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