Magnetotactic bacteria (MTB) synthesize unique organelles termed "magnetosomes," which are membraneenclosed structures containing crystals of magnetite or greigite. Magnetosomes form a chain around MamK cytoskeletal filaments and provide the basis for the ability of MTB to navigate along geomagnetic field lines in order to find optimal microaerobic habitats. Genomes of species of the MTB genus Magnetospirillum, in addition to a gene encoding the tubulin-like FtsZ protein (involved in cell division), contain a second gene termed "ftsZ-like," whose function is unknown. In the present study, we found that the ftsZ-like gene of Magnetospirillum gryphiswaldense strain MSR-1 belongs to a 4.9-kb mamXY polycistronic transcription unit. We then purified the recombinant FtsZ-like protein to homogeneity. The FtsZ-like protein efficiently hydrolyzed ATP and GTP, with ATPase and GTPase activity levels of 2.17 and 5.56 mol phosphorus per mol protein per min, respectively. The FtsZ-like protein underwent GTP-dependent polymerization into long filamentous bundles in vitro. To determine the role of the ftsZ-like gene, we constructed a ftsZ-like mutant (⌬ftsZ-like mutant) and its complementation strain (⌬ftsZ-like_C strain). Growth of ⌬ftsZ-like cells was similar to that of the wild type, indicating that the ⌬ftsZ-like gene is not involved in cell division. Transmission electron microscopic observations indicated that the ⌬ftsZ-like cells, in comparison to wild-type cells, produced smaller magnetosomes, with poorly defined morphology and irregular alignment, including large gaps. Magnetic analyses showed that ⌬ftsZ-like produced mainly superparamagnetic (SP) magnetite particles, whereas wildtype and ⌬ftsZ-like_C cells produced mainly single-domain (SD) particles. Our findings suggest that the FtsZ-like protein is required for synthesis of SD particles and magnetosomes in M. gryphiswaldense.Magnetotactic bacteria (MTB) can orient themselves along geomagnetic field lines and search for microaerophilic environments. These capabilities are based on unique prokaryotic organelles termed magnetosomes (3). Magnetosomes are nanometer-size magnetic particles of iron oxide (magnetite; Fe 3 O 4 ) or iron sulfide (greigite; Fe 3 S 4 ) (4, 5, 45), enclosed within intracytoplasmic vesicles of the magnetosome membrane (MM) (3, 43). Magnetosome formation is a complex process involving vesicle formation, iron transportation, nucleation and growth of magnetite crystals, and their assembly into chain-like structures. A model for magnetosome formation has been proposed by Komeili (18) and Schüler (44). According to this model, magnetosome vesicles are invaginated from the inner membrane, and protein sorting to the MM occurs concurrently. The protein MamA was suggested to activate magnetosome vesicles for magnetite biomineralization (19). With the help of the MamK and MamJ proteins, the membrane invaginations are then assembled into a chain structure. The bacterial actin-like MamK can form filaments required for maintaining magnetosome organization a...