Discovery of Anticostia uniformis from the Xiazhen Formation at Zhuzhai, South China and its stratigraphic implication

被引:11
|
作者
Chen, Zhong-Yang [1 ,2 ]
Kim, Myong-Hak [3 ]
Choh, Suk-Joo [4 ]
Lee, Dong-Jin [5 ,6 ]
Chen, Xu [1 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Key Lab Econ Stratig & Palaeogeog, Nanjing 210008, Jiangsu, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Kim Chaek Univ Technol, Dept Resources Explorat Engn, Pyongyang, South Korea
[4] Korea Univ, Dept Earth & Environm Sci, Seoul 136701, South Korea
[5] Andong Natl Univ, Dept Earth & Environm Sci, Andong 760749, South Korea
[6] Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China
基金
新加坡国家研究基金会; 中国国家自然科学基金;
关键词
Xiazhen Formation; Graptolite; Anticostia uniformis; South China; LATE ORDOVICIAN; YANGTZE REGION; GRAPTOLITE; EXTINCTION;
D O I
10.1016/j.palwor.2015.11.011
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
The Xiazhen Formation is an Upper Ordovician lithostratigraphic unit in the Jiangshan-Changshan-Yushan (JCY) area, which contains series of Late Ordovician reef successions. The reef successions of the Xiazhen Formation at Zhuzhai are critical for evaluation of the Late Ordovician marine diversity and palaeoecology. However, their age has long been uncertain and generally is regarded as of upper Katian, based on the occurrences of shelly fossils and correlation with the stratigraphic equivalent Changwu Formation. The newly discovered graptolite species Anticostia uniformis, in the Xiazhen Formation, together with the combined evidence of brachiopods and sedimentology, indicates an age range for the graptolite locality from the Dicellograptus complanatus Biozone to the Diceratograptus mirus Subzone of late Katian, but the graptolites do not rule out the possibility that it is Hirnantian. (C) 2015 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
引用
收藏
页码:356 / 361
页数:6
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