The microbial communities of in situ reactor columns degrading benzene with sulfate as an electron acceptor were analyzed based on clone libraries and terminal restriction fragment length polymorphism fingerprinting of PCR-amplified 16S rRNA genes. The columns were filled with either lava granules or sand particles and percolated with groundwater from a benzene-contaminated aquifer. The predominant organisms colonizing the lava granules were related to Magnetobacterium sp., followed by a phylotype affiliated to the genera Cryptanaerobacter/Pelotomaculum and several Deltaproteobacteria. From the sand-filled columns, a stable benzene-degrading consortium was established in sand-filled laboratory microcosms under sulfate-reducing conditions. It was composed of Delta- and Epsilonproteobacteria, Clostridia, Chloroflexi, Actinobacteria and Bacteroidetes. The most prominent phylotype of the consortium was related to the genus Sulfurovum, followed by Desulfovibrio sp. and the Cryptanaerobacter/Pelotomaculum phylotype. The proportion of the latter was similar in both communities and significantly increased after repeated benzene-spiking. During cultivation on aromatic substrates other than benzene, the Cryptanaerobacter/Pelotomaculum phylotype was outcompeted by other community members. Hence, this organism appears to be specific for benzene as a growth substrate and might play a key role in benzene degradation in both communities. Based on the possible functions of the community members and thermodynamic calculations, a functional model for syntrophic benzene degradation under sulfate-reducing conditions is proposed.

No abstract

Micro-organisms are known to degrade a wide range of toxic substances. How the environment shapes microbial communities in polluted ecosystems and thus influences degradation capabilities is not yet fully understood. In this study, we investigated microbial communities in a highly complex environment: the capillary fringe and subjacent sediments in a hydrocarbon-contaminated aquifer. Sixty sediment sections were analysed using terminal restriction fragment length polymorphism (T-RFLP) fingerprinting, cloning and sequencing of bacterial and archaeal 16S rRNA genes, complemented by chemical analyses of petroleum hydrocarbons, methane, oxygen and alternative terminal electron acceptors. Multivariate statistics revealed concentrations of contaminants and the position of the water table as significant factors shaping the microbial community composition. Micro-organisms with highest T-RFLP abundances were related to sulphate reducers belonging to the genus Desulfosporosinus, fermenting bacteria of the genera Sedimentibacter and Smithella, and aerobic hydrocarbon degraders of the genus Acidovorax. Furthermore, the acetoclastic methanogens Methanosaeta, and hydrogenotrophic methanogens Methanocella and Methanoregula were detected. Whereas sulphate and sulphate reducers prevail at the contamination source, the detection of methane, fermenting bacteria and methanogenic archaea further downstream points towards syntrophic hydrocarbon degradation.

Information on anaerobic phenol metabolism by physiological groups of bacteria other than nitrate reducers is scarce. We investigated phenol degradation in the strictly anaerobic iron-reducing deltaproteobacterium Geobacter metallireducens GS-15 using metabolite, transcriptome, proteome, and enzyme analyses. The results showed that the initial steps of phenol degradation are accomplished by phenylphosphate synthase (encoded by pps genes) and phenylphosphate carboxylase (encoded by ppc genes) as known from Thauera aromatica, but they also revealed some distinct differences. The pps-ppc gene cluster identified in the genome is functional, as shown by transcription analysis. In contrast to T. aromatica, transcription of the pps-and ppc-like genes was induced not only during growth on phenol, but also during growth on benzoate. In contrast, proteins were detected only during growth on phenol, suggesting the existence of a posttranscriptional regulation mechanism for these initial steps. Phenylphosphate synthase and phenylphosphate carboxylase activities were detected in cell extracts. The carboxylase does not catalyze an isotope exchange reaction between 14 CO 2 and 4-hydroxybenzoate, which is characteristic of the T. aromatica enzyme. Whereas the enzyme of T. aromatica is encoded by ppcABCD, the pps-ppc gene cluster of G. metallireducens contains only a ppcB homologue. Nearby, but oriented in the opposite direction, is a ppcD homologue that is transcribed during growth on phenol. Genome analysis did not reveal obvious homologues of ppcA and ppcC, leaving open the question of whether these genes are dispensable for phenylphosphate carboxylase activity in G. metallireducens or are quite different from the Thauera counterparts and located elsewhere in the genome.Anaerobic phenol degradation is best understood in the facultatively anaerobic denitrifier Thauera aromatica (DSM6984). In this strain, phenol is initially converted to phenylphosphate by phenylphosphate synthase (Pps) with concomitant hydrolysis of ATP (5, 16, 28) (Fig. 1A). The ␣-and ␤-subunits of Pps resemble the central and N-terminal parts of the phosphoenolpyruvate synthase, respectively. The ␤-subunit contains the ATP-binding moiety of the enzyme and is thought to transfer a diphosphoryl group to a conserved histidine residue in the ␣-subunit (23). There, orthophosphate is released and the ␤-phosphate group of ATP is transferred to phenol. Both subunits are therefore required for phosphorylation. The ␥-subunit is dispensable. However, its presence stimulates the reaction severalfold (28).In the next step, phenylphosphate is carboxylated by the action of phenylphosphate carboxylase (Ppc), yielding 4-hydroxybenzoate (4-OHB) (15,17,29). The ␦-subunit of the enzyme shows similarities to proteins of the hydrolase/phosphatase family (29). It was suggested to bind phenylphosphate and to catalyze its dephosphorylation, a reaction that is exergonic and virtually irreversible. The resulting phenolate anion is carboxylated by the core enzyme composed of ␣-, ␤-, an...

