New oxygen isotope evidence for long-term Cretaceous climatic change in the Southern Hemisphere
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...
| المؤلفون الرئيسيون: | , |
|---|---|
| التنسيق: | Journal article |
| اللغة: | English |
| منشور في: |
1999
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