Cyanobacteria are key contributors to global photosynthetic productivity, and iron availability is essential for cyanobacterial proliferation. While iron is abundant in the earth's crust, its unique chemical properties render it a limiting factor for photoautotrophic growth. As compared to other nonphotosynthetic organisms, oxygenic photosynthetic organisms such as cyanobacteria, algae, and green plants need large amounts of iron to maintain functional PSI complexes in their photosynthetic apparatus. Ferritins and bacterioferritins are ubiquitously present iron-storage proteins. We have found that in the cyanobacterium Synechocystis sp. PCC 6803 (Synechocystis 6803), bacterioferritins are responsible for the storage of as much as 50% of cellular iron. Synechocystis 6803, as well as many other cyanobacterial species, have two bacterioferritins, BfrA and BfrB, in which either the heme binding or di-iron center ligating residues are absent. Purified bacterioferritin complex from Synechocystis 6803 has both BfrA and BfrB proteins. Targeted mutagenesis of each of the two bacterioferritin genes resulted in poor growth under iron-deprived conditions. Inactivation of both genes did not result in a more severe phenotype. These results support the presence of a heteromultimeric structure of Synechocystis bacterioferritin, in which one subunit ligates a diiron center while the other accommodates heme binding. Notably, the reduced internal iron concentrations in the mutant cells resulted in a lower content of PSI. In addition, they triggered iron starvation responses even in the presence of normal levels of external iron, thus demonstrating a central role of bacterioferritins in iron homeostasis in these photosynthetic organisms.Iron serves as a cofactor in a multitude of cellular processes. As such, iron accumulation and storage processes are essential for the survival of all organisms. However, the same redox properties that make iron a valuable cofactor also lead to oxidative interactions resulting in the formation of harmful radicals. Therefore, iron accumulation in the cells is tightly regulated to ensure that very little free iron is present (Kakhlon and Cabantchik, 2002).While iron is abundant in the earth's crust, the bioavailability of iron in the current oxidative terrestrial environment is limited. This is due to the fact that in the presence of dioxygen at neutral pH, iron precipitates as Fe(OH) 3 . As a consequence, the bioavailability of iron limits the proliferation of photosynthetic organisms. Indeed, studies conducted in the Southern Ocean have indicated that iron is a limiting factor for primary photosynthetic productivity (Falkowski et al., 1998). In many of the ecological niches occupied by photosynthetic organisms, iron concentrations are limited to nanomolar levels (Morel and Price, 2003). Surges in the iron concentration due to aeolian dust deposition are transient (Falkowski et al., 1998). To accommodate such an infrequent supply of iron, photosynthetic organisms must have efficient iron storage mec...