habitat diversity relative to wave action on rocky shores: implications for the selection of marine...
TRANSCRIPT
AQUATIC CONSERVATION: MARINE AND FRESHWATER ECOSYSTEMS
Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
Published online 29 December 2009 in Wiley InterScience(www.interscience.wiley.com). DOI: 10.1002/aqc.1014
Habitat diversity relative to wave action on rocky shores:implications for the selection of marine protected areas
LAURA K. BLAMEY and GEORGE M. BRANCH�
Marine Biology Research Centre, Department of Zoology, Private Bag X3, University of Cape Town,
Rondebosch 7701, South Africa
ABSTRACT
1. Current selection of marine protected areas in South Africa is based on objective criteria including biogeographicrepresentation and habitat heterogeneity. This paper specifically examines rocky shores on the west coast of SouthAfrica to determine whether they are divisible into discrete ‘habitats’ that need independent conservation.2. Seventeen rocky shores spanning the full spectrum of wave exposure were compared in terms of maximum
wave forces, biomass, species richness and diversity among zones and sites. Three biotic assemblages wereidentified, characterizing sheltered, semi-exposed to exposed, and very exposed habitats. Differences among thesewere clear-cut low on the shore but disappeared at the top of the shore where wave action was attenuated anddesiccation uniformly intense.3. The recognition of three discrete biologically-defined habitats means that rocky shores cannot be regarded as
a uniform habitat for conservation purposes. All three components need protection if the full spectrum of rocky-shore communities is to be conserved.4. It is argued that this approach allows habitats to be defined in an objective manner, and that once this has
been done, habitat heterogeneity constitutes a better measure of conservation value of an area than a ‘hotspot’approach based on species richness and endemism.Copyright r 2008 John Wiley & Sons, Ltd.
Received 16 May 2008; Revised 26 August 2008; Accepted 10 September 2008
KEY WORDS: intertidal biomass; limpets; mussels; marine protected areas; rocky shores; wave action
INTRODUCTION
Selection of sites for conservation has become increasingly
sophisticated with development of algorithms to compare the
rival merits of different sites (Margules and Pressey, 2000;
Leslie et al., 2003). However, the underlying philosophy
remains contentious, with two approaches— ‘hotspots’
versus ‘habitats’—being debated. The ultimate aim of both
is protection of biodiversity, but in different ways. Species are
the biological unit for hotspot designation, with preference
given to conservation of areas high in species richness and
endemism (Myers et al., 2000). By contrast, the ‘habitat’
approach seeks to protect all habitats within all biogeographic
regions, and favour areas that include a high diversity of
habitats (Hockey and Branch, 1997; Roberts et al., 2003a,b).
For most of the 20th century, terrestrial ecosystems have
received the greatest attention in terms of conservation
(Roberts et al., 2003a), so it is no surprise that the design of
reserves has been developed primarily for terrestrial
ecosystems. However, fundamental differences exist between
marine and terrestrial ecosystems, such as geographic
boundaries, dimensions of species distribution and transport
of energy, materials and organisms, implying some unique
criteria in the selection of marine reserves (Hockey and
Branch, 1994; Carr et al., 2003; although Avery et al., 2003
offers a counter view).
Early attempts at developing criteria for Marine Protected
Areas (MPAs) were focused largely on biological measures
such as rarity and diversity (Hockey and Branch, 1994).
Lately, there has been a shift towards incorporating political,
social and economic criteria owing to increasing recognition
that MPAs should fulfil multiple objectives (Kelleher and
Kenchington, 1990; Hockey and Branch, 1997; Friedlander
et al., 2003). Several schemes have been proposed to help select
*Correspondence to: George M. Branch, Marine Biology Research Centre, Department of Zoology, Private Bag X3, University of Cape Town,Rondebosch 770, South Africa. E-mail: [email protected]
Copyright r 2008 John Wiley & Sons, Ltd.
sites for MPAs. Hockey and Branch (1997) developed a
methodology called COMPARE (Criteria and Objectives for
Marine Protected ARea Evaluation) that rates rival sites in
terms of their relative value for conservation. This is based on
a set of 14 objectives for MPAs, covering biodiversity
protection, fisheries management and human utilization, and
a set of 17 criteria that rate the degree to which given areas
meet these objectives. Roberts et al. (2003a,b) subsequently
developed more detailed ecological criteria to evaluate
candidate sites.
