@article {469,
	title = {Polar lipid fatty acids, LPS-hydroxy fatty acids, and respiratory quinones of three Geobacter strains, and variation with electron acceptor.},
	journal = {J Ind Microbiol Biotechnol},
	volume = {36},
	year = {2009},
	month = {2009 Feb},
	pages = {205-9},
	abstract = {The polar lipid fatty acids, lipopolysaccharide hydroxy-fatty acids, and respiratory quinones of Geobacter metallireducens str. GS-15, Geobacter sulfurreducens str. PCA, and Geobacter bemidjiensis str. Bem are reported. Also, the lipids of G. metallireducens were compared when grown with Fe(3+) or nitrate as electron acceptors and G. sulfurreducens with Fe(3+) or fumarate. In all experiments, the most abundant polar lipid fatty acids were 14:0, i15:0, 16:1 omega 7c, 16:1 omega 5c, and 16:0; lipopolysaccharide hydroxy-fatty acids were dominated by 3oh16:0, 3oh14:0, 9oh16:0, and 10oh16:0; and menaquinone-8 was the most abundant respiratory quinone. Some variation in lipid profiles with strain were observed, but not with electron acceptor.},
	keywords = {Culture Media, Electrons, Environmental Microbiology, Fatty Acids, Ferrous Compounds, Geobacter, Lipids, Lipopolysaccharides, Nitrates, Quinones, Vitamin K 2},
	issn = {1476-5535},
	doi = {10.1007/s10295-008-0486-7},
	author = {Hedrick, D B and Peacock, A D and Lovley, D R and Woodard, T L and Nevin, K P and Long, P E and White, D C}
}
@article {557,
	title = {Geobacter sulfurreducens can grow with oxygen as a terminal electron acceptor.},
	journal = {Appl Environ Microbiol},
	volume = {70},
	year = {2004},
	month = {2004 Apr},
	pages = {2525-8},
	abstract = {Geobacter sulfurreducens, previously classified as a strict anaerobe, tolerated exposure to atmospheric oxygen for at least 24 h and grew with oxygen as the sole electron acceptor at concentrations of 10\% or less in the headspace. These results help explain how Geobacter species may survive in oxic subsurface environments, being poised to rapidly take advantage of the development of anoxic conditions.},
	keywords = {Aerobiosis, Anaerobiosis, Electron Transport, Environmental Microbiology, Geobacter, Oxygen},
	issn = {0099-2240},
	author = {Lin, W C and Coppi, M V and Lovley, D R}
}
@article {620,
	title = {Microbiological evidence for Fe(III) reduction on early Earth.},
	journal = {Nature},
	volume = {395},
	year = {1998},
	month = {1998 Sep 3},
	pages = {65-7},
	abstract = {It is generally considered that sulphur reduction was one of the earliest forms of microbial respiration, because the known microorganisms that are most closely related to the last common ancestor of modern life are primarily anaerobic, sulphur-reducing hyperthermophiles. However, geochemical evidence indicates that Fe(III) is more likely than sulphur to have been the first external electron acceptor of global significance in microbial metabolism. Here we show that Archaea and Bacteria that are most closely related to the last common ancestor can reduce Fe(III) to Fe(II) and conserve energy to support growth from this respiration. Surprisingly, even Thermotoga maritima, previously considered to have only a fermentative metabolism, could grow as a respiratory organism when Fe(III) was provided as an electron acceptor. These results provide microbiological evidence that Fe(III) reduction could have been an important process on early Earth and suggest that microorganisms might contribute to Fe(III) reduction in modern hot biospheres. Furthermore, our discovery that hyperthermophiles that had previously been thought to require sulphur for cultivation can instead be grown without the production of toxic and corrosive sulphide, should aid biochemical investigations of these poorly understood organisms.},
	keywords = {Earth (Planet), Electron Transport, Environmental Microbiology, Ferric Compounds, Gram-Negative Anaerobic Bacteria, Oxidation-Reduction, Thermoproteaceae},
	issn = {0028-0836},
	doi = {10.1038/25720},
	author = {Vargas, M and Kashefi, K and Blunt-Harris, E L and Lovley, D R}
}
