“…Whereas in oxic environments, lower chlorinated anilines can be transformed to chlorocatechols and subsequently used as carbon and nitrogen source by a variety of microorganisms, , little is known about their transformation in anoxic environments. Anaerobic transformation was observed in methanogenic aquifers and aquifer slurries, ,− flooded soils, and estuarine sediments; the responsible organisms, however, were not identified. In mixed consortia, different dehalogenation pathways were observed: in anaerobic enrichment cultures with estuarine sediments as an inoculum, pentachloroaniline (PeCA) was converted to 2,3,4,5-tetrachloroaniline (2,3,4,5-TeCA), i.e., via ortho -dechlorination.…”