• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    印度尼西亚弗洛勒斯海LGM以来的古海洋学记录

    丁旋 GuichardF. BassinotF. 魏明军

    丁旋, GuichardF., BassinotF., 魏明军, 2005. 印度尼西亚弗洛勒斯海LGM以来的古海洋学记录. 地球科学, 30(5): 565-572.
    引用本文: 丁旋, GuichardF., BassinotF., 魏明军, 2005. 印度尼西亚弗洛勒斯海LGM以来的古海洋学记录. 地球科学, 30(5): 565-572.
    DING Xuan, Guichard F., Bassinot F., WEI Ming-jun, 2005. Paleoceanography of the Last Glacial Maximum in the Flores Sea of the Indonesian Archipelago. Earth Science, 30(5): 565-572.
    Citation: DING Xuan, Guichard F., Bassinot F., WEI Ming-jun, 2005. Paleoceanography of the Last Glacial Maximum in the Flores Sea of the Indonesian Archipelago. Earth Science, 30(5): 565-572.

    印度尼西亚弗洛勒斯海LGM以来的古海洋学记录

    基金项目: 

    国家自然科学基金项目 40476022

    详细信息
      作者简介:

      丁旋(1964-),女,博士,副教授,主要从事古海洋学和微体古生物学研究.E-mail:dingx@cugb.edu.cn

    • 中图分类号: P53

    Paleoceanography of the Last Glacial Maximum in the Flores Sea of the Indonesian Archipelago

    • 摘要: 弗洛勒斯海位于印度尼西亚穿越流通道上, 它的古海洋学特征对于理解LGM以来穿越流活动历史, 及其与全球气候变化的关系具有重要意义.通过对弗洛勒斯海SHI9011岩心δ18O、δ13C、浮游有孔虫组合及碳酸盐含量等古海洋学记录的研究, 认为研究区沉积速率不高, 生物生产力却并不低于高沉积速率的近陆地区.冰期时海平面下降, 陆源物质输入量增加, 使得古生产力上升.冰消期终止期IA海平面快速上升, 陆源营养物质供应减少, 同时穿越流活动增强, 抑制了下部水体向上运动, 古生产力开始下降.8~6ka前后, 强烈的东南季风使得研究区上升流活动增强.

       

    • 图  1  印尼海区现代八月表层洋流活动示意图和SHI9011岩心位置(Gingele et al., 2002)

      Fig.  1.  Today August currents in the Indonesian Archipelago and the location of the core SHI9011

      图  2  SHI9034、SHI9011岩心氧同位素曲线, SHI9011岩心二、八月SSS以及G. sacculifer/G. ruber比值变化曲线

      Fig.  2.  Curves of oxygen isotope of the cores SHI9034 and SHI9011, curves of the SSS of February and August and rate of G.sacculifer/G. ruber

      图  3  SHI9011岩心氧同位素, 浮游、底栖有孔虫和CaCO3堆积速率, CaCO3含量和有孔虫碎壳率变化曲线

      Fig.  3.  Curves of oxygen isotope, MAR of planktonic and benthic foraminifers and CaCO3, relative abundance of CaCO3, fragments of foraminifera of the core SHI9011

      图  4  SHI9011岩心浮游有孔虫重要属种百分含量变化曲线

      Fig.  4.  Species relative abundance of planktonic foraminifera of the core SHI9011

      图  5  SHI9011岩心粒度分布、碳同位素以及浮游有孔虫浅/深层水种比值变化曲线

      Fig.  5.  Grain size, carbon isotope and the rate of the planktonic foraminifer shallow-water species to deep-water species of the core SHI9011

