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

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 Laguna Me...

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Bibliographic Details
Published in:	Climate of the past Vol. 20; no. 4; pp. 817 - 839
Main Authors:	Franco, Carolina, Maldonado, Antonio, Ohlendorf, Christian, Gebhardt, A. Catalina, de Porras, María Eugenia, Nuevo-Delaunay, Amalia, Méndez, César, Zolitschka, Bernd
Format:	Journal Article
Language:	English
Published:	Katlenburg-Lindau Copernicus GmbH 08-04-2024 Copernicus Publications
Subjects:	Allochthonous deposits Archives & records Carbon 14 Climate Climate control Climatic evolution Environmental aspects Environmental changes Glacial drift Glacial periods Glaciers Holocene Holocene glaciation Ice caps Ice cover Ice fields Ice sheets Lacustrine sedimentation Lacustrine sediments Lakes Moraines Oscillations Precipitation Precipitation variability Productivity Radiocarbon dating Sediment Sedimentation Sediments Sediments (Geology) Southern Hemisphere Spatial variations Topography Valleys Vegetation Westerlies Winds Chile Northern Hemisphere
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