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<br />198 <br /> <br />et al. 1970, Kaeding & Osmundson 1988, Tyus & <br />Haines 1991). <br />Several hypotheses have been forwarded regard- <br />ing mechanisms which control recruitment of fishes <br />early in life (Houde 1987). Starvation, presence and <br />duration hf a critical period during ontogeny, and <br />biotic interactions such as competition and preda- <br />tion may all affect survival of larvae. Outcomes of <br />these processes often depend on size and growth <br />rates of larvae, which may in turn be affected by en- <br />vironmental factors such as water temperature, <br />temperature fluctuations, and food abundance <br />(Houde 1987, Weatherly & Gill 1987, Miller et al. <br />1988). Understanding effects of these environmen- <br />tal factors on growth, survival, and starvation resist- <br />ance may be essential in evaluating the complexity <br />of mechanisms that control recruitment of Colora- <br />do squawfish in the wild. <br />Research on fishes in the upper Colorado River <br />Basin has emphasized effects of altered flow re- <br />gimes on distribution and abundance of endan- <br />gered fishes such as Colorado squawfish (Tyus & <br />Karp 1989, Tyus & Haines 1991). However, few in- <br />ferences can be made about direct effects of tem- <br />perature, habitat availability, and food abundance <br />on growth, survival, and starvation resistance of <br />Colorado squawfish larvae because scant empirical <br />laboratory or field data are available that describe <br />their ecology. Black & Bulkley (1985) studied ef- <br />fects of constant 15, 20, 25 and 300 C temperatures <br />on growth of yearling Colorado squawfish and <br />found fastest growth at 250 C when provided with <br />unlimited food. However, food availability may <br />vary and not always be unlimited in fluctuating riv- <br />erine backwaters of the Colorado River Basin and <br />optimal growth conditions for larvae may be differ- <br />ent than for yearlings. I conducted laboratory stud- <br />ies to determine growth and survival of larvae in <br />constant and fluctuating temperature regimes at <br />several different temperature and food abundance <br />levels. Because food abundance may be seasonally <br />low in the turbid and fluctuating habitat of the Col- <br />orado River Basin, starvation resistance of Colora- <br />do squawfish larvae was also examined. <br /> <br />Methods <br /> <br />Growth and survival experiments <br /> <br />Colorado squawfish embryos were obtained from <br />Dexter National Fish Hatchery and Technology <br />Center, Dexter, New Mexico (Hamman 1981). Em- <br />bryos were from paired matings of 20 broodfish of <br />each sex (R. Hamman personal communication). <br />Test animals were held in 2.01 aquaria (20 cm x <br />10 cm x 12.5 cm deep). Flow-through conditions in <br />each aquarium maintained dissolved oxygen at <br />5-6 mg 1-\ and prevented accumulation of waste <br />products. Photoperiod was 14 h lightlO h dark. <br />Healthy, two-day old embryos after hatching <br />were randomly selected and counted into groups of <br />20, randomly assigned to one of seven experimental <br />treatments, placed in aquaria, and acclimated to <br />test temperatures at a rate of about 20 C h-1. These <br />free embryos and later larvae were subjected to <br />fluctuating or constant temperatures (hereafter <br />called regimes), with nominal constant temper- <br />atures of 18,22,26, or 300 C and nominal fluctuating <br />temperatures of 18, 22, or 260 C (diel fluctuation of <br />:t 2.50 C, 50 C total). Embryos hatched in 1991 were <br />used for the 18, 22, and 260 C fluctuating and 220 C <br />constant-temperature-treatment experiments, and <br />1992 embryos were used for the 18, 26, and 300 C <br />constant and a second 220 C constant-temperature- <br />treatment experiments. <br />Fluctuating temperatures were tested because <br />diel temperature fluctuations of 50 C or more are <br />common in the Yampa and Green rivers in Colora- <br />do and Utah during late June through August (Nes- <br />ler et al. 1988, United States Geological Survey re- <br />cords, published annually). The fluctuating temper- <br />ature cycle mimicked the natural cycle as follows: <br />lowest temperatures occurred from 1:00 to 7:00 h <br />(e.g., 19.50 C for the 220 C fluctuating treatment); <br />warming occurred at a constant rate from 7:00 to <br />13:00 h; temperatures were highest from 13:00 to <br />19:00 h (e.g., 24.50 C for the 220 C fluctuating treat- <br />ment); and cooling occurred at a constant rate from <br />19:00 to 1:00 h. Observed mean water temperatures <br />(SE) in the constant and diel fluctuating regimes <br />were as follows: constant nominal 180 C = 18.2 <br />(0.07), 220 C = 21.95 (0.05), 260 C = 26.0 (0.02), and <br /> <br />~' <br /> <br />.. <br />