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Biologically induced initiation of Neoproterozoic snowball-Earth events

The glaciations of the Neoproterozoic Era (1,000 to 542 MyBP) were preceded by dramatically light C isotopic excursions preserved in preglacial deposits. Standard explanations of these excursions involve remineralization of isotopically light organic matter and imply strong enhancement of atmospheri...

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Autores principales: Tziperman, Eli, Halevy, Itay, Johnston, David T., Knoll, Andrew H., Schrag, Daniel P.
Formato: Artigo
Lenguaje:Inglês
Publicado: National Academy of Sciences 2011
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Acceso en línea:https://ncbi.nlm.nih.gov/pmc/articles/PMC3174660/
https://ncbi.nlm.nih.gov/pubmed/21825156
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1016361108
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