Burning question: Are there sustainable strategies to prevent microbial metal corrosion?

The global economic burden of microbial corrosion of metals is enormous. Microbial corrosion of iron-containing metals is most extensive under anaerobic conditions. Microbes form biofilms on metal surfaces and can directly extract electrons derived from the oxidation of Fe⁰ to Fe²⁺ to support anaerobic respiration. H₂ generated from abiotic Fe⁰ oxidation also serves as an electron donor for anaerobic respiratory microbes. Microbial metabolites accelerate this abiotic Fe⁰ oxidation. Traditional strategies for curbing microbial metal corrosion include cathodic protection, scrapping, a diversity of biocides, alloys that form protective layers or release toxic metal ions, and polymer coatings. However, these approaches are typically expensive and/or of limited applicability and not environmentally friendly. Biotechnology may provide more effective and sustainable solutions. Biocides produced with microbes can be less toxic to eukaryotes, expanding the environments for potential application. Microbially produced surfactants can diminish biofilm formation by corrosive microbes, as can quorum-sensing inhibitors. Amendments of phages or predatory bacteria have been successful in attacking corrosive microbes in laboratory studies. Poorly corrosive microbes can form biofilms and/or deposit extracellular polysaccharides and minerals that protect the metal surface from corrosive microbes and their metabolites. Nitrate amendments permit nitrate reducers to outcompete highly corrosive sulphate-reducing microbes, reducing corrosion. Investigation of all these more sustainable corrosion mitigation strategies is in its infancy. More study, especially under environmentally relevant conditions, including diverse microbial communities, is warranted.     

Isolation of Acetogenic Bacteria That Induce Biocorrosion by Utilizing Metallic Iron as the Sole Electron Donor

Corrosion of iron occurring under anoxic conditions, which is termed microbiologically influenced corrosion (MIC) or biocorrosion, is mostly caused by microbial activities. Microbial activity that enhances corrosion via uptake of electrons from metallic iron [Fe(0)] has been regarded as one of the major causative factors. In addition to sulfate-reducing bacteria and methanogenic archaea in marine environments, acetogenic bacteria in freshwater environments have recently been suggested to cause MIC under anoxic conditions. However, no microorganisms that perform acetogenesis-dependent MIC have been isolated or had their MIC-inducing mechanisms characterized. Here, we enriched and isolated acetogenic bacteria that induce iron corrosion by utilizing Fe(0) as the sole electron donor under freshwater, sulfate-free, and anoxic conditions. The enriched communities produced significantly larger amounts of Fe(II) than the abiotic controls and produced acetate coupled with Fe(0) oxidation prior to CH₄ production. Microbial community analysis revealed that Sporomusa sp. and Desulfovibrio sp. dominated in the enrichments. Strain GT1, which is closely related to the acetogen Sporomusa sphaeroides, was eventually isolated from the enrichment. Strain GT1 grew acetogenetically with Fe(0) as the sole electron donor and enhanced iron corrosion, which is the first demonstration of MIC mediated by a pure culture of an acetogen. Other well-known acetogenic bacteria, including Sporomusa ovata and Acetobacterium spp., did not grow well on Fe(0). These results indicate that very few species of acetogens have specific mechanisms to efficiently utilize cathodic electrons derived from Fe(0) oxidation and induce iron corrosion.     

Lebetimonas natsushimae sp. nov., a novel strictly anaerobic,moderately thermophilic chemoautotroph isolated from a deep-sea hydrothermal vent polychaete nest in the Mid-Okinawa Trough

A moderately thermophilic, strictly anaerobic, chemoautotrophic bacterium, designated strain HS1857^T, was isolated from a deep-sea hydrothermal vent at the Noho site in the Mid-Okinawa Trough. Strain HS1857^T grew between 35 and 63 °C (optimum 55 °C), in the presence of 10–55 g l^?1 NaCl (optimum 25 g l^?1), and pH 5.5–7.1 (optimum 6.4). Growth occurred with molecular hydrogen as the electron donor and elemental sulfur, nitrate, or selenate as the electron acceptors. Formate could serve as an alternative electron donor with nitrate as an electron acceptor. During growth with nitrate as the electron acceptor, strain HS1857^T produced ammonium and formed a biofilm. CO₂ was utilized as the sole carbon source. The G + C content of the genomic DNA was 33.2 mol%. Phylogenetic analysis of the 16S rRNA gene sequence indicated that strain HS1857^T is a member of the order Nautiliales, showing a sequence similarity of 95.0% with Lebetimonas acidiphila Pd55^T. The fatty acid composition was similar to that of L. acidiphila, which was dominated by C_18:0 (47.0%) and C_18:1 (23.7%). Based on the genomic, chemotaxonomic, phenotypic characteristics, the name Lebetimonas natsushimae sp. nov., is proposed. The type strain is HS1857^T (= NBRC 112478^T = DSM 104102^T).     

