@article {3128,
	title = {Magnetite compensates for the lack of a pilin-associated c-type cytochrome in extracellular electron exchange.},
	journal = {Environ Microbiol},
	volume = {17},
	year = {2015},
	month = {2015 Mar},
	pages = {648-55},
	abstract = {<p>Nanoscale magnetite can facilitate microbial extracellular electron transfer that plays an important role in biogeochemical cycles, bioremediation and several bioenergy strategies, but the mechanisms for the stimulation of extracellular electron transfer are poorly understood. Further investigation revealed that magnetite attached to the electrically conductive pili of Geobacter species in a manner reminiscent of the association of the multi-heme c-type cytochrome OmcS with the pili of Geobacter sulfurreducens. Magnetite conferred extracellular electron capabilities on an OmcS-deficient strain unable to participate in interspecies electron transfer or Fe(III) oxide reduction. In the presence of magnetite wild-type cells repressed expression of the OmcS gene, suggesting that cells might need to produce less OmcS when magnetite was available. The finding that magnetite can compensate for the lack of the electron transfer functions of a multi-heme c-type cytochrome has implications not only for the function of modern microbes, but also for the early evolution of microbial electron transport mechanisms.</p>},
	keywords = {Cytochrome c Group, Electron Transport, Electrons, Ferrosoferric Oxide, Fimbriae Proteins, Fimbriae, Bacterial, Gene Expression Regulation, Bacterial, Geobacter, Heme, Oxides},
	issn = {1462-2920},
	doi = {10.1111/1462-2920.12485},
	author = {Liu, Fanghua and Rotaru, Amelia-Elena and Shrestha, Pravin M and Malvankar, Nikhil S and Nevin, Kelly P and Lovley, Derek R}
}
@article {1411,
	title = {Magnetite formation from ferrihydrite by hyperthermophilic archaea from Endeavour Segment, Juan de Fuca Ridge hydrothermal vent chimneys.},
	journal = {Geobiology},
	volume = {12},
	year = {2014},
	month = {2014 May},
	pages = {200-11},
	abstract = {<p>Hyperthermophilic iron reducers are common in hydrothermal chimneys found along the Endeavour Segment in the northeastern Pacific Ocean based on culture-dependent estimates. However, information on the availability of Fe(III) (oxyhydr) oxides within these chimneys, the types of Fe(III) (oxyhydr) oxides utilized by the organisms, rates and environmental constraints of hyperthermophilic iron reduction, and mineral end products is needed to determine their biogeochemical significance and are addressed in this study. Thin-section petrography on the interior of a hydrothermal chimney from the Dante edifice at Endeavour showed a thin coat of Fe(III) (oxyhydr) oxide associated with amorphous silica on the exposed outer surfaces of pyrrhotite, sphalerite, and chalcopyrite in pore spaces, along with anhydrite precipitation in the pores that is indicative of seawater ingress. The iron sulfide minerals were likely oxidized to Fe(III) (oxyhydr) oxide with increasing pH and Eh due to cooling and seawater exposure, providing reactants for bioreduction. Culture-dependent estimates of hyperthermophilic iron reducer abundances in this sample were 1740 and 10 cells per gram (dry weight) of material from the outer surface and the marcasite-sphalerite-rich interior, respectively. Two hyperthermophilic iron reducers, Hyperthermus sp. Ro04 and Pyrodictium sp. Su06, were isolated from other active hydrothermal chimneys on the Endeavour Segment. Strain Ro04 is a neutrophilic (pH opt 7-8) heterotroph, while strain Su06 is a mildly acidophilic (pH opt 5), hydrogenotrophic autotroph, both with optimal growth temperatures of 90-92 \&deg;C. M\&ouml;ssbauer spectroscopy of the iron oxides before and after growth demonstrated that both organisms form nanophase (\&lt;12 nm) magnetite [Fe3 O4 ] from laboratory-synthesized ferrihydrite [Fe10 O14 (OH)2 ] with no detectable mineral intermediates. They produced up to 40 mm Fe(2+) in a growth-dependent manner, while all abiotic and biotic controls produced \&lt;3 mm Fe(2+) . Hyperthermophilic iron reducers may have a growth advantage over other hyperthermophiles in hydrothermal systems that are mildly acidic where mineral weathering at increased temperatures occurs.</p>
},
	keywords = {Ferric Compounds, Ferrosoferric Oxide, Hydrothermal Vents, Iron, Oxidation-Reduction, Pacific Ocean, Photomicrography, Pyrodictiaceae, Spectroscopy, Mossbauer, Sulfides},
	issn = {1472-4669},
	doi = {10.1111/gbi.12083},
	author = {Lin, T Jennifer and Breves, E A and Dyar, M D and Ver Eecke, H C and Jamieson, J W and Holden, J F}
}
