Articles | Volume 18, issue 22
https://doi.org/10.5194/bg-18-5891-2021
https://doi.org/10.5194/bg-18-5891-2021
Research article
 | 
16 Nov 2021
Research article |  | 16 Nov 2021

Particulate biogenic barium tracer of mesopelagic carbon remineralization in the Mediterranean Sea (PEACETIME project)

Stéphanie H. M. Jacquet, Christian Tamburini, Marc Garel, Aurélie Dufour, France Van Vambeke, Frédéric A. C. Le Moigne, Nagib Bhairy, and Sophie Guasco

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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) (21 Apr 2021) by Christine Klaas
ED: Publish subject to minor revisions (review by editor) (21 Apr 2021) by Christine Klaas (Co-editor-in-chief)
AR by Stéphanie Jacquet on behalf of the Authors (21 Apr 2021)  Author's response   Author's tracked changes 
ED: Publish subject to minor revisions (review by editor) (07 Jun 2021) by Christine Klaas
ED: Publish subject to minor revisions (review by editor) (07 Jun 2021) by Christine Klaas (Co-editor-in-chief)
AR by Stéphanie Jacquet on behalf of the Authors (06 Sep 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (29 Sep 2021) by Christine Klaas
ED: Publish subject to technical corrections (29 Sep 2021) by Christine Klaas (Co-editor-in-chief)
AR by Stéphanie Jacquet on behalf of the Authors (11 Oct 2021)  Manuscript 
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Short summary
We compared carbon remineralization rates (MRs) in the western and central Mediterranean Sea in late spring during the PEACETIME cruise, as assessed using the barium tracer. We reported higher and deeper (up to 1000 m depth) MRs in the western basin, potentially sustained by an additional particle export event driven by deep convection. The central basin is the site of a mosaic of blooming and non-blooming water masses and showed lower MRs that were restricted to the upper mesopelagic layer.
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