Articles | Volume 11, issue 6
https://doi.org/10.5194/cp-11-915-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/cp-11-915-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Thermal evolution of the western South Atlantic and the adjacent continent during Termination 1
School of Arts, Sciences and Humanities, University of São Paulo, São Paulo, Brazil
S. Mulitza
MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
G. Mollenhauer
MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
J. B. Silva
Institute of Geosciences, University of São Paulo, São Paulo, Brazil
J. Groeneveld
MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
M. Prange
MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
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Short summary
Here we show that temperatures in the western South Atlantic increased markedly during the major slowdown event of the Atlantic meridional overturning circulation (AMOC) of the last deglaciation. Over the adjacent continent, however, temperatures followed the rise in atmospheric carbon dioxide, lagging changes in oceanic temperature. Our records corroborate the notion that the long duration of the major slowdown event of the AMOC was fundamental in driving the Earth out of the last glacial.
Here we show that temperatures in the western South Atlantic increased markedly during the major...