Lagoons in the UK are essentially bodies of saline water
partially separated from the adjacent sea. They may be
natural or artificial. Lagoons retain a proportion of their
seawater at low tide and may develop as brackish, fully saline or
hyper-saline water bodies. The largest lagoon in the UK is in
excess of 800ha (Loch of Stenness) although the rest are much
smaller and some are less than 1ha. Lagoons can contain a
variety of substrata, often soft sediments which in turn may
support tasselweeds and stoneworts as well as filamentous green and
brown algae. In addition lagoons contain invertebrates rarely
found elsewhere. They also provide important habitat for
waterfowl, marshland birds and seabirds. The flora and invertebrate
fauna present can be divided into three main components: those that
are essentially freshwater in origin, those that are
marine/brackish species and those that are more specialist lagoonal
species. The presence of certain specialist plants and
animals make this habitat important to the UK's overall
biodiversity.
There are several different types of lagoons, ranging from
those separated from the adjacent sea by a barrier of sand or
shingle (typical lagoons), to those arising as ponded waters in
depressions on soft sedimentary shores, to those separated by a
rocky sill or artificial construction such as a sea wall. Sea
water exchange in lagoons occurs through a natural or man-modified
channel or by percolation through, or overtopping of, the
barrier. The salinity of the systems is determined by various
levels of freshwater input from ground or surface waters. The
degree of separation and the nature of the material separating the
lagoon from the sea are the basis for distinguishing several
different physiographic types of lagoon.
Although they can be of conservation value and are
eligible for designation as SSSIs, artifical lagoons are excluded
from SAC selection.