Articles | Volume 14, issue 6
Earth Syst. Sci. Data, 14, 2553–2611, 2022
https://doi.org/10.5194/essd-14-2553-2022
Earth Syst. Sci. Data, 14, 2553–2611, 2022
https://doi.org/10.5194/essd-14-2553-2022
Data description paper
08 Jun 2022
Data description paper | 08 Jun 2022

World Atlas of late Quaternary Foraminiferal Oxygen and Carbon Isotope Ratios

Stefan Mulitza et al.

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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 essd-2021-337', Ralf Schiebel, 03 Dec 2021
  • RC2: 'Comment on essd-2021-337', Anonymous Referee #2, 06 Jan 2022
  • RC3: 'Comment on essd-2021-337', Stefano Bernasconi, 10 Jan 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Stefan Mulitza on behalf of the Authors (16 Mar 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (review by editor) (01 Apr 2022) by Kirsten Elger
AR by Stefan Mulitza on behalf of the Authors (13 Apr 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (26 Apr 2022) by Kirsten Elger
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Short summary
Stable isotope ratios of foraminiferal shells from deep-sea sediments preserve key information on the variability of ocean circulation and ice volume. We present the first global atlas of harmonized raw downcore oxygen and carbon isotope ratios of various planktonic and benthic foraminiferal species. The atlas is a foundation for the analyses of the history of Earth system components, for finding future coring sites, and for teaching marine stratigraphy and paleoceanography.