Water-mass evolution in the Cretaceous Western Interior Seaway of North America and equatorial Atlantic
The Late Cretaceous Epoch was characterized by major global perturbations in the carbon cycle, the most prominent occurring near the Cenomanian–Turonian (CT) transition marked by Oceanic Anoxic Event 2 (OAE-2) at 94.9–93.7 Ma. The Cretaceous Western Interior Seaway (KWIS) was one of several epi...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2017-07-01
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| Series: | Climate of the Past |
| Online Access: | https://www.clim-past.net/13/855/2017/cp-13-855-2017.pdf |