Dojka M A, Hugenholtz P, Haack S K, Pace N R
Department of Plant and Microbial Biology, University of California, Berkeley, Berkeley, California 94720-3102, USA.
Appl Environ Microbiol. 1998 Oct;64(10):3869-77. doi: 10.1128/AEM.64.10.3869-3877.1998.
A culture-independent molecular phylogenetic approach was used to survey constituents of microbial communities associated with an aquifer contaminated with hydrocarbons (mainly jet fuel) and chlorinated solvents undergoing intrinsic bioremediation. Samples were obtained from three redox zones: methanogenic, methanogenic-sulfate reducing, and iron or sulfate reducing. Small-subunit rRNA genes were amplified directly from aquifer material DNA by PCR with universally conserved or Bacteria- or Archaea-specific primers and were cloned. A total of 812 clones were screened by restriction fragment length polymorphisms (RFLP), approximately 50% of which were unique. All RFLP types that occurred more than once in the libraries, as well as many of the unique types, were sequenced. A total of 104 (94 bacterial and 10 archaeal) sequence types were determined. Of the 94 bacterial sequence types, 10 have no phylogenetic association with known taxonomic divisions and are phylogenetically grouped in six novel division level groups (candidate divisions WS1 to WS6); 21 belong to four recently described candidate divisions with no cultivated representatives (OP5, OP8, OP10, and OP11); and 63 are phylogenetically associated with 10 well-recognized divisions. The physiology of two particularly abundant sequence types obtained from the methanogenic zone could be inferred from their phylogenetic association with groups of microorganisms with a consistent phenotype. One of these sequence types is associated with the genus Syntrophus; Syntrophus spp. produce energy from the anaerobic oxidation of organic acids, with the production of acetate and hydrogen. The organism represented by the other sequence type is closely related to Methanosaeta spp., which are known to be capable of energy generation only through aceticlastic methanogenesis. We hypothesize, therefore, that the terminal step of hydrocarbon degradation in the methanogenic zone of the aquifer is aceticlastic methanogenesis and that the microorganisms represented by these two sequence types occur in syntrophic association.
采用一种不依赖培养的分子系统发育方法,对与遭受内在生物修复的、被碳氢化合物(主要是喷气燃料)和氯化溶剂污染的含水层相关的微生物群落成分进行了调查。从三个氧化还原带采集了样本:产甲烷带、产甲烷-硫酸盐还原带以及铁还原或硫酸盐还原带。使用通用保守引物或细菌或古菌特异性引物,通过聚合酶链式反应(PCR)从含水层物质DNA中直接扩增小亚基rRNA基因,并进行克隆。通过限制性片段长度多态性(RFLP)筛选了总共812个克隆,其中约50%是独特的。对文库中出现不止一次的所有RFLP类型以及许多独特类型进行了测序。共确定了104种(94种细菌和10种古菌)序列类型。在94种细菌序列类型中,10种与已知分类群没有系统发育关联,在系统发育上被归为六个新的门类水平组(候选门类WS1至WS6);21种属于最近描述的四个没有培养代表的候选门类(OP5、OP8、OP10和OP11);63种在系统发育上与10个公认的门类相关。从产甲烷带获得的两种特别丰富的序列类型的生理学特征,可以根据它们与具有一致表型的微生物群的系统发育关联来推断。其中一种序列类型与Syntrophus属相关;Syntrophus属的物种通过有机酸的厌氧氧化产生能量,并产生乙酸和氢气。另一种序列类型所代表的生物体与Methanosaeta属的物种密切相关,已知它们仅通过乙酸裂解产甲烷作用来产生能量。因此,我们推测,含水层产甲烷带中碳氢化合物降解的最终步骤是乙酸裂解产甲烷作用,并且这两种序列类型所代表的微生物以互营共生关系存在。