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The isotopic composition of the French Illimani ice core in the Bolivian Andes supports the east-west South American precipitation dipole from the last deglaciation to the mid-Holocene
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The isotopic composition of the French Illimani ice core in the Bolivian Andes supports the east-west South American precipitation dipole from the last deglaciation to the mid-Holocene

Françoise Vimeux et Amaëlle Landais
Quaternary science reviews, Vol.347, p.109098
01/2025

Résumé

Continental interfaces, environment Ocean, Atmosphere Sciences of the Universe

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1 Consultations de la notice

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