We study theoretically the contribution of thermal fluctuations to the
linear theological spectrum of lyotropic smectic A phases at low freq
uencies. The fluctuations are treated at the Gaussian level; their hyd
rodynamics is controlled by the undulation/baroclinic mode. In the lay
er-over-layer sliding geometry, we find an anomalous elasticity varyin
g as /omega/; the corresponding viscous drag is enhanced logarithmical
ly. For other shear geometries we find contributions to the dissipatio
n and elasticity that are in practice small (though formally divergent
when the layer spacing is taken to zero). The connection between thes
e results and those given previously for thermotropic smectics, and fo
r block copolymers, is discussed. We outline the possible experimental
significance of our findings for the rheology of both aligned and pol
ydomain smectics.