Hockey and Branch (1994, 1997) advocate that as a first
step biogeographic regions need to be defined and
conservation implemented in all such regions. They further
argue that nested within each biogeographic region, habitat
heterogeneity should be used to measure the relative prestige of
different areas rather than species richness, because different
habitats are fundamentally different in species richness, and
should not be accorded greater (or lesser) value simply because
they have a high (or low) species richness (Roberts et al.,
2003a). Rather, protected areas should include as many
habitats as possible since the diversity of biological
communities present is related to the range of habitats
present (Hockey and Branch, 1997). Using habitat
heterogeneity as a proxy for biodiversity has been
successfully applied to the initial selection of MPAs (Ward
et al., 1999), and has advantages over the species-based
hotspot approach, as discussed below, but it does require that
habitats be defined. Various terms have been used to describe
these units, including ‘land classes’ (Lombard et al., 2003) or
‘land systems’ (Oliver et al., 2004) and ‘broad habitat units’
(Cowling and Heijnis, 2001). Beger et al. (2003) use the word
‘eco-habitats’ and define them as areas with ‘a distinct
community structure owing to different environmental
factors’. Here, the word ‘habitats’ is used in the same sense,
and it is argued that they must initially be distinguished by the
biota present, although they may ultimately be recognized by
surrogates including physical conditions (e.g. substrate type
and wave action) and biological features such as the dominant
characteristic morphotypes (e.g. mangroves). At a coarse level,
nearshore marine habitats can be defined simply by
distinguishing obvious systems such as mangroves, salt
marshes, sandy beaches, coral reefs or rocky shores.
However, each of these may be divisible into discrete types,
often with radically different biotic communities. Banks and
Skilleter (2007) showed that when applying these coarse level
surrogate measures for biodiversity, they failed to represent
fine-scale habitat and microhabitat diversity and were
therefore less likely to achieve conservation goals. Securing
conservation of each of these smaller-scale units is thus
necessary to protect all community types and maintain all
ecosystem functions. This necessitates defining the units in an
objective and defensible manner.
This paper makes a specific contribution to the habitat
approach by inquiring about the extent to which rocky shores
in the cool-temperate Namaqua Province of southern Africa
are divisible into ‘habitats’ (operationally recognized by their
discrete assemblages of species) that can be objectively
distinguished by quantitative means.
Rocky shores display distinct zonation patterns vertically
and horizontally along shores. Locally, the two most
important physical forces responsible for these gradients are
probably desiccation and wave action, respectively (Dayton,
1971; Sousa, 1979; Menge and Sutherland, 1987; Bustamante
et al., 1997).
Clearly there is need to quantify intertidal community
structure of rocky shores relative to wave action to objectively
determine whether rocky shores are just a single variable
habitat, or comprise different habitats with distinctive
biological communities, each needing conservation. A
substantial amount of research has been done on the effects
of wave exposure on various intertidal organisms/communities
(Ballantine, 1961; Lewis, 1964; Denny, 1985, 1987; Denny
et al., 1985; McGuinness, 1987a,b; Brown and Quinn, 1988;
Carrington, 1990; Bertness et al., 1991; Gaylord et al., 1994;
Bustamante and Branch, 1996a; Blanchette, 1997; Andrew and
Viejo, 1998; Jenkins and Hartnoll, 2001; Harley and Helmuth,
2003; Davenport and Davenport, 2005), but most of these
studies have either focused on the biomechanical implications
of wave action for particular taxa, or have descriptively
distinguished community composition at different grades of
wave action. In South Africa previous studies on rocky-shore
community structure relative to wave action have tended to
contrast subjectively defined ‘exposed’ and ‘sheltered’ sites,
often without quantification of wave action (McQuaid and
Branch, 1984; Bustamante and Branch, 1996a; Bustamante
et al., 1997; but see Steffani and Branch, 2003b,c). The current
study is an advance because it covered the full spectrum of
wave exposure, quantitatively measured both wave action and
biotic composition, and sought objective measures of
community distinctiveness.
Two hypotheses were advanced as a framework. First,
differences in community composition were expected to be
clear-cut in the low shore but non-existent in the high-shore as
the effects of wave action are attenuated upshore and
superseded by the uniformly severe desiccation. Second,
considering entire shores, it was expected that the intensity
of wave action would determine community structure and thus
separate shores with different levels of wave exposure.
