“…Multiple parameters influence the dynamics of the generation and preservation of sedimentary rocks, challenging their recognition in the stratigraphic record. In continental to marine depositional systems, the type and volume of sediment that may be preserved over geologic time is mainly controlled by the interplay of regional tectonics, eustatic fluctuations, climate, sedimentary supply, ecological boundary conditions, and the intrinsic energy of the environment (Catuneanu, 2006;Fragoso et al, 2022;Holbrook & Miall, 2020;Matenco & Haq, 2020;Miall, 2016;Miall et al, 2021;Strasser et al, 1999Strasser et al, , 2006. These parameters act at various temporal and spatial scales and amplitudes, radically altering the physiography of a sedimentary basin across time and leaving their imprints on the stratigraphic record through cycles at multiple scales (Fragoso et al, 2021).…”