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<br />I <br /> <br />captive propagation because these elements are closely interconnected. <br /> <br />I <br /> <br />II. FACTORS LIMITING ABUNDANCE OF SOME ENDEMIC FISHES <br /> <br />I <br /> <br />The Colorado River and its tributaries flow through 2,317 km (1,440 miles) of <br />arid land (Carlson and Muth 1989) and serves over 15 million people with water <br />for various uses including municipal use, irrigated agriculture, industry, and <br />mining (Utah Water Research Laboratory 1975; Bishop 1971). Bishop emphasizes <br />that these various uses of water have resulted in conflicts. This river flows <br />through arid or semi-arid land that is supplied by only about 2.9 hectare- <br />meters per square kilometer (60 acre-feet of water per square mile) of surface <br />water annually which is less than any other major river in the United States <br />(Utah Water Research Laboratory 1975) . <br /> <br />I <br /> <br />I <br /> <br />During the past century, water development in the Upper Colorado River Basin <br />to serve agricultural, domestic, industrial, and mining activities altered the <br />natural river ecosystem (Carlson and Muth 1989; Maddux et al. 1982; Miller et <br />al. 1982; Wydoski 1980; U.S. Fish and Wildlife Service 1990a,b, 1991). Dam <br />construction and water storage to serve human needs changed the natural <br />hydrograph through dam operations that released water for irrigated <br />agriculture (seasonal) or for generating power during peak use periods <br />(daily). Historic spring peaks in the hydrograph in the Green River (Vanicek <br />1967) and in the Colorado and Gunnison rivers (McAda and Kaeding 1991) were <br />decreased and streamflows were increased when the rivers would become <br />naturally low after the spring runoff. Changes in the hydrograph have, in <br />turn, altered aquatic habitats, particularly backwater and floodplain habitats <br />that are considered vital to survival during the early life stages of some <br />native fishes. Coldwater releases from dams reduced water temperatures of the <br />natural and historic warmwater aquatic ecosystem. Water depletions from the <br />system increased through irrigated agriculture. Nonnative fish species were <br />introduced in the rivers and manmade reservoirs, both intentionally and <br />accidentally, that changed the species composition of the fish community. <br />While native fishes in the Colorado River system have apparently been on the <br />decline since the 1800's (Miller 1961), they declined more rapidly in the <br />Upper Basin since the 1960's from habitat alterations of the river and <br />colonization by nonnative fishes (Miller et al. 1982; Carlson and Muth 1989) . <br /> <br />Although native Americans along the Colorado River constructed canals to <br />divert water for irrigating crops around 1000 A.D. (Graf 1985; Powell 1961), <br />irrigated agriculture via small diversions was not renewed until the middle to <br />late 1800's (Fradkin 1983) and did not become extensive until the 1920's (Hunt <br />and Huser 1988). Broad river valleys in the Upper Basin were colonized by <br />people who began to construct levees for flood control (Fradkin 1983). As <br />dams were constructed in the Upper Colorado River Basin -- particularly after <br />the completion of Flaming Gorge Dam on the Green River in 1963 and the Wayne <br />Aspinall Storage Unit on the Gunnison River in 1978 (Carlson and Muth 1989), <br />the historic peak spring streamflows decreased that allowed people to <br />construct levees that more easily controlled overbank flooding. Marshes and <br />floodplain habitats disappeared as levees were built to control the river from <br />regularly flooding agricultural lands. The connectivity of the river with <br />floodplains was severely reduced and dramatically disrupted the natural <br />function of the river/floodplain ecosystem that depended upon floodplains for <br />productivity. Many large, highly productive, floodplain areas in broad, <br />alluvial valleys along the Upper Colorado River Basin rivers are no longer <br />connected with the river. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The geologic isolation of the Colorado River and its <br />watersheds resulted in a fish fauna where 64% of the <br />endemic to the Colorado River system (Miller 1961) . <br />unique, the fish fauna of the Colorado River Basin is <br />compared with other North American river basins. The <br />Colorado River system were adapted to dynamic natural <br /> <br />tributaries from other <br />native species are <br />In addition to being <br />very depauperate when <br />native fishes of the <br />aquatic conditions that <br /> <br />I <br /> <br />I <br /> <br />8 <br /> <br />I <br /> <br />I <br />