LATE FRASNIAN-FAMENNIAN CLIMATES BASED ON PALYNOMORPH ANALYSES AND THE QUESTION OF THE LATE DEVONIAN GLACIATIONS

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dc.contributor.author Streel M.
dc.contributor.author Caputo M.V.
dc.contributor.author Loboziak S.
dc.contributor.author Melo J.H.G.
dc.date.accessioned 2021-02-03T02:20:25Z
dc.date.available 2021-02-03T02:20:25Z
dc.date.issued 2000
dc.identifier https://elibrary.ru/item.asp?id=31906770
dc.identifier.citation Earth-Science Reviews, 2000, 52, 1, 121-173
dc.identifier.issn 0012-8252
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/24468
dc.description.abstract Palynomorph distribution in Euramerica and western Gondwana, from the Latest Givetian to the Latest Famennian, may be explained, to some extent, by climatic changes. Detailed miospore stratigraphy dates accurately the successive steps of these changes. Interpretation is built on three postulates which are discussed: Euramerica at slightly lower latitudes than generally accepted by most paleomagnetic reconstructions; a conodont time-scale accepted as the most used available subdivision of time; and Late Devonian sea-level fluctuations mainly governed by glacio-eustasy. The Frasnian–Famennian timescale is also evaluated.
dc.subject Famennian en
dc.subject Frasnian en
dc.subject Devonian en
dc.title LATE FRASNIAN-FAMENNIAN CLIMATES BASED ON PALYNOMORPH ANALYSES AND THE QUESTION OF THE LATE DEVONIAN GLACIATIONS
dc.type Статья
dc.subject.age Палеозой::Девонская::Верхний::Фаменский ru
dc.subject.age Paleozoic::Devonian::Upper::Frasnian en
dc.subject.age Paleozoic::Devonian en
dc.subject.age Paleozoic::Devonian::Upper::Famennian en
dc.subject.age Палеозой::Девонская::Верхний::Франский ru
dc.subject.age Палеозой::Девонская ru


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