The cooling of the protoplanetary nebula is controlled largely by the opacity of dust grains. Usually nebula structure models employ standard opacity tables calculated for ensembles of micron-sized dust grains, which are assumed to dominate the opacity. In a recent paper, Morfill (1988, Icarus, in press) calculated the radial structure of viscous accretion disks, assuming that “large” millimeter-sized dust particles dominate the opacities. Such disks have an inner “transition zone,” the structure of which is controlled by evaporation and condensation of refractory material. We examine this hot inner region (at temperatures around 1500° K, where refractory material can evaporate) and conclude that the transition zone may evolve through a number of heating and cooling phases. The physical process is the following: If excess energy is supplied, the nebula heats up, and small refractory dust grains evaporate. This lowers the opacity and the nebula cools again. As the gas becomes cooler, the refractory vapor recondenses on surviving (larger) dust particles. This increases the mean particle size, as well as the opacity, and the nebula can heat up once more. This starts the cycle of evaporation up again, etc. In this way, the transition zone may remain at a mean temperature of ∼1500°K, with rapid fluctuations around this mean value occurring. Simple model calculations give temperature fluctuation rates of several 10s of degrees per hour, about 3 to 4 orders of magnitude higher than the temperature cycling due to convective transport. The fluctuations are damped and need to be triggered by short-term low-power heating events. It is possible that, for instance, lightning discharges or rapid magnetic reconnection events might provide such trigger action. There is a great deal of direct evidence of rapid heating and cooling events in meteoritic material, and it is suggested that the above processes may help us to understand some aspects of these observations.