Holocene environmental and climate evolution of central west Patagonia as reconstructed from lacustrine sediments of Meseta Chile Chico (46.5° S, Chile)

<p>Holocene environmental changes in Patagonia were mostly shaped by fluctuating ice cover recession. Consequently, environmental reconstructions are largely based on discontinuous moraine chronologies from valley deposits. Here, we present a 3 m long continuous sediment record recovered from...

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Bibliographic Details
Main Authors: C. Franco, A. Maldonado, C. Ohlendorf, A. C. Gebhardt, M. E. de Porras, A. Nuevo-Delaunay, C. Méndez, B. Zolitschka
Format: Article
Language:English
Published: Copernicus Publications 2024-04-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/20/817/2024/cp-20-817-2024.pdf