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19vb <br />1099 <br />Wetland <br />River (Jensen) <br />10 20 30 10 20 30 10 <br />Dissolved Oxygen 1996 <br />- surface <br />- Bottom <br />10 20 30 10 20 30 10 <br />may Jun Jul ^uy wN may oulI V.. <br />FIGURE 2.-Comparison of temperature, dissolved oxygen, and depth in the Green River (Jensen, Utah) and the <br />Old Charley Wash wetland during the spring and summer of 1995 and 1996. <br />3 <br />SUCKER WETLAND USE <br />U <br />0 <br />J <br />2.7 <br />rn <br />M <br />0.9 <br />0 <br />1995 <br />--- Wetland <br />River (Jensen) <br />Dissolved Oxygen 1995 <br />1 1,5 1 1,5 1 1,5 1 1,5 1 15 <br />5 1 1 <br />Adult fish accessing the wetland from the Green <br />River dominated the biomass of fish collected after <br />draining Old Charley Wash, making up 80% and <br />77% of the biomass in 1995 and 1996, respec- <br />tively. Fathead minnow and red shiners were in- <br />cluded in the category of fish produced in the wet- <br />land, although many probably accessed the wet- <br />land from the river. Although age-0 fish were only <br />a small fraction of the total biomass collected dur- <br />ing draining, they composed the numerical ma- <br />jority of fish collected. <br />The age-0 razorback sucker was the most abun- <br />dant native fish collected in Old Charley Wash <br />during both 1995 and 1996. The 28 fish collected <br />in 1995 averaged 94 mm (range, 74-125 mm) in <br />total length and 9.5 g (range, 3-18 g) in weight. <br />In 1996, another 45 razorback suckers were col- <br />30 <br />24 <br />18 <br />12 <br />6 <br />0 <br />12 <br />10 <br />8 <br />6 <br />4 <br />2 <br />0 <br />30 <br />24 <br />18 <br />12 <br />6 <br />0 <br />12 <br />10 <br />8 <br />6 <br />4 <br />2 <br />0 <br />2. <br />1. <br />0. <br />lected; these fish averaged 65.9 mm (range, 44- <br />83 mm) in total length and 3.8 g (range, 1-6 g) <br />in weight. In 1995, two razorback sucker adults <br />were collected; none were collected in 1996. Other <br />native fishes collected in 1995 and 1996 included <br />the juvenile Colorado pikeminnow, flannelmouth <br />sucker, and roundtail chub. <br />Discussion <br />When razorback sucker larvae in the Green Riv- <br />er emerge during peak discharges in the spring <br />(Tyus 1987), off-channel floodplain wetlands like <br />Old Charley Wash represent a velocity refuge and <br />thermal optimum. During high-volume spring <br />flows, temperatures in the main channel are re- <br />duced by the effect of snowmelt runoff. Main- <br />channel habitats offer little refuge to larval fishes