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DOI10.1016/j.palaeo.2018.07.021
Late Mississippian glacio-eustasy recorded in the eastern Paleo-Tethys Ocean (South China)
Chen J.; Sheng Q.; Hu K.; Yao L.; Lin W.; Montañez I.P.; Tian X.; Qi Y.; Wang X.
发表日期2019
ISSN0031-0182
卷号531
英文摘要Long-lived and extensive glaciation during the Carboniferous and early Permian has been the focus of many studies over the past decade revealing systematic changes in sea level and climatic conditions. The nature of the inception of Carboniferous glaciation, however, remains poorly resolved with uncertainty regarding the timing and dynamics of buildup of continental ice sheets. Here we present detailed sedimentary facies and depositional cycles from Upper Mississippian shallow-water platform and contemporaneous carbonate slope successions from the eastern Paleo-Tethys Ocean region (South China) to reveal systematic variations that provide insight into the sedimentary response to the onset of Carboniferous glaciation. Based on detailed sedimentological logging and facies analysis, four upper Visean cycles and four Serpukhovian cycles were identified from the carbonate platform Yashui section, bounded by either subaerial surfaces or zones, or transgressive surfaces. The cycle tops roughly correspond to intervals rich in normally graded bioclastic wacke- to packstones and with distinct rises (~1‰) in conodont δ18OPO4 in the carbonate slope Naqing section. In particular, the four Serpukhovian cycles correlate well to depositional cycles defined in the Lower Yangtze Platform succession of South China and in the cyclothemic successions in the Donets Basin, Ukraine, suggesting a glacio-eustatic control, most likely caused by repeated advance and retreat of Gondwana glaciation during the onset but prior to widespread glaciation across the mid-Carboniferous boundary. © 2018 Elsevier B.V.
英文关键词Carboniferous; Cyclothem; Depositional cycle; Icehouse; Late Paleozoic ice age; Lithofacies
语种英语
scopus关键词carbonate platform; Carboniferous; conodont; cyclothem; depositional sequence; glaciation; Gondwana; lithofacies; oxygen isotope; Paleozoic; Permian; Pleistocene; Serpukhovian; Visean; China; Donets Basin; Ukraine; Yangtze Platform
来源期刊Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/150876
作者单位CAS Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing, 210008, China; Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Minerals, Shandong University of Science and Technology, Qingdao, 266590, China; Center for Research and Education on Biological Evolution and Environment, Nanjing University, Nanjing, 210023, China; Department of Earth and Planetary Sciences, University of California Davis, California, 95616, United States; University of Science and Technology of China, Hefei, 230026, China
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GB/T 7714
Chen J.,Sheng Q.,Hu K.,et al. Late Mississippian glacio-eustasy recorded in the eastern Paleo-Tethys Ocean (South China)[J],2019,531.
APA Chen J..,Sheng Q..,Hu K..,Yao L..,Lin W..,...&Wang X..(2019).Late Mississippian glacio-eustasy recorded in the eastern Paleo-Tethys Ocean (South China).Palaeogeography, Palaeoclimatology, Palaeoecology,531.
MLA Chen J.,et al."Late Mississippian glacio-eustasy recorded in the eastern Paleo-Tethys Ocean (South China)".Palaeogeography, Palaeoclimatology, Palaeoecology 531(2019).
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