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作 者:邓宇[1] 张辉[1] 钱贻伯[1] 赵一章[1] 朱辉[1]
出 处:《微生物学报》1998年第4期245-250,共6页Acta Microbiologica Sinica
摘 要:在严格的厌氧条件下,用MPN计数的方法测定了莺琼盆地东方1-1-1井垂直剖面不同沉积层的地质样品中的硫酸盐还原菌、发酵细菌的数量,并检测了产甲烷细菌,对各种菌的形态进行了观察,比较了菌数量与一些指标的关系,并对产甲烷细菌的代谢类型和产甲烷能力进行了观察。研究结果表明:硫酸盐还原菌在各样品中均存在,与沉积深度无相关性,而与样品中SO2-4的含量有一定相关性;而发酵细菌的分布也与沉积深度无相关性,而与样品中的有机质有一定的负相关性。全部样品中均检测出两种形态产甲烷细菌,即甲烷球菌(Methanococcus)和甲烷杆菌(Methanobacterium),其营养类型为H2/CO2。Under the strictly anaerobic conditions,the population of Sulfate-reducing bacteria,fermentative bacteria and methanogenic bacteria of serial samples got from erect sections of different Sedimentary of Yingqiong basin (a typical marine sedimentary environment) were measured by MPN method. The morphology of different kinds of bacteria and the metabolic types of methanogen and methanogenic activity were observed. The relation between population of bacteria and some indexes were compared. The results show that SRB present in all of the samples. The distribution of SRB and fermentative baCteria have no interrelation with the depth of samples but SRB has interrelation with the So2-4 concentration, and fermentative bacteria has negative interrelation with the contents of organic maser. Two kinds of methanogen present in all of the samples. They belong to Methanobacterium and Methanococcus, respectively. Their types of nutriment are H2/CO2.
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