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<br />squawfish. Although extremely high flows appear to be associated with weak cohorts of Colorado <br />squawfish and humpback chub, occasional extreme flooding needed to maintain channel <br />morphology and channel-floodplain interactions likely are critical for long-term survival of the <br />fishes. Indeed, the only recent incident of successful recruitment of adult razorback sucker <br />occurred when high flows reconnected riparian gravel pits to the mainstem Colorado River. On the <br />other hand, it is fairly clear that squawfish recruitment can occur over a very wide range of spring <br />flows, and squawfish spawning may be much less site-specific than is suggested by the literature, or <br />a very wide range of preferred. spawning conditions exist on the spawning bars where squawfish are <br />routinely found (e.g., Cleopatra's couch bar on the Yampa, Three Fords on the Green). Presence of <br />nonnative predators and reduced complexity of habitats needed by the different life history stages <br />of the endangered fishes (due to severing of channel-floodplain connections and encroachment of <br />riparian vegetation into the channel) further confound detennination of cause and effect. The <br />fundamental problem with respect to provision of flows to recover the endangered fishes is <br />balancing the many interactive effects in a manner that will favor the native fishes over the long term <br />(i.e., decades). <br />5) The phenologies (life histories) of the endangered fishes, as well as zoo benthos which <br />also have been studied in detail, are either directly or indirectly controlled by flow magnitude and <br />timing and the association between flow and temperature. However, relationships between flow, <br />channel configuration and thennal heterogeneity (cf., Ward 1984) have not been well integrated <br />conceptually or empirically or in the context of the various life history stages of the fishes. A <br />squawfish life history energetics model, for example, likely would be very helpful in this regard. <br />6) Stream regulation has introduced serial discontinuities (i.e., downstream extension of <br />cold water or rhithron environments) within the river continua of the Upper Colorado River Basin. <br />The location and persistence of these discontinuities are directly related to flow, and largely <br />detennine where the endangered and other native fishes can achieve a positive life history energy <br />balance (i.e., complete the life history with net recruitment of young at or above minimum viable <br />population size). Bear in mind that these fishes are adapted to potamon conditions and the length <br /> <br />43 <br /> <br />" <br /> <br />'. <br />