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Eastman (1977, 1980) described the pharyngeal bones, teeth, <br />and caudal skeleton of the razorback sucker. Like most other <br />catostomid genera, Xvrauchen is characterized by an intermediate <br />number of moderately compressed pharyngeal teeth arranged in a <br />comb-like fashion, presumably an adaption benthic feeding <br />(Eastman 1977). The razorback sucker caudal skeleton is <br />relatively heavily ossified, and caudal rays are thickened and <br />foreshortened. Eastman (1980) presumed that these features were <br />adaptions to the strong currents present in rivers occupied by <br />this species. <br />No studies have been attempted to determine if intraspecific <br />variation occurred in the formerly extensive geographic range of <br />the razorback sucker. A qualitative comparison of the few <br />meristic data presented by Hubbs and Miller (1953) indicated that <br />Upper Colorado River and Gila River specimens were similar. <br />DIBTRIHIITION AND BTATIIB <br />The 1922 Colorado River Compact divided the Colorado River <br />Basin into upper (UCRB} and lower (LCRB) portions (Fig. 1) at Lee <br />Ferry, Arizona (review by Carlson and Muth 1989). This provides <br />a convenient point of division for discussion of status and <br />biology of the razorback sucker. <br />6 <br />