The Zitai Formation in South China: unique deeper-water marine red beds in terms of lithology, distribution and delta C-13(carb) chemostratigraphy | |
Luan, Xiao-Cong (栾晓聪)1; Wu, Rong-Chang (吴荣昌)1; Zhan, Ren-Bin (詹仁斌)1,2; Liu, Jian-Bo3 | |
刊名 | PALAEOWORLD |
2019-03-01 | |
卷号 | 28期号:1-2页码:198-210 |
关键词 | Marine Red Beds Zitai Formation Ordovician South China Gobe |
ISSN号 | 1871-174X |
DOI | 10.1016/j.palwor.2018.12.007 |
英文摘要 | During the EarlyoMiddle Ordovician characteristic red carbonate beds, i.e., the Zitai Formation and its coeval units, developed in the deeper water marine setting of the Yangtze Platform, South China. The temporal and spatial distribution of these reddish limestones is discussed based on published data and our own observations and analyses. The red limestones formed along the margin of the Yangtze Platform on a carbonate ramp during six stages. The different stages, (0) early F13 and before, (1) middle to late F13, (2) early Dp1, (3) middle to late Dp1, (4) Dp2, and (5) Dp3 to early Dw1, are associated with regional sea-level changes and tectonic movements. Several positive shifts in the delta C-13(carb) record occur in the succession beneath the red beds. Their formation presumably was induced by a global transgression in association with the drowning of the Yangtze Platform. Better ventilation and oxygenation of sediments on the platform are also indicated by the marine red beds and together intensified the Great Ordovician Biodiversification Event. Other factors such as iron presumably play a significant role in controlling occurrences and distribution of the red limestone beds. (C) 2019 Elsevier Ireland Ltd Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. Published by Elsevier B.V. All rights reserved. |
资助项目 | National Natural Science Foundation of China (NSFC)[41672008] ; National Natural Science Foundation of China (NSFC)[41521061] ; National Natural Science Foundation of China (NSFC)[41472006] ; Chinese Academy of Sciences (CAS)[XDB26000000] ; IGCP Project[653] |
WOS关键词 | Middle Ordovician ; Yangtze Platform ; Black Shales ; Time ; Biodiversification ; Sedimentary ; Radiation ; Examples ; Patterns ; Section |
WOS研究方向 | Paleontology |
语种 | 英语 |
出版者 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:000463600800017 |
资助机构 | National Natural Science Foundation of China (NSFC) ; Chinese Academy of Sciences (CAS) ; IGCP Project |
内容类型 | 期刊论文 |
源URL | [http://ir.nigpas.ac.cn/handle/332004/15806] |
专题 | 中国科学院南京地质古生物研究所 南京地质古生物研究所_其他 |
通讯作者 | Luan, Xiao-Cong (栾晓聪) |
作者单位 | 1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Ctr Excellence Life & Paleoenvironm, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Jiangsu, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China 3.Peking Univ, Sch Earth & Space Sci, Paleontol & Stratig, Beijing 100871, Peoples R China |
推荐引用方式 GB/T 7714 | Luan, Xiao-Cong ,Wu, Rong-Chang ,Zhan, Ren-Bin ,et al. The Zitai Formation in South China: unique deeper-water marine red beds in terms of lithology, distribution and delta C-13(carb) chemostratigraphy[J]. PALAEOWORLD,2019,28(1-2):198-210. |
APA | Luan, Xiao-Cong ,Wu, Rong-Chang ,Zhan, Ren-Bin ,&Liu, Jian-Bo.(2019).The Zitai Formation in South China: unique deeper-water marine red beds in terms of lithology, distribution and delta C-13(carb) chemostratigraphy.PALAEOWORLD,28(1-2),198-210. |
MLA | Luan, Xiao-Cong ,et al."The Zitai Formation in South China: unique deeper-water marine red beds in terms of lithology, distribution and delta C-13(carb) chemostratigraphy".PALAEOWORLD 28.1-2(2019):198-210. |
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