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An explanation for conflicting records of Triassic–Jurassic plant diversity
Macrofossils (mostly leaves) and sporomorphs (pollen and spores) preserve conflicting records of plant biodiversity during the end-Permian (P-Tr), Triassic–Jurassic (Tr-J), and end-Cretaceous (K-T) mass extinctions. Estimates of diversity loss based on macrofossils are typically much higher than est...
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| Auteurs principaux: | , , |
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
National Academy of Sciences
2010
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| Sujets: | |
| Accès en ligne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2932585/ https://ncbi.nlm.nih.gov/pubmed/20713737 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1004207107 |
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