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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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| Publicado no: | Geologica Acta: an international earth science journal |
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| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Universitat de Barcelona
2011
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| Assuntos: | |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=50522124005 |
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