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南海西南陆坡末次冰期以来的浮游有孔虫及其古气候意义

吴庐山 朱照宇 邱燕 陈芳 陈超云 钟和贤 周厚云

吴庐山, 朱照宇, 邱燕, 陈芳, 陈超云, 钟和贤, 周厚云. 南海西南陆坡末次冰期以来的浮游有孔虫及其古气候意义[J]. 海洋地质与第四纪地质, 2006, 26(6): 1-8.
引用本文: 吴庐山, 朱照宇, 邱燕, 陈芳, 陈超云, 钟和贤, 周厚云. 南海西南陆坡末次冰期以来的浮游有孔虫及其古气候意义[J]. 海洋地质与第四纪地质, 2006, 26(6): 1-8.
WU Lu-shan, ZHU Zhao-yu, QIU Yan, CHEN Fang, CHEN Chao-yun, ZHONG He-xian, ZHOU Hou-yun. PLANKTONIC FORAMINIFERA FROM THE SOUTHWESTERN CONTINENTAL SLOPE OF THE SOUTH CHINA SEA SINCE LAST GLACIAL AND THEIR PALEO-CLIMATE IMPLICATION[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 1-8.
Citation: WU Lu-shan, ZHU Zhao-yu, QIU Yan, CHEN Fang, CHEN Chao-yun, ZHONG He-xian, ZHOU Hou-yun. PLANKTONIC FORAMINIFERA FROM THE SOUTHWESTERN CONTINENTAL SLOPE OF THE SOUTH CHINA SEA SINCE LAST GLACIAL AND THEIR PALEO-CLIMATE IMPLICATION[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 1-8.

南海西南陆坡末次冰期以来的浮游有孔虫及其古气候意义

详细信息
    作者简介:

    吴庐山(1970-),男,高级工程师,硕士,主要从事海洋地质和第四纪地质研究,E-mail:563wls@163.com

  • 基金项目:

    国家自然科学基金项目(40272077)

    国土资源大调查项目(19991100011011)

    中国科学院边缘海地质重点实验室开放研究基金项目(MSGL04-7)

  • 中图分类号: P736.2

PLANKTONIC FORAMINIFERA FROM THE SOUTHWESTERN CONTINENTAL SLOPE OF THE SOUTH CHINA SEA SINCE LAST GLACIAL AND THEIR PALEO-CLIMATE IMPLICATION

More Information
  • 摘要: 对南海西南陆坡区SA08-34柱状样浮游有孔虫进行了定量统计分析,并采用古生态转换函数FP-12E计算各样品所代表的海水表层古温度(SST),结合14C测年和CaCO3分析结果,揭示了该海域末次冰期以来的古海洋学特征。末次冰期以来SST具有较大的变化,其中冰后期SST冬季为24.85~26.23℃,夏季为28.81~29.36℃,季节温差为2.66~4.47℃;末次盛冰期SST有明显的周期性波动,SST冬季为23.60~26.86℃,夏季为28.45~29.63℃,季节温差为2.34~5.09℃;末次间冰段SST冬季为23.48~27.57℃,夏季为28.82~29.73℃,季节温差为2.16~5.34℃。南海西南陆坡区在末次冰期出现6次明显的海水表层降温事件,其中"新仙女木"事件的年代约为11.75~12.38 kaBP,H1-H4事件的年代分别约为15.51~16.76、21.15~22.40、26.79~27.42和34.31~34.94 kaBP。
  • [1] 陈木宏,涂霞,郑范,等. 南海南部近20万年沉积序列与古气候变化关系[J]. 科学通报,2000,45(5):542-548.

    [CHEN Mu-hong,TU Xia, ZHENG Fan,et al. A study on paleoclimate and sedimentary sequence of the southern South China Sea during the last 200 ka[J]. Chinese Science Bulletin, 2000,45(5):542-548.]
    [2] 郑范,李前裕,陈木宏,等. 南海西南部晚更新世500 ka以来的古海洋学特征[J]. 地球科学-中国地质大学学报,2005,30(5):534-549.

