Terrestrial and aquatic elemental cycles are tightly linked in upland fluvial networks. Biotic and abiotic mineral weathering, microbially mediated degradation of organic matter, and anthropogenic influences all result in the movement of solutes (e.g., carbon, metals, and nutrients) through these catchments, with implications for downstream water quality. Within the river channel, the region of hyporheic mixing represents a hot spot of microbial activity, exerting significant control over solute cycling. To investigate how snowmelt-driven seasonal changes in river discharge affect microbial community assembly and carbon biogeochemistry, depth-resolved pore water samples were recovered from multiple locations around a representative meander on the East River near Crested Butte, CO, USA. Vertical temperature sensor arrays were also installed in the streambed to enable seepage flux estimates. Snowmelt-driven high river discharge led to an expanding zone of vertical hyporheic mixing and introduced dissolved oxygen into the streambed that stimulated aerobic microbial respiration. These physicochemical processes contributed to microbial communities undergoing homogenizing selection, in contrast to other ecosystems where lower permeability may limit the extent of mixing. Conversely, lower river discharge conditions led to a greater influence of upwelling groundwater within the streambed and a decrease in microbial respiration rates. Associated with these processes, microbial communities throughout the streambed exhibited increasing dissimilarity between each other, suggesting that the earlier onset of snowmelt and longer periods of base flow may lead to changes in the composition (and associated function) of streambed microbiomes, with consequent implications for the processing and export of solutes from upland catchments.
Plain Language SummarySeasonal changes in river discharge in high-altitude watersheds affect patterns of surface and groundwater mixing in the hyporheic zone (the region in the riverbed where these two water sources interact) that impacts how carbon compounds and dissolved metals are transported.One key constraint with respect to hyporheic mixing concerns the rate of water flow, a process driving the change in oxygen concentration in the riverbed. Oxygen concentration controls rates of carbon degradation and metal inputs from surrounding rocks, which, in turn, affect downstream water quality. In this study, we examined a stream in an alpine watershed, the East River, in the Upper Colorado River Basin, sampling a representative meander at discrete depths throughout the year for microbiological and geochemical analyses. We also installed data loggers to continuously collect temperature information to understand the extent of hyporheic mixing. We found that the movement of dissolved materials was strongly correlated with seasonal changes in flow. Under maximum flow, increased oxygen concentration stimulates microbial degradation of carbon compounds, and conversely, during minimum flow, decreased oxygen c...