Articles | Volume 13, issue 4
https://doi.org/10.5194/cp-13-333-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-333-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
10 Apr 2017
Research article |
| 10 Apr 2017
Holocene evolution of the North Atlantic subsurface transport
Institute of Geosciences, Kiel University, 24118 Kiel, Germany
now at: Climate Geochemistry Department, Max Planck Institute for Chemistry,
55128 Mainz, Germany
Dieter Garbe-Schönberg
Institute of Geosciences, Kiel University, 24118 Kiel, Germany
Mara Weinelt
Institute of Prehistoric and Protohistoric Archaeology, Kiel
University, 24118 Kiel, Germany
Ralph Schneider
Institute of Geosciences, Kiel University, 24118 Kiel, Germany
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Latest update: 14 Dec 2024
Short summary
We reconstruct changes in the warm water transport from the subtropical to the subpolar North Atlantic over the last 10 000 years. We use stable isotope and Mg / Ca ratios measured on surface and subsurface dwelling foraminifera. Results indicate an overall stable warm water transport at surface. The northward transport at subsurface evolves stepwise and stabilizes at 7 ka BP on the modern mode. These ocean transport changes seem to be controlled by the meltwater inflow into the North Atlantic.
We reconstruct changes in the warm water transport from the subtropical to the subpolar North...