    [ZHENG Fan,LI Qian-yu,CHEN Mu-hong,et al. Late Pleistocene paleoceanographic characteristics of the southwestern South China Sea since 500 ka[J]. Earth Science-Journal of China University of Geosciences,2005,30(5):534-549.]
    [3] 汪品先,闵秋宝,卞云华,等. 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[J]. 地质学报,1986,60(3):215-225.

    [WANG Pin-xian,Min Qiu-bao,BIAN Yun-hua,et al. Planktonic foraminifera in the continental slope of the northern South China Sea during the last 130000 years and their paleo-oceanographic implications[J].Acta Geologica Sinica,1986,60(3):215-225.]
    [4] 汪品先,赵泉鸿,成鑫荣,等. 十五万年来的南海[M]. 上海:同济大学出版社,1995:46-82.[WANG Pin-xian,ZHAO Quan-hong, CHENG Xin-rong,et al. South China Sea Since 150000 Years[M]. Shanghai:Tongji University Press, 1995

    :46-82.]
    [5] WANG Pin-xian, TIAN Jun,CHEN Xin-rong. Transition of Quaternary glacial cyclicity in deep-sea records at Nansha,the South China Sea[J]. Science in China(Series D), 2001,44(10):927-933.]
    [6] JIAN Zhi-min, CHEN Min-ben, LIN Hui-ling, et al. Stepwise paleoceanographic changes during the last deglaciation in the southern South China Sea:Records of stable isotope and microfossils[J]. Science in China(Series D), 1998,41(2):187-194.
    [7] 李保华,赵泉鸿,陈民本,等. 南沙海区晚第四纪浮游有孔虫演化及其古海洋学意义[J]. 微体古生物学报, 2001, 18(1):1-9.

    [LI Bao-hua, ZHAO Quan-hong, CHEN Min-ben, et al. Late Quaternary evolution of planktonic foraminifera in the southern South China Sea and their paleoceanographic significance[J].Acta Micropaleontologica Sinica,2001,18(1):1-9.]
    [8] JIAN Zhi-min, WANG Pin-xian, CHEN Min-ben, et al. Foraminiferal response to major Pleistocene paleoceanographic changes in the South China[J]. Paleoceanography, 2000, 15(2):229-243.
    [9] LI Bao-hua, JIAN Zhi-min, LI Qian-yu, et al. Paleoceanography of the South China Sea since the middle Miocene:evidence from planktonic foraminifera[J]. Marine Micropaleontology, 2005, 54:49-62.
    [10] Thompson P. Planktonic foraminifera in the Western North Pacific during the past 150000 years:comparison of modern and fossil assemblages[J]. Paleogeography, Paleoclimatology, Paleoecology, 1981,35:241-279.
    [11] 王律江,汪品先. 用转换函数法推算南海古温度的尝试[J]. 科学通报, 1988, 33(5):371-373.

    [WANG Lü-jiang, WANG Pin-xian. An attempt at paleo-temperature estimation in South China Sea using transfer function[J]. Chinese Science Bulletin, 1988, 33(5):371-373.]
    [12] Wang P X, Wang L J, Bian Y H, et al. Late Quaternary paleoceanography of the South China Sea:surface circulation and carbonate cycles[J]. Marine Geology, 1995,127:145-165.
    [13] Thunell R C, Miao Q, Calvert S E, et al. Glacial-Holocene biogenic sedimentation patterns in the South China Sea:productivity variations and surface water pCO2[J]. Paleoceanography, 1992,7:143-162.
    [14] Miao Q, Thunell R C, Anderson D M. Glacial-Holocene carbonate dissolution and sea surface temperatures in the South China and Sulu Seas[J]. Paleoceanography, 1994,9:269-290.
    [15] 吴时国,涂霞,罗又郎. 南沙群岛海区晚第四纪深海碳酸盐沉积作用[J]. 海洋地质与第四纪地质,1996,16(3):67-80.

    [WU Shi-guo, TU Xia, LUO You-lang. Deep-sea carbonate sedimentation of Late Quaternary in Nansha Waters[J]. Marine Geology and Quaternary Geology, 1996,16(3):67-80.]
    [16] 李学杰,段威武,魏国彦,等. 近2万年来南海北部与西部碳酸盐旋回及其古海洋学意义[J]. 海洋地质与第四纪地质,1997,17(2):9-20.

