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Last modified
7/14/2009 5:02:37 PM
Creation date
5/24/2009 7:09:39 AM
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UCREFRP
UCREFRP Catalog Number
9685
Author
Tyus, H. M. and C. A. Karp.
Title
Habitat Use and Streamflow Needs of Rare and Endangered Fishes
USFW Year
1989.
USFW - Doc Type
Flaming Gorge Studies - 2nd Preliminary Draft.
Copyright Material
NO
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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 wei r <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 increased progressively <br />downstream within the study reach, although variability was high among the <br />several backwaters sampled at a site. ... In many samples: chironomid larvae <br />comprised over 90 percent of the benthic 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 i6 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 />Shallow backwaters with a large surface area in the Ouray area that were <br />seasonally permanent after runoff subsided were generally warmer compared to <br />upstream backwaters at Island Park and Jensen; they had higher concentrations <br />14 <br />
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