[an error occurred while processing this directive] | Global Geology 2019, 22(4) 270-279 DOI: 10.3969/j.issn.1673-9736.2019.04.05 ISSN: 1673-9736 CN: 22-1371/P | ||||||||||||||||||||||||||||||||||||||||||||||
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Stratigraphy and palaeoenvironments across the Jurassic-Cretaceous boundary in the reference section (Olenek River) for eastern regions of Laptev Sea area (Arctic Siberia, Russia) | |||||||||||||||||||||||||||||||||||||||||||||||
Boris L. Nikitenko1,2, Ekaterina B. Pestchevitskaya1, Svetlana N. Khafaeva1 | |||||||||||||||||||||||||||||||||||||||||||||||
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 | |||||||||||||||||||||||||||||||||||||||||||||||
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. | |||||||||||||||||||||||||||||||||||||||||||||||
关键词: Upper Jurassic Lower Cretaceous Arctic Siberia biostratigraphy palaeoenvironments microfossils | |||||||||||||||||||||||||||||||||||||||||||||||
Stratigraphy and palaeoenvironments across the Jurassic-Cretaceous boundary in the reference section (Olenek River) for eastern regions of Laptev Sea area (Arctic Siberia, Russia) | |||||||||||||||||||||||||||||||||||||||||||||||
Boris L. Nikitenko1,2, Ekaterina B. Pestchevitskaya1, Svetlana N. Khafaeva1 | |||||||||||||||||||||||||||||||||||||||||||||||
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 | |||||||||||||||||||||||||||||||||||||||||||||||
Abstract: 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. | |||||||||||||||||||||||||||||||||||||||||||||||
Keywords: Upper Jurassic Lower Cretaceous Arctic Siberia biostratigraphy palaeoenvironments microfossils | |||||||||||||||||||||||||||||||||||||||||||||||
收稿日期 2019-10-12 修回日期 2019-10-28 网络版发布日期 | |||||||||||||||||||||||||||||||||||||||||||||||
DOI: 10.3969/j.issn.1673-9736.2019.04.05 | |||||||||||||||||||||||||||||||||||||||||||||||
基金项目:
The authors are grateful to Prof. Dr. SUN Ge for the support allowing the presentation of the material in Global Geology. Financial support:Russian Science Foundation 18-17-00038. Scientific support:Russian FSI 0331-2019-0004; IGCP 679, 632. | |||||||||||||||||||||||||||||||||||||||||||||||
通讯作者: Ekaterina B. Pestchevitskaya | |||||||||||||||||||||||||||||||||||||||||||||||
作者简介: | |||||||||||||||||||||||||||||||||||||||||||||||
作者Email: PeschevickayaEB@ipgg.sbras.ru | |||||||||||||||||||||||||||||||||||||||||||||||
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