中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Redefinition of the Global Stratotype Section and Point (GSSP) and new Standard Auxiliary Boundary Stratotype (SABS) for the base of Wuchiapingian Stage (Lopingian Series, Permian) in South China

文献类型:期刊论文

作者Shen, Shu-zhong1,2; Yuan, Dong-xun3; Zhang, Yi-chun4; Henderson, Charles M.5; Zheng, Quan-feng4; Zhang, Hua4; Zhang, Min6; Dai, Yu7; Xu, Hai-peng1,2; Wang, Wen-qian1,2
刊名EPISODES
出版日期2024-03-01
卷号47期号:1页码:147-177
ISSN号0705-3797
DOI10.18814/epiiugs/2023/023023
通讯作者Shen, Shu-zhong(szshen@nju.edu.cn)
英文摘要The Global Stratotype Section and Point (GSSP) of the base-Wuchiapingian Stage was formally ratified at the Penglaitan section in South China in 2005. However, the riverside GSSP section at Penglaitan and its auxiliary section at Tieqiao have been permanently flooded since 2020. We herein designate an excavated section at Penglaitan as the new GSSP and the Fengshan section as a new Standard Auxiliary Boundary Stratotype (SABS). In addition, we revised the original definition based on a detailed restudy of the conodont succession from the two sections. We define the GSSP of the base-Wuchiapingian by the First Appearance Datum (FAD) of Clarkina postbitteri within the lineage Jinogondolella granti -> Clarkina postbitteri -> C. dukouensis. . It represents a major evolutionary turnover in conodonts from Jinogondolella to Clarkina and marks the end-Guadalupian extinction event. The U-Pb date of 259.51 +/- 0.21 Ma from the uppermost part of the Emeishan basalt is adopted for the GLB age. delta C-13(carb) chemostratigraphy at the SABS exhibits several excursions between 3% and 5% across the GLB interval. Carbonate Sr-87/Sr-86 ratio is 0.707244 at the GLB. Remarkably, the SABS contains six normal and six reverse geomagnetic polarity zones in the uppermost Capitanian and three in the lowest Wuchiapingian.
WOS关键词PALEO-ATOLL CARBONATES ; DOUBLE MASS EXTINCTION ; REEF TRAIL MEMBER ; CONODONT BIOSTRATIGRAPHY ; BRACHIOPODS ; TIMESCALE ; MOUNTAINS ; VOLCANISM ; RECORD ; END
资助项目National Natural Science Foundation
WOS研究方向Geology
语种英语
WOS记录号WOS:001299167300001
出版者GEOLOGICAL SOC KOREA
资助机构National Natural Science Foundation
源URL[http://ir.nigpas.ac.cn/handle/332004/44251]  
专题中国科学院南京地质古生物研究所
通讯作者Shen, Shu-zhong
作者单位1.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Peoples R China
2.Nanjing Univ, Frontiers Sci Ctr Crit Earth Mat Cycling, Nanjing 210023, Peoples R China
3.China Univ Min & Technol, Sch Resources & Geosci, Xuzhou 221116, Peoples R China
4.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
5.Univ Calgary, Dept Geosci, Calgary, AB T2N 1N4, Canada
6.Chinese Acad Sci, Inst Geol & Geophys, Chinese Acad Sci CAS Key Lab Earth & Planetary Phy, Beijing 100029, Peoples R China
7.Reg Geol Survey, Guangxi Inst, 6 Huanchengnaner Rd, Guilin, Guangxi, Peoples R China
8.MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
9.Natl Museum Nat Hist, Dept Paleobiol, MRC 121, Washington, DC 20013 USA
10.Univ Milan, Dipartimento Sci Terra Ardito Desio, Via Mangiagalli 34, I-20133 Milan, Italy
推荐引用方式
GB/T 7714
Shen, Shu-zhong,Yuan, Dong-xun,Zhang, Yi-chun,et al. Redefinition of the Global Stratotype Section and Point (GSSP) and new Standard Auxiliary Boundary Stratotype (SABS) for the base of Wuchiapingian Stage (Lopingian Series, Permian) in South China[J]. EPISODES,2024,47(1):147-177.
APA Shen, Shu-zhong.,Yuan, Dong-xun.,Zhang, Yi-chun.,Henderson, Charles M..,Zheng, Quan-feng.,...&Mei, Shi-long.(2024).Redefinition of the Global Stratotype Section and Point (GSSP) and new Standard Auxiliary Boundary Stratotype (SABS) for the base of Wuchiapingian Stage (Lopingian Series, Permian) in South China.EPISODES,47(1),147-177.
MLA Shen, Shu-zhong,et al."Redefinition of the Global Stratotype Section and Point (GSSP) and new Standard Auxiliary Boundary Stratotype (SABS) for the base of Wuchiapingian Stage (Lopingian Series, Permian) in South China".EPISODES 47.1(2024):147-177.

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来源:南京地质古生物研究所

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