中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Oldest-known Neoproterozoic carbon isotope excursion: Earlier onset of Neoproterozoic carbon cycle volatility

文献类型:期刊论文

作者Zhang, Zhiyue1,2,5; Peng, Peng1,2,5; Feng, Lianjun2,4,5; Gong, Zheng3; Mitchell, Ross N.1,2; Li, Youlian1,2
刊名GONDWANA RESEARCH
出版日期2021-06-01
卷号94页码:1-11
ISSN号1342-937X
关键词North China Craton Neoproterozoic Dalian basin Carbon isotopes Paleogeography
DOI10.1016/j.gr.2021.01.013
英文摘要The Neoproterozoic Era (1000?541 Ma) is characterized by the largest negative carbon isotope excursions in Earth history. Younger Neoproterozoic excursions are well-documented on multiple continental margins and associated with major events including snowball Earth glaciations, ocean-atmosphere oxygenation, and the evolution of animal multicellularity. However, due to a large gap in carbon isotopes before 900 Ma, the onset of early Neoproterozoic carbon cycle volatility has heretofore been obscure. Here, we present a mid-amplitude, negative carbon isotope excursion with 813C values reaching a nadir of- ? 6? from the Majiatun Formation in the Dalian Basin of the North China Craton dated between 950 and 920 Ma. The whole-rock 87Sr/86Sr ratios of limestone and dolostone are as low as -0.7055, which is compatible with the Tonian age of the global carbonate curve. Identification of the Majiatun anomaly thus fills the critical gap in carbon isotopes and implies the onset of Neoproterozoic carbon cycle volatility -130 m.y. earlier than previously thought. Now 5 negative carbon isotope excursions occur with increasing amplitude throughout Neoproterozoic time, implying deeper roots for the biogeochemical processes that may have causally led to late Neoproterozoic snowball glaciation, oxygenation, and biological innovation. (c)& nbsp;2021 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
WOS关键词NORTH CHINA CRATON ; TRUE POLAR WANDER ; U-PB ; AUTHIGENIC CARBONATE ; LIAODONG PENINSULA ; TRACE-ELEMENT ; EVOLUTION ; CONSTRAINTS ; GEOCHRONOLOGY ; GEOCHEMISTRY
资助项目National Natural Science Foundation of China[41890833] ; National Natural Science Foundation of China[41772192] ; National Natural Science Foundation of China[41888101] ; Key Research Programs of Chinese Academy of Sciences[IGGCAS-201905] ; Key Research Programs of Chinese Academy of Sciences[QYZDB-SSWDQC042] ; Key Research Programs of Chinese Academy of Sciences[GJHZ2016] ; Key Research Programs of Chinese Academy of Sciences[XDB41000000] ; Key Research Programs of Chinese Academy of Sciences[XDB18030205]
WOS研究方向Geology
语种英语
出版者ELSEVIER
WOS记录号WOS:000643562600001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences ; Key Research Programs of Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/101112]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Peng, Peng; Mitchell, Ross N.
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Innovat Acad Earth Sci, China Brazil Joint Res Ctr, Beijing 100029, Peoples R China
3.Yale Univ, Dept Earth & Planetary Sci, 210 Whitney Ave, New Haven, CT 06511 USA
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100049, Peoples R China
5.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Zhiyue,Peng, Peng,Feng, Lianjun,et al. Oldest-known Neoproterozoic carbon isotope excursion: Earlier onset of Neoproterozoic carbon cycle volatility[J]. GONDWANA RESEARCH,2021,94:1-11.
APA Zhang, Zhiyue,Peng, Peng,Feng, Lianjun,Gong, Zheng,Mitchell, Ross N.,&Li, Youlian.(2021).Oldest-known Neoproterozoic carbon isotope excursion: Earlier onset of Neoproterozoic carbon cycle volatility.GONDWANA RESEARCH,94,1-11.
MLA Zhang, Zhiyue,et al."Oldest-known Neoproterozoic carbon isotope excursion: Earlier onset of Neoproterozoic carbon cycle volatility".GONDWANA RESEARCH 94(2021):1-11.

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来源:地质与地球物理研究所

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