Offshore Possible SACs
A
possible SAC (pSAC) is a site that has
had Cabinet Committee approval to go to
consultation. A site remains a pSAC until it is submitted
to the European Commission. There are currently six possible
SACs.
North Norfolk Sandbanks
and Saturn Reef and
Wyville Thomson Ridge
were subject to public consultation from
December 2007 to March 2008 but have not yet
been submitted to the European Commission. They therefore remain
pSACs. JNCC are working with Defra to resolve issues regarding
these two sites that were raised during the consultation. These
sites will be submitted to the European Commission as soon as
possible. North Norfolk Sandbanks is in the Southern North Sea and
has been recommended for its
sandbank and the biogenic
Sabellaria spinulosa reef. Wyville Thomson Ridge is located off
northern Scotland and has been recommended for its bedrock and
stony
reef
communities.
Inner Dowsing, Race Bank and North
Ridge,
Haisborough, Hammond and
Winterton,
Bassurelle Sandbank and
North-West Rockall Bank were
consulted
upon from November 2009-February 2010. JNCC are currently
analysing the consultation responses and a report of the
consultation will be issued in due course. Inner Dowsing, Race Bank
and North Ridge, Haisborough, Hammond and Winterton and Bassurelle
Sandbank have all been recommended for their
sandbank
communities. In addition, Inner Dowsing, Race Bank and North Ridge
has been recomended for it's biogenic
Sabellaria spinulosa
reef.
North-West Rockall Bank has been recommended for it's biogenic cold
water coral, stony and bedrock
reef communities.
JNCC provides
advice on the management of Annex I habitats and
Annex II species protected within offshore SACs to Defra and other
Competent Authorities. JNCC is not responsible for the management
of sites, or for producing management plans for them. These are the
responsibilites of the Competent Authorities.
There are three downloads associated with each pSAC:
- SAC Selection Assessment Document - Detailing
the scientific justification for the site;
- Draft Conservation Objectives and Advice on
Operations - Providing, in draft format, guidance to the
Competent Authorities on managing human activities on the
site;
- GIS boundary for the pSAC - Please note that
boundaries for future sites are not fixed until the site has been
submitted to the European Commission. Therefore this site boundary
may change.
North Norfolk Sandbanks and Saturn Reef
The North Norfolk Sandbanks consist of 10 main
sandbanks and a number of smaller banks, which
collectively form the most extensive example of offshore linear
ridge sandbanks in UK waters. The banks are home to invertebrate
communities typical of sandy sediments, such as polychaete
worms, crabs and
brittlestars. One particular polychaete, the ross
worm Sabellaria spinulosa, is capable of
creating biogenic reef structures through
consolidating thousands of fragile sand-tubes to create a solid
structure that rises from the seabed. The Saturn reef is such a
structure.
North
Norfolk Sandbanks and Saturn Reef SAC Selection Assessment
Document (1,008 KB)
North Norfolk Sandbanks and Saturn Reef Draft Conservation
Objectives and Advice on Operations (642 KB)
North Norfolk Sandbanks and Saturn Reef pSAC
boundary
Haisborough, Hammond and Winterton
|
Please note that this site crosses the 12 nautical mile
boundary and JNCC are progressing it jointly with Natural
England.
|
The possible SAC boundary for Haisborough, Hammond
and Winterton contains a collection of
sandbanks off the north-east coast of Norfolk. On
the tops of the banks small numbers of polychaete
worms and amphipods are present. In the
troughs between the banks where the sediments are more stable
bryozoans, hydroids and
sea anemones have settled.
Bivalves and crustaceans are
found throughout the site.
Haisborough, Hammond and
Winterton SAC Selection Assessment Document (1,098 KB)
Haisborough, Hammond and Winterton Draft Conservation Objectives
and Advice on Operations (1,118 KB)
Haisborough, Hammond and Winterton pSAC
boundary
Bassurelle Sandbank
Bassurelle Sandbank is a linear sandbank
in the Dover Strait which straddles the boundary between UK and
French waters and the possible SAC is aligned with the French site
"Ridens et dunes hydrualiques du Detroit du Pas de Calais".
Sandwaves and megaripples are common on the bank and biological
communities are dominated by polychaete worms
including the tube-worm Lagis koreni and bristleworm
Spiophanes bombyx. Sand eels and
weever fish are characteristic of the fish species
present. Further information on the 2005-2006 Eastern English Channel survey that
collected data to support the recommendation of Bassurelle Sandbank
is also available.
Bassurelle
Sandbank SAC Selection Assessment Document (719 KB)
Bassurelle
Sandbank Draft Conservation Objectives and Advice on Operations
(370 KB)
Bassurelle Sandbank pSAC boundary
North-West Rockall Bank
Rockall Bank is an offshore bank in the North-East Atlantic. The
north-west area of Rockall Bank is covered in a layer of fine
sediment, gravel, cobbles and boulders of glacial origin. Some of
these are shaped into characteristic 'ploughmark' formations,
formed by the ploughing movement of icebergs through the seabed at
the end of the last ice age. Animals present include the
coral Caryophyllia sp.,
squat lobsters, brittlestars and
the bluemouth red fish. In between areas of
stony reef are large patches of cold water
coral reef made up of Lophelia
pertusa and Madrepora
oculata, interspersed with other species such as
erect sponges and pencil urchins.
Rockall Bank is potentially one of the most extensive sites of cold
water coral reef in UK waters. Harbour porpoise
are present at North-West Rockall Bank and are included as a
non-qualifying feature. Further details of the 2005-2006 Strategic Environmental Assessment
surveys that visited and collected data at North-West Rockall
Bank are also available.
North-West
Rockall Bank SAC Selection Assessment Document (3,091 KB)
North-West
Rockall Bank Draft Conservation Objectives and Advice on
Operations (727 KB)
North-West Rockall Bank pSAC boundary
Wyville Thomson Ridge
Wyville Thomson Ridge
is a rock ridge at the northern end of Rockall Trough rising from
over 1000 metres at its deepest point to 400 metres at the summit.
Along the ridge there are large areas of stony
reef, thought to have been formed by the ploughing
movement of icebergs through the seabed at the end of the last ice
age. Bedrock reef is present on the flanks of the
ridge and, due to the differences in water masses, there are
different species compositions on either side. These reef
communities support sea urchins, sea
spiders, sea cucumbers and a range of
colourful sponges and soft
corals. Bottlenose dolphins are present
at Wyville Thomson Ridge and are included as a non-qualifying
feature. Further details of the 2005-2006 Strategic Environmental Assessment
surveys that visited and collected data at Wyville Thomson
Ridge are also available.
Wyville
Thomson Ridge SAC Selection Assessment Document (1,489
KB)
Wyville Thomson Ridge Draft Conservation Objectives and Advice on
Operations (623 KB)
Wyville Thomson Ridge pSAC boundary