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Extensive marine anoxia during the terminal Ediacaran Period
The terminal Ediacaran Period witnessed the decline of the Ediacara biota (which may have included many stem-group animals). To test whether oceanic anoxia might have played a role in this evolutionary event, we measured U isotope compositions (δ(238)U) in sedimentary carbonates from the Dengying Fo...
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| Vydáno v: | Sci Adv |
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| Hlavní autoři: | , , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
American Association for the Advancement of Science
2018
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6010336/ https://ncbi.nlm.nih.gov/pubmed/29938217 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aan8983 |
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