
will not be conducted.
Clarity of the Rule
We are required by Executive Orders 12866 and 12988 and by the
Presidential Memorandum of June 1, 1998, to write all rules in plain
language. This means that each rule we publish must:
(1) Be logically organized;
(2) Use the active voice to address readers directly;
(3) Use clear language rather than jargon;
(4) Be divided into short sections and sentences; and
(5) Use lists and tables wherever possible.
If you feel that we have not met these requirements, send us
comments by one of the methods listed in the ADDRESSES section. To
better help us revise the rule, your comments should be as specific as
possible. For example, you should tell us the numbers of the sections
or paragraphs that are unclearly written, which sections or sentences
are too long, the sections where you feel lists or tables would be
useful, etc.
Government-to-Government Relationship with Tribes
In accordance with the President's memorandum of April 29, 1994
(Government-to-Government Relations with Native American Tribal
Governments; 59 FR 22951), Executive Order 13175 (Consultation and
Coordination with Indian Tribal Governments), and the Department of the
Interior's manual at 512 DM 2, we readily acknowledge our
responsibility to communicate meaningfully with recognized Federal
Tribes on a government-to-government basis. In accordance with
Secretarial Order 3206 of June 5, 1997 (American Indian Tribal Rights,
Federal-Tribal Trust Responsibilities, and the Endangered Species Act),
we readily acknowledge our responsibilities to work directly with
tribes in developing programs for healthy ecosystems, to acknowledge
that tribal lands are not subject to the same controls as Federal
public lands, to remain sensitive to Indian culture, and to make
information available to tribes.
We determined that there are no tribal lands within or near the
current or historic ranges of the Phantom Cave snail, Phantom
springsnail, Diamond Y
[[Page 49639]]
Spring snail, Gonzales springsnail, diminutive amphipod, and Pecos
amphipod that contain the features essential for conservation of the
species. Therefore, we are not proposing to designate critical habitat
on tribal lands.
References Cited
A complete list of references cited in this rulemaking is available
on the Internet at https://www.regulations.gov at Docket No. FWS-R2-ES-
2012-0029 and upon request from the Austin Ecological Services Field
Office (see FOR FURTHER INFORMATION CONTACT).
Authors
The primary authors of this package are the staff members of the
Southwest Region of the Service.
List of Subjects in 50 CFR Part 17
Endangered and threatened species, Exports, Imports, Reporting and
recordkeeping requirements, Transportation.
Proposed Regulation Promulgation
Accordingly, we propose to amend part 17, subchapter B of chapter
I, title 50 of the Code of Federal Regulations, as set forth below:
PART 17--[AMENDED]
1. The authority citation for part 17 continues to read as follows:
Authority: 16 U.S.C. 1361-1407; 16 U.S.C. 1531-1544; 16 U.S.C.
4201-4245; Pub. L. 99-625, 100 Stat. 3500; unless otherwise noted.
2. In Sec. 17.11(h) add entries for ``Snail, Diamond Y Spring'',
``Snail, Phantom Cave'', ``Springsnail, Gonzales'', and ``Springsnail,
Phantom'' under ``SNAILS'' and ``Amphipod, diminutive'' and ``Amphipod,
Pecos'' under ``CRUSTACEANS'' to the List of Endangered and Threatened
Wildlife in alphabetical order to read as follows:
Sec. 17.11 Endangered and threatened wildlife.
* * * * *
(h) * * *
--------------------------------------------------------------------------------------------------------------------------------------------------------
Species Vertebrate
--------------------------------------------------------- population where Critical Special
Historic range endangered or Status When listed habitat rules
Common name Scientific name threatened
--------------------------------------------------------------------------------------------------------------------------------------------------------
* * * * * * *
Snails:
* * * * * * *
Snail, Diamond Y Spring........ Pseudotryonia U.S.A. (TX)........... NA............... E......... ............ 17.95(f).... NA
adamantina.
