Electrochemical investigation of a microbial solar cell reveals a nonphotosynthetic biocathode catalyst.

Microbial solar cells (MSCs) are microbial fuel cells (MFCs) that generate their own oxidant and/or fuel through photosynthetic reactions. Here, we present electrochemical analyses and biofilm 16S rRNA gene profiling of biocathodes of sediment/seawater-based MSCs inoculated from the biocathode of a previously described sediment/seawater-based MSC. Electrochemical analyses indicate that for these second-generation MSC biocathodes, catalytic activity diminishes over time if illumination is provided during growth, whereas it remains relatively stable if growth occurs in the dark. For both illuminated and dark MSC biocathodes, cyclic voltammetry reveals a catalytic-current-potential dependency consistent with heterogeneous electron transfer mediated by an insoluble microbial redox cofactor, which was conserved following enrichment of the dark MSC biocathode using a three-electrode configuration. 16S rRNA gene profiling showed Gammaproteobacteria, most closely related to Marinobacter spp., predominated in the enriched biocathode. The enriched biocathode biofilm is easily cultured on graphite cathodes, forms a multimicrobe-thick biofilm (up to 8.2 µm), and does not lose catalytic activity after exchanges of the reactor medium. Moreover, the consortium can be grown on cathodes with only inorganic carbon provided as the carbon source, which may be exploited for proposed bioelectrochemical systems for electrosynthesis of organic carbon from carbon dioxide. These results support a scheme where two distinct communities of organisms develop within MSC biocathodes: one that is photosynthetically active and one that catalyzes reduction of O2 by the cathode, where the former partially inhibits the latter. The relationship between the two communities must be further explored to fully realize the potential for MSC applications.

Isolation of a phenol-utilizing marine bacterium from Durban Harbour (South Africa) and its preliminary characterization as Marinobacter sp. KM2.

Many aromatic hydrocarbons assigned to the so-called high production volume chemicals (HPVCs) are frequently encountered constituents of wastewaters that end up in the sea. Although the pollutant-degrading capabilities of freshwater bacteria are well known, the catabolism of pollutants by marine bacteria has received limited attention. A marine bacterium with the ability to aerobically utilize phenol - an HPVC and common aromatic pollutant - as its sole source of carbon and energy, was isolated from water samples from Durban Harbour, South Africa. The isolate, designated strain KM2, was assigned to the genus Marinobacter based on a variety of phenotypic properties and by analysis of the 16S rRNA gene sequence. The isolate displays an absolute growth requirement for NaCl which cannot be offset by replacement of NaCl with other salts. In addition to 4-methylphenol and 3,4-dimethylphenol, it utilizes a range of aliphatic hydrocarbons such as butan-1-ol and hexadecane under aerobic conditions. The transient formation of an intermediate exhibiting the UV-Vis spectral characteristics for 2-hydroxymuconic semialdehyde in cultures growing on phenol suggests that the isolate catabolizes this compound via the meta cleavage pathway. These results indicate that members of the genus Marinobacter might participate in the elimination of aromatic pollutants in South African marine environments.

Iron transport in the genus Marinobacter.

Marinobacter belong to the class of Gammaproteobacteria and these motile, halophilic or halotolerent bacteria are widely distributed throughout the world's oceans having been isolated from a wide variety of marine environments. They have also been identified as members of the bacterial flora associated with other marine organisms. Here, using a combination of natural products chemistry and genomic analysis, we assess the nature of the siderophores produced by this genus and their potential relationship to phylogeny and lifestyle/ecological niche of this diverse group of organisms. Our analysis shows a wide level of diversity in siderophore based iron uptake systems among this genus with three general strategies: (1) production and utilization of native siderophores in addition to utilization of a variety of exogenous ones, (2) production and utilization of native siderophores only, (3) lack of siderophore production but utilization of exogenous ones. They all share the presence of at least one siderophore-independent iron uptake ABC transport systems of the FbpABC iron metal type and lack the ability for direct transport of ferrous iron. Siderophore production and utilization can be correlated with phylogeny and thus it forms a type of chemotaxonomic marker for this genus.

[Synergic effect of marine obligate hydrocarbonoclastic bacteria in oil biodegradation].

