Revised conodont and fusuline biostratigraphy of the Bamchi Formation (Pyongan Supergroup) at the Bamchi section, Yeongwol and the Carboniferous-Permian boundary in South Korea

被引:3
|
作者
Wang, Qiulai [1 ,6 ]
Wang, Yue [2 ,6 ]
Qi, Yuping [1 ,6 ]
Wang, Xiangdong [1 ,6 ]
Choh, Suk-Joo [3 ]
Lee, Dong-Chan [4 ]
Lee, Dong-Jin [5 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, CAS Key Lab Econ Stratig & Palaeogeog, East Beijing Rd 39, Nanjing 210008, Jiangsu, Peoples R China
[2] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, LPS, East Beijing Rd 39, Nanjing 210008, Jiangsu, Peoples R China
[3] Korea Univ, Dept Earth & Environm Sci, Seoul 02841, South Korea
[4] Chungbuk Natl Univ, Dept Earth Sci Educ, Cheongju 28644, South Korea
[5] Andong Natl Univ, Dept Earth & Environm Sci, Andong 36729, South Korea
[6] Univ Chinese Acad Sci, 19A Yuquan Rd, Beijing 100049, Peoples R China
来源
ALCHERINGA | 2018年 / 42卷 / 02期
基金
新加坡国家研究基金会; 中国国家自然科学基金;
关键词
conodonts; fusulines; Bamchi Formation; Carboniferous-Permian; Korea; STREPTOGNATHODUS CONODONTA; TECTONIC CORRELATION; STRATOTYPE SECTION; CHINA; PENINSULA; AIDARALASH; EVOLUTION; JAPAN; BELT; BASE;
D O I
10.1080/03115518.2017.1395077
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Six 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 the Streptognathodus bellus, S. isolatus, S. cristellaris, S. sigmoidalis, S. fusus and S. barskovi zones 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 the Rugosofusulina complicata-Pseudoschwagerina paraborealis zone. The co-occurrence of the conodont Streptognathodus isolatus (the Global Boundary Stratotype Section and Point index for the base of Permian) and Pseudoschwagerina (a Permian inflated fusuline) indicates that the Carboniferous-Permian boundary can be placed in the lower part of the Bamchi Formation in South Korea.
引用
收藏
页码:244 / 257
页数:14
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