QIN Jun-gan, WU Guo-xuan, ZHENG Hong-bo, ZHOU Qi. CLIMATE FLUCTUATIONS IN THE YANGTZE DELTA DURING THE LAST GLACIAL MAXIMUM[J]. Marine Geology & Quaternary Geology, 2007, 27(6): 71-75.
Citation: QIN Jun-gan, WU Guo-xuan, ZHENG Hong-bo, ZHOU Qi. CLIMATE FLUCTUATIONS IN THE YANGTZE DELTA DURING THE LAST GLACIAL MAXIMUM[J]. Marine Geology & Quaternary Geology, 2007, 27(6): 71-75.
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CLIMATE FLUCTUATIONS IN THE YANGTZE DELTA DURING THE LAST GLACIAL MAXIMUM

  • 1 College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China;

  • 2 School of Ocean and Earth Science, Tongji University, Shanghai 200092, China

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  • Received Date: October 09, 2007
  • Revised Date: October 25, 2007
    Graphical Abstract
    • Abstract
  • Climate fluctuations during the Last Glacial Maximum have been a hot topic recently. Based on fern spores, pollen and algae records of the first hard clay layer from HM core,three palynomorphs assemblages were recognized and climate conditions during the LGM were discussed. Palynomorphs assemblages 1 and 3 show that mixed conifer broadleaf forest developed, indicating relatively warm and wet climate conditions,while palynomorphs assemblage 2 shows that vegetation was almost absent, indicating a cold climate.
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    • References (21)
  • [1]
    Tsukada M. Vegetation and climate during the Last Glacial Maximum in Japan[J]. Quaternary Research, 1983, 19:212-235.
    [2]
    Wang Pin-xian, Sun Xiang-jun. Last Glacial Maximum in China:Comparison between land and sea[J]. Catena, 1994, 23:341-353.
    [3]
    施雅风,郑本兴,李世杰. 青藏高原的末次冰期与最大冰期——对M.Kuhle的大冰盖假设的否定[J].冰川冻土,1990,12(1):1-16.

    [SHI Ya-feng, ZHENG Ben-xing, LI Shi-jie. Last Glaciation and Maximum Glaciation in Qinghai-Xizang Plateau-A controversy to M. Kuhle ice sheet hypothesis[J]. Journal of Glaciology and Geocryology, 1990, 12(1):1-16.]
    [4]
    施雅风,郑本兴,李世杰,等.青藏高原中东部最大冰期时代高度与气候环境探讨[J]. 冰川冻土,1995,17(2):97-112.

    [SHI Ya-feng, ZHENG Ben-xing, LI Shi-jie, et al. Studies on altitude and climatic environment in the middle and east parts of Tibetan Plateau during Quaternary Maximum Glaciation[J]. Journal of Glaciology and Geocryology, 1995,17(2):97-112.]
    [5]
    安芷生,吴锡浩,卢演俦,等. 最近2万年中国古环境变迁的初步研究[C]//黄土、第四纪地质、全球变化(第二集).北京:科学出版社,1990.[AN Zhi-sheng, WU Xi-hao, LU Yan-chou, et al. The preliminary study of paleoenvironment change in China since the last 20 ka[C]//Loess, Quaternary Research,Global Change,Part Ⅱ. Beijing:Science Press, 1990.]
    [6]
    郑祥民,彭家亮,张卫国,等.长江三角洲及海域风尘沉积与环境[M].上海:华东师范大学出版社,1999.[ZHENG Xiang-min, PENG Jia-liang, ZHANG Wei-guo, et al. Aeolian Deposition and Environment in Changjiang Delta and Extending Sea Areas[M]. Shanghai:Normal University of East China Press, 1999.]
    [7]
    吴征镒. 中国植被[M]. 北京:科学出版社,1980.[WU Zheng-yi. The Vegetation of China[M]. Beijing:Science Press, 1980.]
    [8]
    张玉兰. 上海东部地区全新世孢粉组合及古植被和气候[J].古地理学报,2006,8(1):35-41.

    [ZHANG Yu-lan. Palynological assemblages and palaeovegetation and palaeoclimate of the Holocene in eastern Shanghai[J]. Journal of Palaeogeography, 2006, 8(1):35-41.]
    [9]
    Sun Xiang-jun, Li Xun, Beug H J. Pollen distribution in hemipelagic surface sediments of the South China Sea and its relation to modern vegetation distribution[J]. Marine Geology, 1999, 156:211-226.
    [10]
    米立军,毕力刚,龚胜利,等.渤海新近纪古湖发育的直接证据[J].海洋地质与第四纪地质,2004,24(2):37-42.

