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Thursday, January 13, 2011

Peter K. Bijl et al., Science 330 (2010), Transient Middle Eocene atmospheric CO2 and temperature variations

Science (5 November 2010), Vol. 330, No. 6005, pp. 819-821;  DOI: 10.1126/science.1193654

Transient Middle Eocene atmospheric CO2 and temperature variations

  1. Peter K. Bijl1,*
  2. Alexander J. P. Houben1,*
  3. Stefan Schouten2
  4. Steven M. Bohaty3
  5. Appy Sluijs1
  6. Gert-Jan Reichart4
  7. Jaap S. Sinninghe Damsté2,4 and 
  8. Henk Brinkhuis1
+Author Affiliations
  1. 1Biomarine Sciences, Institute of Environmental Biology, Faculty of Science, Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, Netherlands.
  2. 2Department of Marine Organic Biogeochemistry, NIOZ Royal Netherlands Institute of Sea Research, Post Office Box 59, 1790 AB Den Burg, Texel, Netherlands.
  3. 3School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, European Way, Southampton SO14 3ZH, UK.
  4. 4Geochemistry, Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, Netherlands.
  1. *Correspondence e-mail: p.k.bijl@uu.nl (P.K.B.); a.j.p.houben@uu.nl (A.J.P.H.)

Abstract

The long-term warmth of the Eocene (~56 to 34 million years ago) is commonly associated with elevated partial pressure of atmospheric carbon dioxide (pCO2). However, a direct relationship between the two has not been established for short-term climate perturbations. We reconstructed changes in both pCO2 and temperature over an episode of transient global warming called the Middle Eocene Climatic Optimum (MECO; ~40 million years ago). Organic molecular paleothermometry indicates a warming of southwest Pacific sea surface temperatures (SSTs) by 3-6 °C. Reconstructions of pCO2 indicate a concomitant increase by a factor of 2 to 3. The marked consistency between SST and pCO2 trends during the MECO suggests that elevated pCO2 played a major role in global warming during the MECO.

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