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<br />696 <br /> <br />OSMUNDSON ET AL. <br /> <br />be reached by most individuals in the present pop- <br />ulation. Natural mortality probably occurs before <br />these fish reach that point. <br />There are anecdotal accounts of Colorado <br />squawfish historically reaching 1,200-1,800 mm <br />TL in the upper Colorado River basin (upstream <br />of Lees Ferry, Arizona), a length considerably <br />larger than that of any Colorado squawfish caught <br />in the past 20 years (e.g., Jordan 189l; Quarterone <br />1993). Two explanations proposed for the absence <br />of such individuals are that the growth rate has <br />declined or that the survival rate is reduced. Behn- <br />ke and Benson (1983) suggested that the extir- <br />pation of bony tail Gila elegans has impacted the <br />food supply of Colorado squawfish, thereby re- <br />ducing growth. Gilpin (1993) showed with simu- <br />lations that average and maximum sizes would sig- <br />nificantly increase if adult survival rate was in- <br />creased to 0.95, and he suggested that rates have <br />declined through angling mortality. Neither hy- <br />pothesis, however, adequately explains the dis- <br />appearance of very large individuals. Kaeding and <br />Osmundson (1988) concluded that slow growth in <br />the upper Colorado River basin was an historic <br />norm because temperature regimes have, with few <br />local exceptions, remained unchanged and poten- <br />tial foods, such as native Gila species and suckers, <br />remain plentiful. Forage for young Colorado <br />squawfish may even be greater than in the past <br />because of the addition of non-native minnows. <br />Also, size structure of Gilpin's simulated popu- <br />lation with a survival rate of 0.95 indicated the <br />largest individuals would not exceed 1,000 mm <br />TL. <br />We offer a third hypothesis. Large fish may have <br />attained their size in the lower Colorado River ba- <br />sin (downstream of Lees Ferry) and later moved <br />upstream where they were eventually captured. <br />Kaeding and Osmundson (1988) demonstrated that <br />longer growing seasons and warmer temperatures <br />in the lower basin historically provided 1.5-2.3 <br />times the annual thermal units for growth than in <br />upper basin reaches. Additionally, Colorado <br />squawfish are capable of long-distance move- <br />ments: radio-tagged adults have traversed the en- <br />tire length of their current range in the upper Col- <br />orado River (313 km) in less than 3 months <br />(McAda and Kaeding 1991), and similarly long <br />spawning migrations in the Green River have been <br />reported (Tyus 1990). If the lower basin was once <br />a source of upper basin large fish, blockage of <br />upstream movement by main-stem dams and even- <br />tual extirpation of downstream populations may <br /> <br />explain the disappearance of very large individ- <br />uals. <br /> <br />Survival <br /> <br />Our range of suitable (P < 0.05) survival esti- <br />mates of 0.83-0.87 (1991-l994 data) is higher <br />than the estimate of Gilpin (1993) for the Green <br />River population (0.81), which may reflect differ- <br />ences in environment between the two rivers. <br />However, had the methodology used by Gilpin <br />(1993) provided a range rather than a point esti- <br />mate, it may well have overlapped ours, suggesting <br />no difference in survival rates. Deviations from a <br />stable population size in either river would affect <br />comparability of estimates because each was based <br />on that assumption. Our estimates of survival were <br />also higher than that (0.65 for females; 0.80 for <br />males) found for the piscivorous walleye Stizoste- <br />dion vitreum in a lightly harvested population <br />(Schneider et aI. 1977). <br />Our method of determining survival rate was <br />not designed to replace capture-recapture models <br />for open populations, such as Jolly-Seber (Jolly <br />1965; Seber 1965) and variations thereof. It can <br />be applied, however, when the consistent capture <br />effort and long capture histories necessary for Jol- <br />ly-Seber modeling (see Pollock et aI. 1990) are <br />unavailable. Chief limitations of our method are a <br />need for population structure data over several <br />years and capture methods that sample various- <br />sized fish at rates representing the actual popula- <br />tion. Our tests indicated that population size struc- <br />ture of Colorado squawfish 550 mm and longer did <br />not change significantly during 1990-1995 and <br />was similar to that in 1982. We were unable to test <br />for capture bias in trammelnetting, but dispropor- <br />tionate numbers of large fish were caught by elec- <br />trofishing, consistent with known biases of that <br />gear type (Reynolds 1983). When captures by elec- <br />trofishing were included in the analysis, estimated <br />survival increased, as expected (not shown). <br />Though historic survival rates are unknown, <br />there are new sources of mortality that may have <br />recently lowered rates, although other sources of <br />mortality are probably unchanged. Accidents dur- <br />ing high water (abrasions, strandings, etc.), stress <br />during spawning, and predation by great blue her- <br />ons (Ardea herodias) and bald eagles (Haliaeetus <br />leucocephalus) must have been primary sources of <br />adult mortality. Significant change in these factors <br />is unlikely, except perhaps the frequency of strand- <br />ings, which may have increased because of ex- <br />cavation of floodplain gravel pits. Colorado <br />squaw fish are attracted to such habitats during <br /> <br />" <br />