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Phylogeny of cyclic nitramine-degrading psychrophilic bacteria in marine sediment and their potential role in the natural attenuation of explosives

机译:海洋沉积物中降解环硝胺的嗜冷细菌的系统发生及其在炸药自然衰减中的潜在作用

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摘要

Previously we reported on in situ mineralization of cyclic nitramine explosives including hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) and octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX) in marine sediment from Halifax Harbour. In the present study, we isolated several novel psychrophilic bacteria from the sediment with optimal growth temperature at 10 or 15 degreeC. Phylogenetic analysis of their 16S rRNA genes identified the isolates as members of the gamma and delta subdivisions of Proteobacteria, Fusobacteria and Clostridiales. The isolates mineralized 3.7-45.2% of RDX (92 muM) in 82 days of incubation at 10 degreeC under oxygen-limited or anaerobic conditions with the gamma subdivision isolates demonstrating the highest mineralization (45.2% of total C). Removal of RDX by all isolates was accompanied by the formation of all three nitroso derivatives, with the mono nitroso derivative (MNX) being the major one. Isolates of the delta proteobacteria and Fusobacteria removed HMX with concurrent formation of the mononitroso derivative (NO-HMX). Using resting cells of isolates of the gamma subdivision, methylenedinitramine (MEDINA) and 4-vitro-2,4-diazabutanal (NDAB) were detected, suggesting ring-cleavage following denitration of either RDX and/or its initially reduced product, MNX. These results clearly demonstrate that psychrophilic bacteria capable of degrading cyclic nitramines are present in the marine sediment, and might contribute to the in situ biodegradation and natural attenuation of the chemicals. Copyright 2004 Federation of European Microbiological Societies. Published by Elsevier B.V. All rights reserved.
机译:先前我们曾报道过环状硝胺炸药的原位矿化,包括六氢-1,3,5-三硝基-1,3,5-三嗪(RDX)和八氢-1,3,5,7-四硝基-1,3,5哈利法克斯港海洋沉积物中的7,7-四唑辛(HMX)。在本研究中,我们从沉积物中分离出了几种新型嗜冷细菌,其最佳生长温度为10或15摄氏度。对它们的16S rRNA基因进行系统进化分析,确定这些分离株是变形杆菌,梭菌和梭状芽胞杆菌的γ和δ细分的成员。在氧限制或厌氧条件下,在10摄氏度下孵育82天,γ分离菌在82天内培养时,使RDX的3.7-45.2%矿化(92μM),其中γ细分菌显示出最高的矿化度(占总C的45.2%)。所有分离物去除RDX时,都伴随着所有三种亚硝基衍生物的形成,其中主要是单亚硝基衍生物(MNX)。三角洲变形杆菌和融合细菌的分离物去除了HMX,同时形成了亚硝基衍生物(NO-HMX)。使用γ-细分的分离株的静息细胞,检测到了亚甲基二甲基苯乙胺(MEDINA)和4-体外-2,4-二氮杂丁醛(NDAB),这表明RDX和/或其最初还原的产物MNX脱硝后发生了环裂解。这些结果清楚地表明,海洋沉积物中存在能够降解环状硝胺的嗜冷细菌,并且可能有助于化学物质的原位生物降解和自然衰减。版权所有2004欧洲微生物学会联合会。由Elsevier B.V.发布。保留所有权利。

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