Late Quaternary fingerprints of precession and sea level variation over the past 35 kyr as revealed by sea surface temperature and upwelling records from the Indian Ocean near southernmost Sumatra
Li, Ziye1,2; Shi, Xuefa2,3; Chen, Min-Te2,3,4; Wang, Houjie1,3; Liu, Shengfa2,3; Xu, Jian5,6; Long, Haiyan1; Troa, Rainer Arief7; Zuraida, Rina8; Triarso, Eko7
刊名QUATERNARY INTERNATIONAL
2016-12-15
卷号425页码:282-291
关键词SST Upwelling Eastern Indian Ocean Sumatra Pacific Ocean Quaternary
ISSN号1040-6182
DOI10.1016/j.quaint.2016.07.013
英文摘要We report high-resolution paleoclimatic reconstructions using isotope, alkenone sea surface temperature (SST), productivity, and terrigenous proxy variations over the past 35 kyr from core SO184-10043 (07 degrees 18.57'S, 105 degrees 03.53'E) in the eastern tropical Indian Ocean offshore of southernmost (S) Sumatra. The core was retrieved at 2171 m water depth, from the monsoon driven seasonal upwelling area off southernmost Sumatra. Our paleoclimatic reconstructions show that an enhanced marine productivity was closely linked to strengthening of coastal upwelling during the increases of boreal summer insolation and associated southeastern (SE) monsoon strength, with pronounced semi-precession cycles (similar to 11 kyr). In contrast, our record of alkenone SSTs shows glacial to interglacial, a sea-level variation, but this fluctuates at dominant precession cycles (similar to 21 kyr). We also observed four SST "plateaus" with relatively warmer hydrographic stability in our records over the past 35 kyr: 32-27 ka, 24-20 ka, 17-12 ka, and 9-4 ka. The time scale of each plateau is similar to 4-6 kyr. Our study indicates that since the last glacial maximum (LGM), the sea level rise has been responsible for the Sunda shelf flooding and the Indonesian Throughflow (ITF) from the South China Sea (SCS) to the eastern Indian Ocean, leaving a dominant fingerprint of a glacial to interglacial increase in SSTs since similar to 9.5 ka We further argue that the a most recent centennial to millennial scale cooling at similar to 3.5 ka observed in our SST record is a widespread event in the tropical Pacific, which has implications for advancing our understanding of the climate dynamics of the tropical oceans at these time scales. (C) 2016 Elsevier Ltd and INQUA. All rights reserved.
资助项目Ministry of Science and Technology, Taiwan[MOST 105-2116-M-019-004-]
WOS研究方向Physical Geography ; Geology
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000390534700023
内容类型期刊论文
源URL[http://ir.fio.com.cn/handle/2SI8HI0U/3296]  
专题业务部门_海洋地质与地球物理研究室
作者单位1.Ocean Univ China, Coll Marine Geosci, Qingdao 266100, Peoples R China;
2.SOA, 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.Natl Taiwan Ocean Univ, Inst Appl Geosci, Keelung 202, Taiwan;
5.Northwest Univ, State Key Lab Continental Dynam, Xian 710069, Peoples R China;
6.Northwest Univ, Dept Geol, Xian 710069, Peoples R China;
7.Agcy Marine & Fisheries Res & Dev, Res & Dev Ctr Marine & Coastal Resource, Jakarta 14420, Indonesia;
8.Agcy Res & Dev Energy & Mineral Resources, Marine Geol Inst, Bandung 40174, Indonesia
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GB/T 7714
Li, Ziye,Shi, Xuefa,Chen, Min-Te,et al. Late Quaternary fingerprints of precession and sea level variation over the past 35 kyr as revealed by sea surface temperature and upwelling records from the Indian Ocean near southernmost Sumatra[J]. QUATERNARY INTERNATIONAL,2016,425:282-291.
APA Li, Ziye.,Shi, Xuefa.,Chen, Min-Te.,Wang, Houjie.,Liu, Shengfa.,...&Triarso, Eko.(2016).Late Quaternary fingerprints of precession and sea level variation over the past 35 kyr as revealed by sea surface temperature and upwelling records from the Indian Ocean near southernmost Sumatra.QUATERNARY INTERNATIONAL,425,282-291.
MLA Li, Ziye,et al."Late Quaternary fingerprints of precession and sea level variation over the past 35 kyr as revealed by sea surface temperature and upwelling records from the Indian Ocean near southernmost Sumatra".QUATERNARY INTERNATIONAL 425(2016):282-291.
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