A Cultured Greigite-Producing Magnetotactic Bacterium in a Novel Group of Sulfate-Reducing Bacteria

Magnetotactic bacteria contain magnetosomes—intracellular, membrane-bounded, magnetic nanocrystals of magnetite (Fe₃O₄) or greigite (Fe₃S₄)— that cause the bacteria to swim along geomagnetic field lines. We isolated a greigite-producing magnetotactic bacterium from a brackish spring in Death Valley...

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Published inScience (American Association for the Advancement of Science) Vol. 334; no. 6063; pp. 1720 - 1723
Main Authors Lefèvre, Christopher T., Menguy, Nicolas, Abreu, Fernanda, Lins, Ulysses, Pósfai, Mihály, Prozorov, Tanya, Pignol, David, Frankel, Richard B., Bazylinski, Dennis A.
Format Journal Article
LanguageEnglish
Published Washington, DC American Association for the Advancement of Science 23.12.2011
The American Association for the Advancement of Science
American Association for the Advancement of Science (AAAS)
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Summary:Magnetotactic bacteria contain magnetosomes—intracellular, membrane-bounded, magnetic nanocrystals of magnetite (Fe₃O₄) or greigite (Fe₃S₄)— that cause the bacteria to swim along geomagnetic field lines. We isolated a greigite-producing magnetotactic bacterium from a brackish spring in Death Valley National Park, California, USA, strain BW-1, that is able to biomineralize greigite and magnetite depending on culture conditions. A phylogenetic comparison of BW-1 and similar uncultured greigite- and/or magnetite-producing magnetotactic bacteria from freshwater to hypersaline habitats shows that these organisms represent a previously unknown group of sulfate-reducing bacteria in the Deltaproteobacteria. Genomic analysis of BW-1 reveals the presence of two different magnetosome gene clusters, suggesting that one may be responsible for greigite biomineralization and the other for magnetite.
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ISSN:0036-8075
1095-9203
DOI:10.1126/science.1212596