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DOI | 10.1007/s00531-020-01817-9 |
Microfacies and multi-isotope records of Anisian sequences from the Upper Yangtze Block: possible responses to tectonics and climate-driven relative sea-level change | |
Zhong, Yisi; Wang, Licheng; Xu, Yuan; Zhang, Yongming; Liu, Chenglin | |
通讯作者 | Wang, LC (通讯作者) |
发表日期 | 2020 |
ISSN | 1437-3254 |
EISSN | 1437-3262 |
起始页码 | 489 |
结束页码 | 509 |
卷号 | 109期号:2 |
英文摘要 | The Middle Triassic epoch is the key to understanding the environment changes after the Permian-Triassic mass extinction. The Anisian Badong Formation is a carbonate and siliciclastic succession deposited on the Yangtze Platform, Upper Yangtze Block. In this paper, we use facies analysis combined with sequence stratigraphy of the Badong Formation in the Nashuixi section, Yangtze Block, to discuss the Anisian relative sea-level changes. Microfacies analyses were used to define ten microfacies in four depositional facies zones (tidal flat, restricted platform, restricted to open platform, and open platform) indicating an epeiric platform depositional environment. The lowstand, transgressive, and highstand systems tracts and two sequences were identified. Sequence stratigraphy interpretations indicate that relative sea-level at Nashuixi experienced two rises in the Middle Anisian, which is correlated with those in the Yangtze Block, confirming that sea-level changes during the Anisian were of eustatic origin. However, a distinct regression at Nashuixi occurred in the late Bithynian to IIIyrian while the global sea-level rose, which is likely to be caused by interference from regional tectonics during IIIyrian. The carbon and oxygen isotopic shifts in the Nashuixi section exhibit two negative-values stage in the time near end of Aegean and early Pelsonian, which is well correlated with the global typical sections, indicating two middle Anisian warming events. Our study indicated that the relative sea-level at Nashuixi was controlled by global sea-level change and regional tectonics (Indosinian Orogeny), and the C and O isotopes records respond to global climate change. |
关键词 | SR-ISOTOPEPLATFORM CARBONATESCONODONT ZONATIONSTABLE-ISOTOPEMIDDLEOXYGENSTRATIGRAPHYSTRONTIUMBOUNDARYSEAWATER |
英文关键词 | Badong formation; Anisian; Yangtze platform; Sea-level change; Microfacies; Carbon and oxygen isotopes |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000519409900005 |
来源期刊 | INTERNATIONAL JOURNAL OF EARTH SCIENCES
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/259908 |
推荐引用方式 GB/T 7714 | Zhong, Yisi,Wang, Licheng,Xu, Yuan,et al. Microfacies and multi-isotope records of Anisian sequences from the Upper Yangtze Block: possible responses to tectonics and climate-driven relative sea-level change[J]. 中国科学院青藏高原研究所,2020,109(2). |
APA | Zhong, Yisi,Wang, Licheng,Xu, Yuan,Zhang, Yongming,&Liu, Chenglin.(2020).Microfacies and multi-isotope records of Anisian sequences from the Upper Yangtze Block: possible responses to tectonics and climate-driven relative sea-level change.INTERNATIONAL JOURNAL OF EARTH SCIENCES,109(2). |
MLA | Zhong, Yisi,et al."Microfacies and multi-isotope records of Anisian sequences from the Upper Yangtze Block: possible responses to tectonics and climate-driven relative sea-level change".INTERNATIONAL JOURNAL OF EARTH SCIENCES 109.2(2020). |
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