OBJECTIVE: In order to study the synergic effect of two marine obligate hydrocarbonoclastic bacteria in the oil biodegradation process. METHODS: We combined the PAHs degrader Marinobacter sp. PY97S with the oil degrader Alcanivorax sp. 22CO-6 and Alcanivorax sp. JZ9B respectively to construct oil-degrading consortia. Multiple methods including weighting method, gas chromatography-flame ionization detection, gas chromatography-mass spectrometry and thin layer chromatography-flame ionization detection were used to analyze and compare the oil degradation rates as well as the chromatographic figures of degraded oil between the pure cultures of obligate hydrocarbonoclastic bacteria and defined consortia. RESULTS: The two consortia, 22CO-6 + PY97S and JZ9B + PY97S, exhibited synergic effects in the oil biodegradation process. The degradation rates of oil by the consortia were increased from 27.81% and 83.52% to 64.03% and 86.89% compared to the pure culture of oil degrader 22CO-6 and JZ9B, respectively. The consortia could degrade aliphatic and aromatic fraction at the same time, including high molecular weight PAHs chrysene and its alkyl derivatives. CONCLUSION: There are obvious synergic effect of Alcanivorax and Marinobacter strains in the oil biodegradation process, which accelerated the oil biodegradation and decomposed thoroughly the more ecotoxic high molecular weight compounds in crude oil.

Membrane vesicles: a common feature in the extracellular matter of cold-adapted antarctic bacteria.

Many Gram-negative, cold-adapted bacteria from the Antarctic environment produce large amounts of extracellular matter, which has potential biotechnology applications. We examined the ultrastructure of extracellular matter from five Antarctic bacteria (Shewanella livingstonensis NF22(T), Shewanella vesiculosa M7(T), Pseudoalteromonas sp. M4.2, Psychrobacter fozii NF23(T), and Marinobacter guineae M3B(T)) by transmission electron microscopy after high-pressure freezing and freeze substitution. All analyzed extracellular matter appeared as a netlike mesh composed of a capsular polymer around cells and large numbers of membrane vesicles (MVs), which have not yet been described for members of the genera Psychrobacter and Marinobacter. MVs showed the typical characteristics described for these structures, and seemed to be surrounded by the same capsular polymer as that found around the cells. The analysis of MV proteins from Antarctic strains by SDS-PAGE showed different banding profiles in MVs compared to the outer membrane, suggesting some kind of protein sorting during membrane vesicle formation. For the psychrotolerant bacterium, S. livingstonensis NF22(T), the growth temperature seemed to influence the amount and morphology of MVs. In an initial attempt to elucidate the functions of MVs for this psychrotolerant bacterium, we conducted a proteomic analysis on membrane vesicles from S. livingstonensis NF22(T) obtained at 4 and 18 degrees C. At both temperatures, MVs were highly enriched in outer membrane proteins and periplasmic proteins related to nutrient processing and transport in Gram-negative bacteria suggesting that MVs could be related with nutrient sensing and bacterial survival. Differences were observed in the expression of some proteins depending on incubation temperature but further studies will be necessary to define their roles and implications in the survival of bacteria in the extreme Antarctic environment.

Cytoplasmic wax ester accumulation during biofilm-driven substrate assimilation at the alkane--water interface by Marinobacter hydrocarbonoclasticus SP17.

During growth on n-alkanes, the marine bacterium Marinobacter hydrocarbonoclasticus SP17 formed a biofilm at the alkane-water interface. We showed that hexadecane degradation was correlated with biofilm development and that alkane uptake is localized in the biofilm but not in the bulk medium. Biofilms were observed in cultures on metabolizable n-alkanes (C8-C28) and n-alcohols (C12 and C16), but were formed neither on non-metabolizable alkanes (pristane, heptamethylnonane and n-C32) nor on inert substrata (glass, polystyrene and Permanox). This substratum specificity indicates that biofilm formation is determined by the presence of an interface between an insoluble substrate and the aqueous phase. Simultaneously with biofilm growth, planktonic cells were released from the biofilm. Detached cells were in a non-growing state, implying that the growing population was exclusively located within the biofilm. Planktonic and sessile cells exhibited differences in their ultrastructure and lipid content. Biofilm cells contained a large amount of wax esters (0.47mg/mg protein) in rounded or irregularly shaped cytoplasmic inclusions, whereas detached cells displayed rod-shaped inclusions and contained 5 times fewer wax esters (0.10mg/mg protein) than their sessile counterparts. This study points out the inter-relationship between biofilm formation, insoluble substrate uptake and lipid storage.