Classification development - approach and methods used
Review of classification systems and literature
Before embarking on the development of the MNCR BioMar
classification (Connor et al. 1997a, b), a review of
existing classification systems was undertaken (Hiscock &
Connor 1991). From these, proposals for a classification structure
(Connor et al. 1995 a, b) were developed that drew upon
the best features of the existing systems, whilst avoiding their
weaker aspects. There was subsequent wide consultation on the
proposed classification structure, including through two European
workshops held during the EC-funded BioMar project (Hiscock
ed. 1995; Connor ed. 1997). These workshops
helped ensure broad acceptance of the proposed structure and its
wide applicability across European seas.
In addition to a review of classification schemes, an
extensive review of the literature describing marine habitats was
also undertaken. This helped formulate the initial lists of types
which might form the basis of the classification. For this the
scientific literature was of considerable help for sediment
habitats (a traditional area for marine studies) but relatively
poor for rocky habitats (which, in the subtidal, attracted
attention only relatively recently through use of SCUBA diving
techniques). These initial lists of types were then refined on the
basis of new dedicated field surveys, data analyses and field
trials.
Consultation and testing
Phases of external consultation and testing of the
classification system have been essential to ensure the
classification is as robust and usable as possible.
The advice of external consultees has been important in two
key areas:
- Marine scientists have contributed expertise in their
understanding of the marine environment and its communities, both
from a generic perspective and with specific knowledge of
communities at particular sites around the country. Of particular
importance has been advice on the relationships of environmental
factors to community structure and the spatial and temporal
dynamics of the marine environment.
- Environmental and conservation managers and end-users have
helped define their end needs for the classification system. This
has been reflected both in terms of the overall structure of the
classification, such as the orientation of biotope complexes to
mapping and sensitivity needs, the type of information given in the
description of each classification type, and the demands of field
application.
Field surveys and other data acquisition
The
Marine Nature Conservation
Review (MNCR) undertook a programme of field surveys
throughout Britain between 1987 and 1998, collecting data suitable
to develop the classification. In addition, data were acquired from
the published literature and through collaboration with a wide
variety of academic, government and other organisations. Comparable
data were collected in Ireland through the BioMar project between
1992 and 1996.
The data comprise information on the nature of each site (such
as substratum, wave exposure and height or depth surveyed), the
type of sampling undertaken, the site's location and the species
present (together with an indication of their abundance) within
discrete habitats at the site. MNCR field recording techniques are
described in Hiscock (1996), with Appendix 8 providing the guidance
on how to complete MNCR field recording forms (the forms can be
downloaded from
here).The terminology relating to field survey
methods is described further below, and should help users of the
classification interpret the habitat information contained in the
biotope descriptions. Procedural Guidelines for a wide range of
field sampling techniques are given in the
Marine
Monitoring Handbook (Davies
et al. 2001).
In total, data for over 16,000 sites comprising more than
36,000 habitat records from around Britain and Ireland were
collated and entered onto the MNCR database (as described by
Hiscock, 1996). The database includes a module which holds
definitions of each classification type, linked to a national
dictionary of marine species and to the field survey data. The
field survey data have been made widely accessible via the
web-based
MERMAID
application, and more recently, via the
National Biodiversity Network from an MS
Access-based 'relational' database, Marine Recorder. The Marine
Recorder database application has been specifically developed to
accept marine biological data from a wide range of survey
techniques, including the data held originally in the MNCR
database. The application can be downloaded
here, and includes
a dictionary of the habitat classification types.
Terms used for field recording and habitat definition
For semi-quantitative biological recording, the MNCR SACFOR
scale was used.
The following definitions for physical habitat
characteristics are taken from guidance notes for MNCR field
recording (Appendix 8 in Hiscock ed. 1996). Some terms are
modified for use in the classification.
Salinity - The
categories are defined as follows (the points of separation
approximate to critical tolerance limits for marine species):
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Fully marine
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30-40 ‰
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Variable
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18-40 ‰
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Reduced
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18-30 ‰
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Low
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<18 ‰
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Wave exposure - These
categories take account of the aspect of the coast
(related to direction of prevailing or strong winds), the
fetch (distance to nearest land), its
openness (the degree of open water offshore) and
its profile (the depth profile of water adjacent
to the coast). Estimation of wave exposure requires inspection of
charts and maps.
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Extremely exposed
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This category is for the few open coastlines which face into
prevailing wind and receive oceanic swell without any offshore
breaks (such as islands or shallows) for several thousand km and
where deep water is close to the shore (50 m depth contour
within about 300 m, e.g. Rockall).
