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Description of Toluene Inhibition of Methyl Bromide Biodegradation in Seawater and Isolation of a Marine Toluene Oxidizer That Degrades Methyl Bromide

机译:甲苯抑制海水中甲基溴生物降解的描述和分离降解甲基溴的海洋甲苯氧化剂

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摘要

Methyl bromide (CH3Br) and methyl chloride (CH3Cl) are important precursors for destruction of stratospheric ozone, and oceanic uptake is an important component of the biogeochemical cycle of these methyl halides. In an effort to identify and characterize the organisms mediating halocarbon biodegradation, we surveyed the effect of potential cometabolic substrates on CH3Br biodegradation using a 13CH3Br incubation technique. Toluene (160 to 200 nM) clearly inhibited CH3Br and CH3Cl degradation in seawater samples from the North Atlantic, North Pacific, and Southern Oceans. Furthermore, a marine bacterium able to co-oxidize CH3Br while growing on toluene was isolated from subtropical Western Atlantic seawater. The bacterium, Oxy6, was also able to oxidize o-xylene and the xylene monooxygenase (XMO) pathway intermediate 3-methylcatechol. Patterns of substrate oxidation, lack of acetylene inhibition, and the inability of the toluene 4-monooxygenase (T4MO)-containing bacterium Pseudomonas mendocina KR1 to degrade CH3Br ruled out participation of the T4MO pathway in Oxy6. Oxy6 also oxidized a variety of toluene (TOL) pathway intermediates such as benzyl alcohol, benzylaldehyde, benzoate, and catechol, but the inability of Pseudomonas putida mt-2 to degrade CH3Br suggested that the TOL pathway might not be responsible for CH3Br biodegradation. Molecular phylogenetic analysis identified Oxy6 to be a member of the family Sphingomonadaceae related to species within the Porphyrobacter genus. Although some Sphingomonadaceae can degrade a variety of xenobiotic compounds, this appears to be the first report of CH3Br degradation for this class of organism. The widespread inhibitory effect of toluene on natural seawater samples and the metabolic capabilities of Oxy6 indicate a possible link between aromatic hydrocarbon utilization and the biogeochemical cycle of methyl halides.
机译:甲基溴(CH3Br)和甲基氯(CH3Cl)是破坏平流层臭氧的重要前体,海洋吸收是这些甲基卤化物生物地球化学循环的重要组成部分。为了确定和表征介导卤化碳生物降解的生物,我们使用13CH3Br孵育技术调查了潜在的可代谢物质对CH3Br生物降解的影响。甲苯(160至200 nM)明显抑制了北大西洋,北太平洋和南大洋的海水样品中的CH3Br和CH3Cl降解。此外,从亚热带西大西洋海水中分离出了一种能够在甲苯上生长同时共氧化CH3Br的海洋细菌。细菌Oxy6也能够氧化邻二甲苯和3-甲基邻苯二酚中间的二甲苯单加氧酶(XMO)途径。底物氧化的模式,乙炔缺乏抑制和含甲苯4-单加氧酶(T4MO)的细菌Pseudomonas mendocina KR1不能降解CH3Br排除了T4MO途径参与Oxy6。 Oxy6还氧化了多种甲苯(TOL)途径中间体,例如苯甲醇,苄醛,苯甲酸酯和邻苯二酚,但恶臭假单胞菌mt-2不能降解CH3Br提示TOL途径可能与CH3Br的生物降解无关。分子系统发育分析表明,Oxy6是Spphygomonadaceae家族成员,与卟啉菌属中的物种有关。尽管某些Sphingomonadaceae可以降解多种异生物化合物,但这似乎是此类生物对CH3Br降解的首次报道。甲苯对天然海水样品的广泛抑制作用和Oxy6的代谢能力表明芳烃利用与甲基卤化物的生物地球化学循环之间可能存在联系。

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