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Dissolved organic matter and inorganic mercury loadings increase methylmercury production, Clostridia abundance, and recalcitrant organic matter processing in oligotrophic sediments
View ORCID ProfileEmily B. Graham, Joseph E. Knelman, Rachel S. Gabor, Shon Schooler, Diane M. McKnight, Diana R. Nemergut
doi: https://doi.org/10.1101/072017
Emily B. Graham
1Biological Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA
Joseph E. Knelman
2Joint Genome Institute, US Department of Energy, Walnut Creek, CA, USA
Rachel S. Gabor
3Department of Geology and Geophysics, University of Utah, Salt Lake City, UT, USA
Shon Schooler
4Lake Superior National Estuarine Research Reserve, University of Wisconsin-Superior, Superior, WI, USA
Diane M. McKnight
5Institute for Arctic and Alpine Research, University of Colorado at Boulder, Boulder, CO, USA
6Civil Engineering Department, University of Colorado at Boulder, Boulder, CO, USA
7Environmental Studies Program, University of Colorado at Boulder, Boulder, CO, USA
Diana R. Nemergut
5Institute for Arctic and Alpine Research, University of Colorado at Boulder, Boulder, CO, USA
8Biology Department, Duke University, Durham, NC, USA
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Posted November 07, 2016.
Dissolved organic matter and inorganic mercury loadings increase methylmercury production, Clostridia abundance, and recalcitrant organic matter processing in oligotrophic sediments
Emily B. Graham, Joseph E. Knelman, Rachel S. Gabor, Shon Schooler, Diane M. McKnight, Diana R. Nemergut
bioRxiv 072017; doi: https://doi.org/10.1101/072017
Dissolved organic matter and inorganic mercury loadings increase methylmercury production, Clostridia abundance, and recalcitrant organic matter processing in oligotrophic sediments
Emily B. Graham, Joseph E. Knelman, Rachel S. Gabor, Shon Schooler, Diane M. McKnight, Diana R. Nemergut
bioRxiv 072017; doi: https://doi.org/10.1101/072017
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