Appendix - Monitoring of biological attributes
Macrofauna
Birds
Fish
Macrofauna
Intertidal mud and sandflats
i. Sediment cores
On intertidal areas core samples using a 0.01m² corer can be used to take quantitative
samples of the sediment. Generally five replicates are recommended for statistical
analysis. Samples should be taken up to 5m either side of the site location but not up or
down the shore. Each sample should be placed in a sealable plastic bag which is clearly
labelled with a waterproof marker. The samples should be washed through a 0.5mm mesh
within 24 hours and fixed in a 10% buffered saline formalin solution for storage after
which the samples can be sorted aided by an illuminated magnifier or low power binocular
microscope and the animals identified with high power compound microscopes and up to date
taxonomic literature. In coarser sediments an additional five 0.01m² cores or three
0.1m² box cores should be taken depending on the level of silt present. If data is to be
collected on the abundance of specific species then prior knowledge on the density and
aggregation of the species is necessary to determine the number of samples required.
Additional information on the condition of the sediment, anoxic layer and surficial
features should be noted. A 1m²quadrat should also be used at the site to record numbers
of worm casts and algal cover and the area dug over to within 20-30 cm depth to record
larger species. 1m² quadrats can also be used as part of an ACE survey to determine
abundance scales of conspicuous species and epifauna noted over a 10m² area followed by
site photographs. Species which cannot be identified in the field can be taken for
subsequent identification. Information should be noted on an MNCR recording form. Site
positions can be recorded using shore transit mark or DGPS as appropriate.
ii. Remote sampling
This technique generally involves all equipment lowered from a boat to take a
quantitative sample of the sediment. Samples are taken by grabs e.g. the Van Veen or Day
grab. Other equipment includes the Reineck box corer, Knudsen corer (particularly in
softer sediments), Hamon or Shipek grabs (in coarser sediments) and Forster anchor dredge
(for semi quantitative sampling of mobile megafauna). Site conditions, size of vessel and
previous experience will dictate which equipment is most suitable. Details on these and
other models are given in Holme (1971). Samples are generally 0.1m² and sieved through
0.5 or 1mm mesh depending on substratum and between five and ten replicates should be
taken. Notes on the sediment sample should be taken backed up by photographs if possible.
For Day and Van veen grabs samples should be at least 7 cm deep in finer sediments and 5cm
in sands. After sieving samples should be fixed in a 10% saline formalin solution. Site
positions should be recorded by DGPS.
Subtidal mobile sandbanks
i. Towed and remote operated video
The cameras are generally mounted at 45 degrees with video lights and flash strobes
pointed vertically downwards. With ROV systems the cameras are mounted on a submersible
vehicle which is controlled by a surface operator via an umbilical cable. Towed systems
require a vessel which can maintain steerage at low speeds of around 1 to 1.5 knots and
the water depth needs to be monitored and the length of cable checked accordingly.
Both systems usually operate along predefined transects along which the seabed
characteristics are recorded and the benthic animals counted, still photographs may be
taken of interesting features. With towed systems the ships DGPS can give the precise
location of the equipment but this is more problematical with remote systems though in
some areas it is possible to lay a marked transect line onto the seabed with marker buoys
at the surface. ROV systems are hampered by having to remain within a certain radius of
the ship but have the advantage that they may hover over a particular area or retrace its
path and avoid obstructions, some models can also take benthic samples.
The recording of animals with towed systems usually involve time series counts by which
the length of video recording is broken into segments of equal times and either the
presence of animals in each segment noted (rapid visual count) or the total number of
animals counted (visual fast count). ROV systems may also operate in this fashion or if
reliable knowledge on the size of the video frame and a straight transect is possible
(allowing the total distance travelled to be calculated) then the number of target species
in a known area can be calculated. Problems in the quantification of animals with ROVs may
arise because the ROV may not always be a fixed distance from the substratum so the field
of view may change.
ii. Acoustic survey
The underlying principle behind these methods is based on the fact that acoustic energy
is reflected off the sea floor and the amount of reflection depends on the density of the
bed material and the angle of incidence at which the acoustic waves meet the sea floor. It
should be remembered that these systems measure the acoustic properties of the sea bed not
other properties such as grain size although these are related. The most widely used
system available is the RoxAnn® system. This utilises commercial echosounders
set at frequencies of 200 KHz in waters shallower than 60m or in deeper waters frequencies
of 50-120 KHz. The first and second echoes (E1 and E2) are used with E1 used as a measure
of roughness i.e. topographic irregularities and E2 as a measure of hardness which is
related to substratum type.
