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~* <br />INTRODUCTION <br />lJntil 1984, the White River was one of the last free-flowing <br />rivers i~n the state of Colorado. With the completion of Taylor Draw <br />Dam and .the filling of Kenney Reservoir, the White River has now gone <br />the way of the Upper Colorado River and its tributaries which <br />collectively have been impounded more than 120 times (considering <br />reservoirs only in excess of 1.2 cubic hectometers (1000 acre- <br />feet))(Bishop and Porcella 1980). Regulation in the Upper Basin has <br />had a profound effect on the aquatic ecosystem, where biota had adapted <br />and evolved to extreme fluctuations in flow, temperature and turbidity <br />(Holden 1979; Behnke 1980; Behnke and Benson 1980; Molles 1980). A <br />series of four recently published papers (Stanford and Ward 1986, <br />1986a, 1986b; Ward et al. 1986) provide an in depth review of the <br />history, development and ecology of the Colorado River system. <br />The lower White River of Colorado supports seven native <br />species and an equal number of introduced species, although the fish <br />-- community in the vicinity of the Taylor Draw project is still <br />predominantly native (Carlson et al. 1979; Holden 1979). The federally <br />endangered Colorado squawfish (Ptvchocheilus cius) is still found in <br />the White River of Colorado and Utah. Due to their highly migratory <br />nature, which was reported in early accounts (Sigler and Miller 1963) <br />