“…Benzene was anaerobically degraded in sediments coupled to the reduction of Fe(III) (4,10,43,44,53), Mn(IV) (61), sulfate (3,20,23,27,34,35,40,64), carbon dioxide (17,65), and graphite electrodes (67). Enrichment cultures capable of anaerobic oxidation of benzene with either sulfate (1,7,18,19,(49)(50)(51), carbon dioxide (26,54,59), or Fe(III) (11,31,37,53) as the electron acceptor have been described. A number of different species appear to be involved in benzene degradation in these enrichment cultures.…”