Stratigraphical time, temporality and change have frequently been studied and theorized through dichotomy, that is two opposed, “either/or” views. Linear versus cyclical and the principles of uniformitarianism versus catastrophism are classic examples. This paper aims to look beyond these simple tensions. It utilizes sequence stratigraphy as a lens to re-view established dichotomies and to explore the potential for a more paradoxical “both/and” interpretation. The main finding is that the two opposed linear versus cyclical views can be reconceived as one synthesized sinusoidal view; other dichotomies are re-viewed which allow for spatiotemporal explanation and prediction.