Articles | Volume 20, issue 24
https://doi.org/10.5194/bg-20-5177-2023
https://doi.org/10.5194/bg-20-5177-2023
Research article
 | 
21 Dec 2023
Research article |  | 21 Dec 2023

Impact of seawater sulfate concentration on sulfur concentration and isotopic composition in calcite of two cultured benthic foraminifera

Caroline Thaler, Guillaume Paris, Marc Dellinger, Delphine Dissard, Sophie Berland, Arul Marie, Amandine Labat, and Annachiara Bartolini

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Referee Comment on egusphere-2023-631', Julien Richirt, 18 Apr 2023
    • AC1: 'Reply on RC1', Caroline Thaler, 08 Aug 2023
  • RC2: 'Comment on egusphere-2023-631', David Evans, 15 May 2023
    • AC2: 'Reply on RC2', Caroline Thaler, 08 Aug 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (13 Aug 2023) by Chiara Borrelli
AR by Caroline Thaler on behalf of the Authors (22 Aug 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (27 Aug 2023) by Chiara Borrelli
RR by Julien Richirt (28 Aug 2023)
RR by David Evans (19 Sep 2023)
ED: Publish subject to minor revisions (review by editor) (01 Oct 2023) by Chiara Borrelli
AR by Caroline Thaler on behalf of the Authors (22 Oct 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (28 Oct 2023) by Chiara Borrelli
AR by Caroline Thaler on behalf of the Authors (03 Nov 2023)  Author's response   Manuscript 
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Short summary
Our study focuses on one of the most used microfossils in paleoenvironmental reconstructions: foraminifera. We set up a novel approach of long-term cultures under variable and controlled conditions. Our results highlight that foraminiferal tests can be used as a unique record of both SO42−/CaCO3 and δ34S seawater variation. This establishes geological formations composed of biogenic carbonates as a potential repository of paleoenvironmental seawater sulfate chemical and geochemical variation.
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