1996
DOI: 10.1111/j.1574-6968.1996.tb08612.x
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Anaerobic degradation of benzene in BTX mixtures dependent on sulfate reduction

Abstract: Enrichment cultures from marine sediments mineralized benzene while using sulfate as the terminal electron acceptor. Parallel cultures using river marsh sediment displayed no activity. Mineralization was confirmed by release of 14CO2 from radiolabeled benzene. The dependence on sulfate reduction was demonstrated by stoichiometric balances and the use of specific inhibitors. This work supports recent observations that anaerobic benzene degradation takes place coupled to sulfate reduction.

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Cited by 67 publications
(47 citation statements)
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References 12 publications
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“…The first aromatics-oxidizing, sulfate-reducing isolate from Guaymas Basin sediments, Desulfothermus naphthae strain TD3, grows optimally between 55 and 65°C, and couples the oxidation of C 6 –C 16 alkanes and 3-methyloctane to sulfate reduction, although its specific alkane activation and degradation mechanism remains unknown (Rüter et al, 1994; Ehrenreich, 1996). Shortly after the isolation of TD3, a benzene-utilizing enrichment culture was obtained from Guaymas sediments (Phelps et al, 1996), which contained phylotypes that affiliate with members of the Desulfobacterium anilini and Desulfobacter clusters (Phelps et al, 1998); one of these Desulfobacterium phylotypes (SB-21) is possibly involved in benzene activation (Oka et al, 2008). Although benzoate was detected as an intermediate in this enrichment culture, the source of the carboxyl group remains unidentified (Phelps et al, 2001).…”
Section: High-temperature Hydrocarbon Oxidationmentioning
confidence: 99%
“…The first aromatics-oxidizing, sulfate-reducing isolate from Guaymas Basin sediments, Desulfothermus naphthae strain TD3, grows optimally between 55 and 65°C, and couples the oxidation of C 6 –C 16 alkanes and 3-methyloctane to sulfate reduction, although its specific alkane activation and degradation mechanism remains unknown (Rüter et al, 1994; Ehrenreich, 1996). Shortly after the isolation of TD3, a benzene-utilizing enrichment culture was obtained from Guaymas sediments (Phelps et al, 1996), which contained phylotypes that affiliate with members of the Desulfobacterium anilini and Desulfobacter clusters (Phelps et al, 1998); one of these Desulfobacterium phylotypes (SB-21) is possibly involved in benzene activation (Oka et al, 2008). Although benzoate was detected as an intermediate in this enrichment culture, the source of the carboxyl group remains unidentified (Phelps et al, 2001).…”
Section: High-temperature Hydrocarbon Oxidationmentioning
confidence: 99%
“…Benzene mineralization to carbon dioxide has been reported under methanogenic (Grbic-Galic and Vogel, 1987;Kazumi et al, 1997;Weiner and Lovley, 1998), sulphidogenic (Edwards and Grbic-Galic, 1992;Lovley et al, 1995;Phelps et al, 1996;Kazumi et al, 1997), iron-reducing (Lovley et al, 1994;Kazumi et al, 1997;Anderson et al, 1998) and nitrate-reducing (Major et al, 1988;Burland and Edwards, 1999) conditions. Although uncommon, benzene mineralization has recently been demonstrated by several groups of researchers.…”
Section: Introductionmentioning
confidence: 99%
“…Dentre as três espécies químicas em estudo, o benzeno costuma ser considerado o mais resistente frente aos processos de remediação convencionais 28 . Por este motivo foi utilizado como substrato modelo em todos os estudos preliminares de otimização e caracterização dos processos oxidativos propostos neste trabalho.…”
Section: Resultados E Discussão Degradação Fotoquímica De Benzenounclassified