Rule2026-00581

Endangered and Threatened Wildlife and Plants; 12-Month Finding on a Petition To List the Olympic Peninsula Steelhead Distinct Population Segment Under the Endangered Species Act

Primary source

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Published
January 14, 2026

Issuing agencies

Commerce DepartmentNational Oceanic and Atmospheric Administration

Abstract

We, NMFS, have completed a comprehensive status review for the Olympic Peninsula (OP) Distinct Population Segment (DPS) of steelhead, Oncorhynchus mykiss, in response to a petition to list this species as threatened or endangered under the Endangered Species Act (ESA). We have determined that OP steelhead is a DPS under the ESA and that listing is not warranted at this time. Accordingly, NMFS will continue to monitor the OP steelhead DPS status, including working closely with Tribal and State co-managers.

Full Text

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<title>Federal Register, Volume 91 Issue 9 (Wednesday, January 14, 2026)</title>
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[Federal Register Volume 91, Number 9 (Wednesday, January 14, 2026)]
[Rules and Regulations]
[Pages 1449-1461]
From the Federal Register Online via the Government Publishing Office [<a href="http://www.gpo.gov">www.gpo.gov</a>]
[FR Doc No: 2026-00581]


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DEPARTMENT OF COMMERCE

National Oceanic and Atmospheric Administration

50 CFR Part 223

[Docket No. 260109-0027; RTID 0648-XR124]


Endangered and Threatened Wildlife and Plants; 12-Month Finding 
on a Petition To List the Olympic Peninsula Steelhead Distinct 
Population Segment Under the Endangered Species Act

AGENCY: National Marine Fisheries Service (NMFS), National Oceanic and 
Atmospheric Administration (NOAA), Commerce.

ACTION: Notification of 12-month petition finding.

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SUMMARY: We, NMFS, have completed a comprehensive status review for the 
Olympic Peninsula (OP) Distinct Population Segment (DPS) of steelhead, 
Oncorhynchus mykiss, in response to a petition to list this species as 
threatened or endangered under the Endangered Species Act (ESA). We 
have determined that OP steelhead is a DPS under the ESA and that 
listing is not warranted at this time. Accordingly, NMFS will continue 
to monitor the OP steelhead DPS status, including working closely with 
Tribal and State co-managers.

DATES: This finding was made available on January 14, 2026.

ADDRESSES: The petition, status review, Federal Register notices, and 
the list of references can be accessed electronically online at: 
<a href="https://www.fisheries.noaa.gov/species/steelhead-trout">https://www.fisheries.noaa.gov/species/steelhead-trout</a>. The peer review 
plan and charge to peer reviewers are available at <a href="https://www.noaa.gov/information-technology/biological-status-of-olympic-peninsula-steelhead-distinct-population-segment-dps-id478">https://www.noaa.gov/information-technology/biological-status-of-olympic-peninsula-steelhead-distinct-population-segment-dps-id478</a>.

FOR FURTHER INFORMATION CONTACT: Robert Markle, NMFS West Coast Region, 
at <a href="/cdn-cgi/l/email-protection#92e0fdf0f7e0e6bcfff3e0f9fef7d2fcfdf3f3bcf5fde4"><span class="__cf_email__" data-cfemail="a2d0cdc0c7d0d68ccfc3d0c9cec7e2cccdc3c38cc5cdd4">[email&#160;protected]</span></a>, (971) 710-8155.

SUPPLEMENTARY INFORMATION: 

Background

    On August 1, 2022, we received a petition from The Conservation 
Angler and Wild Fish Conservancy (hereafter, the Petitioners) to list 
the OP steelhead (Oncorhynchus mykiss) DPS as a threatened or 
endangered species under the ESA. On February 10, 2023, we published a 
positive 90-day finding (88 FR 8774) announcing that the petition 
presented substantial scientific or commercial information indicating 
that the petitioned action may be warranted. We also announced the 
initiation of a status review of the species, as required by section 
4(b)(3)(A) of the ESA, and requested information to inform the agency's 
decision on whether this species warrants listing as threatened or 
endangered.

[[Page 1450]]

Listing Species Under the Endangered Species Act

    To make a determination whether a species is threatened or 
endangered under the ESA, we first consider whether it constitutes a 
``species'' as defined under section 3 of the ESA, then whether the 
status of the species qualifies it for listing as either threatened or 
endangered. Under the ESA, a listing determination may address a 
species, which is defined to also include subspecies and, for any 
vertebrate species, any DPS that interbreeds when mature (16 U.S.C. 
1532(16)). On February 7, 1996, NMFS and the U.S. Fish and Wildlife 
Service (USFWS) adopted a joint policy for recognizing DPSs under the 
ESA (DPS Policy; 61 FR 4722). The DPS Policy adopted criteria similar 
to those in the evolutionarily significant unit (ESU) policy (ESU 
Policy; 56 FR 58612, November 20, 1991) for determining when a group of 
vertebrates constitutes a DPS: the group must be discrete from other 
populations, and it must be significant to its taxon (species or 
subspecies). A group of organisms is discrete if it is ``markedly 
separated from other populations of the same taxon as a consequence of 
physical, physiological, ecological, and behavioral factors.'' 
Significance is measured with respect to the taxon. Considerations for 
significance include but do not necessarily require the following:
    1. Persistence of the DPS in an ecological setting unusual or 
unique for the taxon,
    2. Evidence that loss of the DPS would result in a significant gap 
in the range of a taxon,
    3. Evidence that the DPS represents the only surviving natural 
occurrence of a taxon that may be more abundant elsewhere as an 
introduced population outside its historic range, or
    4. Evidence that the DPS differs markedly from other populations of 
the species in its genetic characteristics.
    In 2006, NMFS changed its previous practice of applying the ESU 
Policy to delineate species of O. mykiss and instead applied the joint 
DPS Policy (71 FR 834, January 5, 2006). NMFS determined that the use 
of the ESU Policy--originally intended for Pacific salmon--should not 
continue to be extended to O. mykiss, a type of salmonid with 
characteristics not typically exhibited by Pacific salmon. A court 
ruling in 2001 (Alsea Valley Alliance v. Evans, 161 F. Supp. 2d 1154 
(D. Or. 2001)) determined that listing only a subset of a species or 
ESU/DPS, such as the anadromous portion of O. mykiss, was not allowed 
under the ESA. Because of this court ruling, NMFS conducted updated 
status reviews for ESA-listed west coast steelhead ESUs that took into 
account those non-anadromous populations below dams and other major 
migration barriers that were considered to be part of the steelhead 
ESUs (Good et al., 2005). Subsequently, NMFS used the joint USFWS-NMFS 
DPS Policy to delineate steelhead-only DPSs rather than ESUs that 
included both steelhead and the related non-anadromous forms (71 FR 
833, January 5, 2006). OP steelhead (the petitioned entity) were not 
addressed in the 2005 status review (Good et al., 2005) nor in 
subsequent listings (71 FR 833, January 5, 2006).
    Section 3 of the ESA defines an endangered species as ``any species 
which is in danger of extinction throughout all or a significant 
portion of its range'' and a threatened species as one ``which is 
likely to become an endangered species within the foreseeable future 
throughout all or a significant portion of its range.'' Thus, in the 
context of the ESA, we interpret an endangered species to be one that 
is presently in danger of extinction, while a threatened species is not 
currently in danger of extinction but is likely to become so in the 
foreseeable future. The primary statutory difference between a 
threatened and endangered species is the timing of when a species is in 
danger of extinction, either presently (endangered) or not presently 
but within the foreseeable future (threatened).
    When we consider whether a species qualifies as threatened under 
the ESA, we must consider the meaning of the term ``foreseeable 
future.'' This is described in 50 CFR 42.11(d) as follows: ``In 
determining whether a species is a threatened species, the Services 
must analyze whether the species is likely to become an endangered 
species within the foreseeable future. The foreseeable future extends 
as far into the future as the Services can make reasonably reliable 
predictions about the threats to the species and the species' responses 
to those threats. The Services will describe the foreseeable future on 
a case-by-case basis, using the best available data and taking into 
account considerations such as the species' life-history 
characteristics, threat-projection timeframes, and environmental 
variability. The Services need not identify the foreseeable future in 
terms of a specific period of time.''
    Section 4(a)(1) of the ESA requires us to determine whether a 
species is endangered or threatened as a result of any one, or a 
combination of, the following 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 (16 U.S.C. 1533(a)(1)). We are also 
required to make listing determinations based solely on the best 
scientific and commercial data available, after conducting a review of 
the species' status and after taking into account efforts, if any, 
being made by any state or foreign nation (or subdivision thereof) to 
protect the species (16 U.S.C. 1533(b)(1)(A)).

Life History of West Coast Steelhead

    Steelhead is the name commonly applied to the anadromous form of 
the biological species O. mykiss. The present distribution of steelhead 
extends from Kamchatka in Asia, east to Alaska, and down to the U.S.-
Mexico border (Busby et al., 1996; 67 FR 21586, May 1, 2002). O. mykiss 
exhibit perhaps the most complex suite of life history traits of any 
species of Pacific salmonid. They can be anadromous (steelhead) or 
freshwater residents (rainbow or redband trout) and, under some 
circumstances, yield offspring of the alternative life-history form. 
Those that are anadromous can spend up to 7 years in freshwater prior 
to smoltification (the physiological and behavioral changes required 
for the transition to salt water) and then spend up to 3 years in salt 
water prior to first spawning. O. mykiss is also iteroparous, meaning 
individuals may spawn more than once (steelhead that survive spawning 
and return to the ocean are known as kelts), whereas other Pacific 
salmonid species are principally semelparous (meaning individuals 
predominately spawn once and die).
    Within the range of west coast steelhead, spawning migrations occur 
throughout the year, with seasonal peaks of activity. In a given river 
basin, there may be one or more peaks in migration activity known as 
``runs,'' which are usually named for the season in which the peak 
occurs. Rivers can contain one or more runs of winter-, spring-, 
summer-, or fall-run steelhead. In basins with both summer-run and 
winter-run steelhead, the summer run generally occurs where habitat is 
not fully utilized by the winter run or where a temporal hydrologic 
barrier, such as a waterfall, separates them. Summer-run steelhead 
usually spawn farther upstream than winter-run steelhead (Withler 1966; 
Roelofs 1983; Behnke 1992; Myers et al., 2015).