Two novel genes, rdpA and sdpA, encoding the enantiospecific ␣-ketoglutarate dependent dioxygenases catalyzing R,S-dichlorprop cleavage in Delftia acidovorans MC1 were identified. Significant similarities to other known genes were not detected, but their deduced amino acid sequences were similar to those of other ␣-ketoglutarate dioxygenases. RdpA showed 35% identity with TauD of Pseudomonas aeruginosa, and SdpA showed 37% identity with TfdA of Ralstonia eutropha JMP134. The functionally important amino acid sequence motif HX(D/E)X 23-26 (T/S)X 114-183 HX 10-13 R/K, which is highly conserved in group II ␣-ketoglutarate-dependent dioxygenases, was present in both dichlorprop-cleaving enzymes. Transposon mutagenesis of rdpA inactivated R-dichlorprop cleavage, indicating that it was a single-copy gene. Both rdpA and sdpA were located on the plasmid pMC1 that also carries the lower pathway genes. Sequencing of a 25.8-kb fragment showed that the dioxygenase genes were separated by a 13.6-kb region mainly comprising a Tn501-like transposon. Furthermore, two copies of a sequence similar to IS91-like elements were identified. Hybridization studies comparing the wild-type plasmid and that of the mutant unable to cleave dichlorprop showed that rdpA and sdpA were deleted, whereas the lower pathway genes were unaffected, and that deletion may be caused by genetic rearrangements of the IS91-like elements. Two other dichlorprop-degrading bacterial strains, Rhodoferax sp. strain P230 and Sphingobium herbicidovorans MH, were shown to carry rdpA genes of high similarity to rdpA from strain MC1, but sdpA was not detected. This suggested that rdpA gene products are involved in the degradation of R-dichlorprop in these strains.

Syntrophic mineralisation of benzene, as recently proposed for a sulphatereducing enrichment culture, was tested in product inhibition experiments with acetate and hydrogen, both putative intermediates of anaerobic benzene fermentation. Using [ 13 C 6 ]-benzene enabled tracking the inhibition of benzene mineralisation sensitively by analysis of 13 CO 2 . In noninhibited cultures, hydrogen was detected at partial pressures of 2.4 Â 10 À6 AE 1.5 Â 10 À6 atm. Acetate was detected at concentrations of 17 AE 2 mM. Spiking with 0.1 atm hydrogen produced a transient inhibitory effect on 13 CO 2 formation. In cultures spiked with higher amounts of hydrogen, benzene mineralisation did not restart after hydrogen consumption, possibly due to the toxic effects of the sulphide produced. An inhibitory effect was also observed when acetate was added to the cultures (0.3, 3.5 and 30 mM). Benzene mineralisation resumed after acetate was degraded to concentrations found in noninhibited cultures, indicating that acetate is another key intermediate in anaerobic benzene mineralisation. Although benzene mineralisation by a single sulphate reducer cannot be ruled out, our results strongly point to an involvement of syntrophic interactions in the process. Thermodynamic calculations revealed that, under in situ conditions, benzene fermentation to hydrogen and acetate yielded a free energy change of DG 0 = À 83.1 AE 5.6 kJ mol À1 . Benzene mineralisation ceased when DG 0 values declined below À 61.3 AE 5.3 kJ mol À1 in the presence of acetate, indicating that ATP-consuming reactions are involved in the pathway.

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The population genome of an uncultured bacterium assigned to the Campylobacterales (Epsilonproteobacteria) was reconstructed from a metagenome dataset obtained by whole-genome shotgun pyrosequencing. Genomic DNA was extracted from a sulfate-reducing, m-xylene-mineralizing enrichment culture isolated from groundwater of a benzene-contaminated sulfidic aquifer. The identical epsilonproteobacterial phylotype has previously been detected in toluene- or benzene-mineralizing, sulfate-reducing consortia enriched from the same site. Previous stable isotope probing (SIP) experiments with 13C6-labeled benzene suggested that this phylotype assimilates benzene-derived carbon in a syntrophic benzene-mineralizing consortium that uses sulfate as terminal electron acceptor. However, the type of energy metabolism and the ecophysiological function of this epsilonproteobacterium within aromatic hydrocarbon-degrading consortia and in the sulfidic aquifer are poorly understood. Annotation of the epsilonproteobacterial population genome suggests that the bacterium plays a key role in sulfur cycling as indicated by the presence of an sqr gene encoding a sulfide quinone oxidoreductase and psr genes encoding a polysulfide reductase. It may gain energy by using sulfide or hydrogen/formate as electron donors. Polysulfide, fumarate, as well as oxygen are potential electron acceptors. Auto- or mixotrophic carbon metabolism seems plausible since a complete reductive citric acid cycle was detected. Thus the bacterium can thrive in pristine groundwater as well as in hydrocarbon-contaminated aquifers. In hydrocarbon-contaminated sulfidic habitats, the epsilonproteobacterium may generate energy by coupling the oxidation of hydrogen or formate and highly abundant sulfide with the reduction of fumarate and/or polysulfide, accompanied by efficient assimilation of acetate produced during fermentation or incomplete oxidation of hydrocarbons. The highly efficient assimilation of acetate was recently demonstrated by a pulsed 13C2-acetate protein SIP experiment. The capability of nitrogen fixation as indicated by the presence of nif genes may provide a selective advantage in nitrogen-depleted habitats. Based on this metabolic reconstruction, we propose acetate capture and sulfur cycling as key functions of Epsilonproteobacteria within the intermediary ecosystem metabolism of hydrocarbon-rich sulfidic sediments.