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provide the required water quantity and hydrolosic reeime necessary for recovery' of the fishes. <br />The physical habitat includes azeas of the Colorado River system that aze inhabited or potentially <br />habitable for use in spa~~ning and feeding, as a nursery, or serve as corridors between these azeas. <br />In addition, oxbows, backwaters, and other azeas in the 100-year floodplain, when inundated, <br />provide access to spawning, nursery, feeding, and rearing habitats. <br />BIOLOGICAL BACKGROUND <br />Colorado Pikeminnon• <br />The Colorado pikeminnow evolved as the main predator in the Colorado River system. The diet <br />of Colorado pikeminnow longer than 3 or 4 inches consists almost entirely of other fishes <br />(Vanicek and Kramer 1969). The Colorado pikeminnow is the lazgest cyprinid fish (minnow <br />family) native to North America and, during predevelopment times, may have grown as large as <br />6 feet in length and weighed nearly 100 pounds (Behnke and Benson 1983). These lazge fish <br />may have been 25-50 years of age. <br />Based on eazly fish collection records, archaeological fmds, and other observations, the Colorado <br />pikeminnow was once found throughout watmwater reaches of the entire Colorado River Basin, <br />including reaches of the upper Colorado River and its major tributaries, the Green River and its <br />major tributaries, and the Gila River system in Arizona (Seethaler 1978). Colorado pikeminnow <br />were appazently never found in colder, headwater azeas. Seethaler (1978} indicates that the <br />species was abundant in suitable habitat throughout the entire Colorado River Basin prior to the <br />1850's. Historically, Colorado pikeminnow have been collected in the upper Colorado River as <br />faz upstream as Pazachute Creek, Colorado (Kidd 1977). <br />A mazked decline in Colorado pikeminnow populations can be closely correlated with the <br />construction of dams and reservoirs between the 1930's and the 1960's,introduction of nonnative <br />fishes, and removal of water from the Colorado River system. Behnke and Benson (1983) <br />summarized the decline of the natural ecosystem. They pointed out that dams, impoundments, <br />and water use practices are probably the major reasons for drastically modified natural river <br />flows and channel chazacteristics in the Colorado River Basin. Dams on the main stem have <br />essentially segmented the river system, blocking Colorado pikeminnow spawning migrations and <br />drastically changing river characteristics, especially flows and temperatures. In addition, major <br />changes in species composition have occurred due to the introduction of nonnative fishes, many <br />of which have thrived as a result of changes in the natural riverine system (i.e., flow and <br />temperature regimes). The decline of endemic Colorado River fishes seems to be at least <br />partially related to competition or other behavioral interactions with nonnative species, which <br />have perhaps been exacerbated by alterations in the natural fluvial em•ironment. <br />• The Colorado pikeminnow currently occupies about 1,030 river miles in the Colorado River <br />system (2~ percent of i[s original range) and is presently found only in the Upper Basin above <br />Glen Canyon Dam. It inhabits about 350 miles of the main stem Green River from its mouth to <br />