Karnachuk O V, Pimenov N V, Iusupov S K, Frank Iu A, Puhakka J A, Ivanov M V
Mikrobiologiia. 2006 Jan-Feb;75(1):101-9.
The distribution and activity of sulfate-reducing bacteria (SRB) in the water column of the alpine meromictic Gek-Gel lake were studied. Apart from traditional microbiological methods based on cultivation and on measuring the process rates with radioactive labels, in situ fluorescent hybridization (FISH) was used, which enables identification and quantification without cultivating organisms. The peak rate of sulfate reduction, 0.486 microg S/(l day), was found in the chemocline at 33 m. The peak SRB number of 2.5 x 106 cells/ml, as determined by the end-point dilutions method on selective media, was found at the same depth. The phylogenetic position of the SRB, as determined by FISH, revealed the predominance of the Desulfovibrio spp., Desulfobulbus spp., and Desulfoarculus spp./Desulfomonile spp. groups. The numbers of spore-forming Desulfotomaculum spp. increased with depth. The low measured rates of sulfate reduction accompanied with high SRB numbers and the predominance of the groups capable of reducing a wide range of substrates permit us to propose utilization of electron acceptors other than sulfate as the main activity of the SRB in the water column.
对高山半混合湖Gek - Gel湖水柱中硫酸盐还原菌(SRB)的分布和活性进行了研究。除了基于培养以及使用放射性标记测量过程速率的传统微生物学方法外,还采用了原位荧光杂交(FISH)技术,该技术能够在不培养生物体的情况下进行鉴定和定量。在33米深处的化学跃层中发现硫酸盐还原的峰值速率为0.486微克硫/(升·天)。通过在选择性培养基上的终点稀释法测定,在相同深度处发现SRB的峰值数量为2.5×10⁶个细胞/毫升。通过FISH确定的SRB的系统发育位置显示,脱硫弧菌属、脱硫球菌属和脱硫泉古菌属/脱硫单胞菌属占优势。形成孢子的脱硫肠状菌属的数量随深度增加。测得的低硫酸盐还原速率伴随着高SRB数量,以及能够还原多种底物的菌群占优势,这使我们能够提出,水柱中SRB的主要活性是利用除硫酸盐以外的电子受体。