高邮湖GY07-02柱状样的沉积记录与湖泊环境演化

唐薇, 殷勇, 李书恒, 郭伟. 高邮湖GY07-02柱状样的沉积记录与湖泊环境演化[J]. 海洋地质与第四纪地质, 2014, 34(4): 145-151. doi: 10.3724/SP.J.1140.2014.04145
引用本文: 唐薇, 殷勇, 李书恒, 郭伟. 高邮湖GY07-02柱状样的沉积记录与湖泊环境演化[J]. 海洋地质与第四纪地质, 2014, 34(4): 145-151. doi: 10.3724/SP.J.1140.2014.04145
TANG Wei, YIN Yong, LI Shuheng, GUO Wei. SEDIMENTARY CHARACTERISTICS OF GY07-02 COLUMN AND ENVIRONMENTAL CHANGES OF GAOYOU LAKE[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 145-151. doi: 10.3724/SP.J.1140.2014.04145
Citation: TANG Wei, YIN Yong, LI Shuheng, GUO Wei. SEDIMENTARY CHARACTERISTICS OF GY07-02 COLUMN AND ENVIRONMENTAL CHANGES OF GAOYOU LAKE[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 145-151. doi: 10.3724/SP.J.1140.2014.04145

高邮湖GY07-02柱状样的沉积记录与湖泊环境演化

  • 基金项目:

    国家自然科学基金项目(40901101

    40776023)

详细信息
    作者简介: 唐薇(1981-),女,硕士生,从事海岸带地貌与沉积环境研究,E-mail:tangweii158@gmail.com
  • 中图分类号: P736.22

SEDIMENTARY CHARACTERISTICS OF GY07-02 COLUMN AND ENVIRONMENTAL CHANGES OF GAOYOU LAKE

  • 通过对苏北高邮湖GY07-02柱状样沉积物的含水率、粒度、有机碳、碳酸盐含量等环境替代指标的分析,结合14C年代测定,初步揭示了该地区近1 100年来湖泊沉积特征及环境演化历史,大致可以分为3个阶段:920-980AD,为沼泽沉积环境;980-1240AD,湖泊开始扩张,水位上升;1240AD至今,黄河物质通量显著增加。进一步说明湖泊的演变不仅与黄河南泛夺淮有关,也与人类活动如人口迁移、湖泊周围建闸、围湖造地、富营养化程度加剧等关系密切。
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  • [1]

    王苏民, 张振克. 中国湖泊沉积与环境演变研究的新进展[J]. 科学通报, 1999, 44(6):579-587.

    [WANG Sumin, ZHANG Zhenke. The new progress of the study of lake sediment and environmental evolution in China[J]. Chinese Science Bulletin, 1999, 44(6):579-587.]

    [2]

    Gerard Bond, Bernd Kromer. Persistent solar influence on North Atlantic climate during the Holocene[J]. Science, 2001, 294:2130-2136.

    [3]

    Porter S C, An Z S. Correlation between climate events in the North Atlantic and China during the last glaciation[J]. Nature, 1995, 375:305-308.

    [4]

    鹿化煜, 安芷生. 黄土高原黄土粒度组成的古气候意义[J]. 中国科学D辑, 1998, 28(3):278-283.

    [LU Huayu, AN Zhisheng. Paleoclimatic significance of grain-size composition of loess-palaeosol deposit in Chinese Loess Plateau[J]. Science in China (Series D), 1998, 28(3):278-283.]

    [5]

    李志忠, 凌智永, 陈秀玲. 新疆伊犁河谷晚全新世风沙沉积粒度旋回与气候变化[J]. 地理科学, 2010, 30(1):613-619.

    [LI Zhizhong, LING Zhiyong, CHEN Xiuling. Lake Holocene climate change revealed by grain-size cycles in Takemukul desert in Yili of Xinjiang[J]. Scientia Geographica Sinica, 2010, 30(1):613-619.]

    [6]

    罗建育, 陈镇东. 台湾高原湖泊沉积记录指示的近4000a气候与环境变化[J]. 中国科学D辑, 1997, 27(4):366-372.

    [LUO Jianyu, Chen Zhendong. Climatic and environmental changes over the last 4000years recorded in the Mountain lake sedimentary from Taiwan[J]. Science in China (Series D), 1997, 27(4):366-372.]

    [7]

    Chen Jingan, Wan Guojiang, Tang Degui. Recent climate changes recorded by sediment grain sizes and isotopes in Erhai Lake[J]. Progress in Natural Science, 2003, 10(3):253-259.

    [8]

    孙千里, 周杰, 肖举乐. 岱海沉积物粒度特征及其古环境意义[J]. 海洋地质与第四纪地质, 2001, 21(1):93-95.

    [SUN Qianli, ZHOU Jie, XIAO Jule. Grain-size characteristics of lake Daihai sediments and its paleoenvironment significance[J]. Marine Geology and Quaternary Geology, 2001, 21(1):93-95.]

    [9]

    何华春, 丁海燕, 张振克. 淮河中下游洪泽湖湖泊沉积物粒度特征及其沉积环境意义[J]. 地理科学, 2005, 25(5):590-596.

    [HE Huachun, DING Haiyan, ZHANG Zhenke. Grain-size characteristics and their environmental significance of Hongze lake sediments[J]. Scientia Geographica Sinica, 2005, 25(5):590-596.]

