Newberry Carole J, Webster Gordon, Cragg Barry A, Parkes R John, Weightman Andrew J, Fry John C
Cardiff School of Biosciences, Cardiff University, Main Building, Park Place, PO Box 915, Cardiff CF10 3TL, Wales, UK.
Environ Microbiol. 2004 Mar;6(3):274-87. doi: 10.1111/j.1462-2920.2004.00568.x.
Diversity of Bacteria and Archaea was studied in deep marine sediments by PCR amplification and sequence analysis of 16S rRNA and methyl co-enzyme M reductase (mcrA) genes. Samples analysed were from Ocean Drilling Program (ODP) Leg 190 deep subsurface sediments at three sites spanning the Nankai Trough in the Pacific Ocean off Shikoku Island, Japan. DNA was amplified, from three depths at site 1173 (4.15, 98.29 and 193.29 mbsf; metres below the sea floor), and phylogenetic analysis of clone libraries showed a wide variety of uncultured Bacteria and Archaea. Sequences of Bacteria were dominated by an uncultured and deeply branching 'deep sediment group' (53% of sequences). Archaeal 16S rRNA gene sequences were mainly within the uncultured clades of the Crenarchaeota. There was good agreement between sequences obtained independently by cloning and by denaturing gradient gel electrophoresis. These sequences were similar to others retrieved from marine sediment and other anoxic habitats, and so probably represent important indigenous bacteria. The mcrA gene analysis suggested limited methanogen diversity with only three gene clusters identified within the Methanosarcinales and Methanobacteriales. The cultivated members of the Methanobacteriales and some of the Methanosarcinales can use CO2 and H2 for methanogenesis. These substrates also gave the highest rates in 14C-radiotracer estimates of methanogenic activity, with rates comparable to those from other deep marine sediments. Thus, this research demonstrates the importance of the 'deep sediment group' of uncultured Bacteria and links limited diversity of methanogens to the dominance of CO2/H2 based methanogenesis in deep sub-seafloor sediments.
通过对16S rRNA和甲基辅酶M还原酶(mcrA)基因进行PCR扩增和序列分析,研究了深海海洋沉积物中细菌和古菌的多样性。分析的样本来自大洋钻探计划(ODP)第190航次在日本四国岛外太平洋南海海槽三个地点的深层地下沉积物。从1173站点的三个深度(海底以下4.15、98.29和193.29米)扩增DNA,克隆文库的系统发育分析显示出多种未培养的细菌和古菌。细菌序列主要由一个未培养的深分支“深层沉积物组”(占序列的53%)主导。古菌16S rRNA基因序列主要位于泉古菌门的未培养分支内。通过克隆和变性梯度凝胶电泳独立获得的序列之间有很好的一致性。这些序列与从海洋沉积物和其他缺氧生境中检索到的其他序列相似,因此可能代表重要的本土细菌。mcrA基因分析表明产甲烷菌多样性有限,在甲烷八叠球菌目和甲烷杆菌目中仅鉴定出三个基因簇。甲烷杆菌目的培养成员和一些甲烷八叠球菌目成员可以利用CO2和H2进行甲烷生成。在14C放射性示踪剂对产甲烷活性的估计中,这些底物也给出了最高的速率,其速率与其他深海海洋沉积物的速率相当。因此,这项研究证明了未培养细菌的“深层沉积物组”的重要性,并将产甲烷菌的有限多样性与基于CO2/H2的甲烷生成在深海底沉积物中的主导地位联系起来。