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Investigation of iron mineral formation by dissimilatory alcalophilic bacterium Geoalkalibacter ferrihydriticus using Mössbauer spectroscopy

  • Proceedings of the XIth International Conference “Mössbauer Spectroscopy and Its Applications”
  • Published:
Bulletin of the Russian Academy of Sciences: Physics Aims and scope

Abstract

Formation of iron-bearing minerals by the dissimilatory alcalophilic bacterium Geoalkalibacter ferrihydriticus (strain Z-0531) under controlled laboratory conditions was studied using Mössbauer spectroscopy. Strain Z-0531 was isolated from bottom sediments of Lake Khadyn (Tyva, Russia), a soda lake. The effect of the concentration of amorphous iron hydroxide (AFH) and anthraquinone-2,6-disulfonate (quinone) added to the medium was studied along with the effect of the incubation time on iron reduction.

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Authors and Affiliations

  1. Faculty of Physics, Moscow State University, Moscow, 119911, Russia

    N. I. Chistyakova, V. S. Rusakov, K. A. Nazarova & A. A. Shapkin

  2. Vinogradskii Institute of Microbiology, Russian Academy of Sciences, pr. 60-letiya Oktyabrya 7/2, Moscow, 117312, Russia

    T. N. Zhilina & D. G. Zavarzina

Authors
  1. N. I. Chistyakova
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  2. V. S. Rusakov
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  3. K. A. Nazarova
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  4. A. A. Shapkin
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  5. T. N. Zhilina
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  6. D. G. Zavarzina
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Corresponding author

Correspondence to N. I. Chistyakova.

Additional information

Original Russian Text © N.I. Chistyakova, V.S. Rusakov, K.A. Nazarova, A.A. Shapkin, T.N. Zhilina, D.G. Zavarzina, 2010, published in Izvestiya Rossiiskoi Akademii Nauk. Seriya Fizicheskaya, 2010, Vol. 74, No. 3, pp. 433–437.

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Chistyakova, N.I., Rusakov, V.S., Nazarova, K.A. et al. Investigation of iron mineral formation by dissimilatory alcalophilic bacterium Geoalkalibacter ferrihydriticus using Mössbauer spectroscopy. Bull. Russ. Acad. Sci. Phys. 74, 402–406 (2010). https://doi.org/10.3103/S1062873810030251

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  • DOI: https://doi.org/10.3103/S1062873810030251

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