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to-site and can be substantially lower than 1 cm yr–1 in micro-tidal regions where the tidal trapping of sediment is reduced and/or in areas with low sediment availability (Lovelock et al., ; Ganju et al., ; Jankowski et al., ; Watson et al., ). Global environmental change may also to lead to changes in growth rates, productivity and geographic distribution of different mangrove and marsh species, including the replacement of environmentally sensitive species by those possessing greater climatic tolerance (Krauss et al., ; Reef and Lovelock, ; Coldren et al., ). Processes impacting lateral changes at the marsh boundary including wave erosion are just as important, if not more, than Amazing horse in american flag all over print bedding setvertical accretion rates in determining coastal wetland survival (e.g., Mariotti and Carr, 2014). For most low-lying coastlines, a seaward loss of wetland area due to marsh retreat could be offset by a similar landward migration of coastal wetlands (Kirwan and Megonigal, ; Schile et al., ), this landward migration having the potential to maintain and even increase the extent of coastal wetlands globally (Morris et al., ; Kirwan et al., ; Schuerch et al., ). This natural process will however be constrained in areas with steep topography or hard engineering
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