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<br />irrigation canals and ponds below Parker Dam (Minckley et al. 1991), providing little optimism <br />for development of self-sustaining populations. The majority of floodplain habitat in the <br />Colorado River has been lost by inundation within reservoirs, channelization, or reductions in <br />spring flood flows (Minckley and Deacon 1968, Carlson and Muth 1989) resulting in recruitment <br />failure and decline of existing populations through attrition (Minckley 1983). Conversely, the <br />Middle Green River retains much of its floodplain habitat (Irving and Burdick 1994) even though <br />inundation is reduced from predam conditions (Flo Engineering 1996). Wick et al. (1982) stated <br />that recovery of the razorback sucker will be dependent on identifying impediments to <br />recruitment. The growth and survival of age-O razorback sucker in Old Charley Wash suggested <br />that reproductive success and recruitment of this species is possible if suitable habitat is ' <br />provided, despite the presence of large numbers of predacious and competitive nonnative fishes. <br />Thus, if historical nursery habitat can be provided for razorback sucker, predation by nonnative <br />fishes will be a secondary rather than a prevalent force impacting extirpation of the species <br />(Minckley 1983). <br /> <br />Conclusions and Management Recommendations <br /> <br />The greatest number of adult razorback sucker captured in the Upper Colorado River <br />have been collected in floodplain/low gradient reaches of rivers. In addition, the greatest number <br />of juvenile and subadult razorback have been collected in floodplain wetlands within these same <br />low gradient reaches. During high flow years of this study, larval razorback sucker captured in <br />the main channel were coincident with peak zooplankton densities and favorable temperatures <br />for growth in Old Charley Wash (and presumably other inundated floodplains). Therefore, <br />floodplain habitat represents the best nursery environment available in the Middle Green River <br />when larval razorback sucker appear. Favorable water quality and quantity and prey densities <br />were available to support age-O fish in Old Charley Wash through the summer months. In two <br />successive high flow years, razorback sucker used a floodplain wetland and some survived in an <br />environment dominated by nonnative predators and competitors. If the number of razorback <br />sucker juveniles captured in Old Charley Wash was extrapolated to the area of depression <br />wetlands available (Stewart Lake, Sportsman Lake, Leota Bottoms, Johnson Bottoms, and <br />Wyasket Lake) in the Middle Green River, a minimum of 362 and 582 wild, acclimated age-O <br />fish 75-125 mm long would have been produced in the Middle Green River system in 1995 and <br />1996, respectively. <br />However, during both high flow years of the study, larval razorback sucker were collected <br />in the main channel for at least two weeks after Old Charley Wash was disconnected from the <br />Green River. Therefore if higher flows (447 m3/s) were extended another two to three weeks, <br />larval razorback sucker in the main channel would have had a greater opportunity to access <br />floodplain/wetland habitats. Historically, the Green River at Jensen peaked after the Yampa <br />River (28 May, versus 21 May, U.S. Bureau of Reclamation, unpublished data) and provided <br />longer duration of higher flows prior to the construction of Flaming Gorge Dam. Currently, the <br />flows from the Yampa River alone did not maintain floodplain inundation long enough to <br />provide floodplain access for all razorback sucker in the river. <br />An alternative to the use of depression floodplains (i.e., floodplains that maintain water <br />after river flows recede) is to breach levees and manage them as terrace floodplains (i.e., <br />floodplains that dewater as river flows recede) that would reduce reproductive success of <br /> <br />44 <br />