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Last modified
7/14/2009 5:02:35 PM
Creation date
5/17/2009 10:51:31 PM
Metadata
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UCREFRP
UCREFRP Catalog Number
9410
Author
Wydoski, R. S. and E. J. Wick.
Title
Ecological Value of Floodplain Habitats to Razorback Suckers in the Upper Colorado River Basin.
USFW Year
1998.
USFW - Doc Type
Denver.
Copyright Material
NO
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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 />
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