We present a model of sedimentation in a subsiding fluvio-deltaic basin with steady sediment
supply and unsteady base level. We demonstrate that mass transfer in a fluvio-deltaic basin
is analogous to heat transfer in a generalized Stefan problem, where the basin's shoreline
represents the phase front. We obtain a numerical solution to the governing equations
for sediment transport and deposition in this system via an extension of a deforming-grid
technique from the phase-change literature. Through modification of the heat-balance
integral method, we also develop a semi-analytical solution, which agrees well with the
numerical solution. We construct a space of dimensionless groups for the basin and perform a
systematic exploration of this space to illustrate the influence of each group on the shoreline
trajectory. Our model results suggest that all subsiding fluvio-deltaic basins exhibit a standard
autoretreat shoreline trajectory in which a brief period of shoreline advance is followed by
an extended period of shoreline retreat. Base-level cycling produces a shoreline response that
varies relative to the autoretreat signal. Contrary to previous studies, we fail to observe either
a strong phase shift between shoreline and base level or a pronounced attenuation of the
amplitude of shoreline response as the frequency of base-level cycling decreases. However, the
amplitude of shoreline response to base-level cycling is a function of the basin's age.