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Onset of main Phanerozoic marine radiation sparked by emerging Mid Ordovician icehouse
The Great Ordovician Biodiversification Event (GOBE) was the most rapid and sustained increase in marine Phanerozoic biodiversity. What generated this biotic response across Palaeozoic seascapes is a matter of debate; several intrinsic and extrinsic drivers have been suggested. One is Ordovician cli...
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| Gepubliceerd in: | Sci Rep |
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| Hoofdauteurs: | , , , , , , , , , , , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Nature Publishing Group
2016
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4702064/ https://ncbi.nlm.nih.gov/pubmed/26733399 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep18884 |
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