Articles | Volume 16, issue 20
https://doi.org/10.5194/bg-16-4051-2019
https://doi.org/10.5194/bg-16-4051-2019
Research article
 | 
18 Oct 2019
Research article |  | 18 Oct 2019

Insights from mercury stable isotopes on terrestrial–atmosphere exchange of Hg(0) in the Arctic tundra

Martin Jiskra, Jeroen E. Sonke, Yannick Agnan, Detlev Helmig, and Daniel Obrist

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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) (14 Aug 2019) by Michael Weintraub
AR by Martin Jiskra on behalf of the Authors (22 Aug 2019)  Author's response    Manuscript
ED: Publish as is (11 Sep 2019) by Michael Weintraub
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Short summary
The tundra plays a pivotal role in Arctic mercury cycling by storing atmospheric mercury deposition and shuttling it to the Arctic Ocean. We used the isotopic fingerprint of mercury to investigate the processes controlling atmospheric mercury deposition. We found that the uptake of atmospheric mercury by vegetation was the major deposition source. Direct deposition to snow or soils only played a minor role. These results improve our understanding of Arctic mercury cycling.
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