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

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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.
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