Late onset of the Holocene rainfall maximum in northeastern China inferred from a pollen record from the sediments of Tianchi Crater Lake

doi:10.1017/qua.2018.137

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 中国科学院新生代地质与环境重点实验室

	Late onset of the Holocene rainfall maximum in northeastern China inferred from a pollen record from the sediments of Tianchi Crater Lake
	Liu, Xiaoyan 1; Zhan, Tao 2; Zhou, Xinying 3; Wu, Haibin 4; Li, Qin 4; Zhao, Chao 3; Qiao, Yansong 5; Jiang, Shiwei 1; Tu, Luyao 1; Ma, Yongfa 2
刊名	QUATERNARY RESEARCH
	2019-07-01
卷号	92 期号:1 页码:133-145
关键词	Northeastern China Holocene summer monsoon maximum Tianchi Crater lake Pollen-based quantitative reconstruction
ISSN号	0033-5894
DOI	10.1017/qua.2018.137
英文摘要	The timing of the Holocene summer monsoon maximum (HSMM) in northeastern China has been much debated and more quantitative precipitation records are needed to resolve the issue. In the present study, Holocene precipitation and temperature changes were quantitatively reconstructed from a pollen record from the sediments of Tianchi Crater Lake in northeastern China using a plant functional type-modern analogue technique (PFT-MAT). The reconstructed precipitation record indicates a gradual increase during the early to mid-Holocene and a HSMM at similar to 5500-3100 cal yr BP, while the temperature record exhibits a divergent pattern with a marked rise in the early Holocene and a decline thereafter. The trend of reconstructed precipitation is consistent with that from other pollen records in northeastern China, confirming the relatively late occurrence of the HSMM in the region. However, differences in the onset of the HSMM within northeastern China are also evident. No single factor appears to be responsible for the late occurrence of the HSMM in northeastern China, pointing to a potentially complex forcing mechanism of regional rainfall in the East Asian monsoon region. We suggest that further studies are needed to understand the spatiotemporal pattern of the HSMM in the region.
资助项目	National Basic Research Program of China[2015CB953802] ; National Science Foundation of China[41672159] ; National Science Foundation of China[41472149] ; National Science Foundation of China[41301040] ; Ministry of Land and Resources[201311137] ; Youth Innovation Promotion Association CAS[2018498]
WOS关键词	EAST-ASIAN MONSOON ; SUMMER MONSOON ; INNER-MONGOLIA ; QUANTITATIVE RECONSTRUCTION ; PRECIPITATION PATTERN ; MOISTURE EVOLUTION ; NORTHERN CHINA ; INDIAN-OCEAN ; DAIHAI LAKE ; NE CHINA
WOS研究方向	Physical Geography ; Geology
语种	英语
出版者	CAMBRIDGE UNIV PRESS
WOS记录号	WOS:000476591500009
资助机构	National Basic Research Program of China ; National Science Foundation of China ; Ministry of Land and Resources ; Youth Innovation Promotion Association CAS ; National Basic Research Program of China ; National Science Foundation of China ; Ministry of Land and Resources ; Youth Innovation Promotion Association CAS ; National Basic Research Program of China ; National Science Foundation of China ; Ministry of Land and Resources ; Youth Innovation Promotion Association CAS ; National Basic Research Program of China ; National Science Foundation of China ; Ministry of Land and Resources ; Youth Innovation Promotion Association CAS
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/92920]
专题	地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者	Zhan, Tao; Zhou, Xinying; Zhang, Xiaolin; Zhou, Xin
作者单位	1.Univ Sci & Technol China, Sch Earth & Space Sci, Hefei 230026, Anhui, Peoples R China 2.Second Hydrogeol & Engn Geol Prospecting Inst Hei, Harbin 150030, Heilongjiang, Peoples R China 3.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 5.Chinese Acad Geol Sci, Inst Geomech, Beijing 100081, Peoples R China 6.Heilongjiang Bur Geol & Mineral Resources, Harbin 150036, Heilongjiang, Peoples R China
推荐引用方式 GB/T 7714	Liu, Xiaoyan,Zhan, Tao,Zhou, Xinying,et al. Late onset of the Holocene rainfall maximum in northeastern China inferred from a pollen record from the sediments of Tianchi Crater Lake[J]. QUATERNARY RESEARCH,2019,92(1):133-145.
APA	Liu, Xiaoyan.,Zhan, Tao.,Zhou, Xinying.,Wu, Haibin.,Li, Qin.,...&Zhou, Xin.(2019).Late onset of the Holocene rainfall maximum in northeastern China inferred from a pollen record from the sediments of Tianchi Crater Lake.QUATERNARY RESEARCH,92(1),133-145.
MLA	Liu, Xiaoyan,et al."Late onset of the Holocene rainfall maximum in northeastern China inferred from a pollen record from the sediments of Tianchi Crater Lake".QUATERNARY RESEARCH 92.1(2019):133-145.