Fluorinated compounds are known to be more resistant to microbial degradation than other halogenated chemicals. A microbial consortium capable of aerobic biodegradation of fluorobenzene (FB) as the sole source of carbon and energy was isolated by selective enrichment from sediments collected in a drain near an industrial site. A combination of three microbial strains recovered from the enriched consortium was shown to be necessary for complete FB mineralization. Two of the strains (F1 and F3) were classified by 16S rRNA analysis as belonging to the Sphingobacterium/Flavobacterium group, while the third (F4) falls in the -Proteobacteria group, clustering with Alcaligenes species. Strain F4 was consistently found in the liquid cultures in a much greater proportion than strains F1 and F3 (86:8:6 for F4, F1, and F3, respectively). Stoichiometric release of fluoride ions was measured in batch and fed-batch cultures. In batch cultures, the consortium was able to use FB up to concentrations of 400 mg liter ؊1 and was able to utilize a range of other organic compounds, including 4-fluorophenol and 4-fluorobenzoate. To our knowledge this is the first time biodegradation of FB as a sole carbon source has been reported.The advances in organic synthesis have led to the introduction of numerous new organic compounds into the environment, whose susceptibilities to biotreatment processes are unknown. Fluoroaromatics are being increasingly used in a wide range of agrochemical and pharmaceutical products, due to the need to find environmentally acceptable alternatives to chlorinated compounds (17). The diversity of structures and the chemical inertness of many halogenated organics pose particular problems and challenges for microbial degradation (10). Some authors propose that the recalcitrance of a halogenated organic compound usually becomes greater with the increase of the electronegativity of the substituents; thus, the recalcitrance of F-C is greater than that of Cl-C, Br-C, and I-C (9).The biodegradation of a vast range of halogenated aromatic compounds, especially chlorinated compounds, has been described (13,22), but scant information is available on the metabolic and cometabolic fate of fluorinated aromatic compounds in bacteria. Examples of biodegradation of fluorinated compounds most commonly found in the literature involve fluorobenzoic acids (7,15,20,21,24) and fluorophenols (1, 2, 23). Although degradation under aerobic conditions is usually reported, anaerobic degradation of fluorobenzoates under denitrifying conditions has also been reported (26). The existence of various metabolic pathways, some of which may lead to the formation of inhibitor metabolites, has been reported (15,24,25). In some cases, as in the degradation of fluoroacetate, a specific enzyme is responsible for the cleavage of the C-F bond (12). Studies on the metabolism of 2-flurobenzoate have shown that cleavage of the C-F bond occurs incidentally during oxygenase attack on the aromatic ring (20). It has been reported that biodegradation of fluo...