The Wenne river bank section - an excellent section for the Visean-Serpukhovian boundary based on conodonts and ammonoids (Mississippian; Rhenish Mountains, Germany)
Wang, Qiulai (王秋来)1,2,3; Korn, Dieter3; Nemyrovska, Tamara4; Qi, Yuping (祁玉平)1
刊名NEWSLETTERS ON STRATIGRAPHY
2018-09-01
卷号51期号:4页码:427-444
关键词Visean Serpukhovian Boundary Conodont Ammonoid Rhenish Mountains
ISSN号0078-0421
DOI10.1127/nos/2018/0440
英文摘要

We studied the Visean-Serpukhovian boundary section at the Wenne river bank (northern Rhenish Mountains) in detail for its conodont and ammonoid assemblages. A total of 40 productive conodont samples show that the base of the Serpukhovian, marked by the conodont species Lochriea ziegleri, can be precisely determined and correlated to lithostratigraphic and biostratigraphic (ammonoids) marker horizons in the Neoglyphioceras suerlandense Zone. The conodont-defined boundary has a position about 0.50 metres below the base of the so-called Actinopteria Shale', which is a black shale index horizon allowing for lithological correlation in the Rhenish Mountains. For the first time, the Visean-Serpukhovian boundary can now precisely be determined in a section in the Rhenish Mountains; this boundary has a position significantly below the traditional Visean-Namurian boundary.

资助项目National Natural Science Foundation of China[41630101] ; National Natural Science Foundation of China[41290260] ; National Natural Science Foundation of China[41372023] ; National Natural Science Foundation of China[41072009] ; National Natural Science Foundation of China[40772005] ; National Natural Science Foundation of China[40839904] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB18000000] ; Deutsche Forschungsgemeinschaft (DFG project)[Ko1829/2-1]
WOS关键词Verkhnyaya Kardailovka Section ; South China ; Biostratigraphy ; Stage ; Basin ; Goniatites ; Succession ; Lochriea ; Guizhou ; Massif
WOS研究方向Geology
语种英语
出版者GEBRUDER BORNTRAEGER
WOS记录号WOS:000444771600003
资助机构National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Deutsche Forschungsgemeinschaft (DFG project)
内容类型期刊论文
源URL[http://ir.nigpas.ac.cn/handle/332004/16907]  
专题中国科学院南京地质古生物研究所
南京地质古生物研究所_其他
通讯作者Korn, Dieter
作者单位1.Chinese Acad Sci, CAS Key Lab Econ Stratig & Palaeogeog, Nanjing Inst Geol & Palaeontol, East Beijing Rd 39, Nanjing 210008, Jiangsu, Peoples R China
2.Univ Chinese Acad Sci, 19A Yuquan Rd, Beijing 100049, Peoples R China
3.Leibniz Inst Evolut & Biodiversitatsforsch, Museum Nat Kunde, Invalidenstr 43, D-10115 Berlin, Germany
4.Natl Acad Sci Ukraine, Inst Geol Sci, O Gonchar Str 55-B, UA-01601 Kiev, Ukraine
推荐引用方式
GB/T 7714
Wang, Qiulai ,Korn, Dieter,Nemyrovska, Tamara,et al. The Wenne river bank section - an excellent section for the Visean-Serpukhovian boundary based on conodonts and ammonoids (Mississippian; Rhenish Mountains, Germany)[J]. NEWSLETTERS ON STRATIGRAPHY,2018,51(4):427-444.
APA Wang, Qiulai ,Korn, Dieter,Nemyrovska, Tamara,&Qi, Yuping .(2018).The Wenne river bank section - an excellent section for the Visean-Serpukhovian boundary based on conodonts and ammonoids (Mississippian; Rhenish Mountains, Germany).NEWSLETTERS ON STRATIGRAPHY,51(4),427-444.
MLA Wang, Qiulai ,et al."The Wenne river bank section - an excellent section for the Visean-Serpukhovian boundary based on conodonts and ammonoids (Mississippian; Rhenish Mountains, Germany)".NEWSLETTERS ON STRATIGRAPHY 51.4(2018):427-444.
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