IMHE OpenIR  > 山地表生过程与生态调控重点实验室
Holocene vegetation and climate in Northeast China revealed from Jingbo Lake sediment
Li, Chunhai1; Wu, Yanhong1,2; Hou, Xinhua1
Corresponding AuthorLi, Chunhai ; Wu, Yanhong
2011
Source PublicationQUATERNARY INTERNATIONAL
ISSN1040-6182
EISSN1873-4553
Volume229Pages:67-73
SubtypeArticle; Proceedings Paper
AbstractVegetation and climate changes in Northeast China during the Late Quaternary are poorly known. Pollen analyses were undertaken on a 890-cm-long lacustrine sediment core recovered from Jingbo Lake, located in Southeastern Heilongjiang Province, China. Based on C-14 dating, the pollen record provides a basis for the reconstruction of vegetation and climatic changes since 9600 cal. BP in NE China. Prior to 6100 cal. BP, broad-leaved deciduous forest of Quercus, Fraxinus, and Betula dominated this area, which indicates that the climate during this period was warm and the Asian summer monsoon was stronger. From 6100 to 5600 cal. BP, the deciduous trees declined and Pinus increased, which suggests a transition of vegetation from broad-leaved deciduous forest to mixed coniferous-deciduous forest. Mixed coniferous-deciduous forest with Pinus, Quercus, and Betula expanded and dominated since 5600 cal. BP, indicating a gradual weakening of the Asian summer monsoon. During 2000-680 cal. BP, trees such as Pinus and Quercus declined and herbs including Artemisia, Labiatae, and Scrophulariaceae increased, indicating an extensive human impact on the vegetation. After 680 cal. BP, the forest regenerated due to changed agricultural activities, although the forest was cleared after the 18th century. The vegetation changes superimposed upon this general trend, especially the abundance of trees demanding warm climate conditions, show eight low temperature events at 9200-9000, 8200, 7000-6900, 6000-5600, 4200-3800, 2200-1800, 800, and 600 cal. BP. These short-lived events can be correlated to the spells of delta O-18 depletion in the Dongge Cave stalagmite record, which is widely accepted as a summer monsoon record. (C) 2009 Elsevier Ltd and INQUA. All rights reserved.
KeywordScience & Technology
WOS HeadingsScience & Technology ; Physical Sciences
DOI10.1016/j.quaint.2009.12.015
WOS Subject ExtendedPhysical Geography ; Geology
Indexed BySCI
WOS KeywordATLANTIC CLIMATE ; HIGH-RESOLUTION ; POLLEN RECORD ; ASIAN MONSOON ; VARIABILITY ; FORESTS
Language英语
Quartile3区
WOS SubjectGeography, Physical ; Geosciences, Multidisciplinary
WOS IDWOS:000286863700009
Citation statistics
Cited Times:43[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/10583
Collection山地表生过程与生态调控重点实验室
Affiliation1.Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China
2.Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China
Recommended Citation
GB/T 7714
Li, Chunhai,Wu, Yanhong,Hou, Xinhua. Holocene vegetation and climate in Northeast China revealed from Jingbo Lake sediment[J]. QUATERNARY INTERNATIONAL,2011,229:67-73.
APA Li, Chunhai,Wu, Yanhong,&Hou, Xinhua.(2011).Holocene vegetation and climate in Northeast China revealed from Jingbo Lake sediment.QUATERNARY INTERNATIONAL,229,67-73.
MLA Li, Chunhai,et al."Holocene vegetation and climate in Northeast China revealed from Jingbo Lake sediment".QUATERNARY INTERNATIONAL 229(2011):67-73.
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