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Last modified
7/14/2009 5:02:33 PM
Creation date
5/20/2009 10:05:26 AM
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UCREFRP
UCREFRP Catalog Number
8158
Author
Osmundson, D. B.
Title
Longitudinal Variation in Fish Community Structure and Water Temperature in the Upper Colorado River; Final Report.
USFW Year
1999.
USFW - Doc Type
Grand Junction, Colorado.
Copyright Material
NO
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The bulk of fish caught in upstream strata consisted of native species, primarily bluehead and <br />flannelmouth sucker. Catch rates of bluehead sucker were generally higher in upstream strata <br />than in downstream strata. The exception to this was in Stratum 10 where the catch rate was <br />not significantly different from catch rates in downstream strata 2-6 nor from upstream <br />Stratum 7 (Appendix Table 4). Catch rates of bluehead suckers were significantly lower in <br />Stratum 10 than in other upstream strata (strata 8-9 and 11-12). <br />Catch rates of flannelmouth sucker were generally higher in upstream strata than in <br />downstream strata and catch rates among upstream strata 7, 8, 9, 11 and 12 were similar <br />(Figure 2). Again, the Stratum 10 catch rate was not significantly different from catch rates in <br />downstream strata 2-6 (Appendix Table 5). Roundtail chub catch rates in all upstream strata <br />were significantly higher than in all downstream strata and were similar among downstream <br />strata 1-6 and were similar among upstream strata 7-12 (Appendix Table 6). The catch rate <br />of speckled dace Rhinichthys osculus was significantly higher in Stratum 9 than in all other <br />strata (Appendix Table 7). For common carp (Cyprinus carpio), no longitudinal pattern was <br />evident, though catch rates in upstream strata 10 and 11 were some of the lowest and the <br />catch rate in Stratum 2 was significantly higher than in most other strata (Appendix Table 8). <br />The most upstream Colorado River stratum (Stratum 11) had significantly higher catch rates <br />of white suckers Catostomus commersoni (and hybrids with native suckers) and salmonids <br />(primarily mountain whitefish Prosopium williamsoni) than any other stratum (Appendix <br />Tables 9 and 10). In downstream strata 1-6, nonnative common carp and channel catfish were <br />a larger proportion of the total catch than in upstream strata; nevertheless, more than half of <br />the catch in strata 2-6 consisted of native suckers. <br />Prey-size fish --Catch rates of fishes that might serve as forage for Colorado pikeminnow <br />(soft-rayed fish, 100-300 mm TL) were generally highest in strata upstream of Westwater <br />Canyon (Figure 3). Very few such fish were found in Stratum 1. Strata 7, 8, 9, 11 and 12 <br />had statistically similar catch rates and these catch rates were all significantly higher than those <br />in downstream strata 1-6. The Stratum 10 catch rate was significantly higher than catch rates <br />in strata 1 and 2 and was significantly lower than the Stratum 12 catch rate; otherwise, the <br />catch rate there was not significantly different from those in strata 3-11 (Appendix Table 3). <br />In strata 2-6, the bulk of fish vulnerable to Colorado pikeminnow predation were bluehead <br />suckers. In strata 7-9, bluehead and flannelmouth suckers made up nearly equal proportions <br />of the catch and together made up most of the forage-sized fish. Catch rates of forage-size <br />flannelmouth sucker were significantly higher in Strata 7-9 than in downstream strata 1-6 <br />(Appendix Table 5). Also, the catch rate of forage-size bluehead sucker in the Gunnison <br />River stratum was significantly higher than in any Colorado River stratum (Appendix Table 4). <br />Roundtail chub and white sucker (and associated hybrids) were the only other species with <br />relatively abundant numbers of forage-size individuals. Although catch rates of bluehead and <br />flannelmouth sucker (100-300 mm TL) apparently decreased upstream of Stratum 9, <br />abundance of young roundtail chub and salmonids (primarily mountain whitefish) increased. <br />The abundance of forage-size salmonids in Stratum 11 was significantly higher than in any <br />other stratum (Appendix Table 10). <br />11
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