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Very exposed
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These are open coasts which face into prevailing winds and
receive oceanic swell without any offshore breaks (such as islands
or shallows) for several hundred km but where deep water is not
close (>300 m) to the shore. They can be adjacent to
extremely exposed sites but face away from prevailing winds (here
swell and wave action will refract towards these shores) or where,
although facing away from prevailing winds, strong winds and swell
often occur (for instance, the east coast of Fair Isle).
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Exposed
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At these sites, prevailing wind is onshore although there is a
degree of shelter because of extensive shallow areas offshore,
offshore obstructions, a restricted (<90o) window to open water.
These sites will not generally be exposed to strong or regular
swell. This can also include open coasts facing away from
prevailing winds but where strong winds with a long fetch are
frequent.
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Moderately exposed
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These sites generally include open coasts facing away from
prevailing winds and without a long fetch but where strong winds
can be frequent.
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Sheltered
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At these sites, there is a restricted fetch and/or open water
window. Coasts can face prevailing winds but with a short fetch
(say <20 km) or extensive shallow areas offshore or may
face away from prevailing winds.
|
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Very sheltered
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These sites are unlikely to have a fetch greater than
20 km (the exception being through a narrow (<30o) open
water window, they face away from prevailing winds or have
obstructions, such as reefs, offshore.
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Extremely sheltered
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These sites are fully enclosed with fetch no greater than
about 3 km.
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Ultra sheltered
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Sites with fetch of a few tens or at most 100s of
metres.
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In the habitat classification
exposed (as in exposed littoral
rock) encompasses the extremely exposed,
very exposed and exposed
categories, whilst sheltered (as in
sheltered littoral rock) encompasses
sheltered to ultra sheltered
categories.
Tidal currents (or streams)
(maximum at surface) - This is maximum tidal current
strength which affects the actual area surveyed.
Note for shores and inshore areas this may differ
considerably from the tidal currents present offshore. In
some narrows and sounds the top of the shore may only be covered at
slack water, but the lower shore is subject to fast running
water.
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Very strong
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>6 knots
(>3 m/sec.)
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Strong
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3-6 knots
(>1.5-3 m/sec.)
|
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Moderately strong
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1-3 knots
(0.5-1.5 m/sec.)
|
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Weak
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<1 knot
(<0.5 m/sec.)
|
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Very weak
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Negligible
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In the habitat classification tide-swept
habitats typically have moderately strong or stronger tidal
currents.
Zone - These
definitions primarily relate to rocky habitats or those where algae
grow (e.g. stable shallow sublittoral sediments). For use of the
terms
infralittoral and circalittoral in the
classification, especially for sediments, refer also to
Table 5.
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Supralittoral
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Colonised by yellow and grey lichens, above the
Littorina populations but generally below flowering
plants.
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Upper littoral fringe
|
This is the splash zone above High Water of Spring Tides with
a dense band of the black lichen by Verrucaria maura.
Littorina saxatilis and Littorina neritoides
often present. May include saltmarsh species on shale/pebbles in
shelter.
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Lower littoral fringe
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The Pelvetia (in shelter) or Porphyra
(exposed) belt. With patchy Verrucaria maura, Verrucaria
mucosa and Lichina pygmaea present above the main
barnacle population. May also include saltmarsh species on
shale/pebbles in shelter.
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Upper eulittoral
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Barnacles and limpets present in quantity or with dense
Fucus spiralis in sheltered locations.
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Mid eulittoral
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Barnacle-limpet dominated, sometimes mussels or dominated by
Fucus vesiculosus and Ascophyllum nodosum in
sheltered locations. Mastocarpus stellatus and
Palmaria palmata patchy in lower part. Usually quite a
wide belt.
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Lower eulittoral
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Fucus serratus, Mastocarpus stellatus, Himanthalia
elongata or Palmaria palmata variously dominant;
barnacles sparse.
|
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Sublittoral fringe
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Dominated by Alaria esculenta (very exposed),
Laminaria digitata (exposed to sheltered) or Laminaria
saccharina (very sheltered) with encrusting coralline algae;
barnacles sparse.
|
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Upper infralittoral
|
Dense forest of kelp.
|
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Lower infralittoral
|
Sparse kelp park, dominated by foliose algae except where
grazed. May lack kelp.
|
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Upper circalittoral
|
Dominated by animals, lacking kelp but with sparse foliose
algae except where grazed.
|
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Lower circalittoral
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Dominated by animals with no foliose algae but encrusting
coralline algae.
