Millennial-scale paleoceanography in Okinawa Trough during Late Quaternary period
Liu, ZX; Saito, Y; Li, TG; Berne, S; Chen, ZB; Li, PY; Li, Z; Guichard, F; Floch, G
1999-09
发表期刊CHINESE SCIENCE BULLETIN
卷号44期号:18页码:1705-1709
文章类型Article
摘要Based on the analyses of foraminifer and accelerator mass spectrometer radiocarbon dating in DGKS9603 core from mid-Okinawa Trough close to bottom, oscillation curve, which expressed the relation between the surface water temperature and the depth, has been obtained by using foraminifer analysis and calculation of FP-12E transfer function. The whole core indicated seven cold phases and eight warm phases. Obvious expression of low temperature event during Middle and Late Holocene, YD,H1,H2,H3 and H4 events, as well as the short cold phase during the middle last glacial period, implied that short shifts since 50 kaBP would have been global significance. Sedimentation rate during cold phases is usually faster than that in warm stages, with the lowest rate in Holocene, which may be connected with rising sea level and principal axial of Kuroshio Current moving to west. Volcanic activities highly developed in Okinawa Trough during the Quaternary period, thus abundant volcanic glass and pumice were well preserved.
关键词Okinawa Though Late Quaternary period paleoceanograph Heinrich event
学科领域Science & Technology - Other Topics
DOI10.1007/BF03183496
关键词[WOS]PACIFIC
收录类别SCI ; SCIE
语种英语
WOS研究方向Multidisciplinary Sciences
WOS记录号WOS:000083584600018
出版者SCIENCE PRESS
引用统计
被引频次:23[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/12002
专题黄土与第四纪地质国家重点实验室(1985-2004)
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Liu, ZX,Saito, Y,Li, TG,et al. Millennial-scale paleoceanography in Okinawa Trough during Late Quaternary period[J]. CHINESE SCIENCE BULLETIN,1999,44(18):1705-1709.
APA Liu, ZX.,Saito, Y.,Li, TG.,Berne, S.,Chen, ZB.,...&Floch, G.(1999).Millennial-scale paleoceanography in Okinawa Trough during Late Quaternary period.CHINESE SCIENCE BULLETIN,44(18),1705-1709.
MLA Liu, ZX,et al."Millennial-scale paleoceanography in Okinawa Trough during Late Quaternary period".CHINESE SCIENCE BULLETIN 44.18(1999):1705-1709.
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