Biogeosciences Discuss., doi:10.5194/bg-2016-314, 2016 Manuscript under review for journal Biogeosciences Published: 15 August 2016 c Author(s) 2016. CC-BY 3.0 License. Regulators of coastal wetland methane production and responses to simulated global change Carmella Vizza1, William E. West1, 2, Stuart E. Jones1, Julia A. Hart1, 3, and Gary A. Lamberti1 5 1Department of Biological Sciences, University of Notre Dame, Notre Dame, 46556, USA 2Kellogg Biological Station, Michigan State University, Hickory Corners, 49060, USA 3Center for Limnology, University of Wisconsin, Madison, 53706, USA Correspondence to: Carmella Vizza (
[email protected]) Abstract. Wetlands are the largest natural source of methane (CH4) to the atmosphere, but their emissions vary along 10 salinity and productivity gradients. Global change has the potential to reshape these gradients and therefore alter future contributions of wetlands to the global CH4 budget. Our study examined CH4 production along a natural salinity gradient in coastal Alaska wetlands. In the laboratory, we incubated natural sediments to compare CH4 production rates between freshwater and intertidal wetlands, and quantified the abundances of methanogens and sulfate-reducing bacteria in these ecosystems. We also simulated sea-level rise and enhanced organic matter availability, which we predicted would have 15 contrasting effects on coastal wetland CH4 production. Intertidal wetlands produced less CH4 than freshwater wetlands due to high sulfate availability and generally higher abundances of sulfate-reducing bacteria, whereas freshwater wetlands had significantly greater methanogen abundances. Simulated sea-level rise in freshwater sediments, however, did not reduce CH4 production, perhaps because the 14d incubation period was too short to elicit a shift in microbial communities.