The seabed of inshore areas (defined as within six nautical
miles of the shoreline) is dominated by soft sediment. Where
sublittoral rock habitats occur they tend to be immediately
adjacent to the shore, fringing islands, headlands, open coast and
rocky inlets such as rias and sea lochs. Further offshore,
rocky sublittoral habitats may be present as submerged reefs,
pinnacles and ledges, and are often surrounded by areas of soft
sediment.
Most sublittoral rocky habitats are in areas exposed to water
movement, which keeps the rock surface free of sediment.
Rocky areas in sheltered situations are not as common, but do occur
in Scottish sea lochs as well as the rias of South-west
Britain.
Chalk reefs, which occur in parts of southern Britain and off
the East coast, support a diversity of flora and fauna. This
includes foliose red algae and small brown algae on upward facing
surfaces, turfs of hydroids and bryozoans, and an abundance of
sponges and animals which bore into the soft rock.
Sabellaria alveolata reefs are formed by the
honeycomb worm S. alveolata, a polychaete which constructs
tubes in tightly packed masses with a distinctive honeycomb-like
appearance. Reefs are mainly found on the bottom third of the
shore, but may reach mean high water of neap tides and extend into
the shallow subtidal in places. They form on a variety of
hard substrata, from pebbles to bedrock, in areas with a good
supply of suspended sand grains from which the animals form their
tubes, and include areas of sediment when an attachment has been
established. The British Isles represent the northern
extremity of the range in the North-east Atlantic.
Sabellaria spinulosa reefs comprise dense subtidal
aggregations of this small, tube-building polychaete worm. S.
spinulosa can act to stabilise cobble, pebble and gravel
habitats, providing a consolidated habitat for epibenthic
species. They provide a biogenic habitat that allows many
other associated species to become established.