Articles | Volume 17, issue 24
https://doi.org/10.5194/bg-17-6507-2020
https://doi.org/10.5194/bg-17-6507-2020
Research article
 | 
23 Dec 2020
Research article |  | 23 Dec 2020

A new intermittent regime of convective ventilation threatens the Black Sea oxygenation status

Arthur Capet, Luc Vandenbulcke, and Marilaure Grégoire

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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: Reconsider after major revisions (19 Aug 2020) by Katja Fennel
ED: Reconsider after major revisions (19 Aug 2020) by Katja Fennel (Co-editor-in-chief)
AR by Arthur Capet on behalf of the Authors (24 Sep 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (05 Oct 2020) by Katja Fennel
RR by Fabian Große (25 Oct 2020)
ED: Publish subject to minor revisions (review by editor) (27 Oct 2020) by Katja Fennel
ED: Publish subject to minor revisions (review by editor) (30 Oct 2020) by Katja Fennel (Co-editor-in-chief)
AR by Arthur Capet on behalf of the Authors (13 Nov 2020)  Author's response   Manuscript 
ED: Publish as is (16 Nov 2020) by Katja Fennel
ED: Publish as is (16 Nov 2020) by Katja Fennel (Co-editor-in-chief)
AR by Arthur Capet on behalf of the Authors (17 Nov 2020)
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Short summary
The Black Sea is 2000 m deep, but, due to limited ventilation, only about the upper 100 m contains enough oxygen to support marine life such as fish. This oxygenation depth has been shown to be decreasing (1955–2019). Here, we evidence that atmospheric warming induced a clear shift in an important ventilation mechanism. We highlight the impact of this shift on oxygenation. There are important implications for marine life and carbon and nutrient cycling if this new ventilation regime persists.
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