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Quantitative Distributions of Epsilonproteobacteria and a Sulfurimonas Subgroup in Pelagic Redoxclines of the Central Baltic Sea

机译:中波罗的海中上层氧化还原系中的厄普司隆蛋白杆菌和一个硫尿菌亚组的定量分布

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Members of the class Epsilonproteobacteria are known to be of major importance in biogeochemical processes at oxic-anoxic interfaces. In pelagic redoxclines of the central Baltic Sea, an uncultured epsilonproteobacterium related to Sulfurimonas denitrificans was proposed to play a key role in chemolithotrophic denitrification (I. Brettar, M. Labrenz, S. Flavier, J. B?tel, H. Kuosa, R. Christen, and M. G. H?fle, Appl. Environ. Microbiol. 72:1364-1372, 2006). In order to determine the abundance, activity, and vertical distribution of this bacterium in high-resolution profiles, 16S rRNA cloning and catalyzed reporter deposition and fluorescence in situ hybridization (CARD-FISH) and quantitative PCR measurements were carried out. The results showed that 21% of the derived clone sequences, which in the present study were grouped together under the name GD17, had >99% similarity to the uncultured epsilonproteobacterium. A specific gene probe against GD17 (S-*-Sul-0090-a-A-18) was developed and used for enumeration by CARD-FISH. In different pelagic redoxclines sampled during August 2003, May 2005, and February 2006, GD17 cells were always detected from the lower oxic area to the sulfidic area. Maximal abundance was detected around the chemocline, where sulfide and nitrate concentrations were close to the detection limit. The highest GD17 numbers (2 × 105 cells ml?1), representing up to 15% of the total bacteria, were comparable to those reported for Epsilonproteobacteria in pelagic redoxclines of the Black Sea and the Cariaco Trench (X. Lin, S. G. Wakeham, I. F. Putnam, Y. M. Astor, M. I. Scranton, A. Y. Chistoserdov, and G. T. Taylor, Appl. Environ. Microbiol. 72:2679-2690, 2006). However, in the Baltic Sea redoxclines, Epsilonproteobacteria consisted nearly entirely of cells belonging to the distinct GD17 group. This suggested that GD17 was the best-adapted epsilonproteobacterium within this ecological niche.
机译:已知Epsilon变形杆菌属的成员在氧-缺氧界面的生物地球化学过程中具有重要意义。在波罗的海中部的浮游氧化还原层中,有人提出与反硝化硫单胞菌相关的未经培养的ε-变形杆菌在化营养反硝化中起关键作用(I. Brettar,M. Labrenz,S. Flavier,J. B?tel,H.Kuosa,R Christen和MG Hfle,Appl.Environ.Microbiol.72:1364-1372,2006)。为了确定该细菌在高分辨率图谱中的丰度,活性和垂直分布,进行了16S rRNA克隆,催化的报道分子沉积和荧光原位杂交(CARD-FISH)以及定量PCR测量。结果表明,在本研究中以GD17分组在一起的21%的衍生克隆序列与未培养的ε-变形杆菌有> 99%的相似性。开发了针对GD17的特异性基因探针(S-*-Sul-0090-a-A-18),并通过CARD-FISH进行枚举。在2003年8月,2005年5月和2006年2月采样的不同的上层氧化还原细胞中,始终从低氧区到硫化物区检测到GD17细胞。在趋化因子附近检测到最大丰度,其中硫化物和硝酸盐的浓度接近检测极限。 GD17的最高数量(2×105细胞ml?1),占细菌总数的15%,与黑海和Cariaco海沟的浮游氧化还原细胞中的Epsilon变形细菌报告的数量相当(X. Lin,SG Wakeham) ,IF Putnam,YM Astor,MI Scranton,AY Chistoserdov和GT Taylor,Appl。Environ。Microbiol。72:2679-2690,2006)。然而,在波罗的海的氧化还原细胞中,Epsilon变形细菌几乎完全由属于不同的GD17组的细胞组成。这表明GD17是该生态位中最适合的ε变形杆菌。

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