A foraminiferal and stable isotope investigation of the Cenomanian-Turonian extinction and oceanic anoxic event
The Cretaceous was a time of significant global change, particularly around the Cenomanian-Turonian Boundary (CTB) (93.5 Ma). The mid-Cretaceous is considered to mark a period of intense global warming related to widespread tectonic activity, leading to periods of high sea level and no polar ice. Th...
| Main Author: | |
|---|---|
| Published: |
University of Plymouth
2006
|
| Subjects: | |
| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.427976 |