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Last modified
7/14/2009 5:02:37 PM
Creation date
5/24/2009 7:11:02 AM
Metadata
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UCREFRP
UCREFRP Catalog Number
9673
Author
Tyus, H. M. and G. B. Haines.
Title
Distribution, Habitat Use, and Growth of Young Colorado Squawfish in the Green River Basin, Colorado and Utah - Preliminary Report.
USFW Year
n.d.
USFW - Doc Type
Vernal, UT.
Copyright Material
NO
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Colorado squawfish Ptychocheilus Lucius, the largest North American <br />minnow, is endemic to the Colorado River basin where it was once abundant <br />and widely distributed (Jordan and Evermann 1896). The species was <br />classified as federally endangered by the U.S. Fish and Wildlife Service <br />in 1967 (Federal Register 32[43]:4001) and natural populations presently <br />exist only in the upper Colorado River basin (upstream of Lee Ferry, <br />Arizona). The Green River in Utah and its largest tributary, the Yampa <br />River in Colorado (Figure 1), contain the largest known concentration of <br />Colorado squawfish (Holden and Wick 1982; Tyus 1990). <br />Two major spawning areas have been identified in the Green River basin <br />by radiotracking migrations of Colorado squawfish, capture of ripe adults <br />and emergence of newly hatched fry. One spawning area in the lower Yampa <br />River (i.e., Yampa Canyon) was located in 1981 (Tyus and McAda 1984), and <br />a second spawning area in Gray Canyon of the Green River was located in <br />1983 (Tyus 1985]. Other spawning areas have not been confirmed after many <br />years of study. Successful Colorado squawfish reproduction was confirmed <br />at the Yampa Canyon site by collections of newly-hatched larvae (Haynes et <br />al. 1984; Nesler, 1988). However, early life history and ecology of larval <br />and postlarval Colorado squawfish are not well known. Events during the <br />first year of life regulate many fish populations (Braum 1978), and a <br />better understanding of such events aid in recovery efforts for this <br />species. <br />Construction and operation of Flaming Gorge Dam and Reservoir has <br />significantly altered historic flow and temperature regimes in the Green <br />River and this alteration has been implicated in the decline of Colorado <br />3 <br />
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