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2008-04-04_PERMIT FILE - C1981038A
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2008-04-04_PERMIT FILE - C1981038A
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Last modified
8/24/2016 3:26:58 PM
Creation date
6/4/2008 11:12:49 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981038A
IBM Index Class Name
Permit File
Doc Date
4/4/2008
Section_Exhibit Name
Environmental Resources - Fish & Wildlife Appendix Part 3
Media Type
D
Archive
Yes
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BIOLOGICAL BACKGROUND <br />Colorado Squawfish <br />The Colorado Squawfish evolved as the main predator in the Colorado River <br />system. The diet of Colorado Squawfish longer than 3 or 4 inches consists <br />almost entirely of other fishes (Vanicek and Kramer 1969). The Colorado <br />Squawfish is the largest cyprinid fish (minnow family) native to North America <br />and, during predevelopment times, may have grown as large as 6 feet in length <br />and weighed nearly 100 pounds (Behnke and Benson 1983). These large fish may <br />have been 25-50 years of age. <br />Based on early fish collection records, archaeological finds, and other <br />observations, the Colorado Squawfish was once found throughout warmwater <br />reaches of the entire Colorado River Basin, including reaches of the upper <br />Colorado River and its major tributaries, the Green River and its major <br />tributaries, and the Gila River system in Arizona (Seethaler 1478). Colorado <br />Squawfish were apparently never found in colder, headwater areas. Seethaler <br />(1978) indicates that the species was abundant in suitable habitat throughout <br />the entire Colorado River basin prior to the 1850's. Historically, Colorado <br />Squawfish have been collected in the upper Colorado River as far upstream as <br />Parachute Creek, Colorado (Kidd 1977). <br />A marked decline in Colorado Squawfish populations can be closely correlated <br />with the construction of dams and reservoirs between the 1930's and the <br />1960's, introduction of nonnative fishes, and removal of water from the <br />Colorado River system. Behnke and Benson (1983) summarized the decline of the <br />natural ecosystem. They pointed out that dams, impoundments, and water use <br />practices are probably the major reasons for drastically modified natural <br />river flows and channel characteristics in the Colorado River Basin. Dams on <br />the main stem have essentially segmented the river system, blocking Colorado <br />Squawfish spawning migrations and drastically changing river characteristics, <br />especially flows and temperatures. In addition, major changes in species <br />composition have occurred due to the introduction of nonnative fishes, many of <br />which have thrived as a result of changes in the natural riverine system <br />(i.e., flow and temperature regimes). The decline of endemic Colorado River <br />fishes seems to be at least partially related to competition or other <br />behavioral interactions with nonnative species, which have perhaps been <br />exacerbated by alterations in the natural fluvial environment. <br />The Colorado Squawfish currently occupies about ],030 river miles in the <br />Colorado River system (25 percent of its original range) and is presently <br />found only in the Upper Basin above Glen Canyon Dam. It inhabits about <br />350 miles of the main stem Green River from its mouth to the mouth of the <br />Yampa River. Its range also extends 160 miles up the Yampa River and <br />104 miles up the White River, the two major tributaries of the Green River. <br />In the main stem Colorado River, it is currently found from Lake Powell <br />extending about 201 miles upstream to Palisade, Colorado, and in the lower <br />33 miles of the Gunnison River, a tributary to the main stem Colorado River <br />(Tyus et al. ]982). <br />
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