Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-379-2021
https://doi.org/10.5194/cp-17-379-2021
Research article
 | 
08 Feb 2021
Research article |  | 08 Feb 2021

Response of biological productivity to North Atlantic marine front migration during the Holocene

David J. Harning, Anne E. Jennings, Denizcan Köseoğlu, Simon T. Belt, Áslaug Geirsdóttir, and Julio Sepúlveda

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (03 Dec 2020) by Bjørg Risebrobakken
AR by David Harning on behalf of the Authors (03 Dec 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (21 Dec 2020) by Bjørg Risebrobakken
AR by David Harning on behalf of the Authors (22 Dec 2020)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (04 Jan 2021) by Bjørg Risebrobakken
AR by David Harning on behalf of the Authors (04 Jan 2021)  Author's response   Manuscript 
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Short summary
Today, the waters north of Iceland are characterized by high productivity that supports a diverse food web. However, it is not known how this may change and impact Iceland's economy with future climate change. Therefore, we explored how the local productivity has changed in the past 8000 years through fossil and biogeochemical indicators preserved in Icelandic marine mud. We show that this productivity relies on the mixing of Atlantic and Arctic waters, which migrate north under warming.