(Table S1, S4) Campanian-Maastrichtian benthic foraminifera from ODP Hole 113-690C

During the latest Cretaceous cooling phase, a positive shift in benthic foraminiferal d18O values lasting about 1.5 Myr (71.5-70 Ma) can be observed at a global scale (Campanian-Maastrichtian Boundary Event, CMBE). This d18O excursion is interpreted as being influenced by a change in intermediate- t...

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Bibliographic Details
Main Authors: Koch, Mirjam C, Friedrich, Oliver
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
AGE
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.825712
https://doi.org/10.1594/PANGAEA.825712