Continuous Dynamics of Dissolved Methane Over 2 Years and its Carbon Isotopes (δ13C, Δ14C) in a Small Arctic Lake in the Mackenzie Delta

We studied dissolved methane dynamics within a small Mackenzie River Delta lake, autonomously and continuously collecting water samples for two years at various depths.

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Creator Hadley A. McIntosh Marcek, Lance F. W. Lesack, Beth N. Orcutt, C. Geoff Wheat, Scott R. Dallimore, Kimberley Geeves, Laura L. Lapham
Summary Seasonally ice-covered permafrost lakes in the Arctic emit methane to the atmosphere during periods of open-water. However, processes contributing to methane cycling under-ice have not been thoroughly addressed despite the potential for significant methane emission to the atmosphere at ice-out. We studied annual dissolved methane dynamics within a small (0.2 ha) Mackenzie River Delta lake using sensor and water sampling packages that autonomously and continuously collected lake water samples, respectively, for two years at multiple water column depths. Lake physical and biogeochemical properties (temperature; light; concentrations of dissolved oxygen, manganese, iron, and dissolved methane, including stable carbon, and radiocarbon isotopes) revealed annual patterns. Dissolved methane concentrations increase under-ice after electron acceptors (oxygen, manganese, and iron oxides) are depleted or inaccessible from the water column. The radiocarbon age of dissolved methane suggests a source from recently decomposed carbon as opposed to thawed ancient permafrost. Sources of dissolved methane under-ice include a diffusive flux from the sediments and may include water column methanogenesis and/or under-ice hydrodynamic controls. Following ice-out, the water column only partially mixes allowing half of the winter-derived dissolved methane to be microbially oxidized. Despite oxidation at depth, surface water was a source of methane to the atmosphere. The greatest diffusive fluxes to the atmosphere occurred following ice-out (75 mmol CH4 m−2 d−1) and during a mixing episode in mid-July, likely driven by a storm event. This study demonstrates the importance of fine-scale temporal sampling to understand dissolved methane processes in seasonally ice-covered lakes.
Local Relevance This study investigates methane dynamics of a small lake in the Mackenzie River Delta of the NWT.
Notes
Tags Methane,Lake,Freshwater,Research
Geographic Region Beaufort Delta
Release Date 2021-02-08
Last Modified Date 2021-02-08
Funding Program