PALAEOPLEUROCAPSA IN THE RIPHEAN DEPOSITS OF THE NORTH OF THE SIBERIAN CRATON

dc.contributor.author	Goloveenok V.K.
dc.contributor.author	Belova M.Yu.
dc.date.accessioned	2020-11-02T08:03:32Z
dc.date.available	2020-11-02T08:03:32Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31164300
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 1, 236-240
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18399
dc.description.abstract	The microfossils of the genus Palasopleurocapsa are characterized by a very distinctive structure. They are the fossilized remains of attached chamesiphonal blue-green algae, in which the thallus is formed of closely adjoining subparallel or upward-fanning cell rows: this distinguishes them from other taxonomic categories and makes them a conspicuous component of the Precambrian microbiotas. It has recently been learned that Palaeoplsurocapsa is extensively developed geographically and is confined to the youngest Precambrian deposits, so that the genus takes on an important biostratigraphic significance.
dc.subject	Riphean	en
dc.title	PALAEOPLEUROCAPSA IN THE RIPHEAN DEPOSITS OF THE NORTH OF THE SIBERIAN CRATON
dc.type	Статья
dc.subject.age	Precambrian::Proterozoic::Riphean	en
dc.subject.age	Докембрий::Протерозой::Рифей	ru

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