Articles | Volume 22, issue 12
https://doi.org/10.5194/bg-22-3029-2025
https://doi.org/10.5194/bg-22-3029-2025
Research article
 | 
30 Jun 2025
Research article |  | 30 Jun 2025

Controls on Palaeogene deep-sea diatom-bearing sediment deposition and comparison with shallow marine environments

Cécile Figus, Johan Renaudie, Or M. Bialik, and Jakub Witkowski

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-3768', Eunah Han, 06 Jan 2025
    • AC1: 'Reply on RC1', Cécile Figus, 24 Jan 2025
  • RC2: 'Comment on egusphere-2024-3768', Anonymous Referee #2, 14 Feb 2025
    • AC2: 'Reply on RC2', Cécile Figus, 25 Feb 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (06 Mar 2025) by Mark Lever
AR by Cécile Figus on behalf of the Authors (10 Mar 2025)  Author's response   Author's tracked changes   Manuscript 
EF by Katja Gänger (11 Mar 2025)  Supplement 
ED: Reconsider after major revisions (28 Mar 2025) by Mark Lever
ED: Referee Nomination & Report Request started (28 Mar 2025) by Mark Lever
RR by Anonymous Referee #2 (02 Apr 2025)
ED: Publish subject to minor revisions (review by editor) (02 Apr 2025) by Mark Lever
AR by Cécile Figus on behalf of the Authors (02 Apr 2025)  Author's response   Author's tracked changes   Manuscript 
EF by Daria Karpachova (02 Apr 2025)  Supplement 
ED: Publish as is (02 Apr 2025) by Mark Lever
AR by Cécile Figus on behalf of the Authors (03 Apr 2025)
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Short summary
The synthesis of Palaeogene deep-sea diatom-bearing sediment occurrences indicates that the deposition of diatom-bearing sediments is mainly controlled by nutrient availability and ocean circulation in the Atlantic, Pacific, and Indian oceans. Comparison with shallow marine diatomites suggests that the peak in the number of diatom-bearing sites in the Atlantic is indirectly related to tectonic reorganizations that caused the cessation of shallow marine diatomite deposition between ~46 and ~44 Ma.
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