COMPARATIVE ANALYSIS OF THE EOCENE-MIOCENE MICRO-AND MACROFLORAS OF THE EASTERN SIKHOTE ALIN'
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dc.contributor.author | Lopatina D.A. | |
dc.date.accessioned | 2021-11-21T03:19:40Z | |
dc.date.available | 2021-11-21T03:19:40Z | |
dc.date.issued | 2003 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13433659 | |
dc.identifier.citation | Stratigraphy and Geological Correlation, 2003, 11, 1, 74-90 | |
dc.identifier.issn | 0869-5938 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/32310 | |
dc.description.abstract | Comparative characteristic of spore-pollen assemblages from the Son'e (late Eocene), Bui, Svetlovodnaya (late Eocene-early Oligocene), Amgu (late Oligocene-early Miocene), Dembi, Velikaya Kema (late early Miocene-earliest middle Miocene), and Botchi (latest middle Miocene-late Miocene-late Miocene) floral localities in the Eastern Sikhote Alin' are presented. It is shown that assemblages of micro- and macroflora are substantially similar at the generic and family levels. They usually include the following genera in common: Ginkgo, Pinus, Picea, Tsuga, Sciadopitys, Thuja, Alnus, Betula, Carpinus, Ostrya, Carya, Fagus, Quercus, Acer, and Rhus. Differences between assemblages in composition and abundance of taxa are determined by biological peculiarities of plants, fossilization mode of micro- and macrofloras, geographical position of particular areas, conditions of lithogenesis, and genesis of assemblages; in addition, morphology of some spore and pollen species is insufficiently known. | |
dc.subject | Miocene | |
dc.subject | Eocene | |
dc.title | COMPARATIVE ANALYSIS OF THE EOCENE-MIOCENE MICRO-AND MACROFLORAS OF THE EASTERN SIKHOTE ALIN' | |
dc.type | Статья | |
dc.subject.age | Cenozoic::Neogene::Miocene | |
dc.subject.age | Кайнозой::Палеоген::Эоцен | ru |
dc.subject.age | Кайнозой::Неоген::Миоцен | ru |
dc.subject.age | Cenozoic::Paleogene::Eocene |
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