ZOOGEOGRAPHY OF KONKIAN (MIDDLE MIOCENE) BIVALVES AND GASTROPODS

dc.contributor.author	Iljina L.B.
dc.date.accessioned	2022-02-17T11:03:52Z
dc.date.available	2022-02-17T11:03:52Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=13443609
dc.identifier.citation	Paleontological Journal, 2003, 37, 2, 116-123
dc.identifier.issn	0031-0301
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/35493
dc.description.abstract	In the mid-Middle Miocene (Konkian Phase), the Eastern Paratethys reestablished a wide connection with the World Ocean. This resulted in the migration of the marine polyhaline molluskan fauna from the Mediterranean. The expression of marine conditions controlled the distribution and abundance of the Konkian molluskan assemblages. The salinity regime was the main factor that influenced the formation and succession of Zoogeographic units throughout the history of the Eastern Paralethys.
dc.subject	Miocene
dc.title	ZOOGEOGRAPHY OF KONKIAN (MIDDLE MIOCENE) BIVALVES AND GASTROPODS
dc.type	Статья
dc.subject.age	Cenozoic::Neogene::Miocene
dc.subject.age	Кайнозой::Неоген::Миоцен	ru

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