Articles | Volume 16, issue 16
https://doi.org/10.5194/bg-16-3207-2019
https://doi.org/10.5194/bg-16-3207-2019
Research article
 | 
29 Aug 2019
Research article |  | 29 Aug 2019

The ratio of methanogens to methanotrophs and water-level dynamics drive methane transfer velocity in a temperate kettle-hole peat bog

Camilo Rey-Sanchez, Gil Bohrer, Julie Slater, Yueh-Fen Li, Roger Grau-Andrés, Yushan Hao, Virginia I. Rich, and G. Matt Davies

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (18 Jul 2019) by Tina Treude
AR by Camilo Rey Sanchez on behalf of the Authors (20 Jul 2019)  Author's response    Manuscript
ED: Publish as is (31 Jul 2019) by Tina Treude
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Short summary
It is estimated that natural wetlands emit approximately 30 % of all the methane released to the atmosphere; yet these estimates are highly uncertain due to the complexity of biological, chemical, and physical processes controlling methane emissions. In this study, we explore how some of these key processes drive methane emissions in a temperate peat bog. We show that the composition of microbial methane cyclers in the upper portion of the peat drives the velocity of methane release to the air.
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