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? <br />GENERAL IlnRODUCTIm <br />The razorback sucker, X auchen texarnas (Abbott), a native of the <br />Colorado River system of western North America, once ranged from <br />W arcing to the Gulf of California. Development of the Colorado River <br />and its major tributaries for water and power have greatly impacted <br />and reduced razorback sucker populations. <br />Minckley (1983) t oroughly reviewed the historical distribution <br />of this species and documented its demise in the lower Colorado River <br />basin. He suggested that localized extirpations followed a pattern <br />whereby only large individuals can be found in the reservoirs in the <br />years following impatuxhnent. while larval razorbacks may be <br />collected, juveniles are almost never found. After a time, these <br />populations of large, old fish dwindle and disappear (as did those in <br />the Salt River reservoirs, Roosevelt and Saguaro lakes), or became <br />severely reduced (as in Lakes Mead and Havasu on the mainstem Colorado <br />River) (Minddey 1973, 1983). In Lake Mohave, Arizona Nevada, the <br />last reservoir constructed on the lower Colorado River mainstem, <br />remains the only sizable population of adult razorback sucker <br />(Minckley 1983). It is estimated from aging data that these fish <br />hatched in the early 1950s, about the time the reservoir was filling <br />(McCarthy and MinckleY 1987). Each January through March, razorback <br />suckers may be observed moving' onto gravelly shoals to spawn (Minckley <br />1973). Larvae can be captured in February through Apri.l? but, <br />curiously, none larger than about 12.0 mm TL has ever been taken <br />_, (Marsh and Lwighorst 1988).