Grosskopf R, Janssen P H, Liesack W
Max-Planck-Institut für terrestrische Mikrobiologie, Marburg, Germany.
Appl Environ Microbiol. 1998 Mar;64(3):960-9. doi: 10.1128/AEM.64.3.960-969.1998.
A dual approach consisting of cultivation and molecular retrieval of partial archaeal 16S rRNA genes was carried out to characterize the diversity and structure of the methanogenic community inhabiting the anoxic bulk soil of flooded rice microcosms. The molecular approach identified four groups of known methanogens. Three environmental sequences clustered with Methanobacterium bryantii and Methanobacterium formicicum, six were closely related but not identical to those of strains of Methanosaeta concilii, two grouped with members of the genus Methanosarcina, and two were related to the methanogenic endosymbiont of Plagiopyla nasuta. The cultivation approach via most-probable-number counts with a subsample of the same soil as an inoculum yielded cell numbers of up to 10(7) per g of dry soil for the H2-CO2-utilizing methanogens and of up to 10(6) for the acetate-utilizing methanogens. Strain VeH52, isolated from the terminal positive dilution on H2-CO2, grouped within the phylogenetic radiation characterized by M. bryantii and M. formicicum and the environmental sequences of the Methanobacterium-like group. A consortium of two distinct methanogens grew in the terminal positive culture on acetate. These two organisms showed absolute 16S rRNA gene identities with environmental sequences of the novel Methanosaeta-like group and the Methanobacterium-like group. Methanosarcina spp. were identified only in the less-dilute levels of the same dilution series on acetate. These data correlate well with acetate concentrations of about 11 microM in the pore water of this rice paddy soil. These concentrations are too low for the growth of known Methanosarcina spp. but are at the acetate utilization threshold of Methanosaeta spp. Thus, our data indicated Methanosaeta spp. and Methanobacterium spp. to be the dominant methanogenic groups in the anoxic rice soil, whereas Methanosarcina spp. appeared to be less abundant.
采用培养和部分古菌16S rRNA基因分子检索相结合的双重方法,对淹水水稻微宇宙缺氧土体中甲烷生成群落的多样性和结构进行了表征。分子方法鉴定出了四类已知的产甲烷菌。三个环境序列与布氏甲烷杆菌和甲酸甲烷杆菌聚类,六个与协调甲烷八叠球菌菌株的序列密切相关但不完全相同,两个与甲烷八叠球菌属成员聚类,两个与鼻形斜叶虫的产甲烷内共生体相关。通过最可能数计数法,以相同土壤的子样本作为接种物进行培养,结果表明,利用H2-CO2的产甲烷菌每克干土的细胞数可达10(7),利用乙酸盐的产甲烷菌每克干土的细胞数可达10(6)。从H2-CO2的终末阳性稀释液中分离出的菌株VeH52,属于以布氏甲烷杆菌和甲酸甲烷杆菌以及类甲烷杆菌属环境序列为特征的系统发育辐射群。在乙酸盐的终末阳性培养物中,两种不同的产甲烷菌形成了一个聚生体。这两种微生物的16S rRNA基因与新的类甲烷八叠球菌属群和类甲烷杆菌属群的环境序列具有绝对同一性。仅在乙酸盐相同稀释系列的较低稀释度水平中鉴定出了甲烷八叠球菌属。这些数据与该稻田土壤孔隙水中约11 microM的乙酸盐浓度密切相关。这些浓度对于已知的甲烷八叠球菌属的生长来说太低了,但处于甲烷八叠球菌属的乙酸盐利用阈值。因此,我们的数据表明,甲烷八叠球菌属和甲烷杆菌属是缺氧水稻土中主要产甲烷菌群,而甲烷八叠球菌属似乎不太丰富。