Special areas of conservation (SAC) is a framework to protect listed habitats and
species. Rare species are known as “site interest features”. The rare maerl and seagrass
reefs were influential in the Fal & Helford region gaining SAC status in 1994, with
both bed communities being included in Conservation Objective 3 of the Fal & Helford
SAC Management Scheme “to maintain the SUBTIDAL SANDBANKS in ‘favourable condition’,
taking account of natural change”.
Eelgrass (Zostera marina) is a species of seagrass that is widespread around the
world. As in the Fal Estuary, it is found on subtidal/sublittoral sandbanks in shallow
water. Eelgrass provides a habitat for a range of invertebrates, sea slugs, cuttlefish,
and fish nurseries. Any activity that disturbs the sediment in which eelgrass grows,
or reduces light levels, puts the species at risk, for example: eutrophication, algal
blooms, and man-made structures that shade benthic habitats or reduce the supply
of sediments for the base of the habitat.
Sea Lettuce (Ulva lactuca) is one of the most well known shallow water seaweeds,
found in both high and low intertidal zones and marshes. Whilst Zostera marina is
hindered by nutrient loading, Ulva lactuca has a much higher tolerance to pollution
with their growth stimulated by the presence of pollutants; this explains their existence
in the Fal Estuary, where there is a high level of anthropogenic activity. In areas
with a high concentration of sea lettuce, other vegetation (such as eelgrass) is
unable to compete for sunlight, preventing photosynthesis and resulting in the decline
of the other vegetation.
This map of the Fal Estuary (Map 1) has highlighted the locations of interesting
features. The north of our survey area was identified as having sublittoral sediment
with eelgrass. In the south, the substrate changed to tide-swept sheltered sublittoral
rock with kelp. The habitat map we produced shows a similar change in habitat along
this area: eelgrass was found in the north of the transect on finer grained sediment,
and to the south we saw the sediment become coarser with some rocky outcrops closer
to the shore.