All known forms of life require iron, which usually exists in Fe(II) or Fe(III) oxidation states. Many
proteins in living beings contain iron(III) centers. Examples of such
metalloproteins include
oxyhemoglobin,
ferredoxin, and the
cytochromes. Many organisms, from bacteria to humans, store iron as microscopic crystals (3 to 8 nm in diameter) of
iron(III) oxide hydroxide, inside a shell of the protein
ferritin, from which it can be recovered as needed. Insufficient iron in the human diet causes
anemia. Animals and humans can obtain the necessary iron from foods that contain it in assimilable form, such as meat. Other organisms must obtain their iron from the environment. However, iron tends to form highly insoluble iron(III) oxides/hydroxides in aerobic (
oxygenated) environment, especially in
calcareous soils.
Bacteria and
grasses can thrive in such environments by secreting compounds called
siderophores that form soluble complexes with iron(III), that can be reabsorbed into the cell. (The other plants instead encourage the growth around their roots of certain bacteria that
reduce iron(III) to the more soluble iron(II).) The insolubility of iron(III) compounds is also responsible for the low levels of iron in seawater, which is often the limiting factor for the growth of the microscopic plants (
phytoplankton) that are the basis of the marine food web. of aqueous iron ==Iron(III) salts and complexes==