High methane emissions from thermokarst lakes in subarctic peatlands

• Published in: Limnology and Oceanography
• Main Authors: Matveev, Alex, Laurion, Isabelle, Deshpande, Bethany N., Bhiry, Najat, Vincent, Warwick F.
• Other Authors: Natural Sciences and Engineering Research Council of Canada, Networks of Centres of Excellence of Canada, FRQNT
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2016
• Subjects: palsa; palsas; permafrost; Subarctic; Thermokarst
• Online Access: http://dx.doi.org/10.1002/lno.10311; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Flno.10311; https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.10311

Abstract The thawing and subsidence of frozen peat mounds (palsas) in permafrost landscapes results in the formation of organic‐rich thermokarst lakes. We examined the effects of palsa degradation on CH 4 and CO 2 emissions by comparing thermokarst lakes at two peatland locations in subarctic Québec, Canada: in the northern discontinuous permafrost region, and in southern sporadic permafrost where palsas are more rapidly degrading. The lakes were shallow (< 3 m) but stratified at both sites, and most had anoxic bottom waters. The surface waters at both sites were supersaturated in CH 4 and CO 2 , and to a greater extent in the southern lakes, where the surface CH 4 concentrations were up to 3 orders of magnitude above air equilibrium. Concentrations of CH 4 and CO 2 increased by orders of magnitude with depth in the southern lakes, however these gradients were less marked or absent in the North. Strong CH 4 and CO 2 emissions were associated with gas ebullition, but these were greatly exceeded by diffusive fluxes, in contrast to thermokarst lakes studied elsewhere. Also unusual relative to other studies to date, the surface concentrations of both gases increased as a linear function of water column depth, with highest values over the central, deepest portion of the lakes. Radiocarbon dating of ebullition gas samples showed that the CH 4 had 14 C‐ages from 760 yr to 2005 yr before present, while the CO 2 was consistently younger. Peatland thermokarst lakes may be an increasingly important source of greenhouse gases as the southern permafrost limit continues to shift northwards.