Neutrophilic, nitrate-dependent, Fe(II) oxidation by a Dechloromonas species

A species of Dechloromonas, strain UWNR4, was isolated from a nitrate-reducing, enrichment culture obtained from Wisconsin River (USA) sediments. This strain was characterized for anaerobic oxidation of both aqueous and chelated Fe(II) coupled to nitrate reduction at circumneutral pH. Dechloromonas sp. UWNR4 was incubated in anoxic batch reactors in a defined medium containing 4.5–5 mM NO₃ ^?, 6 mM Fe²⁺ and 1–1.8 mM acetate. Strain UWNR4 efficiently oxidized Fe²⁺ with 90 % oxidation of Fe²⁺ after 3 days of incubation. However, oxidation of Fe²⁺ resulted in Fe(III)-hydroxide-encrusted cells and loss of metabolic activity, suggested by inability of the cells to utilize further additions of acetate. In similar experiments with chelated iron (Fe(II)-EDTA), encrusted cells were not produced and further additions of acetate and Fe(II)-EDTA could be oxidized. Although members of the genus Dechloromonas are primarily known as perchlorate and nitrate reducers, our findings suggest that some species could be members of microbial communities influencing iron redox cycling in anoxic, freshwater sediments. Our work using Fe(II)-EDTA also demonstrates that Fe(II) oxidation was microbially catalyzed rather than a result of abiotic oxidation by biogenic NO₂ ^?.     

Autotrophic denitrification by nitrate-dependent Fe(II) oxidation in a continuous up-flow biofilter

A continuous-upflow biofilter packed with sponge iron was constructed for nitrate removal under an anaerobic atmosphere. Microbacterium sp. W5, a nitrate reducing and Fe(II) oxidizing strain, was added to the biofilter as an inoculum. The best results were achieved when NO₃ ^?-N concentration was 30 mg/L and Fe²⁺ was 800 mg/L. Nitrite in influent would inhibit nitrate removal and aqueous Fe²⁺ resulted in encrustation. Fe(II)EDTA would prevent cells from encrustation and the maximum nitrogen removal efficiency was about 90 % with Fe(II)EDTA level of 1100 mg/L. Nitrate reduction followed first-order reaction kinetics. Characteristics of biofilms were analyzed by X-ray fluorescence spectroscopy.     

Growth of moderately thermophilic iron-oxidizing bacterium strain TI-1 in synthetic medium

The moderately thermophilic iron-oxidizing bacterium strain TI-1, which lacks enzyme systems involved in CO₂ fixation, grows at 45°C in Fe²⁺ medium supplemented with yeast extract to give a maximum cell growth of 1.0 × 10⁸ cells per ml, but does not grow in Fe²⁺ medium without yeast extract. To elucidate the physiology of the strain, a synthetic medium was developed. It was found that the best synthetic medium was Fe²⁺-6AA, containing Fe²⁺, salts, and the following six l-amino acids: alanine, aspartic acid, glutamic acid, arginine, serine, and histidine. In this medium, strain TI-1 showed a maximum cell growth of 10 × 10⁸ cells/ml. The six amino acids in the Fe²⁺-6AA medium were used not only as a carbon source but also as a source of nitrogen. Inorganic nitrogen sources, such as ammonium ion, hydrazine, hydroxylamine, nitrite, and nitrate, were not used as a sole source of nitrogen, but rather strongly inhibited the utilization of the six amino acids at 1 mM. In the Fe²⁺ (10 mM)-6AA medium supplemented with 21 mM Fe³⁺, reduction of Fe³⁺ to Fe²⁺ that was dependent on the added amino acids was observed, suggesting another role of the amino acids in the growth of strain TI-1. Washed, intact cells of strain TI-1 had the activity to reduce Fe³⁺ to Fe²⁺.     

