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<br />• <br />of rapidly changing land and water uses. The zoogeographical effects of <br />dams and diversions, water storage, irrigation practices, mining pollution, <br />and the introduction of non-native species were thought to be especially im- <br />portant in terms of native fishes' welfare. Today, municipal pollution, <br />introduced fish diseases, and stream bank channelization could be added to <br />the list of suspicious resource developments. <br />Various authors have documented the decline or disappearance of <br />bonytail chubs and razorback suckers from the Green River in Colorado following <br />the closure and filling of Flaming Gorge Reservoir (Minckley and Deacon 1968; <br />Vanicek and Kramer 1969; Holden and Stalnaker 1975). These two fishes sur- <br />vived below the reservoir for a few years after it was completed and was fil- <br />ling with water. During this time, water temperatures and flows below the <br />impoundment were comparable to historic patterns. However, when full, the <br />cold tailwaters created by hypolimnetic reservoir releases significantly <br />lowered the water temperatures downstream. Lack of reproductive success by <br />bonytail chubs, as well as reduced growth, in the Green River was directly <br />correlated to the lowering of riverine water temperatures. Waters which usually <br />reached 700F in late summer did not approach the minimum 650F needed for <br />spawning. A concurrent disappearance of razorback suckers from the Green <br />River was also blamed on reduced water temperatures. In addition, a project <br />to improve trout fisheries by eliminating Colorado squawfish, suckers, and other <br />"trash" fishes above Flaming Gorge Dam resulted in a fish kill downstream as <br />far as Dinosaur National Monument. When detoxification procedures failed, <br />rotenone escaped downstream and numerous razorback suckers and bonytail chubs <br />were killed (Banks 1964). <br />Backwater nursery habitat for larval and juvenile fishes, usually <br />created during spring runoff by the inundation of low-lying areas adjacent to <br />- 7 -