Accretionary marsh levees act as emerging barriers to interior elevation gain

Many small coastal plain watersheds have experienced extensive land clearing and increased sediment loading as coastal populations expand, yet microtidal marsh platforms are failing to keep pace with sea-level rise while adjacent subtidal areas are infilling. Here, we developed sub-decadal records of sedimentation from the shoreline into the salt marsh in watersheds with distinct land-use histories to determine how emerging microtopography may promote this disconnect. We find a divergence in marsh vertical evolution across short distances ( < 10 meters) and timescales ( < 20 years). Rapid accretion at the marsh edge ( > 10 millimeters per year), a product of sediment loading from deforestation and lateral shoreline erosion, is negatively correlated with contemporaneous interior marsh accretion, suggesting an increasingly prominent levee may reduce interior sedimentation by rerouting flow, trapping sediment, or inhibiting vegetation growth. These findings suggest pulses of suspended sediment can temporarily enhance levee prominence in ways that undermine marsh resilience to sea-level rise. Rapid marsh-edge accretion correlates negatively with contemporaneous interior accretion, suggesting that levee growth reduces interior sedimentation by rerouting flow, trapping sediment, or inhibiting vegetative growth, based on sub-decadal sedimentation records from distinct U.S. watersheds.