Motivated by mounting evidence for the presence of magnetic fields in the a
tmospheres of "normal" early-type main-sequence stars, we investigate the v
arious possible modes of dynamo action in their convective core. Working wi
thin the framework of mean field electrodynamics, we compute alpha (2) and
alpha (2)Omega dynamo models and demonstrate that the transition from the f
ormer class to the latter occurs smoothly as internal differential rotation
is increased. Our models also include a magnetic diffusivity contrast betw
een the core and radiative envelope. The primary challenge facing such mode
ls is to somehow bring the magnetic field generated in the deep interior to
the stellar surface. We investigate the degree to which thermally driven m
eridional circulation can act as a suitable transport agent. In all models
with strong core-to-envelope magnetic diffusivity contrast-presumably close
st to reality-whenever circulation is strong enough to carry a significant
magnetic flux, it is also strong enough to prevent dynamo action. Estimates
of typical meridional circulation speeds indicate that this regime is like
ly not attained in the interior of early-type main-sequence stars. Dynamo a
ction then remains highly probable, but an alternate mechanism must be soug
ht to carry the magnetic field to the surface.