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...

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Bibliographic Details
Main Authors: F. Falzoni, M.R. Petrizzo, B. T. Huber, K. G. MacLeod
Other Authors: B.T. Huber, K.G. Macleod
Format: Conference Object
Language:English
Published: 2013
Subjects:
Online Access:http://hdl.handle.net/2434/222852