[[Page 1451]]

Previous Status Review

    In 1996, NMFS completed a comprehensive status review of coastal 
and inland steelhead populations in Washington, Oregon, Idaho, and 
California (Busby et al., 1996). As part of this review, which was 
prior to the practice of using the DPS Policy to delineate steelhead 
populations, NMFS identified an OP steelhead ESU comprised of 
populations that occupy ``river basins of the Olympic Peninsula, 
Washington, west of the Elwha River and south to, but not including, 
the rivers that flow into Grays Harbor on the Washington coast.'' The 
OP steelhead ESU was primarily made up of winter-run steelhead but also 
included several summer-run steelhead populations (Busby et al., 1996). 
At the time, NMFS included the resident O. mykiss below long-standing 
natural barriers in the ESU because of the opportunity for residents to 
interbreed with anadromous life history forms. In determining OP 
steelhead as an ESU, Busby et al. (1996) stated:
    Genetic data collected by Washington Department of Fish and 
Wildlife support the hypothesis that, as a group, steelhead populations 
from the Olympic Peninsula are substantially isolated from those in 
other regions of western Washington. The Olympic Peninsula ESU is 
further characterized by habitat, climatic, and zoogeographical 
differences between it and adjacent ESUs. The Olympic Peninsula 
includes coastal basins that receive more precipitation than any other 
area in the range of west coast steelhead. Topography on the Olympic 
Peninsula is characterized by much greater relief than that to the 
south (Willapa Hills); the Olympic Mountains range from 1,200 to 2,400 
meters above sea level. This affects precipitation quantity and river-
basin hydrography. The result is ``copious amounts of rain and over 100 
inches of snow during the winter months'' as well as substantial summer 
precipitation (Jackson 1993, p. 50-51) [Figure 3, Figure 4]. One 
manifestation of the ecological difference between Puget Sound and the 
Olympic Peninsula is the shift in vegetation zone, respectively, from 
western hemlock (Tsuga heterophylla) to Sitka spruce (Picea sitchensis) 
(Frenkel 1993).
    NMFS concluded that the OP steelhead ESU was not in danger of 
extinction or likely to become endangered in the foreseeable future 
(Busby et al., 1996). However, NMFS was concerned about the overall 
health of the ESU and specific populations. Although the majority of 
abundance trends for winter-run OP steelhead were positive at the time 
of the 1996 review, including for three of the four largest 
populations, several other populations had downward trends, and for 
three populations this decline was statistically significant. NMFS 
noted concerns that hatchery fish were widespread, and interbreeding 
between natural and hatchery fish could reduce the genetic diversity of 
natural-origin OP steelhead. NMFS also stated that there was a great 
deal of uncertainty about the overall health of the ESU because little 
information exists about the summer-run steelhead stocks, including run 
size trends in the Olympic Peninsula and the amount of interaction 
between hatchery and natural stocks. Informed by the status review 
(Busby et al., 1996), NMFS concluded that the OP steelhead ESU did not 
warrant listing under the ESA (61 FR 41541, August 9, 1996).

Updated Status Review

    To ensure that our review was based on the best available and most 
recent scientific information, we solicited information during a 60-day 
public comment period regarding the DPS structure and extinction risk 
of, and efforts being made to protect, OP steelhead (88 FR 8774, 
February 10, 2023). We also convened a status review team (SRT) to 
review the best available scientific and commercial information 
regarding the DPS structure and extinction risk of steelhead in the 
areas previously identified as the range of OP steelhead and consistent 
with the scope of the listing petition. Specifically, the SRT addressed 
(1) if the population fits the definition of a DPS and whether the 
geographic boundaries previously identified in the past NMFS review 
(Busby et al., 1996) warrant re-delineation or refinement, (2) the 
relation of hatchery programs propagating steelhead to the defined DPS, 
(3) current threats faced by the DPS, and (4) the level of extinction 
risk of the DPS throughout all or a significant portion of its range. 
The status review presents the SRT's professional judgment of the 
extinction risk facing OP steelhead but makes no recommendation as to 
the listing status of the species. The status review (OP Steelhead SRT 
2024) is available electronically (see ADDRESSES).
    The status review was subject to independent peer review pursuant 
to the Office of Management and Budget Final Information Quality 
Bulletin for Peer Review (M-05-03; December 16, 2004). The status 
review was peer-reviewed by two independent scientists selected from 
the academic and scientific community with expertise in salmonid 
biology, conservation, and management, and specific knowledge of 
steelhead. Guidance suggests three reviewers (59 FR 34270; July 1, 
1994), and we contacted multiple other experts in the field, but all 
were not available. The peer reviewers were asked to evaluate the 
adequacy, appropriateness, and application of data used in the status 
review, as well as the findings made in the ``Risk Assessment'' section 
of the report. Peer reviewer comments were addressed prior to 
finalizing the status review.
    We subsequently reviewed the status review, its cited references, 
and peer review comments, and concluded that the status review upon 
which this determination is based, with additions from more recent 
publications and updated data (including a recent report completed by 
Tribal and State co-managers), provides the best available scientific 
and commercial information on OP steelhead. Much of the information 
discussed below on the DPS configuration, demographics, threats, and 
extinction risk is attributable to the status review (OP Steelhead SRT 
2024). We have applied the statutory provisions of the ESA, including 
evaluation of the factors set forth in section 4(a)(1)(A)-(E), our 
regulations regarding listing determinations, and relevant policies 
identified herein in making the listing determination. In the sections 
below, we provide information from the report (supplemented with 
updates since the publication of the status review) regarding threats 
to and the status of OP steelhead.

Review of `Species' Delineation

    Steelhead in the Olympic Peninsula exhibit two distinct anadromous 
life history strategies: summer-run (stream maturing) and winter-run 
migrations, in addition to estuarine and freshwater resident life 
histories (Kendall et al., 2015). We relied upon the Salmon and 
Steelhead Stock Inventory (Washington Department of Fisheries et al., 
1993), Busby et al. (1996), and information from State and Tribal co-
managers (COPSWG 2023) to provide a provisional list of winter-run and 
summer-run populations for analysis. The SRT identified 11 summer-run 
populations and 30 winter-run steelhead populations in the previously 
defined range of OP steelhead (see table 2 in OP Steelhead SRT 2024). 
Winter-run steelhead are found throughout the OP in smaller independent 
streams that drain directly into the Strait of Juan de Fuca and in 
larger rivers and their tributaries that drain into the Pacific Ocean 
(including Queets, Hoh, Quinault, and Quillayute). In the

[[Page 1452]]

Olympic Peninsula, winter-run steelhead predominate. Summer-run 
steelhead are currently reported for portions of the largest four river 
systems draining into the Pacific Ocean: Quinault (East Fork, North 
Fork, and main stem), Queets (mainstem, Clearwater), Hoh (South Fork 
Hoh), and Quillayute (Bogachiel, Sol Duc, Sitkum, and Calawah) (Cram et 
al., 2018). Summer-run steelhead are not currently reported for rivers 
along the Strait of Juan de Fuca. Historically there was a population 
reported in the Lyre River (McHenry et al., 1996; Goin 2009).
    The SRT concluded that the best available scientific information 
did not warrant a reconsideration of the previously described 
geographic boundaries for OP steelhead. Busby et al. (1996) defined OP 
steelhead to include watersheds to the west of the Elwha River and 
north of Grays Harbor. The data contributing to the findings evaluating 
the genetic diversity in O. mykiss in Busby et al. (1996) were from a 
combination of studies that used genetic variation to delineate 
patterns of diversity and differentiation among O. mykiss from 
California to British Columbia, including both inland and coastal 
collections. A number of studies have been published since that time 
(Phelps et al., 1997; Kassler et al., 2010, 2011), and by request from 
the SRT, WDFW and the Northwest Indian Fisheries Commission (NWIFC) 
embarked on an updated analysis of all genetic data that have been 
collected to date on O. mykiss in the range of OP steelhead (Seamons 
and Spidle 2023). Samples analyzed by Seamons and Spidle (2023) ranged 
from collections taken from 1994 through 2021 and included both 
hatchery and natural-origin steelhead, and many collections that had 
been previously analyzed (Kassler et al., 2010, 2011; Phelps et al., 
1997). Though the major coastal streams in the range of OP steelhead 
are represented in the data, many of the collections used for analyses 
are decades old, and some of the smaller streams located on the coast 
and in the Strait of Juan de Fuca, as well as most of the summer-run 
steelhead-occupied streams, are not represented.
    Seamons and Spidle (2023) evaluated the genetic relationships 
between O. mykiss populations on the Olympic Peninsula and surrounding 
regions. Generally, the natural-origin OP steelhead genetic collections 
from streams sampled show very little genetic differentiation from one 
another. The major coastal streams along the Pacific coast, which have 
the best coverage of samples, particularly show little to no 
significant genetic differentiation. This finding supports the idea 
that there is a genetic exchange between populations on the coast and 
is consistent with results from other studies (Kassler et al., 2010 and 
2011; Phelps et al., 1997; Reisenbechler and Phelps 1985). Based on 
genetic data, the southern boundary of OP steelhead, north of Grays 
Harbor (previously defined by Busby et al., 1996), is supported by 
genetic differentiation from populations in southwest Washington. Very 
few samples from within the range of OP steelhead have been collected 
from the small streams draining into the Strait of Juan de Fuca; only 
the Pysht and Lyre River collections from the 1990s have been used for 
genetic analyses. Though there is clear genetic differentiation between 
OP steelhead and the Puget Sound steelhead DPS overall, more recent 
collections would be needed to get a definitive understanding of the 
genetic differentiation among steelhead populations on the Olympic 
Peninsula and, in particular, the genetic differentiation in the Strait 
of Juan de Fuca between the streams to the west of the Elwha River and 
the Elwha River and east (in the Puget Sound DPS). Therefore, we have 
no new genetic information that would indicate that the current 
boundaries for OP steelhead should be modified from those determined by 
Busby et al. (1996). A resident population of O. mykiss exists in Lake 
Crescent, isolated by a series of impassable cascades, and is notably 
genetically different from all other O. mykiss sampled. This endemic 
local form of resident rainbow trout, known as the Beardslee trout (see 
Brenkman et al., 2014 for a review), was not considered by the SRT as 
part of the OP steelhead populations.
    Findings from the SRT (OP Steelhead SRT 2024) and from Busby et al. 
(1996) directly inform our species delineation under the joint DPS 
Policy. First, Busby et al. (1996) found that the OP is characterized 
by habitat, climatic, and zoogeographical differences between it and 
the adjacent regions of western Washington and that genetic data 
collected supported the hypothesis that, as a group, steelhead 
populations from the OP are substantially isolated from populations in 
other regions. More recent genetic information reviewed by the SRT (OP 
Steelhead SRT 2024) continues to indicate that OP steelhead are 
isolated from other regions (as discussed above). These observations 
regarding separation/isolation similarly satisfy the discreteness 
criterion under the joint DPS Policy, as OP steelhead are markedly 
separated from other such populations of O. mykiss due to physical and 
ecological factors.
    Similar factors also satisfy the significance criterion of the DPS 
Policy. As stated above, Busby et al. (1996) described the unique 
ecological region occupied by OP steelhead, including that the Olympic 
Peninsula receives more precipitation than any other area in the range 
of west coast steelhead. Occupation of a unique ecological region 
satisfies a DPS criterion for significance. Loss of steelhead from the 
OP region would also represent a significant gap in the range of the 
species. Finally, as discussed above, OP steelhead are genetically 
distinct from the steelhead found in neighboring regions in Southwest 
Washington and the Puget Sound. Therefore, the loss of OP steelhead 
would be a significant loss to the genetic diversity of the taxon.
    Based on the SRT's findings on new genetic information summarized 
above, the previous considerations of OP steelhead as an ESU, and our 
considerations under the joint DPS Policy, we conclude that OP 
steelhead meet the significance and discreteness criteria and warrant 
delineation as a DPS. Consistent with previous findings under the ESU 
policy, the geographic boundaries of the OP steelhead DPS continue to 
include winter- and summer-run steelhead runs occupying river basins of 
the Olympic Peninsula, Washington, west of the Elwha River (excluded) 
and south to Grays Harbor (excluded) on the Washington coast.

