Temperature signal instability of tree-ring delta C-13 chronology in the northeastern Qinghai-Tibetan Plateau
文献类型:期刊论文
作者 | Wang, Wenzhi1,2![]() |
刊名 | GLOBAL AND PLANETARY CHANGE
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出版日期 | 2016-04-01 |
卷号 | 139页码:165-172 |
关键词 | Tree-ring delta C-13 Temperature instability Dual-isotope approach Qilian juniper Northeastern Qinghai-Tibetan Plateau |
ISSN号 | 0921-8181 |
通讯作者 | Liu, Xiaohong |
英文摘要 | Tree ring delta C-13 as a climate proxy is widely used for palaeoclimate research, however, its temporal stability response to the climate change remains unclear under more than one limited factors on tree growth. Here, we used a millennium tree-ring delta C-13 chronology combining two annual-resolution delta C-13 chronologies since 1800 from long-lived Qilian juniper (Sabina przewalskii) to assess its instability of the climate signal in the northeastern Qinghai-Tibetan Plateau. Tree-ring delta C-13 chronologies were strongly correlated with the regional mean April to August temperature from 1956 to 2008, but the associations were absent within the period 1901 to 1955 values in the CRU TS dataset. Comparison of the millennium-long delta C-13 series with reconstructed Asian temperatures also demonstrated that the delta C-13 chronology exhibited climate signal temporal instability. Substantial oscillations were revealed using a frequency-dependent analysis and 51-year running correlation analysis from the millennium-long tree-ring delta C-13 and delta O-18 series. Dual-isotope approach indicated that stomatal limitations created a statistical significant positive correlation between tree-ring delta C-13 and delta O-18, but photosynthetic rate may be dominant when the correlations were not significant. Our results suggest that tree-ring delta C-13 series in the northeastern Qinghai-Tibetan Plateau is responded instability to temperature variations in the past 1000 years. (C) 2016 Elsevier B.V. All rights reserved. |
WOS标题词 | Science & Technology ; Physical Sciences |
类目[WOS] | Geography, Physical ; Geosciences, Multidisciplinary |
研究领域[WOS] | Physical Geography ; Geology |
关键词[WOS] | MIDDLE QILIAN MOUNTAINS ; OXYGEN-ISOTOPE RATIO ; STABLE CARBON ; CLIMATE-CHANGE ; STOMATAL CONDUCTANCE ; CONCEPTUAL-MODEL ; CHINA ; DELTA-O-18 ; RECORD ; RECONSTRUCTION |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000374626700014 |
源URL | [http://ir.imde.ac.cn/handle/131551/17384] ![]() |
专题 | 成都山地灾害与环境研究所_山地灾害与地表过程重点实验室 成都山地灾害与环境研究所_山地表生过程与生态调控重点实验室 |
作者单位 | 1.Chinese Acad Sci, State Key Lab Cryospher Sci, Cold & Arid Reg Environm & Engn Res Inst, 320 Donggang West Rd, Lanzhou 730000, Peoples R China 2.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Environm Evolut & Regulat, Chengdu 610014, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Wang, Wenzhi,Liu, Xiaohong,Xu, Guobao,et al. Temperature signal instability of tree-ring delta C-13 chronology in the northeastern Qinghai-Tibetan Plateau[J]. GLOBAL AND PLANETARY CHANGE,2016,139:165-172. |
APA | Wang, Wenzhi.,Liu, Xiaohong.,Xu, Guobao.,Zeng, Xiaomin.,Wu, Guoju.,...&Qin, Dahe.(2016).Temperature signal instability of tree-ring delta C-13 chronology in the northeastern Qinghai-Tibetan Plateau.GLOBAL AND PLANETARY CHANGE,139,165-172. |
MLA | Wang, Wenzhi,et al."Temperature signal instability of tree-ring delta C-13 chronology in the northeastern Qinghai-Tibetan Plateau".GLOBAL AND PLANETARY CHANGE 139(2016):165-172. |
入库方式: OAI收割
来源:成都山地灾害与环境研究所
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