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Greenhouse−icehouse transition in the Late Ordovician marks a step change in extinction regime in the marine plankton
Two distinct regimes of extinction dynamic are present in the major marine zooplankton group, the graptolites, during the Ordovician and Silurian periods (486−418 Ma). In conditions of “background” extinction, which dominated in the Ordovician, taxonomic evolutionary rates were relatively low and th...
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| Pubblicato in: | Proc Natl Acad Sci U S A |
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| Autori principali: | , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
National Academy of Sciences
2016
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4760818/ https://ncbi.nlm.nih.gov/pubmed/26811471 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1519092113 |
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