中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A Great late Ediacaran ice age

文献类型:期刊论文

作者Wang, Ruimin1,2; Shen, Bing1,2; Lang, Xianguo3,4; Wen, Bin5; Mitchell, Ross N.6,7; Ma, Haoran8; Yin, Zongjun9,10; Peng, Yongbo8; Liu, Yonggang11; Zhou, Chuanming9,10
刊名NATIONAL SCIENCE REVIEW
出版日期2023-04-25
页码14
ISSN号2095-5138
关键词carbonate carbon isotopes Shuram excursion inertial interchange true polar wander (IITPW) hankalchough glaciation Tarim Block
DOI10.1093/nsr/nwad117
通讯作者Shen, Bing(bingshen@pku.edu.cn) ; Lang, Xianguo(langxianguo19@cdut.edu.cn) ; Wen, Bin(wenbin@cug.edu.cn)
英文摘要A Great Ediacaran Glaciation (GEG) lasting at least 20 million years from continent to continent in mid-to-high latitudes witnessed the evolution of the Ediacara biota. The emergence of the Ediacara biota soon after the Gaskiers glaciation ca. 580 million years ago (Ma) implies a possible glacial fuse for the evolution of animals. However, the timing of Ediacaran glaciation remains controversial because of poor age constraints on the similar to 30 Ediacaran glacial deposits known worldwide. In addition, paleomagnetic constraints and a lack of convincing Snowball-like cap carbonates indicate that Ediacaran glaciations likely did not occur at low latitudes. Thus, reconciling the global occurrences without global glaciation remains a paradox. Here, we report that the large amplitude, globally synchronous ca. 571-562 Ma Shuram carbon isotope excursion occurs below the Ediacaran Hankalchough glacial deposit in Tarim, confirming a post-Shuram glaciation. Leveraging paleomagnetic evidence for a similar to 90 degrees reorientation of all continents due to true polar wander, and a non-Snowball condition that rules out low-latitude glaciations, we use paleogeographic reconstructions to further constrain glacial ages. Our results depict a 'Great Ediacaran Glaciation' occurring diachronously but continuously from ca. 580-560 Ma as different continents migrated through polar-temperate latitudes. The succession of radiation, turnover and extinction of the Ediacara biota strongly reflects glacial-deglacial dynamics.
WOS关键词TRUE POLAR WANDER ; CARBON-ISOTOPE EXCURSION ; YANGTZE PLATFORM ; SOUTH CHINA ; CAMBRIAN EXPLOSION ; GEOMAGNETIC-FIELD ; CAP CARBONATES ; SEPT-ILES ; GLACIATION ; SNOWBALL
WOS研究方向Science & Technology - Other Topics
语种英语
出版者OXFORD UNIV PRESS
WOS记录号WOS:000993522700001
源URL[http://ir.nigpas.ac.cn/handle/332004/42156]  
专题中国科学院南京地质古生物研究所
通讯作者Shen, Bing; Lang, Xianguo; Wen, Bin
作者单位1.Peking Univ, Key Lab Orogen Belts & Crustal Evolut, Minist Educ, Beijing 100871, Peoples R China
2.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
3.Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610059, Peoples R China
4.Chengdu Univ Technol, Inst Sedimentary Geol, Chengdu 610059, Peoples R China
5.China Univ Geosci, Sch Earth Sci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
7.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
8.Nanjing Univ, Sch Earth Sci & Engn, Nanjing 210023, Peoples R China
9.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
10.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing 210008, Peoples R China
推荐引用方式
GB/T 7714
Wang, Ruimin,Shen, Bing,Lang, Xianguo,et al. A Great late Ediacaran ice age[J]. NATIONAL SCIENCE REVIEW,2023:14.
APA Wang, Ruimin.,Shen, Bing.,Lang, Xianguo.,Wen, Bin.,Mitchell, Ross N..,...&Zhou, Chuanming.(2023).A Great late Ediacaran ice age.NATIONAL SCIENCE REVIEW,14.
MLA Wang, Ruimin,et al."A Great late Ediacaran ice age".NATIONAL SCIENCE REVIEW (2023):14.

入库方式: OAI收割

来源:南京地质古生物研究所

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