Uptake of iron in the halotolerant alga Dunaliella salina is mediated by a transferrin-like protein (TTf), which binds and internalizes Fe 31 ions. Recently, we found that iron deficiency induces a large enhancement of iron binding, which is associated with accumulation of three other plasma membrane proteins that associate with TTf. In this study, we characterized the kinetic properties of iron binding and internalization and identified the site of iron internalization. Iron deficiency induces a 4-fold increase in Fe binding, but only 50% enhancement in the rate of iron uptake and also increases the affinity for iron and bicarbonate, a coligand for iron binding. These results indicate that iron deprivation leads to accumulation and modification of iron-binding sites. Iron uptake in iron-sufficient cells is preceded by an apparent time lag, resulting from prebound iron, which can be eliminated by unloading iron-binding sites. Iron is tightly bound to surface-exposed sites and hardly exchanges with medium iron. All bound iron is subsequently internalized. Accumulation of iron inhibits further iron binding and internalization. The vacuolar inhibitor bafilomycin inhibits iron uptake and internalization. Internalized iron was localized by electron microscopy within vacuolar structures that were identified as acidic vacuoles. Iron internalization is accompanied by endocytosis of surface proteins into these acidic vacuoles. A novel kinetic mechanism for iron uptake is proposed, which includes two pools of bound/compartmentalized iron separated by a rate-limiting internalization stage. The major parameter that is modulated by iron deficiency is the iron-binding capacity. We propose that excessive iron binding in iron-deficient cells serves as a temporary reservoir for iron that is subsequently internalized. This mechanism is particularly suitable for organisms that are exposed to large fluctuations in iron availability.Iron is an essential element for survival for all living organisms, including photosynthetic organisms that have a special requirement for iron as a cofactor of multiple elements in their electron transport system. Because of its low solubility in aerobic solutions, iron is recognized as a major limiting factor for proliferation of plants and algae. To counterbalance iron limitation, photosynthetic organisms evolved efficient high-affinity iron uptake mechanisms that are induced under iron limitation. Two major mechanisms of iron acquisition studied in plants are based either on reduction of organic ferric iron chelates, via a membrane-associated ferrireductase (strategy I plants), or on release of phytosiderophores that bind ferric ions and introduce them into the cell via a special receptor (strategy II plants; Mori, 1999;Curie and Briat, 2003;