Pacific Northwest Laboratory, P.O. Box 999, Richland, Washington 99352.
Appl Environ Microbiol. 1991 Mar;57(3):796-803. doi: 10.1128/aem.57.3.796-803.1991.
A bacterium, designated F199, utilized toluene, naphthalene, dibenzothiophene, salicylate, benzoate, p-cresol, and all isomers of xylene as a sole carbon and energy source. This bacterium was isolated from Middendorf sediments, a Cretaceous age formation that underlies the Southeast Coastal Plain in South Carolina, at a depth of approximately 410 m. F199 is a gram-positive, irregular-shaped bacterium that has a varied cell morphology that is dependent on culture medium type and growth stage. F199 required microaerobic conditions (40 to 80 muM O(2)) for growth on hydrocarbons, glucose, acetate, and lactate in mineral salts medium but not for growth on rich media. [C]naphthalene mineralization by F199 was induced by either naphthalene or toulene; however, [C]toluene mineralization by this strain was induced by toluene but not naphthalene. F199 was also found to harbor two plasmids larger than 100 kb. Restricted F199 plasmid and genomic DNA did not hybridize with toluene (pWW0) or naphthalene (NAH7) catabolic plasmid DNA probes. The presence in the Middendorf formation of bacteria with the capacity for degrading a variety of aromatic compounds suggests that indigenous microorganisms may have potential for in situ degradation of organic contaminants.
一种名为 F199 的细菌可以利用甲苯、萘、二苯并噻吩、水杨酸、苯甲酸、对甲酚和二甲苯的所有异构体作为唯一的碳源和能源。该细菌是从米多芬沉积物中分离出来的,米多芬是一种白垩纪地层,位于南卡罗来纳州东南沿海平原之下,深度约为 410 米。F199 是一种革兰氏阳性、不规则形状的细菌,其细胞形态多样,取决于培养基类型和生长阶段。F199 在矿物盐培养基上生长需要微需氧条件(40 至 80 μM O(2)),但在丰富的培养基上生长不需要。F199 可以诱导萘或甲苯矿化[C]萘,但该菌株诱导[C]甲苯矿化需要甲苯而不是萘。还发现 F199 携带两个大于 100 kb 的质粒。限制 F199 质粒和基因组 DNA 与甲苯 (pWW0) 或萘 (NAH7) 代谢质粒 DNA 探针不杂交。在米多芬地层中存在能够降解多种芳香族化合物的细菌,这表明土著微生物可能具有原位降解有机污染物的潜力。