NIGPAS OpenIR
Permian integrative stratigraphy and timescale of China
Shen, Shuzhong (沈树忠)1,2,3; Zhang, Hua (张华)1,2,3; Zhang, Yichun (张以春)1,2,3; Yuan, Dongxun (袁东勋)1,2,3; Chen, Bo (陈波)1,2,3; He, Weihong4; Mu, Lin (牟林)2,3,5; Lin, Wei (林巍)2,3,5; Wang, Wenqian (王文倩)1,2,6; Chen, Jun7; Wu, Qiong1,2,6; Cao, Changqun (曹长群)1,2,3; Wang, Yue (王玥)1,2,3,6; Wang, Xiangdong (王向东)2,3,5
2019
Source PublicationSCIENCE CHINA-EARTH SCIENCES
ISSN1674-7313
Volume62Issue:1Pages:154-188
Abstract

A series of global major geological and biological events occurred during the Permian Period. Establishing a highresolution stratigraphic and temporal framework is essential to understand their cause-effect relationship. The official International timescale of the Permian System consists of three series (i.e., Cisuralian, Guadalupian and Lopingian in ascending order) and nine stages. In China, the Permian System is composed of three series (Chuanshanian, Yansingian and Lopingian) and eight stages, of which the subdivisions and definitions of the Chuanshanian and Yangsingian series are very different from the Cisuralian and Guadalupian series. The Permian Period spanned approximate to 47 Myr. Its base is defined by the First Appearance Datum (FAD) of the conodont Streptognathodus isolatus at Aidaralash, Kazakhstan with an interpolated absolute age 298.9 +/- 0.15 Ma at Usolka, southern Urals, Russia. Its top equals the base of the Triassic System and is defined by the FAD of the conodont Hindeodus parvus at Meishan D section, southeast China with an interpolated absolute age 251.902 +/- 0.024 Ma. Thirty-five conodont, 23 fusulinid, 17 radiolarian and 20 ammonoid zones are established for the Permian in China, of which the Guadalupian and Lopingian conodont zones have been served as the standard for international correlation. The Permian C-13(carb) trend indicates that it is characterized by a rapid negative shift of 3-5 parts per thousand at the end of the Changhsingian, which can be used for global correlation of the end-Permian mass extinction interval, but C-13(carb) records from all other intervals may have more or less suffered subsequent diagenetic alteration or represented regional or local signatures only. Permian O-18{ainpatite} studies suggest that an icehouse stage dominated the time interval from the late Carboniferous to Kungurian (late Cisuralian). However, paleoclimate began to ameriolate during the late Kungurian and gradually shifted into a greenhouse-dominated stage during the Guadalupian. The Changhsingian was a relatively cool stage, followed by a globally-recognizable rapid temperature rise of 8-10 degrees C at the very end of the Changhsingian. The Sr-87/Sr-86 ratio trend shows that their values at the beginning of the Permian were between 0.70800, then gradually decreased to the late Capitanian minimum 0.70680-0.70690, followed by a persistent increase until the end of the Permian with the value 0.70708. Magenetostratigraphy suggests two distinct stages separated by the Illawarra Reversal in the middle Wordian, of which the lower is the reverse polarity Kiaman Superchron and the upper is the mixed-polarity Illawarra Superchron. The end-Guadalupian (or pre-Lopingian) biological crisis occurred during the late Capitanian, when faunal changeovers of different fossil groups had different paces, but generally experienced a relatively long time from the Jinogondolella altudensis Zone until the earliest Wuchiapingian. The end-Permian mass extinction was a catastrophic event that is best constrained at the Meishan section, which occurred at 251.941 +/- 0.037 Ma and persisted no more than 61 +/- 48 kyr. After the major pulse at Bed 25, the extinction patterns are displayed differently in different sections. The global end-Guadalupian regression is manifested between the conodont Jinogondolella xuanhanensis and Clarkina dukouensis zones and the end-Changhsingian transgression began in the Hindeodus changxingensis-Clarkina zhejiangensis Zone. The Permian Period is also characterized by strong faunal provincialism in general, which resulted in difficulties in inter-continental and inter-regional correlation of both marine and terrestrial systems.

KeywordPermian Timescale Global Correlation Biostratigraphy Chemostratigraphy
DOI10.1007/s11430-017-9228-4
Language英语
WOS KeywordLarge Igneous Province ; Selong Xishan Section ; Guadalupian-lopingian Boundary ; Carbon-isotope Stratigraphy ; Global Stratotype Section ; Double Mass Extinction ; Triassic Boundary ; South China ; Changhsingian Stage ; Baoshan Block
Funding ProjectStrategic Priority Research Program (B) from the Chinese Academy of Sciences[XDB18000000] ; Strategic Priority Research Program (B) from the Chinese Academy of Sciences[XDB26000000] ; Key Research Program of Frontier Sciences from the Chinese Academy of Sciences[QYZDY-SSW-DQC023] ; National Natural Science Foundation of China[41290260] ; National Natural Science Foundation of China[41420104003] ; National Natural Science Foundation of China[U1702242]
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000455070400008
Funding OrganizationStrategic Priority Research Program (B) from the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences from the Chinese Academy of Sciences ; National Natural Science Foundation of China
PublisherSCIENCE PRESS
Citation statistics
Cited Times:3[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.nigpas.ac.cn/handle/332004/16083
Collection中国科学院南京地质古生物研究所
其他
Corresponding AuthorShen, Shuzhong (沈树忠)
Affiliation1.Chinese Acad Sci, State Key Lab Palaeobiol & Stratig, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing 210008, Jiangsu, Peoples R China
3.Nanjing Univ, Ctr Res & Educ Biol Evolut & Environm, Nanjing 210023, Jiangsu, Peoples R China
4.China Univ Geosci, Sch Earth Sci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Hubei, Peoples R China
5.Chinese Acad Sci, CAS Key Lab Econ Stratig & Palaeogeog, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China
6.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
7.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Guangdong, Peoples R China
First Author AffilicationNanjing Institute of Geology and Palaeonotology,CAS
Corresponding Author AffilicationNanjing Institute of Geology and Palaeonotology,CAS
Recommended Citation
GB/T 7714
Shen, Shuzhong ,Zhang, Hua ,Zhang, Yichun ,et al. Permian integrative stratigraphy and timescale of China[J]. SCIENCE CHINA-EARTH SCIENCES,2019,62(1):154-188.
APA Shen, Shuzhong .,Zhang, Hua .,Zhang, Yichun .,Yuan, Dongxun .,Chen, Bo .,...&Wang, Xiangdong .(2019).Permian integrative stratigraphy and timescale of China.SCIENCE CHINA-EARTH SCIENCES,62(1),154-188.
MLA Shen, Shuzhong ,et al."Permian integrative stratigraphy and timescale of China".SCIENCE CHINA-EARTH SCIENCES 62.1(2019):154-188.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[Shen, Shuzhong (沈树忠)]'s Articles
[Zhang, Hua (张华)]'s Articles
[Zhang, Yichun (张以春)]'s Articles
Baidu academic
Similar articles in Baidu academic
[Shen, Shuzhong (沈树忠)]'s Articles
[Zhang, Hua (张华)]'s Articles
[Zhang, Yichun (张以春)]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Shen, Shuzhong (沈树忠)]'s Articles
[Zhang, Hua (张华)]'s Articles
[Zhang, Yichun (张以春)]'s Articles
Terms of Use
No data!
Social Bookmark/Share
Add to CiteULike Add to Connotea Add to Del.icio.us Add to Digg Add to Reddit Add to Technorati
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.