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<br />reservoirs, coves can provide warm, shallow shorelines suitable for nursery habitat <br />Minckle et al. 19 1 <br />( y 9 ). <br />~, Movement and Migrations <br />' Historical accounts document spring spawning movements of razorback suckers in <br />r various locations in the basin (Jordan 1891, Hubbs and Miller 1953, Sigler and Miller <br />. 1963). Spawning migrations and other movements presumably evolved in the context <br />of flow regimes, pluvial events, and the diversity of available habitats (Smith 1981; <br />Tyus 1986, 1987; Tyus and Karp 1989, 1990). Similar spawning migrations have been <br />studied for other riverine catostomids and appear to be a major part of their <br />reproductive ecology (Dance 1948, Breder and Rosen 1966, Wemer 1979). The <br />facl;ors controlling migratory behavior in the razorback sucker have not been studied <br />but there is some evidence that imprinting may have an influence (Scholz et al. 1992, <br />Mocide et al. 1995). <br />Razorback suckers may travel long distances in both lacustrine and riverine <br />environments during the spawning season. In Lake Mohave, razorback suckers move <br />throughout the lake, which is about 100 km long (Marsh and Minckley 1989). Spawning <br />migrations of 30 to 106 km (one way) have been recorded in the Green River near <br />Jensen, Utah, and in the lower Yampa River in Dinosaur National Monument (Tyus <br />198'7, Tyus and Karp 1990). <br />' 19 <br /> <br />