Salt marshes are ecosystems of high environmental and economic value that provide a variety of services, including nutrient removal, habitat provision and high rates of carbon sequestration at geological time scales (Barbier et al., 2011;Zedler & Kercher, 2005). As a result of their ability to buffer storm waves, they also provide coastal protection against flooding (e.g., Leonardi et al., 2018;Moller et al., 1999), which led to a worldwide effort to create new salt marshes and/or restore salt marshes that were previously reclaimed for anthropogenic activities to provide long-term and low-cost coastal protection (Temmerman et al., 2013).Salt marshes form when tidal flats increase in elevation with respect to sea-level, through the delivery of fine sediment from rivers and the sea to estuarine accommodation space, which creates newly exposed surfaces that