Mid-Pleistocene transition in glacial cycles explained by declining CO 2 and regolith removal
Author:
Affiliation:
1. Potsdam Institute for Climate Impact Research, Potsdam, Germany.
2. Max Planck Institute for Meteorology, Hamburg, Germany.
Abstract
Funder
Deutsche Forschungsgemeinschaft
Bundesministerium für Bildung und Forschung
Publisher
American Association for the Advancement of Science (AAAS)
Subject
Multidisciplinary
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4. Plio-Pleistocene climate evolution: Trends and transitions in glacial cycle dynamics;Lisiecki L. E.;Quat. Sci. Rev.,2007
5. The evolution of Pleistocene climate: A time series approach;Pisias N. G.;Earth Planet. Sci. Lett.,1981
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