Articles | Volume 17, issue 5
https://doi.org/10.5194/cp-17-2091-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-2091-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Oct 2021
Research article |
| 15 Oct 2021
| 15 Oct 2021
Climate, cryosphere and carbon cycle controls on Southeast Atlantic orbital-scale carbonate deposition since the Oligocene (30–0 Ma)
Anna Joy Drury
CORRESPONDING AUTHOR
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Department of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, UK
Diederik Liebrand
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Thomas Westerhold
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Helen M. Beddow
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Utrecht, the Netherlands
David A. Hodell
Department of Earth Science, University of Cambridge, Cambridge, EH9 3FE, UK
Nina Rohlfs
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Roy H. Wilkens
School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, Hawaii 96822, USA
Mitchell Lyle
College of Earth, Ocean, and Atmospheric Science, Oregon State
University, Corvallis, Oregon 97331, USA
David B. Bell
School of GeoSciences, University of Edinburgh, Edinburgh, CB2 3EQ, UK
Dick Kroon
School of GeoSciences, University of Edinburgh, Edinburgh, CB2 3EQ, UK
Heiko Pälike
MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359 Bremen, Germany
Lucas J. Lourens
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Utrecht, the Netherlands
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Short summary
We use the first high-resolution southeast Atlantic carbonate record to see how climate dynamics evolved since 30 million years ago (Ma). During ~ 30–13 Ma, eccentricity (orbital circularity) paced carbonate deposition. After the mid-Miocene Climate Transition (~ 14 Ma), precession (Earth's tilt direction) increasingly drove carbonate variability. In the latest Miocene (~ 8 Ma), obliquity (Earth's tilt) pacing appeared, signalling increasing high-latitude influence.
We use the first high-resolution southeast Atlantic carbonate record to see how climate dynamics...
