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7/14/2009 5:01:44 PM
Creation date
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UCREFRP
UCREFRP Catalog Number
7147
Author
Holden, P. B. and C. B. Stalnaker
Title
Distribution and Abundance of Mainstream Fishes of the Middle and Upper Colorado River Basins, 1967-1973
USFW Year
1975
USFW - Doc Type
Transactions of the American Fisheries Society
Copyright Material
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<br />:om- <br /> <br />The <br />the <br />:ers. <br />few <br />:udy <br />Irea <br />hed <br />'t'nt <br /> <br />,~w- <br />,jue- <br /> <br />.IOW <br />aJ- <br />!ult <br />Ice <br />'ed <br />III <br />:do <br /> <br />rel <br /> <br />,,1- <br /> <br />'x- <br />If- <br />'ilt <br /> <br />I~r <br /> <br />.\ <br /> <br />I', <br />:il <br /> <br />rn <br /> <br />\1 <br />,f <br /> <br />'e <br /> <br />.1 <br /> <br />'. <br /> <br />'0 <br /> <br />" <br /> <br />~ <br /> <br />HOLDEN AND ST ALNAKER--COLORADO RIVER FISHES <br /> <br />225 <br /> <br />been ideal habitat for this species. Taba, <br />Murphy, and Frost (1965) reported that the <br />red shiner was very abundant near Moab, <br />Utah, in 1962-63. Stone, Fields, and Miller <br />(1965) reported that the red shiner "ex- <br />ploded" in 1963 in Lake Powell. It is <br />therefore doubtful whether this fish, not <br />present in Glen Canyon in 1959, could be- <br />come so abundant over 200 miles upstream <br />by 1962, if it moved upriver from the lower <br />Colorado basin. More probable is an intro- <br />duction near Grand Junction, Colorado, in <br />the late 1950's or early 1960's, with subse- <br />quent downstream movement and more re- <br />cent movement up the Green River. <br />Sand shiner--Notropis stramineus Cope. <br />The sand shiner was first reported from <br />the upper Colorado basin by Holden and <br />Stalnaker (1974). It was collected in 1971 <br />in areas 7 and 8, also in the Dolores River. <br />It was abundant and may spread much as <br />the red sruner. Its numbers and distribu- <br />tion suggest it had been present for several <br />years, perhaps introduced as a uaitfish, as <br />it is common in the South Platte River <br />system of eastern Colorado. <br />The sand shiner was inadvertently <br />planted into the Little Colorado Rivcr in <br />1938 (Miller and Lowe 1964). <br />Creek chub-Semotilus atromaclllatus <br />Mitchill. Another introduced cyprinid is <br />the creek chub. It was found only around <br />Echo Park in areas 2 and 3. Vanicek, <br />Kramer, and Franklin (1970) found it below <br />Flaming Gorge Dam, collecting ouly 12 <br />specimens in fOllr years. Most of these <br />werc taken in the area between the Dam <br />and the mouth of the Yampa River. Simon <br />(1946) reported the creek chub's presence <br />in the Little Snake River. Therefore it has <br />been in the Green River system fo~ some <br />time but apparently has not fonnd condi- <br />tions favorable for maintaining large popu- <br />lations. <br /> <br />Catostomidae <br /> <br />Flannelmollth sllcker-Catostomus lati- <br />pinnis Baird and Girard. The Oannelmouth <br />"'.\cker is by far the mosl abundant large <br />native species. Wen over 6000 adults were <br />(\lllected during the study (Table 2). Adults <br /> <br />and young were caught in all study sec- <br />tions. The species was least abundant in <br />areas 5 and 6. They were collected in all <br />habitat types, fast current, riffles, eddies, <br />and stagnant backwaters. In area 12 they <br />were collected only in tributary streams. <br />In upper parts of the study area, flan- <br />nelmouth suckers were usually dark <br />brownish- green dorsally, yellowish or <br />orange laterally, and white ventrally. In <br />river sections of generally more turbid <br />water and sand bottom, they were light tan <br />on the back and silvery white on the sides <br />and belly. <br />Bluehead sucker-Catostomus discoholus <br />Cope. The bluehead sucker is abundant in <br />areas 1, 2, 3, 8, 9, and 10; common in 4, <br />7, and 12; and rare in 5 and 6. This dis- <br />tribution corresponds to the relative <br />amount of rocky substrate in the valious <br />areas. The bluehead sucker was usually <br />collected over rocky bottom and was com- <br />mon in riffles. In the sandy bottom <br />reaches of the study area it was collected <br />only over the few rocky areas created by <br />talus slopes extending into the river. <br />Bluehead suckers were also common in <br />clear, rocky tributary streams. Stream <br />specimens seldom exceed 20 cm in total <br />J'ength, whereas 25-30 cm spccimens are <br />common in the main river. In area 12 they <br />were collected only in tributaries, but were <br />common in riffle habitats of the main <br />stream in 1968 (J. E. Deacon, personal <br />communication). <br />The bluehead sucker is polymorphic in <br />the Colorado River system with slender <br />and dcep peduncled forms present. The <br />slender peduncled type is thought to be <br />adapted for swift-water areas (Miller 1946). <br />Both forms were collected during the <br />study, as were intermediate individuals. All <br />types were collected together. Deep forms <br />are most common in the upper, colder <br />parts of the basin and slender forms most <br />common in the middle sections, especially <br />area 4. No difference in habitat preference <br />was noted when they were collected <br />together. <br />Liule or no difference was noted ill the <br />hl\storical distribution or abundance of this <br />species (Jordan and Evermann 1896). <br /> <br />..;;r: <br />
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