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Science 14 March 2003:
Vol. 299. no. 5613, pp. 1728 - 1731
DOI: 10.1126/science.1078758

Reports

Timing of Atmospheric CO2 and Antarctic Temperature Changes Across Termination III

Nicolas Caillon,12* Jeffrey P. Severinghaus,2 Jean Jouzel,1 Jean-Marc Barnola,3 Jiancheng Kang,4 Volodya Y. Lipenkov5

The analysis of air bubbles from ice cores has yielded a precise record of atmospheric greenhouse gas concentrations, but the timing of changes in these gases with respect to temperature is not accurately known because of uncertainty in the gas age-ice age difference. We have measured the isotopic composition of argon in air bubbles in the Vostok core during Termination III (~240,000 years before the present). This record most likely reflects the temperature and accumulation change, although the mechanism remains unclear. The sequence of events during Termination III suggests that the CO2 increase lagged Antarctic deglacial warming by 800 ± 200 years and preceded the Northern Hemisphere deglaciation.

1 Institut Pierre Simon Laplace/Laboratoire des Sciences du Climat et de l'Environnement, Commissariat à l'Energie Atomique/CNRS, L'Orme des Merisiers, CEA Saclay, 91191, Gif sur Yvette, France.
2 Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093-0244, USA.
3 Laboratoire de Glaciologie et Géophysique de l'Environnement, CNRS, BP96, 38402, Saint Martin d'Hères, France.
4 Polar Research Institute of China, Pudong, Shanghai, 200129, People's Republic of China.
5 Arctic and Antarctic Research Institute, Beringa Street 38, 199397 St. Petersburg, Russia.
*   To whom correspondence should be addressed. E-mail: ncaillon{at}ucsd.edu


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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Stable Carbon Cycle-Climate Relationship During the Late Pleistocene.
U. Siegenthaler, T. F. Stocker, E. Monnin, D. Luthi, J. Schwander, B. Stauffer, D. Raynaud, J.-M. Barnola, H. Fischer, V. Masson-Delmotte, et al. (2005)
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Science. ISSN 0036-8075 (print), 1095-9203 (online)