    [LI Xue-jie, DUAN Wei-wu, WEI Guo-yan, et al. Carbonate cycles of the last 20 ka in the northern and western South China Sea and their paleooceanographic significance[J]. Marine Geology and Quaternary Geology, 1997,17(2):9-20.]
    [17] 汪品先,卞云华,翦知湣. 南沙海区晚第四纪的碳酸盐旋回[J]. 第四纪研究,1997,17(4):293-300.

    [WANG Pin-xian,BIAN Yun-hua, JIAN Zhi-min. Late Quaternary carbonate cycles in the Nansha Islands area, South China Sea[J]. Quaternary Sciences, 1997,17(4):293-300.]
    [18] 李粹中. 南海深水碳酸盐沉积作用[J]. 沉积学报,1989(7):35-43.[LI Cui-zhong. Deep water carbonate sedimentation of the South China Sea[J].Acta Sedimentologica Sinica, 1989

    (7):35-43.]
    [19] 汪品先. 西太平洋边缘海的冰期碳酸盐旋回[J]. 海洋地质与第四纪地质,1998,18(1):1-11.

    [WANG Pin-xian. Glacial carbonate cycles in western Pacific marginal seas[J]. Marine Geology and Quaternary Geology, 18(1):1-11.]
    [20] 乔培军,邵磊. 南海南部末次冰期以来的沉积物特点及其古环境意义[J]. 海洋地质与第四纪地质,2003,23(2):73-78.

    [QIAO Pei-jun, SHAO Lei. Characteristics of sediments in the Southern South China Sea since the last glaciation and their paleoenvironmental significance[J]. Marine Geology and Quaternary Geology, 2003,23(2):73-78.]
    [21] 郑连福,郭育廷,Winn K,等.南海北部晚第四纪碳酸盐旋回及其地层学意义[M]//南海海洋沉积作用过程与地球化学研究.北京:海洋出版社,1993:109-123.[ZHENG Lian-fu,GUO Yu-ting,Winn K,et al. Carbonate sedimentation cycles in the northern South China Sea during the Late Quaternary[M]//Contributions to Sedimentation Process and Geochemistry of the South China Sea.Beijing:China Ocean Press,1993:109

    -123.]
    [22] 王汝建,李保华,成鑫荣,等. 南沙深水区第四纪生物地层学研究[J]. 第四纪研究,1999,19(6):541-548.

    [WANG Ru-jian, LI Bao-hua, CHENG Xin-rong, et al. Quaternary biostratigraphy in the Nansha area of the South China Sea[J]. Quaternary Sciences, 1999,19(6):541-548.]
    [23] 陈史坚,陈特固,徐锡桢,等. 浩瀚的南海[M]. 北京:科学出版社,1985.[CHEN Shi-jian,CHEN Te-gu, XU Xi-zhen, et al. The Vast South China Sea[M]. Beijing:Science Press, 1985.]
    [24] 龚庆杰, 涂霞,罗又郎. 南沙群岛海区94-10柱样浮游有孔虫碳氧同位素与古气候研究[J]. 热带海洋,1998,17(4):14-20.

    [GONG Qing-jie,TU Xia,LUO You-lang. A study on oxygen and carbon isotopes of planktonic foraminifera in core 94-10 of Nansha Islands sea area and its meaning in paleoclimate[J].Tropic Oceanology, 1998,17(4):14-20.]
    [25] 涂霞,郑范,陈木宏,等. 南海南部陆坡区的浮游有孔虫及其所表征的表层古水温[J]. 热带海洋,2000,19(3):40-49.

    [TU Xia,ZHENG Fan,CHEN Mu-hong. Planktonic foraminifera and paleo-SST of southern slope of South China Sea since 200 kaBP[J].Tropic Oceanology, 2000,19(3):40-49.]
    [26] 李学杰,江茂生. 南海西沙海槽末次冰期以来浮游有孔虫与表层水温[J]. 中国科学D辑, 2002,32(5):423-429.

