The first explicit realization of the conjecture that phason dynamics
leads to self-diffusion in quasicrystals is presented for the icosahed
ral Ammann tilings. On short time scales, the transport is found to be
subdiffusive with the exponent beta approximate to 0.57(1), while on
long time scales it is consistent with normal diffusion that is up to
an order of magnitude larger than in the typical room temperature vaca
ncy-assisted self-diffusion. No simple finite-size scaling is found, s
uggesting anomalous corrections to normal diffusion, or existence of a
t least two independent length scales. A connection with transport in
membranes is also noted.