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首页> 外文期刊>Geomicrobiology Journal >Sulfate-reducing Bacteria and Mercury Methylation in the Water Column of the Lake 658 of the Experimental Lake Area
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Sulfate-reducing Bacteria and Mercury Methylation in the Water Column of the Lake 658 of the Experimental Lake Area

机译:实验湖区658湖水柱中的硫酸盐还原细菌和汞甲基化

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Sulfate-reducing bacteria (SRB) appear to be the main mediators of mercury methylation in sediments, which are deemed to be major sites of methylmercury (MMHg) production. However, recent studies have also found significant MMHg formation in the water column of lakes across North America. To investigate the potential involvement of SRB in mercury methylation in the water column of a stratified oligotrophic lake, two of the main families of SRB (Desulfobacteraceae and Desulfovibrionaceae) were quantified by Real-Time Polymerase Chain Reaction of the 16S rRNA gene. MMHg production was measured applying a stable isotope technique using 198HgCl. Methylation assays were conducted at different water depths and under stimulation with lactate, acetate or propionate and inhibition with molybdate. Desulfobacteraceae and Desulfovibrionaceae16S rRNA gene copies in control samples accounted for 0.05% to 33% and 0.01% to 1.12% of the total bacterial 16S rRNA, respectively. MMHg formation was as high as 0.3 ng L−1 day−1 and largest in lactate amended samples. Strain isolation was only achieved in lactate amended media with all isolated strains being SRB belonging to the Desulfovibrio genus according to their 16S rRNA gene sequence. Isolated strains methylated between 0.06 and 0.2% of 198HgCl per day. Acetate and propionate did not stimulate mercury methylation as much as lactate. Two strains were identified as Desulfovibrio sp. 12ML1 (FJ865472) and Desulfovibrio sp. 12ML3 (FJ865473), based on partial sequences of their 16S rRNA and DSR gene. Methylation assays and bacteria characterization suggest that Desulfovibrionaceae is an important mercury methylators in Lake 658. Supplemental materials are available for this article. Go to the publisher's online edition of Geomicrobiology Journal to view the free supplemental file.View full textDownload full textKeywordsmercury, methylmercury, sulfate-reducing bacteria, water column, mercury methylation, Desulfovibrionaceae Related var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/01490451.2011.606289
机译:硫酸盐还原菌(SRB)似乎是沉积物中汞甲基化的主要介质,这些沉积物被认为是甲基汞(MMHg)生产的主要场所。但是,最近的研究还发现,整个北美湖泊的水柱中均会形成大量的MMHg。为了研究分层贫营养湖水柱中SRB可能与汞甲基化有关,通过16S rRNA基因的实时聚合酶链反应对SRB的两个主要家族(脱硫杆菌科和脱硫弧菌科)进行了定量。通过使用 198 HgCl的稳定同位素技术测量MMHg的产生。在不同的水深下,在乳酸,乙酸盐或丙酸盐的刺激下和钼酸盐的抑制下进行甲基化测定。对照样品中的脱硫杆菌科和脱硫弧菌科16S rRNA基因拷贝分别占细菌16S rRNA总数的0.05%至33%和<0.01%至1.12%。 MMHg的形成高达0.3 ng L -1> 天 -1 ,在乳酸修正样品中最大。菌株分离仅在乳酸改良培养基中实现,所有分离的菌株都是根据其16S rRNA基因序列属于脱硫弧菌属的SRB。每天分离出的菌株甲基化的 198 HgCl的0.06-0.2%。乙酸根和丙酸根没有像乳酸那样刺激汞甲基化。确定了两个菌株为Desulfovibrio sp。 12ML1(FJ865472)和Desulfovibrio sp。 12ML3(FJ865473),基于其16S rRNA和DSR基因的部分序列。甲基化分析和细菌鉴定表明,脱硫弧菌科是658湖中重要的汞甲基化剂。本文提供了补充材料。转到出版商的《地球微生物杂志》的在线版本以查看免费的补充文件。查看全文下载全文关键词汞,甲基汞,硫酸盐还原细菌,水柱,甲基化汞,脱硫弧菌科相关变量var addthis_config = {ui_cobrand:“ Taylor&Francis Online”, services_compact:“ citeulike,netvibes,twitter,technorati,美味,linkedin,facebook,stumbleupon,digg,google,更多”,发布:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/01490451.2011.606289

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