Benthic and planktic foraminiferal stable isotope records combined with Nd isotope ratios of ODP Hole 198-1210B

The Pacific Ocean is the largest water body on Earth, and circulation in the Pacific contributed significantly to climate evolution in the latest Cretaceous, the culmination of a period of long-term cooling. Here, we present new high-resolution late Campanian to Maastrichtian benthic and planktic fo...

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Bibliographic Details
Main Authors: Jung, Claudia, Voigt, Silke, Friedrich, Oliver, Koch, Mirjam C, Frank, Martin
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.821024
https://doi.org/10.1594/PANGAEA.821024