“…On a wider geographical scale, climatic factors (abiotic) including temperature and precipitation have an association with carbon storage 9,30 , while the local or regional hydrological system, such as freshwater flow or the tidal regime, controls porewater salinity in the sediment 9,37,39,40 , which, in turn, influences plant growth, stand structure and ecosystem productivity 41 and therefore blue carbon storage. Sediment salinity also controls total sediment nutrients 39 (nitrogen, phosphorus and total organic matter), as well as the distribution of the plant species 42 and, hence, their functional traits. For example, low-salinity areas are rich in plant species with a higher potential for photosynthetic nitrogen use efficiency 43 , resulting in higher dry matter content and higher growth form (maximum canopy height) compared to plant species in high-salinity areas.…”