METHODS
Study site
The study was located roughly 600 km north of Cape Town on
the west coast of South Africa in a relatively pristine stretch of
coastline around Groenrivier. Its pristine condition, high
diversity of habitats and representation of the Namaqua
biogeographic province (Emanuel et al., 1992) were prime
motivations for a ministerial declaration of intention in
February 2004 to promulgate the area as an MPA.
Samples were taken during the autumn/winter at 17 sites
spanning the full spectrum of wave exposure (Figure 1).
Maximum wave force was measured at 14 of these sites using a
maximum wave-force dynamometer (Steffani and Branch,
2003b), and estimates interpolated for the three additional
sites. Wave forces were divided a priori into four categories:
sheltered, semi-exposed, exposed, and very exposed,
respectively experiencing maximum wave forces of 0–5, 5–10,
10–15 and 415 (� 103) Nm�2, following Steffani and Branch
(2003a).
L.K. BLAMEY AND G.M. BRANCH646
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
Sampling methods
At each site, five replicate transects from the low shore to
the high shore were randomly chosen. Within each transect,
four 0.25m2 quadrats (divided into 100 squares each
representing 1% cover) were sampled in the low, mid, high
and top zones.
Percentage cover of sessile fauna and flora and numbers of
mobile organisms were scored (Bustamante and Branch,
1996a). Subsamples of species were taken to convert
abundance to biomass (g wet weight m�2).
Statistical analyses
The biomass data were analysed with PRIMER (Plymouth
Routines In Multivariate Ecological Research version 5.2.2).
The data set was too large to simultaneously analyse all
replicates (n5 340 samples) so two complimentary analyses
were undertaken. First, the biomass values for each species
were averaged for the five replicates per zone, thus reducing
the replicates per site from 20 to 4, yielding 68 samples. This
produced a ‘site-by-zone’ comparison of all zones among sites
(Figure 2). Second, the data for each species were averaged for
Figure 1. Map showing location and detail of sites sampled at Groenrivier (1) and Cape Columbine and Jacobsbaai (2). Site codes, coordinates andmaximum wave force measurements per site are listed. Estimates of wave force were made for sites at Cape Columbine and Jacobsbaai.
HABITAT DIVERSITY RELATIVE TO WAVE ACTION ON ROCKY SHORES 647
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
the four zones in each replicate transect to give single values
for each transect (distilling the data to five replicate transects
per site; Figure 2). These data allowed a ‘site-by-transect’
analysis comparing all replicate transects among sites. Both
data sets were analysed by Bray–Curtis hierarchical clustering
and multidimensional scaling (MDS) to compare community
structure among sites and zones. SIMPER (similarity
percentage) analysis (with a cut off of 85%) was performed
on the ‘site-by-transect’ data to determine which species were
responsible for similarities or dissimilarities among and within
sites.
The zones and sites were also compared in terms of species
richness, species diversity and biomass. Species richness was
calculated by counting the number of different species present
per zone (pooling the five replicates). Species diversity was
measured using the Shannon–Wiener function (H05�Sipi(log2 pi)), based on biomass values. Species richness, diversity,
overall biomass, and filter-feeder, grazer and algal biomass
were regressed against wave force at each site, using
polynomial regressions.
Validation
Once discrete habitats based on the biota had been defined the
classification was independently validated. First, using aerial
orthophotographs showing coastal contours (scale 1:10 000)
and considering prevailing wave swell direction, five rocky-
shore sites lying in the same biogeographic province but
250 km to the south of Groenrivier were selected: sites D, I, S
and V representing sheltered, semi-exposed, exposed, and very
exposed situations at Cape Columbine, and Site E representing
a sheltered site at Jacobsbaai (Figure 1). These sites were
assigned to the habitat types as defined, based on the wave
exposure that was anticipated on the basis of coastline
topography and wave direction. Second, the biota at each of
these sites was sampled as above (during autumn/winter) and
then these data were inserted with those obtained from
Groenrivier and the analysis rerun with Primer to test
whether the additional sites were indeed classed in the
habitat types it was assumed they would represent. This
provided two tests of the approach: (1) whether other localities
outside the initial study area conformed to the proposed
classification of habitats, and (2) whether a simple physical
surrogate (estimated wave action) could serve as a proxy for
the biologically-defined habitats.
