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7/14/2009 5:02:31 PM
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UCREFRP
UCREFRP Catalog Number
7758
Author
Stanford, J. A. and P. C. Nelson.
Title
Instream Flows to Assist the Recovery of Endangered Fishes of the Upper Colorado River Basin.
USFW Year
1994.
USFW - Doc Type
Denver, Colorado.
Copyright Material
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6 BIOLOGICAL REPORT 24 <br />of nonnative fishes that may migrate upstream, <br />thereby influencing the native fishes living in the <br />Upper Colorado River Basin. However, I viewed <br />Lake Powell as the downstream boundary of the <br />river ecosystem examined in this report (Fig. 1). <br />A vital characteristic of river ecosystems is that <br />their biophysical processes are inherently vari- <br />able. The essence of ecology is understanding the <br />complex processes that control observed variabil- <br />ity in the distribution and abundance of biota. <br />Quantification of the structure and function of <br />complex systems, like the Upper Colorado River <br />Basin ecosystem, in time and space must be based <br />on long-term (> 5 years) measurements to detect <br />patterns or trends that in shorter time frames are <br />overwhelmed by variability. Hence, an ecosystem <br />approach strives to determine how and why the <br />river changes in time and space, not simply to <br />describe current conditions. <br />Like most scientists, I view model building and <br />logistic descriptions of dynamic events in ecology <br />as mechanistic tools for formalizing a better under- <br />standing of what is known about a system; such <br />tools should not be used to predict the future. <br />Predicting the consequences of environmental <br />change is the ultimate challenge of contemporary <br />ecology. This must be resolved through strong in- <br />ferences based on properly scaled measurements <br />of biophysical variables that integrate the myriad <br />system-specific ecological processes that are spa- <br />tially and temporally dynamic (Magnuson 1990; <br />Stanford and Ward 1992a). The problem of in- <br />stream flow provision must be resolved from <br />strong inferences derived from long-term trends in <br />ecological processes and responses of the river <br />ecosystem in which the endangered fishes live. <br />River Ecology and Effects of <br />Regulation on the Endangered <br />Fishes of the Upper Colorado <br />River Basin <br />Ecology of the Endangered Fishes <br />Information about the endangered fishes is very <br />detailed, given that they are relatively rare fishes; <br />several reviews of the scientific information have <br />been published (e.g., Stanford and Ward 1986b; <br />Minckley et al. 1991; Tyus 1991a). Therefore, I <br />repeat here only salient points of particular impor- <br />tance to my review of the flow recommendations <br />made by the U.S. Fish and Wildlife Service. <br />As noted above, the historical range of the four <br />species included the potamon and transitional <br />reaches of the Green and Colorado river systems, <br />including most of the larger tributaries, in particu- <br />lar the Yampa, White, Dolores, and Gunnison riv- <br />ers. Today, ranges of these fish are fragmented by <br />dams and diversions, and populations have de- <br />clined significantly in relation to distributions at <br />the turn of the century (Quartarone 1993). <br />Bonytail chub are close to extirpation, but they <br />have been successfully cultured, along with hump- <br />back chub, squawfish, and razorback sucker, at the <br />Dexter National Fish Hatchery, Dexter, New Mex- <br />ico (Johnson and Jensen 1991), and brood stocks <br />currently are being held in several locations. Be- <br />cause of their comparative rarity in the wild, eco- <br />logical information on the historical range of <br />bonytail chub is more fragmentary than for the <br />other species. A few specimens of bonytail chub <br />were collected in the 1970's in the Green and <br />Yampa rivers (Kaeding et al. 1986), but their phe- <br />nology (life history) and exact cause of disappear- <br />ance in the Upper Colorado River Basin system are <br />unknown. <br />Humpback chub are found only in whitewater <br />canyon segments (Fig. 1). Migrations are limited, <br />and humpback chub may have always been re- <br />stricted to specific canyon segments, at least as <br />adults. Spawning in the Upper Colorado River Ba- <br />sin occurs on the declining limb of the spring runoff <br />event in association with the 20° C isotherm <br />(Kaeding and Zimmerman 1983). Humpback chub <br />interact behaviorally (and probably hybridize) with <br />congeneric, endemic roundtail chub (Gila robusta), <br />which are more abundant throughout the Upper <br />Colorado River Basin (Kaeding et al. 1990; Karp <br />and Tyus 1990). Much of what is known about the <br />life cycle of humpback chub is based on unpublished <br />studies in the Grand Canyon, where they migrate <br />from the regulated Colorado River into the unregu- <br />lated Little Colorado River to spawn. Similar mi- <br />gratory behavior has not been documented in the <br />Upper Colorado River Basin, and exact locations of <br />spawning sites are unknown (Richard Valdez, <br />BioWest Inc., Logan, Utah, personal communica- <br />tion; Larry Crist, U.S. Bureau of Reclamation, Salt <br />Lake City, Utah, personal communication). <br />Lanigan and Tyus (1989) estimated that only <br />978 ± 232 adult razorback sucker remained in the <br />Green River above Desolation Canyon during <br />1981-86, which very likely is only a small fraction <br />of the historic population. Some researchers be- <br />lieve that significant declines have occurred since
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