Ferrous Iron and Sulfur Oxidation and Ferric Iron Reduction Activities of Thiobacillus ferrooxidans Are Affected by Growth on Ferrous Iron, Sulfur, or a Sulfide Ore

Eight strains of Thiobacillus ferrooxidans (laboratory strains Tf-1 [= ATCC 13661] and Tf-2 [= ATCC 19859] and mine isolates SM-1, SM-2, SM-3, SM-4, SM-5, and SM-8) and three strains of Thiobacillus thiooxidans (laboratory strain Tt [= ATCC 8085] and mine isolates SM-6 and SM-7) were grown on ferrous iron (Fe²⁺), elemental sulfur (S⁰), or sulfide ore (Fe, Cu, and Zn). The cells were studied for their aerobic Fe²⁺ - and S⁰-oxidizing activities (O₂ consumption) and anaerobic S⁰-oxidizing activity with ferric iron (Fe³⁺) (Fe²⁺ formation). Fe²⁺-grown T. ferrooxidans cells oxidized S⁰ aerobically at a rate of 2 to 4% of the Fe²⁺ oxidation rate. The rate of anaerobic S⁰ oxidation with Fe³⁺ was equal to the aerobic oxidation rate in SM-1, SM-3, SM-4, and SM-5, but was only one-half or less that in Tf-1, Tf-2, SM-2, and SM-8. Transition from growth on Fe²⁺ to that on S⁰ produced cells with relatively undiminished Fe²⁺ oxidation activities and increased S⁰ oxidation (both aerobic and anaerobic) activities in Tf-2, SM-4, and SM-5, whereas it produced cells with dramatically reduced Fe²⁺ oxidation and anaerobic S⁰ oxidation activities in Tf-1, SM-1, SM-2, SM-3, and SM-8. Growth on ore 1 of metal-leaching Fe²⁺-grown strains and on ore 2 of all Fe²⁺-grown strains resulted in very high yields of cells with high Fe²⁺ and S⁰ oxidation (both aerobic and anaerobic) activities with similar ratios of various activities. Sulfur-grown Tf-2, SM-1, SM-4, SM-6, SM-7, and SM-8 cultures leached metals from ore 3, and Tf-2 and SM-4 cells recovered showed activity ratios similar to those of other ore-grown cells. It is concluded that all the T. ferrooxidans strains studied have the ability to produce cells with Fe²⁺ and S⁰ oxidation and Fe³⁺ reduction activities, but their levels are influenced by growth substrates and strain differences.     

Anaerobic Oxidation of Arsenite in Mono Lake Water and by a Facultative, Arsenite-Oxidizing Chemoautotroph, Strain MLHE-1

Arsenite [As(III)]-enriched anoxic bottom water from Mono Lake, California, produced arsenate [As(V)] during incubation with either nitrate or nitrite. No such oxidation occurred in killed controls or in live samples incubated without added nitrate or nitrite. A small amount of biological As(III) oxidation was observed in samples amended with Fe(III) chelated with nitrolotriacetic acid, although some chemical oxidation was also evident in killed controls. A pure culture, strain MLHE-1, that was capable of growth with As(III) as its electron donor and nitrate as its electron acceptor was isolated in a defined mineral salts medium. Cells were also able to grow in nitrate-mineral salts medium by using H₂ or sulfide as their electron donor in lieu of As(III). Arsenite-grown cells demonstrated dark ¹⁴CO₂ fixation, and PCR was used to indicate the presence of a gene encoding ribulose-1,5-biphosphate carboxylase/oxygenase. Strain MLHE-1 is a facultative chemoautotroph, able to grow with these inorganic electron donors and nitrate as its electron acceptor, but heterotrophic growth on acetate was also observed under both aerobic and anaerobic (nitrate) conditions. Phylogenetic analysis of its 16S ribosomal DNA sequence placed strain MLHE-1 within the haloalkaliphilic Ectothiorhodospira of the γ-Proteobacteria. Arsenite oxidation has never been reported for any members of this subgroup of the Proteobacteria.     

