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<br />28 <br /> <br />this greater mass of cold water must have remained cooler further down <br />the river because ambient conditions were not able to raise the water <br />temperature nearly as fast as it had during the low release period of <br />1963-1966. Therefore, squawfish reproduction in Dinosaur National <br />Monument was reduced in about 1967 or 1968 because the Yampa River <br />could no longer ameliorate the cold inflow of the Green River. Col- <br />lections of young squawfish the past few years suggest the river does <br />not return to a normal temperature pattern until it reaches the Jensen <br />area. <br /> <br />Additional data could be presented to indicate Colorado squawfish <br />reproductive success in portions of the Upper Colorado basin. Unfortu- <br />nately no other areas than the two discussed above have more than one <br />or two years of data. Holden (1973) found young-of-the-year squawfish <br />to be quite common in the lower Green River in Canyonlands National <br />Park in 1970 and 1971. He also found yearlings to be quite common be- <br />tween Ouray and Gray Canyon as well as a few young-of-the-year in 1971. <br />These data would suggest that squawfish did spawn successfully in much <br />of the Green River in 1970 and 1971, years of normal flow patterns <br />(Figures 14 and 15). <br />As mentioned earlier, Holden (1977) sampled the Jensen-Ouray area <br />in August, 1977, and also continued downstream to Green River, Utah, in <br />September. Young-of-the-year squawfish were not found in 1977 between <br />Ouray and Gray Canyon, but were found at a point about 25 miles upstream <br />from Green River. This data reinforces the conclusion that 1977 was a <br />very poor year for Colorado squawfish reproductive success in the Green <br />River, at least above Gray Canyon (Figure 16). <br />