Project description:The ability of Geobacter species to readily donate electrons to extracellular electron acceptors makes the study of their physiology not only important for the understanding of environmental processes, but also for industrial applications such as bioelectronics and electrosynthesis. Studies in G. sulfurreducens have shown that outer surface components, such as c-type cytochromes and conductive type IV pili play an important role in direct electron transfer to extracellular electron acceptors such as Fe(III) oxides and electrodes. However, many of these thoroughly studied outer surface components, including c-type cytochromes, are not well conserved among Geobacter species. In order to better understand which components are involved in extracellular electron transfer in Geobacter species other than G. sulfurreducens, studies were conducted with its close relative G. metallireducens. Whole-genome microarray analysis revealed that 23 of the 91 putative c-type cytochromes encoded in the G. metallireducens genome were upregulated at least 2-fold in cells grown with Fe(III) oxide compared to cells in which Fe(III) citrate was provided as the terminal electron acceptor. Protein identification with liquid-chromatography/mass spectrometry detected 6 c-type cytochromes that were more abundant in the outer surface cell fraction of cells that were grown with Fe(III) oxide as the terminal electron acceptor compared to cells grown on Fe(III) citrate. 22 genes encoding c-type cytochromes were chosen for gene deletion. Deletion of 6 genes encoding for c-type cytochromes, a gene encoding for a lipopolysaccharide biosynthesis-associated protein, and a gene encoding for a NHL- repeat containing protein inhibited growth when Fe(III) oxide was provided as the electron acceptor. This study suggests that there are different roads for extracellular electron transfer in Geobacteraceae since homologous c-type cytochromes have different functions from one species to the other, and novel components not previously found to be essential for extracellular electron transfer were identified.

Project description:The ability of Geobacter species to readily donate electrons to extracellular electron acceptors makes the study of their physiology not only important for the understanding of environmental processes, but also for industrial applications such as bioelectronics and electrosynthesis. Studies in G. sulfurreducens have shown that outer surface components, such as c-type cytochromes and conductive type IV pili play an important role in direct electron transfer to extracellular electron acceptors such as Fe(III) oxides and electrodes. However, many of these thoroughly studied outer surface components, including c-type cytochromes, are not well conserved among Geobacter species. In order to better understand which components are involved in extracellular electron transfer in Geobacter species other than G. sulfurreducens, studies were conducted with its close relative G. metallireducens. Whole-genome microarray analysis revealed that 23 of the 91 putative c-type cytochromes encoded in the G. metallireducens genome were upregulated at least 2-fold in cells grown with Fe(III) oxide compared to cells in which Fe(III) citrate was provided as the terminal electron acceptor. Protein identification with liquid-chromatography/mass spectrometry detected 6 c-type cytochromes that were more abundant in the outer surface cell fraction of cells that were grown with Fe(III) oxide as the terminal electron acceptor compared to cells grown on Fe(III) citrate. 22 genes encoding c-type cytochromes were chosen for gene deletion. Deletion of 6 genes encoding for c-type cytochromes, a gene encoding for a lipopolysaccharide biosynthesis-associated protein, and a gene encoding for a NHL- repeat containing protein inhibited growth when Fe(III) oxide was provided as the electron acceptor. This study suggests that there are different roads for extracellular electron transfer in Geobacteraceae since homologous c-type cytochromes have different functions from one species to the other, and novel components not previously found to be essential for extracellular electron transfer were identified. An eight-chip study using total RNA recovered from four separate cultures of Geobacter metallireducens GS-15 grown with acetate (10mM)-Fe(III) oxide (100 mmol l-1) (experimental condition) or with acetate (10 mM)-Fe(III) citrate (55mM) (control condition) during exponential growth. Each chip measures the expression level of 3,627 genes from Geobacter metallireducens GS-15 with nine 45-60-mer probe pairs (PM/MM) per gene, with three-fold technical redundancy.

