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Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth
The terminal Neoproterozoic Era (850–542 Ma) is characterized by the most pronounced positive sulfur isotope ((34)S/(32)S) excursions in Earth's history, with strong variability and maximum values averaging δ(34)S∼+38‰. These excursions have been mostly interpreted in the framework of steady-st...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group
2016
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4961837/ https://www.ncbi.nlm.nih.gov/pubmed/27447895 http://dx.doi.org/10.1038/ncomms12192 |