Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining 𝑝CO2

Vittoria Lauretano, Alan T. Kennedy-asser, Vera A. Korasidis, Malcolm W. Wallace, Paul J. Valdes, Daniel J. Lunt, Richard D. Pancost, B. David A. Naafs

Research output: Contribution to journalArticle (Academic Journal)peer-review

Original languageEnglish
Pages (from-to)659-664
Number of pages6
JournalNature Geoscience
Issue number9
Early online date2 Aug 2021
Publication statusPublished - Sep 2021

Bibliographical note

Funding Information:
We thank NERC (reference: CC010) and NEIF (www.isotopesuk.org) for funding and maintenance of the instrumentation used for this work. We thank S. Blackbird at the University of Liverpool for technical assistance with the TOC analyses. This research was carried out with funding from the European Research Council under the European Union’s Seventh Framework Programme (FP/2007-2013) and European Research Council Grant Agreement number 340923 “The greenhouse earth system” T-GRES (awarded to R.D.P.). Further funding was provided by the Royal Society as part of a Tata University Research Fellowship to B.D.A.N. and the associated enhancement award that funded V.L. Climate model simulations were carried out using the computational facilities of the Advanced Computing Research Centre, University of Bristol, and were supported by NERC (grant number NE/L002434/1).

Publisher Copyright:
© 2021, The Author(s), under exclusive licence to Springer Nature Limited.
  • HPC (High Performance Computing) Facility

    Susan L Pywell (Manager), Simon A Burbidge (Other), Polly E Eccleston (Other) & Simon H Atack (Other)

    Facility/equipment: Facility

Cite this