DPS Membership of Resident O. mykiss

    The SRT concluded that the contribution of resident (non-migratory) 
O. mykiss to the productivity and genetic diversity in anadromous O. 
mykiss is currently unknown for OP steelhead, and there is no existing 
information on the genetic diversity and differentiation of resident 
versus migratory O. mykiss in OP steelhead range. Studies of O. mykiss 
in the southern portion of the species' range have identified a major 
genome region associated with migration and residency in O. mykiss 
(Nichols et al., 2008; Hale et al., 2014; Pearse et al., 2019), but 
later research on O. mykiss in the Elwha River contradicted these 
earlier studies, finding no association between genetic variation at 
this region and migration or residency (Fraik et al., 2021). Diversity 
in this region of the genome has not been examined in OP steelhead. The 
association of this part of the genome with migration and residency is 
not consistent across the range northward and inland, where the 
resident DNA variant for this genome region increases in frequency in 
both anadromous

[[Page 1453]]

(migratory) and resident O. mykiss (Pearse et al., 2019; Weinstein et 
al., 2019). However, there is additional evidence for genetic 
differences between resident and anadromous O. mykiss related to smolt 
transformation (Nichols et al., 2008), metabolism (Sloat and Reeves 
2014), and growth (Kelson et al., 2020), and further evidence for 
genetic divergence between the two life history forms (Narum et al., 
2004).
    Resident and anadromous forms can interbreed, but the extent to 
which this occurs in the Olympic Peninsula is unknown. It has been 
demonstrated that below long-standing barriers, resident fish can 
contribute to the anadromous population, and the resident form can be 
derived from the anadromous form (Zimmerman and Reeves 2000; Pascual et 
al., 2011; Thrower et al., 2004, Kendall et al., 2015). Resident fish 
are known to be present in the watersheds of the Olympic Peninsula, but 
there have been limited efforts to quantify their abundance and 
demographic relationship with the anadromous form across the OP region. 
Notably, the DPS Policy says, ``the standard adopted [for discreteness] 
does not require absolute separation of a DPS from other members of its 
species, because this can rarely be demonstrated in nature for any 
population of organisms. . . . [T]he standard adopted allows for some 
limited interchange among population segments considered to be 
discrete, so that loss of an interstitial population could well have 
consequences for gene flow and demographic stability of a species as a 
whole'' (61 FR 4722, 4724; February 7, 1996).
    Physical, physiological, ecological, and behavioral differences 
between resident and anadromous life forms continue to be apparent, as 
similarly detailed in previous steelhead listings. The 2006 listing of 
multiple steelhead DPSs (71 FR 834; January 5, 2006) detailed 
fundamental biological differences between resident and anadromous 
forms of steelhead, including differences in prey, predators, size 
(anadromous are larger), fecundity (anadromous produce more eggs), 
smoltification process, and migratory strategy. A primary difference 
between the two life forms is that the resident fish complete their 
life cycle solely in freshwater while the anadromous fish migrate to 
the ocean. Additionally, work in a limited number of rivers in the 
Olympic Peninsula found that the two life history forms varied in their 
arrival timing in spawning reaches, with anadromous males primarily 
entering in late winter/early spring and resident males in late spring/
early summer (McMillan et al., 2007). Resident males were more common 
than anadromous males in upper reaches (though both overlapped in time 
and space with anadromous females), and the two life forms showed 
differences in mating behavior tactics. Also, the genetic differences 
related to growth and metabolism result in physical and physiological 
differences (larger size at a younger age in resident fish, higher 
metabolic costs in anadromous fish; see review by Kendall et al., 
2015).
    Based on the best available information, the SRT found, and we 
agree, that the resident and anadromous forms are markedly separate in 
physical, physiological, and ecological factors. There is some evidence 
of genetic differences between anadromous and resident populations, 
though this has not been studied specifically in the range of OP 
steelhead. Additionally, though there can be physical overlap between 
the two forms, and interbreeding and gene flow can occur, discreteness 
under the DPS Policy does not require no overlap whatsoever. Therefore, 
under the DPS Policy, the resident form is discrete from the anadromous 
form and is not part of the OP steelhead DPS.

DPS Membership of Hatchery-Origin Steelhead

    On July 28, 2005, NMFS released a policy on the inclusion of 
hatchery-origin fish in the ESA listing determinations for Pacific 
salmon and steelhead ESUs [or DPS in the case of steelhead but not 
specified] (70 FR 37204). This policy states that ``[i]n delineating an 
ESU [or DPS] to be considered for listing, NMFS will identify all 
components of the ESU, including populations of natural fish (natural 
populations) and hatchery stocks that are part of the ESU. Hatchery 
stocks with a level of genetic divergence relative to the local natural 
population(s) that is no more than what occurs within the ESU: (a) are 
considered part of the ESU; (b) will be considered in determining 
whether an ESU should be listed under the ESA; and (c) will be included 
in any listing of the ESU.''
    The SRT summarized what is currently known about the genetic 
distinction between natural-origin and hatchery-origin steelhead in the 
Olympic Peninsula. Few studies have been undertaken to specifically 
evaluate the influence of hatchery stocks on natural-origin steelhead 
in the Olympic Peninsula. Kassler et al. (2010, 2011) used DNA 
sequences in an evaluation of the genetic diversity among natural- and 
hatchery-origin steelhead from coastal collections of OP steelhead, 
including the Hoh, South Fork Hoh, Sol Duc, Calawah, and Bogachiel 
Rivers, as well as hatchery-origin steelhead from four Olympic 
Peninsula hatcheries. For the most part, Kassler et al. (2010, 2011) 
failed to find significant introgression (transfer of genetic material 
from one population to another) of hatchery steelhead with natural-
origin OP steelhead, except in the 2008 South Fork Hoh River winter 
collection, which shows evidence of interbreeding with the Cook Creek 
hatchery collection. This same finding was reported by Seamons and 
Spidle (2023) in a reanalysis of the samples with newer data (but note 
some of these data are outdated and not comprehensive for the entire 
DPS). Furthermore, samples were taken from sites with minimal hatchery 
influence to be more representative of natural populations. In the 2009 
and 2010 Hoh River winter collections, these steelhead were more 
similar to other OP natural-origin steelhead collections (see Seamons 
and Spidle 2023). Also, DNA analyses (Kassler et al., 2010, 2011; 
Seamons et al., 2017) showed presumed natural-origin population samples 
with mixed ancestry (that includes genetic information from non-native 
early-winter and early-summer run steelhead) however, natural-origin 
fish were still overall genetically distinct from hatchery broodstock.
    Seamons and Spidle (2023), in their more recent genetic analysis, 
included three hatchery stocks that currently propagate and release 
juvenile steelhead in Olympic Peninsula streams: Chambers Creek early 
winter steelhead (Puget Sound origin), Skamania early hatchery summer 
steelhead (Lower Columbia River origin), and Cook Creek early winter 
steelhead (putatively Olympic Peninsula origin). The majority (9 of 11) 
of hatcheries are operated as segregated programs, so they should 
retain their own genetic identity. While the early winter Chamber Creek 
Hatchery and early summer Skamania Hatchery stocks are derived from 
out-of-DPS sources and are therefore genetically distinct and not 
considered part of the DPS, the origin of the Cook Creek/Quinault 
National Fish Hatchery stock is unclear. There are limited data on if 
Cook Creek stock is similar to natural stocks. Furthermore, although 
current sampling for genetic analysis provides limited coverage of the 
DPS, there is some indication that hatchery stocks in the Queets and 
Quinault Rivers are not representative of the natural populations in 
those watersheds (HSRG 2004; Kassler et al., 2012; Seamons et al., 
2017). For the two integrated programs (Quinault Lake and

