Laserfiche WebLink
<br />INTRODUCTION <br />~ Since the construction of Flaming Gorge Dam, the magnitude and duration of <br />spring peak flows in the Green River have decreased (Muth et al. 2000). This has <br /> <br />reduced the frequency and duration of the river-floodplain connection. Floodplains are <br />presumed to be important rearing habitat for the endangered razorback sucker <br />(Xyrauchen texanus) (Wydoski and Wick 1998; Muth et al. 1998; Lentsch et al. 1996a). <br />~ Elevated temperatures, nutrients and light intensities combine to make floodplain <br />wetlands areas of high primary productivity (Birchell et al. 2002; Wydoski and Wick <br />1998; Lentsch et al. 1996a; Cooper and Severn 1994), and zooplankton density (fish <br />~ food items) is also high. <br />Wydoski and Wick (1998) summarized data collected from zooplankton studies <br />conducted in the Upper Colorado River Basin. Zooplankton densities (mean number of <br />organisms/liter) were lowest in the main channel (0 - 1.3), higher in backwaters (0 - <br />13.1) and highest in floodplain habitats (4.2 - 81.5). The minimum quantity of food <br />~ required by razorback sucker larvae to survive following swim-up is 30 - 60 shrimp <br />nipple per fish per day (Peepuls and Mickey 1992 in Wydoski and Wick 1998). The <br />highest density of zooplankton commonly occurs in floodplains along the middle Green <br />River, rarely in backwaters, and never in the main channel (Birchell et al. 2002; <br />Wydoski and Wick 1998). Reproduction by razorback sucker occurs in the spring <br />~ during peak flows when highly productive floodplain habitats are accessible to fish <br />(Muth et al. 1998). This seasonal timing of razorback sucker spawning, and drift, <br /> <br />indicates possible adaptation for using floodplain habitats (Muth et al. 1998). <br />1 <br /> <br />