LATE CARBONIFEROUS ASSEMBLAGES OF SCHWAGERINIDS (FORAMINIFERA, SCHWAGERINIDA) IN TWO TYPES OF ORGANOGENIC STRUCTURES OF THE CENTRAL URALS

dc.contributor.author	Vilesov A.P.
dc.date.accessioned	2021-06-10T12:09:37Z
dc.date.available	2021-06-10T12:09:37Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=13409875
dc.identifier.citation	Paleontological Journal, 2002, 36, 3, 240-248
dc.identifier.issn	0031-0301
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/28995
dc.description.abstract	Two types of organogenic structures of the Central Uralian Melekhov Horizon (Gzhelian Stage, Upper Carboniferous) contain essentially different schwagerinid assemblages. Owing to the diversity of its surface biotopes, the algal-palaeoaplysinal biohermal massif is characterized by a diversity of genera and ecological groups (nine and three, respectively). The biostromal palaeoaplysinal massif contains a less diverse schwagerinid assemblage (five genera and one ecological group), which formed in uniform biotic and abiotic environments of the massif's smooth surface.
dc.subject	Carboniferous
dc.title	LATE CARBONIFEROUS ASSEMBLAGES OF SCHWAGERINIDS (FORAMINIFERA, SCHWAGERINIDA) IN TWO TYPES OF ORGANOGENIC STRUCTURES OF THE CENTRAL URALS
dc.type	Статья
dc.subject.age	Paleozoic::Carboniferous
dc.subject.age	Палеозой::Каменноугольная	ru

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