RESULTS
Zonation
Comparing among zones, both cluster analysis (Figure 3(a))
and MDS (Figure 3(b)) distinguished six groups. Group 1
united the top zones for all sites, spanning all grades of wave
exposures (C–V). Group 2 was made up of the upper-most
zones (i.e. the high and top zones) for mainly sheltered sites
(Q3 being an exception as it was at an exposed site). Group 3
comprised a mixture of mid and high zones from exposed or
very exposed sites. Group 4 contained the low and mid zones
from very exposed sites T–V. Group 5 also incorporated the
low and mid zones, but from semi-exposed to exposed sites
(mostly G–S). Group 6 consisted of low zone and mid zone
samples from the six sheltered sites A–F.
Wave exposure
Pooling across zones to compare the five replicate transects at
each site, both the hierarchical cluster analysis (Figure 4(a))
and the MDS plot (Figure 4(b)) revealed five clusters. Group 1
comprised the very exposed sites T–V. Two exposed sites, K
and Q made up group 2, and the exposed sites L, M, N, O, P
and R constituted group 3. Group 4 included three semi-
exposed sites, G, H and I, to which a fourth site, J, was
added because (a) it was allied with the other semi-exposed
sites in the MDS if not in the cluster analysis, and (b)
measurements of wave action there classed it as semi-exposed.
Group 5 comprised sites A–F, which were all sheltered.
Typically, the replicate transects at each site clustered closely
and were more similar to each other than to transects at other
sites. Sheltered and very exposed sites formed completely
Top
High
Mid
Low
Sea
1 2 3 4 5
Mean zone(n = 4 zones)
Mean transect(n = 5 transects)
Rocky shorezones
TransectsMHWS
MLWS
Figure 2. Sampling protocol and pooling of data: at each site four zones were sampled in five replicate transects. For analyses, the quadrat data ateach site were pooled horizontally to create mean low, mid, high and top zones, and vertically to create five replicate transects.
L.K. BLAMEY AND G.M. BRANCH648
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
discrete clusters, but those classed as semi-exposed and
exposed tended to merge.
Validation of patterns
Five sites from outside the study area (D, E, I, S and V) were
first rated according to their estimated wave action and then
sampled to examine their community composition. All five
yielded community compositions that classed them with other
sites of comparable wave action (Figure 4).
Characteristic species
Species characterizing the four grades of wave action
recognized a priori were identified by SIMPER (Figure 5).
Sheltered shores were typified by the limpets Cymbula
granatina and Scutellastra granularis, which contributed
52.4% and 12.1%, respectively, to this similarity. Semi-
exposed shores were characterized by the mussel Mytilus
galloprovincialis and the limpet Scutellastra argenvillei. On
exposed shores M. galloprovincialis and S. argenvillei were
100
80
60
40
20
112
3
45
6
J3
C3
Q4
O4
P4
C4
S4
M4
V4
U4
T4
K4
I4
G4
J4
H4
L4
R4
A4A4
E4
F4
B4
D4
F3
E3
A3
Q3
Q2
R2
T2
T3
P1
O1
S2
M2
P2
N2
P3
N3
N4
K3
O2
S3
M3
I3
H3
L2
L3
R3
V3
U3
J2
O3
B3
G3
T1
V2
U2
V1
U1
K2
G2
K1
I1
H2
G1
S1
M1
R1
L1
Q1
J1
N1
I1
H1
E2
A2
C1
F1
D1
A1
B1
E1
F2
C2
D3
D2
B2
High-topSheltered
Top zonesAll grades of wave action
Mid-highExposed & very exposed
Low-midVery exposed
Low-midSemi-exposed & exposed
Low-midSheltered
0
Bra
y-C
urt
is S
imila
rity
E1E2
E3
E4
D1D2
D3
D4
I1
I2
I3
I4
S1
S2
S3
S4
V1V2V3
V4
H1
H2
H3
H4
G1
G2
G3
G4
A1
A2
A3
A4 L1
L2L3
L4
B1B2
B3
B4
M1
M2
M3
M4
U1
U2
U3
U4
T1
T2
T3
T4
C1
C2
C3
C4
J1
J2
J3
J4
O1
O2
O3
O4
Q1
Q2
Q3
Q4
R1
R2
R3R4 P1P2
P3P4
N1
N2N3N4
F1F2
F3F4
K1
K2
K3
K4
Stress:0.121. Top zones
All grades of wave action
2. High-top Sheltered
3. Mid-high Exposed & Very exp
6. Low-mid Sheltered
4. Low-mid Very exp
5. Low-mid Semi-exp & Exposed
(a)
(b)
Figure 3. (a) Dendrogram showing hierarchical cluster analysis and (b) MDS plot based on standardized root transformed biomass data from four zones(1–4, where 15 low zone, 25mid zone, 35high zone and 45 top zone) at 22 sites (A–V). The data for each zone were an average of five replicates.
