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Table 5. Eight general categories of habitat types on the Colorado River. <br />CATEGORY HABITAT TYPE CATEGORY HABITAT TYPE <br />Low Velocity Types Pool Backwater Types Backwater <br /> Debris Pool Backwater Pool <br /> Rootwad Pool Embayment <br /> Eddy <br /> Edge Pool Shoal Types Sand Shoal <br /> Riffle/Eddy Cobble Shoal <br />Run Types Shoal/Run Slackwater Types Slackwater <br /> Run Pocket water <br /> Scour Run <br /> Shore Run Vegetation Overhanging Vegetation <br /> Undercut Run Associated Types Inundated Vegetation <br /> Run/Riffle <br /> Other Types Isolated Pool <br />Riffle Types Riffle Cobble Bar <br /> Shore Riffle Rootwad Pile <br /> Riffle Chute Sand Bar <br /> Shoal/Riffle Tributary <br /> Chute Island <br /> Rapid Irrigation Return <br /> Boulder <br />Biological Parameters-The primary <br />producer trophic level in the <br />Colorado River and Gunnison River <br />was measured as instantaneous <br />biomass (chlorophyll-a) estimates. <br />These data, expressed as river-wide <br />mean values (Figure 24) for each <br />sample period, indicated that riffles <br />had significantly higher periphyton <br />biomass than runs (paired t-test, <br />P=0.05). The only exception was the <br />fall of 1995. Both habitat types Figure 23. The river-wide summary of habitats mapped in the <br />demonstrated the same temporal Colorado River during September 1996. <br />pattern with an initial increase <br />between the spring and fall of 1994 followed by a large decrease over the winter of 1994. <br />The subsequent increase between the spring and fall of 1995 was greater than the previous <br />increase from spring to fall in 1994. Highest concentrations occurred in the fall of 1995. <br />When compared to the Colorado River, the Gunnison River had higher periphyton <br />concentrations in riffles and lower concentrations in runs (although not significant at the <br />P=0.05 level) in the spring of 1994. In the fall of 1994 and 1995, the higher periphyton <br />biomass levels in riffles and runs in the Gunnison were found to be significantly greater than <br />the Colorado River (Figure 24). <br />The detrital component of the primary producer trophic level was determined by quantifying <br />the coarse particulate organic material (detritus dry weight) within the river substrate. Figure <br />23