The End-Devonian Hangenberg Event and its aftermath in South China: Stratigraphic and sedimentary records from shallow to deep water facies
文献类型：期刊论文
| 作者 | Hou, Hongfei7; Ma, Xueping6; Zhou, Huailing5; Ogg, James G.3,4; Shen, Yang1,2 |
| 刊名 | EARTH-SCIENCE REVIEWS
 |
| 出版日期 | 2022-09-01 |
| 卷号 | 232页码:20 |
| 关键词 | Devonian Sea -level Volcanism Microbialites Paleotethys |
| ISSN号 | 0012-8252 |
| DOI | 10.1016/j.earscirev.2022.104137 |
| 通讯作者 | Hou, Hongfei(hou_hongfei@126.com) ; Shen, Yang(shenybj@126.com) |
| 英文摘要 | The global End-Devonian Hangenberg Event was one of the most important mass extinction events during the Phanerozoic eon. The stratigraphical, paleontological, and sedimentological evolution of strata equivalent to the Hangenberg Event have been widely investigated in three depositional environments of shallow-marine plat-form, of margin and upper slope, and of deep-water facies along the South China Platform. In this representative region within the eastern Paleotethys, the volcanic tuffs, storm deposits, and microbialites deposited during the time of the Hangenberg Event differ from the record of the Hangenberg Crisis in the Rhenish Slate Mountains of Germany, which is a standard for the western Paleotethys. The Upper Crisis Interval (so-called Stockum Lime-stone Event) in the Rhenish record is interpreted as correlative to the aftermath of the Hangenberg Event in South China rather than a crisis record per se. The unique Cap Microbialite of peloids and oncoids in South China is linked to onset of a new shallow-marine ecosystem characterized by microbe resurgence during a delayed biotic recovery. This microbialite resurgence in association with low-diversity metazoan ecosystems may be a common feature of post-extinction episodes. The new synthesis of records from South China provide insights into global changes that contributed to the Hangenberg biotic extinctions. |
| WOS关键词 | CARBONIFEROUS BOUNDARY ; SEQUENCE STRATIGRAPHY ; MASS EXTINCTION ; MICROBIAL CARBONATES ; NORTHERN FRANCE ; SEA-LEVEL ; BELGIUM ; FLUCTUATIONS ; CONODONT ; PROVINCE |
| 资助项目 | National Natural Science Foundation of China[42172037] ; National Natural Science Foundation of China[41702023] ; National Natural Science Foundation of China[41872003] ; China Geological Survey[DD20190009] ; China Geological Survey[DD20190601] ; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Insti- tute of Geology and Palaeontology, CAS)[173122] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000847360600001 |
| 出版者 | ELSEVIER |
| 资助机构 | National Natural Science Foundation of China ; China Geological Survey ; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Insti- tute of Geology and Palaeontology, CAS) |
| 源URL | [http://ir.nigpas.ac.cn/handle/332004/41195]  |
| 专题 | 中国科学院南京地质古生物研究所 |
| 通讯作者 | Hou, Hongfei; Shen, Yang |
| 作者单位 | 1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, 39 East Beijing Rd, Nanjing 210008, Peoples R China 2.China Univ Geosci Beijing, Museum, 29 Xueyuan Rd, Beijing 100083, Peoples R China 3.Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA 4.Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610059, Peoples R China 5.Guangxi Geol Survey, Nanning 530012, Peoples R China 6.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China 7.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China |
| 推荐引用方式 GB/T 7714 | Hou, Hongfei,Ma, Xueping,Zhou, Huailing,et al. The End-Devonian Hangenberg Event and its aftermath in South China: Stratigraphic and sedimentary records from shallow to deep water facies[J]. EARTH-SCIENCE REVIEWS,2022,232:20. |
| APA | Hou, Hongfei,Ma, Xueping,Zhou, Huailing,Ogg, James G.,&Shen, Yang.(2022).The End-Devonian Hangenberg Event and its aftermath in South China: Stratigraphic and sedimentary records from shallow to deep water facies.EARTH-SCIENCE REVIEWS,232,20. |
| MLA | Hou, Hongfei,et al."The End-Devonian Hangenberg Event and its aftermath in South China: Stratigraphic and sedimentary records from shallow to deep water facies".EARTH-SCIENCE REVIEWS 232(2022):20. |
入库方式： OAI收割
来源：南京地质古生物研究所
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