Degradation of ioxynil to CO2 in soil

Degradation of ioxynil (4-hydroxy-3,5-diiodobenzonitrile) to CO₂ was detected in a clay loam, high organic matter content soil. The majority of radioactivity was recovered as ¹⁴CO₂ from both ring-labeled and cyano-labeled ioxynil; however, ¹⁴CO₂ was always released from cyano-labeled ioxynil at a much faster initial rate. No ¹⁴CO₂ was released in treated sterile soil, either aerobically or anaerobically. Production of ¹⁴CO₂ from cyanolabeled and ring-labeled ioxynil was greatly inhibited by HgCl₂ (10^?5M), and p-chloromercuribenzoate (5 × 10^?5M), but slightly inhibited by ferricyanide (10^?4M). No ¹⁴CO₂ was evolved from ring-labeled ioxynil under anaerobic conditions. These observations indicated that the degradation of ioxynil to CO₂ in soil was a microbial action and was oxygen dependent. This is consistent with the known mechanism of oxygenases in degrading benzene rings. Anaerobically, a small amount of ¹⁴CO₂ was released from cyano-labeled ioxynil. Thin-layer chromatographic analyses of the culture supernatant revealed that 3,5-diiodo-4-hydroxybenzamide and 3,5-diiodo-4-hydroxybenzoic acid were intermediate metabolites.