KMS Nanjing Institute of Geology and Palaeonotology,CAS
Integrated study of the Doushantuo Formation in northwestern Hunan Province: Implications for Ediacaran chemostratigraphy and biostratigraphy in South China | |
Shi, Hongyi(史弘毅)1,2,3; Ouyang, Qing(欧阳晴)1,2,4![]() ![]() ![]() ![]() | |
2022-08-01 | |
发表期刊 | PRECAMBRIAN RESEARCH
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ISSN | 0301-9268 |
卷号 | 377页码:22 |
摘要 | The Ediacaran Doushantuo Formation in South China documents profound biological and environmental changes after the Neoproterozoic global glaciations. However, since the geological records of these changes are scattered in various lithofacies, the establishment of the co-evolutionary pattern of life and environment largely relies on regional stratigraphic correlation. A negative delta C-13 excursion in the upper Doushantuo Formation in the shelf-margin facies has been correlated with different delta C-1(3) chemostratigraphic features in the Doushantuo Formation in the shelf-lagoon facies: either with EN3 (widely regarded as equivalent to the Shuram excursion in Oman) or with EN2, which occur respectively in the upper and middle Doushantuo Formation in the Yangtze Gorges area of South China. Here we report new litho-, chemo-, and biostratigraphic data of the Douoshantuo Formation at the Caojunba section in shelf-margin facies, where the lithostratigraphic sequence and carbon isotopic profile resemble those at other shelf-margin sections, e.g., the Yangjiaping and Zhongling sections. Diverse microfossils including nine genera and eighteen species of acanthomorphic acritarchs are found from the upper Doushantuo Formation at Caojunba, which represent to date the first report of the upper Doushantuo acritarch assemblage from the shelf-margin facies in South China. The newly recovered microfossil assemblage includes Hocosphaeridium anozos, H. scaberfacium, Tanarium conoideum, and clustered leiospheres, and these taxa support the stratigraphic correlation of upper Doushantuo Formation between shelf-margin and shelf-lagoon facies. This correlation indicates that the interval with negative delta(13) C values in the upper Doushantuo Formation of shelf-margin facies is likely equivalent to EN3. This correlation also suggests that the delta C-13 profiles of the EN3/Shuram excursion interval in different facies in South China have various expressions (e.g., stratigraphic range, magnitude), making its regional and continental correlations more challenging. On the other hand, the discovery of acritarch assemblage characteristic of the upper Doushantuo Formation in the Yangtze Gorges area from shelf-margin facies confirms their potential as an independent stratigraphic tool in the subdivision and correlation of Ediacaran strata. |
关键词 | Ediacaran Period Yangtze Block Acanthomorphic acritarch Carbon isotopic profile Shuram excursion Facies change |
DOI | 10.1016/j.precamres.2022.106699 |
收录类别 | SCI |
语种 | 英语 |
关键词[WOS] | YANGTZE GORGES AREA ; UPPER SLOPE SECTION ; ACANTHOMORPHIC ACRITARCHS ; SHURAM EXCURSION ; CARBON ; MICROFOSSILS ; PLATFORM ; EVOLUTION ; OXIDATION ; MARGIN |
资助项目 | Strategic Priority Research Program (B) of Chinese Academy of Sciences[XDB26000000] ; National Natural Science Foundation of China[41902006] ; National Natural Science Foundation of China[41921002] ; National Natural Science Foundation of China[41972005] ; National Key R & D Program of China[2017YFC0603101] ; State Key Laboratory of Biogeology and Environmental Geology[GBL22106] ; National Science Foundation[EAR-2021207] |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000832717900001 |
项目资助者 | Strategic Priority Research Program (B) of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Key R & D Program of China ; State Key Laboratory of Biogeology and Environmental Geology ; National Science Foundation |
出版者 | ELSEVIER |
文献类型 | 期刊论文 |
条目标识符 | http://ir.nigpas.ac.cn/handle/332004/41100 |
专题 | 中国科学院南京地质古生物研究所 |
通讯作者 | Ouyang, Qing(欧阳晴) |
作者单位 | 1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China 2.Chinese Acad Sci, Ctr Excellence Life & Palaeoenvironm, Nanjing 210008, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.China Univ Geosci Wuhan, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China 5.Virginia Tech, Dept Geosci, Blacksburg, VA 24061 USA |
第一作者单位 | 中国科学院南京地质古生物研究所 |
通讯作者单位 | 中国科学院南京地质古生物研究所 |
推荐引用方式 GB/T 7714 | Shi, Hongyi,Ouyang, Qing,Zhou, Chuanming,et al. Integrated study of the Doushantuo Formation in northwestern Hunan Province: Implications for Ediacaran chemostratigraphy and biostratigraphy in South China[J]. PRECAMBRIAN RESEARCH,2022,377:22. |
APA | Shi, Hongyi,Ouyang, Qing,Zhou, Chuanming,Xiao, Shuhai,Chen, Zhe,&Guan, Chengguo.(2022).Integrated study of the Doushantuo Formation in northwestern Hunan Province: Implications for Ediacaran chemostratigraphy and biostratigraphy in South China.PRECAMBRIAN RESEARCH,377,22. |
MLA | Shi, Hongyi,et al."Integrated study of the Doushantuo Formation in northwestern Hunan Province: Implications for Ediacaran chemostratigraphy and biostratigraphy in South China".PRECAMBRIAN RESEARCH 377(2022):22. |
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