Dissimilatory Iodate Reduction by Marine Pseudomonas sp. Strain SCT

Bacterial iodate (IO₃⁻) reduction is poorly understood largely due to the limited number of available isolates as well as the paucity of information about key enzymes involved in the reaction. In this study, an iodate-reducing bacterium, designated strain SCT, was newly isolated from marine sediment slurry. SCT is phylogenetically closely related to the denitrifying bacterium Pseudomonas stutzeri and reduced 200 μM iodate to iodide (I⁻) within 12 h in an anaerobic culture containing 10 mM nitrate. The strain did not reduce iodate under the aerobic conditions. An anaerobic washed cell suspension of SCT reduced iodate when the cells were pregrown anaerobically with 10 mM nitrate and 200 μM iodate. However, cells pregrown without iodate did not reduce it. The cells in the former category showed methyl viologen-dependent iodate reductase activity (0.31 U mg⁻¹), which was located predominantly in the periplasmic space. Furthermore, SCT was capable of anaerobic growth with 3 mM iodate as the sole electron acceptor, and the cells showed enhanced activity with respect to iodate reductase (2.46 U mg⁻¹). These results suggest that SCT is a dissimilatory iodate-reducing bacterium and that its iodate reductase is induced by iodate under anaerobic growth conditions.     

Nutritional Requirements of Methanosarcina sp. Strain TM-1

Methanosarcina sp. strain TM-1, an acetotrophic, thermophilic methanogen isolated from an anaerobic sludge digestor, was originally reported to require an anaerobic sludge supernatant for growth. It was found that the sludge supernatant could be replaced with yeast extract (1 g/liter), 6 mM bicarbonate-30% CO₂, and trace metals, with a doubling time on methanol of 14 h. For growth on either methanol or acetate, yeast extract could be replaced with CaCl₂ · 2H₂O (13.6 μM minimum) and the vitamin p-aminobenzoic acid (PABA, ca. 3 nM minimum), with a doubling time on methanol of 8 to 9 h. Filter-sterilized folic acid at 0.3 μM could not replace PABA. The antimetabolite sulfanilamide (20 mM) inhibited growth of and methanogenesis by Methanosarcina sp. strain TM-1, and this inhibition was reversed by the addition of 0.3 μM PABA. When a defined medium buffered with 20 mM N,N-bis(2-hydroxyethyl)-2-aminoethanesulfonic acid was used, it was shown that Methanosarcina sp. strain TM-1 required 6 mM bicarbonate-30% CO₂ for optimal growth and methanogenesis from methanol. Cells growing on acetate were less dependent on bicarbonate-CO₂. When we used a defined medium in which the only organic compounds present were methanol or acetate, nitrilotriacetic acid (0.2 mM), and PABA, it was possible to limit batch cultures of Methanosarcina sp. strain TM-1 for nitrogen at NH₄⁺ concentrations at or below 2.0 mM, in marked contrast with Methanosarcina barkeri 227, which fixes dinitrogen when grown under NH₄⁺ limitation.     

Characterization of the Reduction of Selenate and Tellurite by Nitrate Reductases

Preliminary studies showed that the periplasmic nitrate reductase (Nap) of Rhodobacter sphaeroides and the membrane-bound nitrate reductases of Escherichia coli are able to reduce selenate and tellurite in vitro with benzyl viologen as an electron donor. In the present study, we found that this is a general feature of denitrifiers. Both the periplasmic and membrane-bound nitrate reductases of Ralstonia eutropha, Paracoccus denitrificans, and Paracoccus pantotrophus can utilize potassium selenate and potassium tellurite as electron acceptors. In order to characterize these reactions, the periplasmic nitrate reductase of R. sphaeroides f. sp. denitrificans IL106 was histidine tagged and purified. The V_max and K_m were determined for nitrate, tellurite, and selenate. For nitrate, values of 39 μmol · min⁻¹ · mg⁻¹ and 0.12 mM were obtained for V_max and K_m, respectively, whereas the V_max values for tellurite and selenate were 40- and 140-fold lower, respectively. These low activities can explain the observation that depletion of the nitrate reductase in R. sphaeroides does not modify the MIC of tellurite for this organism.     

Enhanced start-up of anaerobic facultatively autotrophic biocathodes in bioelectrochemical systems

