The isolated soil bacteria Acinetobacter strain BEM2 is able to utilize som
e xenobiotic aromatic compounds as a carbon source. In this study the metab
olism of 4-hydroxybenzoate (4-HBA) by strain BEM2 was characterized. Degrad
ation involved a meta-cleavage pathway yielding 3,4-dihydroxybenzoate (3,4-
DHBA) as an intermediate and CO2 as the principal product from the C atoms
in the aromatic ring. 4-HBA uptake was studied, and the kinetic parameters
were determined. The uptake was shown to be directly coupled to ATP hydroly
sis and its synthesis, according to the Mitchell chemiosmotic hypothesis.