Carboniferous conodont zonation of China

doi:10.1127/nos/2019/0498

NIGPAS OpenIR

	Carboniferous conodont zonation of China
通讯作者	Qi, Yuping([email protected])
	Hu, Keyi （胡科毅）; Qi, Yuping （祁玉平）; Qie, Wenkun （郄文昆）; Wang, Qiulai （王秋来）
	2019
发表期刊	Newsletters on Stratigraphy
ISSN	0078-0421
卷号	53 期号:2 页码:141-190
摘要	Carboniferous conodonts from the candidate GSSPs of the four stages Serpukhovian, Moscovian, Kasimovian and Gzhelian in the Naqing and the adjacent sections of South China have been intensely studied in recent decades. The Carboniferous conodont zonation of China is updated based on the conodont material from South China; 39 conodont zones including 11 Tournaisian zones, 4 Visean zones, 3 Serpukhovian zones, 6 Bashkirian zones, 5 Moscovian zones, 5 Kasimovian zones and 5 Gzhelian zones are separated and discussed in detail. Species of the genera Siphonodella, Polygnathus, Protognathodus and Gnathodus dominate the zonation for Early Mississippian (Tournaisian) strata, Pseudognathodus, Lochriea and Gnathodus are most important for the zonation for Middle and Late Mississippian (Visean and Serpukhovian) strata, Declinog-nathodus, Idiognathoides, Neognathodus provide the zonation of early Bashkirian strata and Diplognathodus, Mesogondolella, Idiognathodus and the related genera Swadelina and Streptognathodus provide the zonation for late Bashkirian through the middle and late Pennsylvanian interval. In South China, the Carboniferous conodont zonation is mainly characterized by deep-water conodont biofacies with Siphonodella, Lochriea, Gnathodus, Declinognathodus, Idiognathoides, "Streptognathodus" expansus group, Diplognathodus and Streptognathodus. The updated Carboniferous conodont zonation of China is dominated mainly by cosmopolitan species, which may eventually allow refined global correlation.
关键词	Carboniferous conodont zonation China global correlation
DOI	10.1127/nos/2019/0498
收录类别	SCI
语种	英语
关键词[WOS]	VISEAN-SERPUKHOVIAN BOUNDARY ; GLOBAL STRATOTYPE SECTION ; VERKHNYAYA KARDAILOVKA SECTION ; MIDCARBONIFEROUS BOUNDARY ; SOUTH URALS ; PENNSYLVANIAN CONODONTS ; DEVONIAN/CARBONIFEROUS BOUNDARY ; BARCALIENTE FORMATION ; MORPHOMETRIC-ANALYSIS ; PERMIAN BOUNDARY
资助项目	Chinese Academy of Sciences[XDB26000000] ; Chinese Academy of Sciences[XDB18000000] ; National Natural Science Foundation of China[41630101] ; National Natural Science Foundation of China[41802010] ; National Natural Science Foundation of China[41772004] ; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences)[173110]
WOS研究方向	Geology
WOS类目	Geology
WOS记录号	WOS:000541129400002
项目资助者	Chinese Academy of Sciences ; National Natural Science Foundation of China ; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences)
出版者	GEBRUDER BORNTRAEGER
文献类型	期刊论文
条目标识符	http://ir.nigpas.ac.cn/handle/332004/31488
专题	中国科学院南京地质古生物研究所
推荐引用方式 GB/T 7714	Hu, Keyi ,Qi, Yuping ,Qie, Wenkun ,et al. Carboniferous conodont zonation of China[J]. Newsletters on Stratigraphy,2019,53(2):141-190.
APA	Hu, Keyi ,Qi, Yuping ,Qie, Wenkun ,&Wang, Qiulai .(2019).Carboniferous conodont zonation of China.Newsletters on Stratigraphy,53(2),141-190.
MLA	Hu, Keyi ,et al."Carboniferous conodont zonation of China".Newsletters on Stratigraphy 53.2(2019):141-190.