    [10]

    王心源, 吴立, 张广胜, 等. 安徽巢湖全新世湖泊沉积物磁化率与粒度组合的变化特征及其环境意义[J]. 地理科学, 2008, 28(4):548-553.

    [WANG Xinyuan, WU Li, ZHANG Guangsheng, et al. Characteristics and environmental significance of magnetic susceptibility and grain size of lake sediments since Holocene in Chaohu lake, Anhui province[J]. Scientia Geographica Sinica, 2008, 28(4):548-553.]

    [11]

    廖高明. 高邮湖的形成和发展[J]. 地理学报, 1992, 47(2):139-145.

    [LIAO Gaoming. The formation and development of Gaoyou lake[J]. Acta Geographica Sinica, 1992, 47(2):139-145.]

    [12]

    Li SH, Fu G H, Guo W, He H C, Zhang Z K. Environmental changes during modern period from the record of Gaoyou Lake sediments, Jiangsu, China[J]. Journal of Geographical Science, 2007, 17(1):62-72.

    [13]

    王苏民, 窦鸿身. 中国湖泊志[M]. 北京:科学出版社, 1998.[WANG Sumin, DOU Hongshen. China Lakes Chorography[M]. Beijing:Science Press, 1998.]

    [14]

    魏文志, 付立霞, 陈日明, 等. 高邮湖水质与浮游植物调查及营养状况评价[J]. 长江流域资源与环境, 2010, 19(1):106-110.

    [WEI Wenzhi, FU Lixia, CHEN Riming, et al. Water quality and phytoplankton investigation and trophic status evaluation in Lake Gaoyou[J]. Resources and Environment in the Yangtze Basin., 2010, 19(1):106-110.]

    [15]

    Blott S. Pye K. GRADISIAT:grain size distribution and statistics package for the analysis of unconsolidated sediments[J]. Earth Surfaces Processes and Landforms, 2001, 26, 1237-1248.

    [16]

    成都地质学院陕北队. 沉积岩(物)粒度分析及其应用[M]. 北京:地质出版社, 1978.[The Geology Team of Chengdu College of Geology. Application analysis of grain size[M]. Beijing:Geological Publishing House, 1978]

    [17]

    Chen Muhong, Zheng Fan, Lu Jun, et al. Original component of grain size index in core sediment from southwestern slope of the South China Sea and its paleo-environmental implication[J]. Chinese Science Bulletin, 2005, 50(9):66-72.

    [18]

    Ball D F. Carbon analysis in a mud sample based on loss on ignition[J]. Journal of Soil Science, 1964, 15:84-91.

    [19]

    Sutherland R A. Comparison of the loss-on-ignition and thermo gravimetric analysis techniques in measuring unburned carbon in coal ash[J]. Hydrobiology, 1998, 389:353-367.

    [20]

    李树峰, 阎顺. 乌鲁木齐东道海子剖面的硅藻记录与环境演变[J]. 干旱区地理, 2005, 28(1):81-87.

    [LI Shufeng, YAN Shun. Diatom records and environmental changes of Dongdaohaizi area in Urumqi, Xinjiang[J]. Arid Land Geography., 2005, 28(1):81-87.]

    [21]

    马妮娜, 穆桂金, 阎顺. 中全新世以来乌鲁木齐东道海子B剖面沉积物源探讨与分析[J]. 干旱区地理, 2005, 28(2):188-193.

    [MA Nina, MU Guijin, YAN Shun. Grain-size analyses and detrital sediment discuss of the B profile of Dongdaohaizi in Urumqi since the middle Holocene[J]. Arid Land Geogaphy, 2005, 28(2):188-193.]

    [22]

    王苏民, 李建仁. 湖泊沉积——研究历史气候的有效手段:以青海、岱海为例[J]. 科学通报, 1991, 36(1):54-56.

    [WANG Sumin, LI Jianren. Lacustrine sediments-An indicator of historical climatic variation-The case of Qinghai lake and Daihai lake[J]. Chinese Science Bulletin, 1991, 36(1):54-56.]

    [23]

    袁旭音, 陈骏, 季峻峰, 等. 太湖沉积物和湖岸土壤的污染元素特征及环境变化效应[J]. 沉积学报, 2002, 20(3):427-434.

    [YUAN Xuyin, CHEN Jun, JI Junfeng, et al. Characteristics and environmental changes of pollution elements in Taihu sediments and soils near the lake[J]. Acta Sedimentologica Sinica, 2002, 20(3):427-434.]

    [24]

    陈敬安, 万国江, 张峰, 等. 不同时间尺度下的湖泊沉积物环境记录——以沉积物粒度为例[J]. 中国科学D辑, 2003, 33(6):563-568.

    [CHEN Jingan, WAN Guojiang, ZHANG feng, et al. The record of lake sediments in different scales-Taking grain size for example[J]. Science in China (Series D), 2003, 33(6):563-568.]

    [25]

    蓝勇. 中国历史地理学[M]. 北京:高等教育出版社, 2005.[LAN Yong. The Chinese Historical Geography[M]. Beijing:Higher Education Press. 2005]

    [26]

    金相灿, 刘鸿亮, 屠清英, 等. 中国湖泊富营养化[M]. 北京:中国环境科学出版社, 1990.[JIN Xiangcan, LIU Hongliang, TU Qingying, et al. Lake Eutrophication in China[M]. Beijing:China Environmental Science Press, 1990.]

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出版历程
收稿日期:  2013-10-11
修回日期:  2013-12-25

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