* * * * * * *
Snail, Phantom Cave............ Pyrgulopsis texana..... U.S.A. (TX)........... NA............... E......... ............ 17.95(f).... NA
* * * * * * *
Springsnail, Gonzales.......... Tryonia circumstriata.. U.S.A. (TX)........... NA............... E......... ............ 17.95(f).... NA
* * * * * *
Springsnail, Phantom........... Tryonia cheatumi....... U.S.A. (TX)........... NA............... E......... ............ 17.95(f).... NA
* * * * * * *
Crustaceans:
Amphipod, diminutive........... Gammarus hyalleloides.. U.S.A. (TX)........... NA............... E......... ............ 17.95(h).... NA
* * * * * * *
Amphipod, Pecos................ Gammarus pecos......... U.S.A. (TX)........... NA............... E......... ............ 17.95(h).... NA
* * * * * * *
--------------------------------------------------------------------------------------------------------------------------------------------------------
3. Amend Sec. 17.95 by:
a. In paragraph (f), adding an entry for ``Diamond Y Spring snail
(Pseudotryonia adamantina) and Gonzales springsnail (Tryonia
circumstriata)'' followed by an entry for ``Phantom Cave snail
(Pyrgulopsis texana) and Phantom springsnail (Tryonia cheatumi)'' after
the entry for ``Interrupted Rocksnail (Leptoxis foremani)'', to read as
follows:
b. In paragraph (h), adding an entry for ``Diminutive amphipod
(Gammarus hyalleloides)'' and an entry for ``Pecos amphipod (Gammarus
pecos)'' in the same alphabetical order that these species appear in
the table at Sec. 17.11(h), to read as follows.
Sec. 17.95 Critical habitat--fish and wildlife.
* * * * *
(f) Clams and Snails.
* * * * *
Diamond Y Spring snail (Pseudotryonia adamantina) and Gonzales
springsnail (Tryonia circumstriata)
(1) A critical habitat unit is depicted for Pecos County, Texas, on
the map below.
(2) Within this area, the primary constituent elements of the
physical or biological features essential to the conservation of
Diamond Y Spring snail and Gonzales springsnail are springs and spring-
fed aquatic systems that contain:
(i) Permanent, flowing, unpolluted water (free from contamination)
emerging from the ground and flowing on the surface;
(ii) Water temperatures that vary between 11 and 27 [deg]C (52 to
81[emsp14][deg]F) with natural seasonal and diurnal variations slightly
above and below that range;
(iii) Substrates that include cobble, gravel, pebble, sand, silt,
and aquatic vegetation, for breeding, egg laying, maturing, feeding,
and escape from predators;
(iv) Abundant food, consisting of algae, bacteria, decaying organic
material, and submergent vegetation that contributes the necessary
nutrients, detritus, and bacteria on which these species forage; and
(v) Either an absence of nonnative predators and competitors or
nonnative
[[Page 49640]]
predators and competitors at low population levels.
(3) Critical habitat does not include manmade structures (such as
buildings, aqueducts, runways, roads, and other paved areas) and the
land on which they are located existing within the legal boundaries on
the effective date of this rule.
(4) Critical habitat map unit. Data layers defining the map unit
were created on 2010 aerial photography from U.S. Department of
Agriculture, National Agriculture Imagery Program base maps using
ArcMap (Environmental Systems Research Institute, Inc.), a computer
geographic information system (GIS) program. The maps in this entry, as
modified by any accompanying regulatory text, establish the boundaries
of the critical habitat designation. The coordinates or plot points or
both on which each map is based are available to the public at the
Service's internet site, (https://www.fws.gov/southwest/es/AustinTexas/
), Regulations.gov (https://www.regulations.gov at Docket No. FWS-R2-ES-
2012-0029) and at the field office responsible for this designation.
You may obtain field office location information by contacting one of
the Service regional offices, the addresses of which are listed at 50
CFR 2.2.
(5) Diamond Y Spring Unit, Pecos County, Texas. Map of Diamond Y
Spring Unit follows:
BILLING CODE 4310-55-P
[[Page 49641]]
[GRAPHIC] [TIFF OMITTED] TP16AU12.015
Phantom Cave snail (Pyrgulopsis texana) and Phantom springsnail
(Tryonia cheatumi)
(1) Critical habitat units are depicted for Jeff Davis County and
Reeves County, Texas, on the maps below.