Biocathodes in bioelectrochemical systems (BESs) can be used to convert CO₂ into diverse organic compounds through a process called microbial electrosynthesis. Unfortunately, start-up of anaerobic biocathodes in BESs is a difficult and time consuming process. Here, a pre-enrichment method was developed to improve start-up of anaerobic facultatively autotrophic biocathodes capable of using cathodes as the electron donor (electrotrophs) and CO₂ as the electron acceptor. Anaerobic enrichment of bacteria from freshwater bog sediment samples was first performed in batch cultures fed with glucose and then used to inoculate BES cathode chambers set at −0.4 V (versus a standard hydrogen electrode; SHE). After two weeks of heterotrophic operation of BESs, CO₂ was provided as the sole electron acceptor and carbon source. Consumption of electrons from cathodes increased gradually and was sustained for about two months in concert with a significant decrease in cathode chamber headspace CO₂. The maximum current density consumed was −34 ± 4 mA/m². Biosynthesis resulted in organic compounds that included butanol, ethanol, acetate, propionate, butyrate, and hydrogen gas. Bacterial community analyses based on 16S rRNA gene clone libraries revealed Trichococcus palustris DSM 9172 (99% sequence identity) as the prevailing species in biocathode communities, followed by Oscillibacter sp. and Clostridium sp. Isolates from autotrophic cultivation were most closely related to Clostridium propionicum (99% sequence identity; ZZ16), Clostridium celerecrescens (98–99%; ZZ22, ZZ23), Desulfotomaculum sp. (97%; ZZ21), and Tissierella sp. (98%; ZZ25). This pre-enrichment procedure enables simplified start-up of anaerobic biocathodes for applications such as electrofuel production by facultatively autotrophic electrotrophs.     

Characterization of the Mineral Phosphate-Solubilizing Activity of <Emphasis Type="Italic">Pantoea aglomerans</Emphasis> MMB051 Isolated from an Iron-Rich Soil in Southeastern Venezuela (Bolívar State)

The mineral phosphate-solubilizing (MPS) activity of a Pantoea agglomerans strain, namely MMB051, isolated from an iron-rich, acidic soil near Ciudad Piar (Bolívar State, Venezuela), was characterized on a chemically defined medium (NBRIP). Various insoluble inorganic phosphates, including tri-calcium phosphate [Ca₃(PO₄)₂], iron phosphate (FePO₄), aluminum phosphate (AlPO₄), and Rock Phosphate (RP) were tested as sole sources of P for bacterial growth. Solubilization of Ca₃(PO₄)₂ was very efficient and depended on acidification of the external milieu when MMB051 cells were grown in the presence of glucose. This was also the case when RP was used as the sole P source. On the other hand, the solubilization efficiency toward more insoluble mineral phosphates (FePO₄ and AlPO₄) was shown to be very low. Even though gluconic acid (GA) was detected on culture supernatants of strain MMB051, a consequence of the direct oxidation pathway of glucose, inorganic-P solubilization seemed also to be related to other processes dependent on active cell growth. Among these, proton release by ammonium (NH₄⁺) fixation appeared to be of paramount importance to explain inorganic-P solubilization mediated by strain MMB051. On the contrary, the presence of nitrate (NO₃^–) salts as the sole N source affected negatively the ability of MMB051 cells to solubilize inorganic P.     

Rationalization of properties of nitrate reductases in Rhodopseudomonas capsulata

1. The properties of nitrate reductase activities have been compared in several strains of Rhodopseudomonas capsulata grown phototrophically in the presence of nitrate as sole nitrogen source.
2. Strains AD2 and BK5 resemble the spontaneous mutant N22DNAR⁺ (described by McEwan et al. 1982 FEBS Lett. 150, 277\2-280) in that reduction of nitrate was inhibited by either illumination or oxygen but not by NH ₄ ⁺ , and that electron flow to nitrate under dark anaerobic conditions generated a cytoplasmic membrane potential (as judged by an electrochromic shift in the absorbance spectrum of endogenous carotenoid pigments). In contrast disappearance of nitrate from suspensions of strains N22 and St. Louis was dependent upon illumination and was inhibited by NH ₄ ⁺ . Membrane potentials were not generated by addition of nitrate in the dark to N22, St. Louis or strain Kbl.
3. Nitrate reductase was shown to be located in the periplasmic space of both strain AD2 and mutant N22DNAR⁺. The nitrate reductase activity in cells of AD2 and N22DNAR⁺ was relatively insensitive to azide, with 0.5mM azide required for 50% inhibition. The nitrate reductase of strain BK5 was more strongly associated with the cytoplasmic membrane and no conclusion could be reached about whether it was located on the periplasmic or cytoplasmic surface. In BK5 cells nitrate reductase activity was sensitive to low concentrations of azide (50% inhibition with 2 \gmM azide). It is proposed that functionally the nitrate reductase activity in strains AD2, BK5 and N22DNAR⁺ has identical roles. These roles are suggested to include:
4. The first step in the assimilation of nitrate.
5. Provision of an alternative electron acceptor to oxygen for generating a membrane potential.
6. A mechanism for disposing of excess reducing equivalents in the maintenance of balanced growth. This type of nitrate reductase, especially in AD2 and N22DNAR⁺, appears to resemble that described in a denitrifying strain of Rps. sphaeroides, but to differ markedly from its membrane-bound counterpart in other bacteria including the denitrifying Paracoccus denitrificans and Escherichia coli.
7. In other strains of Rps. capsulata including St. Louis, N22 and Kbl, only an assimilatory nitrate reductase, whose activity in intact cells is relatively sensitive to azide, is present in anaerobic, phototrophic cultures grown with nitrate as nitrogen source. As this reductase cannot be detected after breakage of cells, no conclusion can be made as to its location in the cell.