    • Arnold, B. E., Maurice, M. P., 1987. Retreat velocity of the North Atlantic polar front during the last deglaciation determined by 14C accelerator mass spectrometry. Nature, 328: 791-794. doi: 10.1038/328791a0
      Bé, A. W. H., 1977. An ecological, zoogeographical and taxonomic review of recent planktonic foraminifera. In: Ramasay, A.T.S., ed., Oceanic micropaleontology. Academic Press, London, 1-100.
      Bray, N. A., Hautala, S., Chong, J., et al., 1996. Large-scale sea level, thermocline, and wind variations in the Indonesian throughflow region. J. Geophys. Res. , 101: 12239-12254. doi: 10.1029/96JC00080
      Ding, X., Fang, N. Q., Guichard, F., et al., 2004. Indonesian throughflow actions during last glacial maximum. Earth Science—Journal of China University of Geosciences, 29 (2): 151-156 (in Chinese with English abstract).
      Ding, X., Guichard, F., Bassinot, F., et al., 2002. Evolution of heat transport pathways in the Indonesian Archipelago during last deglaciation. Chinese Science Bulletin, 47 (22): 1912-1917. doi: 10.1360/02tb9418
      Ding, X., Guichard, F., Fang, N. Q., et al., 2002. The exhibition of the East Asian monsoon action in the Indonesian Archipelago in the Holocene. Earth Science Frontiers, 9 (1): 154 (in Chinese with English abstract).
      Duplessy, J. C., Arnold, M., Maurice, P., et al., 1986. Direct dating of the oxygen-isotope record of the last deglacia- tion by 14C accelerator mass spectrometry. Nature, 320: 350-352. doi: 10.1038/320350a0
      Duplessy, J. C., Bé, A. W. H., Blanc, P. L., 1981a. Oxygen and carbon isotopic composition and biogeographic distribution of planktonic foraminifer in the Indian Ocean. Palaeogeogr. Palaeoclimatol. Palaeoeco. , 33: 9-46. doi: 10.1016/0031-0182(81)90031-6
      Duplessy, J. C., Delibrias, G., Turon, J. L., et al., 1981b. De- glacial warming of the northeastern Atlantic Ocean: Correlation with the paleoclimate evolution of European continent. Palaeog. Palaeocl. Palaeoeco. , 35: 121-144. doi: 10.1016/0031-0182(81)90096-1
      Fairbanks, R. G., 1989. A 17 000-year glacio-eustatic sea level record: Influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature, 342: 637-642. doi: 10.1038/342637a0
      Fairbanks, R. G., Sverdlove, M., Free, R., et al., 1982. Vertical distribution and isotopic fractionation on living planktonic foraminifera from the Panama basin. Nature, 198: 841-844.
      Gingele, F. X., DeDeckker, P., Girault, A., et al., 2002. History of the south Java current over the past 80 ka. Palaeogeo. Palaeocli. Palaeoeco. , 183: 247-260. doi: 10.1016/S0031-0182(01)00489-8
      Ganssen, G., Sarthein, M., 1983. Stable-isotope composition of foraminifers: The surface and bottom water record of coastal upwelling. In: Thiede, J., Suess, E., eds., Coastal upwelling: Its sediment record. Part A, Responses of the Sedimentary Regime to Present Coastal Upwelling. Plenum Press, New York, 99-121.
      Gordon, A. L., Fine, R. A., 1996. Pathways of water between the Pacific and Indian oceans in the Indonesian seas. Nature, 379: 146-149. doi: 10.1038/379146a0
      Herguera, J. C., Berger, W. H., 1991. Paleoproductivity from benthic foraminifera abundance: Glacial to postglacial change in the West-Equatorial Pacific. Geology, 19: 1173-1176.
      Hilbrecht, H., 1997. Morphologic gradation and ecology in Neogloboquadrina pachyderma and N. dutertrei (planktonic foraminifera) from core top sediments. Mar. Micropaleontol., 31 (1-2): 31-44. doi: 10.1016/S0377-8398(96)00054-0
      Hirst, A. C., Godfrey, J. S., 1993. The role of Indonesian throughflow in a global ocean GCM. J. Phys. Ocean-ogr. , 23: 1057-1085. doi: 10.1175/1520-0485(1993)023<1057:TROITI>2.0.CO;2
