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<br />I <br />I <br />I <br /> <br />Larval fishes in the Missouri River are dominated by freshwater drum, catostomids, <br />cyprinids, and carp (Hergenrader, et al. 1982). Larval fish were found to be common in the <br />drift from early May through July, Spawning areas used are along the shoreline, in backwaters, <br />and behind channel control structures. Only limited suitable nursery areas exist in the <br />channelized Missouri River because of high current velocity, turbulent flows, and silt and sand <br />loads. Hergenrader, et al, (1982) found evidence that backwater areas function as nursery <br />zones, <br /> <br />II <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />II <br /> <br />The relative abundance of fish species in the Missouri River has changed dramatically <br />since the channelization of the river (Hesse, et al. 1982). This is believed to be due to the <br />changing availability of aquatic insects. Hesse, et al. (1982) contend that midchannel sandbar <br />production has assumed a larger proportion of the total system production following a reduction <br />in overhanging trees, snag production, and off-channel backwater production as a result of <br />channelization, Species such as flathead chubs and plains minnows have been replaced by those <br />species, such as emerald shiners, which rely more on zooplankton availabilities in swifter <br />currents, <br /> <br />According to Carter, et al, (1982), benthic densities and numbers of taxa were typically <br />lowest in June and increased in late summer and autumn. This was attributed to a relatively <br />stable river flow, higher water temperatures, and increased photoperiod, At other times the <br />swift current, high turbidity, and substrate instability of the main channel of the Missouri River <br />seriously limit the development of macroinvertebrate populations. Major colonizers are <br />restricted to pile dikes, riprap, and a narrow zone near shore. Trichoptera, Ephemeroptera, and <br />Diptera inhabit the dikes and Chironomidae and Oligochaeta are commonly found in depositional <br />areas near shore (Carter, et al. 1982), <br /> <br />I <br />I <br />I <br />I <br />,I <br />II <br />I <br />I <br /> <br />The periphyton of the channelized Missouri River is dominated by a combination of <br />diatoms, green algae, and blue-green algae, Bacillariophyta, Chlorophyta, and Cyanophyta are <br />dominant forms of periphyton in the river (Farrell and Tesar 1982), Seasonal patterns of <br />zooplankton abundance were measured by Repsys and Rogers (1982) in the vicinity of Fort <br />Calhoun and Cooper Nuclear Stations. Fort Calhoun Nuclear Station is 90 river miles north of <br />the project site and Cooper Nuclear Station is 24 river miles south of the site. Extensive studies <br />of river biota have been conducted throughout this stretch of the Missouri River to evaluate the <br />effects of the two nuclear stations. They found that the populations were characterized by <br />relatively high microcrustacean densities from late fall to spring, with reduced populations <br />occurring during summer and early autumn. Most of the zooplankton present in this lower <br />portion of the river originate in the mainstem reservoirs located in the upper portions of the <br />Missouri River. <br /> <br />g. Terrestrial/Wetland Resources: The following information was obtained through <br />interpretation of aerial photographs taken in March 1994, The information was verified and <br />enhanced through a field investigation, <br /> <br />11 <br />