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<br />., <br /> <br />humpbacK, and roundtai 1 chubs, and may be a major factor in disappearance <br />oJ f the fir s t s p e c i e san d d ec 1 i n e 0 f the see 0 n d .: J 0 s e p h tl..!l. 1 9 77; Sm i t h <br />et:<.1. 1979; 'Jalde: 1980; ')alde: et..!l. 1982). The same potentials for <br />hYbridization between bony tail and roundtail chub exist in the lower basin, <br />and must be considered a possible result of any reintroduction program. <br />The Gila River mainstream in eastern Arizona seems the most logical place <br />to attempt re-establ:shment of this species.. ROlJn,jtail chub is extirpate,j <br />or rare in that area and chubs in New Mexico segments of the Gila River <br />tend to be in smaller habitats far upstream from historical records or <br />probable penetration b;1 stocked bon/tai1. <br /> <br />Humpback chub, Gila cyoha t1illt?r, 1946 U1ap 9) <br /> <br />Historic occurrence in United States: probably widespread in <br />can/on-bound segments of the Colorado River. Historic abundance: abundant <br />to common. Geographic distribution: endemic to larger streams of the <br />Colorado River basin (Holden and HincKley 1980a). Status: endangered. <br />Reasons for decl ine or 1 isting: basically unKnown - habitat loss <br />(dewatering of lower portions of major streams in lower basin); habitat <br />modification (direct and indirect effects of impoundment, channel ization, <br />diversion, and regulation of discharges); hybridization with bony tail and <br />roundtai1 chubs due in part to factors just given and to increasing rarity <br />in the system; and possible interactions with non-native species. <br /> <br />The late discovery and description of humpbacK chub in 1946 and its <br />procl ivity for inaccessible canyons of the Colorado River system precluded <br />collection of data on its ecology, abundance, and distribution until after <br />major modifications had occurred. The bizzare species remains common in <br />the lower Colorado River basin only in the lowermost few kilometers of the <br />Li ttle Colorado River, Arizona (MincKley 1977, 1979; Suttkus and Clemmer <br />1977; Minckley tl Al. 1981; Keading and Zimmermann 1983). It infrequently <br />occurs in the adjacent Colorado River mainstream. which presumably is <br />avoided due to persistently cold waters (10-150 C) from the hypol imnion of <br />Lake Powell. The river warms only a few degrees in its entire passage <br />through Grand Canyon National ParK from Glen Canyon Dam to LaKe Head, even <br />in mid-summer (Kubly and Cole 1979). Similar exclusion of native fishes <br />downstream from Flaming Gorge Dam on the Green River, Wyoming-Utah, was <br />documented by VaniceK (1967) and Vanicek et Al. 1970). Colorado squawfish, <br />bony tail , humpback chub, and razorback sucKer may have suffered the same <br />fate in the Grand Canyon region. Concentrations of humpbacK chub in the <br />upper basin are in the most natural habitats, the lower Yampa River, Gray <br />Canyon of Green River, and Westwater and BlacK Rocks reaches of the <br />mainstream Colorado (Valdez 1980; Tyus et 11. 1982; Valdez et ~. 1982; <br />CRBSC 1984). <br /> <br />Interspecific hybridization, already mentioned with reference to <br />bonyta i 1, seems a maj or fac tor i nf 1 uenc i ng humpbacK chub popu I at ions in the <br />upper Colorado River basin. Despite ample evidence of a major and perhaps <br />long-term problem (Holden and Stalnaker 1970; Smit~ et .il. 1979. 'JaLdez <br />17'80; 'hldez et al. 1982), the e:<tent and sio;ni-fc:<.nce of hybrid influence <br />on any or a11 Gila of the upper basin iemains to ~e thoroughl;; documented. <br />The reader is referred to discussions of Colorado squawfish, bonytai J, and <br />razorback suc~:er for considerations of other factors relating to declines <br />of big-river fishes, including humpbacK chub. <br /> <br /><:". <br />..n <br />