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

• Main Authors: Haiblen, Anna M, Opdyke, Bradley N, Roberts, Andrew P, Heslop, David, Wilson, Paul A
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2019
• Subjects: benthic foraminiferal stable isotopes and Mg/Ca; Eocene-Oligocene boundary; paleoclimatology; paleomagnetic record of C13r/C13n; South Australia; Site; Sample type; Stratigraphy; Stratigraphic height; Foraminifera, benthic δ18O; Foraminifera, benthic δ13C; Magnesium/Calcium ratio; Inclination; Declination; Method comment; Number; Multiple investigations; Antarctic; Southern Ocean; Pacific; Blanche; Blanche Point; Antarc*
• Online Access: https://dx.doi.org/10.1594/pangaea.907397; https://doi.pangaea.de/10.1594/PANGAEA.907397

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...