Articles | Volume 16, issue 2
Clim. Past, 16, 523–541, 2020
Clim. Past, 16, 523–541, 2020

Research article 12 Mar 2020

Research article | 12 Mar 2020

A new age model for the Pliocene of the southern North Sea basin: a multi-proxy climate reconstruction

Emily Dearing Crampton-Flood et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (07 Nov 2019) by Arne Winguth
AR by Emily Dearing Crampton Flood on behalf of the Authors (06 Jan 2020)  Author's response    Manuscript
ED: Publish as is (06 Feb 2020) by Arne Winguth
Short summary
The mid-Pliocene warm period (mPWP; 3.3–3.0 million years ago) is thought to be the last geological interval with similar atmospheric carbon dioxide concentrations as the present day. Further, the mPWP was 2–3 °C warmer than present, making it a good analogue for estimating the effects of future climate change. Here, we construct a new precise age model for the North Sea during the mPWP, and provide a detailed reconstruction of terrestrial and marine climate using a multi-proxy approach.