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冻融循环对青藏高原腹地不同生态系统土壤细菌群落结构的影响
引用本文:张宝贵,张威,刘光琇,陈拓,王鹭,章高森,伍修锟,台喜生,龙昊知,毛文梁. 冻融循环对青藏高原腹地不同生态系统土壤细菌群落结构的影响[J]. 冰川冻土, 2012, 34(6): 1499-1507
作者姓名:张宝贵  张威  刘光琇  陈拓  王鹭  章高森  伍修锟  台喜生  龙昊知  毛文梁
作者单位:1. 中国科学院 寒区旱区环境与工程研究所 沙漠与沙漠化重点实验室, 甘肃 兰州 730000;2. 兰州大学 生命科学学院,甘肃 兰州 730000;3. 甘肃农业大学 资源与环境学院, 甘肃 兰州 730070
基金项目:国家基础研究重点发展计划(973计划)项目(2012CB026105);国家自然科学基金创新群体项目(40821001);国家自然科学基金项目(30800154;31170465;31100365;40971034)资助
摘    要:通过构建16S rRNA基因克隆文库,研究了冻融循环对青藏高原腹地北麓河的高寒沼泽草甸和高寒沙化草原两种不同生态系统土壤细菌群落结构的影响. 结果表明: α-、 β-、 γ- 和δ-变形菌门(α-、 β-、 γ- 和δ-Proteobacteria)、 酸杆菌门(Acidobacteria)、 放线菌门(Actinobacteria)、 拟杆菌门(Bacteroidetes)和浮霉菌门(Planctomycetes)为两个生态系统土壤共有的细菌类群, 其中, 变形菌门、 酸杆菌门及浮霉菌门细菌为研究区域优势菌, 而厚壁菌门(Firmicutes)为高寒沼泽草甸土壤所特有, 疣微菌门(Verrucomicrobia)和绿弯菌门(Chloroflexi)细菌是高寒沙化草原土壤特有的细菌类群, 表明青藏高原腹地两种生态系统土壤具有丰富的细菌多样性. 冻融循环会降低区域土壤的细菌多样性, 随冻融循环, 高寒沼泽草甸和高寒沙化草原生态系统土壤放线菌门丰度均呈现下降趋势, 但大部分细菌随冻融循环的变化在两种生态类型中呈现不同的变化规律, 结果说明冻融循环对于不同生态系统土壤细菌群落结构的影响既存在相似性, 也存在着较大的差异.

关 键 词:青藏高原  高寒沼泽草甸  高寒沙化草原  冻融循环  克隆文库  
收稿时间:2012-08-26
修稿时间:2012-11-05

Effect of Freeze-Thaw Cycles on the Soil Bacterial Communities in Different Ecosystem Soils in the Tibetan Plateau
ZHANG Bao-gui,ZHANG Wei,LIU Guang-xiu,CHEN Tuo,WANG Lu,ZHANG Gao-Sen,WU Xiu-kun,TAI Xi-sheng,LONG Hao-zhi,MAO Wen-liang. Effect of Freeze-Thaw Cycles on the Soil Bacterial Communities in Different Ecosystem Soils in the Tibetan Plateau[J]. Journal of Glaciology and Geocryology, 2012, 34(6): 1499-1507
Authors:ZHANG Bao-gui  ZHANG Wei  LIU Guang-xiu  CHEN Tuo  WANG Lu  ZHANG Gao-Sen  WU Xiu-kun  TAI Xi-sheng  LONG Hao-zhi  MAO Wen-liang
Affiliation:1. Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou Gansu 730000, China;2. School of Life Sciences, Lanzhou University,Lanzhou Gansu 730000, China;3. School of Environmental and Resource Sciences,Gansu Agricultural University, Lanzhou Gansu 730070, China
Abstract:In this paper, the effects of freeze-thaw cycle on the structure of soil bacterial communities in the soils of two ecosystems in the interior of the Tibetan Plateau are studied by the method of 16S rDNA clone libraries. The soil samples were taken from two ecosystems: alpine-cold swamp meadow and alpine sandy grassland in the Beiluhe located in the plateau. It is found that α-, β-, γ-, δ-Proteobacteria, Cidobacteria, Actinobacteria, Bacteroidetes, and Planctomycetes are the common bacterial groups in the soils of the two ecosystems. Among them, Proteobacteria, Acidobacteria and Planctomycetes are the predominant ones. Firmicutes is the one that only exists in the alpine-cold swamp meadow soils, while Verrucomicrobia and Chloroflexi are the two that only exist in the alpine sandy grassland soils. Phylogenetic analysis has revealed the rich diversity of bacteria, which decreases with freeze-thaw cycle. Furthermore, Actinobacteria decreases with freeze-thaw cycle in the two ecosystem soils. However, majority of the bacteria shows different variation in the two ecosystems. It is demonstrated that the effect of freeze-thaw cycles on soil bacterial communities has similarity in the two ecosystem soils, but great discrepancy also shows in some bacterial groups.
Keywords:Tibetan Plateau  alpine-cold swamp meadow  alpine sandy grassland  freeze-thaw cycle  clone library
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