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<br /> <br />BIOLOGY OF YOUNG COLORADO SQUA WFISH <br /> <br />81 <br /> <br />mg the river into 8-km reaches <br />t two backwaters in each reach. <br />and 1986-1988 was expanded <br />at weekly intervals during July <br />Yampa Canyon and Gray Can- <br />. Seine samples were taken with <br />eep seine with 0.63-mm2 mesh. <br />i conducted about 25 km below <br />sites in June and July 1986- <br />)a River near the confluence of <br />,reen rivers, and in the Green <br />, below Gray Canyon (Figure I). <br />IS were about 4 m in length and <br />penings of 0.5 x 0.3 m. Each <br />i in the river channel by attach- <br />:e posts. Nets were set for about <br />It 0600, 1200, 1800, and 2400 <br />city was recorded at each loca- <br />period with a Marsh-McBirney <br />11 meter. <br />preserved in 5% buffered for- <br />d sent to the Larval Fish Lab- <br />do State University, Fort Col- <br />. identification. <br />'ctions. - Postlarval Colorado <br />nm TL) were sampled with 5-m- <br />seines of 3.2 x 4.8-mm woven <br />r and October 1979-1985, and <br />I-m-deep seines in 1987-1988 <br />atic sampling design. A stratum <br />.ndom and the first two back- <br />d in each 8-km reach of that <br />led. Sampling then proceeded <br />:h of the remaining 8-km reach- <br />,wfish were counted and mea- <br />:st millimeter total length. All <br />"ere counted and placed in 10- <br />. The area seined, depth of wa- <br />~K) of each backwater sampled <br />1979-1981, runs, eddies, side <br />'eline habitats were also seined. <br />I as stretches of the main chan- <br />vely deep and fast with laminar <br />oortions of the stream with dis- <br />ItS and were usually deeper than <br />leI. A side channel was defined <br />:1 in a braided river section that <br />e flow during high water. A <br />:onsisted of shallow water next <br /> <br />to shore. Backwaters were defined as shallow <br />ephemeral embayments adjacent to the main river <br />channel with no measurable water velocity. <br />Maximum depth of each backwater was mea- <br />sured and surface temperature was recorded at that <br />point. The dominant substrate was classified as <br />silt (< I mm in diameter), sand (1-3 mm), gravel <br />(3-75 mm), cobble (76-305 mm), and boulder <br />(> 305 mm). In 1988, backwaters were classified <br />as clear (bottom visible throughout), turbid (bot- <br />tom not visible), and partly turbid (clear at ter- <br />minal end, turbid at mouth). Backwaters were also <br />sampled in spring (March 30-May 10) 1984, and <br />each spring in 1986-1989 to evaluate overwinter <br />survival. Spring sampling began soon after river <br />ice began to break up, and this was usually the <br />first part of April. Spring sampling was confined <br />to river reaches known to contain Colorado <br />squawfish (i.e., F, E and B, A) and done with the <br />same procedures used in the previous autumn. <br />Data analysis. - Larval hatching dates were es- <br />timated by back-calculation from total length at <br />capture by use of equations developed by Haynes <br />et al. (1984) and modified by Nesler et al. (1988). <br />For Y = number of days after hatching, <br /> <br />Y = -76.71 + 17.49 TL - 1.056 TU <br />+ 0.0221 TL3 (for TL < 22 mm); <br />Y= -26.64 + 2.78 TL (for 22 < TL <br />< 47 mm). <br /> <br />(fish/I 00 m2) of young Colorado squawfish in riv- <br />er reaches sampled in the autumn of 1983, 1985, <br />1987, and 1989 into the catch in those reaches the <br />following spring. In each evaluation, the upper <br />Green River strata (E and F) were evaluated sep- <br />arately from the lower strata (A and B), so that <br />two comparisons were made for each year. <br />Differences in mean total length of Colorado <br />squawfish between the lower and upper Green <br />River and between autumn and spring samples <br />were tested with independent t-tests, with unequal <br />variances. Standard regression techniques were <br />used to determine the relationships between fish <br />abundance (Io&,fish/ I 00 m2), size (total length), <br />and late-summer (August and September) stream- <br />flow. Independent t-tests and G-tests of indepen- <br />dence (Sokal and Rohlf 1981) were used to eval- <br />uate the relationship between environmental <br />conditions (backwater temperatures, depths, and <br />sizes; substrate; turbidity) and the presence (at least <br />one fish captured) or absence of Colorado squaw- <br />fish. <br /> <br /> <br />Results <br /> <br />Distribution <br /> <br />Altogether, 11,379 age-O Colorado squawfish <br />were captured in the lower Yampa and Green riv- <br />er study area: 60 I in drift nets in June and July; <br />3,079 in seines in July and August; 6,459 in seines <br />in September and October; and 1,240 in seines in <br />April (Table I). <br />No Colorado squawfish larvae were found in the <br />Green River above its confluence with the Yampa <br />River (RK 552-584) or in the lower 225 km of <br />the White River. Larvae were present from RK <br />29 on the Yampa River downstream to the lower <br />boundary of our study area at RK 35 on the Green <br />River. When all years were combined, the average <br />July-August seine catch showed two areas of post- <br />larval abundance that were about 130 km down- <br />stream of the spawning areas: one downstream of <br />the Yampa River, but upstream of Gray Canyon <br />(i.e., near RK 448), the other downstream of the <br />Gray Canyon spawning area (i.e., near RK 112; <br />Figure 2). Within-year seining also demonstrated <br />this pattern, but catches varied among years in <br />both the upper and lower Green River strata (Ta- <br />ble 1). <br />Hatching of Colorado squawfish was associated <br />with declining water levels and rising water tem- <br />peratures after the peak spring runoff, and lasted <br />2--6 weeks (Table 2). Fish captured in the Yampa <br />and upper Green rivers hatched about 54.0 d <br /> <br />Equations were derived from hatchery-reared <br />progeny of parents collected from the upper Col- <br />orado River basin (Hamman 1981). Colorado <br />squawfish fry were raised at Willow Beach Na- <br />tional Fish Hatchery (Arizona) for 107 d at tem- <br />peratures of 21-260C. We reported annual hatch- <br />ing dates as means and as ranges that included <br />90% of fish-hatching dates each year (i.e., dates <br />read from a cumulative frequency distribution at <br />5% and 95%). Age-O fish captured above Gray <br />Canyon (RK 256) were judged to have hatched in <br />the Yampa River and fish captured below RK 256 <br />presumably hatched in the Yampa and Green riv- <br />ers. Hatching dates of larval Colorado squawfish <br />were compared with streamflows by use of U.S. <br />Geological Survey water resources data from gag- <br />ing stations at Deerlodge, Colorado, and the town <br />of Green River, Utah (Figure 1). Water temper- <br />atures during the hatching period in the Green <br />River were obtained from the Green River gaging <br />station. No temperature records were available for <br />the Yampa River spawning area. <br />An evaluation of relative overwinter survival of <br />age-O fish was calculated by dividing the seine catch <br /> <br /> <br />: names does not indicate endorse- <br />products by the Fish and Wildlife <br />