Articles | Volume 19, issue 12
https://doi.org/10.5194/cp-19-2569-2023
https://doi.org/10.5194/cp-19-2569-2023
Research article
 | 
20 Dec 2023
Research article |  | 20 Dec 2023

Warming drove the expansion of marine anoxia in the equatorial Atlantic during the Cenomanian leading up to Oceanic Anoxic Event 2

Mohd Al Farid Abraham, Bernhard David A. Naafs, Vittoria Lauretano, Fotis Sgouridis, and Richard D. Pancost

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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-2023-260', Alexandre Pohl, 27 Apr 2023
  • RC2: 'Comment on egusphere-2023-260', Anonymous Referee #2, 03 Jul 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (22 Sep 2023) by Luc Beaufort
AR by Mohd Al Farid Abraham on behalf of the Authors (11 Oct 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (24 Oct 2023) by Luc Beaufort
AR by Mohd Al Farid Abraham on behalf of the Authors (24 Oct 2023)
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Short summary
Oceanic Anoxic Event 2 (OAE 2), about 93.5 million years ago, is characterized by widespread deoxygenated ocean and massive burial of organic-rich sediments. Our results show that the marine deoxygenation at the equatorial Atlantic that predates the OAE 2 interval was driven by global warming and associated with the nutrient status of the site, with factors like temperature-modulated upwelling and hydrology-induced weathering contributing to enhanced nutrient delivery over various timescales.