Magnetotactic bacteria (MTB) represent a wide range of Gram-negative prokaryotes ubiquitous in freshwater and marine aquatic habitats1. These bacteria share the ability to produce magnetic crystals made of either magnetite (Fe3O4) or greigite (Fe3S4), which are in most cases assembled into chains inside the cells. This particular structural motif is due to the presence of several specific proteins acting both in the cytoplasm of the bacteria and on the lipid membrane that surrounds each crystal2. Each individual crystal and its surrounding membrane vesicle is called a magnetosome and is ranging in size from about 30 to 50 nm in Magnetospirillum species3. Because of the chain arrangement of magnetosomes, these bacteria possess a permanent magnetic dipole moment that makes them align passively with externally applied magnetic fields. Therefore, these bacteria actively swim along magnetic field lines, acting as self-propelled micro-compasses presumably to more effectively locate the most favorable conditions (e.g., O2 concentration) for growth.
An interesting property of MTB is their ability to regulate both the chemistry and the crystallography of their magnetosome crystals. Most strains produce relatively high purity crystals of either magnetite or greigite, although some biomineralize both minerals4. In all cases, the bacteria are able to precisely control the size and the shape of their single magnetic domain crystals. This explains why a great amount of research is undertaken to develop a better understanding of how MTB perform this biomineralization process. Understanding this process might allow the researchers to tailor-make magnetic nanocrystals for many commercial and medical applications.
A substantial obstacle to extensive research on MTB has been the difficulty of growing them in the laboratory. Most species, including the strains used in this work, are obligately microaerophilic when grown with O2 as a terminal electron acceptor. This explains why these bacteria are most often found at the transition zone between oxic and anoxic conditions (the oxic-anoxic interface, OAI). This clearly shows that MTB have precise O2 concentration requirements which obviously needs to be taken into account when devising growth media for these organisms. Moreover, the great existing diversity of MTB implies that different strains will need different types of chemical gradients and nutrients to achieve optimal growth.
In this work, we describe the methods for growing three of the most widely studied MTB: Magnetospirillum magneticum (strain AMB-1), M. magnetotacticum (MS-1) and M. gryphiswaldense (MSR-1). These species phylogenetically belong to the Alphaproteobacteria class in the Proteobacteria phylum, are helical in morphology and possess a polar flagellum at each end of the cell. We provide the protocols for growing strain MSR-1 in both liquid and O2 concentration gradient semi-solid media, based on previously published medium recipes5,6. We also present a detailed protocol for growing strains AMB-1 and MS-1 in modified Magnetic Spirillum Growth Medium (MGSM)7.