      Kawahata, W., Nishimura, A., Gagan, M. K., 2000. Seasonal change in foraminiferal production in the western equatorial Pacific warm pool: Evidence from sediment trap experiments. Deep-Sea Research Ⅱ, 49: 2783-2800.
      Martinez, J. I., DeDekker, P., Chivas, A. R., 1997. New estimate for salinity changes in the Western Pacific Warm Pool during the last glacial maximum: Oxygen-isotope evidence. Mar. Micropaleontol. , 32: 311-340. doi: 10.1016/S0377-8398(97)00029-7
      Martinez, J. I., DeDeckker, P., Barrows, T. T., 1999. Palaeoceanography of the last glacial maximum in the eastern Indian Ocean: Planktonic foraminiferal evidence. Palaeog. Palaeocl. Palaeoco. , 147: 73-99. doi: 10.1016/S0031-0182(98)00153-9
      Martinez, J. I., Lynda, T., DeDeckker, P., 1998. Planktonic foraminifera from the eastern Indian Ocean: Distribution and ecology in relation to the western Pacific warm pool (WPWP). Mar. Micropaleontol. , 34: 121-151. doi: 10.1016/S0377-8398(97)00045-5
      Martinson, D. G., Pisias, W. G., Hays, J. D., et al., 1987. Age dating and the orbital theory of the ice age: Devel- opment of a high resolution 0 to 300 000 year chronos- tratigraphy. Quaternary Research, 27: 1-29. doi: 10.1016/0033-5894(87)90046-9
      Pflaumann, U., Duprat, J., Pujol, C., 1996. SIMMAX: A modern analog technique to deduce Atlantic sea surface temperatures from planktonic foraminifera in deep-sea sediments. Paleoceanography, 11 (1): 15-35. doi: 10.1029/95PA01743
      Pflaumann, U., Jian, Z. M., 1999. Modern distribution pat- terns of planktonic foraminifera in the South China Sea and western Pacific: A new transfer technique to esti- mate regional sea-surface temperatures. Mar. Geology, 156: 41-83. doi: 10.1016/S0025-3227(98)00173-X
      Porter, S. C., An, Z., 1995. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature, 375: 305-308. doi: 10.1038/375305a0
      Ravelo, A. C., Fairbanks, R. G., 1992. Oxygen isotopic composition of multiple species of planktonic foraminifera: Records of the modern photic zone temperature gradient. Paleoceanography, 7 (6): 815-831. doi: 10.1029/92PA02092
      Sirocko, F., Sarnthein, M., Erlenkeuser, H., et al., 1993. Centuryscale events in monsoonal climate over the past 24 000 years. Nature, 364: 322-324. doi: 10.1038/364322a0
      Thompson, P. R., 1981. Planktonic foraminifer in the western North Pacific during the past 150 000 years: Comparison of modern and fossil assemblages. Palaeogrogr. Palaeoclimatol. Palaeoecol. 35: 441-479.
      Wang, L., Sarnthern, M., Erlenkeuser, H., et al., 1999. East Asian monsoon climate during the late Pleistocene: High-resolution sediment records from the South China Sea. Marine Geology, 156: 245-284.
      Wang, P.X., 1995. The South China Sea during the last 150 ka. Tongji University Press, Shanghai(in Chinese).
      Wang, P.X., Min, Q.B., Bian, Y.H., et al., 1986. Plankton- ic foraminifera in the continental slope of the northern South China Sea during the last 130 000 years and their paleo-oceanographic implications. Acta Geologica Sinica, (3): 215-225(in Chinese with English abstract).
      丁旋, 方念乔, GuichardF., 等, 2004. 印度尼西亚多岛海末次冰期最盛期以来的穿越流活动. 地球科学——中国地质大学学报, 29 (2): 151-156. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200402005.htm
      丁旋, GuichardF., 方念乔, 等, 2002. 全新世东亚季风活动在印度尼西亚多岛海的表现. 地学前缘, 9 (1): 154. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200201029.htm
      汪品先, 1995. 十五万年来的南海. 上海: 同济大学出版社.
      汪品先, 闵秋宝, 卞云华, 等, 1986. 十三万年来南海北部陆坡的浮游有孔虫及其古海洋学意义. 地质学报, (3): 215-225.
    • 加载中
    图(5)
    计量
    • 文章访问数:  3773
    • HTML全文浏览量:  490
    • PDF下载量:  7
    • 被引次数: 0
    出版历程
    • 收稿日期:  2005-05-17
    • 刊出日期:  2005-09-25

    目录

      /

      返回文章
      返回