[[Page 1454]]

Salmon River), the broodstocks were founded by Quinault Lake winter-run 
steelhead, but with uncertainty about origin (see OP Steelhead SRT 
2024; Marston and Huff 2022). In Seamons and Spidle (2023), none of the 
hatchery stock samples grouped with samples taken from presumptive 
natural-origin OP steelhead in a cluster analysis (statistical analysis 
where samples are grouped based on genetic similarity). This analysis 
also showed some evidence of hatchery influence on the natural-origin 
steelhead in OP streams in historical collections. Individuals 
collected from the Lyre and Pysht Rivers (in 1995 and 1994, 
respectively) in the Strait of Juan de Fuca are similar to Chambers 
Creek hatchery winter steelhead, and individuals collected from the Hoh 
River in 2008 appear to have been influenced by Skamania summer 
steelhead hatchery individuals (Seamons and Spidle 2023). Newer 
collections would be needed to assess the influence of past and extant 
hatchery releases on the genetic diversity and provenance of natural-
origin O. mykiss, particularly since the termination of or modification 
of hatchery programs and releases that occurred relatively recently. 
Finally, out-of-DPS hatchery stocks were possibly selected by local 
resource managers because of differences in the run and spawn timing 
between the hatchery broodstocks and the native populations; therefore, 
the hatchery-origin steelhead exhibit a unique life history compared to 
the natural-origin steelhead.
    Based on the SRT's conclusions, we conclude that where genetic 
information is available, hatchery steelhead stocks are genetically 
distinct from co-occurring natural-origin steelhead populations, 
indicating a level of genetic divergence relative to local natural 
populations greater than what occurs within the OP steelhead DPS. The 
SRT also found that the best available information suggests the 
hatchery stocks were founded with out-of-DPS stocks and/or out-of-DPS 
stocks were incorporated later, and, therefore, we conclude that the 
hatchery stocks are not included as part of the DPS.

Determination of ``Species''

    Based on the best available information, we find that natural-
origin steelhead (anadromous life history) occupying river basins of 
the Olympic Peninsula, Washington, west of the Elwha River (excluded) 
and south to Grays Harbor (excluded) on the Washington coast, are a DPS 
and constitute a species under the ESA. Furthermore, we find that none 
of the steelhead hatchery stocks within the geographic range of OP 
steelhead meets the criteria to be considered part of the OP steelhead 
DPS.

Assessment of Extinction Risk

    The SRT synthesized the best scientific and commercial data 
available regarding the DPS's status, which includes its life history, 
demographic trends, and susceptibility to threats, and evaluated the 
extinction risk of the DPS. The SRT included in its assessment an 
evaluation of the likely effects of hatchery-origin fish on the 
viability of the DPS. Additionally, the SRT assessed demographic 
components and threats that contribute to the uncertainty of the status 
of OP steelhead. Here we summarize information of status and threats, 
identifying uncertainties throughout. Following publication of the 
Status Review report (OP Steelhead SRT 2024), the Tribal and State co-
managers provided a review of the SRT report, highlighting additional 
uncertainties in the status and threats related to OP steelhead.

Demographic Risk Analysis

    The SRT identified 11 summer-run populations and 30 winter-run 
populations in the DPS (see table 2 in OP Steelhead SRT 2024). 
Steelhead on the Olympic Peninsula are most abundant in the major 
Pacific coastal basins of the Quinault, Quillayute, Queets, and Hoh 
Rivers (collectively, the ``four major basins''), and less abundant in 
rivers along the Strait of Juan de Fuca. Winter-run steelhead, 
presently and historically, are more abundant in the smaller drainages 
and are distributed more ubiquitously throughout the Olympic Peninsula 
than summer-run steelhead (Houston and Contour 1983; Scott and Gill 
2008; Cram et al., 2018).
    The SRT, utilizing data previously provided by Washington State and 
Tribal co-managers (collectively, ``co-managers''), estimated that 
total run size (abundance) for winter-run in the four major basins has 
decreased by 42 percent, from 32,556 (1991-1995) to 18,821 (2018-2022). 
Using combined escapement estimates as additional information on 
abundance, escapement in the four major basins has decreased by 16 
percent from 18,597 (1991-1995) (Busby et al., 1996) to a current level 
of 15,653 (2018-2022). Adequate escapement data (i.e., more than a few 
years of dispersed data) were not available to complete trend analysis 
for all winter-run populations. Of the 14 populations for which 
adequate escapement data were available for trend analysis (of 30 total 
winter-run populations), 1 had a stable trend and 13 were negative (10 
significantly negatively different from 0). Analysis of the four major 
basins by WDFW indicated that total run size had nearly halved in size 
from the late 1970s and 1980s to 2022, while the trend in escapements 
was slightly declining or stable (Harbison et al., 2022). Notably, 
adequate information was not available for 16 of 30 winter-run 
populations.
    The most recent 15-year spawner abundance trend estimates (2008-
2022) indicate that 5 of the 15 populations that we have 15-year trend 
estimates for across the entire range had negative trends, mainly for 
the larger rivers that account for the largest proportion of the DPS. 
Of those negative trends, 4 were significantly different from 0, 
including the larger Queets River and Bogachiel River (part of the 
Quillayute River system) winter-run populations. Positive recent 15-
year trends were observed in 8 of the 15 populations. The positive 
trends in two of the populations were significant, specifically the 
trends for the smaller Pysht River and East Twin River winter-run 
populations along the Strait of Juan de Fuca. Under dramatically 
reduced harvest conditions experienced in the last 3 years for winter-
run populations in the four major basins, total run size appears to 
have stabilized or increased slightly. Though recent years may exhibit 
some stabilization in the 15-year spawner abundance estimates, the 
long-term trends still suggest long-term decline.
    Factors related to how these abundances are estimated lead to 
biases and uncertainty in the estimates. Escapement abundance was 
estimated using redd (salmon nests) counts from after March 15 only, 
assuming that redds after March 15 are produced by natural-origin, not 
hatchery-origin, fish. However, steelhead spawn prior to March 15, and 
evidence suggests that both natural-origin (unmarked) and hatchery-
origin steelhead contribute to this pre-cutoff date production (Marston 
and Huff 2022). Overall, from an abundance perspective, current 
estimates of escapement may underestimate natural production, and early 
natural-origin spawners may represent an additional 10 percent increase 
in overall abundance (Marston and Huff 2022). The relative contribution 
of hatchery-origin versus natural-origin spawners prior to March 15 
varies with changes in harvest effort and timing and the intensity, 
location, and timing of hatchery releases, creating variable bias in 
abundance estimates depending on the year and/or river basin. Further, 
there is uncertainty in

[[Page 1455]]

