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<br />October 1986 <br /> <br />TYUS: COLORADO SQU A WFISH <br /> <br />657 <br /> <br /> <br />r\- ---1 <br />J II lOIUOI) I <br />I j <br />L__ __.____J <br /> <br />UTAH <br /> <br />ft_..,.Oi, <br /> <br />Fig. 1. Upper Colorado River Basin and Green River study area (shaded). <br /> <br />~ <br /> <br />occurred in Ptychocheilu8 by the mid- <br />Pliocene (Miller 1961). Nonetheless, the <br />largest Ptychocheilu8 reported in the fossil <br />record lived in Pliocene Lake Idaho (Smith <br />1975), indicating that Ptychocheilu8 success- <br />fully utilized both riverine and lacustrine sys- <br />tems. <br />The Southwestern United States is more <br />arid today than in the Late Cenozoic, and this <br />increasing aridity no doubt resulted in the loss <br />or reduction of lacustrine habitats and the <br />extinction oflake dwelling salmonids and cen- <br /> <br />trarchids from the Colorado River system. <br />This change was progressive from the <br />Pliocene, when a system of lakes covered the <br />lower and upper Colorado River Basins, and <br />persisted during pluvial periods until the <br />Pleistocene. During this epoch the life history <br />of fishes was remarkably impacted by such <br />long pluvial periods interrupted by short peri- <br />ods of desert conditions (G. Smith 1981). <br />An evaluation of the fish fauna of the Colo- <br />rado River in recent times (before introduc- <br />tions by man) might lead one to conclude that <br />