Articles | Volume 17, issue 7
https://doi.org/10.5194/bg-17-1933-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-1933-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Apr 2020
Research article |
| 09 Apr 2020
| 09 Apr 2020
Benthic foraminifera as tracers of brine production in the Storfjorden “sea ice factory”
Eleonora Fossile
CORRESPONDING AUTHOR
LPG-BIAF UMR-CNRS 6112, UNIV Angers, CNRS, UFR Sciences, 2 bd Lavoisier 49045, Angers CEDEX 01, France
Maria Pia Nardelli
LPG-BIAF UMR-CNRS 6112, UNIV Angers, CNRS, UFR Sciences, 2 bd Lavoisier 49045, Angers CEDEX 01, France
Arbia Jouini
LPG-BIAF UMR-CNRS 6112, UNIV Angers, CNRS, UFR Sciences, 2 bd Lavoisier 49045, Angers CEDEX 01, France
Bruno Lansard
LSCE, UMR 8212, IPSL-CEA-CNRS-UVSQ-Université Paris Saclay, 91198
Gif-sur-Yvette, France
Antonio Pusceddu
Department of Life and Environmental Sciences, University of
Cagliari, 09126 Cagliari, Italy
Davide Moccia
Department of Life and Environmental Sciences, University of
Cagliari, 09126 Cagliari, Italy
Elisabeth Michel
LSCE, UMR 8212, IPSL-CEA-CNRS-UVSQ-Université Paris Saclay, 91198
Gif-sur-Yvette, France
Olivier Péron
SUBATECH, UMR 6457, CNRS-Université de Nantes, 4 rue A. Kastler,
44307 Nantes, France
Hélène Howa
LPG-BIAF UMR-CNRS 6112, UNIV Angers, CNRS, UFR Sciences, 2 bd Lavoisier 49045, Angers CEDEX 01, France
Meryem Mojtahid
LPG-BIAF UMR-CNRS 6112, UNIV Angers, CNRS, UFR Sciences, 2 bd Lavoisier 49045, Angers CEDEX 01, France
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27 citations as recorded by crossref.
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Latest update: 13 Dec 2024
Short summary
This study focuses on benthic foraminiferal distribution in an Arctic fjord characterised by continuous sea ice production during winter and the consequent cascading of salty and corrosive waters (brine) to the seabed. The inner fjord is dominated by calcareous species (C). In the central deep basins, where brines are persistent, calcareous foraminifera are dissolved and agglutinated (A) dominate. The high A/C ratio is suggested as a proxy for brine persistence and sea ice production.
This study focuses on benthic foraminiferal distribution in an Arctic fjord characterised by...
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