Did Late Cretaceous cooling trigger the Campanian–Maastrichtian Boundary Event?
The Campanian – Maastrichtian (83–66 Ma) was a period of global climate cooling, featuring significant negative carbon-isotope (δ13C) anomalies, such as the Late Campanian Event (LCE) and the Campanian – Maastrichtian Boundary Event (CMBE). A variety of factors, including changes in temperature, oce...
| المؤلفون الرئيسيون: | , , , , , , , , |
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| التنسيق: | Journal article |
| منشور في: |
Borntraeger Science Publishers
2018
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