Anaerobic Metabolism: Linkages to Trace Gases and Aerobic Processes

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Building the Biomarker Tree of Life (2005, background): “…remaining sedimentary organic matter is degraded further by anaerobic heterotrophic organisms such as sulfate reducers, fermenters and methanogens (Megonigal et al. 2004); the chemical structure of the remains is altered by biological and chemical processes (Hedges and Keil 1995; Hedges et al.…”
Bacterial Iron Oxidation in Circumneutral Freshwater Habitats: Findings from the Field and the Laboratory (2004, background): “It is this latter pathway that is now recognized as dominant mechanism for Fe-reduction (Nealson and Little 1997; Lovley 2000; Megonigal et al. 2004).”
Denitrification across landscapes and waterscapes: a synthesis. (2006, background): “Key words: continental shelf; denitrification; estuaries; lakes; nitrogen; oxygen minimum zones; rivers; sediments; soils.”
Permafrost Meta-Omics and Climate Change (2016, background): “Aerobic methane oxidation (thought to be much more important than anaerobic oxidation in terrestrial environments) is conducted by methanotrophic bacteria, which may consume 40–70% of gross wetland CH4 production globally (Megonigal et al. 2003).”
Plant species traits regulate methane production in freshwater wetland soils (2011, background): “Second, oxygen can directly inhibit CH4 production due to oxygen toxicity (Fridovich, 1998; Megonigal et al., 2004).”