IGGCAS OpenIR  > 新生代地质与环境院重点实验室
Interdecadal to Centennial Climate Variability Surrounding the 8.2 ka Event in North China Revealed Through an Annually Resolved Speleothem Record From Beijing
Duan, Pengzhen1,2; Li, Hanying2; Ma, Zhibang3; Zhao, Jingyao2; Dong, Xiyu2; Sinha, Ashish4; Hu, Peng5; Zhang, Haiwei2; Cai, Yanjun2; Ning, Youfeng2; Edwards, R. Lawrence6; Cheng, Hai2,7
2023-01-16
Source PublicationGEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
Volume50Issue:1Pages:11
AbstractThe 8.2 ka event has been extensively studied, whereas its structure is ambiguous in North China. Here we present a high-resolution (similar to 1 year) delta O-18 record from annual laminated speleothem from Beijing to characterize the detailed variability across this event in North China. Our record indicates a dry 8.2 ka event spanning 8.254-8.107 ka BP with a two-stage structure superimposed by three prominent high delta O-18 excursions. The identical structure of speleothem delta O-18 records between North and central China during the event suggests a common forcing/response in East China, whereas the progressively increased offset between their average values may reflect changes in moisture source or rainout effect. A close comparison with the Greenland ice core records suggests a strong linear response of the Asian summer monsoon to the North Atlantic climate changes across the early and middle stages of the event, but a different mechanism in the termination processes.
DOI10.1029/2022GL101182
Funding OrganizationNational 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
WOS KeywordASIAN SUMMER MONSOON ; LAMINATED STALAGMITES ; ATLANTIC CLIMATE ; HOLOCENE ; LINKS ; TELECONNECTIONS ; QUANTIFICATION ; MECHANISMS ; INTERVALS ; RAINFALL
Language英语
Funding ProjectNational Natural Science Foundation of China ; [41731174] ; [41888101] ; [42150710534]
Funding OrganizationNational 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
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000916264900030
PublisherAMER GEOPHYSICAL UNION
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/106816
Collection新生代地质与环境院重点实验室
Corresponding AuthorLi, Hanying; Cheng, Hai
Affiliation1.PetroChina, Res Inst Petr Explorat & Dev, Beijing, Peoples R China
2.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing, Peoples R China
4.Calif State Univ Dominguez Hills, Dept Earth Sci, Carson, CA USA
5.Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
6.Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN USA
7.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Peoples R China
Recommended Citation
GB/T 7714
Duan, Pengzhen,Li, Hanying,Ma, Zhibang,et al. Interdecadal to Centennial Climate Variability Surrounding the 8.2 ka Event in North China Revealed Through an Annually Resolved Speleothem Record From Beijing[J]. GEOPHYSICAL RESEARCH LETTERS,2023,50(1):11.
APA Duan, Pengzhen.,Li, Hanying.,Ma, Zhibang.,Zhao, Jingyao.,Dong, Xiyu.,...&Cheng, Hai.(2023).Interdecadal to Centennial Climate Variability Surrounding the 8.2 ka Event in North China Revealed Through an Annually Resolved Speleothem Record From Beijing.GEOPHYSICAL RESEARCH LETTERS,50(1),11.
MLA Duan, Pengzhen,et al."Interdecadal to Centennial Climate Variability Surrounding the 8.2 ka Event in North China Revealed Through an Annually Resolved Speleothem Record From Beijing".GEOPHYSICAL RESEARCH LETTERS 50.1(2023):11.
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