It is shown that the state of "isothermal" homogeneous fluidization can be
linearly unstable to small-amplitude "non-isothermal" disturbances transver
se to the direction of gravity. Conditions for instability of this new mode
are examined and the marginal stability conditions are derived. The underl
ying physical mechanism of the instability is discussed and contrasted with
the widely known particle-phase-inertia driven longitudinal modes of plana
r instability voidage waves.