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Biological Opinions - Bureau of Reclamation

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Oregon Department <strong>of</strong> Fish and Wildlife requires scientific take permits that are reviewed to<br />

ensure there is minimal impact to native fish populations.<br />

7.10.6 Conclusions Regarding the Ability <strong>of</strong> the Action Area to Support LRS and SNS<br />

Conservation<br />

The recovery plan for the LRS and the SNS establishes a strategy that is intended to produce<br />

healthy, self-sustaining populations <strong>of</strong> the LRS and the SNS within the action area by reducing<br />

sucker mortality; restoring habitat, including sucker spawning, larval, and juvenile habitats; and<br />

increasing connectivity between sucker spawning and rearing habitats (USFWS 2013).<br />

Recovery also involves ameliorating the adverse effects <strong>of</strong> degraded water quality, disease, and<br />

nonnative fish on LRS and SNS populations. The recovery goal is to produce naturally selfsustaining<br />

populations that possess healthy long-term demographic traits and trends (USFWS<br />

2013).<br />

UKL is especially critical to the conservation <strong>of</strong> the LRS and the SNS because it provides the<br />

most habitat and has the greatest variety <strong>of</strong> spawning sites. Currently, the largest population <strong>of</strong><br />

the LRS is found in UKL and its tributaries. It is possible that UKL supported the largest SNS<br />

population, but its abundance there has decreased substantially from a decade ago (Hewitt et al.<br />

2012). Even though the LRS and the SNS are dependent on UKL during nearly every life stage,<br />

conditions in the lake are seasonally adverse due to poor water quality, algal toxins, and other<br />

factors. Suckers stressed by poor water quality are more vulnerable to disease, predators, and<br />

entrainment. There is also a variety <strong>of</strong> parasites in the lake that reduce sucker survival. Habitat<br />

conditions also have been degraded by loss <strong>of</strong> wetlands. Substantial entrainment <strong>of</strong> larval and<br />

juvenile suckers occurs at the outlet <strong>of</strong> UKL. The nearly universal disappearance <strong>of</strong> juvenile<br />

suckers from UKL beginning in August and extending into October (Simon et al. 2011), likely in<br />

response to the synergistic effects <strong>of</strong> the above factors, has precluded adequate recruitment into<br />

the adult populations <strong>of</strong> the LRS and the SNS in UKL in over a decade; neither the LRS or the<br />

SNS populations in UKL exhibit normal population demographic patterns and are not selfsustaining.<br />

This lack <strong>of</strong> recruitment is increasing the risk for a collapse and extirpation <strong>of</strong> the<br />

LRS and the SNS from UKL as the older adult populations continue to age and die.<br />

Keno Reservoir and the downstream hydroelectric reservoirs are highly altered systems that<br />

currently support small sucker populations, mostly <strong>of</strong> the SNS. All <strong>of</strong> these areas provide<br />

recovery benefits by adding redundancy, but currently they do not support self-sustaining<br />

populations because <strong>of</strong> habitat limitations. Because Keno Reservoir is downstream <strong>of</strong> UKL, and<br />

large numbers <strong>of</strong> suckers disperse there from upstream, it has the potential to provide rearing<br />

habitat for suckers that ultimately could migrate back to UKL. Nevertheless, habitat and water<br />

quality conditions in the Keno Reservoir are seasonally adverse, and are unlikely to change<br />

substantially over the next decade.<br />

Climate change is having a small but measureable effect over the entire Klamath River Basin.<br />

Air and water temperatures are increasing, and inflows to UKL are diminishing, at least during<br />

the summer to early winter period. The effects <strong>of</strong> climate change on air and water temperatures<br />

and on the magnitude, duration, and timing <strong>of</strong> inflows to UKL are expected to get more severe in<br />

the future (Flint and Flint 2011, Markstrom et al. 2011).<br />

103

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