Articles | Volume 15, issue 10
https://doi.org/10.5194/bg-15-3243-2018
https://doi.org/10.5194/bg-15-3243-2018
Research article
 | 
01 Jun 2018
Research article |  | 01 Jun 2018

Climate and marine biogeochemistry during the Holocene from transient model simulations

Joachim Segschneider, Birgit Schneider, and Vyacheslav Khon

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (08 Mar 2018) by Christoph Heinze
AR by Joachim Segschneider on behalf of the Authors (17 Apr 2018)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (25 Apr 2018) by Christoph Heinze
AR by Joachim Segschneider on behalf of the Authors (27 Apr 2018)  Author's response   Manuscript 
ED: Publish as is (02 May 2018) by Christoph Heinze
AR by Joachim Segschneider on behalf of the Authors (08 May 2018)  Author's response 
Download
Short summary
To gain a better understanding of climate and marine biogeochemistry variations over the last 9500 years (the Holocene), we performed non-accelerated model simulations with a global coupled climate and biogeochemistry model forced by orbital parameters and atmospheric greenhouse gases. One main outcome is an increase in the volume of the eastern equatorial Pacific oxygen minimum zone, driven by a slowdown of the large-scale circulation.
Altmetrics
Final-revised paper
Preprint