The curious phenomenon of similar levels of methylmercury (MeHg) accumulation in fish from contaminated and pristine environments may be explained by the observation that the proportion of total mercury (HgT) present as MeHg is inversely related to HgT in natural waters. We hypothesize that this "MeHg accumulation paradox" is explained by the quantitative induction of bacterial enzymes that are encoded by the mercury resistance (mer) operon, organomercury lyase (MerB), and mercuric reductase (MerA) by inorganic Hg (Hg[II]). We tested this hypothesis in two ecosystems in New Jersey: Berry's Creek in the Meadowlands (ML) and Pine Barren (PB) lakes. Across all sites, an inverse correlation (r2 = 0.80) between the concentration of HgT (ML, 113-4220 ng L(-1); PB, 0.3-5.4 ng L(-1)) and the proportion of HgT as MeHg (MeHg in ML and PB ranged from 0.08 to 1.6 and from 0.03 to 0.34 ng L(-1), respectively) was observed. The planktonic microbial community in Meadowlands surface waters exhibited adaptation to mercury, the presence of mer genes and mRNA transcripts, and high rates of reductive demethylation (k(deg) = 0.19 day(-1)). In contrast, the microbial community of PB was not adapted to mercury and demonstrated low rates of oxidative demethylation (k(deg) = 0.01 day(-1)). These results strongly support our hypothesis and show that the degradation of MeHg by mer-encoded enzymes by the water column microbiota of contaminated environments can significantly affect the amount of MeHg that is available for entry into the aquatic food web.

Since deep-sea hydrothermal vent fluids are enriched with toxic metals, it was hypothesized that (i) the biota in the vicinity of a vent is adapted to life in the presence of toxic metals and (ii) metal toxicity is modulated by the steep physical-chemical gradients that occur when anoxic, hot fluids are mixed with cold oxygenated seawater. We collected bacterial biomass at different distances from a diffuse flow vent at 9°N on the East Pacific Rise and tested these hypotheses by examining the effect of mercuric mercury [Hg(II)] on vent bacteria. Four of six moderate thermophiles, most of which were vent isolates belonging to the genus Alcanivorax, and six of eight mesophiles from the vent plume were resistant to >10 M Hg(II) and reduced it to elemental mercury [Hg(0)]. However, four psychrophiles that were isolated from a nearby inactive sulfide structure were Hg(II) sensitive. A neighbor-joining tree constructed from the deduced amino acids of a PCR-amplified fragment of merA, the gene encoding the mercuric reductase (MR), showed that sequences obtained from the vent moderate thermophiles formed a unique cluster (bootstrap value, 100) in the MR phylogenetic tree, which expanded the known diversity of this locus. The temperature optimum for Hg(II) reduction by resting cells and MR activity in crude cell extracts of a vent moderate thermophile corresponded to its optimal growth temperature, 45°C. However, the optimal temperature for activity of the MR encoded by transposon Tn501 was found to be 55 to 65°C, suggesting that, in spite of its original isolation from a mesophile, this MR is a thermophilic enzyme that may represent a relic of early evolution in high-temperature environments. Results showing that there is enrichment of Hg(II) resistance among vent bacteria suggest that these bacteria have an ecological role in mercury detoxification in the vent environment and, together with the thermophilicity of MR, point to geothermal environments as a likely niche for the evolution of bacterial mercury resistance.Heavy metals are highly enriched in hydrothermal vent fluids of mid-oceanic ridge systems (35), reaching concentrations that are considered to be toxic to living organisms (26). The steep physical-chemical gradients that occur when reduced, hot, element-and sulfur-rich vent fluids are diluted with oxygenated, cold seawater create a gradient in metal toxicity in the vent environment (20). As oxygen mixes with the anoxic, sulfur-rich fluid, metal speciation can shift from metal sulfides that show poor bioavailability and low toxicity to more soluble and oxidized forms with increased bioavailability and toxicity. With such a change in metal speciation, high tolerance to metals is expected among microbes inhabiting niches of the vent ecosystem where mixing between hydrothermal fluids and oxygenated seawater occurs, such as diffuse flow vents and associated plumes. This hypothesis is supported by experimental data showing that thermophilic archaea and bacteria from highly reduced vent microhabitats were metal su...

