A salt marsh is a type of marsh found in the intertidal transition between land and ocean. They are dominated by halophytic herbaceous plants. They are also called tidal marshes or saltings. 'Ing' is a word of Nordic origin, meaning 'meadow' and saltings made quite rich cattle pasture which was also free of liver fluke (Fasciola hepatica and others). Care should be taken not to confuse 'salting' with 'saltern', which is a salt-house. Salterns were found among salt marshes and are places where brine is evaporated to produced salt.
The sediment in salt marshes is delivered not constantly, as in other types of marshes, but cyclically, owing to the tides. As would be expected at the coast, the sediment is rich in sand, shells, and organic material from the ocean.
The flora of a salt marsh is differentiated into levels according to the plants' individual tolerance of salinity and water table levels. Vegetation found at the water must be able to survive high salt concentrations, periodical submersion, and a certain amount of water movement, while plants further inland in the marsh can sometimes experience dry, low-nutrient conditions.
Salt marshes are quite photosynthetically active and are extremely productive habitats. They serve as depositories for a large amount of organic matter, and are full of decomposition, which feeds a broad food chain of organisms from bacteria to mammals.
In wintertime the saltmarsh looks more open than in summer. More space is seen between reeds as snow falls between them. The water partly freezes, which makes it look rather spectacular.
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