Subtidal Biotope Complex: Subtidal Mobile Sandbanks
Organic Production and Phytobenthos
Benthic fauna in relation to hydrography
Organic Production and Phytobenthos
The physical environment of subtidal mobile sandbanks with stronger currents is often
too harsh for vegetation to become established; they are less productive with lower levels
of organic matter. However, sheltered subtidal sandbanks may support the sugar kelp Laminaria
saccharina attached to stones and shallow conditions with adequate light will maintain
a microphytobenthic community. Similarly, adequate light conditions will allow maerl to
develop (see Volume V).
Benthic fauna in relation to hydrography
Macrofauna
Mobile sandbanks are colonised by infaunal/epifaunal small crustaceans, polychaetes and
molluscs which are adapted to the changing hydrography and substratum; they are able to
reburrow rapidly following being washed-out of the sediment during storms (Vanosmael et
al, 1982). For example, the body form and mobility of magelonid polychaetes and
species such as Nephtys cirrosa and Micropthalamus similis are well suited
to burrowing in mobile sands. These features indicate that the communities are clearly
shaped by physical rather than biological forces.
The sediment in a mobile sandbank system may range from fine to coarse clean sands, and
the density of individuals and species richness is often highest in the coarsest grade,
mainly due to large numbers of interstitial polychaetes (Vanosmael et al, 1982).
The mean macrobenthic diversity and species richness of clean mobile sandbanks is
generally lower than the surrounding sea bed (reflecting the greater stresses inherent in
these environments) although the fauna is essentially comparable with that of the open
sea. The mouth of the Teign estuary has been noted to only contain Scolelepis squamata,
Eteone longa, Anonides oxycephala, Nemertea indet. and an occasional
juvenile Mytilus edulis in the mobile sandbanks.
Due to the continual sediment disturbance, the community may have a large opportunistic
component with species such as Chaetozone setosa and may be prevented from reaching
a climax community. For example, subtidal areas along the eroding Holderness Coast have
large populations of C. setosa indicating a community held in a disturbed condition
(Allen, in prep.).
The fauna of nearshore sandbanks vary geographically and are often impoverished
extensions of the communities found at exposed intertidal areas, especially where currents
are high and the substratum is clean sand. The MNCR classification of clean mobile
subtidal sands describes the fauna as barren or characterised by Pagurus bernhardus
and Ammodytes species (Connor et al, 1997). However if pockets of silt
develop e.g. between ripples on the sand banks, a richer fauna may develop (Vanosmael et
al, 1982) and substratum with an increased silt content may be characterised by
epifaunal and infaunal echinoderms. As in intertidal areas, species which help to
consolidate the substratum such as the reef forming polychaete Sabellaria spinulosa
will help promote the settlement of other fauna.
The characteristic fauna of the subtidal mobile sandbanks is similar to Petersons
Venus community (in broad terms) which is comparable to the boreal offshore
sand association (Table 3.0) with the number of species reflecting the stability of
the area. Depending on the hydrodynamic regime of the area, the assemblage may also have
elements of the boreal off-shore gravel association of Jones (1950) (Vanosmael
et al, 1982). More stable sandbanks comprised of finer sediments may also resemble
the boreal offshore muddy sand association. Such an association is often
better characterised by less frequent species than by dominant ones, and the interstitial
polychaetes and archiannelids, especially, seem to be characteristic of the communities
described by Petersen (1913) and Jones (1950).
As an example, Vanosmael et al (1982) found that sandbanks off the Dutch coast
were characterised by mobile and rapid-burrowing crustaceans and polychaetes such as Nephtys
cirrosa, Hesionura elongata and Microphthalmus listensis. Sessile tube
building polychaetes were represented by only a small number of individuals.
Hesionura augeneri (an interstitial polychaete) made up 55% of the macrofaunal
population which occurred in the highest densities in the coarser sediments. The
polychaetes Micropthalmus listensis, Nephtys cirrosa and N. hombergii occurred
separately because of differing sediment preferences. The mollusc Spisula elliptica
was common in muddy sand, fine sand and shell gravel banks and the crustaceans, Tanaissus
lilljeborgi and Bathyporeia elegans were the most common species on the sand banks,
both showing a preference for fine sand. The macro-crustacea may be generally more
abundant in finer sediments (Willems et al, 1982a).
Various epifaunal brittle stars are associated with this biotope complex e.g. Amphiura
filiformis which extends its arms up into the water column to feed on suspended
material. The heart urchin Echinocardium cordatum may also be common but replaced
by another heart urchin, Brissopsis lyrifera in siltier areas. Sandeels e.g. Ammodytes
tobianus and A. marinus, are widespread (and Corbins sandeel and the greater
sandeel to a lesser extent) on subtidal mobile sandbanks.
Meiofauna
The meiofauna also form an important component of the sandbank fauna. Interstitial
organisms occur in sediments with a median grain size above 200 µm and polychaetes are
found to be abundant (although they also live in finer sediments) in sediments with a
particle size above 300 µm (Willems et al, 1982a). The meiofauna may be
characterised by low densities of nematodes and high densities of copepods, annelids and
halacarid mites. The meiofauna (particularly nematodes and copepods) are not correlated
with sediment type although ostracods and halacarids may be more numerous in coarser
sediments. In finer sediments, studies showed most copepods were species of Cylindropsillidae
and Parameschridae, (the smallest harpacticoids). In coarser sands, above 300 µm
median particle diameter, interstitial fauna included the nematode families, Ameiridae,
Ectinosomatidae and Diosaccidae.
The occurrence of rare species and very high diversity is unusual in mobile sandbanks.
However, three important species of interstitial polychaetes were recorded by Vanosmael et
al (1982) in mobile subtidal sandbanks in the North Sea: Polygordius
appendiculatus, (with a preference for coarse and medium sands), Protodriloides
chaetifer (fine medium and coarse sands) and a species of the genus Protodrilus.
The nematode densities in these sandbanks were generally higher than the surrounding
seabed. Whilst the generic composition of the nematode communities in mobile sandbanks is
similar to those of other clean sandy biotopes the large number of Epsilonematidae and
Draconematoidea (Nematoda) found in this study is exceptional for offshore communities.
These are adapted to the extreme instability of the substratum of the sandbanks and are
confined to these biotopes. The fauna of these unstable habitats consists largely of
erratic colonists brought in by water movement (Willems et al, 1982).
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References
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