Aitken M D, Stringfellow W T, Nagel R D, Kazunga C, Chen S H
Department of Environmental Sciences and Engineering, School of Public Health, University of North Carolina, Chapel Hill 27599-7400, USA.
Can J Microbiol. 1998 Aug;44(8):743-52.
Ten bacterial strains were isolated from seven contaminated soils by enrichment with phenanthrene as the sole carbon source. These isolates and another phenanthrene-degrading strain were examined for various characteristics related to phenanthrene degradation and their ability to metabolize 12 other polycyclic aromatic hydrocarbons (PAH), ranging in size from two to five rings, after growth in the presence of phenanthrene. Fatty acid methyl ester analysis indicated that at least five genera (Agrobacterium, Bacillus, Burkholderia, Pseudomonas, and Sphingomonas) and at least three species of Pseudomonas were represented in this collection. All of the strains oxidized phenanthrene according to Michaelis-Menten kinetics, with half-saturation coefficients well below the aqueous solubility of phenanthrene in all cases. All but one of the strains oxidized 1-hydroxy-2-naphthoate following growth on phenanthrene, and all oxidized at least one downstream intermediate from either or both of the known phenanthrene degradation pathways. All of the isolates could metabolize (oxidize, mineralize, or remove from solution) a broad range of PAH, although the exact range and extent of metabolism for a given substrate were unique to the particular isolate. Benz[a]anthracene, chrysene, and benzo[a]pyrene were each mineralized by eight of the strains, while pyrene was not mineralized by any. Pyrene was, however, removed from solution by all of the isolates, and the presence of at least one significant metabolite from pyrene was observed by radiochromatography for the five strains in which such metabolites were sought. Our results support earlier indications that the mineralization of pyrene by bacteria may require unique metabolic capabilities that do not appear to overlap with the determinants for mineralization of phenanthrene or other high molecular weight PAH.
通过以菲作为唯一碳源进行富集培养,从7份污染土壤中分离出了10株细菌菌株。在菲存在的条件下生长后,对这些分离菌株以及另一株菲降解菌株进行了与菲降解相关的各种特性检测,以及它们代谢其他12种多环芳烃(PAH)的能力检测,这些多环芳烃的环数从2环到5环不等。脂肪酸甲酯分析表明,该菌株集合中至少代表了5个属(农杆菌属、芽孢杆菌属、伯克霍尔德菌属、假单胞菌属和鞘氨醇单胞菌属)以及至少3种假单胞菌。所有菌株均按照米氏动力学氧化菲,在所有情况下,半饱和系数均远低于菲在水中的溶解度。除1株菌株外,所有菌株在以菲为碳源生长后均能氧化1-羟基-2-萘甲酸,并且所有菌株均能氧化已知菲降解途径中任一条或两条途径的至少一种下游中间体。所有分离菌株都能代谢(氧化、矿化或从溶液中去除)多种PAH,尽管给定底物的具体代谢范围和程度因特定分离菌株而异。苯并[a]蒽、屈和苯并[a]芘分别被8株菌株矿化,而芘未被任何菌株矿化。然而,所有分离菌株都能将芘从溶液中去除,并且通过放射色谱法在5株寻找芘显著代谢物的菌株中观察到了至少一种芘的重要代谢物。我们的结果支持了早期的迹象,即细菌对芘的矿化可能需要独特的代谢能力,这些能力似乎与菲或其他高分子量PAH的矿化决定因素不重叠。