HABITAT DIVERSITY RELATIVE TO WAVE ACTION ON ROCKY SHORES 649
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
again the major contributors but in different proportions. Very
exposed shores were characterized by M. galloprovincialis and
Plocamium cornutum.
Dissimilarities among shores with different grades of wave
action were defined by distinguishing species (Figure 5).
Sheltered shores were 75.3% dissimilar to semi-exposed
shores. The components most responsible were Cymbula
granatina, the algae Porphyra capensis and Ulva species, and
the whelk Burnupena lagenaria (all with biomasses that were
greatest on sheltered shores and declined progressively with
wave action); and Mytilus galloprovincialis, Scutellastra
argenvillei and the alga Champia lumbricalis (absent or scarce
on sheltered shores). Semi-exposed and exposed shores were
45.17% dissimilar due to S. argenvillei, C. lumbricalis,
C. granatina and S. granularis being more abundant on semi-
exposed shores and M. galloprovincialis, Scutellastra cochlear
and G. capensis reaching higher values on exposed shores
(Figure 5). Finally, the average dissimilarity between the
exposed and very exposed shores was 46.38%, largely due to
Plocamium cornutum, Corallina species and S. cochlear (greater
biomasses on very exposed shores) and S. argenvillei,
M. galloprovincialis and G. capensis (lower values there).
Diversity and biomass
Species richness peaked at semi-exposed to exposed shores
(Figure 6(a)). There was, however, no significant trend in
species diversity (Figure 6(b)). Total biomass also peaked at
intermediate intensities of wave action (Figure 6(c)). Not
surprisingly, filter feeders (which constituted the bulk of the
biomass) followed the same trend (Figure 6(d)). One site (N)
had an exceptionally high biomass of filter feeders (35 kgm�2),
inflating overall biomass as well; but even if this site was
excluded from the analysis, the polynomial relationship
100
80
60
40
20
1
23 4 5
6
T U UV V K Q N P L LO RM MS I IH H J G F C E A B D
ShelteredSemi-exposedExposedExposedVery exposed
E
EE
E
E
DDD
D
D
I
I
II I
SSS S
S
VV V
V V
HHHH
H
G
G
G
GGA A
AA
A
L L
L
L
L
BBBB
B
M MM M
M
U
U
U
UU
T
T
TTT
CCC
CC
J
JJ
JJ
O
O
O
OO
Q
Q
Q
Q
Q
R
R
RR
R
PP
P
P
P
N
NNN
N
FFF
FF
K
KK
KK
Stress: 0.1
6. Sheltered
4.Semi exposed
2.Exposed
1. VeryExposed
3. Exposed
(a)
(b)
5.Semi exposed
Bra
y-C
urt
is S
imila
rity
Figure 4. (a) Dendrogram showing hierarchical cluster analysis and (b) MDS plot based on standardized root transformed biomass data from 22sites (A–V) with five replicate transects per site.
L.K. BLAMEY AND G.M. BRANCH650
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
remained significant and biomass still peaked at intermediate
wave forces. Grazer biomass was high at sheltered and semi-
exposed sites, predominantly due to Cymbula granatina and
Scutellastra argenvillei respectively, but declined at high
intensities (Figure 6(e)). There was no significant relationship
between algal biomass and wave force, despite a tendency to
increase at higher exposures (Figure 6(f)). Predator/scavenger
biomass was too low to consider statistically.
DISCUSSION
What is a habitat?
To employ habitats as a surrogate for biodiversity surveys
requires that they first be defined. As Stevens and Connolly
(2004, p. 351) state: ‘Little confidence can be placed in marine
habitat classifications based solely or largely on abiotic
surrogates without calibration by rigorous biological
surveys’. This survey addressed this question with a specific
focus on rocky shores on the west coast of South Africa, but
the approach is applicable to other regions and other
ecosystems.
