Context
Coastal saltmarshes in the UK (also known as 'merse' in
Scotland) comprise the upper, vegetated portions of intertidal
mudflats, lying approximately between mean high water neap tides
and mean high water spring tides.
Saltmarshes are usually restricted to comparatively sheltered
locations in five main physiographic situations: in estuaries, in
saline lagoons, behind barrier islands, at the heads of sea lochs,
and on beach plains. The development of saltmarsh vegetation
is dependent on the presence of intertidal mudflats.
Communities are additionally affected by differences in climate,
the particle size of the sediment and, within estuaries, by
decreasing salinity in the upper reaches.
The characteristic vegetation consists of a limited number of
halophytic (salt tolerant) species adapted to regular immersion by
the tides. A natural saltmarsh system shows a clear zonation
according to the frequency of inundation. At the lowest level
the pioneer glassworts Salicornia spp. can withstand
immersion by as many as 600 tides per year, while transitional
species of the upper marsh can only withstand occasional
inundation.
Saltmarshes are an important resource for wading birds and
wildfowl. Areas with high structural and plant diversity,
particularly where freshwater seepages provide a transition from
fresh to brackish conditions, are particularly important for
invertebrates. Saltmarshes also provide sheltered nursery
sites for several species of fish.
Interpretation
58% of saltmarsh features reported are in favourable
condition. This is about the average for marine and coastal
features, above the average for all habitat features and just above
the average for all features combined. 62% of A/SSSI features
reported are in favourable condition and 6% are
unfavourable-recovering. 43% of the SAC features reported are
in favourable condition. Data from the SAC series indicate
that the 'Salicornia' feature seems to be in poorer
condition than the 'Atlantic saltmeadow' feature.
Coastal squeeze is a major cause of unfavourable condition in
this reporting category. Coastal squeeze occurs when sea
defences prevent vegetation migrating landwards in response to
sea-level rise. The result is a loss of shoreline
habitats. Inappropriate coastal management includes the use
of rock armour or groynes that interrupt sediment transport along
the coast and therefore natural coastal processes. Coastal
squeeze and inappropriate coastal management are being addressed in
England through shoreline management plans, estuary strategies and
through other mechanisms such as high level biodiversity targets
within the Environment Agency. However, much of this has a
long lead-in time and outcomes will be constrained by strategic
considerations outwith the control of the country conservation
agencies.
Water quality also affects habitats in the intertidal
zone. Pollution arises from point sources, such as sewage
treatment outfalls, or diffuse sources such as agricultural
run-off. This is in part being addressed through a review of
consents for discharges being carried out and for plans to increase
tertiary treatment in waste water treatment works. Recent
work indicates water quality may be more important for the
condition of saltmarshes and mudflats than hitherto recognised, and
links between condition assessments and water quality issues need
to be strengthened.
Agricultural operations may also cause unfavourable condition,
as can under- or over-grazing. Saltmarshes are affected by
the difficulties of obtaining sustainable grazing at appropriate
levels in such areas.