环境变化

藏南沉错地区近1400年来的介形类与环境变化

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李元芳 (1939- ), 女, 研究员。E-mail: Liby@igsnrr.ac.cn

收稿日期: 2001-06-04

  修回日期: 2002-01-09

  网络出版日期: 2002-07-25

基金资助

国家重点基础研究规划项目 (G1998040800); 中科院知识创新方向性项目 (KZCX2-314-2); 中科院地理科学与资源研究所知识创新项目 (CXIOG-A1-02)

Environmental Changes and Ostracoda in the Chen Co Lake of Southern Tibet in Recent 1400 Years

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  • Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China

Received date: 2001-06-04

  Revised date: 2002-01-09

  Online published: 2002-07-25

Supported by

National Key Research Project, No.G1998040800

摘要

null

本文引用格式

李元芳, 朱立平, 李炳元 . 藏南沉错地区近1400年来的介形类与环境变化[J]. 地理学报, 2002 , 57(4) : 413 -421 . DOI: 10.11821/xb200204005

Abstract

The CC1 core, with a length of 216 cm, was drilled in the western part of Chen Co Lake in Tibetan Plateau. The 210Pb and 137Cs test indicated that it was a continuous sedimentary sequence since ca. 1400 years. A total of 15 species of ostracodes belonging to 7 genera in the core sediments had been identified. The ostracoda assemblages and their ecological features, together with the sediments dating decision were used to infer the past ca. 1400 years environmental changes as follows: (1) from the end of the 6th century to the 1370s Chen Co was a deeper water lake. The replenished water that flew into the lake increased obviously and the lake water deepened during ca. 708-780 AD; (2) from the 1370s to the 1890s Chen Co gradually became a shallow water lake. However, the lake level still experienced intensive fluctuation in this period. The lake water impetus was stronger in two stages from ca. 1454 to 1525 AD and from ca. 1803 to 1891 AD, during which sediments were subjected to disturbance, transportation and redeposition. The lake shrank and became a shallow water environment. During the stage of ca. 1645-1670 AD the lake environment deteriorated, which led ostracoda fauna not to be able to live. The lake level rose while the depth of the lake increased relatively during ca. 1731-1803 AD; and (3) from the 1890s to the present Chen Co had evolved from a deeper water lake before the mid-1960s to a shallow one at present. The lake had been shrinking since the mid-1960s and became a shallow water lake environment.

参考文献


[1] Zhu Kezhen. Preliminary study of recent 5000 years climatic change in China. Science in China, 1973, (2): 168-189.
[竺可桢. 中国近五千年气候变化的初步研究. 中国科学, 1973, (2): 168-189.]

[2] Shi Yafeng. Decadal climatic variations recorded in Guliya ice core and comparison with the historical documentary data from East China during the last 2000 years. Science in China (D), 1999, 29(supp.1): 79-86.
[施雅风,. 近2000a古里雅冰芯10a尺度的气候变化及其与中国东部文献记录的比较. 中国科学(D辑), 1999, 29 (增刊1): 79-86.]

[3] Zhang Piyuan. Stages of climatic evolution in China during recent 2000 years. Science in China (B), 1994, 24(9): 998-1008.
[张丕远. 中国近2000年来气候演变的阶段性. 中国科学(B辑), 1994, 24(9): 998-1008.]

[4] Yao Tandong. A continuous climatic and environmental records during recent 2 ka: preliminary study of Guliya ice core in recent 2000 years. Chinese Science Bulletin, 1996, 41(12): 1103-1106.
[姚檀栋. 近2ka来高分辨率的连续气候环境变化记录—古里雅冰芯近2Ka记录初步研究. 科学通报, 1996, 41(12): 1103-1106.]

[5] Yao Tandong. Climatic and environmental records of Guliya ice core in recent 2000 years. Quaternary Sciences, 1997, (1): 52-59.
[姚檀栋. 古里雅冰芯近2000年来气候环境变化记录. 第四纪研究, 1997, (1): 52-59.]

[6] Zhang De'er. High resolution paleo-climatic records from Chinese history documents. Quaternary Sciences, 1995, (1): 75-81.
[张德二. 中国历史文献中的高分辨古气候记录. 第四纪研究, 1995, (1): 75-81.]

[7] Li Bingyuan, Zhu Liping. "Greatest lake period" and its palaeo-environment on the Tibetan Plateau. Journal of Geographical Sciences, 2001, 11(1): 34-42.

[8] Wang Sumin, Dou Hongshen. Records of Lakes in China. Beijing: Science Press, 1998.
[王苏民, 窦鸿身. 中国湖泊志. 北京: 科学出版社, 1998.]

[9] Integrated Scientific Survey Team of Qinghai-Tibet Plateau, CAS. Climate in Tibet. Beijing: Science Press, 1984.
[中国科学院青藏高原综合科学考察队. 西藏气候. 北京: 科学出版社, 1984.]

[10] Integrated Scientific Survey Team of Qinghai-Tibet Plateau, CAS. Vegetation in Tibet. Beijing: Science Press, 1988.
[中国科学院青藏高原综合科学考察队. 西藏植被. 北京: 科学出版社, 1988.]

[11] Carbonel P, Colin J P, Danielopol D L et al. Palaeoecology of limnic ostracodes: a review of same major topics. Palaeogeography, Palaeoclimatology, Palaeoecology, 1988, 62: 413-461.

[12] Danielopol D L, Handl M, Yu Yin. Benthic ostracods in the prealpine deep Lake Mondsee, nates on their origin and distribution. In: McKenzie K G, Jones P J (eds.), Ostracoda in the Earth and Life Science. Balkema, 1993. 465-479.

