HUANG Yue, RAN Li-hua, JIANG Hui. DIATOM FROM THE SOUTH CHINA SEA DURING THE LATEST PLEISTOCENE AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2006, 26(4): 7-13.
Citation: HUANG Yue, RAN Li-hua, JIANG Hui. DIATOM FROM THE SOUTH CHINA SEA DURING THE LATEST PLEISTOCENE AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2006, 26(4): 7-13.
shu

DIATOM FROM THE SOUTH CHINA SEA DURING THE LATEST PLEISTOCENE AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE

  • Department of Geography, East China Normal University, Shanghai 200062, China

More Information
  • Received Date: December 01, 2005
  • Revised Date: March 09, 2006
    Graphical Abstract
    • Abstract
  • Diatom study on core 17940 from the northern slope of the South China Sea (SCS) reveals that subtropical planktonic species are the most important components in the diatom assemblages during the latest Pleistocene. The changes in the diatom assemblages indicate that the SCS at that time was more closed and the sea level was lower than at present. Meanwhile, the Bølling-Allerød wet phase and the cold and dry Younger Dryas event were recorded based on changes in some characteristic species. However, the boundary between Younger Dryas and Holocene in diatom record is not clear.
    • FullText(HTML)
    • References (26)
  • [1]
    赵泉鸿,汪品先.南海第四纪古海洋学研究进展[J].第四纪研究,1999,19(6):481-501.

    [ZHAO Quan-hong, WANG Pin-xian. Progress in Quaternary paleoceanography of the South China Sea:A review[J]. Quaternary Sciences, 1999, 19(6):481-501.]
    [2]
    Wang P, Prell W, Blum P, et al. Proceedings of ocean drilling program, Initial Reports[J]. College Station:Ocean Drilling Program, 2000,77:125-134.
    [3]
    Sancettac. Distribution of diatom species in surface sediments of the Bering and Okhotsk Seas[J]. Micropaleontology, 1982, 28:221-257.
    [4]
    Stoermer E F, Smol J P. The Diatom, Applications for the Environmental and Earth Sciences[M]. Cambridge University Press, 1999.
    [5]
    苏纪兰.南海北部环流动力机制[C]//南海环境与资源基础研究前瞻.北京:海洋出版社,2001:1-7.[SU Ji-lan. The dynamical mechanism of circulation in the north area of the South China Sea[C]//Perspective in researches of the resource and the environment of the South China Sea. Beijing:China Ocean Press, 2001:1

    -7.]
    [6]
    丁一汇,李宗银.南海季风爆发和演变及其与海洋的相互作用[M].北京:气象出版社,1999:423.[DING Yi-hui, LI Zong-yin. Onset and Evolution of the South China Sea Monsoon and its Interaction with Ocean[M]. Beijing:Meteorology Press, 1999:423.]
    [7]
    Wang P, Wang L, Bian Y, et al. Late Quaternary paleoceanography of the South China Sea:Surface circulation and carbonate cycles[J]. Marine Geology, 1995, 127:145-165.
    [8]
    钱建兴.晚第四纪以来南海古海洋学研究[M].北京:科学出版社,1999:5-6.[QIAN Jian-xing. The Research of Late Quaternary Paleoceanography of the South China Sea[M]. Beijing:Science Press, 1999:5

    -6.]
    [9]
    陈史坚,陈特固,徐锡桢,等.浩瀚的南海[M].北京:科学出版社,1985:116-123.[CHEN Shi-jian, CHEN Te-gu, XU Xi-zhen, et al. The Vast South China Sea[M]. Beijing:Science Press, 1985:116

    -123.]
    [10]
    苏志京,卢筠,候一筠,等.南海表层流场的卫星跟踪浮标观测结果分析[J].海洋与湖沼,2002,33(2):121-127.

    [SU Zhi-jing, LU Jun, HOU Yi-jun, et al. Analysis of satellite-tracked drifting buoys in the South China Sea[J]. Oceanologia et Limnologia Sinica, 2002, 33(2):121-127.]
    [11]
    李薇,刘秦玉,杨海军.吕宋海峡海洋环流的基本特征[J].青岛海洋大学学报,1998,28(3):245-252.

