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Two-Stage Mineralization of Phenanthrene by Estuarine Enrichment Cultures

机译:河口富集培养的菲的两阶段矿化作用

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The polycyclic aromatic hydrocarbon phenanthrene was mineralized in two stages by soil, estuarine water, and sediment microbial populations. At high concentrations, phenanthrene was degraded, with the concomitant production of biomass and accumulation of Folin-Ciocalteau-reactive aromatic intermediates. Subsequent consumption of these intermediates resulted in a secondary increase in biomass. Analysis of intermediates by high-performance liquid chromatography, thin-layer chromatography, and UV absorption spectrometry showed 1-hydroxy-2-naphthoic acid (1H2NA) to be the predominant product. A less pronounced two-stage mineralization pattern was also observed by monitoring 14CO2 production from low concentrations (0.5 mg liter?1) of radiolabeled phenanthrene. Here, mineralization of 14C-labeled 1H2NA could explain the incremental 14CO2 produced during the later part of the incubations. Accumulation of 1H2NA by isolates obtained from enrichments was dependent on the initial phenanthrene concentration. The production of metabolites during polycyclic aromatic hydrocarbon biodegradation is discussed with regard to its possible adaptive significance and its methodological implications.
机译:多环芳烃菲在两个阶段中被土壤,河口水和沉积物微生物种群矿化。在高浓度下,菲被降解,随之而来的是生物量的产生和福林-乔卡蒂奥-反应性芳族中间体的积累。这些中间体的后续消耗导致生物量的二次增加。通过高效液相色谱法,薄层色谱法和紫外吸收光谱法对中间体进行分析,结果显示1-羟基-2-萘甲酸(1H2NA)是主要产物。通过监测低浓度(0.5 mg升?1)的放射性同位素菲产生的14CO2产量,也观察到不太明显的两阶段矿化模式。在这里,14C标记的1H2NA的矿化可以解释在孵育后期产生的增量14CO2。从浓缩物中分离出的1H2NA的积累取决于初始菲的浓度。讨论了多环芳烃生物降解过程中代谢产物的产生及其可能的适应性意义和方法学意义。

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