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Substratum
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Bedrock
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Includes very soft rock-types such as chalk, peat and
clay.
|
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Boulders
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Very large (>1024 mm), large (512-1024 mm), small (256-512
mm)
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Cobbles
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64-256 mm
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Pebbles
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16-64 mm
|
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Gravel
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4-16 mm
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Coarse sand
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1-4 mm
|
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Medium sand
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0.25-1 mm
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Fine sand
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0.063 - 0.25 mm
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Mud
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<0.063 mm (the silt/clay fraction)
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Each division of sediment type above represents
two divisions on the Wentworth scale (Wentworth 1922).
In the habitat classification, bedrock, stable
boulders, cobbles or pebbles and habitats of mixed boulder, cobble,
pebble and sediment (mixed substrata) as well as
artificial substrata (concrete, wood, metal) are collectively
referred to as rock. Highly mobile cobbles and
pebbles (shingle), together with gravel and coarse sand are
collectively referred to as coarse sediments.
Mixed sediment consists of heterogeneous mixtures
of gravel, sand and mud and may often have shells and stones
also.
Data analysis
For the 1997 classification, data analyses
using the TWINSPAN and DECORANA clustering and ordination
techniques were employed to help define the types. The analytical
processes adopted are described in Mills (1994).
The 1997 version was revised and refined to develop the
present version. Extensive re-analyses of the data were carried out
using the analytical techniques available in PRIMER (Clarke
& Warwick, 2001). The data were initially divided into the five
broad habitat types shown in the
primary habitat matrix, i.e. Littoral Rock,
Littoral Sediment, Infralittoral Rock, Circalittoral Rock and
Sublittoral Sediment. Due to the large size of the datasets within
each broad habitat, some further
a priori divisions of the
data within broad habitats were necessary before analysis was
possible. Additional analyses were carried out on data from
"borderline" habitats to ensure these
a priori splits did
not force artificial divisions into the classification where this
was not supported by differences in the survey data. Analysis
within each broad habitat was led by a specialist for that habitat
type. Figure 2 shows the data analysis process for the littoral
sediment section. The following paragraphs describe the
analyses
carried out within each broad habitat:
Littoral rock
As the biotopes defined in version 97.06
(Connor
et al., 1997 a, b) were generally considered
satisfactory, analysis focused on clarifying the boundaries between
closely related types and confirming the validity of certain
less-well defined types. This included attention to the
inter-relationship of fucoid-dominated types regarding the
bedrock/boulder/mixed substrata and fully marine/variable salinity
transitions and examination of the various red algal-dominated
types. Additionally new data from intertidal caves enabled
substantial development of the classification here. On the basis of
these analyses, some restructuring at biotope complex level was
necessary.
Littoral sediment
Due to the size of the Littoral Sediment dataset
(>4000 records), some
a priori division was necessary
to provide datasets that could be managed within PRIMER (Clarke
& Warwick, 2001). Data were divided based on the sediment type
categories at habitat complex level in the 97.06 classification
(Connor
et al., 1997a, b): gravels and sands, muddy sands,
sandy muds, muds and mixed sediments. Semi-quantitative epifaunal
data were considered to be of less value than quantitative infaunal
data for the purposes of the analysis and were thus excluded.
Epifaunal data were however used to define types where a
significant proportion of species would be sampled in epibiota
sampling techniques, and/or where few infaunal samples were
available, e.g. for mussel beds.
Cluster analysis was carried out based on species matrices
listing individual counts per m
2 in each sample, using
the PRIMER software package (Clarke & Warwick, 2001). The data
were divided into small clusters of biologically similar records,
based on the resulting dendrograms. Comparative tables were
produced to compare the species data and physical data between each
of the small clusters. Where there were no notable differences
between the physical and biological characteristics of the small
clusters, they were amalgamated into larger groups which would form
the preliminary basis for biotopes and sub-biotopes. Where similar
biological and physical profiles appeared from clusters derived
from different datasets, those data were joined and re-analysed. In
particular, there was some overlap between the 'gravels and sands'
and the 'muddy sands', and between the 'muddy sands' and 'mud'
datasets. This re-analysis was carried out to ensure that the
a
priori divisions of the data did not artificially force
divisions of otherwise coherent clusters. The resulting preliminary
biotope and sub-biotope groups of records were then checked to
ensure cohesion of both the environmental and species data.