We analysed the genome of the aromatic hydrocarbon-degrading, facultatively chemolithotrophic betaproteobacterium, Polaromonas naphthalenivorans strain CJ2. Recent work has increasingly shown that Polaromonas species are prevalent in a variety of pristine oligotrophic environments, as well as polluted habitats. Besides a circular chromosome of 4.4 Mb, strain CJ2 carries eight plasmids ranging from 353 to 6.4 kb in size. Overall, the genome is predicted to encode 4929 proteins. Comparisons of DNA sequences at the individual gene, gene cluster and whole-genome scales revealed strong trends in shared heredity between strain CJ2 and other members of the Comamonadaceae and Burkholderiaceae. blastp analyses of protein coding sequences across strain CJ2's genome showed that genetic commonalities with other betaproteobacteria diminished significantly in strain CJ2's plasmids compared with the chromosome, especially for the smallest ones. Broad trends in nucleotide characteristics (GC content, GC skew, Karlin signature difference) showed at least six anomalous regions in the chromosome, indicating alteration of genome architecture via horizontal gene transfer. Detailed analysis of one of these anomalous regions (96 kb in size, containing the nag-like naphthalene catabolic operon) indicates that the fragment's insertion site was within a putative MiaB-like tRNA-modifying enzyme coding sequence. The mosaic nature of strain CJ2's genome was further emphasized by the presence of 309 mobile genetic elements scattered throughout the genome, including 131 predicted transposase genes, 178 phage-related genes, and representatives of 12 families of insertion elements. A total of three different terminal oxidase genes were found (putative cytochrome aa(3)-type oxidase, cytochrome cbb(3)-type oxidase and cytochrome bd-type quinol oxidase), suggesting adaptation by strain CJ2 to variable aerobic and microaerobic conditions. Sequence-suggested abilities of strain CJ2 to carry out nitrogen fixation and grow on the aromatic compounds, biphenyl and benzoate, were experimentally verified. These new phenotypes and genotypes set the stage for gaining additional insights into the physiology and biochemistry contributing to strain CJ2's fitness in its native habitat, contaminated sediment.

The propensity for groundwater ecosystems to recover from contamination by organic chemicals (in this case, coal-tar waste) is of vital concern for scientists and engineers who manage polluted sites. The microbially mediated cleanup processes are also of interest to ecologists because they are an important mechanism for the resilience of ecosystems. In this study we establish the long-term dynamic nature of a coal-tar waste-contaminated site and its microbial community. We present 16 years of chemical monitoring data, tracking responses of a groundwater ecosystem to organic contamination (naphthalene, xylenes, toluene, 2-methyl naphthalene and acenaphthylene) associated with coal-tar waste. In addition, we analyzed small-subunit (SSU) ribosomal RNA (rRNA) genes from two contaminated wells at multiple time points over a 2-year period. Principle component analysis of community rRNA fingerprints (terminal-restriction fragment length polymorphism (T-RFLP)) showed that the composition of native microbial communities varied temporally, yet remained distinctive from well to well. After screening and analysis of 1178 cloned SSU rRNA genes from Bacteria, Archaea and Eukarya, we discovered that the site supports a robust variety of eukaryotes (for example, alveolates (especially anaerobic and predatory ciliates), stramenopiles, fungi, even the small metazoan flatworm, Suomina) that are absent from an uncontaminated control well. This study links the dynamic microbial composition of a contaminated site with the long-term attenuation of its subsurface contaminants.

Microbial processes are crucial for ecosystem maintenance, yet documentation of these processes in complex open field sites is challenging. Here we used a multidisciplinary strategy (site geochemistry, laboratory biodegradation assays, and field extraction of molecular biomarkers) to deduce an ongoing linkage between aromatic hydrocarbon biodegradation and nitrogen cycling in a contaminated subsurface site. Three site wells were monitored over a 10-month period, which revealed fluctuating concentrations of nitrate, ammonia, sulfate, sulfide, methane, and other constituents. Biodegradation assays performed under multiple redox conditions indicated that naphthalene metabolism was favored under aerobic conditions. To explore in situ field processes, we measured metabolites of anaerobic naphthalene metabolism and expressed mRNA transcripts selected to document aerobic and anaerobic microbial transformations of ammonia, nitrate, and methylated aromatic contaminants. Gas chromatography-mass spectrometry detection of two carboxylated naphthalene metabolites and transcribed benzylsuccinate synthase, cytochrome c nitrite reductase, and ammonia monooxygenase genes indicated that anaerobic metabolism of aromatic compounds and both dissimilatory nitrate reduction to ammonia (DNRA) and nitrification occurred in situ. These data link formation (via DNRA) and destruction (via nitrification) of ammonia to in situ cycling of nitrogen in this subsurface habitat, where metabolism of aromatic pollutants has led to accumulation of reduced metabolic end products (e.g., ammonia and methane).Nonphotosynthetic microorganisms (particularly members of the Archaea and Bacteria) colonizing natural habitats generate metabolic energy by linking the transfer of electrons from reduced substrates (electron donors; e.g., ammonia, methane, sulfide, carbohydrates, and hydrocarbons) to oxidized substrates (electron acceptors; e.g., O 2 , nitrate, Fe 3ϩ , and sulfate) (18,40,62,73). Whenever possible, strategies for documenting biogeochemical change involve mass balance approaches that quantitatively link materials subject to a given metabolic process (e.g., consumption of carbon substrates) to formation of metabolic by-products (e.g., CO 2 ). However, owing to the open nature of many natural systems (including ocean water, rivers, and soils), convergent lines of evidence obtained using a variety of approaches (e.g., model incubations, analytical chemistry of metabolites, and molecular biology of genes and mRNA) are often needed to understand site biogeochemistry (40,46,71). Direct detection of mRNA in environmental samples has increasingly become an effective approach for documenting the in situ biogeochemical activity of microbial communities in field sites (33,34,42). This approach has included at least three techniques: (i) reverse transcription-PCR (RT-PCR)-based targeting of expression of specific functional genes (e.g., genes encoding naphthalene dioxygenase [74], Fe(II) uptake protein [47], RubisCo [70], or the anammox and denitrification pro...