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  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
  4. 中国科学院新生代地质与环境重点实验室
Annual resolution records of sea-level change since 1850 CE reconstructed from coral d(18)O from the South China Sea

文献类型：期刊论文

作者Tao, Shichen6,7; Yu, Kefu5,7; Yan, Hongqiang6,7; Zhang, Huiling4; Wang, Luo3; Rioual, Patrick1,3; Shi, Qi6,7; Huang, Zhongzhou2; Chen, Tegu6
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
出版日期2022-04-15
卷号592页码:12
ISSN号0031-0182
关键词South China Sea Coral delta O- 18 Sea-level Sea surface temperature Sea surface salinity NINO 3, 4 SST
DOI10.1016/j.palaeo.2022.110897
英文摘要Compared with other ocean basins, annual resolution long-term series of sea-level records in the South China Sea (SCS) are still rare. Here we first analyzed the correlation mechanism between the oxygen stable isotopes (delta O-18) of Porites coral and instrumental sea-level, sea surface salinity (SSS), sea surface temperature (SST) and rainfall of the SCS, and NINO 3.4 SST during 1980-2015 CE (Common Era); and we then quantitatively reconstructed sea-level at an annual resolution based on the coral delta O-18 in the SCS. The results show that the sea-level fell slightly (-0.73 +/- 0.27 mm/yr) during 1850-1900 CE; then has continuously risen (1.31 +/- 0.06 mm/yr) with a total increase of 152 & PLUSMN; 7 mm from 1900 to 2015 CE. On the inter-annual timescale, ENSO by mediating the overflow effect of seawater in the Western Pacific Warm Pool and the location of storm genesis in the western Pacific, indirectly affects sea-level, rainfall and SSS, which is finally reflected in changes in coral delta O-18 in the SCS. On the long-term timescale, especially since the 1900s, the gradual increase in SST and glaciers and ice sheets meltwater injected into the ocean due to the continuous warming mainly caused by human activities has not only promoted the rise of sea-level, but also caused a gradual negative bias of delta(18)Oseawater (i.e. a gradual decrease of SSS), these processes are faithfully recorded by coral delta O-18. Compared with SST, SSS or delta(18)Oseawater may play a more important role in promoting the negative bias of coral delta O-18 in the SCS. Our study not only provides a better understanding of sea-level history and relationship mechanism around the SCS during 1850-2015 CE, but also may have the potential to provide a valuable proxy for the accurate quantitative reconstruction of sea-level at an annual resolution over a longer time scale for recent past periods.
WOS关键词SURFACE TEMPERATURE ; ISOTOPE RECORD ; PORITES CORAL ; VARIABILITY ; CLIMATE ; PACIFIC ; OXYGEN ; DELTA-O-18 ; RISE ; OSCILLATION
资助项目NSFC[42090041] ; NSFC[41876132] ; NSFC[41772379] ; NSFC[41776128] ; National Key R&D Program of China[2021YFC3100600] ; National Science & Technology Fundamental Resources Investigation Program of China[2018FY100103] ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)[GML2019ZD0206]
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
出版者ELSEVIER
WOS记录号WOS:000806586900002
资助机构NSFC ; NSFC ; NSFC ; NSFC ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; NSFC ; NSFC ; NSFC ; NSFC ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; NSFC ; NSFC ; NSFC ; NSFC ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; NSFC ; NSFC ; NSFC ; NSFC ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; National Science & Technology Fundamental Resources Investigation Program of China ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
源URL[http://ir.iggcas.ac.cn/handle/132A11/105879]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Yu, Kefu; Wang, Luo
作者单位1.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
2.Guangdong Ocean Univ, Coll Mech & Power Engn, Zhanjiang 524088, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
4.Guangdong Ocean Univ, Coll Ocean Engn, Zhanjiang 524088, Peoples R China
5.Guangxi Univ, Coral Reef Res Ctr China, Sch Marine Sci, Guangxi Lab Study Coral Reefs South China Sea, Nanning 530004, Peoples R China
6.Southern Marine Sci & Engn Guangdong Lab Guangzho, Guangzhou 511458, Peoples R China
7.Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Ocean & Marginal Sea Geol, Guangzhou 510301, Peoples R China
推荐引用方式
GB/T 7714		 Tao, Shichen,Yu, Kefu,Yan, Hongqiang,et al. Annual resolution records of sea-level change since 1850 CE reconstructed from coral d(18)O from the South China Sea[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2022,592:12.
APA Tao, Shichen.,Yu, Kefu.,Yan, Hongqiang.,Zhang, Huiling.,Wang, Luo.,...&Chen, Tegu.(2022).Annual resolution records of sea-level change since 1850 CE reconstructed from coral d(18)O from the South China Sea.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,592,12.
MLA Tao, Shichen,et al."Annual resolution records of sea-level change since 1850 CE reconstructed from coral d(18)O from the South China Sea".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 592(2022):12.

入库方式： OAI收割

来源：地质与地球物理研究所

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