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A novel bacterial sulfur oxidation pathway provides a new link between the cycles of organic and inorganic sulfur compounds

机译:一种新颖的细菌硫氧化途径为有机和无机硫化合物的循环之间提供了新的联系

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摘要

Dimethylsulfide (DMS) plays a globally significant role in carbon and sulfur cycling and impacts Earth’s climate because its oxidation products serve as nuclei for cloud formation. While the initial steps of aerobic DMS degradation and the fate of its carbon atoms are reasonably well documented, oxidation of the contained sulfur is largely unexplored. Here, we identified a novel pathway of sulfur compound oxidation in the ubiquitously occurring DMS-degrader Hyphomicrobium denitrificans XT that links the oxidation of the volatile organosulfur compound with that of the inorganic sulfur compound thiosulfate. DMS is first transformed to methanethiol from which sulfide is released and fully oxidized to sulfate. Comparative proteomics indicated thiosulfate as an intermediate of this pathway and pointed at a heterodisulfide reductase (Hdr)-like system acting as a sulfur-oxidizing entity. Indeed, marker exchange mutagenesis of hdr-like genes disrupted the ability of H. denitrificans to metabolize DMS and also prevented formation of sulfate from thiosulfate provided as an additional electron source during chemoorganoheterotrophic growth. Complementation with the hdr-like genes under a constitutive promoter rescued the phenotype on thiosulfate as well as on DMS. The production of sulfate from an organosulfur precursor via the Hdr-like system is previously undocumented and provides a new shunt in the biogeochemical sulfur cycle. Furthermore, our findings fill a long-standing knowledge gap in microbial dissimilatory sulfur metabolism because the Hdr-like pathway is abundant not only in chemoheterotrophs, but also in a wide range of chemo- and photolithoautotrophic sulfur oxidizers acting as key players in global sulfur cycling.
机译:二甲基硫醚(DMS)在碳和硫的循环中起着全球性的重要作用,并影响地球的气候,因为其氧化产物可作为形成云的核。尽管有氧DMS降解的初始步骤及其碳原子的命运已得到充分的文献证明,但所含硫的氧化在很大程度上尚未得到探索。在这里,我们确定了普遍存在的DMS降解物次硝化双氧菌X T 中硫化合物氧化的新途径,该途径将挥发性有机硫化合物的氧化与无机硫化合物硫代硫酸盐的氧化联系在一起。首先将DMS转化为甲硫醇,然后从其中释放出硫化物并完全氧化为硫酸盐。比较蛋白质组学表明硫代硫酸盐是该途径的中间产物,并指向杂二硫键还原酶(Hdr)样系统,该系统充当硫氧化实体。实际上,hdr-样基因的标记交换诱变破坏了反硝化链霉菌代谢DMS的能力,还阻止了硫代硫酸盐在化学有机异养生长过程中作为额外电子源而形成的硫酸盐。在组成型启动子下与hdr-like基因的互补拯救了硫代硫酸盐以及DMS上的表型。以前没有文献记载通过类似Hdr的系统从有机硫前体生产硫酸盐,这为生物地球化学硫循环提供了新的分流方法。此外,我们的发现填补了微生物异化硫代谢中长期存在的知识空白,因为类似Hdr的途径不仅在化学异养菌中丰富,而且在作为全球硫循环的关键参与者的广泛的化学和光自养硫氧化剂中也很丰富。

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