Carbon and oxygen isotopic characteristics of the Ediacaran Doushantuo;Formation in Fanjingshan area, northeastern Guizhou Province, China | |
Xiong, Guoqing4; Duan, Taizhong1; Wu, Hao; Zhang, Haiquan; Yu, Qian; Yan, Jianfei; Jiang, Xinsheng; Cui, Xiaozhuang2; Wang, Jian; Wang, Zhengjiang | |
刊名 | CARBONATES AND EVAPORITES
![]() |
2013 | |
卷号 | 28期号:4页码:399-412 |
关键词 | Carbon and oxygen isotope Ediacaran Fanjingshan area Chemostratigraphic correlation Carbon negative excursion |
ISSN号 | 0891-2556;EI 1878-5212 |
DOI | 10.1007/s13146-013-0135-8 |
英文摘要 | New data of carbon and oxygen isotopes of the Ediacaran Doushantuo Formation from two measured sections in Fanjingshan area, northeastern Guizhou Province are presented in this paper. Carbon isotopes from Tongluo section and Nongjing section intervene between -3.2 and -5.4 aEuro degrees, an average value -4.3 aEuro degrees and between -3.6 and +0.5 aEuro degrees, an average value -1.5 aEuro degrees, respectively; oxygen isotopes range from -7.0 to -11.0 aEuro degrees, an average value -9.3 aEuro degrees; and from -10.2 to -2.9 aEuro degrees, an average value -7.6 aEuro degrees, individually. Carbon and oxygen isotopes both display a negative-excursion trend. Carbon isotopes reduce dramatically in the middle of these sections. Average carbon isotope is the most negative from Yongyi section, moderate negative from Tongluo section and less negative from Nongjing section, which is characteristic of a large surface-to-deep ocean delta C-13 gradient/carbon isotopic stratification during Doushantuo period. The spatio-temporal variations of carbon isotope perhaps should be related to sedimentary facies and the relief of palaeo-ocean floor. Moreover, carbon isotope profiles from three sections in Fanjingshan area, northeastern Guizhou Province could compare to South China elsewhere and make interbasin high-resolution chemostratigraphic correlation possible in South China. The such large-scale carbon negative excursion worldwide must be the interactional result of multi-factors such as overturn of a redox-stratified ocean, extreme chemical weathering, massive oxidation of destabilized methane hydrates, and sudden formation and gradual dissipation of a global meltwater plume caused by sea-level rise during deglaciation. |
学科主题 | 前寒武纪地质 |
WOS关键词 | NEOPROTEROZOIC CAP CARBONATES ; UPPER PROTEROZOIC SUCCESSIONS ; SOUTH ; CHINA ; YANGTZE PLATFORM ; SNOWBALL EARTH ; MARINOAN GLACIATION ; METHANE ; SEEPS ; DEATH-VALLEY ; CHEMOSTRATIGRAPHIC CORRELATION ; PALEOCEANOGRAPHIC ; CHANGES |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SPRINGER |
WOS记录号 | WOS:000327495800002 |
内容类型 | 期刊论文 |
源URL | [http://119.78.100.197/handle/2HKVOGP0/39992] ![]() |
专题 | 中国地质调查局成都地质调查中心 |
作者单位 | 1.Chengdu Inst Geol & Mineral Resources, Chengdu 610082, Peoples R China. 2.Marathon Oil UK Ltd, Aberdeen AB15 6FZ, Scotland. 3.Chinese Acad Geol Sci, Beijing 100037, Peoples R China. 4.中国地质调查局成都地质调查中心 |
推荐引用方式 GB/T 7714 | Xiong, Guoqing,Duan, Taizhong,Wu, Hao,et al. Carbon and oxygen isotopic characteristics of the Ediacaran Doushantuo;Formation in Fanjingshan area, northeastern Guizhou Province, China[J]. CARBONATES AND EVAPORITES,2013,28(4):399-412. |
APA | Xiong, Guoqing.,Duan, Taizhong.,Wu, Hao.,Zhang, Haiquan.,Yu, Qian.,...&Wang, Zhengjiang.(2013).Carbon and oxygen isotopic characteristics of the Ediacaran Doushantuo;Formation in Fanjingshan area, northeastern Guizhou Province, China.CARBONATES AND EVAPORITES,28(4),399-412. |
MLA | Xiong, Guoqing,et al."Carbon and oxygen isotopic characteristics of the Ediacaran Doushantuo;Formation in Fanjingshan area, northeastern Guizhou Province, China".CARBONATES AND EVAPORITES 28.4(2013):399-412. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论