Articles | Volume 15, issue 2
https://doi.org/10.5194/bg-15-507-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/bg-15-507-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
26 Jan 2018
Research article |
| 26 Jan 2018
| 26 Jan 2018
Glacial–interglacial changes and Holocene variations in Arabian Sea denitrification
Birgit Gaye
CORRESPONDING AUTHOR
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Anna Böll
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Joachim Segschneider
Institute for Geosciences, Universität Kiel,
Ludewig-Meyn-Straße 10, 24118 Kiel, Germany
Nicole Burdanowitz
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Kay-Christian Emeis
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Institute of Coastal Research, Helmholtz Center Geesthacht,
Max-Planck-Straße 1, 21502 Geesthacht, Germany
Venkitasubramani Ramaswamy
National Institute of Oceanography, Dona Paula, Goa, 403004, India
Niko Lahajnar
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Andreas Lückge
Bundesanstalt für Geowissenschaften und Rohstoffe, Stilleweg 2,
30655 Hannover, Germany
Tim Rixen
Institute for Geology, Universität Hamburg, Bundesstraße 55,
20146 Hamburg, Germany
Leibniz-Zentrum für Marine Tropenforschung (ZMT) GmbH,
Fahrenheitstraße 6, 28359 Bremen, Germany
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33 citations as recorded by crossref.
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Discussed (final revised paper)
Latest update: 18 Apr 2024
Short summary
The Arabian Sea has one of the most severe oxygen minima of the world's oceans between about 100 and 1200 m of water depth and is therefore a major oceanic nitrogen sink. Stable nitrogen isotopic ratios in sediments record changes in oxygen concentrations and were studied for the last 25 kyr. Oxygen concentrations dropped at the end of the last glacial and became further reduced during the Holocene, probably due to the increasing age of the low-oxygen water mass.
The Arabian Sea has one of the most severe oxygen minima of the world's oceans between about 100...
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