Arthrobacter chlorophenolicus A6, a previously described 4-chlorophenol-degrading strain, was found to degrade 4-chlorophenol via hydroxyquinol, which is a novel route for aerobic microbial degradation of this compound. In addition, 10 open reading frames exhibiting sequence similarity to genes encoding enzymes involved in chlorophenol degradation were cloned and designated part of a chlorophenol degradation gene cluster (cph genes). Several of the open reading frames appeared to encode enzymes with similar functions; these open reading frames included two genes, cphA-I and cphA-II, which were shown to encode functional hydroxyquinol 1,2-dioxygenases. Disruption of the cphA-I gene yielded a mutant that exhibited negligible growth on 4-chlorophenol, thereby linking the cph gene cluster to functional catabolism of 4-chlorophenol in A. chlorophenolicus A6. The presence of a resolvase pseudogene in the cph gene cluster together with analyses of the G؉C content and codon bias of flanking genes suggested that horizontal gene transfer was involved in assembly of the gene cluster during evolution of the ability of the strain to grow on 4-chlorophenol.Arthrobacter chlorophenolicus A6 is a gram-positive actinobacterium that was previously isolated from a soil slurry enriched with increasing concentrations of 4-chlorophenol (4-CP) (28). This bacterium can degrade unusually high concentrations of 4-CP (up to 2.7 mM) and other p-substituted phenols, such as 4-nitrophenol and 4-bromophenol (28). In addition, A. chlorophenolicus A6 can degrade 4-CP at low temperatures (5°C) and during temperature fluctuations between 28°C and 5°C (3). Strain A6 was previously tagged with marker genes encoding the green fluorescent protein (gfp) or firefly luciferase (luc) in order to specifically monitor its ability to survive in nonsterile soil as it degraded 4-CP (9). The tagged cells survived well and were metabolically active in soil contaminated with 4-CP (9, 12). A larger fraction of the cell population remained viable after incubation in soil at 5°C than after incubation in soil at 28°C (4).There have been several reports of 4-CP degradation in other bacteria, but none of these bacteria have been shown to degrade concentrations of 4-CP as high as those degraded by A. chlorophenolicus A6. Successful mineralization of 4-CP by bacteria is usually accomplished by the oxidation of 4-CP to 4-chlorocatechol, followed by ortho cleavage of the aromatic ring. After ring cleavage, the chlorine is removed and the carbon skeleton is transformed into products that are assimilated into the central metabolism of the cell. By contrast, two strains belonging to the actinobacterium group, Arthrobacter ureafaciens CPR706 (5) and Nocardioides sp. strain NSP41 (8), were reported to transform 4-CP into hydroquinone instead of 4-chlorocatechol. However, the degradation pathways in these strains have not been described further.The aim of the present study was to elucidate the biochemistry and genetics of 4-chlorophenol degradation in A. chlorophenolicus A6. Our...