the use of redd counts to derive spawner abundances, specifically 
regarding assumptions of redd-to-adult ratios and the accuracy of redd 
observations, which can bias estimates either high or low (see 
Gallagher et al., 2007, 2010; Dauphin et al., 2010; Murdoch et al., 
2018). The WDFW coastal steelhead proviso plan (Harbison et al., 2022) 
also points out other information about redd spawning surveys that 
could over- or under-estimate spawner abundances.
    There was less data available for summer-run steelhead in the OP 
steelhead DPS. Information was limited to past and present harvests 
(based on run timing, we assumed that steelhead caught between April 
and October were summer-run steelhead) and intermittent snorkel surveys 
carried out in the last two decades. It is possible that some of the 
fish caught in the spring are winter-run kelts (repeat spawners). 
Likewise, fish caught in October could be very early returning winter-
run fish. Summer-run steelhead are currently present in the Quillayute 
(Sol Duc, Calawah, and Bogachiel Rivers), Hoh, Queets, and Quinault 
Rivers. Based on historical summer-run harvest data, it appears that, 
prior to the releases of hatchery-origin summer-run fish, many of the 
rivers supported runs of several hundred natural-origin summer-run 
fish. Further, it is unclear if a remnant summer-run population still 
exists in the Lyre River (McHenry et al., 1996; Goin 2009).
    Based on snorkel surveys, recent summer-run steelhead abundances in 
individual rivers likely range from less than a hundred to a few 
hundred adults, though potentially into the thousands for Sol Duc River 
and Quinault River, with considerable uncertainty in these estimates. 
Based on riverscape surveys, the average estimated abundance across 
rivers was 66 breeding fish per year, or roughly a breeding population 
size of approximately 260 per river, assuming a 4-year generation time. 
The co-managers also developed abundance estimates for summer steelhead 
populations in the Hoh, Quillayute, and Quinault River systems and 
estimated summer-run median abundance at 90 to over 550 individuals per 
river but with ranges extending from low hundreds to approximately 
1,350 depending on the river (Co-Manager OP Steelhead Working Group 
[COPSWG] 2023; and see table 8 in the status review). Therefore, there 
is substantial uncertainty in the current abundances of summer-run 
populations, but they are likely at low abundance.
    Few measures of productivity are available for natural populations. 
Modeling conducted by the SRT indicates that in most years fishing 
mortality in the four major basins was greater than the intrinsic 
growth rate (natural population growth based on births minus natural 
deaths), which will result in declining populations. Only a small 
minority of years in each population were judged to have population 
growth greater than zero. Estimates of population growth rate for the 
smaller populations along the Strait also indicate that, on average, 
past harvest was depressing growth rates. However, the effect of past 
harvest was more subtle than in the four major basins on the coast; 
these Strait populations have not rebounded in the 10 or so years since 
harvest was terminated. The four major basins (Queets, Hoh, Quinault, 
and Quillayute), which contain the majority of the DPS abundance, 
exhibited diminished productivity as indicated by below-replacement 
population growth rates in most years and declining short- and long-
term trends in natural-origin escapement and total run size.
    Smolt survival (both natural and hatchery) has decreased since the 
1980s (Harbison et al., 2022). Certain analyses point to correlations 
with oceanographic processes and other environmental factors (COPSWG 
2023; Ohlberger et al., 2025), but those correlations were studied only 
in the four major basins within the DPS range. Similarly, the survival 
of kelts in the four major basins has declined by nearly half since the 
1980s, with some evidence pointing to similar factors as with the smolt 
declines (COPSWG 2023).
    OP steelhead currently occupy nearly their entire historical range 
because they lie in a region of the west coast that is not impacted by 
dams or other major artificial passage blockages, though there are 
multiple smaller culverts and barriers. State, county, and forest road 
stream crossings may block or impair passage at culverts, which may 
reduce spatial structure. However, in general, road culverts block 
tributary access to relatively small areas of spawning and rearing 
habitats, and collectively they do not appear to be a major limitation 
on habitat. Impassable culverts on state roads are required to be 
upgraded under the 2013 U.S. District Court Injunction (U.S. v. WA 
Culvert Case), whereas forestry road culverts are covered under the 
Road Maintenance and Abandonment Plan (RMAP). Considerable progress has 
been made in replacing culverts in the past decade, especially under 
the RMAP process where over 80 percent of culverts are now fish-
passable. Still, some additional culverts exist that are not included 
within the RMAP (NWIFC 2020). Consequently, the SRT generally viewed 
current population connectivity as good; i.e., no barriers that prevent 
access to significant juvenile rearing or adult spawning habitat.
    The potential exists for future restrictions in spatial structure 
with present and future environmental variability due to low summer 
flows that may limit passage to headwater areas. Future projections for 
flow and temperature into the foreseeable future suggest that low-flow 
or high water-temperature barriers may develop and create temporal 
passage blockages, which would disproportionately affect spatial extent 
for summer-run steelhead. Changes in summer flows, with some reaches 
going dry, directly affect summer-run steelhead in their ability to 
reach their headwater spawning reaches. The upstream spatial extent of 
the DPS is influenced by the presence of summer-run populations in the 
larger river systems. Generally, but not necessarily, summer-run 
steelhead return-timing is coordinated with river flow patterns and 
temporal flow windows that allow access to headwater spawning areas; 
thus, summer-run steelhead access some spawning and rearing habitat 
that is unavailable to winter-run steelhead. However, over 99.3 percent 
of summer-run habitat is also winter-run habitat. In other words, of 
the habitat utilized by summer-run, only about 0.7 percent is summer-
run only. Given the generally good connectivity and lack of 
anthropogenic barriers overall, as well as that summer-run spatial 
extent largely overlaps with winter-run, the SRT concluded the risk to 
the viability of OP steelhead from reduced spatial structure ranges 
from very low to low.
    Available historical harvest information reviewed by the SRT 
indicated that the winter-run steelhead return timing was historically 
earlier than is currently expressed. McLachlan (1994) found a 
contraction in run timing in the Quillayute River, with a decrease in 
the proportion of the run return before January 1 from 35 percent of 
the run to 20 percent of the run. McMillan et al. (2022) estimated that 
peak run-timing has shifted 1 to 2 months later for winter-run 
steelhead in the Hoh and Quillayute, and run timing is up to 26 days 
shorter for some populations. Large numbers of winter-run steelhead 
were harvested from November to January (in some years fish were 
harvested in October, although these numbers may include summer-run 
steelhead) prior to and following the initiation of hatchery programs 
in the range of the OP steelhead DPS. With the beginning of hatchery 
programs in the DPS utilizing

[[Page 1456]]

early-returning winter-run steelhead (i.e., Chambers Creek Hatchery 
Stock from south Puget Sound), there was a directed harvest of the 
early-returning portion of the run targeting hatchery fish. As a 
consequence of this continued harvest, it is likely that a proportion 
of the early-returning (November-January) natural-origin winter-run 
steelhead were and continue to be harvested, even if incidentally (OP 
Steelhead SRT 2024).
    Hatcheries in the region utilize out-of-DPS stocks, and there is 
concern about the potential impacts on natural-origin steelhead genetic 
diversity from the use of out-of-DPS broodstock in most hatcheries 
(namely, Chambers Creek and Skamania origin). Though the use of out-of-
DPS stocks prevents natural-origin runs from being taken for 
broodstock, there can be negative impacts if non-native hatchery 
steelhead interbreed with natural-origin steelhead. Non-native 
broodstocks are presumed to be more adapted to the ecology of their 
watershed of origin and, therefore, express life history traits that 
are not necessarily adapted to the watershed to which they are 
transferred. If non-native hatchery-origin steelhead are present on 
native spawning grounds, maladaptive genotypes (because the out-of-DPS 
stocks are not adapted to this environment) may be integrated into the 
naturally spawning native population through interbreeding with 
hatchery fish (known as introgression).
    Information on the amount of interbreeding between hatchery-origin 
and natural-origin steelhead is limited. Some genetic data show the 
likely influence of non-native stocks on natural-origin OP steelhead, 
but in the absence of systematic genetic sampling and spawner surveys, 
it was not possible for the SRT to quantitatively assess this risk. DNA 
analyses (Kassler et al., 2010, 2011; Seamons et al., 2017) show 
presumed Olympic Peninsula natural-origin population samples with mixed 
ancestry that includes genetics from non-native early-winter steelhead 
and early-summer steelhead, though natural-origin fish were still 
overall distinct from hatchery broodstock. Also, while early-winter run 
hatchery steelhead females may generally spawn earlier than the 
natural-origin females, there is a tendency for hatchery-origin males 
to remain on the spawning grounds for extended periods, increasing the 
likelihood of hybridizing with natural-origin female steelhead (though 
hatcheries select for different spawn timing compared to natural-origin 
to help reduce spawning overlap).
    There are limited releases of summer-run hatchery steelhead in the 
range of OP steelhead DPS and releases have been eliminated in many 
tributaries on the Strait. Even with limited releases, snorkel surveys 
for summer-run steelhead observed that natural-origin and hatchery-
origin fish often co-occurred within the same kilometer of river 
channel in the Hoh, Bogachiel, and Sol Duc Rivers. Natural populations 
along the Strait and Cape Flattery are at relatively low abundances 
and, although hatchery releases in many tributaries draining to the 
Strait were eliminated almost a decade ago, past and continuing 
releases are more likely to have a significant effect on abundance and 
genetic composition because of their small population size.
    There are circumstances that also help limit interactions and limit 
genetic impacts from hatchery-origin steelhead. There have been changes 
in hatchery operations to reduce off-station releases in order to 
increase the proportion of fish returning to the hatchery and decrease 
the number of hatchery-origin fish straying and spawning naturally 
(including eliminated off-station release in the Hoh River). Co-
managers have made changes to reduce negative effects; for example, 
releases of winter-run and summer-run fish have been eliminated from 
the Clallam River, Goodman Creek, Lyre River, Pysht River, and Sol Duc 
River (COPSWG 2023). Also, larger rivers draining to the Pacific Ocean 
have larger natural populations and greater spatial structure; thus, 
despite the large size of many of the corresponding hatchery programs, 
it is possible that there is somewhat limited interaction and 
introgression between the hatchery- and natural-origin populations. 
Resident O. mykiss, multiple spawner ages, and repeat spawners all 
contribute to bolstering the number of effective spawners and provide 
some buffering against inbreeding. Additionally, the relative nearness 
of the populations within the DPS to each other allows for the 
continued exchange of individuals between populations, and helps 
maintain genetic diversity.

Threats Assessment

    As described above, section 4(a)(1) of the ESA and NMFS' 
implementing regulations (50 CFR 424.11(c)) state that we must 
determine whether a species is endangered or threatened because of any 
one or a combination of the 4(a)(1) 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 (16 U.S.C. 1533(a)(1)). We evaluated 
whether and the extent to which each of the foregoing factors 
contributes to the overall extinction risk of the DPS, identifying 
uncertainties throughout.
    Related to listing factor (A), while cumulative impacts of land-use 
practices have been large over space and time, the four major basins 
still exhibit fundamental natural watershed processes and associated 
habitat characteristics. These include a large, forested floodplain, 
relative to other watersheds, which is still intact and functioning. 
The SRT noted moderate-to-good conditions in river and riparian 
habitat, large percentages of forest cover, and declines in timber 
harvest activity (see NWIFC 2020), especially those rivers with 
substantial portions being located within Olympic National Park (ONP) 
or headwaters in the ONP (mainly the four major basins). OP steelhead 
currently occupy nearly all of their historical range because they lie 
in a region of the West Coast that is not impacted by dams or other 
major in-stream artificial passage blockages. For steelhead watersheds 
outside the ONP the majority of land use is for timber harvest and 
despite recent habitat improvement efforts, the legacy of past 
industrial logging practices will continue to negatively affect 
steelhead productivity in a number of rivers for the foreseeable 
future. Still, several restoration programs to retire forest roads, 
repair culverts, and supplement woody debris, amongst other things, 
were also seen as having improved habitat. Generally, habitat in many 
of the rivers has improved since the review by Busby et al. (1996), 
although it was recognized that the natural recovery from past timber 
harvest events and stream ``clearing'' practices takes decades. Despite 
some legacy effects of forestry and land use practices, habitat quality 
and connectivity are generally good within the DPS due to declining 
timber harvest activity, especially within the ONP, and the absence of 
dams or other major artificial passage blockages in the region.
    For listing factor (B), utilization in the form of harvest of OP 
steelhead has declined within the last decade (particularly the last 
few years) and varies greatly by region (Strait vs. the four major 
basins). Annual harvest rates of OP steelhead in the four major basins 
have declined in most recent years (2021-2024). Estimates of harvest 
rate for the DPS and the four major basins average across population 
prior to 2014 were 25.6 percent and 36.5 percent, respectively (Cram et 
al., 2018). Based on data from the co-managers, between

[[Page 1457]]

