A strongly positive sulphur isotopic shift in late Ediacaran-early Cambrian seawater: evidence from evaporites in the Salt Range Formation, northern Pakistan | |
Meng, Fanwei(孟凡巍)3; Zhang, Zhili4; Bukowski, Krzysztof5; Zhuo, Qingong6; Ahsan, Naveed2; Ur-Rehman, Saif2; Ni, Pei1 | |
刊名 | GEOLOGICAL QUARTERLY |
2021 | |
卷号 | 65期号:2页码:13 |
关键词 | sulphur isotope gypsum Salt Range Formation Indo-Pakistan Plate South China Yangtze Block |
ISSN号 | 1641-7291 |
DOI | 10.7306/gq.1598 |
英文摘要 | The Salt Range Formation in northern Pakistan is globally well-known for its extremely large evaporite deposits dated to the upper Ediacaran-lower Cambrian. This huge evaporite belt formed an area covering present-day parts of India, Pakistan, Iran, Oman, and even South China (similar to 200,000 km(2) in South China). Sulphate minerals, including anhydrite and gypsum, can continuously record seawater sulphur isotopic composition. Until now, there was only one dataset reporting the isotopic composition of evaporites in Pakistan. This study reports new data, which points to a strongly positive sulphur isotopic shift (>+30 parts per thousand, VCDT values) in the Salt Range Formation in Pakistan. Based on the stratigraphic position, similarity in lithology, age, and sulphur isotope data of the evaporitic sequences, it can be inferred that the Neoproterozoic Indo-Pakistan Plate and the Yangtze Platform were closely related palaeogeographically during the terminal Neoproterozoic. This interpretation can improve understanding of the palaeogeographical evolution of the area during the Neoproterozoic, with particular reference to the origin of biogeochemical cycles and the diagenetic evolution of the evaporitic deposits. |
资助项目 | National Natural Science Foundation of China[41672142] ; National Natural Science Foundation of China[41561144009] ; Basic Frontier Scientific Research Program of the Chinese Academy of Sciences[ZDBS-LY-DQC021] ; AGH University of Science and Technology[16.16.140.315] ; Bureau of International Co-operation, Chinese Academy of Sciences |
WOS关键词 | NAGAUR-GANGANAGAR BASIN ; FLUID INCLUSIONS ; SALINITY HISTORY ; BADENIAN SALT ; BOUND SULFATE ; WESTERN INDIA ; CHEMISTRY ; EVOLUTION ; HALITE ; CONSTRAINTS |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | POLISH GEOLOGICAL INST |
WOS记录号 | WOS:000672475200011 |
资助机构 | National Natural Science Foundation of China ; Basic Frontier Scientific Research Program of the Chinese Academy of Sciences ; AGH University of Science and Technology ; Bureau of International Co-operation, Chinese Academy of Sciences |
内容类型 | 期刊论文 |
源URL | [http://ir.nigpas.ac.cn/handle/332004/38393] |
专题 | 中国科学院南京地质古生物研究所 |
通讯作者 | Bukowski, Krzysztof |
作者单位 | 1.Nanjing Univ, Sch Earth Sci & Engn, Inst Geofluids, State Key Lab Mineral Deposit Res, Nanjing 210093, Peoples R China 2.Univ Punjab, Inst Geol, Quaid E Azam Campus, Lahore 54590, Pakistan 3.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China 4.SINOPEC, Petr Explorat & Dev Res Inst, Beijing 100083, Peoples R China 5.AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Al A Mickiewicza 30, PL-30059 Krakow, Poland 6.CNPC, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China |
推荐引用方式 GB/T 7714 | Meng, Fanwei,Zhang, Zhili,Bukowski, Krzysztof,et al. A strongly positive sulphur isotopic shift in late Ediacaran-early Cambrian seawater: evidence from evaporites in the Salt Range Formation, northern Pakistan[J]. GEOLOGICAL QUARTERLY,2021,65(2):13. |
APA | Meng, Fanwei.,Zhang, Zhili.,Bukowski, Krzysztof.,Zhuo, Qingong.,Ahsan, Naveed.,...&Ni, Pei.(2021).A strongly positive sulphur isotopic shift in late Ediacaran-early Cambrian seawater: evidence from evaporites in the Salt Range Formation, northern Pakistan.GEOLOGICAL QUARTERLY,65(2),13. |
MLA | Meng, Fanwei,et al."A strongly positive sulphur isotopic shift in late Ediacaran-early Cambrian seawater: evidence from evaporites in the Salt Range Formation, northern Pakistan".GEOLOGICAL QUARTERLY 65.2(2021):13. |
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