Eocene-Oligocene paleomagnetic and foraminiferal stable isotopic and Mg/Ca record from South Australia, supplement to: Haiblen, Anna M; Opdyke, Bradley N; Roberts, Andrew P; Heslop, David; Wilson, Paul A (2019): Midlatitude Southern Hemisphere Temperature Change at the End of the Eocene Greenhouse Shortly Before Dawn of the Oligocene Icehouse. Paleoceanography and Paleoclimatology, 34(12), 1995-2004
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...
Main Authors: | , , , , |
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Format: | Dataset |
Language: | English |
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PANGAEA - Data Publisher for Earth & Environmental Science
2019
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Online Access: | https://dx.doi.org/10.1594/pangaea.907397 https://doi.pangaea.de/10.1594/PANGAEA.907397 |