Abstract
For energetic reasons, iron reduction suppresses methanogenesis in tidal freshwater wetlands; however, when iron reduction is limited by iron oxide availability, methanogenesis dominates anaerobic carbon mineralization. Plants can mediate this microbial competition by releasing oxygen into the rhizosphere and supplying oxidized iron for iron reducers. We utilized a plant removal experiment in two wetland sites to test the hypothesis that, in the absence of plants, rates of iron reduction would be diminished, allowing methanogenesis to dominate anaerobic metabolism. In both sites, methanogenesis was the primary anaerobic mineralization pathway, with iron reduction dominating only early and late in the growing season in the site with a less organic soil. These patterns were not influenced by the presence of plants, demonstrating that plants were not a key control of microbial metabolism. Instead, we suggest that site conditions, including soil chemistry, and temperature are important controls of the pathways of anaerobic metabolism.
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Acknowledgments
Chris Swarth at the Jug Bay Wetlands Sanctuary allowed unfettered access to our research sites for this project. We thank Jim Duls, Nick Mudd, Lucinda Williams, Pamela Weisenhorn, Sara McQueeney, Kyle Chambers, and Eric Pfoutz for assistance with field and laboratory work on this project. Comments from two anonymous reviewers greatly improved this manuscript. This research was supported by NSF DEB-0516400 to JPM and Smithsonian Post-Doctoral Fellowships to JKK and AES-G.
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Keller, J.K., Sutton-Grier, A.E., Bullock, A.L. et al. Anaerobic Metabolism in Tidal Freshwater Wetlands: I. Plant Removal Effects on Iron Reduction and Methanogenesis. Estuaries and Coasts 36, 457–470 (2013). https://doi.org/10.1007/s12237-012-9527-6
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DOI: https://doi.org/10.1007/s12237-012-9527-6