FIVE MAXIMA OF BIODIVERSITY IN THE PALEOZOIC OF CENTRAL ASIA
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dc.contributor.author | Leleshus V.L. | |
dc.date.accessioned | 2022-02-22T05:08:03Z | |
dc.date.available | 2022-02-22T05:08:03Z | |
dc.date.issued | 2003 | |
dc.identifier | https://elibrary.ru/item.asp?id=27786802 | |
dc.identifier.citation | Paleontological Journal, 2003, 37, 3, 230-237 | |
dc.identifier.issn | 0031-0301 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/35648 | |
dc.description.abstract | Five maxima of biodiversity are identified in the Paleozoic of Central Asia: Late Cambrian, Caradoc-Ashgill, Early Devonian, Early Carboniferous, and late Early Permian. These maxima regularly alternated with the minima of biodiversity in the Early Ordovician, Early Silurian, Late Devonian, Middle Carboniferous, and Early Triassic. | |
dc.subject | Paleozoic | |
dc.title | FIVE MAXIMA OF BIODIVERSITY IN THE PALEOZOIC OF CENTRAL ASIA | |
dc.type | Статья | |
dc.subject.age | Paleozoic | |
dc.subject.age | Палеозой | ru |
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