    [MI Li-jun, BI Li-gang, GONG Sheng-li, et al. Direct evidence for development of Bohai paleolake during the Neogene[J]. Marine Geology and Quaternary Geology, 2004, 24(2):37-42.]
    [11]
    覃军干,吴国瑄,郑洪波,等. 长江三角洲及邻区海域第一硬质黏土层的生物化石标志[J].海洋地质与第四纪地质, 2004,24(3):11-18.

    [QIN Jun-gan, WU Guo-xuan, ZHENG Hong-bo,et al. Fossil sign in the uppermost hard clay of the Yangtze delta and adjacent continental shelves[J]. Marine Geology and Quaternary Geology, 2004, 24(3):11-18.]
    [12]
    李楠.论松科植物的地理分布、起源和扩散[J].植物分类学报, 1995,33(2):105-130.

    [LI Nan. Studies on the geographic distribution, origin and dispersal of the family Pinaceae lindl[J]. Acta Phytotaxonomica Sinica, 1995, 33(2):105-130.]
    [13]
    李建强. 山毛榉科植物的起源和地理分布[J].植物分类学报, 1996, 34(4):376-396.

    [LI Jian-qiang. The origin and distribution of the family Fagaceae[J]. Acta Phytotaxonomica Sinica, 1996, 34(4):376-396.]
    [14]
    陈之端. 桦木科植物的系统发育和地理分布[J]. 植物分类学报, 1994, 32(1):1-31.

    [CHEN Zhi-duan. Phylogeny and phytogeography of the Betulaceae[J]. Acta Phytotaxonomica Sinica, 1994, 32(1):1-31.]
    [15]
    陈之端. 桦木科植物的系统发育和地理分布(续)[J]. 植物分类学报, 1994, 32(2):101-153.

    [CHEN Zhi-duan. Phylogeny and phytogeography of the Betulaceae (Cont.)[J]. Acta Phytotaxonomica Sinica, 1994, 32(2):101-153.]
    [16]
    林有润. 菊科植物的系统分类与区系地理的初步探讨[J]. 植物研究, 1993,13(2):151-201.

    [LIN You-run. On the primary study of the systematic and floristics of Compositae[J]. Bulletin of Botanical Research, 1993, 13(2):151-201.]
    [17]
    中国第四纪孢粉数据库小组.中国中全新世(6 kaBP)和末次盛冰期(18 kaBP)生物群区的重建[J].植物学报,2000, 42(11):1201-1209.

    [Members of China Quaternary Pollen Data Base, 2000. Pollen-based Biome Reconstruction at Middle Holocene (6 kaBP) and Last Glacial Maximum (18 kaBP) in China[J]. Acta Botanica Sinica, 2000, 42(11):1201-1209.]
    [18]
    刘金陵,王伟铭. 关于华南地区末次盛冰期植被类型的讨论[J]. 第四纪研究,2004,24(4):213-216.

    [LIU Jin-ling, WANG Wei-ming. A discussion on the vegetation types during LGM time in south China[J]. Quaternary Research, 2004, 24(4):213-216.]
    [19]
    黄镇国,张伟强,许世远,等. 中国日本全新世环境演变对比研究[M]. 广东:广东科技出版社,2002.[HUANG Zhen-guo, ZHANG Wei-qiang, XU Shi-yuan,et al. Holocene Environment Develop of China and Japan[M]. Guangdong:Guangdong Science and Technology Press, 2002.]
    [20]
    WANG Kai-fa,ZHANG Yu-lan, JIANG Hui, et al. Palynological assemblages from the Quaternary sediments of the Changjiang river delta and the age of strata and paleogeography[J]. Acta Oceanologica Sinica, 1986, 5(2):257-270.
    [21]
    刘宝柱,李从先, 业治铮. 长江三角洲地区晚第四纪古土壤中的植物硅酸体及其古环境意义[J]. 海洋地质与第四纪地质, 1995, 15(2):17-24.

    [LIU Bao-zhu, LI Cong-xian, YE Zhi-zheng. Phytolith and its paleoenvironmental significance in the studies of the late Quaternary hard clays in the Yangtze Delta area[J]. Marine Geology and Quaternary Geology, 15(2):17-24.]
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