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Discussion <br />The study site is 259 km downstream of Flaming Gorge Dam on the Green <br />River. Studies on other rivers by Herlong and Mallin (1985) and Sandlund (1982) <br />have shown that up to 45 % of plankton aze removed within 200 m downstream of the <br />dam and 76 % aze removed within 2.2 km. They still report influences at 3.4 km from <br />the dam. Reservoir plankton may exist in reduced numbers for several hundred <br />kilometers on lazge rivers (Wazd 1975). However, at great distances the river <br />plankton may be dominated by plankton from source areas along the river (Repsys <br />and Rogers 1982). The study site is 259 km downstream of the Flaming Gorge Dam <br />and reservoir plankton is not believed to influence the microcrustacean densities of the <br />communities, at the Ouray Refuge azea of the Green River. <br />n i' <br />Many studies of invertebrate drift address microcrustaceans secondarily (eg. <br />Clifford 1972, Benke et al. 1991) and their data aze not directly comparable with this <br />study. This is a result of too lazge of mesh size or failure to identify species. Other <br />studies have specifically assessed microcrustaceans densities (Holden and Green 1960, <br />Hanf 1982, Saunders and Lewis 1988x, 1988b, 1989; Grawbowski and Heibert 1989). <br />Backwater. This study reported plankton densities of 1,450-7,131/m3 for the <br />Ouray backwater and 63,353/m3 and for Intersection Wash. The benthic densities at <br />the Ouray backwater were 6x greater per squaze meter than for the plankton in <br />August and equal in July, but no existing density estimates aze available for <br />14 <br />