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Article
Nature 316, 591 - 596 (15 August 1985); doi:10.1038/316591a0

A 150,000-year climatic record from Antarctic ice

C. Lorius*, J. Jouzel, C. Ritz*, L. Merlivat, N. I. Barkov, Y. S. Korotkevich & V. M. Kotlyakov§

*Laboratoire de Glaciologie et de Géophysique de l'Environnement, CNRS, BP96, 38402 Saint Martin d'Héres Cedex, France
Laboratoire de Géochimie Isotopique DPC, CEN Saclay, 91191 Gif-sur-Yvette Cedex, France
The Arctic and Antarctic Research Institute, Fontanka 34, Leningrad 191104, USSR
§Institute of Geography, Academy of Sciences of USSR, Staronometry, St 29, Moscow 109017, USSR

During much of the Quaternary, the Earth's climate has undergone drastic changes most notably successive glacial and interglacial episodes. The past 150 kyr includes such a climatic cycle: the last interglacial, the last glacial and the present holocene interglacial. A new climatic−time series for this period has been obtained using delta18 O data from an Antarctic ice core.

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