Microbiology Laboratory, National Institute of Oceanography, Dona Paula 403 004, Goa, India.
Antonie Van Leeuwenhoek. 2010 Jun;98(1):9-18. doi: 10.1007/s10482-010-9423-7. Epub 2010 Mar 13.
Sediment underlying the oxygen minimum zone of the eastern Arabian Sea is rich in organic matter. Bacteria in this sediment-water interface are of great ecological importance as they are responsible for decomposing, mineralizing and subsequent recycling of organic matter. This study has for the first time addressed the phylogenetic and functional description of culturable bacteria of this region. Genotypic characterization of the isolates using amplified rDNA restriction analysis (ARDRA) followed by 16SrRNA sequencing grouped them into various phylogenetic groups such as Firmicutes, Gammaproteobacteria, Low G+C Gram positive bacteria, Actinobacteria and unaffiliated bacteria. Among the enzyme activities, phosphatase was predominant (52%) and was associated with all the phylotypes followed by amylase (37%) and gelatinase (33%). These hydrolytic enzymes were expressed at a wide range of temperature and pH. Firmicutes expressed most of the hydrolytic activities, consistent with a role in degradation of organic matter. Multiple enzyme expression (>/=3) was exhibited by Actinobacteria (100%), followed by unaffiliated group (62.5%) and Firmicutes (61.5%). Besides hydrolytic enzymes, the phylotypes also elaborated functional enzymes such as nitrate reductase and catalase (58 and 81% of the isolates, respectively). In the oxygen minimum zone, the diversity was high with 28 phylotypes. Culturable bacterial assemblages encountered were Bacillus sp., Halobacillus sp., Virgibacillus sp., Paenibacillus sp., Marinilactibacillus sp., Kytococcus sp., Micrococcus sp., Halomonas sp. and Alteromonas sp. The high diversity and high percentage of extracellular hydrolytic enzyme activities of the culturable bacteria reflect their important ecological role in biogeochemical cycling of organic matter in the oxygen minimum zone.
阿拉伯海东部氧最小层下的沉积物富含有机物。这些沉积物-水界面中的细菌具有重要的生态意义,因为它们负责分解、矿化和随后的有机物再循环。本研究首次对该区域可培养细菌的系统发育和功能描述进行了研究。使用扩增 rDNA 限制分析(ARDRA)对分离株进行基因型特征分析,然后进行 16SrRNA 测序,将它们分为各种系统发育群,如厚壁菌门、γ-变形菌纲、低 GC 阳性革兰氏菌、放线菌和未分类细菌。在酶活性中,磷酸酶占主导地位(52%),与所有的菌群都有关联,其次是淀粉酶(37%)和明胶酶(33%)。这些水解酶在很宽的温度和 pH 值范围内表达。厚壁菌门表达了大多数水解活性,与有机物的降解作用一致。放线菌表现出多种酶的表达(>/=3)(100%),其次是未分类组(62.5%)和厚壁菌门(61.5%)。除了水解酶外,菌群还表达了功能酶,如硝酸盐还原酶和过氧化氢酶(分别为 58%和 81%的分离株)。在氧最小层,多样性很高,有 28 个菌群。遇到的可培养细菌组合有芽孢杆菌属、盐杆菌属、海洋盐单胞菌属、类芽孢杆菌属、海洋乳杆菌属、滑行菌属、微球菌属、盐单胞菌属和交替单胞菌属。可培养细菌的高多样性和高比例的细胞外水解酶活性反映了它们在氧最小层有机物生物地球化学循环中的重要生态作用。