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<br />" <br /> <br />disconnected from the river channel either by man-made revetments or by sand bars or encroaching <br />riparian vegetation that are no longer scoured owing to truncation of peak: flows by regulation (e.g., <br />Graf 1978, Stanford and Ward 1986a). Indeed, I believe loss of productive backwater <br />environments may in part explain why humpback chub are found only in canyon segments and why <br />, . <br /> <br />razorback sucker and squawfish move around a great deal. Food webs associated with gravel bars <br /> <br />are very likely more productive and pennanent (e.g., Ward and Stanford 1991), and the larger <br /> <br />razorback sucker and squawfish adults must search for these more productive sites, owing to their <br />large size and need for abundant, large forage items. Squawfish adults may be most commonly <br />found in or near the rhithron-potamon transition zone (Figure 5) because the trcUlsition zone is the <br />only area with sufficient productivity and a pennanent food web to support the life history energy <br />balance of this large predatory animal. Indeed, other native fishes that are the natural prey of adult <br />squawfish, especially roundtail chub and bluehead sucker (Catostomus discobolus), are more <br />abundant in or near the transition zones (Doug Osmundson, U.S. Fish and Wildlife Service, Grand <br />Junction, CO, personal communication) where algae and zoo benthos forage likely is most <br />abundant <br /> <br />The trophically dynamic nature of the potamon reaches of the Upper Colorado River Basin <br /> <br />and the interactive influences with geomorphic controls are poorly understood aspects of the <br />ecology of the endangered fishes. On the one hand, it is apparent that these fishes prefer low <br />velocity habitats; on the other, these low velocity habitats may not be as productive as higher <br />velocity reaches owing to fluctuating flows caused by regulation. Measurements are needed to <br />more firmly establish cause and effect. The problem is complicated by the fact that site-specific <br /> <br />velocities vary with flow, which is precisely why channel geomorphology is so complex and <br />dynamic in time and space. I conclude that throughout their life cycle these fishes are highly <br />adapted to variations in flow velocity, depth, turbidity and food web structure and function <br />associated with this spatially and temporally dynamic biophysical interaction. They simply move <br />around as flow varies, constantly seeking the best energy return on energy invested in foraging. In <br />the case of squawfish, their large size apparently allows considerable movement to efficiently use a <br /> <br />21 <br />