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祁连山高寒草原碱性土壤固氮微生物数量及固氮基因(nifH)群落结构研究
引用本文:康文龙,台喜生,李师翁,董康,刘光琇,张威.祁连山高寒草原碱性土壤固氮微生物数量及固氮基因(nifH)群落结构研究[J].冰川冻土,2013,35(1):208-216.
作者姓名:康文龙  台喜生  李师翁  董康  刘光琇  张威
作者单位:1. 兰州交通大学 化学与生物工程学院, 甘肃 兰州 730070; 2. 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
基金项目:中国科学院重点部署项目,国家自然科学基金项目
摘    要:对祁连山高寒草原碱性土壤可培养固氮菌数量、 固氮基因(nifH)群落结构及其理化性质进行了研究. 结果表明: 固氮菌数量在土层0~40 cm处于3.6×105~0.21×105CFUs·g-1之间, 除了海拔3 001 m的土样AQ4外, 其他3个土样固氮菌数量随着土壤深度的加深而减小. 固氮菌数量与地下生物量呈显著正相关性, 与有机碳、 可溶有机氮、 速效磷和速效钾呈正相关性, 而与pH值和全盐呈负相关性. 通过基因测序得到的37个固氮基因nifH克隆中, 蓝藻门占41%, 变形菌门占8%, 厚壁菌门占14%, 未知菌株占37%; 蓝藻门在除了AQ4外的土样中普遍存在, 并且是AQ1的优势固氮菌群. 此外, 还发现了4个新的nifH基因, 分别是AQ1-12(KC412109)、 AQ4-3(KC412133)、 AQ4-4(KC412133)、 AQ4-5(KC412133), 其中后三者是土样AQ4的优势种群.

关 键 词:祁连山高寒草原  碱性土壤  固氮微生物  固氮基因  群落结构  
收稿时间:2012-09-22
修稿时间:2012-12-03

Research on the Number of Nitrogen-Fixing Microorganism and Community Structure of Nitrogen-Fixing (nifH) Genes in the Alkali Soils of Alpine Steppe in the Qilian Mountains
KANG Wen-long,TAI Xi-sheng,LI Shi-weng,DONG Kang,LIU Guang-xiu,ZHANG Wei.Research on the Number of Nitrogen-Fixing Microorganism and Community Structure of Nitrogen-Fixing (nifH) Genes in the Alkali Soils of Alpine Steppe in the Qilian Mountains[J].Journal of Glaciology and Geocryology,2013,35(1):208-216.
Authors:KANG Wen-long  TAI Xi-sheng  LI Shi-weng  DONG Kang  LIU Guang-xiu  ZHANG Wei
Institution:1. School of Chemical and Biological Engineering, Lanzhou Jiaotong University, Lanzhou Gansu 730070, China; 2. Key laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China
Abstract:The physicochemical characteristics, the number of culturable nitrogen-fixing bacteria and the community structure of nitrogen-fixing (nifH) genes in the alkali soils of alpine steppe in the Qilian Mountains are investigated in the present study. It is found that the number of culturable nitrogen-fixing bacteria is between 3.6×105~0.21×105 CFUs5g-1 within the depth of 0-40 cm. The number of nitrogen-fixing bacteria decreases with soil depth in three soil samples, except one sample (AQ4) at the altitude of 3 001 m.The number of nitrogen-fixing bacteria has a significant positive correlation with the underground biomass, and positive correlations with organic carbon, soluble organic nitrogen, rapidly available phosphorus and rapidly available potassium. However, it has negative correlations with soil pH value and total salt. Gene sequencing shows that in a community structure of 37 nitrogen-fixing (nifH) genes there are Cyanobacteria genes (41%), Proteobacteria genes (8%), Firmicutes genes (14%) and unknown bacterium genes (37%). Cyanobacteria genes exist in all soil samples, except for the sample AQ4, and are dominate nitrogen-fixing (nifH) genes in the sample AQ1. It is also found four new nitrogen-fixing (nifH) genes. They are AQ1-12(KC412109), Q4-3(KC412133), AQ4-4(KC412133) and AQ4-5(KC412133), among which AQ4-3(KC412133), AQ4-4(KC412133) and AQ4-5(KC412133) are the dominate genes in sample AQ4.
Keywords:alpine steppe in the Qilian Mountains  alkali soils  nitrogen-fixing microorganism  nifH genes" target="_blank">nifH genes')" href="#">nifH genes  community structure
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