Semi-quantitative reconstruction of early to late Holocene spring and summer sea ice conditions in the northern Barents Sea
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]
Search for more papers by this authorKatrine Husum
Fram Centre, Norwegian Polar Institute, Tromsø, N-9296, Norway
Search for more papers by this authorAlba Navarro-Rodriguez
Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK
Search for more papers by this authorSimon T. Belt
Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK
Search for more papers by this authorSteffen Aagaard-Sørensen
Department of Geology, UiT – The Arctic University of Norway, Tromsø, N-9037, Norway
Search for more papers by this authorCorresponding 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]
Search for more papers by this authorKatrine Husum
Fram Centre, Norwegian Polar Institute, Tromsø, N-9296, Norway
Search for more papers by this authorAlba Navarro-Rodriguez
Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK
Search for more papers by this authorSimon T. Belt
Biogeochemistry Research Centre, School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK
Search for more papers by this authorSteffen Aagaard-Sørensen
Department of Geology, UiT – The Arctic University of Norway, Tromsø, N-9037, Norway
Search for more papers by this authorABSTRACT
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.
Supporting Information
Additional supporting information related to this article may be found in the online version of this article.
Filename | Description |
---|---|
jqs2953-sup-0001-SuppTable-S1.xlsx212.1 KB | Table S1. CTD data presented in Fig. |
jqs2953-sup-0002-SuppTable-S2.xlsx12 KB | Table S2. Age model presented in Fig. |
jqs2953-sup-0003-SuppTable-S3.xlsx16.7 KB | Table S3. Biomarker data presented in Fig. |
jqs2953-sup-0004-SuppTable-S4.xlsx14.4 KB | Table S4. Foraminiferal fauna data presented in Fig. |
jqs2953-sup-0005-SuppTable-S5.xlsx20.8 KB | Table S5. Stable isotope data presented in Fig. |
Please note: The publisher is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.
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