We study the pressure induced phase transformation of BeO using a first-pri
nciples pseudopotential method within the local-density-functional approxim
ation, and find a transition sequence from wurtzite to zinc blende, and the
n to rocksalt. With the generalized-gradient approximation for the exchange
-correlation potential, we find the transition pressures to be increased si
gnificantly, without altering the transition sequence. The wurtzite structu
re transforms into the zinc-blende structure at 91 GPa, while the zinc-blen
de-to-rocksalt transition occurs at 147 GPa. This unusual transition sequen
ce is attributed to the large charge asymmetry and the small bond length of
BeO.