Transects across the study area are made at moderate speeds with the data logged as an
average over a set time e.g. 5-10 seconds. The two parameters are plotted against each
other to derive sediment type and this information together with depth and positional
information from DGPS allow a 3 dimensional representation of the seabed to built up and
the main substratum types determined. The differences in acoustic properties of the sea
floor are related to factors such as grain size which is itself an important factor in
determining benthic communities and as such these methods can give an idea of biotope. The
benthos itself affects the substratum e.g. through bioturbation, tube building etc so the
system can also detect biological features such as Modiolus beds, seagrass, Nephrops
burrows, Sabellaria reefs etc. The information gathered from these systems needs to
be ground-truthed either by grab sample or towed or remote operated video and post
processing of the data may be required to recalibrate the system to get the most accurate
representation. Successful studies of candidate SACs have been made using RoxAnnTM e.g.
Strangford Lough (Magorrian et al, 1995).
The advantages of systems such as RoxAnnTM is that they can map extremely
large areas of substratum fairly quickly with no depth constraints in coastal areas. Other
factors such as turbidity are unimportant. With accurate ground-truthing a much more
representative idea of the main substratum types in a SAC can be gained than from spot
grab samples and the information can be used stratify other direct sampling regimes for an
area and reduce the cost and time spent undertaking these surveys. At large areas acoustic
methods are probably the only way to effectively map the main biotope complexes. However
the system is an indirect representation of the substratum and detailed ground-truthing is
required as no direct information is produced on the sediment type or of the detailed
composition of the community. The equipment is also expensive an needs a skilled operator
to derive accurate results. Care should be taken not to interpret the data at too higher a
level of precision as the results may be misleading and the differences between the
echosounders and frequencies used may mean that results from different surveys may not be
entirely comparable.
Birds
WeBS counts are probably the most effective method. Current WeBS counts are carried out
by volunteers and cover the majority of UK wetland sites including estuaries and some open
coastal areas. A very large dataset over the last 30 years has been built up for many
areas so there is a large amount of existing data available. These counts can be made on a
monthly or yearly basis (in the winter) depending on the size of the area, although in
extremely large areas e.g. the Wash it may not be possible for financial reasons to sample
this regularly.
Bird counts on the intertidal areas are made around high water (usually ± 2 hours
depending on location) with the area divided into sectors and counted separately. These
counts give a good indication of usage in general and counting is easy as the birds are
pushed to the top of the shore. High water counts are also inexpensive. However depending
on the topography of the site and tidal conditions birds can be pushed off sites into
different areas at high water and give misleading usage. Low water counts may be used in
smaller areas and these give a good indication of preferred feeding areas on the flats not
just general usage and identifies which species are using the site as predators rather
than roosting. However there is a shorter historical dataset and the method is difficult
over large areas. Goss Custard (1985) showed that there was often a good correlation
between high and low water counts although this is not true in all areas. In large areas
remote sensing techniques although costly can provide useful information on habitat usage
and may give initial information on the changes in feeding distribution reflecting changes
in sediment type.
Fish
A quantitative survey of the juvenile fish populations using the intertidal areas can
be carried out with push nets. Small beam trawls should also be made of the subtidal sand
banks whilst minimising any damage to the epibenthic population. The beam trawl will
usually be around 2m diameter with tickler chains across the front of the net to disturb
fish buried in the substratum. Transects of around 20 minute duration can be made with
positions fixed by DGPS. Demersal fish are rarely evenly distributed throughout an area so
a random sampling method is usually applicable. With beam trawls it is fairly easy to
calculate the absolute abundance per area using the width of the trawl and the distance
trawled to determine the area trawled, a catchability component may also be included.
Seasonal components should be taken into account in the sampling strategy and analysis
of production and age classes (cohort analysis) carried out. Analysis of the stomach
content of the fish population may also prove useful and may dispense with the need to
sample the infauna.
References
|