The pores of ion channel proteins are often modeled as static structur
es. In this view, selectivity reflects rigidly constrained backbone or
ientations. Such a picture is at variance with the generalization that
biological proteins are flexible, capable of major internal motions o
n biologically relevant time scales. We tested for motions in the sodi
um channel pore by systematically introducing pairs of cysteine residu
es throughout the pore-lining segments. Two distinct pairs of residues
spontaneously formed disulfide bonds bridging domains I and II. Nine
other permutations, involving all four domains, were capable of disulf
ide bonding in the presence of a redox catalyst, The results are incon
sistent with a single fixed backbone structure for the pore; instead,
the segments that line the permeation pathway appear capable of sizabl
e motions.