The term ‘habitats’ is used to distinguish spatial units that
have biological assemblages that can be distinguished by
objective quantitative means. In doing so, it is recognized that
such units are a response to an interplay between physical
conditions and biotic interactions, and that their ultimate
definition must incorporate the physical factors that set the
scene.
To be useful, habitats must be objectively definable, and
easily distinguishable.
Defining rocky-shore habitats
Zonation
The differences recorded between zones supported our first
hypothesis that greater diversity and heterogeneity exist in the
low shore: divergence between sites was greatest in the
lowshore and diminished upshore. This accords with the idea
that desiccation-related factors constitute a uniform stress at
the top of the shore, whereas wave action is not uniform in the
low shore (Bustamante et al., 1997). This is, however, largely
of academic interest when choosing MPAs, because entire
rocky shores will be selected for protection, not individual
zones within sites, although it is true that in principle MPAs
are often zoned for different activities. Thus comparisons of
the differences among sites were the issue of central interest
when deciding how many discrete habitats should be
recognized on rocky shores.
Wave action
Corresponding to the wave-force measurements, biotic clusters
were evident in the analysis of community composition
(Figure 4), supporting the second hypothesis that intensity of
wave action influences community structure, as noted by many
authors (Ballantine, 1961; Lewis, 1964; Dayton, 1971;
McQuaid and Branch, 1984; Denny et al., 1985; Emanuel et
al., 1992; Bustamante et al., 1995a,b, 1997; Bustamante and
Branch, 1996a; Steffani and Branch, 2003a,b; Branch and
Steffani, 2004). The gradient evident in Figure 4 (extending
from the bottom left corner up to the top right corner) displays
groupings from the most sheltered sites (group 5) moving
through a cluster of semi-exposed and exposed sites (groups 2,
3 and 4) and finally, a cluster of the very exposed sites
(group 1). Groups formed between sites that experienced
similar levels of wave exposure.
Biological characterization
Three readily distinguishable clusters emerged: sheltered, semi-
exposed plus exposed, and very exposed, corresponding to
wave forces of o5, 5–15 and 415 (� 103) Nm�2. Greater
distinction between semi-exposed and exposed shores might
have been expected, but they merged. Previous work in the
Plocamium cornutum Scutellastra cochlearCorallina spp.Mytilus galloprovincialisLaminaria pallidaGunnarea capensisScutellastra argenvilleiScutellastra granularisChampia lumbricalisPorphyra capensisUlva sp.
Cymbula granatina
Sheltered(S=56.2%)
Biomass (log g/m2)
***
Semi-exposed(S=61.6%)
Exposed(S=64.2%)
Very exposed(S=72.5%)
***
*
-1 0 1 2 3 4 -1 0 1 2 3 4 -1 0 1 2 3-1 0 1 2 3 4
**
*
**
***
***
*
*
*
*
D=75.3% D=45.2% D=46.3%
Burnupena lagenaria
00
0
0
000
0
Characteristic species
Distinguishing species
Figure 5. Average wet biomass (log gm�2) of species responsible for the similarities (S) within grades of wave action and the dissimilarities (D)between sheltered and semi-exposed shores, semi-exposed and exposed shores, and exposed and very exposed shores. Significance differences areshown for �0.05, ��0.01 and ���0.001 levels. White dots identify species distinguishing between grades of wave action; black dots identify species
characteristic of each level; 05 absence.
HABITAT DIVERSITY RELATIVE TO WAVE ACTION ON ROCKY SHORES 651
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
region has shown that the alien mussel Mytilus
galloprovincialis dominates exposed shores whereas the
limpet Scutellastra argenvillei achieves exceptionally high
densities on semi-exposed shores and retards the
development of mussel beds (Steffani and Branch, 2003a,b,c;
Branch and Steffani, 2004). This was reflected in the results, as
M. galloprovincialis attained highest biomasses on exposed
shores whereas S. argenvillei was more abundant on semi-
exposed shores (Figure 5). Despite these and comparable
significant differences for other species, the aggregate effect
was too blurred to consider semi-exposed and exposed shores
as separate habitats. The dissimilarity between semi-exposed
and exposed shores was smaller than for any other
comparisons among grades of wave action. Moreover, little
value was placed on M. galloprovincialis as an indicator
because it is an alien species. Thus, it was considered that only
three distinct types of habitat exist on the rocky shores
examined, all of which require conservation.
