IGGCAS OpenIR  > 新生代地质与环境院重点实验室
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 PublicationPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
Volume558Pages:14
AbstractConsiderable 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).
KeywordDendrochronology Oxygen isotope Hydroclimate Paleoclimate Precipitation delta O-18
DOI10.1016/j.palaeo.2020.109954
Funding OrganizationNational 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 KeywordASIAN SUMMER MONSOON ; OXYGEN-ISOTOPE VARIABILITY ; MAXIMAL T-TEST ; STABLE-ISOTOPES ; RELATIVE-HUMIDITY ; ATMOSPHERIC CONTROLS ; YANGTZE-RIVER ; LOWER REACHES ; WATER ; CELLULOSE
Language英语
Funding ProjectNational Natural Science Foundation of China[41671193] ; National Key R&D Program of China[2016YFA0600503] ; Science and Technology Planning Program of Jiangsu Province[BK20161394]
Funding OrganizationNational 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 AreaPhysical Geography ; Geology ; Paleontology
WOS SubjectGeography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS IDWOS:000577193100012
PublisherELSEVIER
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/98338
Collection新生代地质与环境院重点实验室
Corresponding AuthorShi, Jiangfeng; Lu, Huayu
Affiliation1.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.
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