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<br />a <br /><:) <br />(~ <br />j'\) <br />CJl <br />~ <br /> <br />Mr. Calvin Joyner <br /> <br />12 <br /> <br />from some localities, coupled with the species' continued decline in numbers <br />and distribution, has prompted some research; however, details of its life <br />history requirements, particularly in riverine environments, are still not <br />fully understood. <br /> <br />In general, a natural hydrograph with a large spring peak, a gradually <br />descending limb into early summer, and low stable flows through summer, fall, <br />and winter are thought to create the best habitat conditions for razorback <br />suckers. Prior to construction of large main stem dams and the suppression of <br />spring peak flows, low velocity, off-channel habitats (seasonally flooded <br />bottomlands and shorelines) were commonly available throughout the Upper Basin <br />(Tyus and Karp 1989; Osmundson and Kaeding 1991). The absence of these <br />seasonally flooded riverine habitats is believed to be a limiting factor in <br />the successful recruitment of razorback suckers in their native environment <br />(Tyus and Karp 1989; Osmundson and Kaeding 1991). Tyus (1987) and McAda and <br />Wydoski (1980) reported springtime aggregations of razorback suckers in <br />off-channel impoundments and tributaries; such aggregations are believed to be <br />associated with reproductive activities. Tyus and Karp (1990) and Osmundson <br />and Kaeding (1991) reported off-channel habitats to be much warmer than the <br />main stem river and that razorback suckers presumably moved to these areas for <br />feeding, resting, sexual maturation, spawning, and other activities associated <br />with their reproductive cycle. While razorback suckers have never been <br />directly observed spawning in turbid riverine environments within the Upper <br />Basin, captures of ripe specimens, both males and females, have been recorded <br />(Valdez et al. 1982; McAda and Wydoski 1980; Tyus 1987; Osmundson and Kaeding <br />1989; Tyus and Karp 1989; Tyus and Karp 1990; Platania 1990; Osmundson and <br />Kaeding 1991) in the Yampa, Green, Colorado, and San Juan Rivers. Sexually <br />mature razorback suckers are generally collected on the ascending limb of the <br />hydrograph from mid-April through June and are associated with coarse gravel <br />substrates (depending on the specific location). <br /> <br />Outside of the spawning season, adult razorback suckers occupy a variety of <br />shoreline and main channel habitats including slow runs, shallow to deep <br />pools, backwaters, eddies, and other relatively slow velocity areas associated <br />with sand substrates (Tyus 1987; Tyus and Karp 1989; Osmundson and Kaeding <br />1989; Valdez and Masslich 1989; Tyus and Karp 1990; Osmundson and Kaeding <br />1991). <br /> <br />The virtual absence of any recruitment suggests a combination of biological, <br />physical, and/or chemical factors that may be affecting the survival and <br />recruitment of early life stages of razorback suckers. Within the Upper <br />Basin, recovery efforts endorsed by the "Recovery Implementation Program for <br />Endangered Fish Species in the Upper Colorado River" (U.S. Fish and Wildlife <br />Service 1987), include the capture and removal of razorback suckers from all <br />known locations for genetic analyses and development of discrete brood stocks <br />if necessary. These measures have been undertaken to develop refugia <br />populations of razorback sucker from the same genetic parentage as their wild <br />counterparts such that, if these fish are genetically unique by subbasin or <br />individual population, then separate stocks will be available for future <br />augmentation. Such augmentation may be a necessary step to prevent the <br />extinction of razorback suckers in the Upper Basin. <br />