Articles | Volume 13, issue 5
https://doi.org/10.5194/cp-13-491-2017
© 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-13-491-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Decadal resolution record of Oman upwelling indicates solar forcing of the Indian summer monsoon (9–6 ka)
Philipp M. Munz
CORRESPONDING AUTHOR
Senckenberg Centre for Human Evolution and Palaeoenvironment (HEP) at the University of Tübingen, Hölderlinstr. 12, 72074 Tübingen, Germany
Department of Geosciences, University of Tübingen, Hölderlinstr. 12, 72074 Tübingen, Germany
Stephan Steinke
Department of Geological Oceanography, Xiamen University, Xiping Building, Xiang'an South Road, Xiamen 361102, China
Anna Böll
Institute of Geology, University of Hamburg, Bundesstr. 55, 20146 Hamburg, Germany
Andreas Lückge
Bundesanstalt für Geowissenschaften und Rohstoffe (BGR), Stilleweg 2, 30655 Hannover, Germany
Jeroen Groeneveld
MARUM – Center for Marine Environmental Sciences, Germany, Leobener Str., 28359 Bremen, Germany
Michal Kucera
MARUM – Center for Marine Environmental Sciences, Germany, Leobener Str., 28359 Bremen, Germany
Hartmut Schulz
Department of Geosciences, University of Tübingen, Hölderlinstr. 12, 72074 Tübingen, Germany
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Latest update: 14 Dec 2024
Short summary
We present the results of several independent proxies of summer SST and upwelling SST from the Oman margin indicative of monsoon strength during the early Holocene. In combination with indices of carbonate preservation and bottom water redox conditions, we demonstrate that a persistent solar influence was modulating summer monsoon intensity. Furthermore, bottom water conditions are linked to atmospheric forcing, rather than changes of intermediate water masses.
We present the results of several independent proxies of summer SST and upwelling SST from the...