Uncoupling of acetate degradation from methane formation in Alaskan wetlands: Connections to vegetation distribution

By M. Hines, K. Duddleston, J. Rooney-Varga, D. Fields, J. Chanton. 2008

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Methanotrophs and copper. (2010, background): “…growth in situ, (Dedysh et al., 2005), and can have significant implications in our understanding of the CH 4 cycle, particularly in peat bogs where acetate can be a terminal end product of metabolism, and concentrations can reach as high as 1 mM (Hines et al., 2001, 2008; Duddleston et al., 2002).”
Methane emissions from wetlands: biogeochemical, microbial, and modeling perspectives from local to global scales (2013, background): “…not detected (Methanosarcinaceae) or were at very low abundance (Methanosaetaceae) in the Alaskan sites, and no CH4 was produced by the acetoclastic pathway in the Alaskan bog sites despite significant rates of acetate production and accumulation (Rooney-Varga et al., 2007; Hines et al., 2008).”