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<br />36 <br /> <br />the lower station was sampled and May 21 when the upper and middle sta- <br />tions were sampled. Therefore, the lower station was sampled while <br />the water was low and the sample was taken in an area that had sup- <br />ported invertebrates for some time. The habitat sampled at the upper <br />and middle stations had just recently been inundated, and therefore had <br />supported invertebrates for only a few days. <br />The actual numbers of organisms found have little value for deter- <br />mining the size of invertebrate populations in the study area because <br />samples were taken in cobble substrate, which represents only about 1% <br />of the total river bed. Few, if any, organisms are found on the shifting <br />sand bottom which constitutes most of the river bed (Pearson 1967). <br />Therefore, our data should be taken as indicative of the invertebrate <br />community, and its general complexity, which occurs along the shorelines <br />of the study area. <br />Taxa collected in 1979 are generally similar to that found by <br />Holden and Crist (1978). More slow water forms such as Ephoron and <br />fewer swift water forms such as Simuliidae were collected in our study <br />as was expected as Holden and Crist (1978) sampled an area with abundant <br />cobble substrate and swifter flows. <br /> <br />Plankton, Periphyton, and Macrophytes <br />The trend indicated by the plankton and periphyton data follows <br />that noted for macroinvertebrates. High water samples are limited to <br />sampling areas that were essentially dry a short time earlier. This is <br />actually an equipment problem, but in many ways reflects what is actually <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />1 <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />t <br />I <br />I <br />I <br />