     

Vibrio salinus sp. nov., a marine nitrogen-fixing bacterium isolated from the lagoon sediment of an islet inside an atoll in the western Pacific Ocean

A marine, facultatively anaerobic, nitrogen-fixing bacterium, designated strain DNF-1^T, was isolated from the lagoon sediment of Dongsha Island, Taiwan. Cells grown in broth cultures were Gram-negative rods that were motile by means of monotrichous flagella. Cells grown on plate medium produced prosthecae and vesicle-like structures. NaCl was required and optimal growth occurred at about 2–3% NaCl, 25–30 °C and pH 7–8. The strain grew aerobically and was capable of anaerobic growth by fermenting D-glucose or other carbohydrates as substrate. Both the aerobic and anaerobic growth could be achieved with NH₄Cl as a sole nitrogen source. When N₂ served as the sole nitrogen source only anaerobic growth was observed. Major cellular fatty acids were C_14:0, C_16:0 and C_16:1 ω7c, while major polar lipids were phosphatidylethanolamine and phosphatidylglycerol. The DNA G+C content was 42.2 mol% based on the genomic DNA data. Phylogenetic analyses based on 16S rRNA genes and the housekeeping genes, gapA, pyrH, recA and gyrB, revealed that the strain formed a distinct lineage at species level in the genus Vibrio of the family Vibrionaceae. These results and those from genomic, chemotaxonomic and physiological studies strongly support the assignment of a novel Vibrio species. The name Vibrio salinus sp. nov. is proposed for the novel species, with DNF-1^T (=?BCRC 81209^T?=?JCM 33626^T) as the type strain. This newly proposed species represents the second example of the genus Vibrio that has been demonstrated to be capable of anaerobic growth by fixing N₂ as the sole nitrogen source.

     

Marinobacter nanhaiticus sp. nov., polycyclic aromatic hydrocarbon-degrading bacterium isolated from the sediment of the South China Sea

A Gram-negative, rod-shaped, slightly halophilic and facultatively anaerobic bacterium, designated strain D15-8W^T, was isolated from the sediment of the South China Sea. Growth was found to occur optimally at 25 °C, between pH 7.0 and 8.0 and with 1–5 % (w/v) NaCl. The strain was observed to utilize a variety of organic substrates and polycyclic aromatic hydrocarbons as sole carbon sources. The G+C content of the genomic DNA was determined to be 58.7 %. The predominant respiratory quinone was found to be Q-9. The significant fatty acids were determined to be C_16:0, C_16:1 ω9c, C_18:1 ω9c, C_12:0 and C_14:0 3OH. Analysis of 16S rRNA gene sequences showed that strain D15-8W^T fits within the phylogenetic cluster of the genus Marinobacter and is most closely related to Marinobacter segnicrescens CGMCC 1.6489^T, Marinobacter bryozoorum DSM 15401^T, Marinobacter lacisalsi CECT 7297^T and Marinobacter daqiaonensis CGMCC1.9167^T. The DNA–DNA hybridization values between strain D15-8W^T and the type strains of the most closely related species were 42.3 % (CGMCC 1.6489^T), 39.8 % (DSM 15401^T), 37.3 % (CECT 7297^T) and 35.2 % (CGMCC1.9167^T). The results of this polyphasic study indicate that strain D15-8W^T represents a novel species of the genus Marinobacter, for which the name Marinobacter nanhaiticus sp. nov. is proposed. The type strain is D15-8W^T (=CGMCC 1.11019^T=KCTC 23749^T).     

