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作 者:Boris L.Nikitenko Ekaterina B.Pestchevitskaya Svetlana N.Khafaeva
机构地区:[1]Trofimuk Institute of Petroleum Geology and Geophysics,Siberian Branch of the Russian Academy of Sciences,Novosibirsk 630090,Russia [2]Novosibirsk State University,Novosibirsk 630090,Russia
出 处:《Global Geology》2019年第4期270-279,共10页世界地质(英文版)
基 金:Financial support:Russian Science Foundation 18-17-00038;Scientific support:Russian FSI 0331-2019-0004;IGCP 679,632
摘 要:The Volgian-Valanginian succession of shallow-water deposits from the Olenek section(Anabar-Lena region,Arctic Siberia)has been studied by sedimentological and palaeontological methods.High-resolution biostratigraphy of studied interval is based on the ammonites,foraminifers,marine and terrestrial palynomorphs.Foraminiferal and palynological zones have important regional implications providing well-constrained biostratigraphy of the Anabar-Lena region.Sedimentological studies together with ecological analysis of the associations of microbenthos,microphytoplankton and terrestrial palynomorphs allow the palaeoenvironmental reconstructions for the marginal area of the Anabar-Lena palaeosea and coastal land areas.The Volgian-Valanginian succession of shallow-water deposits from the Olenek section(Anabar-Lena region, Arctic Siberia) has been studied by sedimentological and palaeontological methods. High-resolution biostratigraphy of studied interval is based on the ammonites, foraminifers, marine and terrestrial palynomorphs. Foraminiferal and palynological zones have important regional implications providing well-constrained biostratigraphy of the Anabar-Lena region. Sedimentological studies together with ecological analysis of the associations of microbenthos, microphytoplankton and terrestrial palynomorphs allow the palaeoenvironmental reconstructions for the marginal area of the Anabar-Lena palaeosea and coastal land areas.
关 键 词:Upper Jurassic Lower Cretaceous Arctic Siberia BIOSTRATIGRAPHY PALAEOENVIRONMENTS MICROFOSSILS
分 类 号:P53[天文地球—古生物学与地层学]
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