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

Qiulai Wang; Yue Wang; Yuping Qi; Xiangdong Wang; Suk Joo Choh; Dong Chan Lee; Dong Jin Lee

doi:10.1080/03115518.2017.1395077

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

Qiulai Wang, Yue Wang, Yuping Qi, Xiangdong Wang, Suk Joo Choh, Dong Chan Lee, Dong Jin Lee

Research output: Contribution to journal › Article › peer-review

4 Citations (Scopus)

Abstract

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.

Original language	English
Pages (from-to)	244-257
Number of pages	14
Journal	Alcheringa
Volume	42
Issue number	2
DOIs	https://doi.org/10.1080/03115518.2017.1395077
Publication status	Published - 2018 Apr 3

Bibliographical note

Funding Information:
We wish to thank V. Chernykh for his useful comments on the identification of the conodonts, Y. Gatovsky and an anonymous reviewer for reviewing the manuscript and the journal’s editors for very useful comments and suggestions. This work is supported by the National Natural Science Foundation of China (Grants No. 41290260, 41630101, 41372024), the Strategic Priority Research Program (B) of the Chinese Academy of Sciences (XDB18030400), the Ministry of Science and Technology of China (grant number 2015FY310100, 2011CB808905) and National Research Foundation of Korea (2014K2A3A2000787).

Funding Information:
This work was supported by the National Natural Science Foundation of China [grant number 41290260,41372024,41630101]; Ministry of Science and Technology of China [grant number 2011CB808905,2015FY310100]; National Research Foundation of Korea [grant number 2014K2A3A2000787]; Strategic Priority Research Program (B) of the Chinese Academy of Sciences [grant number XDB18030400].

Publisher Copyright:
© 2017, © 2017 Geological Society of Australia Inc., Australasian Palaeontologists.

Copyright:
Copyright 2018 Elsevier B.V., All rights reserved.

Keywords

Bamchi Formation
Carboniferous–Permian
Korea
conodonts
fusulines

ASJC Scopus subject areas

Ecology, Evolution, Behavior and Systematics
Palaeontology

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10.1080/03115518.2017.1395077

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

abstract = "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.",

keywords = "Bamchi Formation, Carboniferous–Permian, Korea, conodonts, fusulines",

author = "Qiulai Wang and Yue Wang and Yuping Qi and Xiangdong Wang and Choh, {Suk Joo} and Lee, {Dong Chan} and Lee, {Dong Jin}",

note = "Funding Information: We wish to thank V. Chernykh for his useful comments on the identification of the conodonts, Y. Gatovsky and an anonymous reviewer for reviewing the manuscript and the journal{\textquoteright}s editors for very useful comments and suggestions. This work is supported by the National Natural Science Foundation of China (Grants No. 41290260, 41630101, 41372024), the Strategic Priority Research Program (B) of the Chinese Academy of Sciences (XDB18030400), the Ministry of Science and Technology of China (grant number 2015FY310100, 2011CB808905) and National Research Foundation of Korea (2014K2A3A2000787). Funding Information: This work was supported by the National Natural Science Foundation of China [grant number 41290260,41372024,41630101]; Ministry of Science and Technology of China [grant number 2011CB808905,2015FY310100]; National Research Foundation of Korea [grant number 2014K2A3A2000787]; Strategic Priority Research Program (B) of the Chinese Academy of Sciences [grant number XDB18030400]. Publisher Copyright: {\textcopyright} 2017, {\textcopyright} 2017 Geological Society of Australia Inc., Australasian Palaeontologists. Copyright: Copyright 2018 Elsevier B.V., All rights reserved.",

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doi = "10.1080/03115518.2017.1395077",

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AU - Wang, Yue

AU - Qi, Yuping

AU - Wang, Xiangdong

AU - Choh, Suk Joo

AU - Lee, Dong Chan

AU - Lee, Dong Jin

N1 - Funding Information: We wish to thank V. Chernykh for his useful comments on the identification of the conodonts, Y. Gatovsky and an anonymous reviewer for reviewing the manuscript and the journal’s editors for very useful comments and suggestions. This work is supported by the National Natural Science Foundation of China (Grants No. 41290260, 41630101, 41372024), the Strategic Priority Research Program (B) of the Chinese Academy of Sciences (XDB18030400), the Ministry of Science and Technology of China (grant number 2015FY310100, 2011CB808905) and National Research Foundation of Korea (2014K2A3A2000787). Funding Information: This work was supported by the National Natural Science Foundation of China [grant number 41290260,41372024,41630101]; Ministry of Science and Technology of China [grant number 2011CB808905,2015FY310100]; National Research Foundation of Korea [grant number 2014K2A3A2000787]; Strategic Priority Research Program (B) of the Chinese Academy of Sciences [grant number XDB18030400]. Publisher Copyright: © 2017, © 2017 Geological Society of Australia Inc., Australasian Palaeontologists. Copyright: Copyright 2018 Elsevier B.V., All rights reserved.

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N2 - 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.

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

Abstract

Bibliographical note

Keywords

ASJC Scopus subject areas

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