2014 and 2020, rates averaged across years for each of the four major 
basins ranged from 21 percent to 41 percent. Most recently (2021-2024), 
based on data including co-manager provided data since publication of 
the status review, harvest rate estimates for the four major basins 
have ranged from 7 percent to 25 percent. While harvest rates have 
declined recently, as stated above, modeling by the SRT with data 
through 2022 indicates that in most past years fishing mortality in the 
four major basins was greater than intrinsic natural growth, resulting 
in continued declines in populations (a small minority of years had 
growth above zero) (OP Steelhead SRT 2024). Population estimates 
associated with the most recent harvest rates have yet to be determined 
since the progeny of those brood years have not yet fully returned to 
spawn. Increases in abundance in the last couple of years in certain 
basins are promising, and it will take several years to detect a 
response signal from such recent actions.
    For most rivers along the Strait, harvest was terminated in various 
years between 2005 and 2020 (see OP Steelhead SRT 2024). Population 
growth rate patterns considered by the SRT appear very similar among 
streams, including in streams where fishing continues. Therefore, it 
appears that other non-harvest factors (such as freshwater and/or ocean 
conditions) may also be influencing trends in Strait populations.
    Multiple factors lead to uncertainty in harvest rates, which leads 
to difficulty in determining the level of threat under factor (B). 
Rivers within the OP steelhead range with recreational fishing have 
been catch and release since 2016, and the state assumes a 10 percent 
hooking mortality for all state-wide steelhead sport fisheries. Certain 
commenters on the 90-day Petition finding questioned this estimate and 
believe the hooking mortality rate to be lower, citing research from 
river systems not in the Olympic Peninsula, and there are no known data 
to precisely calculate hooking mortality rates for rivers within the OP 
DPS range. For the harvest estimates presented above, a hooking 
mortality estimate is included for only the Hoh River sport fishery 
harvest rate; therefore, rates for other basins are likely higher if 
incorporating catch and release mortality. Additionally, evidence 
suggests a sport angler encounter rate of 1.14 for natural-origin 
steelhead, implying some steelhead are caught and released more than 
once (Bently 2017; Harbison et al., 2022). Estimates of the effect of 
multiple captures on hooking mortality are not available, but, 
presumably, multiple captures would increase hooking mortality. Winter-
run harvest rates include all steelhead caught between management week 
45 (approximately November 1) and week 18 (April) no matter the target 
fishery, but not any steelhead caught outside that time period (pers. 
comm. Jim Scott on behalf of co-managers, July 17, 2024), leading to 
additional uncertainty in harvest rates if any late returning fish are 
caught after week 18. Finally, harvest typically occurs from November 
to May, while escapement is calculated from counts of redds created 
after March 15 when it is assumed that all the fish present are 
natural-origin steelhead, resulting in a potential underestimate of run 
sizes and an overestimate of harvest rate. All in all, there are 
factors that both underestimate and overestimate harvest rates/
mortality.
    For summer-run steelhead, since 1992, catch-and-release regulations 
have been in place in state waters and the ONP. Fisheries data show 
low, limited harvest (and/or catch and release mortality) of summer-run 
steelhead in recent years (see OP Steelhead SRT 2024, including 
appendix B). It is difficult to interpret an impact of catch given the 
level of uncertainty associated with summer-run abundance, but 
available information suggests that the directed harvest of natural-
origin summer-run steelhead has declined since the 1996 status review. 
Contributing further to the uncertainty, data on indirect harvest of 
summer-run steelhead in fisheries targeting other Pacific salmon were 
not available for review.
    For listing factor (C), as detailed in the status review, most of 
all known disease cases are in hatchery fish populations, and little 
information exists on the impacts to natural-origin steelhead in the 
Olympic Peninsula as natural-origin steelhead are less commonly sampled 
(Breyta et al., 2013; data from Tony Capps, WDFW). To accurately assess 
the potential threat of disease in this population, we would need 
annual pathology reports from each hatchery to effectively assess the 
presence/prevalence of pathogens, viruses, and bacteria. Because most 
known disease outbreaks have been in hatchery-origin steelhead, most 
hatcheries are segregated from natural-origin, and hatchery fish are 
not part of the DPS, the status review team considered disease to be a 
very low-risk threat for natural-origin OP steelhead.
    Though the consumption of salmonids by predators, especially marine 
mammals, has increased, we have little information on the consumption 
of OP steelhead. Recent research suggests that predation pressure on 
salmon and steelhead from marine mammals has been increasing in the 
northeastern Pacific over the past few decades (Chasco et al., 2017 a, 
b; Couture et al., 2024; Rub et al., 2018), but this work mainly 
focused on predation on Chinook salmon (Couture et al. (2024) also 
discuss other salmonids but there is limited mention of steelhead). 
Also, predation from marine mammals likely is not a primary cause of 
the lack of salmonid population recovery in Washington state (WSAS 
2022). Studies have found that pinnipeds can have a significant 
predation impact on outmigrating juvenile steelhead in Puget Sound 
(Moore et al., 2021, 2024; Moore and Berejikian 2022), winter adult 
steelhead at the Ballard Locks in Lake Washington (NMFS 1995), and 
other adult salmonids (see Rub et al., 2018). Scordino et al. (2022) 
found consumption of multiple sizes of steelhead in coastal Washington 
by Steller and California sea lions based on scat samples (though most 
consumption was on Coho salmon [O. kisutch]). Seabirds are present in 
the Olympic Peninsula watersheds and consume juvenile salmonids, but we 
are unaware of any unusual or excessive predation events by seabirds or 
hotspots of seabird predation (based on pers. Comm. with Thomas Good, 
15 October 2023, NMFS NWFSC). Invasions of non-native fish species pose 
threats to native fish fauna, but little is known about the extent or 
effects on OP steelhead.
    Anthropogenic habitat alterations, including dams, irrigation 
diversions, fish ladders, and human-created islands, have the potential 
to create sites that may increase predation opportunities on adult and 
juvenile salmonids (Antolos et al., 2005; Evans et al., 2012; Hostetter 
et al., 2012; Moore & Berejikian 2022; Collins et al., 1976). However, 
there are no large dams or barriers in the OP steelhead range. While 
increases in predation associated with increases in pinniped 
populations along the West Coast are possible, we have no specific 
information to indicate that predation has increased for OP steelhead 
and no quantitative information on predation over time. Also, less is 
known about predation of steelhead in the marine environment. Tribal 
managers in the area have voiced concern about pinniped predation on 
these populations, but we lack quantitative data about the level of 
threat or if predation is a factor limiting the viability of OP 
steelhead specifically.

[[Page 1458]]

Therefore, the SRT concluded that predation was a low risk.
    Related to listing factor (D), various Federal and State protection 
measures exist across the Olympic Peninsula and the state of Washington 
to protect forests and salmonid habitat. Many provide protection to the 
species and its habitat. These include the Northwest Forest Plan (NWFP) 
and the associated Aquatic Conservation Strategy, the General 
Management Plan for the ONP, the Washington Forest Practices Act, the 
Washington State Forest Practices Rules, the DNR Habitat Conservation 
Plan, and state legislation to remove fish passage barriers. 
Additionally, multiple rivers and streams where OP steelhead occur have 
been designated as bull trout (Salvelinus confluentus) critical habitat 
(75 FR 63875-63978, October 18, 2010) and other ESA-listed species like 
Lake Ozette sockeye salmon (Oncorhynchus nerka), marbled murrelet 
(Brachyramphus marmoratus), and Northern spotted owl (Strix 
occidentalis caurina) occur on the peninsula. NMFS and USFWS have 
conducted biological opinions under section 7 of ESA for Federal 
actions in this region, including for the forest management activities 
in the Olympic National Forest, that lead to the prevention of 
activities that may jeopardize listed species and/or adversely modify 
their critical habitat. However, it is difficult to assess if these 
actions are adequate to conserve OP steelhead. Progress towards habitat 
protection is hard to measure since any ongoing efforts related to 
habitat restoration may take decades (if not longer) to show an effect. 
There is a spectrum of regulatory mechanisms protecting and restoring 
habitat, and the degree of protection depends on the entity with 
regulatory authority and the specific land activities in each area.
    Regulations related to harvest and hatcheries within Washington 
State also affect OP steelhead. OP steelhead fisheries are collectively 
managed by WDFW (State waters outside of the ONP) and Treaty Tribes (in 
their usual and accustomed fishing areas) and also by the ONP (in the 
park). The Treaty Tribes regulate commercial and subsistence fisheries 
and on-reservation sport and tribal-guided fisheries. Martin (2023) 
notes that sustainable harvest management is a core principle of 
traditional resource management and is embedded into the tribes' 
societal roles. Salmon and steelhead have been managed since time 
immemorial during a time when steelhead thrived (including their 
habitat), and this management included both traditional hatchery 
practices and harvest practices. Strategies have been implemented since 
the 1990s to support sustainable fishing including: prohibiting 
retention of natural-origin winter-run steelhead for recreational 
fisheries in state waters (since 2016, recreational fishing on certain 
tribal lands allows for retention of natural-origin), harvest 
restrictions (such as bag limits), shorter seasons, and gear 
restrictions (limits on hooks, prohibiting bait, prohibiting fishing 
from boats in certain rivers) in the face of declining natural-origin 
steelhead populations (Harbison et al., 2022). In recent years, 
recreational fisheries have been closed inside and outside of the ONP 
for certain rivers due to low returns. As noted above, reductions in 
harvest rates, with large reductions in tribal harvest rates, have 
occurred in recent years (2021, 2022, and 2023-2024 season). For most 
rivers along the Strait, steelhead-directed harvest has been prohibited 
since between 2005 and 2020 (depending on the river).
    The state of Washington has proposed, but not yet implemented, the 
2022 WDFW Coastal Steelhead Proviso Implementation Plan (``Proviso'') 
(Harbison et al., 2022) and has begun the process for updating state 
harvest regulations (<a href="https://wdfw.wa.gov/fishing/management/steelhead/coastal">https://wdfw.wa.gov/fishing/management/steelhead/coastal</a>). The Proviso outlines management strategies for the future of 
OP steelhead and other coastal steelhead populations. The Proviso Plan 
is based on existing state policies and does not represent a change in 
policy. It was developed as a response to recent declines in coastal 
steelhead and the need for adaptive management strategies to address 
these declines. There are additional plans by the State to update 
coastal steelhead management, though there are limited details on the 
plan at this time (<a href="https://wdfw.wa.gov/fishing/management/steelhead/coastal">https://wdfw.wa.gov/fishing/management/steelhead/coastal</a>). Finally, as noted throughout, the Tribal and State co-
managers actively monitor and have a policy of protectively managing 
the species. The co-managers have also committed to changes to hatchery 
and harvest regulations (see Co-manager Olympic Steelhead Working Group 
2025), most notably efforts to mark all hatchery fish, testing of 
natural-derived broodstock in the Quillayute, evaluation of the March 
15 management cut-off date, updating catch-and-release mortality, and 
expanding methods for abundance estimation. NMFS will continue to work 
with the co-managers to evaluate the effectiveness of the existing 
regulatory mechanisms and the future impact of these commitments on the 
species' status.
    WDFW operation of hatcheries is currently subject to the Statewide 
Steelhead Management Plan and the Anadromous Salmon and Steelhead 
Hatchery Policy C-3624 (2021), superseding the policy from 2009 
(Hatchery and Fishery Reform Policy C-3619). This policy provides 
general guidelines and notes that Hatchery Monitoring Plans (HMPs) will 
be developed for all state hatcheries. We did not find any evidence of 
completed HMPs at this point. This policy applies to state hatcheries 
and not to Federal or Tribal facilities. The C-3624 policy is not an 
enforceable regulation, but a guiding policy. However, the co-managers 
are currently working to develop hatchery management plans for hatchery 
facilities within the Olympic Peninsula (Harbison et al., 2022).
    Extensive hatchery programs have been implemented throughout the 
range of west coast steelhead. While some programs may have succeeded 
in providing harvest opportunities and increasing the total number of 
naturally spawning fish, the programs have also likely increased risks 
to natural populations, though this can depend on specific management 
and if measures are taken to reduce impacts to native runs. Hatchery 
operations, especially those utilizing non-native broodstocks, could 
introduce maladapted life history traits through interbreeding between 
natural-origin and hatchery-origin fish (introgression). We cannot 
currently quantitatively estimate the level of reproductive exchange 
between natural-origin and hatchery-origin steelhead in the Olympic 
Peninsula. Estimates of the proportion of hatchery-origin spawners 
(pHOS) and genetic data give some insight into the level of possible 
introgression but were only available for a limited proportion of the 
DPS, and many were not from recent years. Available information 
suggests some introgression, and the continued use of non-native 
broodstocks presents ecological and genetic risks, though this risk 
varies with the specifics of the particular hatchery program and 
natural population. There have been changes in hatchery operations to 
reduce straying. NMFS will continue to work with the co-managers to 
evaluate the impacts of hatchery operations and the effectiveness of 
efforts to reduce risks to OP steelhead.
    Finally, for listing factor (E) scientists predict the rising 
temperatures and associated ecosystem changes caused by environmental 
variation to impact Pacific salmon by a variety of mechanisms 
throughout their life cycle (Crozier et al., 2008, 2019, Isaak et al., 
2022, Crozier and Siegel 2023). These impacts are complex and vary 
among species, DPSs, and habitats. For U.S. West Coast salmon and 
steelhead,

