Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2547-2020
https://doi.org/10.5194/cp-16-2547-2020
Review article
 | Highlight paper
 | 
23 Dec 2020
Review article | Highlight paper |  | 23 Dec 2020

Plateaus and jumps in the atmospheric radiocarbon record – potential origin and value as global age markers for glacial-to-deglacial paleoceanography, a synthesis

Michael Sarnthein, Kevin Küssner, Pieter M. Grootes, Blanca Ausin, Timothy Eglinton, Juan Muglia, Raimund Muscheler, and Gordon Schlolaut

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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 (19 Mar 2020) by André Paul
AR by Michael Sarnthein on behalf of the Authors (27 Mar 2020)
ED: Referee Nomination & Report Request started (09 Apr 2020) by André Paul
RR by Anonymous Referee #2 (12 May 2020)
ED: Publish subject to minor revisions (review by editor) (19 May 2020) by André Paul
AR by Michael Sarnthein on behalf of the Authors (10 Jun 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (24 Jun 2020) by André Paul
AR by Michael Sarnthein on behalf of the Authors (16 Jul 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (30 Jul 2020) by André Paul
AR by Michael Sarnthein on behalf of the Authors (07 Aug 2020)  Author's response   Manuscript 
ED: Publish subject to technical corrections (16 Nov 2020) by André Paul
AR by Michael Sarnthein on behalf of the Authors (17 Nov 2020)  Manuscript 
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Short summary
The dating technique of 14C plateau tuning uses U/Th-based model ages, refinements of the Lake Suigetsu age scale, and the link of surface ocean carbon to the globally mixed atmosphere as basis of age correlation. Our synthesis employs data of 20 sediment cores from the global ocean and offers a coherent picture of global ocean circulation evolving over glacial-to-deglacial times on semi-millennial scales to be compared with climate records stored in marine sediments, ice cores, and speleothems.