Eocene-Oligocene paleomagnetic and foraminiferal stable isotopic and Mg/Ca record from South Australia

The Eocene-Oligocene transition (EOT) marked the initiation of large-scale Antarctic glaciation. This fundamental change in Cenozoic climate state is recorded in deep-sea sediments by a rapid benthic foraminiferal δ18O increase and appearance of ice-rafted debris in the Southern Ocean. However, we k...

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Bibliographic Details
Main Authors: Haiblen, Anna M, Opdyke, Bradley N, Roberts, Andrew P, Heslop, David, Wilson, Paul A
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.907397
https://doi.org/10.1594/PANGAEA.907397