Articles | Volume 20, issue 1
https://doi.org/10.5194/bg-20-121-2023
https://doi.org/10.5194/bg-20-121-2023
Research article
 | 
09 Jan 2023
Research article |  | 09 Jan 2023

Paleoecology and evolutionary response of planktonic foraminifera to the mid-Pliocene Warm Period and Plio-Pleistocene bipolar ice sheet expansion

Adam Woodhouse, Frances A. Procter, Sophie L. Jackson, Robert A. Jamieson, Robert J. Newton, Philip F. Sexton, and Tracy Aze

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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-2022-844', Anonymous Referee #1, 17 Oct 2022
    • AC1: 'Reply on RC1', Adam Woodhouse, 08 Nov 2022
  • RC2: 'Comment on egusphere-2022-844', Anonymous Referee #2, 02 Nov 2022
    • AC2: 'Reply on RC2', Adam Woodhouse, 08 Nov 2022

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) (10 Nov 2022) by Petr Kuneš
AR by Adam Woodhouse on behalf of the Authors (10 Nov 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (18 Nov 2022) by Petr Kuneš
AR by Adam Woodhouse on behalf of the Authors (14 Dec 2022)
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Short summary
This study looked into the regional and global response of planktonic foraminifera to the climate over the last 5 million years, when the Earth cooled significantly. These single celled organisms exhibit the best fossil record available to science. We document an abundance switch from warm water to cold water species as the Earth cooled. Moreover, a closer analysis of certain species may indicate higher fossil diversity than previously thought, which has implications for evolutionary studies.
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