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: | Clarke, L, Jenkyns, H |
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التنسيق: | Journal article |
اللغة: | English |
منشور في: |
1999
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مواد مشابهة
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New oxygen isotope evidence for long-term Cretaceous climatic change in the Southern Hemisphere
حسب: Clarke, L, وآخرون
منشور في: (1999) -
New oxygen isotope evidence for long-term Cretaceous climatic change in the Southern Hemisphere
حسب: Clarke, L, وآخرون
منشور في: (1999) -
Cretaceous oceanic anoxic events and carbon isotopes: Implications for global change
حسب: Jenkyns, H
منشور في: (2000) -
Upper Cretaceous carbon- and oxygen-isotope stratigraphy of hemipelagic carbonate facies from southern Tibet, China
حسب: Li, X, وآخرون
منشور في: (2006) -
Isotopic evidence for changes in the zinc cycle during Oceanic Anoxic Event 2 (Late Cretaceous)
حسب: Sweere, T, وآخرون
منشور في: (2018)