Planktic carbon and oxygen isotopes and NGR-derived K, U and Th data, supplement to: De Vleeschouwer, David; Auer, Gerald; Smith, Rebecca; Bogus, Kara A; Christensen, Beth A; Groeneveld, Jeroen; Petrick, Benjamin F; Henderiks, Jorijntje; Castañeda, Isla S; O'Brian, Evan; Ellinghausen, Maret; Gallagher, Stephen John; Fulthorpe, Craig S; Pälike, Heiko (2018): The amplifying effect of Indonesian Throughflow heat transport on Late Pliocene Southern Hemisphere climate cooling. Earth and Planetary Science Letters, 500, 15-27

• Main Authors: De Vleeschouwer, David, Auer, Gerald, Smith, Rebecca, Bogus, Kara A, Christensen, Beth A, Groeneveld, Jeroen, Petrick, Benjamin F, Henderiks, Jorijntje, Castañeda, Isla S, O'Brian, Evan, Ellinghausen, Maret, Gallagher, Stephen John, Fulthorpe, Craig S, Pälike, Heiko
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2018
• Subjects: Integrated Ocean Drilling Program / International Ocean Discovery Program IODP; Christensen; Indian; Pacific; Antarc*; Antarctica
• Online Access: https://dx.doi.org/10.1594/pangaea.892422; https://doi.pangaea.de/10.1594/PANGAEA.892422

An unusually short glaciation interrupted the warm Pliocene around 3.3 Ma (Marine Isotope Stage (MIS) M2). Different hypotheses exist to explain why this glaciation event was so pronounced, and why the global climate system returned to warm Pliocene conditions relatively quickly afterwards. One of t...