Observations on the bacterial oxidation of chlorophenoxyacetic acids

Summary Three bacterial strains, one ofF. peregrinum (Stapp and Spicher) and two Achromobacter strains, have been isolated from soil and shown to decompose either 2,4-D, MCPA orp-chlorophenoxyacetic acid. Aerobic conditions are essential for the bacterial decomposition of 2,4-D. Pretreatment of soil with one of the three chlorophenoxyacetic acids accelerated the rate of breakdown of either of the other two. In a liquid medium, growth of theF. peregrinum strain caused breakdown of 2,4-D and liberated 76% of the chlorine in 2,4-D in ionic form. An unknown acidic substance, colourless in acid solution but forming a yellow sodium salt has been detected in cultures ofF. peregrinum or an MCPA-decomposing Achromobacter strain growing inp-chlorophenoxyacetate medium. The bacterial oxidation of chlorophenoxyacetic acid herbicides was attributed to adaptive enzyme formation. Respiration experiments showed that the oxidation of 2,4-D or ofp-chlorophenoxyacetic acid is incomplete. 4-Chloro-2-hydroxyphenoxyacetic acid and 4-chlorocatechol may be metabolic intermediates in the case ofp-chlorophenoxyacetic acid, but no intermediary metabolites have as yet been established for 2,4-D.