THE SAGAN-NUR: A NEW LOCALITY OF THE LATE PLIOCENE AND NEOPLEISTOCENE BIOTA IN THE WESTERN TRANSBAIKAL REGION

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dc.contributor.author Kalmykov N.P.
dc.contributor.author Budaev R.Ts.
dc.contributor.author Savinov V.V.
dc.date.accessioned 2022-08-03T05:20:55Z
dc.date.available 2022-08-03T05:20:55Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=13463645
dc.identifier.citation Doklady Earth Sciences, 2004, 399, 9, 1280-1282
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38437
dc.description.abstract At stripping conducted at coal deposit Sagan-Nur, in the basement of old-frozen rocks overlaying the coal tar productive layer the sediments of slopewash genesis were found. Palynological spectra confirmed the tendency in Western Transbaikalia flora changing during Pliocene-Quaternary period from boreal spruce forests with considerable admixture of broad-leaved to light coniferous forests. The analysis results for Sagan-Nur biota and geologic peculiarities enabled to recover not only chiatus in biocenotic coat evolution but also the missing member in Tugnuisk basin history on the stage of its erosion development after durable Mesozoic accumulation period.
dc.subject Pleistocene
dc.subject Pliocene
dc.title THE SAGAN-NUR: A NEW LOCALITY OF THE LATE PLIOCENE AND NEOPLEISTOCENE BIOTA IN THE WESTERN TRANSBAIKAL REGION
dc.type Статья
dc.subject.age Cenozoic::Quaternary::Pleistocene
dc.subject.age Cenozoic::Neogene::Pliocene
dc.subject.age Кайнозой::Четвертичная::Плейстоцен ru
dc.subject.age Кайнозой::Неоген::Плиоцен ru


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