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<br />14 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />CONCEPTUAL ECOLOGICAL MODEL OF THE VALUE OF LOW WATER VELOCITY HABITATS IN THE <br />UPPER COLORADO RIVER BASIN TO THE ENDANGERED FISHES <br /> <br />Generally, the input of terrestrial organic matter provides the basis for energy in headwater streams (Vannote <br /> <br /> <br />et al. 1980). Large rivers, such as those of the upper basin, depend upon fine particulate organic matter <br /> <br /> <br />from upstream reaches for basic productivity (Vannote et al. 1980; Sedell and Richey 1989). Although <br /> <br /> <br />detailed ecological studies of the various habitats in the upper basin have not been made, inferences can <br /> <br /> <br />be drawn from the published literature. <br /> <br />A. Relation of Nutrients. Sunlight Penetration. and Warm Water Temoeratures to Phytoplankton Production. <br /> <br /> <br />Phytoplankton productivity provides the basis for development of a food web. Phytoplankton production <br /> <br /> <br />and standing crops increase in concert with increases in annual input of nutrients regardless of latitude. <br /> <br /> <br />Carbon, nitrogen, and phosphorus are key elements for phytoplankton production. Phosphorus is perhaps <br /> <br /> <br />most limiting in north temperate and subarctic climates (Schindler 1978). Nitrogen is the most abundant <br /> <br /> <br />element in the atmosphere and is generally not limiting. Also. abundant carbon dioxide in the atmosphere <br /> <br /> <br />provides the necessary carbon. Therefore, phytoplankton production and standing crop in north temperate <br /> <br /> <br />freshwaters is generally proportional to the phosphorus input. Particulate phosphorus, either chemically <br /> <br />desorbed or actively mobilized by microbiota, is not readily available in rivers with a high sediment load <br /> <br /> <br />because most of the phosphorus is bound to the sediments (Ellis and Stanford 1988). Watts and Lamarra <br /> <br /> <br />(1983) determined that between 21 % and 49% of the total phosphorus in Colorado River water at the bridge <br /> <br /> <br />upstream from Moab, Utah in September and October 1978 was bioavailable with most of the extractable <br /> <br /> <br />element in the form of calcium-bound phosphorus. Therefore, Watts and Lamarra (1983) concluded that <br /> <br /> <br />algae production was not nutrient limited in this reach of the Colorado River but that primary production was <br /> <br /> <br />inversely related to the turbidity of the riverine environment. <br />