Indicator species
The similarities within the four grades of wave action
distinguished a priori, and the dissimilarities between them,
were due to a few select species. Sheltered shores were
dominated by the limpet Cymbula granatina, which is known
to be intolerant of wave-exposed conditions because of its low
tenacity (Branch and Marsh, 1978), as is its sister species
C. oculus (Branch and Odendaal, 2003). C. granatina was the
2y= -0.023x + 0.317x + 1.7712r = 0.201; p<0.05
35
45
55
65
75
85
25A C FB E
D
G
H
I
J
K
L
M
N [35]
O P
Q
S
R
T
U
V
0
0.5
1.5
2
1
2.5
3
3.5
A
C
F
B
E
D
TU
V
G
H
IJ
K
L
M
N
O
P
R
Q
S
0
5
10
15
20
25
AB
C
D EF
G
H
I
J
K
L
M
N [40]
OP
Q
S
R
TU
V
0
2
4
6
8
10
12
14
2 4 6 8 10 12 14 16 18 2000
0.5
1.5
2
1
2.5
3
A
C
F
B
E
D
T
U
V
G
H
I
JK
L
M
N
O
P
R
Q
S
00.5
1.52
1
2.53
3.54
4.55
A
C
F
B
E
D
TU
V
GH
I
J
K [9]
L
M
N
O
PR
QS
(a)
0-5 5-10 10-15 >15
(d)
(b) (e)
(c) (f)
Sp
ecie
s R
ich
nes
s(n
um
ber
of
spec
ies)
Sh
ann
on
-Wie
ner
Sp
ecie
sD
iver
sity
(H
’)
Alg
al B
iom
ass
(Kg
.m-2
)G
raze
r B
iom
ass
(Kg
.m-2
)F
ilter
Fee
der
Bio
mas
s (K
g.m
-2)
Ove
rall
Bio
mas
s (K
g.m
-2)
AC
F
BE
D
T
U
V
G
H
I
J
K
L
M
N
O
P
R
Q
S
Maximum Wave Force (x10 3N.m-2)
2 4 6 8 10 12 14 16 18 200
Maximum Wave Force (x10 3N.m-2)
2 4 6 8 10 12 14 16 18 200
Maximum Wave Force (x10 3N.m-2)
2 4 6 8 10 12 14 16 18 200
Maximum Wave Force (x10 3N.m-2)
2 4 6 8 10 12 14 16 18 200
Maximum Wave Force (x10 3N.m-2)
2 4 6 8 10 12 14 16 18 200
Maximum Wave Force (x10 3N.m-2)
Categories of Wave Force (x10 3N.m-2)
0-5 5-10 10-15 >15
Categories of Wave Force (x10 3N.m-2)
2y = -0.160x + 3.526x - 6.4512r = 0.258; p < 0.02
2y= -0.289x + 5.751x + 26.1172r = 0.298; p < 0.01
2y= -0.143x + 3.223x - 9.0082r = 0.243; p = 0.02
Figure 6. (a) Species richness, (b) Shannon–Wiener diversity, (c) overall biomass, (d) filter-feeder biomass, (e) grazer biomass and (f) algal biomass,all relative to maximum wave forces experienced at the 22 sites sampled (A–V). Curves are polynomial trend lines.
L.K. BLAMEY AND G.M. BRANCH652
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
species most responsible for the similarity between the four
sheltered sites, and their dissimilarity to semi-exposed sites
(Figure 5). At all shores with wave forces greater than
‘sheltered’, M. galloprovincialis and the limpet S. argenvillei
were abundant. S. argenvillei was most abundant on semi-
exposed shores, M. galloprovincialis on exposed shores, and
both diminished on very exposed shores (see also Branch and
Steffani, 2004). Other species helped distinguish these
communities: the red alga Champia lumbricalis peaked on
semi-exposed shores, the tubeworm Gunnarea capensis on
exposed shores, and the red algae Plocamium cornutum and
Corallina spp. on very exposed shores.
Communities on shores with different grades of wave
action were also functionally different. On sheltered shores, C.
granatina controls algal growth but depends on a subsidy of
drift kelp from subtidal kelp beds to sustain its high densities
(Bustamante et al., 1995b). Only in the high shore did the
influence of grazers abate, and there hardy algae such as
Porphyra capensis and Ulva spp. proliferated.
