Coastal salt marshes are dynamic, intertidal ecosystems that are increasingly being recognised for their contributions to ecosystem services, including carbon (C) accumulation and storage. The survival of salt marshes and their capacity to store C under rising sea levels, however, is partially reliant upon sedimentation rates and influenced by a combination of physical and biological factors. In this study, we use several complementary methods to assess short-term (days) deposition and medium-term (months) accretion dynamics within a single marsh that contains three salt marsh vegetation types common throughout southeastern (SE) Australia. br br We found that surface accretion varies among vegetation assemblages, with medium-term (19 months) bulk accretion rates in the upper marsh rush (Juncus) assemblage (1.74g ±g 0.13g mmg yrg '1) consistently in excess of estimated local sea-level rise (1.15g mmg yrg '1). Accretion rates were lower and less consistent in both the succulent (Sarcocornia, 0.78g ±g 0.18g mmg yrg '1) and grass (Sporobolus, 0.88g ±g 0.22g mmg yrg '1) assemblages located lower in the tidal frame. Short-term (6 days) experiments showed deposition within Juncus plots to be dominated by autochthonous organic inputs with C deposition rates ranging from 1.14g ±g 0.41g mgg Cg cmg '2g dg '1 (neap tidal period) to 2.37g ±g 0.44g mgg Cg cmg '2g dg '1 (spring tidal period), while minerogenic inputs and lower C deposition dominated Sarcocornia (0.10g ±g 0.02 to 0.62g ±g 0.08g mgg Cg cmg '2g dg '1) and Sporobolus (0.17g ±g 0.04 to 0.40g ±g 0.07g mgg Cg cmg '2g dg '1) assemblages. br br Elemental (Cg :g N), isotopic (?13C), mid-infrared (MIR) and 13C nuclear magnetic resonance (NMR) analyses revealed little difference in either the source or character of materials being deposited among neap versus spring tidal periods. Instead, these analyses point to substantial redistribution of materials within the Sarcocornia and Sporobolus assemblages, compared to high retention and preservation of organic inputs in the Juncus assemblage. By combining medium-term accretion quantification with short-term deposition measurements and chemical analyses, we have gained novel insights into above-ground biophysical processes that may explain previously observed regional differences in surface dynamics among key salt marsh vegetation assemblages. Our results suggest that Sarcocornia and Sporobolus assemblages may be particularly susceptible to changes in sea level, though quantification of below-ground processes (e.g. root production, compaction) is needed to confirm this.