A number of recently discovered extrasolar planet candidates have surp
risingly small orbits, which may indicate that considerable orbital mi
gration takes place in protoplanetary systems. A natural consequence o
f orbital migration is for a series of planets to be accreted, destroy
ed, and then thoroughly mixed into the convective envelope of the cent
ral star: We study the ramifications of planet accretion for the final
main-sequence metallicity of the star. If maximum disk lifetimes are
on the order of similar to 10 Myr, stars with masses near 1.0 M-circle
dot are predicted to have virtually no metallicity enhancement. On th
e other hand, early F-and late A-type stars with masses M- approximat
e to 1.5-2.0 M circle dot can experience significant metallicity enhan
cements due to their considerably smaller convection zones during the
first 10 Myr of pre-main-sequence evolution. We show that the metallic
ities of an aggregate of unevolved F stars are consistent with an aver
age star accreting similar to 2 Jupiter-mass planets from a protoplane
tary disk having a 10 Myr dispersal time.