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7/14/2009 5:01:46 PM
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UCREFRP
UCREFRP Catalog Number
7969
Author
Karp, C. A. and H. M. Tyus
Title
Humback Chub (
USFW Year
1990
Copyright Material
YES
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1990] HUMPBACK CHUB IN DINOSAUR NATIONAL MONUMENT 259 <br />hand-held thermometers (methods after <br />Nielsen and Johnson 1983). We did not at- <br />tempt quantification of water velocities be- <br />cause most humpback chub were captured in <br />habitats where water currents swirled in both <br />upstream and downstream directions and ini- <br />tial efforts with a flow meter yielded a wide <br />range of positive (upstream) and negative <br />(downstream) velocities. Habitat use data was <br />not recorded for species other than humpback <br />chub. River flows were obtained as daily aver- <br />agesfrom the U. S. Geological Survey gauging <br />station at Deerlodge Park, Yampa River (Fig. <br />1). Stream gradient was obtained from U. S. <br />Geological Survey stream profile maps. <br />Data Analyses <br />Capture data were analyzed by total catch <br />(all years, all gear types, and sampling) and <br />standardized catch (1987-1989: catch of all <br />species and effort recorded for each sample). <br />Total catch data were used to describe general <br />fish distribution, and standardized data were <br />used to evaluate relative abundance. Stan- <br />dardized catch data were summed by gear <br />(i.e., angling or electrofishing) and for each <br />river reach (i. e. , Yampa, Lodore, Whirlpool, <br />and Split Mountain canyons, Echo and Island <br />parks), and catch per unit effort (C/f) was cal- <br />culated by dividing numbers of fish captured <br />by effort. Angling and electrofishing datafrom <br />1986 were not included in C/f estimates be- <br />cause numbers of fishes other than chubs <br />were not recorded and because of significant <br />differences in angler ability. Trammel netting <br />C/f was not reported because of limited use. <br />Electrofishing was biased toward catch of <br />larger individuals, and small fishes (e. g. , non- <br />native reside shiner [Richardsonius baltea- <br />tus ]and native mottled sculpin [Cottus spp. ]) <br />and juveniles of larger species were not <br />recorded because they often slipped through <br />our 1-in2 mesh dip-nets. Angling efforts in <br />September 1989 were excluded from the C/f <br />estimates because this effort represented a <br />unique fall sample. Sampling was initiated <br />late in 1986, and those data were excluded <br />from our evaluation of spawning period. <br />RESULTS <br />Distribution and Habitat Use <br />HvMrsncx exus.-Humpback chub were <br />collected only in whitewater reaches of Yampa <br />(n = 130) and Whirlpool (n = 3) canyons (Fig. <br />1). The Whirlpool Canyon fish were captured <br />in the same location, about 6 km downstream <br />of the confluence with the Yampa River. No <br />other humpback chub were captured in the <br />Green River. Humpback chub constituted <br />7.3% (n = 51) of the standardized angling and <br /><1% (n = 58) of the standardized electrofish- <br />ing catch. They were most abundant (85% of <br />all humpback chub captures, n = 113) in the <br />upper 44.8 km of Yampa Canyon, a moder- <br />ately steep-gradient section (3.2 m/km) domi- <br />nated byrocky runs, riffles, and rapids. Lower <br />Yampa Canyon (km 0-28.8), alower-gradient <br />system (1.0 m/km) consisting mostly of long, <br />deep runs and incised meanders, yielded rela- <br />tively few humpback chub (n = 17). <br />During spring runoff, humpback chub were <br />most often captured in larger shoreline eddies <br />(20-100 m2) that were either downstream of <br />boulders or upstream of rapids, or in smaller <br />eddies (<20 m2) within shoreline runs. Adult <br />fish (>230 mm TL; based on capture of the <br />smallest ripe fish, a232-mm-TL male) were <br />consistently captured in, and apparently se- <br />lected, seasonally flooded shoreline eddies <br />(i. e. , formed and maintained by spring <br />runof fl. These habitats were dominated by <br />low or negative water velocities and influ- <br />enced by river surges (i. e. , water velocities at <br />any particular point varied in magnitude of <br />up-and downstream currents). Substrate con- <br />sisted mostly of sand and boulders, and water <br />depth averaged 1.3 m at the estimated point of <br />capture. Humpback chub were not collected <br />in riffles and rapids. <br />Eleven of 76Carlin-tagged humpback chub <br />(z = 312 mm TL, SD = 19) were recaptured <br />one week to two years after initial capture (5 <br />within a year, 6 from one to two years). Ten <br />fish were recaptured in the immediate vicin- <br />ity of their original capture, and one was col- <br />lected about 8 km downstream from its initial <br />capture site. Eight fish (73%, n = ll) were <br />recaptured in breeding condition on at least <br />one occasion. We detected no growth in re- <br />captured fish. <br />About 22% (n = 29) of humpback chub were <br />juveniles (88-228 mm TL). These were most <br />often captured by electrofishing in rocky <br />shoreline runs and small shoreline eddies. <br />One juvenile (122 mm TL) was taken from <br />the stomach of a 61-cm-TL garter snake <br />(Thamnophis species) caught at the conflu- <br />ence of the Yampa and Green rivers. <br />
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