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<br />BIOLOGY OF YOUNG COLORADO SQUA WFISH <br /> <br />87 <br /> <br />backwater temperatures were higher than the 21- <br />260C temperature range in which the hatchery fish <br />were raised, and we expected Green River fish to <br />grow faster. However, otoliths from 14 postlarvae <br />collected in 1987 (mean, 38.2 mm T1.; range, 29- <br />45 mm) indicated that otolith-aged fish averaged <br />about 13 d older than ages calculated from labo- <br />ratory fish of the same size (R. Muth, Colorado <br />State University, personal communication). This <br />could be the result of slower growth by the wild <br />fish, inadequate sample size, or invalid otolith ag- <br />ing. However, growth equations for post1arvae <br />should be further validated or refined by aging <br />wild fish of different sizes before the equations are <br />applied to management of this endangered fish. <br /> <br />Habitat Use <br /> <br />The timing of spawning, and thus of hatching, <br />is critical to larval survival. Spawning occurred <br />during the period of declining flows and increasing <br />temperatures after spring peak runofl: This tem- <br />poral adaptation (midsummer spawning associ- <br />ated with declining flows) is associated with the <br />reproductive biology of the species (Tyus 1986), <br />whereby the length of exposure of eggs and larvae <br />to cold temperatures of spring and to predation is <br />reduced. It is perhaps critical that rapid growth is <br />attained during the remaining short growth peri- <br />od, and that the larvae are transported into suit- <br />able feeding areas before their yolk supplies are <br />depleted. Backwaters used by the young fish as <br />nursery habitats were created by gradually de- <br />creasing summer flows after spring runoff (snow- <br />melt). <br /> <br />Growth and Survival <br /> <br />We expected greater growth of age-O fish in the <br />lower Green River because the watler was 40C <br />warmer than in the upper river. However, we found <br />that age-O fish in the upper Green River were the <br />same average annual size as, or were larger than, <br />in the lower area. We assumed that other envi- <br />ronmental factors (e.g., habitat availability and <br />food abundance) may influence growth more in <br />the Green River, at least in some years, than water <br />temperatures alone. One plausible explanation is <br />a difference in available habitat; annual sampling <br />records indicated that there were about 150% more <br />backwaters per kilometer in the upper than in the <br />lower Green River. Backwaters in the lower Green <br />River may yield a higher catch of young Colorado <br />squawfish than in the upper Green River (Figure <br />2) and greater numbers may have resulted in less <br />growth. Reduced growth at lower temperatures, as <br /> <br />hypothesized by Kaeding and Osmundson (1988), <br />was not detected in our study. <br />Reduced abundance and growth of age-O fish in <br />1983 and 1984 were attributed to abnormally high <br />summer flows from Flaming Gorge Dam. We were <br />initially concerned that higher flows might have <br />reduced our success in catching young fish in 1983 <br />and 1984, and thus biased our results. However, <br />spring sampling in 1984 produced few age-l Col- <br />orado squawfish, indicating that the reduced <br />standing crops of age-O fish recorded the previous <br />autumn was accurate. However, low catches in <br />autumn 1985 and 1987 may reflect sampling bias. <br />Spring sampling produced more young in 1986 <br />than in the preceding autumn for the upper and <br />lower Green River, and more young were cap- <br />tured in the lower river in spring 1988 than in the <br />preceding autumn. <br />Although it was impractical to count all back- <br />waters in the Green River by boat because of the <br />width of the river and limited personnel, we ob- <br />served fewer backwaters during high-flow years <br />(1982, 1983, and 1984) than during low- and av- <br />erage-flow years (1979-1981, 1987-1988). These <br />riverwide observations were similar to those not- <br />ed in a Bureau of Reclamation study conducted <br />during 1986-1988 on four reaches of the Green <br />River. Aerial photographic mapping of shoreline <br />habitats at different water levels revealed that <br />backwaters were reduced in area when flows in <br />the Green River increased above average historic <br />summer flows (M. Pucherelli, U.S. Bureau of Rec- <br />lamation, personal communication). <br />We were unable to assess overwintering mor- <br />tality of young Colorado squawfish adequately. <br />Catches of age-1 fish in the spring (fish/lOO m2) <br />were greater in half of our samples than catches <br />of the same cohort the previous autumn. We as- <br />sume that differences in habitats or in habitat use <br />made the fish more vulnerable to capture with <br />seines in the spring than the preceding autumn, at <br />least during some years. Management and future <br />recovery of the Colorado squawfish may require <br />development of a better method for assessing re- <br />cruitment during the early life stages if recruit- <br />ment failure is determined to be a problem in the <br />Green River. <br />Age-1 fish were generally larger in the spring <br />(mean, 45.2 mm) than in the previous autumn <br />(42.3 mm), presumably a result of growth or a <br />size-selective mortality. Thompson (1989) ob- <br />served that age-O fish actively fed and survived in <br />laboratory aquaria under simulated winter con- <br />ditions (3-40C, 210 d), but they grew very little. <br />