New oxygen isotope evidence for long-term Cretaceous climatic change in the Southern Hemisphere

New oxygen isotope evidence for long-term Cretaceous climatic change in the Southern Hemisphere

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A new composite δ18O record, generated from calcareous fine-fraction and bulk sediments from the Exmouth Plateau, details long-term Cretaceous climatic change at mid-latitudes in the Southern Hemisphere. Assessment of new and previously published δ18O data indicates that a mid-Cretaceous global clim...

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Príomhchruthaitheoirí:	Clarke, L, Jenkyns, H
Formáid:	Journal article
Teanga:	English
Foilsithe / Cruthaithe:	1999

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