Volume 32, Issue 5 pp. 587-603
Research Article

Semi-quantitative reconstruction of early to late Holocene spring and summer sea ice conditions in the northern Barents Sea

Sarah M. P. Berben

Corresponding Author

Sarah M. P. Berben

Department of Geology, UiT – The Arctic University of Norway, Tromsø, N-9037, Norway

Correspondence: S. M. P. Berben. Current address: Department of Earth Science, University of Bergen and the Bjerknes Centre for Climate Research, N-5007 Bergen, Norway.

E-mail: [email protected]

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Katrine Husum

Katrine Husum

Fram Centre, Norwegian Polar Institute, Tromsø, N-9296, Norway

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Alba Navarro-Rodriguez

Alba Navarro-Rodriguez

Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK

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Simon T. Belt

Simon T. Belt

Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK

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Steffen Aagaard-Sørensen

Steffen Aagaard-Sørensen

Department of Geology, UiT – The Arctic University of Norway, Tromsø, N-9037, Norway

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First published: 07 June 2017
Citations: 37

ABSTRACT

Semi-quantitative estimates of early to late Holocene spring sea ice concentration (SpSIC) and occurrence of summer sea ice for the northern Barents Sea have been obtained by analysing the biomarkers IP25, brassicasterol and a tri-unsaturated highly branched isoprenoid lipid in a Holocene marine sediment core. Sub-surface water mass variations were derived from planktic foraminiferal assemblages and stable isotopes (δ18O, δ13C). The record indicates paleoceanographic changes over three intervals. During Period I (ca. 9500–5900 cal a BP), the study location experienced the lowest recorded SpSIC (ca. 25%) with short spring seasons and long productive summers, resulting partly from increased Atlantic Water inflow that caused a stronger ocean–atmosphere heat exchange. Throughout Period II (ca. 5900–2700 cal a BP), the winter sea ice margin migrated southwards and an overall cooling trend resulted in higher SpSIC (ca. 60%) and increased delivery of cold Arctic Water. During Period III (ca. 2700 cal a BP to present), SpSIC increased further (ca. 75%) and some sea ice remained during summer months. A sub-surface warming probably indicates a decoupling of heat exchange between the ocean and the atmosphere. Longer springs and shorter summers were accompanied by the most southerly location of the winter sea ice margin.

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