Institutional Repository of Key Laboratory of Cenozoic Geology and Environment, Chinese Academy of Sciences
Tree-ring delta O-18 from Southeast China reveals monsoon precipitation and ENSO variability | |
Shi, Shiyuan1; Shi, Jiangfeng1,2; Xu, Chenxi3,4; Leavitt, Steven W.2; Wright, William E.2; Cai, Zhongyin5; Zhang, Hongyan1; Sun, Xuguang6; Zhao, Yesi1; Ma, Xiaoqi1; Zhang, Weijie1; Lu, Huayu1 | |
2020-11-15 | |
Source Publication | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
![]() |
ISSN | 0031-0182 |
Volume | 558Pages:14 |
Abstract | Considerable advances have been made in use of tree-ring delta O-18 for climate reconstructions in Southeast China, the East Asian summer monsoon region. However, the relationships among tree-ring cellulose delta O-18 (delta O-18(cell)), local hydroclimate, precipitation delta O-18 (delta O-18(pre)) and El Nino-Southern Oscillation (ENSO) have not yet been fully resolved. The usual interpretation has been that local hydroclimate influences delta O-18(cell) through both the "amount effect" on delta O-18(pre) and evaporative enrichment, but it cannot fully explain the high inter-site correlation of delta O-18(cell) chronologies or their response pattern to ENSO. In this study, we use a newly-developed delta O-18(cell) chronology of Pinus massoniana from a water-stressed site in Zhejiang province, in combination with another three delta O-18(cell) chronologies in Southeast China, to investigate their climatic implications from a regional perspective. The results show that besides local hydroclimate, delta O-18(pre) is also significantly correlated with delta O-18(cell) but with different effects. Spatially homogeneous delta O-18(pre) variation causes high spatial correlations among delta(18)O(cell )from different sites. Analyses show that ENSO variations are responsible for the large-scale common signals in delta O-18(cell) by modulating delta O-18(pre). Therefore, combining delta O-18(cell) chronologies from different locations can enhance ENSO signals, which provides us new opportunities to reconstruct paleo-ENSO activities. Furthermore, eliminating the part of ENSO signal that is not related to the growing season hydroclimate from delta O-18(cell) can increase the explained variance of observed values. These findings provide a guide for future optimized ENSO and local paleoclimate reconstructions using delta O-18(cell). |
Keyword | Dendrochronology Oxygen isotope Hydroclimate Paleoclimate Precipitation delta O-18 |
DOI | 10.1016/j.palaeo.2020.109954 |
Funding Organization | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; Science and Technology Planning Program of Jiangsu Province ; Science and Technology Planning Program of Jiangsu Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; Science and Technology Planning Program of Jiangsu Province ; Science and Technology Planning Program of Jiangsu Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; Science and Technology Planning Program of Jiangsu Province ; Science and Technology Planning Program of Jiangsu Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; Science and Technology Planning Program of Jiangsu Province ; Science and Technology Planning Program of Jiangsu Province |
WOS Keyword | ASIAN SUMMER MONSOON ; OXYGEN-ISOTOPE VARIABILITY ; MAXIMAL T-TEST ; STABLE-ISOTOPES ; RELATIVE-HUMIDITY ; ATMOSPHERIC CONTROLS ; YANGTZE-RIVER ; LOWER REACHES ; WATER ; CELLULOSE |
Language | 英语 |
Funding Project | National Natural Science Foundation of China[41671193] ; National Key R&D Program of China[2016YFA0600503] ; Science and Technology Planning Program of Jiangsu Province[BK20161394] |
Funding Organization | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; Science and Technology Planning Program of Jiangsu Province ; Science and Technology Planning Program of Jiangsu Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; Science and Technology Planning Program of Jiangsu Province ; Science and Technology Planning Program of Jiangsu Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; Science and Technology Planning Program of Jiangsu Province ; Science and Technology Planning Program of Jiangsu Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; Science and Technology Planning Program of Jiangsu Province ; Science and Technology Planning Program of Jiangsu Province |
WOS Research Area | Physical Geography ; Geology ; Paleontology |
WOS Subject | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS ID | WOS:000577193100012 |
Publisher | ELSEVIER |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.iggcas.ac.cn/handle/132A11/98338 |
Collection | 新生代地质与环境院重点实验室 |
Corresponding Author | Shi, Jiangfeng; Lu, Huayu |
Affiliation | 1.Nanjing Univ, Sch Geog & Ocean Sci, 163 Xianlin Rd, Nanjing 210023, Peoples R China 2.Univ Arizona, Lab Tree Ring Res, Tucson, AZ 85721 USA 3.Chinese Acad Sci, Key Lab Cenozo Geol & Environm, Inst Geol & Geophys, Beijing 100029, Peoples R China 4.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China 5.Yunnan Univ, Inst Int Rivers & Ecosecur, Kunming 650500, Yunnan, Peoples R China 6.Nanjing Univ, Sch Atmospher Sci, Nanjing 210023, Peoples R China |
Recommended Citation GB/T 7714 | Shi, Shiyuan,Shi, Jiangfeng,Xu, Chenxi,et al. Tree-ring delta O-18 from Southeast China reveals monsoon precipitation and ENSO variability[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2020,558:14. |
APA | Shi, Shiyuan.,Shi, Jiangfeng.,Xu, Chenxi.,Leavitt, Steven W..,Wright, William E..,...&Lu, Huayu.(2020).Tree-ring delta O-18 from Southeast China reveals monsoon precipitation and ENSO variability.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,558,14. |
MLA | Shi, Shiyuan,et al."Tree-ring delta O-18 from Southeast China reveals monsoon precipitation and ENSO variability".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 558(2020):14. |
Files in This Item: | There are no files associated with this item. |
Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.
Edit Comment