Indonesian Throughflow drove Australian climate from humid Pliocene to arid Pleistocene

Indonesian Throughflow drove Australian climate from humid Pliocene to arid Pleistocene

Abstract Late Miocene to mid‐Pleistocene sedimentary proxy records reveal that northwest Australia underwent an abrupt transition from dry to humid climate conditions at 5.5 million years (Ma), likely receiving year‐round rainfall, but after ~3.3 Ma, climate shifted toward an increasingly seasonal p...

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Main Authors: Beth A. Christensen, Willem Renema, Jorijntje Henderiks, David De Vleeschouwer, Jeroen Groeneveld, Isla S. Castañeda, Lars Reuning, Kara Bogus, Gerald Auer, Takeshige Ishiwa, Cecilia M. McHugh, Stephen J. Gallagher, Craig S. Fulthorpe, IODP Expedition 356 Scientists
Format: Article
Language:English
Published: Wiley 2017-07-01
Series:Geophysical Research Letters
Subjects:
IODP
Australia
continental climate
Maritime Continent
Indonesian Throughflow
Neogene
Online Access:https://doi.org/10.1002/2017GL072977
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https://doi.org/10.1002/2017GL072977

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