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Applied and Environmental Microbiology, September 2009, p. 5586-5591, Vol. 75, No. 17
0099-2240/09/$08.00+0     doi:10.1128/AEM.00490-09
Copyright © 2009, American Society for Microbiology. All Rights Reserved.

Extracellular Iron Biomineralization by Photoautotrophic Iron-Oxidizing Bacteria {triangledown} ,{dagger}

Jennyfer Miot,1* Karim Benzerara,1 Martin Obst,2,3 Andreas Kappler,3 Florian Hegler,3 Sebastian Schädler,3 Camille Bouchez,1 François Guyot,1 and Guillaume Morin1

Institut de Minéralogie et de Physique des Milieux Condensés, UMR 7590, CNRS, Universités Paris 6 et Paris 7, Paris, and IMPMC, 140 Rue de Lourmel, Paris, France,1 BIMR, McMaster University, Hamilton, and Canadian Light Source, 101 Perimeter Road, Saskatoon, Saskatchewan, Canada,2 Geomicrobiology, Center for Applied Geoscience, University of Tuebingen, Sigwartstrasse 10, 72076 Tuebingen, Germany3

Received 27 February 2009/ Accepted 6 July 2009

Iron oxidation at neutral pH by the phototrophic anaerobic iron-oxidizing bacterium Rhodobacter sp. strain SW2 leads to the formation of iron-rich minerals. These minerals consist mainly of nano-goethite ({alpha}-FeOOH), which precipitates exclusively outside cells, mostly on polymer fibers emerging from the cells. Scanning transmission X-ray microscopy analyses performed at the C K-edge suggest that these fibers are composed of a mixture of lipids and polysaccharides or of lipopolysaccharides. The iron and the organic carbon contents of these fibers are linearly correlated at the 25-nm scale, which in addition to their texture suggests that these fibers act as a template for mineral precipitation, followed by limited crystal growth. Moreover, we evidence a gradient of the iron oxidation state along the mineralized fibers at the submicrometer scale. Fe minerals on these fibers contain a higher proportion of Fe(III) at cell contact, and the proportion of Fe(II) increases at a distance from the cells. All together, these results demonstrate the primordial role of organic polymers in iron biomineralization and provide first evidence for the existence of a redox gradient around these nonencrusting, Fe-oxidizing bacteria.


* Corresponding author. Mailing address: IPGP, 140 rue de Lourmel, 75015 Paris, France. Phone: 0033144279832. Fax: 0033144273785. E-mail: miot{at}impmc.jussieu.fr

{triangledown} Published ahead of print on 10 July 2009.

{dagger} Supplemental material for this article may be found at http://aem.asm.org/.


Applied and Environmental Microbiology, September 2009, p. 5586-5591, Vol. 75, No. 17
0099-2240/09/$08.00+0     doi:10.1128/AEM.00490-09
Copyright © 2009, American Society for Microbiology. All Rights Reserved.




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