Late cretaceous temperature evolution of the southern high latitudes: a TEX86 perspective
The Late Cretaceous was a greenhouse world, characterized by elevated temperatures and high atmospheric pCO2. Even in the context of an extreme greenhouse climate, existing planktic foraminiferal δ18O data from the Falkland Plateau (paleolatitude of ~55°S) suggest anomalous warmth, with sea‐surface...
| প্রধান লেখক: | , , , , , , |
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| বিন্যাস: | Journal article |
| প্রকাশিত: |
Wiley
2019
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