[13] Bhatia S B, Batra R S, Kotlia B S. Ostracodes and palaeoecology of the Karewa Formation of Hirpur and Romushi Sections, Kashmir, India. Current Trends in Geology, 1985, 6 (Climate and Geology of Kashmir): 45-52.

[14] Huang Baoren. Ostracodes of Pliocene and early Pleistocene in Gonghe Basin, Qinghai. In: Collections of Nanjing Institute of Geology and Palaeontology, CAS (19). Beijing: Science Press, 1984. 1-12.
[黄宝仁. 青海共和盆地上新世及早更新世介形类. 见: 中国科学院南京地质古生物研究所集刊(19). 北京: 科学出版社, 1984. 1-12.]

[15] Huang Baoren. Ostracodes in modern lakes bottom sediments of Tibet. Acta Micropalaeonotologica Sinica, 1985, 2(4): 369-376.
[黄宝仁. 西藏现代湖泊表层沉积物中的介形类. 微体古生物学报, 1985, 2(4): 369-376.]

[16] Pang Qiqing. Ostracod fossils in Qilin Lake-Bange Lake areas, Tibet and their stratum significance during late Cenozoic. In: Geological Collections of Qinghai-Tibet Plateau, 1985, 16: 243-264.
[庞其清. 西藏奇林湖-班戈湖地区晚新生代介形虫化石及其地层意义. 见: 青藏高原地质文集, 1985, 16: 243-264.]

[17] Wang Sumin. Daihai: Lake Environment and Climatic Change. Hefei: China Science and Technology University Press, 1990.
[王苏民. 岱海—湖泊环境与气候变化. 合肥: 中国科学技术大学出版社, 1990.]

[18] Peng Jinlan. Ostracodes and environmental changes in Peigu Co in 13000-4500 aBP. Acta Micropalaeonotologica Sinica, 1997, 14(3)
[彭金兰. 西藏佩枯错距今13000—4500年间的介形类及环境变迁. 微体古生物学报, 1997, 14(3): 239-254.]

[19] Hao Daomeng. Introduction to Ecology. Taibei: Xushi Foundation, 1978.
[郝道猛. 生态学概论. 台北: 徐氏基金会, 1978.]

[20] Gasse F, Arnold M, Fontes J C et al. A 13000 year climate record from western Tibet. Nature, 1991, 353(24): 742-745.

[21] Zhu Liping, Chen Ling, Zhang Pingzhong et al. Cold/warm fluctuations of the last 1300 years reflected by environmental magnetism in the Chen Co area, southern Tibet. Journal of Quaternary Sciences, 2001, 21(6): 520-527.
[朱立平, 陈玲, 张平中 等. 环境磁学反映的藏南沉错地区1300年来冷暖变化. 第四纪研究, 2001, 21(6): 520-527.]

[22] De Deckker P, Forester R M. The use of ostracodes to reconstruct continental paleoenvironmental records. In: De Deckker P et al. (eds.), Ostracoda in the Earth Sciences. Elsevier, 1988. 175-200.

[23] Gong Gaofa, Hameed S. Correlations between changes of temperature and humidity in China during recent 2000 years. In: Climatic Changes and Their Influences. Beijing: Meteorological Press, 1993. 70-77.
[龚高法, Hameed S. 近2000年来中国温度变化与湿润状况变化之间的关系. 见: 气候变化及其影响. 北京: 气象出版社, 1993. 70-77.]

[24] Yao Tandong. Climatic changes in Guliya ice core since Little Ice Age. Science in China (B), 1995, 25(10): 1108-1114.
[姚檀栋. 古里雅冰芯中小冰期以来的气候变化. 中国科学(B辑), 1995, 25(10): 1108-1114.]

[25] Xu Jinghua. Sun, climate, famine and nationality movement. Science in China (D), 1998, 28(4): 366-384.
[许靖华. 太阳、气候、饥荒与民族大迁移. 中国科学(D辑), 1998, 28(4): 366-384.]

[26] Zhang Piyuan. Historical Climatic Changes in China. Jinan: Shandong Science and Technology Press, 1996.
[张丕远. 中国历史气候变化. 济南: 山东科学技术出版社, 1996.]

[27] Shi Yafeng. Uplift and Environmental Changes of Qinghai-Tibet Plateau in the Late Cenozoic. Guangzhou: Guangdong Science and Technology Press, 1998.
[施雅风. 青藏高原晚新生代隆升与环境变化. 广州: 广东科技出版社, 1998.]

[28] Lin Zhenyao. Climatic variations of Xizang in recent 200 years. In: Climatic Changes and Their Influences, Beijing: Meteorological Press, 1993.
[林振耀. 近200年西藏的气候变动. 见: 气候变化及其影响. 北京: 气象出版社, 1993. 50-56.]

[29] Lin Zhenyao. The abnormity of climate in 1980s in Tibet and its influence. In: Climatic Changes and Their Influences. Beijing: Meteorological Press, 1993. 43-49.
[林振耀. 80年代西藏气候异常及其影响评价. 见: 气候变化及其影响. 北京: 气象出版社, 1993. 43-49.]

[30] Li Yuanfang, Zhu Liping, Li Bingyuan. Ostracoda and environmental changes of south Hongshan Lake on Tibetan Plateau during the past 150 years. Geographical Research, 2001, 20(2): 199-205.
[李元芳, 朱立平, 李炳元. 150年来青藏高原南红山湖的介形类与环境变化. 地理研究, 2001, 20(2): 199-205.]

[31] Zhu Liping, Chen Ling, Li Bingyuan et al. Environmental changes reflected by the lake sediments of the south Hongshan Lake, northwest Tibet. Science in China (D), 2001, 31(7): 601-607.
[朱立平, 陈玲, 李炳元 等. 西昆仑山南红山湖沉积反映的过去150年湖区环境变化. 中国科学(D辑), 2001, 31(7): 601-607.]

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