乌鲁木齐河源区微生物群落演替与气候演变的关系研究

乌鲁木齐河源区 微生物 冰缘植被 冻土
刘光琇 2008-01 项目
【英文摘要】The microorganisms community structures of the soil and snow with different altitude and depth in the headwaters of the Urumqi River was analysised by combianing with the microorganisms number and diversity researches. The results showed that: (1) the vegetation type and altitude were main factors which influenced the number of cultivable bacteria; (2) the number of the microorganims was significantly correlated with soil physicochemical properties and deposit ages; (3) the rhizosphere of periglacial plants contained abundance bacteria resources, and the bacteria abundance were differented with different periglacial plants,which were closely correlated with plant succession, plant diversity and its primary productivity; (4) the community structure, the diversity and cultivable number of snow microorganism were closely correlated with δ18O values and ion concerntration. Based on these, we proposed that the distribution of bacteria could be a biological index for climate and environment change record.
【中文摘要】本研究分别以乌鲁木齐河源区土壤和雪冰为介质,通过对样品中微生物的数量和多样性的研究,分析了不同海拔、不同深度中微生物的群落结构特征,并结合相关的理化性质资料,揭示微生物的来源及其演替规律以及与气候环境演变的关联度。主要结果如下:1.揭示了植被类型和海拔是影响土壤可培养细菌数量的主要因素,阐述了微生物多样性水平分布特征。2.揭示了微生物的数量与土壤理化参数和其沉积年代的关联度,阐述了其微生物多样性垂直分布特征。3.分析了冰缘植物根系土微生物数量及其与植被关系,阐明极端环境下的冰缘植物根际土中含有丰富的细菌资源,不同冰缘植物根际土中所含细菌的菌群密度都有较大的差异,指出这些差异与植物群落演替、植物多样性及其初级生产力密切相关。4.研究表明:雪冰微生物群落结构、多样性、可培养数量和演替规律与δ18O值、阴阳离子密切相关,提出以此作为一种研究气候和环境变化新指标,为利用冰芯微生物研究乌鲁木齐河源区气候演变奠定了基础。