• 1
<br />69
<br />suggestions that multiple spawning may occur to a certain extent, on the same
<br />sites (Jones and Sumner 1954; Linda Ulmer, pres. comm.). The same spawning
<br />areas were used for 2 consecutive years at SWR. Relative fecundity, based on a
<br />small sample size, was estimated at 27,000-144,00 eggs per female with a poor correla-
<br />tion between the number of eggs and the units of female body length (McAda and
<br />Wydoski, 1980; Minckley, 1981 in press). There are suggestions that viability
<br />decreases in older females, but a good sequence of gonads from aged individuals
<br />or a reliable aging technique has not been available. Eggs are mildlyadhesive to
<br />the substrate (Moyle, 1976; Minckley, 1973) and range in size from 1.8 to 3.2 mm in
<br />diameter (Gustafson, 1975; Calif. Fish and Game, unpublished data). Time to
<br />hatching is variable, but appears to decrease as temperatures increase. Culture
<br />experiments at Willow Beach National Fish Hatchery indicated poor survival occurs
<br />when incubation temperatures are near 12°C (Toney, 1974). At Dexter National Fish
<br />Hatchery 14-16°C incubation temperatures resulted in 10-20% survival, but many other
<br />factors besides water temperature may explain the low survival (Inslee, 1981).
<br />We removed 100 eggs from spawning areas at Senator Wash Reservoir (SWR) and incu-
<br />bated them in aquaria at 20-23.50C and had 46% survival (Loudermilk et al., 1981, unUU-
<br />blished manuscript).. Experiments at Utah State University using sub-adult fish (1974
<br />fereni d:
<br />C OIL-Lort frviaa i„ t' _ ch" H stock' 'w thL' n-ai -refci. °ia:.e -.ia, -ci di?ccu tee „rrE'- s
<br />i. 1i0?+ if''
<br />a .,o?.++ j om. rcaTaa?l.S` indicated of 25.4°C were chosen (Bulkey, et al. 1981). Within four years after the closure of
<br />Flaming Gorge Dam, native fish of all ages, including razorbacks, were displaced for
<br />7 miles downstream, their abundance was reduced for many miles further downstream,
<br />and cold hypolimnetic releases were suggested as the major cause (Vanicek, 1967;
<br />Vanicek et al. 1970; Holden, 1973).
<br />Very little is known about the larval stage of this species other than identi-
<br />fication characters of the post larvae (Winn and Miller, 1954). For 2-3 days after
<br />swim-up, post larvae in aquaria used the upper 1/3 of the water column and displayed
<br />little tendency to seek shelter. If in a mild current, they would have been carried
<br />downstream. After this period they began moving to the bottom and gradually began
<br />feeding on or near the substrate and began using the vegetation and rock provided
<br />as cover when disturbed. They rarely entered the upper half of the water column
<br />beyond 15 days after hatching (Loudermilk et al., 1981, unpublished manuscript). At
<br />larvae were collected from both the surface and by disturbing the substrate. Dead
<br />or mortibund larvae were observed in relatively high numbers (Linda Ulmer, pers.
<br />comm.) there.
<br />It has been suggested (Hubbs and Miller, 1953) that young razorbacks followed
<br />adults back out of streams to the main river. The young have been reported to travel
<br />in large schools along stream or reservoir margins. The terminal mouth migrates O
<br />the sub-terminal position within m_ the of hatching and the nuchal keel
<br />--=' rs when the young are n total length. Adults reach 5 to 6 kg in
<br />weight and feed on algae, dipteran larvae and zooplankton. They have long digestive
<br />tracts, poorly differentiated stomachs, no pyloric caecae and well-developed hearing.
<br />Based on very limited information, egg survival may be best between 16-250C and
<br />spawning occurs between 12-18°C. Tributary water temperatures in that range histor-
<br />ically would have occurred March - July, depending on the water year, but generally
<br />during the later part of the runoff period. Before dams, gravel bars or wash fans W'
<br />likely available for spawning and water temperatures were rising with ambient temper-
<br />ature increases as runoff subsided. In the river below Parker, Arizona most of the
<br />substrate was and is sand, mud or silt. The only likely spawning gravels, with a few
<br />exceptions, were alluvial fans created by flood events down tributary washes or up
<br />the Gila River drainage into southwest Arizona.
|