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

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period, habitat improvements included the removal of several small dams <strong>and</strong> increases<br />

in summer flows in the watersheds, a reduced ocean fisheries, <strong>and</strong> a favorable terrestrial<br />

<strong>and</strong> marine climate. All three spring-run Chinook populations in the Sacramento River<br />

tributaries have long-<strong>and</strong> short-term lambdas >1, indicating population growth.<br />

However, population sizes are relatively small compared to fall-run Chinook salmon<br />

populations, <strong>and</strong> there have been some extreme fluctuations in population size, which is<br />

often indicative of an impending collapse in small populations. Additionally, Feather<br />

River hatchery <strong>and</strong> Feather River spring-run Chinook salmon are not closely related to<br />

the Mill, Deer, <strong>and</strong> Butte creek spring-run Chinook salmon populations. This group<br />

represents a distinct genetic legacy. Although protective measures <strong>and</strong> critical habitat<br />

restoration likely have contributed to recent increases in spring-run Chinook salmon<br />

abundance, the ESU is still below levels observed from the 1960s through 1990. Threats<br />

from hatchery production (i.e., competition for food between naturally spawned <strong>and</strong><br />

hatchery fish, <strong>and</strong> run hybridization <strong>and</strong> homogenization), climatic variation, reduced<br />

stream flow, high water temperatures, predation, <strong>and</strong> large scale unscreened water<br />

diversions persist.<br />

Critical Habitat<br />

Critical habitat was designated for this species on September 2, 2005 (70 FR 52630).<br />

The critical habitat designation for this ESU identifies PCEs that include sites necessary<br />

to support one or more Chinook salmon life stages. Specific sites include freshwater<br />

spawning sites, freshwater rearing sites, freshwater migration corridors, nearshore marine<br />

habitat, <strong>and</strong> estuarine areas. The physical or biological features that characterize these<br />

sites include water quality <strong>and</strong> quantity, natural cover, forage, adequate passage<br />

conditions, <strong>and</strong> floodplain connectivity. Factors contributing to the downward trends in<br />

this ESU include: loss of most historical spawning habitat, reduced access to<br />

spawning/rearing habitat behind impassable dams, climatic variation, water management<br />

activities, hybridization with fall-run Chinook salmon, predation, <strong>and</strong> harvest. Additional<br />

factors include the degradation <strong>and</strong> modification of remaining rearing <strong>and</strong> migration<br />

habitats in the natal stream, the Sacramento River, <strong>and</strong> the Sacramento delta. The natal<br />

tributaries have many small hydropower dams <strong>and</strong> water diversions that in some years<br />

70

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