Holocene hydroclimate variability along the Southern Patagonian margin (Chile) reconstructed from Cueva Chica speleothems

Patagonia is ideally situated to reconstruct past migrations of the southern westerly winds (SWWs) due to its southerly maritime location. The SWWs are an important driver of Southern Ocean upwelling and their strength and latitudinal position changed dur We thank the Corporacion Nacional Forestal C...

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Bibliographic Details
Published in:Global and Planetary Change
Main Authors: Nehme, Carole, Todisco, Dominique, Breitenbach, S F M, Couchoud, I, Marchegiano, M, Peral, M, Vonhof, H, Hellstrom, J, Tjallingii, R, Claeys, P, Borrero, Luis, Martin, Fabiána María
Format: Article in Journal/Newspaper
Language:English
Published: 2023
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Online Access:https://hdl.handle.net/10533/71876
https://doi.org/10.1016/j.gloplacha.2023.104050
Description
Summary:Patagonia is ideally situated to reconstruct past migrations of the southern westerly winds (SWWs) due to its southerly maritime location. The SWWs are an important driver of Southern Ocean upwelling and their strength and latitudinal position changed dur We thank the Corporacion Nacional Forestal Chile (CONAF) authorities and the rangers of the Park Monumento Natural Cueva del Milodon for their permission to sample in the Cueva Chica. Jorge Canales Helmer and Mario Margoni are thanked for the permission t FONDECYT REGULAR Proyectos de Investigación Fondo Nacional de Desarrollo Cientifico y Tecnologico, Chile (FONDECYT) [1180272]; Centre National pour la Recherche Scientifique, France (CNRS); Foundation Flanders, Belgium (FWO); VUB Wos 222