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in Island Park or Jensen backwaters. ... Among the backwaters sampled, those <br />larger backwaters with narrow connections to the river, with a lower exchange <br />rate and a greater retention time (BA 300.5 and BA 251.0), generally had <br />higher densities of zooplankton. <br />... Fluctuations in riverflow that increase water level in backwaters <br />result in importation of riverine nutrients and POM into backwaters, as well <br />as resuspension of organic material from the inundated periphery of the <br />backwater with possible leaching of nutrients from organic material increase <br />turbidity which may provide cover for the native fish that evolved in this <br />ecosystem, and reduce the likelihood of predation on Colorado squawfish by <br />nonnative fish. Decreasing water levels in backwaters resulting from reduced <br />riverflows-may result in export of nutrients and biota to the river. The <br />extent of export of nutrients and biota to the river cannot be addressed at <br />this time. <br />Concentrations of major nutrients (nitrate-N, ammonia-N, and phosphorus) <br />generally increased in backwaters from upstream at Island Park to downstream <br />at Ouray. ... Ouray backwater nutrient concentrations exceeded river <br />concentrations. Higher nutrient concentrations in Ouray backwaters compared to <br />Island Park and Jensen backwaters and the river at Ouray may indicate internal <br />nutrient recycling within these backwaters or a response to attenuated <br />riverflows compared to upstream wherein nutrients transported into the <br />backwaters from the river during rising water levels are retained as riverflow <br />decreases, or leached from the inundated backwater shoreline. The less severe <br />action of inundation and draining in Ouray backwaters caused by attenuated <br />riverflows may reduce the tendency for violent mixing of water in backwaters, <br />and reduce export of POM and nutrients during draining. <br />Average macroinvertebrate abundance in backwaters decreased downstream <br />in 1987, but was greater in Ouray backwaters in 1988, compared both to 1987 <br />and to upstream backwaters. However, average macroinvertebrate dry biomass <br />increased progressively downstream in both 1987 and 1988, with greatest dry <br />biomass present in Ouray backwaters, particularly.the reference site at river <br />mile 251. In many samples, chironomid larvae comprised over 90% of the benthic <br />fauna. <br />Benthic algae and detritus ... comprised a large portion of the stomach <br />contents of the young suckers collected. Predatory chironomid larvae, <br />although few in number in the backwaters sampled, likely prey on the grazing <br />chironomids. Food web interactions at this lower trophic level may result in <br />nutrient recycling within some Green River backwaters. <br />Food habit studies of 16 species of native and nonnative fish collected <br />from backwaters, indicated some dietary overlap due to heavy utilization of <br />chironomid larvae by some young fish <20mm TL. The 14 Colorado squawfish <20mm <br />TL collected in 1987 and 1988 consumed mostly chironomid larvae, while <br />Colorado squawfish >20mm TL showed evidence of piscivory, but continued to <br />consume chironomid larvae. As the Colorado squawfish grow and include larval <br />fishes, primarily red shiner, in their diet, along with chironomid larvae, <br />dietary overlap with other fish species diminishes because of the expanded <br />food resource. The stomachs of some young fish, such as the native suckers, <br />contained mostly algae. Few fish species other than Colorado squawfish and <br />Gila spp. consumed larval fish. After Colorado squawfish become piscivorous, <br />red shiners, fathead minnows, occasional catostomids, and other introduced <br />fish species are found in the diet suggesting less dependence on the <br />relatively abundant chironomid larvae. <br />14 <br />