Santonian–Campanian (Late Cretaceous) planktonic foraminiferal turnover, depth ecology and paleoceanographic implications
The Santonian–Campanian time interval is a transitional phase from the extreme greenhouse warmth during the Turonian to more temperate conditions and to a thermohaline circulation that was more like that of the modern day. These environmental changes led to a re-organization of marine ecosystems in...
Main Authors: | , , , |
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Other Authors: | , |
Format: | Conference Object |
Language: | English |
Published: |
2013
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Subjects: | |
Online Access: | http://hdl.handle.net/2434/222852 |