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Carboniferous conodont zonation of China
Corresponding AuthorQi, Yuping(ypqi@nigpas.ac.cn)
Hu, Keyi (胡科毅); Qi, Yuping (祁玉平); Qie, Wenkun (郄文昆); Wang, Qiulai (王秋来)
2019
Source PublicationNewsletters on Stratigraphy
ISSN0078-0421
Volume53Issue:2Pages:141-190
AbstractCarboniferous 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.
KeywordCarboniferous conodont zonation China global correlation
DOI10.1127/nos/2019/0498
Indexed BySCI
Language英语
WOS KeywordVISEAN-SERPUKHOVIAN BOUNDARY ; GLOBAL STRATOTYPE SECTION ; VERKHNYAYA KARDAILOVKA SECTION ; MIDCARBONIFEROUS BOUNDARY ; SOUTH URALS ; PENNSYLVANIAN CONODONTS ; DEVONIAN/CARBONIFEROUS BOUNDARY ; BARCALIENTE FORMATION ; MORPHOMETRIC-ANALYSIS ; PERMIAN BOUNDARY
Funding ProjectChinese 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 Research AreaGeology
WOS SubjectGeology
WOS IDWOS:000541129400002
Funding OrganizationChinese 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)
PublisherGEBRUDER BORNTRAEGER
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Document Type期刊论文
Identifierhttp://ir.nigpas.ac.cn/handle/332004/31488
Collection中国科学院南京地质古生物研究所
Recommended Citation
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.
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