FIVE MAXIMA OF BIODIVERSITY IN THE PALEOZOIC OF CENTRAL ASIA

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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