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persist in areas scattered throughout the basin where cold, hypolimnetic water is discharged <br />from reservoirs (Vanicek, 1967; Vanicek and Franklin, 1970; Kaeding and Zimmerman, 1983; <br />Holden, 1990). Even when natural conditions are considered, today's upstream distribution <br />for these fishes in the upper basin is temperature-limited (in part, Kaeding and Osmundson, <br />1990). Water in these areas rarely achieves 20°C for any length of time in the summer, <br />resulting in spawning a considerable distance downstream from their upstream distributional <br />limits. <br />Conditions for reproduction and survival are almost certainly less optimal .for peripheral <br />populations than central ones, resulting in smaller effective population sizes toward the <br />periphery. If the Lake Mohave region is neazer the focal point of the razorback's recent <br />geographical distribution, upper basin populations are peripheral (as was similarly <br />hypothesized for Colorado squawfish by Kaeding and Osmundson [1990)). Because genetic <br />drift eliminates- variation more rapidly in smaller populations, those in the upper basin would <br />be expected to exhibit fewer variants than more central ones. Since these populations are <br />connected by considerable gene flow, the more common haplotypes in larger populations at <br />the center of the range would eventually achieve the highest frequencies in peripheral areas. <br />Available information is consistent with tl~e recolonization scenario outlined above. Lt <br />addition to the progressive decline in diversity in populations further upstream, two of the <br />more common haplotypes of Lake Mohave (e.g., ABADA'AAA, ACDCFBAB) become even <br />more frequent in the upstream Lake Powell and Green River sample, with the most common <br />haplotype (i.e., ABADA'AAA) fixed in our upper Colorado River sample. Known patterns of <br />abundance indicate a cline in population size, as razorbacks appear to have been more <br />numerous historically in the lower basin (Minckley et al., 1991); however, it is impossible to <br />determine with available data if the system has achieved equilibrium. <br />14 <br />