Publication
The dynamics of methane generation and evasion from well-oxygenated, oligotrophic streams have been traditionally neglected. We estimated evasion of methane and assessed its sources and production pathways using a stable isotope approach in 16 oxygen-rich and C-poor (dissolved organic carbon: 55.32 +/- 57.56 mu mol/L) Alpine headwater streams. Methane was often supersaturated relative to the atmosphere (0.093 +/- 0.179 mu mol/L). Fluxes (0.87 +/- 1.34 mmol.m(-2).day(-1)) were unexpectedly high and comparable to those from high-latitude lakes and reservoirs. Our findings suggest that methane in the streambed was largely produced from carbon dioxide reduction, whereas acetoclastic pathways and major deliveries from adjacent soils, assessed from a mass balance, may have contributed to stream water methane. This study sheds new light on high-alpine streams as a hitherto unaccounted source of methane to the atmosphere.