首页> 美国卫生研究院文献>Philosophical Transactions of the Royal Society B: Biological Sciences >Distribution of dehalogenation activity in subseafloor sediments of the Nankai Trough subduction zone
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Distribution of dehalogenation activity in subseafloor sediments of the Nankai Trough subduction zone

机译:南开海槽俯冲带海底沉积物中脱卤活性的分布

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摘要

Halogenated organic matter buried in marine subsurface sediment may serve as a source of electron acceptors for anaerobic respiration of subseafloor microbes. Detection of a diverse array of reductive dehalogenase-homologous (rdhA) genes suggests that subseafloor organohalide-respiring microbial communities may play significant ecological roles in the biogeochemical carbon and halogen cycle in the subseafloor biosphere. We report here the spatial distribution of dehalogenation activity in the Nankai Trough plate-subduction zone of the northwest Pacific off the Kii Peninsula of Japan. Incubation experiments with slurries of sediment collected at various depths and locations showed that degradation of several organohalides tested only occurred in the shallow sedimentary basin, down to 4.7 metres below the seafloor, despite detection of rdhA in the deeper sediments. We studied the phylogenetic diversity of the metabolically active microbes in positive enrichment cultures by extracting RNA, and found that Desulfuromonadales bacteria predominate. In addition, for the isolation of genes involved in the dehalogenation reaction, we performed a substrate-induced gene expression screening on DNA extracted from the enrichment cultures. Diverse DNA fragments were obtained and some of them showed best BLAST hit to known organohalide respirers such as Dehalococcoides, whereas no functionally known dehalogenation-related genes such as rdhA were found, indicating the need to improve the molecular approach to assess functional genes for organohalide respiration.
机译:埋在海洋地下沉积物中的卤化有机物可作为电子受体的来源,用于海底微生物的厌氧呼吸。对多种还原性脱卤化酶同源(rdhA)基因的检测表明,海底有机卤化物呼吸微生物群落可能在海底生物圈的生物地球化学碳和卤素循环中发挥重要的生态作用。我们在这里报告了日本纪伊半岛西北太平洋西北海南海海槽板块俯冲带中脱卤活性的空间分布。对在不同深度和位置收集的泥浆进行的孵化实验表明,尽管在较深的沉积物中检测到rdhA,但所测试的几种有机卤化物的降解仅发生在海床以下4.7米的浅沉积盆地中。我们通过提取RNA研究了正富集培养中代谢活性微生物的系统发育多样性,并发现Desulfuromonadales细菌占主导地位。另外,为了分离涉及脱卤反应的基因,我们对从富集培养物中提取的DNA进行了底物诱导的基因表达筛选。获得了不同的DNA片段,其中一些片段对已知的有机卤化物呼吸器(如Dehalococcoides)表现出最好的BLAST打击,而未找到功能上已知的与卤代反应相关的基因(如rdhA),这表明需要改进分子方法来评估有机卤化物呼吸的功能基因。

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