Project description:The conductive pili of Geobacter sulfurreducens are essential for optimal extracellular electron transfer to Fe(III) and long-range electron transport through current-producing biofilms. The KN400 strain of G. sulfurreducens reduces poorly crystalline Fe(III) oxide more rapidly than the more extensively studied DL-1 strain. Deletion of the gene for PilA, the structural pilin protein, in strain KN400 inhibited Fe(III) oxide reduction. However, slow rates of Fe(III) reduction were detected after extended (> 30 days) incubation in the presence of Fe(III) oxide. After seven consecutive transfers the PilA-deficient strain adapted to reduce Fe(III) oxide as fast as the wild type. Microarray, proteomic, and gene deletion studies indicated that this adaptation was associated with greater production of the c-type cytochrome PgcA, which was released into the culture medium. It is proposed that the extracellular cytochrome acts as an electron shuttle, promoting electron transfer from the outer cell surface to Fe(III) oxides. The adapted PilA-deficient strain competed well with the wild-type strain when both were grown together on Fe(III) oxide. However, when 50% of the culture medium was replaced with fresh medium every three days, the wild-type strain out-competed the adapted strain. A possible explanation for this is that the necessity to produce additional PgcA, to replace the PgcA continually removed, put the adapted strain at a competitive disadvantage, similar to the apparent selection against electron-shuttling producing Fe(III) reducers in most soils and sediments. Despite increased extracellular cytochrome production, the adapted PilA-deficient strain produced low levels of current; consistent with the concept that long-range electron transport through G. sulfurreducens biofilms cannot be achieved without PilA-pili. An eight-chip study using total RNA recovered from four separate cultures of Geobacter sulfurreducens JS-1 (experimental condition) or Geobacter sulfurreducens KN400 (control condition) grown with acetate (10mM)-Fe(III) oxide (100 mmol l-1) exponential growth. Each chip measures the expression level of 3,328 genes from Geobacter sulfurreducens KN400 with nine 45-60-mer probe pairs (PM/MM) per gene, with three-fold technical redundancy.

Project description:To evaluate the microbial populations involved in the reduction of Fe(III) in an acidic, iron-rich sediment, the anaerobic flow of supplemental carbon and reductant was evaluated in sediment microcosms at the in situ temperature of 12 degrees C. Supplemental glucose and cellobiose stimulated the formation of Fe(II); 42 and 21% of the reducing equivalents that were theoretically obtained from glucose and cellobiose, respectively, were recovered in Fe(II). Likewise, supplemental H(2) was consumed by acidic sediments and yielded additional amounts of Fe(II) in a ratio of approximately 1:2. In contrast, supplemental lactate did not stimulate the formation of Fe(II). Supplemental acetate was not consumed and inhibited the formation of Fe(II). Most-probable-number estimates demonstrated that glucose-utilizing acidophilic Fe(III)-reducing bacteria approximated to 1% of the total direct counts of 4', 6-diamidino-2-phenylindole-stained bacteria. From the highest growth-positive dilution of the most-probable-number series at pH 2. 3 supplemented with glucose, an isolate, JF-5, that could dissimilate Fe(III) was obtained. JF-5 was an acidophilic, gram-negative, facultative anaerobe that completely oxidized the following substrates via the dissimilation of Fe(III): glucose, fructose, xylose, ethanol, glycerol, malate, glutamate, fumarate, citrate, succinate, and H(2). Growth and the reduction of Fe(III) did not occur in the presence of acetate. Cells of JF-5 grown under Fe(III)-reducing conditions formed blebs, i.e., protrusions that were still in contact with the cytoplasmic membrane. Analysis of the 16S rRNA gene sequence of JF-5 demonstrated that it was closely related to an Australian isolate of Acidiphilium cryptum (99.6% sequence similarity), an organism not previously shown to couple the complete oxidation of sugars to the reduction of Fe(III). These collective results indicate that the in situ reduction of Fe(III) in acidic sediments can be mediated by heterotrophic Acidiphilium species that are capable of coupling the reduction of Fe(III) to the complete oxidation of a large variety of substrates including glucose and H(2).

Dataset Information

Fe(III) and S0 reduction by Pelobacter carbinolicus.

Publications

Fe(III) and S0 reduction by Pelobacter carbinolicus.

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