Anaerobic Benzene Oxidation by Geobacter Species

The abundance of Geobacter species in contaminated aquifers in which benzene is anaerobically degraded has led to the suggestion that some Geobacter species might be capable of anaerobic benzene degradation, but this has never been documented. A strain of Geobacter, designated strain Ben, was isolated from sediments from the Fe(III)-reducing zone of a petroleum-contaminated aquifer in which there was significant capacity for anaerobic benzene oxidation. Strain Ben grew in a medium with benzene as the sole electron donor and Fe(III) oxide as the sole electron acceptor. Furthermore, additional evaluation of Geobacter metallireducens demonstrated that it could also grow in benzene-Fe(III) medium. In both strain Ben and G. metallireducens the stoichiometry of benzene metabolism and Fe(III) reduction was consistent with the oxidation of benzene to carbon dioxide with Fe(III) serving as the sole electron acceptor. With benzene as the electron donor, and Fe(III) oxide (strain Ben) or Fe(III) citrate (G. metallireducens) as the electron acceptor, the cell yields of strain Ben and G. metallireducens were 3.2 × 10⁹ and 8.4 × 10⁹ cells/mmol of Fe(III) reduced, respectively. Strain Ben also oxidized benzene with anthraquinone-2,6-disulfonate (AQDS) as the sole electron acceptor with cell yields of 5.9 × 10⁹ cells/mmol of AQDS reduced. Strain Ben serves as model organism for the study of anaerobic benzene metabolism in petroleum-contaminated aquifers, and G. metallireducens is the first anaerobic benzene-degrading organism that can be genetically manipulated.     

Iron-Corroding Methanogen Isolated from a Crude-Oil Storage Tank

Microbiologically influenced corrosion of steel in anaerobic environments has been attributed to hydrogenotrophic microorganisms. A sludge sample collected from the bottom plate of a crude-oil storage tank was used to inoculate a medium containing iron (Fe⁰) granules, which was then incubated anaerobically at 37°C under an N₂-CO₂ atmosphere to enrich for microorganisms capable of using iron as the sole source of electrons. A methanogen, designated strain KA1, was isolated from the enrichment culture. An analysis of its 16S rRNA gene sequence revealed that strain KA1 is a Methanococcus maripaludis strain. Strain KA1 produced methane and oxidized iron much faster than did the type strain of M. maripaludis, strain JJ^T, which produced methane at a rate expected from the abiotic H₂ production rate from iron. Scanning electron micrographs of iron coupons that had been immersed in either a KA1 culture, a JJ^T culture, or an aseptic medium showed that only coupons from the KA1 culture had corroded substantially, and these were covered with crystalline deposits that consisted mainly of FeCO₃.Iron (Fe⁰) is an inexpensive metal and is widely used in many industrial processes and industrial/commercial products. When iron contacts an aqueous electrolyte, it readily corrodes. This happens because, as a result of metallurgical and environmental heterogeneities, the electrolytes are not evenly distributed across the surface of the metal and consequently the electric potential is also unevenly distributed. Therefore, electrons flow within the metal from an area of higher electrical potential (the anode) to an area of lower electrical potential (the cathode). At the anode, iron atoms lose electrons and dissolve into ferrous ions (Fe²⁺), whereas cations or elements dissolved in solution (e.g., H⁺ under anaerobic conditions or O₂ under aerobic conditions) are reduced by electrons at the cathode.The corrosion of structures that contain iron is economically devastating. It has been estimated that in the United States alone, the cost of corrosion is 276 billion dollars annually (17). Iron is corroded not only by physiochemical processes but also by the metabolic activity of microorganisms; this metabolic process is termed microbiologically influenced corrosion (MIC). Some 10% of all corrosion damage may be the result of microbial activity (15), and sulfate-reducing bacteria (SRB) are widely regarded as the causative agents of MIC in anaerobic environments (11, 12, 18, 21). The mechanism by which SRB stimulate iron corrosion may occur via the uptake of electrons at the cathodic surface of iron (cathodic depolarization) in conjunction with sulfate reduction (8e⁻ + SO₄²⁻ + 10H⁺ → H₂S + 4H₂O) (27), while at the anionic surface, iron atoms are oxidized to ferrous ions (Fe → Fe²⁺ + 2e⁻). In fact, certain SRB use not only hydrogen but also iron as a source of electrons for sulfate reduction (1, 9, 22). Because not all SRB grow as fast in the presence of iron as they do in the presence of hydrogen (9), fast-growing SRB on iron may have a specific enzyme(s) that removes electrons from iron.Because some methanogens are viable in a hydrogen atmosphere, as are most SRBs, these methanogens may also cause iron corrosion under anaerobic conditions. Several methanogens have been shown to grow and produce methane in medium containing iron as the sole source of electrons (5). The extent of the corrosion by these methanogens, however, was not substantial (2). Others have reported that methanogens do not increase the rate of iron corrosion in comparison with aseptic solutions (6, 7). Recently Dinh and colleagues (9) isolated a methanogen (strain IM1) that produces methane more rapidly than does Methanococcus maripaludis (DSMZ 2771) when cultured with iron granules. Although the rate of iron oxidation was not measured in their experiments, their results suggests that strain IMI oxidizes iron more rapidly than does strain DSMZ 2771.We report herein that a methanogen that was isolated from the sludge of an oil storage tank can unequivocally oxidize iron.     

