Abstract: Soil Redox Conditions Are a Strong Determinant of Microbial Community Composition and the Fate of Carbon Following Permafrost Thaw. (2016 AGU Fall Meeting)

Soil Redox Conditions Are a Strong Determinant of Microbial Community Composition and the Fate of Carbon Following Permafrost Thaw.

Eric Matthew Bottos¹, Lisa Bramer¹, Young-Mo Kim², Sarah Fansler³, Carrie Nicora⁴, Erika Zink⁵, Rosalie Kae Chu², Malak M Tfaily⁶, Thomas O Metz¹, Janet Jansson⁷ and James Stegen¹, (1)Pacific Northwest National Laboratory, Richland, WA, United States, (2)Pacific Northwest National Laboratory, Environmental Molecular Sciences Laboratory, Richland, WA, United States, (3)Battelle PNNL, Richland, United States, (4)Pacific Northwest National Laboratory, Earth and Biological Sciences Directorate, Richland, United States, (5)Pacific Northwest National Laboratory, Biological Sciences Division, Richland, WA, United States, (6)University of Arizona, Department of Environmental Sciences, Tucson, United States, (7)Pacific Northwest National Laboratory, Earth and Biological Sciences, Richland, WA, United States

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