Individual records which differed significantly from the average
profile for the group (in terms of biology or physical habitat
characteristics) were removed, resulting in a group of records
which formed the basis of the biotope descriptions (core biotope
records). The physical and biological profiles from the core
biotope records were then used to group biotopes of similar
character into biotope complexes, and these in turn were assigned
to habitat complexes and broad habitats. Note that, in addition to
the habitat complexes defined on sediment character, two additional
categories were created based on epifaunal characteristics
(littoral sediments dominated by macrophytes, and littoral biogenic
reefs).
Infralittoral rock
As the biotopes defined in version 97.06 were generally
considered satisfactory, analysis focused on clarifying the
boundaries between closely related types and confirming the
validity of certain less-well defined types. This included
particular attention to the tide-swept kelp types and the
inter-relationship of highly grazed and poorly grazed kelp
habitats. On the basis of these analyses, some restructuring at
biotope complex level was necessary. Attention was also paid
to the vertical rock section of the infralittoral rock
classification, and examining how these additional biotopes could
be fitted into the existing biotope complexes, reflecting the
subtle differences in their biological character.
Circalittoral rock
Due to the complexities of this part of the classification,
especially the more subtle differences between types on the open
coast, a full re-analysis of the data were undertaken. The
large size of the circalittoral rock dataset meant that some a
priori division was necessary to provide datasets that could
be managed within PRIMER (Clarke & Warwick, 2001). Data were
divided on the basis of three previously determined energy levels;
high, moderate and low energy. Cluster analysis was carried
out using epifaunal species matrices exported from the AREV
database, using the PRIMER software package (Clarke & Warwick,
2001). The data were divided into small clusters of biologically
similar records, based on the resulting dendrograms. Comparative
tables were produced to compare the species data and physical data
between each of the small clusters. Where there were no notable
differences between the physical and biological characteristics of
the small clusters, they were amalgamated into larger groups which
would form the preliminary basis for biotopes and sub-biotopes.
Where similar biological and physical profiles appeared from
clusters derived from different datasets, those data were joined
and re-analysed. This re-analysis was carried out to ensure
that the a priori divisions of the data did not
artificially force divisions of otherwise coherent clusters. The
resulting preliminary biotope and sub-biotope groups of records
were then checked to ensure cohesion of both the environmental and
species data. Individual records which differed significantly from
the average profile for the group (in terms of biology or physical
habitat characteristics) were removed, resulting in a group of
records which formed the basis of the biotope descriptions (core
biotope records). The physical and biological profiles from the
core biotope records were then used to group biotopes of similar
character into biotope complexes, and these in turn were assigned
to habitat complexes and broad habitats. As in the
infralittoral rock section, further analysis was also carried out
on the vertical rock section of the circalittoral rock
classification.
Sublittoral sediment
A full re-analysis of the existing data on the MNCR database
in addition to data supplied by the sublittoral specialist was
carried out (approximately 10,000 records in total). This followed
a similar approach to that described for littoral sediment and as
outlined in Figure 2. Data were split according to sediment type,
data type (infaunal or epibiota) and sampling technique (where
appropriate). Poor quality data was also removed prior to analysis
for later manual assessment. Cluster analysis was undertaken using
either PRIMER (as described for the littoral sediments) or TWINSPAN
(following the guidelines in Mills, 1994). Clusters of biologically
similar records were produced and assessed using comparative
tables. Clusters with poor species definition or highly variable
physical characteristics were further sub-divided until more
homogenous groups were derived. Where similar biological and
physical profiles appeared from clusters derived from different
main habitat datasets those data were combined and re-analysed
using the same clustering methods as described above in order
ensure that the a priori divisions of the data did not
bias the results of the analysis.
Where similar biological and physical profiles were found in
clusters from datasets of differing sampling method or those with
different types of data (e.g. epibiota or infauna) the groups were
re-analysed where possible at a lower level of resolution (either
presence-absence or on the MNCR SACFOR scale) using PRIMER or
TWINSPAN such that the differences in data type were reduced. As
for the littoral sediments the resulting groups were then checked
for cohesion with regard the physical and biological data, and
individual records assigned to the groups were checked against the
profiles of the groups as a whole and re-assigned if
necessary.
The physical and biological profiles from the core records for
each type were then used to group types of similar character into
the broader biotope complexes and these in turn were assigned to
one of the six main habitats for sublittoral sediment, derived from
the EUNIS classification. The relationship between the sublittoral
sediment biotopes is shown for separate depth bands in a series of
habitat matrices, available to download as images from the
classification website.