Articles | Volume 37, issue 2
https://doi.org/10.5194/jm-37-403-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/jm-37-403-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Assessing proxy signatures of temperature, salinity, and hypoxia in the Baltic Sea through foraminifera-based geochemistry and faunal assemblages
Jeroen Groeneveld
CORRESPONDING AUTHOR
Center for Marine Environmental Sciences (MARUM), University of
Bremen, Klagenfurter Strasse 2–4, 28359 Bremen, Germany
Department of Geology, Lund University, Sölvegatan 12, 223 62
Lund, Sweden
Helena L. Filipsson
Department of Geology, Lund University, Sölvegatan 12, 223 62
Lund, Sweden
William E. N. Austin
School of Geography and Sustainable Development, University of St.
Andrews, North Street, St. Andrews, KY16 9AL, UK
Scottish Association for Marine Science, Scottish Marine Institute,
Oban, PA37 1AQ, UK
Kate Darling
School of Geography and Sustainable Development, University of St.
Andrews, North Street, St. Andrews, KY16 9AL, UK
School of Geosciences, University of Edinburgh, James Hutton Road,
Edinburgh, EH9 3FE, UK
David McCarthy
School of Geography and Sustainable Development, University of St.
Andrews, North Street, St. Andrews, KY16 9AL, UK
Nadine B. Quintana Krupinski
Department of Geology, Lund University, Sölvegatan 12, 223 62
Lund, Sweden
Clare Bird
School of Geosciences, University of Edinburgh, James Hutton Road,
Edinburgh, EH9 3FE, UK
Biological and Environmental Sciences, University of Stirling,
Stirling, FK9 4LA, UK
Magali Schweizer
School of Geosciences, University of Edinburgh, James Hutton Road,
Edinburgh, EH9 3FE, UK
LPG-BIAF UMR CNRS 6112, University of Angers, 2 bd Lavoisier, 49045
Angers CEDEX 01, France
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Cited
33 citations as recorded by crossref.
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Latest update: 06 Jan 2025
Short summary
Current climate and environmental changes strongly affect shallow marine and coastal areas like the Baltic Sea. The combination of foraminiferal geochemistry and environmental parameters demonstrates that in a highly variable setting like the Baltic Sea, it is possible to separate different environmental impacts on the foraminiferal assemblages and therefore use chemical factors to reconstruct how seawater temperature, salinity, and oxygen varied in the past and may vary in the future.
Current climate and environmental changes strongly affect shallow marine and coastal areas like...