[[Page 1459]]

expected changes to freshwater habitats include increased air and 
stream temperatures and changes in seasonal (but not necessarily annual 
mean) rainfall patterns, with larger and more extreme storms and 
droughts. These increased temperatures will result in more winter 
precipitation falling as rain than snow at intermediate elevations, 
which alters both seasonal streamflow and water temperatures.
    Many changes in temperature and stream flow have already been 
observed in the Olympic Peninsula watersheds (see OP Steelhead SRT 
2024). Additionally, multiple papers have already documented extensive 
glacier losses in the Olympic Mountains; between 1980 and 2015, 35 
glaciers and an additional 16 perennial snowfields disappeared from the 
Olympic Mountains (Fountain et al., 2022; Riedel et al., 2015; NWIFC 
2020). Increases in summer stream temperatures especially pose risks to 
steelhead due to extended freshwater rearing; i.e., juvenile steelhead 
that spend up to 2 or 3 years in freshwater (Halofsky et al., 2011; 
Climate Impacts Group 2009). Winter-run steelhead predominate in the 
Olympic Peninsula and are expected to be somewhat less susceptible to 
risks from changing stream temperatures than summer-run steelhead. Low 
summer stream flows can affect summer-run steelhead migration by 
dewatering stream reaches or limiting the accessibility of waterfalls 
or cascades (Halofsky et al., 2011). Future increases in flows at other 
times of year can displace juvenile fish and/or reduce the availability 
of suitable slow-water habitats for young fish. However, winter-run 
steelhead generally spawn after peak flow events and are less 
susceptible to redds being scoured (Halofsky et al., 2011). Still, 
future increases in streamflow can increase the magnitude and frequency 
of streambed mobilization and scour, impacting eggs and embryos, while 
warmer temperatures may result in more rapid incubation leading to 
earlier timed and smaller individuals at emergence (Dalton et al., 
2016).
    Environmental variability now and into the future will also likely 
impact steelhead in the marine environment. Modeling analysis predicted 
an 8 to 43 percent contraction of steelhead species' marine habitat due 
to changing thermal conditions between the 2020s and 2080s, depending 
on time period (Abdul-Aziz et al., 2011). The assessment by the co-
managers (COPSWG 2023) and subsequent publication (Ohlberger et al., 
2025) suggested that interannual variation in recruitment and kelt 
survival were both partially explained by summer sea surface 
temperatures (SST) with lower recruitment and kelt survival with warmer 
summer SST. Models showed that pink salmon abundance as well as North 
Pacific Gyre Oscillation (NGPO) also influence recruitment (Ohlbergur 
et al., 2025). There is uncertainty in how smolt survival and 
recruitment and kelt survival will change over time, but kelt survival 
has already declined since the 1980s.
    There may be positive impacts from environmental variability, 
particularly temperature, such as possible longer rearing seasons due 
to temperature increases at certain times of the year, increased 
productivity within the food web, and more rapid growth at certain 
times and life stages (Halofsky et al., 2011; Dalton 2016). Warmer 
conditions in summer would likely reduce growth, but warmer 
temperatures at other times of the year could increase growth rates 
(Dalton et al., 2016) and improve rearing conditions for juveniles, 
especially in the lower river reaches. However, warmer temperatures 
also potentially increase susceptibility to disease and increase 
competition with other species or predation, through the increased 
presence of non-native piscivorous species.
    At the population level, the ability of organisms to genetically 
adapt to environmental variability depends on how selection on multiple 
traits interact and whether those traits are linked genetically. 
Factors that affect genetic diversity can limit the ability of a 
population to adapt to variability in environmental conditions. These 
factors include, but are not limited to, small population size, 
domestication in hatchery environments, and/or introgression by 
introduced non-native stocks. Also, future environmental changes are 
likely to happen much faster than normal adaptation processes can 
respond.

Rangewide Risk of Extinction

    The SRT's determination of rangewide extinction risk to the OP 
steelhead DPS used the categories of high, moderate, or low risk of 
extinction. The risk levels are defined as:
    (1) High risk: A species or ESU with a high risk of extinction is 
at or near a level of abundance, productivity, diversity, and/or 
spatial structure that places its continued existence in question. The 
demographics of a species or ESU at such a high level of risk may be 
highly uncertain and strongly influenced by stochastic and/or 
depensatory processes. Similarly, a species or ESU may be at high risk 
of extinction if it faces clear and present threats (e.g., confinement 
to a small geographic area; imminent destruction, modification, or 
curtailment of its habitat; disease epidemic) that are likely to create 
such imminent demographic risks.
    (2) Moderate risk: A species or ESU is at moderate risk of 
extinction if it exhibits a trajectory indicating that it is more 
likely than not to reach a high level of extinction risk in the 
foreseeable future. A species or ESU may be at moderate risk of 
extinction due to projected threats and/or declining trends in 
abundance, productivity, spatial structure, or diversity. The 
appropriate time horizon for evaluating whether a species or DPS is 
more likely than not to become at high risk in the future depends on 
various case- and species-specific factors. For example, the time 
horizon may reflect certain life-history characteristics (e.g., long 
generation time or late age-at-maturity) and may also reflect the 
timeframe or rate over which identified threats are likely to impact 
the biological status of the species or ESU (e.g., rate of disease 
spread). The appropriate time horizon is not limited to the period that 
status can be quantitatively modeled or predicted within predetermined 
limits of statistical confidence.
    (3) Low risk: A species or ESU is at low risk if it is not at 
moderate or high risk of extinction.
    The SRT considered the ``foreseeable future'' to be a time period 
of approximately 40 to 60 years. Following Stout et al. (2012), the 
shorter end of this timeframe corresponds to roughly 10 steelhead 
generations, which the SRT concluded was a reasonable value over which 
to consider current demographic trends. The longer end of this 
timeframe corresponds to a timeframe over which scientific studies of 
the impacts of environmental variability on salmonid freshwater and 
ocean habitat are available. For example, the SRT utilized analyses of 
predicted future stream temperatures and stream flow in the years 2040 
and 2080 and marine studies for O. mykiss that center on the 2040s and 
2080s (Abdul-Aziz et al., 2011).
    The SRT used a likelihood point method to account for uncertainty 
in the overall extinction risk by allocating ten risk points across the 
low, moderate, and high-risk categories. In their overall evaluation of 
the DPS status, the majority of the SRT members put the majority of 
their 10 allocated risk likelihood points in the moderate extinction 
risk category leading to an average of 5.5 in moderate, 4 in low, and 
0.5 in high. A minority of members (\2/8\) put either equal points 
between low and

