Articles | Volume 18, issue 6
https://doi.org/10.5194/bg-18-2139-2021
https://doi.org/10.5194/bg-18-2139-2021
Research article
 | 
24 Mar 2021
Research article |  | 24 Mar 2021

Organic carbon densities and accumulation rates in surface sediments of the North Sea and Skagerrak

Markus Diesing, Terje Thorsnes, and Lilja Rún Bjarnadóttir

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (15 Dec 2020) by Jack Middelburg
ED: Reconsider after major revisions (16 Dec 2020) by Jack Middelburg
AR by Markus Diesing on behalf of the Authors (20 Jan 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (20 Jan 2021) by Jack Middelburg
RR by Anonymous Referee #2 (29 Jan 2021)
RR by Anonymous Referee #1 (12 Feb 2021)
ED: Publish subject to minor revisions (review by editor) (12 Feb 2021) by Jack Middelburg
AR by Markus Diesing on behalf of the Authors (18 Feb 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (18 Feb 2021) by Jack Middelburg
AR by Markus Diesing on behalf of the Authors (22 Feb 2021)  Author's response    Manuscript
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Short summary
The upper 10 cm of the seafloor of the North Sea and Skagerrak contain 231×106 t of carbon in organic form. The Norwegian Trough, the deepest sedimentary basin in the studied area, stands out as a zone of strong organic carbon accumulation with rates on par with neighbouring fjords. Conversely, large parts of the North Sea are characterised by rapid organic carbon degradation and negligible accumulation. This dual character is likely typical for continental shelf sediments worldwide.
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