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Estuaries as complex systems
Estuaries provide a complex of habitats of which tidal waters, sand
and mud flats and saltmarshes
are the primary habitats. Sand and shingle structures can be associated with
them and in some cases provide the shelter necessary for the development of
the primary habitats. Estuaries are usually defined as:
- "a semi-enclosed coastal body of water which has a free connection
to the open sea and within which sea water is measurably diluted with fresh
water derived from land drainage" (Pritchard
1952) or;
- "an inlet of the sea reaching into a river valley as far as the upper
limit of tidal rise" (Fairbridge 1980).
Estuaries are most extensive in coastal areas with macro-meso tidal
range and/or an abundant supply of sediment, in Europe these are
especially significant around the southern North Sea.
Although not considered as a separate section in the context of this guide,
the individual habitats, transitions
between them and the plants and animals associated with them are key concerns.
This is especially true where managed
realignment is being considered as there is often a trade off as
one habitat (such as coastal
grazing marsh) is replaced by another (saltmarsh).
This has important knock-on effects on the habitats and species at a particular
site, which may affect their conservation status.
References
Fairbridge, R.W.
1980.
The estuary its definition and geodynamic cycle
.
In: Chemistry and Biogeochemistry of Estuaries, ed.Olausson, E. & Cato, I.Wiley, New York, 1-35.
Pritchard, D.
1952.
.
Advances in Geophysics, 1., 243-280.
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