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<br />I <br />I <br /> <br />monitoring and research. Areas that are enhanced/restored should be <br />thoroughly evaluated to determine the responses of the endangered and <br />nonnative fishes to such efforts and refinements made as necessary to <br />achieve desired Recovery Program goals and objectives. Enhanced areas <br />will either have to be large enough or numerous enough to ensure that <br />responses by fishes can be detected. <br /> <br />I <br /> <br />I <br />I <br />I <br /> <br />I <br /> <br />Larval and juvenile razorback suckers apparently require inundated <br />floodplains to grow and survive (Mueller 1995; Mueller et al. 1993; Tyus <br />and Karp 1989, 1990, 1991). Rapid growth of razorback sucker juveniles <br />in off-channel habitats was reported by Osmundson and Kaeding (1989) and <br />Mueller et al. (1993). Reconnecting floodplain habitats with rivers in <br />the Upper Colorado River Basin is expected to benefit razorback suckers <br />most since these habitats will provide an adequate quantity of food of <br />the right size and at the right time for survival of larval razorback <br />suckers during their critical period. Larvae and juveniles of other <br />native fishes including the three other endangered species (Colorado <br />squawfish, humpback chub, and bony tail) will also benefit from floodplain <br />production of zooplankton and benthic invertebrates that enter the river <br />when streamflows subside after spring flooding, enhancing the <br />productivity of the main channel and backwaters of Upper Basin rivers. <br /> <br />I <br /> <br />Adult razorback suckers are flexible in their use of habitats. Although <br />this species evolved in large riverine systems, adults have survived well <br />in both lacustrine (Wallis 1951, Marsh and Langhorst 1988, Minckley et <br />al. 1991) and lotic (Miller et al. 1982; Tyus 1987) habitats. During <br />high spring runoff, adult razorback suckers in the Upper Colorado River <br />Basin congregated in large eddies at the mouths of rivers, off-channel <br />ponds that have a connection to the rivers, and wetlands in floodplain <br />areas (McAda and Wydoski 1980; Modde 1997; Tyus and Karp 1990; Valdez and <br />Wick 1983). The use of low velocity habitats by adult razorbacks may be <br />to escape the high velocities associated with the spring runoff and <br />possibly to feed after spawning to regain their body condition. <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />Razorback suckers spawn annually on clean cobble and gravel in rivers <br />(Tyus and Karp 1990; Wick and Cluer 1998) and on the wave-swept rubble <br />shoreline of Lake Mohave (Minckley et al. 1991). It is possible that <br />floodplain habitats may have been used more extensively for spawning in <br />the past by razorback suckers (Osmundson and Kaeding 1989) when they had <br />access to them and riverine conditions were unsuitable as suggested by <br />Sparks (1995) for other riverine fish species. <br /> <br />I <br /> <br />Breachinq Levees. Removal of levees that are located on the lowest <br />floodplain terraces (public property or acquired private property) is the <br />most practical way to reconnect mainstem and tributary rivers with <br />productive floodplain habitats using present streamflows. Such removal <br />should be done on properties that can be easily reconnected with the main <br />channel where thorough evaluations can be made of zooplankton/benthic <br />invertebrate production and responses by native and nonnative fish <br />species. <br /> <br />I <br /> <br />I <br /> <br />Ideally, reconnect ion of floodplain habitats with main river channels <br />should simulate natural conditions where possible and be relatively <br />maintenance free. <br /> <br />I <br />I <br /> <br />Floodolain Terraces. Existing floodplain terraces were deposited by high <br />peak streamflows that occurred before high dams were constructed and the <br />streamflows were regulated (i.e., peak streamflows that resulted in <br />inundation, scouring, and deposition of floodplains were lost). Existing <br />streamflow conditions may not permit annual inundation of the floodplain <br />by simply removing levees. It may be necessary to excavate existing <br />terraces so that present streamflow regimes can inundate floodplains <br /> <br />) <br /> <br />31 <br /> <br />I <br />