PERMIAN-TRIASSIC BIOTIC CRISIS AND FORAMINIFERS

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dc.contributor.author Leven E.Ja.
dc.contributor.author Korchagin O.A.
dc.date.accessioned 2021-02-16T10:52:27Z
dc.date.available 2021-02-16T10:52:27Z
dc.date.issued 2001
dc.identifier https://elibrary.ru/item.asp?id=13368050
dc.identifier.citation Stratigraphy and Geological Correlation, 2001, 9, 4, 364-372
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/25027
dc.description.abstract Two phases can be distinguished in development of foraminifers during the Late Permian crisis. The first phase was marked by extinction of 40% of total foraminiferal genera. The crisis affected particularly fusulinids, which lost 76% of genera and 70% of families. At the end of the Permian, all foraminifers became extinct. Moreover, fusulinids die off completely, whereas some smaller foraminifers (Lazarus-taxa) appear again in the I. isarcica conodont zone. At the beginning, they were represented by archaic Paleozoic forms. The renewal of assemblages owing to development of Mesozoic forms commenced at the end of the Induan Age and significantly accelerated in the Anisian Age.
dc.subject Permian
dc.subject Triassic
dc.subject Foraminifers
dc.subject Crisis
dc.title PERMIAN-TRIASSIC BIOTIC CRISIS AND FORAMINIFERS
dc.type Статья
dc.subject.age Палеозой::Пермская ru
dc.subject.age Мезозой::Триасовая ru
dc.subject.age Mesozoic::Triassic en
dc.subject.age Paleozoic::Permian en


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