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Biological Opinions - Bureau of Reclamation

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The April through September 4,034.60 ft (1229.75 m) minimum elevation was set, in part, to<br />

provide access to spawning areas below Anderson-Rose Dam (USFWS 2008). Spawning runs<br />

have occurred in years that Anderson-Rose Dam spills or releases water. Releases were required<br />

as provisions <strong>of</strong> earlier biological opinions (USFWS 1992, 2001, 2008). In 2006 and 2007,<br />

USFWS entered into an agreement with Tulelake Irrigation District to provide releases during<br />

the spawning season, but high flows in 2006 flushed out newly placed spawning gravel, and no<br />

further efforts were made to support spawning below the dam. As a result, in 2009, the 2008<br />

biological opinion was amended and minimum flows were no longer required at Anderson-Rose<br />

Dam. Successful egg incubation and survival <strong>of</strong> larvae to swim-up below Anderson-Rose Dam<br />

has been infrequent in recent years and, because only two juvenile suckers were captured in Tule<br />

Lake in recent years, natural recruitment is thought to be very low or nonexistent (Hodge and<br />

Buettner 2008, USFWS 2008). The 2013 Revised Recovery Plan and the 2012 Final Rule for<br />

Critical Habitat both emphasize that agencies should continue to evaluate the feasibility <strong>of</strong><br />

restoring spawning habitat and self-sustaining populations <strong>of</strong> suckers in Tule Lake. <strong>Reclamation</strong><br />

has put suckers salvaged from the California portion <strong>of</strong> the Project into Sump 1A as part <strong>of</strong> their<br />

efforts to meet BiOp canal salvage requirements. This has occurred on a yearly basis since the<br />

early 1990s and numbers <strong>of</strong> suckers placed here varied from 2 to 625 between 2006 to 2010, and<br />

averaged 444 per year.<br />

Water depths <strong>of</strong> Tule Lake Sumps 1A and 1B are shallow (mostly less than 4 ft [1.2 m] deep),<br />

and consequently there is a lack <strong>of</strong> adequate depth for suckers in large portions <strong>of</strong> the sumps.<br />

Additionally, gradual sedimentation is a potential threat to adult suckers that require water depths<br />

greater than 3 ft (1 m) to avoid predation by fish-eating birds, particularly pelicans (USFWS<br />

2008).<br />

During severe winters with thick ice cover, only small, isolated pockets <strong>of</strong> water with depths<br />

greater than 3 ft (1 m) exist in Sump 1A, increasing the risk <strong>of</strong> winter die-<strong>of</strong>fs (USFWS 2008).<br />

However, the April 1 to September 30 minimum elevation <strong>of</strong> 4,034.60 ft (1229.75 m) was set, in<br />

part, to provide rearing habitat in Sump 1A, and the October 1 to March 31 minimum elevation<br />

<strong>of</strong> 4,034.00 ft (1229.56 m) was set to provide adequate winter depths for cover and to reduce the<br />

likelihood <strong>of</strong> fish die-<strong>of</strong>fs from low DO concentrations below ice cover (USFWS 2008).<br />

Water quality also is considered a threat to suckers in Tule Lake sumps. Tule Lake is classified<br />

as highly eutrophic (enriched) because <strong>of</strong> high concentrations <strong>of</strong> nutrients and resultant elevated<br />

aquatic plant productivity (Dileanis et al. 1996). Because Tule Lake is shallow and the nutrient<br />

content high, photosynthesis and respiration by aquatic plants and algae causes large fluxes in<br />

DO and pH. During the irrigation season, water reaching the sumps has been used multiple<br />

times on agricultural lands, which leads to increases in nutrient and pesticide concentrations<br />

(Orlob and Woods 1964, Dileanis et al. 1996).<br />

<strong>Reclamation</strong> has documented surface temperatures up to 26 ºC (79º F); DO levels from<br />

supersaturation (>15.0 mg/L to near zero); and pH occasionally exceeds 10.0 (<strong>Reclamation</strong><br />

2009). During the winter, most inflow to Tule Lake is from localized run<strong>of</strong>f and water quality<br />

conditions are relatively good, except during prolonged periods <strong>of</strong> ice-cover when DO levels<br />

decline.<br />

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