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  2. 地质与地球物理研究所
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  4. 岩石圈演化国家重点实验室
Quaternary integrative stratigraphy and timescale of China

文献类型：期刊论文

作者Deng, Chenglong1,2,3; Hao, Qingzhen2,3,4; Guo, Zhengtang2,3,4,5; Zhu, Rixiang1,2,3
刊名SCIENCE CHINA-EARTH SCIENCES
出版日期2019
卷号62期号:1页码:324-348
关键词Quaternary Chronostratigraphy Magnetic stratigraphy Biostratigraphy Climatostratigraphy China
ISSN号1674-7313
DOI10.1007/s11430-017-9195-4
英文摘要Quaternary strata in China mainly comprise continental deposits in a variety of depositional settings. The continental Quaternary in temperate northern China consists mainly of eolian and fluvio-lacustrine deposits; that in subtropical southern China, mainly of vermiculated red soils, cave/fissure deposits, and fluvio-lacustrine deposits; and that in the alpine Tibetan Plateau, mainly of fluvio-lacustrine and piedmont deposits. The marine Quaternary in China consists of detrital deposits and biogenic reef deposits. The integration of biostratigraphy, magnetostratigraphy, climatostratigraphy and an astronomically calibrated chronology has led to the establishment of high-precision climatochronostratigraphic timescales for the detrital marine Quaternary in the South China Sea and the loess-paleosol sequence in the Chinese Loess Plateau. Extremely high-precision Th-230 dating has provided a high-precision absolute age model for cave stalagmites over the past 640000 years as well as high-resolution oxygen isotope records representing orbital- to suborbital-scale climate changes. By combining magnetic stratigraphy and biostratigraphy, robust chronostratigraphic frameworks for non-eolian continental Quaternary deposits on the scale of Quaternary geomagnetic polarities have been established. The continental Pleistocene Series consists, from oldest to youngest, of the Nihewanian Stage of the Lower Pleistocene, the Zhoukoudianian Stage of the Middle Pleistocene, and the Salawusuan Stage of the Upper Pleistocene. Stages of the continental Holocene Series have not yet been established. This review summarizes recent developments in the Quaternary chronostratigraphy of representative Quaternary strata and associated faunas, and then proposes an integrative chronostratigraphic framework and a stratigraphic correlation scheme for Quaternary continental strata in China. In the near-future, it is hoped to establish not only a Chinese continental Quaternary climatochronostratigraphic chart on the scale of glacial-interglacial cycles but also a Quaternary integrative chronostratigraphic chart including both continental and marine strata in China.
WOS关键词PLEISTOCENE GIGANTOPITHECUS FAUNAS ; LOESS-SOIL SEQUENCES ; NIHEWAN BASIN ; TIBETAN PLATEAU ; MAMMALIAN FAUNA ; HOMO-ERECTUS ; YELLOW SEA ; CHRONOLOGICAL SEQUENCE ; ASTRONOMICAL TIMESCALE ; SOUTHERN CHINA
资助项目National Natural Science Foundation of China[41690110] ; National Natural Science Foundation of China[41621004] ; National Natural Science Foundation of China[L152401]
WOS研究方向Geology
语种英语
WOS记录号WOS:000455070400014
出版者SCIENCE PRESS
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/90224]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Deng, Chenglong
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
5.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714		 Deng, Chenglong,Hao, Qingzhen,Guo, Zhengtang,et al. Quaternary integrative stratigraphy and timescale of China[J]. SCIENCE CHINA-EARTH SCIENCES,2019,62(1):324-348.
APA Deng, Chenglong,Hao, Qingzhen,Guo, Zhengtang,&Zhu, Rixiang.(2019).Quaternary integrative stratigraphy and timescale of China.SCIENCE CHINA-EARTH SCIENCES,62(1),324-348.
MLA Deng, Chenglong,et al."Quaternary integrative stratigraphy and timescale of China".SCIENCE CHINA-EARTH SCIENCES 62.1(2019):324-348.

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来源：地质与地球物理研究所

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