Articles | Volume 21, issue 2
https://doi.org/10.5194/cp-21-571-2025
https://doi.org/10.5194/cp-21-571-2025
Research article
 | 
28 Feb 2025
Research article |  | 28 Feb 2025

Sediment fluxes dominate glacial–interglacial changes in ocean carbon inventory: results from factorial simulations over the past 780 000 years

Markus Adloff, Aurich Jeltsch-Thömmes, Frerk Pöppelmeier, Thomas F. Stocker, and Fortunat Joos

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (28 Oct 2024) by Qiuzhen Yin
AR by Markus Adloff on behalf of the Authors (31 Oct 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (06 Nov 2024) by Qiuzhen Yin
RR by Anonymous Referee #2 (30 Nov 2024)
RR by Anonymous Referee #1 (07 Dec 2024)
ED: Publish subject to minor revisions (review by editor) (17 Dec 2024) by Qiuzhen Yin
AR by Markus Adloff on behalf of the Authors (23 Dec 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (05 Jan 2025) by Qiuzhen Yin
AR by Markus Adloff on behalf of the Authors (11 Jan 2025)
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Short summary
We simulated how different processes affected the carbon cycle over the last eight glacial cycles. We found that the effects of interactive marine sediments enlarge the carbon fluxes that result from these processes, especially in the ocean, and alter various proxy signals. We provide an assessment of the directions of regional and global proxy changes that might be expected in response to different glacial–interglacial Earth system changes in the presence of interactive marine sediments.
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