Articles | Volume 18, issue 5
https://doi.org/10.5194/cp-18-1231-2022
https://doi.org/10.5194/cp-18-1231-2022
Research article
 | 
01 Jun 2022
Research article |  | 01 Jun 2022

Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped-isotope paleothermometry

David De Vleeschouwer, Marion Peral, Marta Marchegiano, Angelina Füllberg, Niklas Meinicke, Heiko Pälike, Gerald Auer, Benjamin Petrick, Christophe Snoeck, Steven Goderis, and Philippe Claeys

Data sets

Clumped isotopes on planktonic foraminiferal calcite from IODP Site U1459 (Plio-Pleistocene) D. De Vleeschouwer, M. Peral, and M. Marchegiano https://doi.org/10.26022/IEDA/112262

Biomarkers (TEX86), planktic isotopes and XRF records of IODP Site 356-U1459 (Perth Basin) D. De Vleeschouwer, B. F. Petrick, and A. Martínez‐García https://doi.org/10.1594/PANGAEA.903102

Natural Gamma Radiation-derived K, U and Th contents of marine sediments obtained during IODP Expeditions with DV JOIDES Resolution, Version 1.0 D. De Vleeschouwer https://doi.org/10.1594/IEDA/100668

Planktic carbon and oxygen isotopes and NGR-derived K, U and Th data D. De Vleeschouwer, G. Auer, R. Smith, K. A. Bogus, B. A. Christensen, J. Groeneveld, B. F. Petrick, J. Henderiks, I. S. Castañeda, E. O'Brian, M. Ellinghausen, S. J. Gallagher, C. S. Fulthorpe, and H. Pälike https://doi.org/10.1594/PANGAEA.892422

Indian Ocean Pliocene Paired Foraminiferal d18O and Mg/Ca Data C. Karas, D. Nürnberg, R. Tiedemann, and D. Garbe-Schönberg https://www.ncei.noaa.gov/pub/data/paleo/contributions_by_author/karas2011/karas2011.txt

Model code and software

Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped isotope paleothermometry D. De Vleeschouwer, M. Peral, M. Marchegiano, A. Füllberg, N. Meinicke, H. Pälike, G. Auer, B. Petrick, C. Snoeck, S. Goderis, and P. Claeys https://doi.org/10.5281/zenodo.6380452

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Short summary
The Leeuwin Current transports warm water along the western coast of Australia: from the tropics to the Southern Hemisphere midlatitudes. Therewith, the current influences climate in two ways: first, as a moisture source for precipitation in southwestern Australia; second, as a vehicle for Equator-to-pole heat transport. In this study, we study sediment cores along the Leeuwin Current pathway to understand its ocean–climate interactions between 4 and 2 Ma.