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<br />OJ(73) <br /> <br />determine whether groundwater was a source of nutri- <br />ents to surface water (McMahon et ai" 1994), Analyses <br />of nutrient concentrations followed methods described <br />in Fishman (1993) and Patton & Truitt (1992), Dissolved <br />oxygen and temperature, pH, and specific conductance <br />were measured in situ in surface and hyporheic waters. <br />Values of altitude, sinuosity, slope and stream order <br />were derived from 1:24000 scale topographical maps <br />(Meador et ai" 1993)_ <br /> <br />Data analyses <br /> <br />., <br /> <br />Ordination of sites by taxa was performed using <br />detrended correspondence analyses (DCA) on natural <br />log-transformed abundance data using the FORTRAN <br />program DECORANA (Hill, 1979), Analyses included <br />the sixty-six taxa that were collected at more than one <br />site and composed greater than 05% of the total <br />abundance of organisms (taxa with asterisks in <br />Table 2). These criteria for the inclusion of taxa in the <br />analyses were used to decrease the effect of rare <br />species. Ordination by DCA arranges sites with similar <br />taxonomic composition to cluster more closely <br />together and produces site scores that can be related <br />to environmental variables. From the DCA ordination <br />plot, four site groups were identified: mountains, <br />plains/braided channel, plains/tributary, and plains/ <br />downstream from point source. Invertebrate taxa, <br />functional feeding groups, and environmental vari- <br />ables were further defined based on these four site <br />groups, <br />Univariate analyses of environmental variables, <br />comparison of linear regression analyses of DCA axis <br />1 and 2 to individual environmental variables, and <br />analyses of variance (ANOVA) among site groups <br />were made using SAS statistical programs (SAS, 1990), <br />Natural log or square-root transformations were per- <br />formed on environmental variables to achieve approxi- <br />mate normal distribution of the data, <br />A Shannon diversity index was calculated using the <br />dominant taxa (excluding rare taxa) for each site <br />(Shannon & Weaver, 1963), Phi values were calculated <br />for the dominant and subdominant substrate sizes <br />and the mean substrate size (Folk, 1980), All inverteb- <br />rate taxa including rare taxa were assigned to func- <br />tional feeding groups using Merritt & Cummins (1984) <br />for insects and Pennak (1978) for non-insects, <br /> <br />@ 1995 Blackwell Science Ltd, Freshwater Biology, 33, 439-454 <br /> <br />Invertebrates of the South Platte River 443 <br /> <br />Results <br /> <br />A total of 104 invertebrate taxa were collected from <br />all twenty-one sites in the stream survey (Table 2), <br />Invertebrate density and number of taxa at a site <br />ranged from 100 to 20 300 organisms m -, and six to <br />thirty-six taxa/site (Table 1), Invertebrate density in <br />streams of the Southern Rockies ecoregion (mountains) <br />ranged from 1980 to 18100 m -2 and streams of the <br />Western High Plains ecoregion (plains) ranged from <br />100 to 20 300 m -', The mean number of taxa at a site <br />was greater in the mountains (mean = 25; range = <br />10-36, n = 9) compared with the plains (mean = 14; <br />range = 6-26, n = 12)(ANOVA, P < 0,005, Table 1), <br />The relative magnitude of eigenvalues for each DCA <br />axis is an expression of the relative importance of <br />the axis, DCA axis 1 (eigenvalue = 0,44) and axis 2 <br />(eigenvalue ~ 0,28) accounted for about 72% of the <br />variance in the data set, whereas, OCA axis 3 <br />(eigenvalue = 0,16) and DCA axis 4 (eigenvalue = <br />0,10) together accounted for < 30% of the variance <br />and were not strongly correlated to any measured <br />envirorunental variables. In contrast, regression of <br />DCA axis 1 and 2 scores with environmental variables <br />indicates significant relationship with seven physical <br />and seven surface- and hyporheic- water chemistry <br />variables for DCA axis 1 and two physical and four <br />surface-water chemistry variables for DCA axis 2 <br />(Table 3), Thus, DCA axis 1 separated sites in the <br />mountains (Southern Rocky Mountain ecoregion) from <br />sites in the plains (Western High Plains ecoregion) <br />based primarily on stream slope, water temperature, <br />specific conductance, and surface water organic <br />nitrogen + ammonia and total phosphorus concentra- <br />tions; each variable accounted for 48% or more of the <br />variance in DCA axis 1 scores (P < 0,05, ,2 '" 0,48; <br />Table 3), DCA axis 2 separated sites in the plains based <br />on surface water nitrate + nitrite concentrations and <br />channel width, which accounted for 36 and 32%, <br />respectively, of the variance in DCA axis 2 scores <br />(P < 0,05, ,2 > 0.30, Table 3), Four site groups were <br />then identified from plotting DCA axis 1 and 2 scores: <br />mountains, plains tributaries near their confluence <br />with the South Platte River (plains/tributary), plains <br />streams with braided channels (plains/braided <br />channel), and plains sites affected by wastewater- <br />treatment-plant effluent (plains/downstream from <br />point source) (Fig, 2), <br />The South Platte River above eleven-mile Canyon <br /> <br />I <br />~ <br />, <br />r <br />! <br />f <br />~;l <br /> <br />~ <br />