The influence of the Sunda Strait opening on paleoenvironmental changes in the eastern Indian Ocean
Xu, Yonghang1; Wang, Liang1; Yin, Xijie1; Ye, Xiang1; Li, Dongyi1; Liu, Shengfa2,3; Shi, Xuefa2,3; Troa, Rainer Arief4; Zuraida, Rina5; Triarso, Eko4
刊名JOURNAL OF ASIAN EARTH SCIENCES
2017-09-15
卷号146页码:402-411
关键词Sr-Nd-Pb isotopes Biogenic elements Provenance Paleoproductivity Sunda Strait Eastern Indian Ocean
ISSN号1367-9120
DOI10.10164/j.jseaes.2017.06.014
英文摘要With sea level rise in the early Holocene, the warm and low-salinity sea water from the Java Sea was transported into the eastern Indian Ocean after the opening of the Sunda Strait. However, the impact of this process on sediment provenance and paleoproductivity is rarely known. In this study, we analyzed the grain size, Sr-Nd-Pb isotopic compositions and biogenic elements of core CJ01-185 (1538 m water depth) in the eastern Indian Ocean off the Sunda Strait. Our new results reveal a large volcanic eruption in the west of Java at 2.1 ka, and the Krakatau eruption at 1883 CE. On the basis of the Pb isotopic compositions, Sr-87/Sr-86 ratios, and epsilon(Nd) values, we infer that sediments from core CJ01-185 were derived primarily from Java Island. There is a distinct change in Sr-Nd-Pb isotopic compositions of the sediments from the last glacial period to the Holocene, indicating less radiogenic Nd isotopes from the Java Sea into the eastern Indian Ocean after the opening of the Sunda Strait at similar to 10 ka. Moreolier, the sedimentation rate increased significantly from 6.5 cm kyr(-1) during the last glacial period to 20 cm kyr-1 in the Holocene. The input of additional terrigenous nutrients from the Java Sea induced paleoproductivity with higher TOC and TN concentrations after the opening of the Sunda Strait. Our results thus suggest that the paleoproductivity was mainly influenced by terrigenous materials input in the Holocene, other than southeast monsoon or upwelling in the last glacial period.
资助项目National Programme on Global Change and Air-Sea Interaction[GASI-GEOGE-06-03] ; National Programme on Global Change and Air-Sea Interaction[GASI-02-IND-CJ01]
WOS研究方向Geology
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000414820300029
内容类型期刊论文
源URL[http://ir.fio.com.cn/handle/2SI8HI0U/3085]  
专题业务部门_海洋地质与地球物理研究室
作者单位1.State Ocean Adm, Inst Oceanog 3, Lab Ocean & Coast Geol, Xiamen 361005, Peoples R China;
2.State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao 266061, Peoples R China;
3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China;
4.Agcy Res & Human Resources Marine & Fisheries, Marine Res Ctr, Jakarta 14420, Indonesia;
5.Agcy Res & Dev Energy & Mineral Resources, Marine Geol Inst, Bandung 40174, Indonesia;
6.Indonesia Inst Sci, Res Ctr Geotechnol, Jakarta 40135, Indonesia
推荐引用方式
GB/T 7714
Xu, Yonghang,Wang, Liang,Yin, Xijie,et al. The influence of the Sunda Strait opening on paleoenvironmental changes in the eastern Indian Ocean[J]. JOURNAL OF ASIAN EARTH SCIENCES,2017,146:402-411.
APA Xu, Yonghang.,Wang, Liang.,Yin, Xijie.,Ye, Xiang.,Li, Dongyi.,...&Hendrizan, Marfasran.(2017).The influence of the Sunda Strait opening on paleoenvironmental changes in the eastern Indian Ocean.JOURNAL OF ASIAN EARTH SCIENCES,146,402-411.
MLA Xu, Yonghang,et al."The influence of the Sunda Strait opening on paleoenvironmental changes in the eastern Indian Ocean".JOURNAL OF ASIAN EARTH SCIENCES 146(2017):402-411.
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