First physical evidence for forested environment in the Arctic during MIS 3

Old sedimentological and geochronological records can be preserved underneath the central parts of the continental ice sheets under non-erosive, cold-based subglacial conditions. Organic deposits that predate the last deglaciation are of particular value for the information held on glacial-time clim...

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Detalles Bibliográficos
Autores principales: Sarala, Pertti, Väliranta, Minna, Eskola, Tiina, Vaikutiené, Giedré
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4929562/
https://www.ncbi.nlm.nih.gov/pubmed/27363905
http://dx.doi.org/10.1038/srep29054

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4929562/
https://www.ncbi.nlm.nih.gov/pubmed/27363905
http://dx.doi.org/10.1038/srep29054

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