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2 <br />Abstract. Regional geology controls the geomorphic organization of the Green River <br />in Colorado and Utah and produces a series of river segments that are either restricted <br />meanders, fixed meanders, or canyons with abundant debris fans. The distribution of <br />channel planform controls the distribution of shoreline complexity, and there is no <br />systematic downstream change in channel planform or in shoreline complexity. <br />Backwater habitats, which typically are abundant where complexity is high, are used as <br />nursery areas by age-0 Colorado squawfish Ptychocheilus lucius. Field measurements <br />of channel and bar topography, air photo and geographic information system analysis, <br />and simulation modeling show that the location of critical nursery habitat segments of <br />the river is ultimately determined by channel geomorphology. Longitudinal dispersion <br />establishes a system-wide pattern wherein downstream segments have higher age-0 <br />populations, but restricted meandering reaches have proportionally higher populations <br />than predicted soley by longitudinal dispersion. Streamflow at the time of larval drift <br />also affects population and distribution. The interaction of hydrology, geomorphology, <br />and the characteristics of spawning and larval drift must be understood collectively if <br />operations of Flaming Gorge Dam are to be adjusted to maintain the present distribution <br />of river segments critical as nursery habitats in the Green River. <br />Keywords. fluvial geomorphology, endangered fish, Green River