Alpine river ecosystem response to glacial and anthropogenic flow pulses

Alpine glacier-fed river hydrology, chemistry and biology can vary significantly both in space and over diurnal to inter-annual timescales, as a function of dynamic inputs of water from snow, ice and groundwater. The sensitivity of biota to these water source dynamics potentially makes them susceptible to hydrological changes induced by anthropogenic activities, such as flow regulation, but most alpine studies have focused on intact rivers and during summer only. We examined the patiotemporal dynamics of physicochemical habitat and macroinvertebrate communities in a high (>2000m) altitude floodplain in the European Alps over an 18 month period. A novel insight is presented into the river system and macroinvertebrate community responses to both natural glacier melt driven expansion-contraction of unregulated river sites, and intermittent flow pulses due to hydropower regulation. Mainstem glacier-fed river sites displayed cyclical seasonal dynamics in macroinvertebrate community composition, shifting to be partly reminiscent of groundwater tributaries in winter then back to meltwater again in the following spring. Significant unimodal relationships were observed between glacial influence and macroinvertebrate community density, richness, Simpson's diversity, evenness and beta diversity. These relationships suggest that glacial influence can have positive effects on biodiversity where glacier meltwater mixes with non-glacial water and habitat diversity is maximised. Regulationinduced flow pulses led to inconsistent responses amongst macroinvertebrates, with no significant effects in summer 2008 but increased density and decreased taxonomic richness in 2009. Furthermore, macroinvertebrate community composition was not affected significantly by reservoir releases despite significant increases in water temperature and discharge at these times. The effects of alpine river management for hydropower production on macroinvertebrate communities in this river system appear to be relatively minor, but further studies need to be undertaken in other alpine locations to assess the generality of this finding.