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Carbaryl, Carbofuran, and Methomyl - National Marine Fisheries ...

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Status <strong>and</strong> Trends<br />

SR sockeye salmon were originally listed as endangered in 1991. Their classification<br />

was retained following a status review on June 28, 2005 (70 FR 37160). The only extant<br />

sockeye salmon population in the SR basin at the time of listing was that in Redfish Lake,<br />

in the Stanley Basin (upper Salmon River drainage) of Idaho. Other lakes in the SR basin<br />

historically supported sockeye salmon populations, including Wallowa Lake (Gr<strong>and</strong>e<br />

Ronde River drainage, Oregon), Payette Lake (Payette River drainage, Idaho) <strong>and</strong> Warm<br />

Lake (South Fork Salmon River drainage, Idaho) (Gustafson, Wainwright et al. 1997).<br />

These populations are now considered extinct. Although kokanee, a resident form of O.<br />

nerka, occur in numerous lakes in the SR basin, resident O. nerka were not considered<br />

part of the species at the time of listing in 1991. Subsequent to the 1991 listing, a<br />

residual form of sockeye residing in Redfish Lake was identified. The residuals are nonanadromous.<br />

They complete their entire life cycle in freshwater, but spawn at the same<br />

time <strong>and</strong> in the same location as anadromous sockeye salmon. In 1993, NMFS<br />

determined that residual sockeye salmon in Redfish Lake were part of the SR sockeye<br />

salmon. Also, artificially propagated sockeye salmon from the Redfish Lake Captive<br />

Propagation program are considered part of this species (June 28, 2005, 70 FR 37160).<br />

NMFS has determined that this artificially propagated stock is genetically no more than<br />

moderately divergent from the natural population (Good, Waples et al. 2005). Five lakes<br />

in the Stanley Basin historically contained sockeye salmon: Alturas, Pettit, Redfish,<br />

Stanley <strong>and</strong> Yellowbelly (Bjornn, Craddock et al. 1968). It is generally believed that<br />

adults were prevented from returning to the Sawtooth Valley from 1910 to 1934 by<br />

Sunbeam Dam. Sunbeam Dam was constructed on the Salmon River approximately 20<br />

miles downstream of Redfish Lake. Whether or not Sunbeam Dam was a complete<br />

barrier to adult migration remains unknown. It has been hypothesized that some passage<br />

occurred while the dam was in place, allowing the Stanley Basin population or<br />

populations to persist (Bjornn, Craddock et al. 1968; Matthews <strong>and</strong> Waples 1991).<br />

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