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The turnover of continental planktonic diatoms near the middle/late Miocene boundary and their Cenozoic evolution
Fossil evidence indicates that modern assemblages of temperate nonmarine planktonic diatoms began near the middle/late Miocene boundary when the genus Actinocyclus, an important constituent of lacustrine planktonic diatom assemblages during the early to middle Miocene, was replaced by genera of the...
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| Vydáno v: | PLoS One |
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| Hlavní autoři: | , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Public Library of Science
2018
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5988279/ https://ncbi.nlm.nih.gov/pubmed/29870528 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1371/journal.pone.0198003 |
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