Wilcoxon’s paired sample signed rank this website test revealed that 6 of 11 DOM parameters differed between up and downstream of golf courses ( Fig. 4). Specifically, DOM downstream of golf courses was relatively higher in one microbial humic-like (C5, p = 0.001), one terrestrial humic-like (C2, p = 0.012), and protein-like (C7, p = 0.005) marker and lower in one microbial humic-like (C6, p = 0.024), one terrestrial humic-like (C3, p = 0.001) marker with an overall loss in the humic content of the DOM pool (HIX, p = 0.017). These differences were subtle and these patterns were

not evident for the multivariate DOM group. The DOM group was similar up and downstream of golf course facilities (Pillai’s T = 1.3, p = 0.276) but significantly different among streams (Pillai’s T = 6.8, p = 0.001; Fig. 2C). Post hoc comparison revealed that DOM characteristics at GC1 were significantly different than

GC3, GC4, and GC6. GC2 significantly differed from all streams, except GC1. DOM characteristics between GC3, GC4, GC5, and GC6 were similar ( Fig. 2C). Benthic parameters were more variable than water column parameters between streams and sampling points (Table 4). Leaf ergosterol content (a fungal biomass indicator) and epilithic algal biomass (Chlrock) ranged from 0.6 to 22.5 μg Erg. mg−1 AFDW leaf and www.selleckchem.com/products/dinaciclib-sch727965.html 0.8 to 10.6 μg Chl a cm−2 rock, respectively. N2 flux and Rleaf ranged from 18.8 to 171.9 μg-N2 h−1 g−1AFDW leaf and 22.0 to 146.8 μg-O2 h−1 g−1AFDW leaf, respectively. k exhibited the least variance, ranging from 0.015 to 0.030 d−1. These benthic parameters were similar up and downstream of golf courses based on Wilcoxon’s paired sample rank tests ( Fig. 5). Closer inspection Idelalisib cost of these paired data, however, revealed that k, ergosterol, and Rleaf deviate from zero but in different directions among sites. These patterns were captured in the benthic multivariate group comparison, which had a significant interaction between stream and sampling

location (Pillai’s T = 1.95, p = 0.050; Fig. 2D). Trajectory analysis indicated that this interaction was significantly influenced by the magnitude and direction of the golf course response among and within streams ( Fig. 6). The magnitude (multivariate distance) between up and downstream sampling points differed between GC5 with GC2 (p = 0.05), GC3 (p = 0.07), and GC6 (p = 0.05). The direction of benthic multivariate change from up to downstream sampling locations differ between GC1 and GC5 (p = 0.06) and GC4 and GC6 (p = 0.05). The landscape group correlated positively with the benthic group (r = 0.30, p = 0.022). Water quality and DOM groups did not correlate with the benthic group. The best dimensional representation (partial least squares; PLS) of the landscape group and that of the benthic group correlated strongly (r = 0.90, p < 0.001; Fig. 7A).