<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 />
|