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Article by Wang C
Article by Lang J
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1. �й���ѧԺ�Ͼ����ʹ������о���, �Ͼ� 210008;
2. ���ִ�ѧ������ѧ��ز�ѧ�о�����, ���� 130026;
3. ���ִ�ѧ�����������ݻ��뻷���������ص�ʵ����, ���� 130026
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Triassic stages and conodont biostratigraphy
WANG Cheng-yuan1,3, LANG Jia-bin2,3
1. Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing 210008, China;
2. Research Center of Paleontology & Stratigraphy, Jilin University, Changchun 130026, China;
3. Key Laboratory for Evolution of Past Life and Environment in NE Asia(Jilin University), Ministry of Education, Changchun 130026, China
Abstract: The time interval of three series and seven stages of Triassic are quite different,of which the Late Triassic is the longest. As a leading fossil group, conodont becomes more and more important in the divisions of biostratigraphy. The Triassic conodont biozones in China have reached 50 biozones,and could be increased more in the future,especially in the Upper Triassic. Stage is a global chronological unit,it should be used globally,with uniform name and definition. It should not be established based on country,lithological facies or biogroup. Terrestrial strata are not suitable for establishing stage,the terrestrial chronostratigraphic stage names should be abandoned.
Keywords: stage   terrestrial chronostratigraphic stage   conodont   biostratigraphy  
�ո����� 2018-10-14 �޻����� 2018-12-28 ����淢������  
DOI: 10.3969/j.issn.1004-5589.2019.01.003
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