中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Climatic or tectonic control on organic matter deposition in the South China Sea? A lesson learned from a comprehensive Neogene palynological study of IODP Site U1433

文献类型:期刊论文

作者Miao, Yunfa1,2; Warny, Sophie1,3; Clift, Peter D.1; Gregory, Mitch1,3; Liu, Chang1
刊名INTERNATIONAL JOURNAL OF COAL GEOLOGY
出版日期2018-04-01
卷号190页码:166-177
关键词Organic matters Tectonics Monsoon Driving forces Neogene
ISSN号0166-5162
DOI10.1016/j.coal.2017.10.003
通讯作者Miao, Yunfa(yunfine2000@sina.com) ; Warny, Sophie(swarny@lsu.edu)
英文摘要Palynomorphs and other organic particles are basic key components of palynofacies, yet quantitative analyses of all types are rarely used together to investigate organic matter assemblage changes and evaluate the driving forces behind the observed changes. In this paper, eight organic-walled microfossil and particle morphologies (sporopollen, Pediastrum, Concentricystes, fungi, dinoflagellate cysts, structured/amorphous organic matters, stomatal apparatus and scolecodonts) are tabulated and their concentrations and fluxes are evaluated over the past 17 million years (Ma) in sediments recovered from the South China Sea at International Ocean Discovery Program (IODP) Site U1433. Overall, these morphologies show roughly similar increasing trends but with different levels of fluctuations. The uniform increase in all morphologies at 8 Ma (named the 8 Ma event) is the most notable feature of the past 17 Ma. To explain the trend, and because these various organic matters reflect various environmental conditions, we argue that the uniformity of the signal implies that tectonically-driven basin and drainage evolution played the key role, rather than paleoclimate (Asian summer monsoon). The similar to 8 Ma event was likely triggered by the onset of the Mekong River in its present location, although the role of monsoon evolution cannot be excluded completely.
收录类别SCI ; ISTP
WOS关键词ASIAN SUMMER MONSOON ; WESTERN QAIDAM BASIN ; TIBETAN PLATEAU ; MIDDLE MIOCENE ; EXPEDITION 349 ; POLLEN RECORD ; 20 MA ; EVOLUTION ; OLIGOCENE ; PALYNOFACIES
WOS研究方向Energy & Fuels ; Geology
WOS类目Energy & Fuels ; Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000431159700011
出版者ELSEVIER SCIENCE BV
URI标识http://www.irgrid.ac.cn/handle/1471x/2557845
专题寒区旱区环境与工程研究所
通讯作者Miao, Yunfa; Warny, Sophie
作者单位1.Louisiana State Univ, Dept Geol & Geophys, E-235 Howe Russell, Baton Rouge, LA 70803 USA
2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Inst, Key Lab Desert & Desertificat, Lanzhou 730000, Gansu, Peoples R China
3.Louisiana State Univ, Museum Nat Sci, 109 Foster Hall, Baton Rouge, LA 70803 USA
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Miao, Yunfa,Warny, Sophie,Clift, Peter D.,et al. Climatic or tectonic control on organic matter deposition in the South China Sea? A lesson learned from a comprehensive Neogene palynological study of IODP Site U1433[J]. INTERNATIONAL JOURNAL OF COAL GEOLOGY,2018,190:166-177.
APA Miao, Yunfa,Warny, Sophie,Clift, Peter D.,Gregory, Mitch,&Liu, Chang.(2018).Climatic or tectonic control on organic matter deposition in the South China Sea? A lesson learned from a comprehensive Neogene palynological study of IODP Site U1433.INTERNATIONAL JOURNAL OF COAL GEOLOGY,190,166-177.
MLA Miao, Yunfa,et al."Climatic or tectonic control on organic matter deposition in the South China Sea? A lesson learned from a comprehensive Neogene palynological study of IODP Site U1433".INTERNATIONAL JOURNAL OF COAL GEOLOGY 190(2018):166-177.

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