The anaerobic degradation of benzene is of interest because of its environmental significance (
25,
38,
63) and because the mechanisms for the initial metabolic attack on such a stable molecule are expected to be novel (
14,
22,
63,
66). The lack of pure cultures in which it can definitely be stated that benzene is metabolized without molecular oxygen has greatly stymied the study of this process.
The only previously described pure cultures suggested to anaerobically degrade benzene have used nitrate or chlorate as an electron acceptor (
21,
32,
62). Anaerobic benzene degradation has been studied in detail in one of these organisms,
Dechloromonas aromatica (
15,
16,
21,
55). One of the most surprising findings in the study of
D. aromatica is that it lacks all of the otherwise highly conserved genes involved in the anaerobic degradation of monoaromatic compounds (
55), such as benzoate and phenol, which are otherwise found in all
Bacteria (
13) and
Archaea (
30) that can metabolize these compounds. In addition, it appears that oxygen incorporated into the benzene ring does not come from water as would be expected for anaerobic benzene degradation (
15). These results have lead to the suggestion that
D. aromatica might activate benzene with oxygen produced intracellularly during growth on nitrate (
55,
63).
However, benzene is clearly degraded under anoxic conditions in natural communities and enrichment cultures. 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–
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. For example, different species of Gram-positive bacteria and
Delta- and/or
Epsilonproteobacteria have been associated with benzene degradation in sulfate-reducing (
1,
52), Fe(III)-reducing (
37), and methanogenic (
60) enrichments. Archaeal species have also been detected in sulfate-reducing enrichments (
7).
Multiple pathways for anaerobic benzene degradation have been proposed, and different microorganisms may employ alternate pathways (
22,
46). In early studies with methanogenic benzene-degrading enrichment cultures, phenol and cyclohexanone were detected as intermediates, leading to the suggestion that first benzene was hydroxylated to phenol and then the ring was reduced to produce cyclohexanone (
26). Detection of phenol in sulfate-reducing enrichments also supported the hydroxylation pathway (
12). However, the potential for abiotic production of phenol from benzene during sampling has demonstrated that evidence beyond mere detection of phenol may be required before phenol can be designated an intermediate (
1,
36). Production of [
13C]toluene and [
13C]benzoate in methanogenic and nitrate-reducing enrichments metabolizing [
13C]benzene suggested that benzene was initially methylated, followed by transformation of toluene to benzoate (
59). It has also been proposed that benzene may be directly carboxylated to benzoate, based on the production of benzoate in enrichment cultures (
1,
36), and a putative carboxylase was detected in protein extracts from an Fe(III)-reducing enrichment culture during growth on benzene but not phenol or benzoate (
2).
The vast majority of studies on the anaerobic degradation of aromatic compounds have focused on mesophilic bacteria. However, it was previously demonstrated that the hyperthermophilic archaeon
Ferroglobus placidus is able to anaerobically oxidize benzoate and phenol with Fe(III) as the electron acceptor (
30,
58). The
F. placidus genes for benzoate and phenol metabolism are homologous to those found in mesophilic bacteria, many of the genes are arranged in clusters similar to those found in bacteria, and the expression of the appropriate genes is specifically increased during growth on benzoate or phenol (
30). A unique feature of benzoate metabolism in
F. placidus is that it appears to use a ATP-consuming class I benzoyl coenzyme A (benzoyl-CoA) reductase, similar to those found in facultative bacteria, rather than the ATP-independent class II benzoyl-CoA reductase found in all other strict anaerobes (
30).
Here we report that
F. placidus is capable of anaerobic growth on benzene with Fe(III) serving as the electron acceptor. Gene expression patterns and metabolite data suggest that benzene is converted directly to benzoate and that phenol is not an important intermediate. This study also identifies a putative carboxylase protein involved in benzene activation that is homologous to a protein identified by proteomic and genomic analysis of benzene degradation in an Fe(III)-reducing enrichment culture (
2).