Rapid magnetosome formation shown by real-time x-ray magnetic circular dichroism

Magnetosomes are magnetite nanoparticles formed by biomineralization within magnetotactic bacteria. Although there have been numerous genetic and proteomic studies of the magnetosome-formation process, there have been only limited and inconclusive studies of mineral-phase evolution during the format...

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Veröffentlicht in:Proceedings of the National Academy of Sciences - PNAS 2007-12, Vol.104 (49), p.19524-19528
Hauptverfasser: Staniland, Sarah, Ward, Bruce, Harrison, Andrew, van der Laan, Gerrit, Telling, Neil
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container_end_page 19528
container_issue 49
container_start_page 19524
container_title Proceedings of the National Academy of Sciences - PNAS
container_volume 104
creator Staniland, Sarah
Ward, Bruce
Harrison, Andrew
van der Laan, Gerrit
Telling, Neil
description Magnetosomes are magnetite nanoparticles formed by biomineralization within magnetotactic bacteria. Although there have been numerous genetic and proteomic studies of the magnetosome-formation process, there have been only limited and inconclusive studies of mineral-phase evolution during the formation process, and no real-time studies of such processes have yet been performed. Thus, suggested formation mechanisms still need substantiating with data. Here we report the examination of the magnetosome material throughout the formation process in a real-time in vivo study of Magnetospirillum gryphiswaldense, strain MSR-1. Transmission EM and x-ray absorption spectroscopy studies reveal that full-sized magnetosomes are seen 15 min after formation is initiated. These immature magnetosomes contain a surface layer of the nonmagnetic iron oxide-phase hematite. Mature magnetite is found after another 15 min, concurrent with a dramatic increase in magnetization. This rapid formation result is contrary to previously reported studies and discounts the previously proposed slow, multistep formation mechanisms. Thus, we conclude that the biomineralization of magnetite occurs rapidly in magnetotactic bacteria on a similar time scale to high-temperature chemical precipitation reactions, and we suggest that this finding is caused by a biological catalysis of the process.
doi_str_mv 10.1073/pnas.0704879104
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Although there have been numerous genetic and proteomic studies of the magnetosome-formation process, there have been only limited and inconclusive studies of mineral-phase evolution during the formation process, and no real-time studies of such processes have yet been performed. Thus, suggested formation mechanisms still need substantiating with data. Here we report the examination of the magnetosome material throughout the formation process in a real-time in vivo study of Magnetospirillum gryphiswaldense, strain MSR-1. Transmission EM and x-ray absorption spectroscopy studies reveal that full-sized magnetosomes are seen 15 min after formation is initiated. These immature magnetosomes contain a surface layer of the nonmagnetic iron oxide-phase hematite. Mature magnetite is found after another 15 min, concurrent with a dramatic increase in magnetization. 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subjects Absorption spectroscopy
Bacteria
Biological Sciences
Biomineralogy
Catalysis
Chemical precipitation
Circular Dichroism - methods
Crystals
Ferrosoferric Oxide - analysis
Ferrosoferric Oxide - metabolism
Genetics
High temperature
Inclusion Bodies - chemistry
Inclusion Bodies - metabolism
Inductive reasoning
Iron oxides
Magnetic fields
Magnetics
Magnetite
Magnetization
Magnetosomes
Magnetospirillum
Magnetospirillum - growth & development
Magnetospirillum - metabolism
Magnetospirillum - ultrastructure
Microscopy, Electron, Transmission
Mineralization
Minerals
Nanoparticles
Nanoparticles - analysis
Proteomics
Spectrum analysis
X-Rays
title Rapid magnetosome formation shown by real-time x-ray magnetic circular dichroism
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