Revised conodont and fusuline biostratigraphy of the Bamchi Formation (Pyongan Supergroup) at the Bamchi section, Yeongwol and the Carboniferous-Permian boundary in South Korea
Revised conodont and fusuline biostratigraphy of the Bamchi Formation (Pyongan Supergroup) at the Bamchi section, Yeongwol and the Carboniferous-Permian boundary in South Korea
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韩国宁越 Bamchi 剖面和石炭系 - 二叠纪边界的 Bamchi 组（平安超群）修正的牙形刺和梭状生物地层学
DOI：
10.1080/03115518.2017.1395077
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发表时间：
2018
期刊：
影响因子：
1.3
通讯作者：
Dong-Jin Lee
中科院分区：
文献类型：
--
作者：
Qiulai Wang;Yue Wang;Yuping Qi;Xiangdong Wang;Suk-Joo Choh;Dong-Chan Lee;Dong-Jin Lee
王勤、王勇、齐勇、王霞、周星杰、李连杰、李连杰，2017年11月。韩国的永武和石炭系-二叠系界线。根据ISSN0311-5518共鉴定出25种牙形刺和13种(包括7个未鉴定种和7个未鉴定种)，识别出6个牙形刺和1个丝状牙形带。或者是Af。总共)，来自韩国永武的Bamchi组。牙形刺带由大到小依次为：链形刺带Bellus、S.solatus、S.cristellaris、S.sigmoidaris、S.fusus和S.barskovizones，可与全球二叠纪最晚Gzhelian-Asselian时代的牙形刺带对比。该丝状带被命名为复合型Rugosofusulina-Partioschwagerina paraboreiszone。二叠纪底全球界线层型剖面和点指数的共生表明石炭-二叠系界线可置于韩国班其组的下部。中国科学院南京地质古生物研究所经济地层与古地理重点实验室，南京东路39号，南京，210008；中国科学院南京地质古生物研究所，北京东路39号，南京210008，PR中国；中国科学院南京地质古生物研究所经济地层与古地理重点实验室，中国科学院南京地质古生物研究所，北京东路39号，南京210008，PR；韩国首尔，韩国首尔，韩国大学地球环境科学系，韩国首尔，02841；李东灿[dclee@chungbuk.ac.kr]韩国清州28644忠北国立大学地球科学教育系；韩国安东国立大学地球与环境科学系，韩国安东36729。*隶属于：中国科学院大学，石景山区玉泉路19A号，邮编：100049，PR中国。
Wang, Q., Wang, Y., Qi, Y., Wang, X., Choh, S.J., Lee, D.C. & Lee, D.J., November 2017. Yeongwol and the Carboniferous–Permian boundary in South Korea.Alcheringa 42, 245–258. ISSN 0311-5518Six conodont and one fusuline zones are recognized on basis of a total of 25 conodont and 13 fusuline species (including seven unidentified species or species given with cf. or aff. in total) from the Bamchi Formation, Yeongwol, Korea. The conodont zones include theStreptognathodus bellus,S.isolatus,S.cristellaris,S.sigmoidalis,S.fususandS.barskovizones in ascending order, which can be correlated with the conodont zones spanning the uppermost Gzhelian to Asselian Age of the Permian globally. The fusuline zone is named theRugosofusulina complicata–Pseudoschwagerina paraborealiszone. The co-occurrence of the conodontStreptognathodus isolatus(the Global Boundary Stratotype Section and Point index for the base of Permian) andPseudoschwagerina(a Permian inflated fusuline) indicates that the Carboniferous–Permian boundary can be placed in the lower part of the Bamchi Formation in South Korea.Qiulai Wang* [qlwang@nigpas.ac.cn] CAS Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, East Beijing Road 39, Nanjing 210008, PR China; Yue Wang* [yuewang@nigpas.ac.cn] LPS, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, East Beijing Road 39, Nanjing 210008, PR China; Yuping Qi* [ypqi@nigpas.ac.cn] Xiangdong Wang* [xdwang@nigpas.ac.cn] CAS Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, East Beijing Road 39, Nanjing 210008, PR China; Suk-Joo Choh [sjchoh@korea.ac.kr] Department of Earth and Environmental Sciences, Korea University, Seoul 02841, Republic of Korea; Dong-Chan Lee [dclee@chungbuk.ac.kr] Department of Earth Sciences Education, Chungbuk National University, Cheongju 28644, Republic of Korea; Dong-Jin Lee [djlee@andong.ac.kr] Department of Earth and Environmental Sciences, Andong National University, Andong 36729, Republic of Korea. *Also affiliated with: University of Chinese Academy of Sciences, 19A Yuquan Road, Shijingshan District, Beijing 100049, PR China.