    [LI Wei, LIU Qin-yu, YANG Hai-jun. Principal features of ocean circulation in the Luzon Strait[J]. Journal of Ocean University of Qingdao, 1998, 28(3):245-252.]
    [12]
    JIAN Zhi-min, WANG Lu-jiang, Markus Kienast, et al. Benthic foraminiferal paleoceanography of the South China Sea over the last 40000 years[J]. Marine Geology, 1999, 156:159-186.
    [13]
    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.]
    [14]
    WANG L, Sarnthein M, Erlenkeuser H, et al. East Asian monsoon climate during the Late Pleistocene:high-resolution sediment records from the South China Sea[J]. Marine Geology, 1999, 156:245-284.
    [15]
    Carmelo R Tomas. Identifying Marine Phytoplankton[M]. The United States of America:Academic Press, 1997:33-385.
    [16]
    Hendey N I. An Introductory Account of the Smaller Algae of British Coastal Water, Part V:Bacillariophceae(Diatoms)[M]. Fishery Investigations London Series, 1964:74-165.
    [17]
    蓝东兆,程兆第,刘师成.南海晚第四纪沉积硅藻[M].北京:海洋出版社,1995:43.[LAN Dong-zhao, CHENG Zhao-di, LIU Shi-cheng. Diatoms in Late Quaternary Sediments from the South China Sea[M]. Beijing:China Ocean Press, 1995:43.]
    [18]
    王开发,蒋辉,张玉兰.南海及沿岸地区第四纪孢粉藻类与环境[M].上海:同济大学出版社,1990:68-75.[WANG Kai-fa, JIANG Hui, ZHANG Yu-lan. Pollen algae and environment of Quaternary in South China Sea[M]. Shanghai:Tongji University Press, 1990:68

    -75.]
    [19]
    陆钧.南海深海表层沉积硅藻的分布[J].海洋地质与第四纪地质, 2001,21(2):27-30.

    [LU Jun. Diatom distribution in surface sediments in the deep-sea area of the South China Sea[J]. Marine Geology and Quaternary Geology, 2001, 21(2):27-30.]
    [20]
    冉莉华,蒋辉.南海某些表层沉积硅藻的分布及其古环境意义[J].微体古生物学报,2005,22(1):97-106.

    [RAN Li-hua, JIANG Hui. Distributions of the surface sediment diatoms from the South China Sea and their palaeoceanographic significance[J]. Acta Micropalaeontologica Sinica, 2005, 22(1):97-106.]
    [21]
    郭玉洁.中国海藻志,第五卷第一册,硅藻门中心纲[M].北京:科学出版社,2003:18-119.[GUO Yu-jie. The Algae Record of China, Volumn V[M]. Beijing:Science Press, 2003:18

    -119.]
    [22]
    Jiang H, Zheng Y, Ran L, et al. Diatoms from the surface sediments of the South China Sea and their relationships to modern hydrography[J]. Marine Micropaleontology, 2004, 53:279-292.
    [23]
    金德祥,程兆弟,林均民.中国海洋底栖硅藻类(上)[M].北京:海洋出版社,1982:81.[JIN De-xiang, CHENG Zhao-di, LIN Jun-min. Benthic diatoms of China Seas, Vol. I[M]. Beijing:China Ocean Press, 1982:81.]
    [24]
    Jousé A P, Kozlova O G, Muhina V V. Distribution of diatoms in the surface layer of sediment from the Pacific Ocean[M].London:Cambridge University Press,1971:263-269.
    [25]
    Muhina V V. Problems of Diatom and Silicoflagellate Quaternary Stratigraphy in the Equatorial Pacific Ocean[M]. London:Cambridge University Press,1971:423-431.
    [26]
    汪品先,卞云华.西太平洋边缘海的"新仙女木"事件[J].中国科学D辑,1996,26(5):457-460.

