Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate

Eleni Anagnostou (), Eleanor H. John, Kirsty M. Edgar, Gavin L. Foster, Andy Ridgwell, Gordon N. Inglis, Richard D. Pancost, Daniel J. Lunt and Paul N. Pearson
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Eleni Anagnostou: Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus
Eleanor H. John: School of Earth and Ocean Sciences, Cardiff University
Kirsty M. Edgar: School of Earth and Ocean Sciences, Cardiff University
Gavin L. Foster: Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus
Andy Ridgwell: School of Geographical Sciences, Bristol University
Gordon N. Inglis: Organic Geochemistry Unit, School of Chemistry, University of Bristol, Cantock’s Close
Richard D. Pancost: Organic Geochemistry Unit, School of Chemistry, University of Bristol, Cantock’s Close
Daniel J. Lunt: School of Geographical Sciences, Bristol University
Paul N. Pearson: School of Earth and Ocean Sciences, Cardiff University

Nature, 2016, vol. 533, issue 7603, 380-384

Abstract: A reconstruction of atmospheric CO2 concentration from boron isotopes recorded in planktonic foraminifera examines climate–carbon interactions over the past tens of millions of years and confirms a strong linkage between climate and atmospheric CO2.

Date: 2016
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DOI: 10.1038/nature17423

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