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Late Visean – early Serpukhovian conodont succession at the Naqing (Nashui) section in Guizhou, South China

Published online by Cambridge University Press:  08 October 2013

YUPING QI ,
TAMARA I. NEMYROVSKA ,
XIANGDONG WANG ,
JITAO CHEN ,
ZHIHAO WANG ,
H. RICHARD LANE ,
BARRY C. RICHARDS ,
KEYI HU  and
QIULAI WANG
YUPING QI*
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, China
TAMARA I. NEMYROVSKA
Affiliation:
Institute of Geological Sciences, National Academy of Sciences of Ukraine, 55-b O. Gonchar Str., 01601, Kiev, Ukraine
XIANGDONG WANG
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, China
JITAO CHEN
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, China
ZHIHAO WANG
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, China
H. RICHARD LANE
Affiliation:
National Science Foundation of USA, 4201 Wilson Blvd., Arlington, VA, 22230, USA
BARRY C. RICHARDS
Affiliation:
Geological Survey of Canada, 3303–33rd Street, NW, Calgary AB, T2L 2A7, Canada
KEYI HU
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, China
QIULAI WANG
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, China
*
†Author for correspondence: ypqi@nigpas.ac.cn
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Abstract

This study reports the conodont succession across the Visean–Serpukhovian (V/S) boundary interval at the Naqing section, South China. Continuous centimetre-scale sampling of the relatively deep-water section in recent years has provided new data for a more detailed biostratigraphy of conodonts across the Visean–Serpukhovian boundary. Three conodont zones were described in ascending order: the Gnathodus bilineatus, Lochriea nodosa and Lochriea ziegleri zones. The first appearance datum (FAD) of L. ziegleri has been moved down to 60.1 m above the base of the Naqing section. The correlation of the conodont succession across the Visean–Serpukhovian boundary in the Naqing section with other sections in Eurasia is discussed.

Keywords

conodont successionVisean–Serpukhovian boundarycandidate GSSPNaqing sectionSouth China
Type
Original Articles
Information
Geological Magazine , Volume 151 , Issue 2 , March 2014 , pp. 254 - 268
Copyright
Copyright © Cambridge University Press 2013 

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