Reaction sequence of iron sulfide minerals in bacteria and their use as biomarkers

M. Pósfai, Peter R. Buseck, Dennis A. Bazylinski, Richard B. Frankel

Research output: Contribution to journalArticle

161 Citations (Scopus)

Abstract

Some bacteria form intracellular nanometer-scale crystals of greigite (Fe3S4) that cause the bacteria to be oriented in magnetic fields. Transmission electron microscope observations showed that ferrimagnetic greigite in these bacteria forms from nonmagnetic mackinawite (tetragonal FeS) and possibly from cubic FeS. These precursors apparently transform into greigite by rearrangement of iron atoms over a period of days to weeks. Neither pyrrhotite nor pyrite was found. These results have implications for the interpretation of the presence of pyrrhotite and greigite in the martian meteorite ALI-184001.

Original languageEnglish
Pages (from-to)880-883
Number of pages4
JournalScience
Volume280
Issue number5365
DOIs
Publication statusPublished - May 8 1998

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Sulfides
Minerals
Iron
Biomarkers
Bacteria
Meteoroids
Magnetic Fields
greigite
Electrons

ASJC Scopus subject areas

  • General

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Reaction sequence of iron sulfide minerals in bacteria and their use as biomarkers. / Pósfai, M.; Buseck, Peter R.; Bazylinski, Dennis A.; Frankel, Richard B.

In: Science, Vol. 280, No. 5365, 08.05.1998, p. 880-883.

Research output: Contribution to journalArticle

Pósfai, M. ; Buseck, Peter R. ; Bazylinski, Dennis A. ; Frankel, Richard B. / Reaction sequence of iron sulfide minerals in bacteria and their use as biomarkers. In: Science. 1998 ; Vol. 280, No. 5365. pp. 880-883.
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