    [LI Xue-jie, JIANG Mao-sheng. Planktonic foraminifera and surface sea temperature of Xisha Trough of the South China Sea since the last glaciation[J]. Science in China(Series D), 2002,32(5):423-429.]
    [27] CHEN Mu-hong, LI Qian-yu, ZHENG Fan, et al. Variations of the open Western Pacific and South China Sea[J]. Paleoceanography, 20(2), PA2005, dio:10.1029/2004PA001057.
    [28] Thunell R, Anderson D, Gellar D, et al. Sea-surface temperature estimates for the tropical Western Pacific during the last glaciation and their implications for the Pacific Warm Pool[J]. Quaternary Research, 1994, 41:255-264.
    [29] 汪品先. 新生代亚洲形变与海陆相互作用[J]. 地球科学——中国地质大学学报,2005,30(1):1-18.

    [WANG Pin-xian. Cenozoic deformation and history of sea-land interactions in Asia[J]. Earth Science-Journal of China University of Geosciences, 2005,30(1):1-18.]
    [30] WANG Pin-xian.Western Pacific in glacial cycles:Seasonality in marginal seas and variabilities of Warm Pool[J]. Science in China(Series D),1998,41(1):35-41.
    [31] WANG Pin-xian, BIAN Yun-hua, LI Bao-hua, et al. The Younger Dryas in the West Pacific marginal seas[J]. Science in China(Series D), 1996,39(5):522-532.
    [32] Mayewski P A. The Younger Dryas as viewed through the Summit Greenland ice cores[J]. PAGES, 1995,3(1):5-6.
    [33] 王律江,卞云华,汪品先. 南海北部末次冰消期及快速气候回返事件[J]. 第四纪研究, 1994,14(1):1-12.

    [WANG Lü-jiang, BIAN Yun-hua, WANG Pin-xian. The last deglaciation in the South China Sea and the rapid climate return event[J]. Quaternary Sciences, 1994,14(1):1-12.]
    [34] 王律江,Sarnthein M. 南海北部陆坡近四万年的高分辨率古海洋学记录[J]. 第四纪研究, 1999,19(1):27-31.

    [WANG Lü-jiang, Sarnthein M.High-resolution paleoceanographic records during the last 40000 years from the northern slope of the South China Sea[J]. Quaternary Sciences, 1999,19(1):27-31.]
    [35] 赵泉鸿,Kuhnt W, Stattegger K,等. 南海巽他陆坡晚更新世以来的微体化石和古环境[J]. 海洋地质与第四纪地质,2002,22(2):63-68.

    [ZHAO Quan-hong, Kuhnt W, Stattegger K,et al. Microfossils and paleoenvironments of the Sunda slope of the South China Sea since the Late Pleistocene[J]. Marine Geology and Quaternary Geology, 2002,22(2):63-68.]
    [36] Bond G,Broecker W,Johnson S,et al. Correlations between climate records from North Atlantic sediments and Greenland ice[J]. Nature,1993,365:143-147.
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南海西南陆坡末次冰期以来的浮游有孔虫及其古气候意义

    作者简介:

    吴庐山(1970-),男,高级工程师,硕士,主要从事海洋地质和第四纪地质研究,E-mail:563wls@163.com

基金项目:

国家自然科学基金项目(40272077)

国土资源大调查项目(19991100011011)

中国科学院边缘海地质重点实验室开放研究基金项目(MSGL04-7)

  • 中图分类号: P736.2

摘要: 对南海西南陆坡区SA08-34柱状样浮游有孔虫进行了定量统计分析,并采用古生态转换函数FP-12E计算各样品所代表的海水表层古温度(SST),结合14C测年和CaCO3分析结果,揭示了该海域末次冰期以来的古海洋学特征。末次冰期以来SST具有较大的变化,其中冰后期SST冬季为24.85~26.23℃,夏季为28.81~29.36℃,季节温差为2.66~4.47℃;末次盛冰期SST有明显的周期性波动,SST冬季为23.60~26.86℃,夏季为28.45~29.63℃,季节温差为2.34~5.09℃;末次间冰段SST冬季为23.48~27.57℃,夏季为28.82~29.73℃,季节温差为2.16~5.34℃。南海西南陆坡区在末次冰期出现6次明显的海水表层降温事件,其中"新仙女木"事件的年代约为11.75~12.38 kaBP,H1-H4事件的年代分别约为15.51~16.76、21.15~22.40、26.79~27.42和34.31~34.94 kaBP。

English Abstract

参考文献 (36)

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