Evolution of heat transport pathways in the Indonesian Archipelago during last deglaciation
Labeyrie, L; Ding, X; Guichard, F; Bassinot, F; Fang, NQ
刊名CHINESE SCIENCE BULLETIN
2002
卷号47期号:22页码:1912-1917
关键词Indonesian Archipelago Last Deglaciation Heat Transport Pathways Delta O-18 Planktonic Foraminifer Assemblages
ISSN号1001-6538
英文摘要The Indonesian Archipelago provides important heat transport pathways of the Western Pacific Warm Pool between the northern Indian Ocean and western equatorial Pacific Ocean, that exert important impacts on global climate change. This study investigated AMS C-14, delta(18)O, planktonic foraminifer assemblages and sedimentation rates in three piston cores collected in the Indonesian Archipelago. The results indicate that changes in the Indonesian Archipelago heat transport pathways were phase characteristic and in steps during the last deglaciation. In the deglaciation Termination IA, at about 12.5 kaBP, sea level rose rapidly in a short time period, and Makassar and Lombok straits widened suddenly for warm and fresh water from the Pacific to pour into the Java Sea and eastern Indian Ocean. During the Termination IB, about 9.5 kaBP, sea level rose rapidly again, and the South China Sea (SCS) started to connect with the Java Sea. With monsoon actions, a large amount of fresh water from the SCS shelf area flew through the Indonesian Archipelago.
学科主题Multidisciplinary Sciences
URL标识查看原文
公开日期2011-07-14
内容类型期刊论文
源URL[http://ir.scsio.ac.cn/handle/344004/8501]  
专题南海海洋研究所_海洋科技动态信息-印太暖池系统研究
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GB/T 7714
Labeyrie, L,Ding, X,Guichard, F,et al. Evolution of heat transport pathways in the Indonesian Archipelago during last deglaciation[J]. CHINESE SCIENCE BULLETIN,2002,47(22):1912-1917.
APA Labeyrie, L,Ding, X,Guichard, F,Bassinot, F,&Fang, NQ.(2002).Evolution of heat transport pathways in the Indonesian Archipelago during last deglaciation.CHINESE SCIENCE BULLETIN,47(22),1912-1917.
MLA Labeyrie, L,et al."Evolution of heat transport pathways in the Indonesian Archipelago during last deglaciation".CHINESE SCIENCE BULLETIN 47.22(2002):1912-1917.
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