IntroductionStepped terrace sequences or terrace staircases (TSCs) are defined as remnants of the former floodplains within a fluvial system that are fossilized at different elevations above the present-day river channel (Bull, 2008;Pazzaglia, 2013). Formation of the TSCs was dependent on various factors. Climate-induced changes in the sediments and water flux formed cycles of aggradation and incision; therefore, the stratigraphy of the floodplains reflect the changes in the regional hydrological regime at various time-scales (Faust and Wolf, 2017). Floodplains are also known to adapt and form in response to major and long-term fluctuations in the global climate, such as stadial-interstadial cycles, i.e. marine isotope stages (