PALEOBOTANICAL ANALYSIS OF MATERIALS FROM FOSSIL GOPHER BURROWS AND UPPER PLEISTOCENE HOST DEPOSITS, THE KOLYMA RIVER LOWER REACHES

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dc.contributor.author Lopatina D.A.
dc.contributor.author Zanina O.G.
dc.date.accessioned 2024-07-20T12:14:02Z
dc.date.available 2024-07-20T12:14:02Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=13526857
dc.identifier.citation Stratigraphy and Geological Correlation, 2006, 14, 5, 549-560
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/44496
dc.description.abstract The comparative analysis of palynomorphs and plant megafossils (fruits, seeds, twigs, leaves) in the Upper Pleistocene host sediments and materials filling in fossil burrows of gophers, their coprolites included, at the Duvannyi Yar, Stanchikovskii Yar and Zelenyi Mys sites of the Kolyma Lowland is carried out. Genera Salix, Lychnis, Silene, Draba, Potentilla, Larix, and families Poaceae, Polygonaceae, Cyperaceae, Compositae, and Leguminosae are determined among palynological remains and megafossils. Factors responsible for qualitative and quantitative differences in taxonomic compositions of palynological and megafossil assemblages are biological peculiarities of plants, different character of fossilization of palynomorphs and large plant remains, geographic conditions, different genesis of assemblages (allochthonous for microfossils and autochthonous for megafossils), and inadequately known morphology of certain spore and pollen taxa. The comprehensive paleobotanical analysis leads to the conclusion that the study region was occupied in the Late Pleistocene by plant communities of humid to somewhat dryer tundra with separate areas of pioneering and steppe vegetation. © MAIK "Nauka/Interperiodica" 2006.
dc.subject BURROWS OF FOSSIL RODENTS
dc.subject GLACIAL COMPLEX
dc.subject KARGA BEDS
dc.subject KOLYMA RIVER
dc.subject PALEOBOTANICAL ANALYSIS
dc.subject UPPER PLEISTOCENE
dc.title PALEOBOTANICAL ANALYSIS OF MATERIALS FROM FOSSIL GOPHER BURROWS AND UPPER PLEISTOCENE HOST DEPOSITS, THE KOLYMA RIVER LOWER REACHES
dc.type Статья
dc.identifier.doi 10.1134/S0869593806050078
dc.subject.age Кайнозой::Четвертичная::Плейстоцен
dc.subject.age Cenozoic::Quaternary::Pleistocene


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