Shields M S, Hooper S W, Sayler G S
J Bacteriol. 1985 Sep;163(3):882-9. doi: 10.1128/jb.163.3.882-889.1985.
Strains of Alcaligenes and Acinetobacter spp. were isolated from a mixed culture already proven to be proficient at complete mineralization of monohalogenated biphenyls. These strains were shown to harbor a 35 X 10(6)-dalton plasmid mediating a complete pathway for 4-chlorobiphenyl (4CB) oxidation. Subsequent plasmid curing of these bacteria resulted in the abolishment of the 4CB mineralization phenotype and loss of even early 4CB metabolism by Acinetobacter spp. Reestablishment of the Alcaligenes plasmid, denoted pSS50, in the cured Acinetobacter spp. via filter surface mating resulted in the restoration of 4CB mineralization abilities. 4CB mineralization, however, proved to be an unstable characteristic in some subcultured strains. Such loss was not found to coincide with any detectable alteration in plasmid size. Cultures capable of complete mineralization, as well as those limited to partial metabolism of 4CB, produced 4-chlorobenzoate as a metabolite. Demonstration of mineralization of a purified 14C-labeled chlorobenzoate showed it to be a true intermediate in 4CB mineralization. Unlike the mineralization capability, the ability to produce a metabolite has proven to be stable on subculture. These results indicate the occurrence of a novel plasmid, or evolved catabolic plasmid, that mediates the complete mineralization of 4CB.
从一种已被证明能完全矿化单卤代联苯的混合培养物中分离出了产碱杆菌属和不动杆菌属的菌株。这些菌株被证明含有一个35×10⁶道尔顿的质粒,该质粒介导了4-氯联苯(4CB)氧化的完整途径。随后对这些细菌进行质粒消除,导致4CB矿化表型消失,不动杆菌属甚至失去了早期4CB代谢能力。通过滤膜表面交配将产碱杆菌的质粒(命名为pSS50)重新导入已消除质粒的不动杆菌属中,导致4CB矿化能力得以恢复。然而,在一些传代培养的菌株中,4CB矿化被证明是一种不稳定的特性。这种丢失并未发现与质粒大小的任何可检测到的变化相一致。能够完全矿化的培养物以及那些仅限于4CB部分代谢的培养物,都产生4-氯苯甲酸作为代谢产物。对纯化的¹⁴C标记氯苯甲酸矿化的证明表明它是4CB矿化过程中的一个真正中间产物。与矿化能力不同,产生代谢产物的能力在传代培养中已被证明是稳定的。这些结果表明存在一种新型质粒,即进化的分解代谢质粒,它介导了4CB的完全矿化。