| 8.4 ka以来纳木错湖芯介形类组合的环境变化意义 |
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| 引用本文： | 谢曼平,朱立平,彭萍,王君波,汪勇,SCHWALB Antje.8.4 ka以来纳木错湖芯介形类组合的环境变化意义[J].地理学报(英文版),2009,19(4):387-402. |
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| 作者姓名： | 谢曼平 朱立平 彭萍 王君波 汪勇 SCHWALB Antje |
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| 作者单位： | |
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| 基金项目： | 国家重点基础研究发展规划(973计划)，国家自然科学基金，The sixth framework project BRAHMATWINN |
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| 摘 要： |
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| 关 键 词： | 介形亚纲动物 环境论 生态学 地理学 |
Ostracod assemblages and their environmental significance from the lake core of the Nam Co on the Tibetan Plateau 8.4 kaBP |
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| Manping Xie,Liping Zhu,Ping Peng,Junbo Wang,Yong Wang,Antje Schwalb.Ostracod assemblages and their environmental significance from the lake core of the Nam Co on the Tibetan Plateau 8.4 kaBP[J].Journal of Geographical Sciences,2009,19(4):387-402. |
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| Authors: | Manping Xie Liping Zhu Ping Peng Junbo Wang Yong Wang Antje Schwalb |
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| Institution: | [1]Institute of Tibetan Plateau Research, CAS, Beijing 100085, China [2]Graduate University of Chinese Academy of Sciences, Beijing 100049, China [3]Institut fur Umweltgeologic, Technische Universitat, Braunschweig, Germany |
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| Abstract: | A 332-cm long lacustrine core was drilled in the Nam Co in the central-southern part of the Tibetan Plateau. From the core, 15 species of ostracods (Crustacea: Ostracoda), which belong to 6 genera have been identified. According to the variations of the ostracod assem-blages and the ostracods ecological features, which are sensitive to the changing environ-ment, three main stages can be distinguished as follows: Stage I was from 8400 to 6800 a BP, during which the climate was cold-humid, and the lake depth changed from shallow to deep. Stage II was from 6400 to 2500 a BP, during which the climate changed from warm-humid to cold-humid, and then to cold-dry. The lake depth gradually became deep. The shifting of cli-mate, from wet-cold to dry-cold during this period, had constructed the basis of present en-vironment in the Nam Co. Stage III was from 2500 a BP to the present, which showed a trait of lake depth increasing. At the earlier period of this stage, the climate kept as cold-dry as that in the former stage, but the salinity of the lake increased. At the later period of this stage, the degree of cold-dry was enhanced, and the activities of land surface runoff tended to be weakened. Our research also found that the peak values of ostracods with black shell was coherent with the maximum production of the ostracods, and agreed with the increasing sedimentary water dynamics. This indicated that the ostracods with black shell was simulta-neous with the high prolificacy of ostracod, and transported from other places. The abun-dance of Candona juvenile shells reflected the high mortality of that kind of ostracods under an unfavorable condition. This was probably a result of the rapid change of water dynamics of sedimentary environment. |
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| Keywords: | ostracods environmental change lacustrine core Nam Co Tibetan Plateau |
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