Palynology and sea surface temperature reconstruction for the mid-Cretaceous Oceanic Anoxic Event 2 at ODP Hole 210-1276A

The mid-Cretaceous is thought to be a greenhouse world with significantly higher atmospheric pCO2 and sea-surface temperatures as well as a much flatter latitudinal thermal gradient compared to the present. This time interval was punctuated by the Cenomanian/Turonian Oceanic Anoxic Event (OAE-2, ~ 9...

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Bibliographic Details
Main Authors: Sinninghe Damsté, Jaap S, van Bentum, Elisabeth C, Reichart, Gert-Jan, Pross, Jörg, Schouten, Stefan
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.786508
https://doi.org/10.1594/PANGAEA.786508