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Nature Geoscience 1, 294–295 (1 May 2008) | doi:10.1038/ngeo191
Palaeoclimatology: A tale of two climates
Abstract
Substantial Antarctic glaciation commenced rapidly 34 million years ago at the geologic interval known as the Eocene–Oligocene boundary, which separates one of the warmest intervals of the past 65 million years from one of its coldest periods (Fig. 1).
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