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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 1
Clim. Past, 10, 293–303, 2014
https://doi.org/10.5194/cp-10-293-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 10, 293–303, 2014
https://doi.org/10.5194/cp-10-293-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 10 Feb 2014

Research article | 10 Feb 2014

Deglacial intermediate water reorganization: new evidence from the Indian Ocean

S. Romahn1, A. Mackensen1, J. Groeneveld2, and J. Pätzold2 S. Romahn et al.
  • 1Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Am Alten Hafen 26, 27568 Bremerhaven, Germany
  • 2MARUM – Center for Marine Environmental Sciences, Bremen University, Leobener Straße, 28359 Bremen, Germany

Abstract. The importance of intermediate water masses in climate change and ocean circulation has been emphasized recently. In particular, Southern Ocean Intermediate Waters (SOIW), such as Antarctic Intermediate Water and Subantarctic Mode Water, are thought to have acted as active interhemispheric transmitter of climate anomalies. Here we reconstruct changes in SOIW signature and spatial and temporal evolution based on a 40 kyr time series of oxygen and carbon isotopes as well as planktic Mg/Ca based thermometry from Site GeoB12615-4 in the western Indian Ocean. Our data suggest that SOIW transmitted Antarctic temperature trends to the equatorial Indian Ocean via the "oceanic tunnel" mechanism. Moreover, our results reveal that deglacial SOIW carried a signature of aged Southern Ocean deep water. We find no evidence of increased formation of intermediate waters during the deglaciation.

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