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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: | , , , , |
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| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
National Academy of Sciences
2011
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| Materias: | |
| 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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