Chemolithotrophic growth ofDesulfovibrio desulfuricans with hydrogen coupled to ammonification of nitrate or nitrite

Two of nine sulfate reducing bacteria tested,Desulfobulbus propionicus andDesulfovibrio desulfuricans (strain Essex 6), were able to grow with nitrate as terminal electron acceptor, which was reduced to ammonia. Desulfovibrio desulfuricans was grown in chemostat culture with hydrogen plus limiting concentrations of nitrate, nitrite or sulfate as sole energy source. Growth yields up to 13.1, 8.8 or 9.7 g cell dry mass were obtained per mol nitrate, nitrite or sulfate reduced, respectively. The apparent half saturation constants (K _s) were below the detection limits of 200, 3 or 100 mol/l for nitrate, nitrite of sulfate, respectively. The maximum growth rates {ie63-1} raised from 0.124 h^-1 with sulfate and 0.150 h^-1 with nitrate to 0.193 h^-1 with nitrite as electron acceptor. Regardless of the electron acceptor in the culture medium, cell extracts exhibited absorption maxima corresponding to cytochromec and desulfoviridin. Nitrate reductase was found to be inducible by nitrate or nitrite, whereas nitrite reductase was synthesized constitutively. The activities of nitrate and nitrite reductases with hydrogen as electron donor were 0.2 and 0.3 mol/min·mg protein, respectively. If limiting amounts of hydrogen were added to culture bottles with nitrate as electron acceptor, part of the nitrate was only reduced to the level of nitrite. In media containing nitrate plus sulfate or nitrite plus sulfate, sulfate reduction was suppressed.The results demonstrate that the ammonification of nitrate or nitrite can function as sole energy conserving process in some sulfate-reducing bacteria.     

Aerobic and Anaerobic Catabolism of Vanillic Acid and Some Other Methoxy-Aromatic Compounds by Pseudomonas sp. Strain PN-1

Vanillic acid (4-hydroxy-3-methoxybenzoic acid) supported the anaerobic (nitrate respiration) but not the aerobic growth of Pseudomonas sp. strain PN-1. Cells grown anaerobically on vanillate oxidized vanillate, p-hydroxybenzoate, and protocatechuic acid (3,4-dihydroxybenzoic acid) with O₂ or nitrate. Veratric acid (3,4-dimethoxybenzoic acid) but not isovanillic acid (3-hydroxy-4-methoxybenzoic acid) induced cells for the oxic and anoxic utilization of vanillate, and protocatechuate was detected as an intermediate of vanillate breakdown under either condition. Aerobic catabolism of protocatechuate proceeded via 4,5-meta cleavage, whereas anaerobically it was probably dehydroxylated to benzoic acid. Formaldehyde was identified as a product of aerobic demethylation, indicating a monooxygenase mechanism, but was not detected during anaerobic demethylation. The aerobic and anaerobic systems had similar but not identical substrate specificities. Both utilized m-anisic acid (3-methoxybenzoic acid) and veratrate but not o- or p-anisate and isovanillate. Syringic acid (4-hydroxy-3,5-dimethoxybenzoic acid), 3-O-methylgallic acid (3-methoxy-4,5-dihydroxybenzoic acid), and 3,5-dimethoxybenzoic acid were attacked under either condition, and formaldehyde was liberated from these substrates in the presence of O₂. The anaerobic demethylating system but not the aerobic enzyme was also active upon guaiacol (2-methoxyphenol), ferulic acid (3-[4-hydroxy-3-methoxyphenyl]-2-propenoic acid), 3,4,5-trimethoxycinnamic acid (3-[3,4,5-trimethoxyphenyl]-2-propenoic acid), and 3,4,5-trimethoxybenzoic acid. The broad specificity of the anaerobic demethylation system suggests that it probably is significant in the degradation of lignoaromatic molecules in anaerobic environments.