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Paleoproterozoic snowball Earth: Extreme climatic and geochemical global change and its biological consequences

Geological, geophysical, and geochemical data support a theory that Earth experienced several intervals of intense, global glaciation (“snowball Earth” conditions) during Precambrian time. This snowball model predicts that postglacial, greenhouse-induced warming would lead to the deposition of bande...

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Autori principali: Kirschvink, Joseph L., Gaidos, Eric J., Bertani, L. Elizabeth, Beukes, Nicholas J., Gutzmer, Jens, Maepa, Linda N., Steinberger, Rachel E.
Natura: Artigo
Lingua:Inglês
Pubblicazione: The National Academy of Sciences 2000
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Accesso online:https://ncbi.nlm.nih.gov/pmc/articles/PMC26445/
https://ncbi.nlm.nih.gov/pubmed/10677473
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