“…Once aeolian sedimentation became dominant, the finer fraction of materials sourced from the adjacent stream channel and bank was winnowed away, leaving deposition of the coarser and saltated fraction. This is in line with other sedimentary analyses of PSB from locations above c.7 m AHD (Gale, 2021, p. 7, 2022, p. 2; GML 2021; Player, 2019, p. 7; Quinn et al., 2023; Williams et al., 2012, p. 8; Williams et al., 2014; p. 737, Williams et al., 2021, pp. 7–8), and align with the definition of sedimentary signatures for aeolian reworking evidenced at Agnes Banks (Gale & Wales, 2023, pp.…”