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Harpacticoida <br />One copepod group absent from much of this study is the harpacticoids. Densities <br />of 200-10,200/m2 in Lake Michigan have been reported by Nalepa and Quigley <br />(1983). Shiozawa (1991) reported densities of up to 100,000/m2 in Minnesota streams, <br />but also found that harpacticoids preferred gravel, not shifting sand substrates, such as <br />are found in the Green River. Adult specimens of Canthocamntus staphvliT_noides were <br />collected in the floodplain with densities ranging from 158-2,106/m2. Two adult <br />specimens of Nannopus spp. were sampled in the Ouray backwater plankton (7/m3) <br />and an unidentified species was collected in the backwater benthos at a density of <br />359/m2. No harpacticoids were collected in the river. The harpacticoid densities <br />reported in this study are low and are most similar to Lake Michigan densities. <br />Implications <br />High densities of microcrustaceans in floodplain plankton have been reported <br />before. This study gave evidence of the additional importance of the benthos as a <br />source of microcrustaceans in backwaters, river channels, and especially floodplains. <br />The benthic densities at times were greater than the plankton densities. <br />Most of the large rivers in the U.S. have been dammed to provide hydroelectric <br />power, flood control, or water for irrigation. These dams have caused many changes <br />downstream, including temperature, turbidity, sediment transport, and flood regimes. <br />The Green River is no exception. Development of the Flaming Gorge Dam has <br />changed the hydrological profile of the river downstream. Concomitant with that- has <br />19 <br />