Indo-Pacific Warm Pool variability during the Holocene and Last Glacial Maximum
文献类型:期刊论文
作者 | Xu, JA ; Kuhnt, W ; Holbourn, A ; Regenberg, M ; Andersen, N |
刊名 | PALEOCEANOGRAPHY
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出版日期 | 2010 |
卷号 | 25页码:-PA4230 |
ISSN号 | 0883-8305 |
通讯作者 | jx08@live.cn ; wk@gpi.uni-kiel.de ; ah@gpi.uni-kiel.de ; regenberg@gpi.uni-kiel.de ; nandersen@leibniz.uni-kiel.de |
中文摘要 | We measured oxygen isotopes and Mg/Ca ratios in the surface-dwelling planktonic foraminifer Globigerinoides ruber (white s.s.) and the thermocline dweller Pulleniatina obliquiloculata to investigate upper ocean spatial variability in the Indo-Pacific Warm Pool (IPWP). We focused on three critical time intervals: the Last Glacial Maximum (LGM; 18-21.5 ka), the early Holocene (8-9 ka), and the late Holocene (0-2 ka). Our records from 24 stations in the South China Sea, Timor Sea, Indonesian seas, and western Pacific indicate overall dry and cool conditions in the IPWP during the LGM with a low thermal gradient between surface and thermocline waters. During the early Holocene, sea surface temperatures increased by similar to 3 degrees C over the entire region, indicating intensification of the IPWP. However, in the eastern Indian Ocean (Timor Sea), the thermocline gradually shoaled from the LGM to early Holocene, reflecting intensification of the subsurface Indonesian Throughflow (ITF). Increased surface salinity in the South China Sea during the Holocene appears related to northward displacement of the monsoonal rain belt over the Asian continent together with enhanced influx of saltier Pacific surface water through the Luzon Strait and freshwater export through the Java Sea. Opening of the freshwater portal through the Java Sea in the early Holocene led to a change in the vertical structure of the ITF from surface- to thermocline-dominated flow and to substantial freshening of Timor Sea thermocline waters. |
学科主题 | Geosciences, Multidisciplinary; Oceanography; Paleontology |
收录类别 | SCI |
原文出处 | AMER GEOPHYSICAL UNION |
公开日期 | 2011-07-14 |
源URL | [http://ir.scsio.ac.cn/handle/344004/8387] ![]() |
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 |
推荐引用方式 GB/T 7714 | Xu, JA,Kuhnt, W,Holbourn, A,et al. Indo-Pacific Warm Pool variability during the Holocene and Last Glacial Maximum[J]. PALEOCEANOGRAPHY,2010,25:-PA4230. |
APA | Xu, JA,Kuhnt, W,Holbourn, A,Regenberg, M,&Andersen, N.(2010).Indo-Pacific Warm Pool variability during the Holocene and Last Glacial Maximum.PALEOCEANOGRAPHY,25,-PA4230. |
MLA | Xu, JA,et al."Indo-Pacific Warm Pool variability during the Holocene and Last Glacial Maximum".PALEOCEANOGRAPHY 25(2010):-PA4230. |
入库方式: OAI收割
来源:南海海洋研究所
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