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学科主题: Geochemistry & Geophysics
题名: Glacial to Holocene surface hydrography of the tropical eastern Indian Ocean
作者: Mohtadi, M ; Steinke, S ; Luckge, A ; Groeneveld, J ; Hathorne, EC
通讯作者: mohtadi@uni-bremen.de
关键词: Indian Ocean ; Indonesia ; foraminifera ; oxygen isotopes ; Mg/Ca ; seawater delta 18O
刊名: EARTH AND PLANETARY SCIENCE LETTERS
发表日期: 2010-01-01
卷: 292, 期:40545, 页:89-97
收录类别: sci
部门归属: [Mohtadi, Mahyar; Steinke, Stephan; Groeneveld, Jeroen] Univ Bremen, Ctr Marine Environm Sci MARUM, D-2800 Bremen 33, Germany; [Lueckge, Andreas] Fed Inst Geosci & Nat Resources BGR, Hannover, Germany; [Groeneveld, Jeroen] Alfred Wegener Inst Polar & Marine Res, D-2850 Bremerhaven, Germany; [Hathorne, Ed C.] Leibniz Inst Marine Sci IFM GEOMAR, Kiel, Germany
摘要: Quantifying the spatial and temporal sea surface temperature (SST) and salinity changes of the Indo-Pacific Warm Pool is essential to understand the role of this region in connection with abrupt climate changes particularly during the last deglaciation. In this study we reconstruct SST and seawater delta O-18 of the tropical eastern Indian Ocean for the past 40,000 years from two sediment cores (GeoB 10029-4, 1 degrees 30'S, 100 degrees 08'E, and GeoB 10038-4, 5 degrees 56'S, 103 degrees 15'E) retrieved offshore Sumatra. Our results show that annual mean SSTs increased about 2-3 degrees C at 19,000 years ago and exhibited southern hemisphere-like timing and pattern during the last deglaciation. Our SST records together with other Mg/Ca-based SST reconstructions around Indonesia do not track the monsoon variation since the last glacial period, as recorded by terrestrial monsoon archives. However, the spatial SST heterogeneity might be a result of changing monsoon intensity that shifts either the annual mean SSTs or the seasonality of G. ruber towards the warmer or the cooler season at different locations. Seawater delta O-18 reconstructions north of the equator suggest fresher surface conditions during the last glacial and track the northern high-latitude climate change during the last deglaciation. In contrast, seawater delta O-18 records south of the equator do not show a significant difference between the last glacial period and the Holocene, and lack Bolling-Allerod and Younger Dryas periods suggestive of additional controls on annual mean surface hydrology in this part of the Indo-Pacific Warm Pool. (c) 2010 Elsevier B.V. All rights reserved.
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内容类型: 期刊论文
URI标识: http://ir.scsio.ac.cn/handle/344004/8403
Appears in Collections:海洋科技动态信息-印太暖池系统研究_期刊论文

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Recommended Citation:
Mohtadi, M; Steinke, S; Luckge, A; Groeneveld, J; Hathorne, EC.Glacial to Holocene surface hydrography of the tropical eastern Indian Ocean,EARTH AND PLANETARY SCIENCE LETTERS,2010,292(40545):89-97
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文件名: Glacial to Holocene surface hydrography of the tropical eastern Indian Ocean.pdf
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