The Coast Mountains of southeast Alaska are currently experiencing some of the highest rates of glacier volume loss on Earth, with unknown implications for proglacial stream biogeochemistry. We analyzed streamwater for Œ¥18O and dissolved organic matter (DOM) biogeochemistry (concentration, Œ¥13C-dissolved organic carbon (DOC), and fluorescence characterization) during the 2012 glacial runoff season from three coastal watersheds in southeast Alaska that ranged in glacier coverage from 0 to 49% and a glacier outflow stream. Our goal was to assess how DOM biogeochemistry may change as receding glaciers are replaced by forests and glaciers contribute less meltwater to streamflow. Discharge and streamwater Œ¥18O varied seasonally reflecting varying contributions of rainfall and snow/icemelt to streamflow over the runoff season. Mean DOC concentrations were lowest in the glacial outflow and highest in the non-glacial stream reflecting an increasing contribution of vascular plant-derived carbon with decreasing watershed glaciation. Fluorescence and Œ¥13C-DOC signatures indicated that DOM shifted from vascular plant-derived, humic-like material in the non-glacial stream toward more Œ¥13C-DOC enriched, glacier-derived DOM in the glacial outflow. Streamwater Œ¥18O was significantly correlated to DOC concentration, Œ¥13C-DOC, and protein-like fluorescence of streamwater DOM (all P < 0.05), demonstrating that changes in the source of streamwater across the glacial watershed continuum have important implications for the amount and quality of stream DOM export. Overall, our findings show that continued glacial recession and subsequent changes in glacial runoff could substantially influence the biogeochemistry of coastal temperature watersheds by altering the timing, magnitude, and chemical signature of DOM delivered to streams.
Fellman, J. B., E. Hood, R. G. M. Spencer, A. Stubbins, P. A. Raymond. 2014. Watershed glacier coverage influences dissolved organic matter biogeochemistry in SE Alaska. Ecosystems. 17: 1014-1025. http://link.springer.com/article/10.1007/s10021-014-9777-1.