Articles | Volume 11, issue 3
https://doi.org/10.5194/cp-11-587-2015
https://doi.org/10.5194/cp-11-587-2015
Research article
 | 
27 Mar 2015
Research article |  | 27 Mar 2015

Late Weichselian and Holocene palaeoceanography of Storfjordrenna, southern Svalbard

M. Łącka, M. Zajączkowski, M. Forwick, and W. Szczuciński

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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
AR by Magdalena Łącka on behalf of the Authors (23 Oct 2014)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by Editor) (01 Dec 2014) by Andrea Dutton
AR by Magdalena Łącka on behalf of the Authors (11 Dec 2014)  Author's response   Manuscript 
ED: Reconsider after major revisions (20 Jan 2015) by Denis-Didier Rousseau
AR by Magdalena Łącka on behalf of the Authors (22 Jan 2015)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (23 Jan 2015) by Denis-Didier Rousseau
RR by Thomas M. Cronin (27 Jan 2015)
RR by Anonymous Referee #2 (06 Feb 2015)
ED: Publish subject to technical corrections (26 Feb 2015) by Denis-Didier Rousseau
AR by Magdalena Łącka on behalf of the Authors (27 Feb 2015)  Author's response   Manuscript 
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Short summary
Storfjordrenna was deglaciated about 13,950 cal yr BP. During the transition from the sub-glacial to glaciomarine setting, Arctic Waters dominated its hydrography. However, the waters were not uniformly cold and experienced several warmer spells. Atlantic Water began to flow onto the shelves off Svalbard and into Storfjorden during the early Holocene, leading to progressive warming and significant glacial melting. A surface-water cooling and freshening occurred in late Holocene.