The CorA Mg
2+
channel is present in about 50% of bacteria and many archaea. Its ubiquitous eukaryotic homolog is Mrs2, the mitochondrial Mg
2+
channel. Physiologically, CorA mediates the influx of Mg
2+
down its electrochemical gradient. It can also mediate the influx of Ni
2+
and Co
2+
but only at concentrations that are toxic to the cell. A subclass of the CorA superfamily in the bacteria mediates the efflux of Zn
2+
. The sequence analysis of the CorA superfamily shows a complete lack of homology to any other protein. The crystal structure of CorA confirms its unique nature. CorA is a homopentamer shaped like a funnel with the stem of the funnel within the membrane. Each monomer has two transmembrane segments at the C terminus. All prokaryotic CorA proteins have the same basic structure. A 250–290 amino acid cytosolic N‐terminal domain is followed by transmembrane segment 1, which is followed by a nine amino acid periplasmic loop. This loop is followed by the transmembrane segment 2. Neither transmembrane segment contains any charged amino acids. The C‐terminal cytosolic tail of CorA is almost always six amino acids in length and contains three or four arginine and/or lysine residues. In the structures currently available, the Mg
2+
‐conducting pore is formed completely by transmembrane segment 1. The cytosolic domain is formed of a seven‐stranded antiparallel β sheet flanked on both sides by three α helices (α
1–3
β
1–7
α
4–6
). This domain is followed by the 100‐Å‐long α
7
helix, which forms most of the inner face of the funnel and transmembrane segment 1. In the cytosolic domain, a Mg
2+
cation is bound between an aspartate residue in the α
7
helix of one monomer and the α
3
helix of the adjacent monomer, giving five bound Mg
2+
cations per channel. These bound ions seem poised to act as ‘sensors’ of intracellular Mg
2+
, and their dissociation from the channel is proposed to allow the monomers to rotate apart, thus opening the channel.