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Pulse of atmospheric oxygen during the late Cambrian
A rise in atmospheric O(2) has been linked to the Cambrian explosion of life. For the plankton and animal radiation that began some 40 million yr later and continued through much of the Ordovician (Great Ordovician Biodiversification Event), the search for an environmental trigger(s) has remained el...
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| Asıl Yazarlar: | , , , , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
National Academy of Sciences
2011
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| Konular: | |
| Online Erişim: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3053972/ https://ncbi.nlm.nih.gov/pubmed/21368152 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1011836108 |
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