Biological Feedbacks as Cause and Demise of Neoproterozoic Icehouse: Astrobiological Prospects for Faster Evolution and Importance of Cold Conditions

Several severe glaciations occurred during the Neoproterozoic eon, and especially near its end in the Cryogenian period (630–850 Ma). While the glacial periods themselves were probably related to the continental positions being appropriate for glaciation, the general coldness of the Neoproterozoic a...

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Detalles Bibliográficos
Autores principales: Janhunen, Pekka, Kaartokallio, Hermanni, Oksanen, Ilona, Lehto, Kirsi, Lehto, Harry
Formato: Texto
Lenguaje:English
Publicado: Public Library of Science 2007
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC1788933/
https://www.ncbi.nlm.nih.gov/pubmed/17299594
http://dx.doi.org/10.1371/journal.pone.0000214

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC1788933/
https://www.ncbi.nlm.nih.gov/pubmed/17299594
http://dx.doi.org/10.1371/journal.pone.0000214

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