Late Miocene and Pliocene dinoflagellate cysts, acritarchs and terrestrial palynomorphs from ODP Hole 642B, Vøring Plateau, Norwegian Sea

The globally warm climate of the early Pliocene gradually cooled from 4 million years ago, synchronous with decreasing atmospheric CO2 concentrations. In contrast, palaeoceanographic records indicate that the Nordic Seas cooled during the earliest Pliocene, before global cooling. However, a lack of...

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Bibliographic Details
Main Authors: De Schepper, Stijn, Beck, Kristina Marie, Mangerud, Gunn, Schreck, Michael, Matthiessen, Jens
Format: Dataset
Language:English
Published: PANGAEA 2015
Subjects:
AGE
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.846838
https://doi.org/10.1594/PANGAEA.846838