Magnetospirillum gryphiswaldense and related magnetotactic bacteria form magnetosomes, which are membrane-enclosed organelles containing crystals of magnetite (Fe 3 O 4 ) that cause the cells to orient in magnetic fields. The characteristic sizes, morphologies, and patterns of alignment of magnetite crystals are controlled by vesicles formed of the magnetosome membrane (MM), which contains a number of specific proteins whose precise roles in magnetosome formation have remained largely elusive. Here, we report on a functional analysis of the small hydrophobic MamGFDC proteins, which altogether account for nearly 35% of all proteins associated with the MM. Although their high levels of abundance and conservation among magnetotactic bacteria had suggested a major role in magnetosome formation, we found that the MamGFDC proteins are not essential for biomineralization, as the deletion of neither mamC, encoding the most abundant magnetosome protein, nor the entire mamGFDC operon abolished the formation of magnetite crystals. However, cells lacking mamGFDC produced crystals that were only 75% of the wild-type size and were less regular than wild-type crystals with respect to morphology and chain-like organization. The inhibition of crystal formation could not be eliminated by increased iron concentrations. The growth of mutant crystals apparently was not spatially constrained by the sizes of MM vesicles, as cells lacking mamGFDC formed vesicles with sizes and shapes nearly identical to those formed by wild-type cells. However, the formation of wild-type-size magnetite crystals could be gradually restored by in-trans complementation with one, two, and three genes of the mamGFDC operon, regardless of the combination, whereas the expression of all four genes resulted in crystals exceeding the wild-type size. Our data suggest that the MamGFDC proteins have partially redundant functions and, in a cumulative manner, control the growth of magnetite crystals by an as-yet-unknown mechanism.The ability of magnetotactic bacteria (MTB) to orient in the earth's magnetic field is based on specific organelles, the magnetosomes, which are membrane-enveloped crystals of a magnetic mineral that are arranged in chain-like structures within the cell (5). Magnetosome crystals display a variety of species-specific shapes and sizes, which for most MTB are between 35 and 120 nm (3, 4). In MTB of the genus Magnetospirillum, cubo-octahedral nanocrystals of the magnetic mineral magnetite (Fe 3 O 4 ) are synthesized within magnetosome membrane (MM) vesicles, which are roughly spherical and are formed by invagination from the cytoplasmic membrane prior to magnetite biomineralization (2, 15, 16). The MM is a phospholipid bilayer with a distinctive biochemical composition (8,29,35). In Magnetospirillum gryphiswaldense, a specific set of 20 MM proteins (MMPs) was identified by biochemical and proteomic approaches (9,10,22), and these proteins were speculated to be involved in magnetosome biomineralization (29). However, the individual functions of M...