Skip to main content

Bacterial magnetosomes: microbiology, biomineralization and biotechnological applications

Abstract

Magnetotactic bacteria orient and migrate along geomagnetic field lines. This ability is based on intracellular magnetic structures, the magnetosomes, which comprise nanometer-sized, membrane-bound crystals of the magnetic iron minerals magnetite (Fe3O4) or greigite (Fe3S4). Magnetosome formation is achieved by a mineralization process with biological control over the accumulation of iron and the deposition of the mineral particle with specific size and orientation within a membrane vesicle at specific locations in the cell. This review focuses on the current knowledge about magnetotactic bacteria and will outline aspects of the physiology and molecular biology of the biomineralization process. Potential biotechnological applications of magnetotactic bacteria and their magnetosomes as well as perspectives for further research are discussed.

This is a preview of subscription content, access via your institution.

Author information

Authors and Affiliations

Authors

Additional information

Received: 2 December 1998 / Received revision: 2 March 1999 / Accepted: 5 March 1999

Rights and permissions

Reprints and Permissions

About this article

Cite this article

Schüler, D., Frankel, R. Bacterial magnetosomes: microbiology, biomineralization and biotechnological applications. Appl Microbiol Biotechnol 52, 464–473 (1999). https://doi.org/10.1007/s002530051547

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1007/s002530051547

Keywords

  • Fe3O4
  • Magnetite
  • Biological Control
  • Field Line
  • Magnetic Structure