(2) Within these areas, the primary constituent elements of the
physical or biological features essential to the conservation of
Phantom Cave snail and Phantom springsnail are springs and spring-fed
aquatic systems that contain:
(i) Permanent, flowing, unpolluted water (free from contamination)
emerging from the ground and flowing on the surface;
(ii) Water temperatures that vary between 11 and 27 [deg]C (52 to
81[emsp14][deg]F) with natural seasonal and diurnal variations slightly
above and below that range;
(iii) Substrates that include cobble, gravel, pebble, sand, silt,
and aquatic vegetation, for breeding, egg laying, maturing, feeding,
and escape from predators;
(iv) Abundant food, consisting of algae, bacteria, decaying organic
material, and submergent vegetation that contributes the necessary
nutrients, detritus, and bacteria on which these species forage; and
[[Page 49642]]
(v) Either an absence of nonnative predators and competitors or
nonnative predators and competitors at low population levels.
(3) Critical habitat does not include manmade structures (such as
buildings, aqueducts, runways, roads, and other paved areas) and the
land on which they are located existing within the legal boundaries on
the effective date of this rule.
(4) Critical habitat map units. Data layers defining map units were
created on 2010 aerial photography from U.S. Department of Agriculture,
National Agriculture Imagery Program base maps using ArcMap
(Environmental Systems Research Institute, Inc.), a computer geographic
information system (GIS) program. The maps in this entry, as modified
by any accompanying regulatory text, establish the boundaries of the
critical habitat designation. The coordinates or plot points or both on
which each map is based are available to the public at the Service's
Internet site (https://www.fws.gov/southwest/es/AustinTexas/),
Regulations.gov (https://www.regulations.gov at Docket No. FWS-R2-ES-
2012-0029) and at the field office responsible for this designation.
You may obtain field office location information by contacting one of
the Service regional offices, the addresses of which are listed at 50
CFR 2.2.
(5) San Solomon Spring Unit, Reeves County, Texas. Map of San
Solomon Spring Unit follows:
[[Page 49643]]
[GRAPHIC] [TIFF OMITTED] TP16AU12.016
(6) Giffin Spring Unit, Reeves County, Texas. Map of Giffin Spring
Unit is provided at subparagraph (5) of this entry.
(7) East Sandia Spring Unit, Jeff Davis County, Texas. Map of East
Sandia Spring Unit follows:
[[Page 49644]]
[GRAPHIC] [TIFF OMITTED] TP16AU12.017
(8) Phantom Lake Spring Unit, Jeff Davis County, Texas. Map of
Phantom Lake Spring Unit follows:
[[Page 49645]]
[GRAPHIC] [TIFF OMITTED] TP16AU12.018
* * * * *
(h) Crustaceans.
Diminutive amphipod (Gammarus hyalleloides)
(1) Critical habitat units are depicted for Jeff Davis County and
Reeves County, Texas, on the maps below.
(2) Within these areas, the primary constituent elements of the
physical or biological features essential to the conservation of
diminutive amphipod are springs and spring-fed aquatic systems that
contain:
(i) Permanent, flowing, unpolluted water (free from contamination)
emerging from the ground and flowing on the surface;
(ii) Water temperatures that vary between 11 and 27 [deg]C (52 to
81[emsp14][deg]F) with natural seasonal and diurnal variations slightly
above and below that range;
(iii) Substrates that include cobble, gravel, pebble, sand, silt,
and aquatic vegetation, for breeding, maturing, feeding, and escape
from predators;
(iv) Abundant food, consisting of algae, bacteria, decaying organic
material, and submergent vegetation that contributes the necessary
nutrients, detritus, and bacteria on which these species forage; and
[[Page 49646]]
(v) Either an absence of nonnative predators and competitors or
nonnative predators and competitors at low population levels.
(3) Critical habitat does not include manmade structures (such as
buildings, aqueducts, runways, roads, and other paved areas) and the
land on which they are located existing within the legal boundaries on
the effective date of this rule.
