Katian (Late Ordovician) conodonts on the northwestern margin of the North China Craton

被引:6
作者
Yang, Zhihua [1 ]
Jing, Xiuchun [1 ]
Zhou, Hongrui [1 ]
Wang, Xunlian [1 ]
Ren, Hui [1 ]
Shen, Yang [2 ,3 ]
Fan, Ru [4 ]
机构
[1] China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
[2] China Univ Geosci, Museum, Beijing 100083, Peoples R China
[3] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
[4] Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China
基金
中国国家自然科学基金;
关键词
CLIEFDEN CAVES LIMESTONE; NEW-SOUTH-WALES; INNER-MONGOLIA; SANDBIAN CONODONTS; MIDDLE ORDOVICIAN; WUHAI AREA; BIOSTRATIGRAPHY; AGE; MEMBER; REDEFINITION;
D O I
10.1017/jpa.2021.11
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Upper Ordovician strata exposed from the Baiyanhuashan section is the most representative Late Ordovician unit in the northwestern margin of the North China Craton (NCC). In total, 1,215 conodont specimens were obtained from 24 samples through the Wulanhudong and Baiyanhuashan formations at the Baiyanhuashan section. Thirty-six species belonging to 17 genera, including Tasmanognathus coronatus new species, are present. Based on this material, three conodont biozones-the Belodina confluens Biozone, the Yaoxianognathus neimengguensis Biozone, and the Yaoxianognathus yaoxianensis Biozone-have been documented, suggesting that the Baiyanhuashan conodont fauna has a stratigraphic range spanning the early to middle Katian. The Baiyanhuashan conodont fauna includes species both endemic to North China and widespread in tropical zones, allowing a reassessment of the previous correlations of the Katian conodont zonal successions proposed for North China with those established for shallow-water carbonate platforms at low latitudes. UUID: http://zoobank.org/7cedbd4a-4f7a-4be6-912f-a27fd041b586
引用
收藏
页码:805 / 826
页数:22
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