Center for Molecular Biology Severo Ochoa, CSIC-UAM, Cantoblanco, Madrid, Spain.
Int Microbiol. 2011 Sep;14(3):143-54. doi: 10.2436/20.1501.01.143.
The composition of the microbial community inhabiting the anoxic coastal sediments of the Bay of Cádiz (southern Spain) was investigated using a molecular approach consisting of PCR cloning and denaturing gradient gel electrophoresis (DGGE), based on 16S rRNA sequences. The total cell count was 1-5 × 10⁸ cells/g sediment and, as determined by catalyzed reporter deposition-fluorescent in situ hybridization (CARD-FISH), the proportion of Bacteria to Archaea was about 70:30. The analysis of 16S-rRNA gene sequences revealed a wide spectrum of microorganisms, which could be grouped into 111 operational taxonomic units (OTUs). Many of the OTUs showed high phylogenetic similarity to microorganisms living in marine sediments of diverse geographic origin. The phylogenetic groups that were predominantly detected were Firmicutes, Deltaproteobacteria, and Gammaproteobacteria, accounting for 23, 15, and 14% of the clones, respectively. Diversity in the domain Archaea was significantly lower than in the domain Bacteria. The majority of the archaeal OTUs belonged to the Crenarchaeota phylum. Since most of the sequences could not be identified precisely at the genus/species level, the functional roles of the microorganisms in the ecosystem could not be inferred. However, seven OTUs affiliated with the Delta- and Epsilonproteobacteria were identified down to the genus level, with all of the identified genera known to occur in sulfate-rich marine environments.
采用聚合酶链反应克隆和变性梯度凝胶电泳(DGGE)的分子方法,研究了卡迪斯湾(西班牙南部)缺氧沿海沉积物中微生物群落的组成,该方法基于 16S rRNA 序列。总细胞计数为 1-5×10⁸个细胞/克沉积物,通过催化报告物沉积-荧光原位杂交(CARD-FISH)测定,细菌与古菌的比例约为 70:30。16S-rRNA 基因序列分析揭示了广泛的微生物,可分为 111 个操作分类单位(OTU)。许多 OTU 与来自不同地理来源的海洋沉积物中的微生物具有高度的系统发育相似性。主要检测到的系统发育群是厚壁菌门、Delta 变形菌门和 Gamma 变形菌门,分别占克隆的 23%、15%和 14%。古菌域的多样性明显低于细菌域。大多数古菌 OTU 属于泉古菌门。由于大多数序列无法在属/种水平上精确识别,因此无法推断微生物在生态系统中的功能作用。然而,有 7 个 OTU 与 Delta 和 Epsilonproteobacteria 有关,可识别到属水平,所有鉴定的属都存在于富含硫酸盐的海洋环境中。