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Novel Pelagic Iron-Oxidizing Zetaproteobacteria from the Chesapeake Bay Oxic–Anoxic Transition Zone

机译:切萨皮克湾缺氧-缺氧过渡区的新型上层铁氧化Zetaproteobacteria。

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摘要

Chemolithotrophic iron-oxidizing bacteria (FeOB) could theoretically inhabit any environment where Fe(II) and O2 (or nitrate) coexist. Until recently, marine Fe-oxidizing Zetaproteobacteria had primarily been observed in benthic and subsurface settings, but not redox-stratified water columns. This may be due to the challenges that a pelagic lifestyle would pose for Zetaproteobacteria, given low Fe(II) concentrations in modern marine waters and the possibility that Fe oxyhydroxide biominerals could cause cells to sink. However, we recently cultivated Zetaproteobacteria from the Chesapeake Bay oxic–anoxic transition zone, suggesting that they can survive and contribute to biogeochemical cycling in a stratified estuary. Here we describe the isolation, characterization, and genomes of two new species, Mariprofundus aestuarium CP-5 and Mariprofundus ferrinatatus CP-8, which are the first Zetaproteobacteria isolates from a pelagic environment. We looked for adaptations enabling strains CP-5 and CP-8 to overcome the challenges of living in a low Fe redoxcline with frequent O2 fluctuations due to tidal mixing. We found that the CP strains produce distinctive dreadlock-like Fe oxyhydroxide structures that are easily shed, which would help cells maintain suspension in the water column. These oxides are by-products of Fe(II) oxidation, likely catalyzed by the putative Fe(II) oxidase encoded by the cyc2 gene, present in both CP-5 and CP-8 genomes; the consistent presence of cyc2 in all microaerophilic FeOB and other FeOB genomes supports its putative role in Fe(II) oxidation. The CP strains also have two gene clusters associated with biofilm formation (Wsp system and the Widespread Colonization Island) that are absent or rare in other Zetaproteobacteria. We propose that biofilm formation enables the CP strains to attach to FeS particles and form flocs, an advantageous strategy for scavenging Fe(II) and developing low [O2] microenvironments within more oxygenated waters. However, the CP strains appear to be adapted to somewhat higher concentrations of O2, as indicated by the presence of genes encoding aa3-type cytochrome c oxidases, but not the cbb3-type found in all other Zetaproteobacteria isolate genomes. Overall, our results reveal adaptations for life in a physically dynamic, low Fe(II) water column, suggesting that niche-specific strategies can enable Zetaproteobacteria to live in any environment with Fe(II).
机译:化学营养型铁氧化细菌(FeOB)在理论上可以居住在Fe(II)和O2(或硝酸盐)共存的任何环境中。直到最近,海洋铁氧化的Zetaproteobacteria细菌主要在底栖和地下环境中观察到,但还没有在氧化还原分层的水柱中观察到。鉴于现代海水中Fe(II)的浓度低以及羟基氧化铁生物矿物质可能导致细胞下沉的可能性,这可能是由于上层生活方式对Zetaproteobacteria构成的挑战所致。但是,我们最近在切萨皮克湾有氧-缺氧过渡带培养了轮状细菌,这表明它们可以生存并有助于在分层河口中进行生物地球化学循环。在这里,我们描述了两个新物种的分离,鉴定和基因组,即马里氏河口鱼类CP-5和马里氏河藻CP-8,它们是从远洋环境中分离出来的第一个Zetaproteobacteria细菌。我们寻找能够使菌株CP-5和CP-8适应气候变化的挑战,以克服由于潮汐混合而导致O2频繁波动的低铁氧化还原茶碱所带来的挑战。我们发现CP菌株产生独特的长辫状铁羟基氧化物结构,这些结构很容易脱落,这将有助于细胞保持在水柱中的悬浮。这些氧化物是Fe(II)氧化的副产物,可能由cyc2基因编码的推定Fe(II)氧化酶催化,同时存在于CP-5和CP-8基因组中。 cyc2在所有微需氧的FeOB和其他FeOB基因组中的一致存在支持了其在Fe(II)氧化中的假定作用。 CP菌株还具有两个与生物膜形成相关的基因簇(Wsp系统和广泛定植岛),而其他Zetaproteobacteria则不存在或罕见。我们提出生物膜的形成使CP菌株能够附着到FeS颗粒上并形成絮凝物,这是一种在更多含氧水中清除Fe(II)和发展低[O2]微环境的有利策略。但是,CP菌株似乎适应了较高的O2浓度,这是由编码aa3型细胞色素c氧化酶的基因的存在所表明的,而不是在所有其他Zetaproteobacteria分离基因组中发现的cbb3型。总体而言,我们的结果显示了在动态动态的低Fe(II)水柱中对生命的适应性,这表明利基特有的策略可使Zetaproteobacteria能够在任何含有Fe(II)的环境中生活。

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