[[Page 1460]]

moderate extinction risk or the majority of points in low extinction 
risk category (six points in low, four in moderate). SRT members with 
the majority of points in low extinction risk concluded that the 
overall DPS abundance was still relatively moderate compared to other 
steelhead DPSs and that the major threats, other than environmental 
variability, could be addressed directly through management actions. 
Therefore, there was uncertainty across the members about the level of 
risk facing OP steelhead (not unanimous).
    In consideration of the factors identified in 4(a)(1) of the ESA 
and our analysis of the viability of the DPS, including any 
uncertainties, we are unable to find the DPS faces a high or moderate 
risk of extinction now or in the foreseeable future. Despite some 
legacy effects of forestry and land use practices, habitat quality and 
connectivity are generally good within the DPS due to declining timber 
harvest activity, especially within the ONP, and the absence of dams or 
other major artificial passage blockages in the region. OP steelhead 
habitat has also benefitted from several restoration programs including 
efforts to repair culverts, retire forest service roads, and supplement 
woody debris. Additionally, under existing regulatory mechanisms, the 
co-managers have implemented improved harvest management strategies and 
harvest of OP steelhead has declined within the last decade, 
particularly the last few years. There have also been changes in 
hatchery operations to reduce straying. Abundance trends suggest 
populations have declined over the long-term; however, increases in 
abundance in the last couple of years in certain basins are promising, 
and overall DPS abundance is still relatively moderate compared to 
other steelhead DPSs. The co-managers and NMFS will continue monitoring 
populations for response signals from recent and future conservation 
management actions. While information is limited, disease risk to 
natural-original OP steelhead is considered very low risk. Some 
evidence suggests introgression between hatchery-origin and native 
fish, though data regarding the current levels of genetic mixing are 
limited. The extent to which predation may be limiting the viability of 
OP steelhead is uncertain, although pinniped predation is not 
considered a primary threat to steelhead in these ecosystems. Predicted 
variation in stream temperatures and flows, changes to the marine 
environment, and alterations in seasonal rainfall patterns are likely 
to negatively impact the DPS in the foreseeable future; however, some 
beneficial impacts are also possible, and there remains considerable 
uncertainty about the localized effects of environmental variation to 
OP steelhead populations. Based on the foregoing, we have determined 
the DPS is not at a high risk of extinction or near a level of 
abundance, productivity, diversity, and/or spatial structure that 
places its continued existence in question; nor does the DPS exhibit a 
trajectory indicating that it is more likely than not to reach a high 
level of extinction risk in the foreseeable future.

Significant Portion of Its Range Analysis

    As noted in the introduction above, the definitions in section 3 of 
the ESA of both ``threatened species'' and ``endangered species'' 
contain the term ``significant portion of its range'' (SPR), which we 
interpret to refer to an area smaller than the entire range of the 
species. As indicated by these definitions, we can list a species based 
on their status in all of their range or based on their status in a 
SPR. The range of a species is considered to be the general 
geographical area within which that species can be found at the time 
NMFS or USFWS makes any particular status determination. This range 
includes those areas used throughout all or part of the species' life 
cycle, even if they are not used regularly (e.g., seasonal habitats). 
(79 FR 37578, 37583, July 1, 2014).
    In construing the statutory definitions of threatened species and 
endangered species, we are thus required to give some independent 
meaning to the SPR phrase to avoid rendering it superfluous to the 
``throughout all'' language (See Defenders of Wildlife v. Norton, 258 
F.3d 1136 (9th Cir. 2001)). Under the 2014 policy regarding the 
interpretation of the phrase ``significant portion of its range'' (SPR 
Policy), which was issued jointly by NMFS and USFWS, first we evaluate 
the status of the species throughout its range and, unless we find the 
species is endangered based on the rangewide analysis, we must go on to 
consider whether the species may have a higher risk of extinction in an 
SPR (79 FR 37578, July 1, 2014). The assessment consisted of 
identifying and evaluating portions of the DPS that are potentially at 
high risk of extinction and are important to the overall DPS's long-
term viability, yet not so important as to be determinative of its 
current or foreseeable status. In other words, the goal of the SPR 
analysis was to determine if there are biologically important portions 
of the DPS that are currently at higher risk than the DPS rangewide but 
that are not so important that their status would lead to the entire 
DPS being currently at higher risk.
    Because a species' range can theoretically be divided into an 
infinite number of portions, the SRT first discussed and identified 
several sub-DPS portions that had a reasonable likelihood of being at 
higher risk of extinction than the DPS rangewide and a reasonable 
likelihood of being biologically significant to the species. Unless a 
portion meets both conditions, they will not be further considered in 
the SPR analysis (as they could not form the basis for a proposed 
listing). In evaluating whether a portion was biologically significant, 
the SRT considered whether the species within that portion was 
important to the DPS's long-term viability but not so important that 
their status would drive current or foreseeable DPS-wide extinction 
risk. After considering multiple possibilities, the SRT settled on a 
more detailed evaluation of two types of strata based on geography or 
adult run-timing.
    In this case, the geographic units considered include steelhead 
populations in rivers that drain to the Strait and steelhead 
populations in rivers that drain to the Pacific Ocean. These two 
regions were identified as potential portions due to the hydrological 
and geographic distinctiveness of the rivers supporting Strait 
populations and coastal populations. The majority of the SRT members 
assigned a majority of their 10 allocated points in the not 
biologically significant category for populations in rivers draining to 
the Strait. The SRT concluded that populations in the Strait portion 
may express distinct life-history strategies, however, there are 
coastal populations in streams ecologically similar to those in the 
Strait, and over the long term it is likely that the rivers on the 
Strait could be recolonized by coastal OP steelhead runs. So, though 
these runs are important to diversity and spatial structure, they are 
not so important as to be biologically significant relative to the 
overall long-term viability of the species. Because the SRT determined 
that the Strait populations did not meet the agency's criteria for 
significance, the Strait portion of the range is not considered to be 
an SPR. Coastal populations are the most numerous and widespread 
portion of the DPS. The status of the coastal component is 
determinative of the rangewide status of the DPS and is therefore not a 
valid SPR.
    The team also considered whether the variation in adult run-timing 
might form the basis for identifying alternative portions. In general, 
summer- and

[[Page 1461]]

winter-run steelhead utilize spatially different freshwater habitats, 
particularly during the adult freshwater migration and spawning 
portions of the life cycle. Generally, summer-run steelhead tend to 
spawn in the upper portions of river systems. Sometimes these areas are 
above temporal flow barriers that are only accessible during high 
spring flows (Withler 1966; Myers et al., 2015; Waples et al., 2022), 
thus not utilized by winter-run and leading to a different geographic 
extent for summer-run.
    However, we have determined the summer-run stratum does not qualify 
as a valid portion of the OP steelhead range because, consistent with 
the ESA and the 2014 SPR Policy (79 FR at 37583), the selection of 
portions for consideration should be premised at least in part on a 
geographically oriented rationale. Here, the summer-run component lacks 
sufficient spatial segregation from the winter-run to be considered a 
valid portion of the DPS's range for the purposes of SPR analysis under 
the ESA. A review of spawning and rearing habitat utilized by summer-
run steelhead, found only 0.7 percent of the habitat was used solely by 
summer-run steelhead. In other words, >99.3 percent of summer-run 
geography is shared with winter-run fish. Therefore, the summer-run 
component does not qualify as a valid portion of the OP steelhead 
range.
    Additionally, the SRT concluded that the summer-run portion did not 
meet the criteria to be considered biologically significant to the 
DPS's long-term viability. The SRT concluded that summer-run 
populations contribute to genetic diversity and spatial structure 
diversity of the DPS. However, the SRT ultimately concluded the summer-
run fish to be not significant because summer-run steelhead currently 
are not and historically were not a major contributor to overall DPS 
abundance, winter-run and summer-run populations in the same watershed 
are not reproductively isolated and have generally been found to be 
genetically very similar (thus there is some possibility for 
reestablishment if a summer-run population is lost), and summer-run 
specific habitat (predominantly just for spawning) represents a minor 
fraction of the total accessible spatial structure. Summer-run 
steelhead was voted to have a higher risk than the DPS range-wide, but 
given that summer-run steelhead did not meet the agency's criteria to 
be considered significant and a valid portion, this grouping is not 
considered an SPR.
    Finally, winter-run populations are the most numerous and 
widespread portion of the DPS. The status of the winter-run component 
is determinative of the rangewide status of the DPS and is therefore 
not a valid SPR. We conclude that there are no portions of the DPS's 
range that are both significant and at higher risk of extinction than 
the DPS as a whole.

Final Determination

    Section 4(b)(1) of the ESA requires that we make listing 
determinations based solely on the best scientific and commercial data 
available after conducting a review of the status of the species and 
taking into account those efforts, if any, being made by any State or 
foreign nation, or political subdivisions thereof, to protect and 
conserve the species. We have independently reviewed the best available 
scientific and commercial information, including references cited in 
the petition, public comments submitted on the 90-day finding (88 FR 
8774; February 10, 2023), the status review report, and information 
provided by co-managers, and we have consulted with species experts and 
individuals familiar with steelhead.
    Based on the foregoing information, we determine OP steelhead do 
not warrant listing at this time. Primary factors leading to this 
conclusion include: habitat quality and connectivity are generally good 
within the DPS and are benefitting from ongoing restoration efforts; 
spatial distribution is good; State and Tribal co-managers have 
implemented improved harvest and hatchery practices and reduced harvest 
significantly in recent years; abundance trends suggest declining 
populations, but the response to recent management actions has yet to 
be seen; and while environmental variation is expected to have some 
negative impacts on the DPS, there could also be positive impacts while 
the precise localized effects are unclear. Additionally, we did not 
identify any portions of the DPS that were both significant and facing 
a higher level of extinction risk than the DPS rangewide. Therefore, we 
determine listing is not warranted. NMFS intends to continue to monitor 
the status of the OP steelhead DPS and work closely with the State and 
Tribal co-managers.

References

    A complete list of all references cited herein is available upon 
request (See FOR FURTHER INFORMATION CONTACT).

Authority

    The authority for this action is the Endangered Species Act of 
1973, as amended (16 U.S.C. 1531 et seq.).

Samuel D. Rauch, III,
Deputy Assistant Administrator for Regulatory Programs, National Marine 
Fisheries Service.
[FR Doc. 2026-00581 Filed 1-13-26; 8:45 am]
BILLING CODE 3510-22-P


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