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<br />Postlaryal Voung-of-Year Occurrence <br />No postlarval young-of-year Colorado squawfish greater than 25 mm total length <br />were collected from above the Gunnison River confluence in a total of <br />57 samples collected in the fall of 1982-1986. However, a total of <br />62 Colorado squawfish were collected in an 18-mile reach below the confluence <br />of the Gunnison River (54 samples). The 1982-1984 catch rate of young-of-year <br />Colorado squawfish in the 10-mile reach immediately downstream of the <br />confluence of the Gunnison River (river miles 160-170) warranted <br />classification of this reach as a "Young-of-Year Nursery Area" by the Basin <br />Biology Subcommittee (U.S. Fish and Wildlife Service 1984). <br />Nonspawning Adult Occurrence <br />Osmundson and Kaeding (1989) reported that adult Colorado squawfish catch <br />rates in the upstream 15-mile reach were twice as high as those in the <br />adjacent downstream river reach. During 1986-1989 adults were most abundant <br />in a 1.3-mile segment (river miles 174.4-175.7) of the 15-mile reach during <br />high water, particularly in two gravel-pit ponds that were accessible during <br />high flows. These fish may have moved into these ponds to feed and rest, or <br />they may have been attracted to the warm, productive environments that the <br />ponds provided (pond temperatures were as much as 10.5 °C warmer than the <br />adjacent river). Some of the squawfish captured from one pond were well <br />• tuberculated by June 3, when nearby river temperatures were only 10 °C-13 °C <br />(Kaeding, pers. comm.). It has been hypothesized by some investigators that <br />thermal energy units above those provided in the mainstream are important <br />to gonadal maturation. If this is true, then access to these sheltered <br />off-channel pools may be very important to successful spawning in the upper <br />reaches of the Colorado River. Historically, bottomlands that routinely <br />flooded during the spring runoff period would have provided these warm <br />productive habitats; in recent years, flooded gravel pits may have provided <br />the only comparable habitat. <br />Razorback Sucker <br />The razorback sucker, an endemic species unique to the Colorado River Basin, <br />was historically abundant and widely distributed within warmwater reaches <br />throughout the Colorado River Basin. Historically, razorback suckers were <br />found in the main stem Colorado River and major tributaries in Arizona, <br />California, Colorado, Nevada, New Mexico, Utah, Wyoming, and in Mexico (Ellis <br />1914; Minckley 1983). Bestgen (1990) reported that this species was once so <br />numerous that it was commonly used as food by early settlers and, further, <br />that commercially marketable quantities were caught in Arizona as recently as <br />1949. In the Upper Basin, razorback suckers were reported in the Green River <br />to be very abundant near Green River, Utah, in the late 1800's (Jordan 1891). <br />An account in Osmundson and Kaeding (1989) reported that residents living <br />along the Colorado River near Clifton, Colorado, observed several thousand <br />razorback suckers during spring runoff in the 1930's and early 1940's. In the <br />San Juan River drainage, Platania and Young (1989) relayed historical accounts <br />• of razorback suckers ascending the Animas River to Durango, Colorado, around <br />the turn of the century. <br />