Ca2+ channels display remarkable selectivity and permeability, traditi
onally attributed to multiple, discrete Ca2+ binding sites lining the
pore. Each of the four pore-forming segments of Ca2+ channel al subuni
ts contains a glutamate residue that contributes to high-affinity Ca2 interactions. Replacement of all four P-region glutamates with glutam
ine or alanine abolished micromolar Ca2+ block of monovalent current w
ithout revealing any additional independent high-affinity Ca2+ binding
site. Pairwise replacements of the four glutamates excluded the hypot
hesis that they form two independent high-affinity sites. Systematic a
lterations of side-chain length, charge, and polarity by glutamate rep
lacement with aspartate, glutamine, or alanine weakened the Ca2+ inter
action, with considerable asymmetry from one repeat to another. The P-
region glutamate in repeat I was unusual in its sensitivity to asparta
te replacement but not glutamine substitution. While all four glutamat
es cooperate in supporting high-affinity interactions with single Ca2 ions, they also influence the interaction between multiple divalent c
ations.