Fossil leaves from the last interglacial in central-southern Chile: Inferences regarding the vegetation and paleoclimate

Fossil leaves from the last interglacial in central-southern Chile: Inferences regarding the vegetation and paleoclimate

The continental equivalent of the most temperate part of the last interglacial (MIS 5e) is called Valdivia in southern Chile. It is characterised by extensive terraces mostly composed of detrital sediments and pyroclastic flows. Peat deposits are found within these terraces. In this paper we analyze...

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Bibliographic Details
Main Authors: G. ASTORGA, M. PINO
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2011-05-01
Series:Geologica Acta
Subjects:
Interglacial
Flora
Leaves
Chile
South America
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/2099

Internet

https://revistes.ub.edu/index.php/GEOACTA/article/view/2099

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