    [WANG Pin-xian, BIAN Yun-hua. the "Younger Dryas" event in the marginal sea on the west Pacific[J]. Science in China(Ser. D), 1996, 26(5):457-460.]
    • Related Articles

  • Related Articles

    [1]CHEN Xiaohui, LU Kai, TIAN Zhenxing, WEN Zhenhe, XU Xiaoda, ZHANG Yong, KONG Xianghuai. Progradational sediment: succession and paleo-channel system in the central South Yellow Sea since the Late Pleistocene[J]. Marine Geology & Quaternary Geology, 2023, 43(4): 85-96. DOI: 10.16562/j.cnki.0256-1492.2022072701
    [2]PENG Zhiyuan, CHEN Chixin, WU Cong, CHEN Fang, ZHOU Yang, YU Shaohua, JIA Lei, SHI Cui. Diatom assemblage since late Pleistocene in the east coast of Lingdingyang Bay and its environmental implications[J]. Marine Geology & Quaternary Geology, 2021, 41(2): 126-135. DOI: 10.16562/j.cnki.0256-1492.2020103001
    [3]LI Jie, LI Rihui, YANG Shixiong, CHEN Xiaohui, CHE Shanshan. Pollen spore assemblages and induced palaeoenvironmental changes in the western Bohai Sea since Late Pleistocene[J]. Marine Geology & Quaternary Geology, 2018, 38(2): 115-128. DOI: 10.16562/j.cnki.0256-1492.2018.02.012
    [4]LIU Meng, WANG Yonghong, LI Sanzhong. THE DISTRIBUTION PATTERN AND EVOLUTION MECHANISM OF WINTER PALEOCURRENTS IN SOUTH CHINA SEA SINCE LATE PLEISTOCENE[J]. Marine Geology & Quaternary Geology, 2015, 35(5): 87-94. DOI: 10.16562/j.cnki.0256-1492.2015.05.010
    [5]LI Jie, MEI Xi, LI Rihui, LAN Xianhong, ZHANG Xunhua. ENVIRONMENTAL CHANGES INFERRED FROM POLLEN RECORDS IN THE SOUTH YELLOW SEA SINCE LATE PLEISTOCENE[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 93-105. DOI: 10.3724/SP.J.1140.2014.04093
    [6]LI Li, CHEN Yuxing, WANG Hui, HE Juan. SEA SURFACE TEMPERATURE CHANGE IN SOUTH CHINA SEA SINCE PLEISTOCENE AND ITS PALEOCLIMATIC IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2012, 32(4): 1-7. DOI: 10.3724/SP.J.1140.2012.04001
    [7]TAO Qianqian, LIU Baohua, LI Xishuang, ZHANG Weigang, LI Da. LATE PLEISTOCENE EVOLUTION OF THE PALEO YANGTZE DELTA IN THE SOUTH YELLOW SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 15-24. DOI: 10.3724/SP.J.1140.2009.02015
    [8]ZHANG Yulan. PALYNOLOGICAL RECORDS ON DEEP-SEA SEDIMENTS IN THE SOUTH CHINA SEA AND ITS PALEOENVIRONMENT[J]. Marine Geology & Quaternary Geology, 2009, 29(1): 25-29. DOI: 10.3724/SP.J.1140.2009.01025
    [9]YE Fang, LIU Zhi-fei, TUO Shou-ting, JIAN Zhi-min. GRAIN SIZE RECORD OF TERRIGENOUS CLAST DURING MID-PLEISTOCENE TRANSITION (0.78~1.0 Ma) IN THE NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2007, 27(2): 77-83.
    [10]QIAO Pei-jun, SHAO Lei, YANG Shou-ye. THE PALEOENVIRONMENTAL SIGNIFICANCE OF THE CHARACTER OF THE ELEMENT GEOCHEMISTRY IN THE SOUTHWESTERN SOUTH CHINA SEA SINCE LATE PLEISTOCENE[J]. Marine Geology & Quaternary Geology, 2006, 26(4): 59-65.

Catalog

    Get Citation
    PDF
    XML
    Article views (1968) PDF downloads (14) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles
    WeChat WeChat
    Order Code Order Code

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return