Patterns and isotopic composition of greenhouse gases under ice in lakes of interior Alaska

• Published in: Environmental Research Letters
• Main Authors: O’Dwyer, Madeline, Butman, David E, Striegl, Robert G, Dornblaser, Mark M, Wickland, Kimberly P, Kuhn, Catherine D, Bogard, Matthew J
• Other Authors: National Aeronautics and Space Administration, University of Washington, U.S. Geological Survey
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: IOP Publishing 2020
• Subjects: Arctic; Boreal Lake; Yukon; Alaska
• Online Access: http://dx.doi.org/10.1088/1748-9326/abb493; https://iopscience.iop.org/article/10.1088/1748-9326/abb493; https://iopscience.iop.org/article/10.1088/1748-9326/abb493/pdf; https://iopscience.iop.org/article/10.1088/1748-9326/abb493/ampdf

Abstract Arctic and boreal lake greenhouse gas emissions (GHG) are an important component of regional carbon (C) budgets. Yet the magnitude and seasonal patterns of lake GHG emissions are poorly constrained, because sampling is limited in these remote landscapes, particularly during winter and shoulder seasons. To better define patterns of under ice GHG content (and emissions potential at spring thaw), we surveyed carbon dioxide (CO 2 ) and methane (CH 4 ) concentrations and stable isotopic composition during winter of 2017 in 13 lakes in the arid Yukon Flats Basin of interior Alaska, USA. Partial pressures of CO 2 and CH 4 ranged over three orders of magnitude, were positively correlated, and CO 2 exceeded CH 4 at all but one site. Shallow, organic matter-rich lakes located at lower elevations tended to have the highest concentrations of both gases, though CH 4 content was more heterogeneous and only abundant in oxygen-depleted lakes, while CO 2 was negatively correlated to oxygen content. Isotopic values of CO 2 spanned a narrow range (−10‰ to −23‰) compared to CH 4 , which ranged over 50‰ (−19‰ to −71‰), indicating CH 4 source pathways and sink strength varied widely between lakes. Miller-Tans and Keeling plots qualitatively suggested two groups of lakes were present; one with isotopically enriched source CH 4 possibly more dominated by acetoclastic methanogenesis, and one with depleted signatures suggesting a dominance of the hydrogenotrophic production. Overall, regional lake differences in winter under ice GHG content appear to track landscape position, oxygen, and organic matter content and composition, causing patterns to vary widely even within a relatively small geographic area of interior Alaska.