Articles | Volume 13, issue 9
https://doi.org/10.5194/cp-13-1097-2017
https://doi.org/10.5194/cp-13-1097-2017
Research article
 | 
05 Sep 2017
Research article |  | 05 Sep 2017

Deglacial sea level history of the East Siberian Sea and Chukchi Sea margins

Thomas M. Cronin, Matt O'Regan, Christof Pearce, Laura Gemery, Michael Toomey, Igor Semiletov, and Martin Jakobsson

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (13 Jul 2017) by Carlo Barbante
AR by Anna Mirena Feist-Polner on behalf of the Authors (17 Jul 2017)  Author's response
ED: Publish as is (31 Jul 2017) by Carlo Barbante
AR by Thomas M. Cronin on behalf of the Authors (31 Jul 2017)  Author's response    Manuscript
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Short summary
Global sea level rise during the last deglacial flooded the Siberian continental shelf in the Arctic Ocean. Sediment cores, radiocarbon dating, and microfossils show that the regional sea level in the Arctic rose rapidly from about 12 500 to 10 700 years ago. Regional sea level history on the Siberian shelf differs from the global deglacial sea level rise perhaps due to regional vertical adjustment resulting from the growth and decay of ice sheets.