(4) Critical habitat map units. Data layers defining map units were
created on 2010 aerial photography from U.S. Department of Agriculture,
National Agriculture Imagery Program base maps using ArcMap
(Environmental Systems Research Institute, Inc.), a computer geographic
information system (GIS) program. The maps in this entry, as modified
by any accompanying regulatory text, establish the boundaries of the
critical habitat designation. The coordinates or plot points or both on
which each map is based are available to the public at the Service's
Internet site (https://www.fws.gov/southwest/es/AustinTexas/),
Regulations.gov (https://www.regulations.gov at Docket No. FWS-R2-ES-
2012-0029) and at the field office responsible for this designation.
You may obtain field office location information by contacting one of
the Service regional offices, the addresses of which are listed at 50
CFR 2.2.
(5) San Solomon Spring Unit, Reeves County, Texas. Map of San
Solomon Spring Unit follows:
[[Page 49647]]
[GRAPHIC] [TIFF OMITTED] TP16AU12.019
(6) Giffin Spring Unit, Reeves County, Texas. Map of Giffin Spring
Unit is provided at paragraph (5) of this entry.
(7) East Sandia Spring Unit, Jeff Davis County, Texas. Map of East
Sandia Spring Unit follows:
[[Page 49648]]
[GRAPHIC] [TIFF OMITTED] TP16AU12.020
(8) Phantom Lake Spring Unit, Jeff Davis County, Texas. Map of
Phantom Lake Spring Unit follows:
[[Page 49649]]
[GRAPHIC] [TIFF OMITTED] TP16AU12.021
* * * * *
Pecos amphipod (Gammarus pecos)
(1) The critical habitat unit is depicted for Pecos County, Texas,
on the map below.
(2) Within this area, the primary constituent elements of the
physical or biological features essential to the conservation of Pecos
amphipod are springs and spring-fed aquatic systems that contain:
(i) Permanent, flowing, unpolluted water (free from contamination)
emerging from the ground and flowing on the surface;
(ii) Water temperatures that vary between 11 and 27 [deg]C (52 to
81[emsp14][deg]F) with natural seasonal and diurnal variations slightly
above and below that range;
(iii) Substrates that include cobble, gravel, pebble, sand, silt,
and aquatic vegetation, for breeding, maturing, feeding, and escape
from predators;
(iv) Abundant food, consisting of algae, bacteria, decaying organic
material, and submergent vegetation that contributes the necessary
nutrients, detritus, and bacteria on which these species forage; and
(v) Either an absence of nonnative predators and competitors or
nonnative
[[Page 49650]]
predators and competitors at low population levels.
(3) Critical habitat does not include manmade structures (such as
buildings, aqueducts, runways, roads, and other paved areas) and the
land on which they are located existing within the legal boundaries on
the effective date of this rule.
(4) Critical habitat map units. Data layers defining map units were
created on 2010 aerial photography from U.S. Department of Agriculture,
National Agriculture Imagery Program base maps using ArcMap
(Environmental Systems Research Institute, Inc.), a computer geographic
information system (GIS) program. The maps in this entry, as modified
by any accompanying regulatory text, establish the boundaries of the
critical habitat designation. The coordinates or plot points or both on
which each map is based are available to the public at the Service's
Internet site (https://www.fws.gov/southwest/es/AustinTexas/),
Regulations.gov (https://www.regulations.gov at Docket No. FWS-R2-ES-
2012-0029) and at the field office responsible for this designation.
You may obtain field office location information by contacting one of
the Service regional offices, the addresses of which are listed at 50
CFR 2.2.
(5) Diamond Y Spring Unit, Pecos County, Texas. Map of Diamond Y
Spring Unit follows:
[[Page 49651]]
[GRAPHIC] [TIFF OMITTED] TP16AU12.022
* * * * *
Dated: August 2, 2012.
Eileen Sobeck,
Deputy Assistant Secretary for Fish and Wildlife and Parks.
[FR Doc. 2012-19829 Filed 8-15-12; 8:45 am]
BILLING CODE 4310-55-C