Glacier loss and vegetation expansion alter organic and inorganic carbon dynamics in alpine streams

Abstract

Abstract. High-mountain ecosystems are experiencing acute effects of climate change, most visibly through glacier recession and the greening of the terrestrial environment. The streams draining these landscapes are affected by these shifts, integrating hydrologic, geologic, and biological signals across the catchment. We examined the organic and inorganic carbon dynamics of streams in four Alpine catchments in Switzerland to assess how glacier loss and vegetation expansion are affecting the carbon cycle of these high mountain ecosystems. We find that organic carbon concentration and fluorescence properties associated with humic-like compounds increase with vegetation cover within a catchment, demonstrating the increasing importance of allochthonous carbon sources following glacier retreat. Meanwhile, streams transitioned from carbon dioxide sinks to sources with decreasing glacier coverage and increased vegetation coverage, with chemical weathering and soil respiration likely determining the balance. Periods of sink behavior were also observed in non-glaciated streams, indicating geochemical consumption of carbon dioxide may be more common in high-mountain, minimally vegetated catchments than previously described. Together, these results demonstrate the dramatic shifts in carbon dynamics of alpine streams following glacier recession, with significant changes to both the organic and inorganic carbon cycles. The clear link between the terrestrial and aquatic zones further emphasizes the coupled dynamics with which all hydrologic and biogeochemical changes in these ecosystems should be considered, including the role of mountain streams in the global carbon cycle.

A Comprehensive Biogeochemical Assessment of Climate‐Threatened Glacial River Headwaters on the Eastern Slopes of the Canadian Rocky Mountains

“…Following this, yields of basic chemical parameters mostly decreased along the SR‐AR and BR, but DOC increased from the most upstream sites to the most downstream sites along all three rivers (Figure 7a). The increase in DOC yields with distance from glacier can potentially be explained by the transition from a glacierized altitudinal life zone with fast‐flowing cold, turbid meltwaters to an alpine altitudinal life zone with freshwaters more hospitable to in situ biological productivity and/or more additions of allochthonous terrestrial organic matter (Robison et al., 2023). Dissolved Si yields also increased with distance downstream and was the only nutrient to do so (Figure 7b).…”