Journal Article
mSystems, vol. 4, iss. 6, 2019
Authors
Adrienne B. Narrowe, Mikayla A. Borton, David W. Hoyt, Garrett J. Smith, Rebecca A. Daly, Jordan C. Angle, Elizabeth K. Eder, Allison R. Wong, Richard A. Wolfe, Alexandra Pappas, Gil Bohrer, Christopher S. Miller, Kelly C. Wrighton, William Orsi
Abstract
Understanding the sources and controls on microbial methane production from wetland soils is critical to global methane emission predictions, particularly in light of changing climatic conditions. Current biogeochemical models of methanogenesis consider only acetoclastic and hydrogenotrophic sources and exclude methylotrophic methanogenesis, potentially underestimating microbial contributions to methane flux. Our multi-omic results demonstrated that methylotrophic methanogens of the family
Methanomassiliicoccaceae
were present and active in a freshwater wetland, with metatranscripts indicating that methanol, not methylamines, was the likely substrate under the conditions measured here. However, laboratory experiments indicated the potential for other methanogens to become enriched in response to trimethylamine, revealing the reservoir of methylotrophic methanogenesis potential residing in these soils. Collectively, our approach used coupled field and laboratory investigations to illuminate metabolisms influencing the terrestrial microbial methane cycle, thereby offering direction for increased realism in predictive process-oriented models of methane flux in wetland soils.
