Articles | Volume 11, issue 3
https://doi.org/10.5194/cp-11-587-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-11-587-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Late Weichselian and Holocene palaeoceanography of Storfjordrenna, southern Svalbard
M. Łącka
CORRESPONDING AUTHOR
Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, 81-712 Sopot, Poland
M. Zajączkowski
Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, 81-712 Sopot, Poland
M. Forwick
Department of Geology, University of Tromsø – The Arctic University of Norway, 9037 Tromsø, Norway
W. Szczuciński
Institute of Geology, Adam Mickiewicz University in Poznan, Maków Polnych 16, 61-606 Poznań, Poland
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30 citations as recorded by crossref.
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Latest update: 21 Nov 2024
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.
Storfjordrenna was deglaciated about 13,950 cal yr BP. During the transition from the...