On semi-exposed and exposed shores, S. argenvillei was
abundant, curtailing foliar algae but promoting encrusting
corallines. It too depends on access to fronds of subtidal kelp
plants to maintain its populations (Bustamante et al., 1995b).
Dominant filter-feeders, notably M. galloprovincialis and G.
capensis, are also maintained by particulate matter derived
from the kelp beds (Bustamante and Branch, 1996b). Shores
spanning sheltered to exposed therefore depend on various
forms of subsidization from subtidal kelp beds and are net
importers of materials (Hartnoll, 1983). Provisioning of
intertidal shores on the west coast of South Africa by
products from subtidal kelp beds is central to the high
overall biomass recorded there (Bustamante and Branch,
1996a).
On very exposed shores, almost all species diminished and
the system appeared to be physically rather than biologically
controlled. Plocamium cornutum and upright corallines peaked
there, promoted by their tolerance of wave action, diminished
spatial competition from mussels, and reduced grazing by
limpets.
Overall patterns relative to wave action
Species richness peaked at intermediate levels of wave action
(Figure 6(a)), as might be predicted by the intermediate
disturbance hypothesis, with biological control by a few
dominant species at the lower end of the wave action
spectrum, and physical control of most species at the upper
end (Connell, 1978). Shannon–Wiener diversity showed no
relationship with wave action (Figure 6(b)), probably due to
dominance by a few species: other work has shown that
diversity indices are sensitive to dominance (Soetaert and
Heip, 1990; Gray, 2000). Where communities are dominated
by a single species, diversity is reduced relative to sites with a
more even spread of species (McQuaid and Branch, 1984). The
greater richness of species at intermediate levels of wave action
was therefore offset by a reduction in evenness, levelling
diversity across the gradient of wave action.
Total biomass was clearly domed, being maximal at
intermediate wave intensity (Figure 6(c)), predominantly
influenced by filter feeders, which dominated the biomass
and exhibited the same pattern (Figure 6(d)). McQuaid and
Branch (1984), McQuaid et al. (1985) and Bustamante and
Branch (1996a) have previously described how filter-feeder
biomass is greater on wave-exposed than sheltered shores, but
they sampled only two grades of wave action. When Steffani
and Branch (2003a,b,c) sampled mussels across the entire
spectrum of wave action intensities experienced on the west
coast, domed relationships emerged for biomass, growth,
recruitment and condition (Branch and Steffani, 2004). The
shape of the biomass curve for filter feeders reflects inadequate
supplies of food at the sheltered extreme of the spectrum, and
physical limitations at the very exposed extreme. The major
contributor to filter-feeder biomass, M. galloprovincialis,
interacts strongly with grazers, depressing the biomass of the
S. argenvillei at sites where wave action is strong, but
coexisting with it at semi-exposed sites (Branch and Steffani,
2004). This uneasy truce between the two species was the main
factor distinguishing between semi-exposed and exposed
shores: M. galloprovincialis peaked on exposed shores and S.
argenvillei on semi-exposed shores. A notable feature of all
grades of wave action was the scarcity of barnacles. It is likely
that upwelling—a feature of the region—exports barnacle
larvae and provides little opportunity for their return to the
shore. In California and Chile barnacle settlement is inversely
related to upwelling (Connolly et al., 2001; Navarrete et al.,
2005). Maximum values of filter-feeder biomass as a whole
were higher than those for sites with equivalent wave action on
the south and east coasts of South Africa (Van Erkom
Schurink and Griffiths, 1990; Bustamante et al., 1995a;
Bustamante and Branch, 1996a), reflecting the higher
productivity on the west coast associated with upwelling.
Grazer biomass was high at most sites, but declined where
wave action was strong to very strong (Figure 6(e)), probably
curtailed by the physical demands of remaining attached and
inhibition of feeding (Denny et al., 1985). High biomasses at
sheltered sites were attributable to C. granatina, and those at
semi-exposed sites to S. argenvillei, both of which reach
exceptionally high densities and biomasses on the west coast of
South Africa, supported by subsidies of drift or attached kelp
provided by subtidal kelp beds (Bustamante et al., 1995b).
Algal biomass was generally low, implying that all shores
would have been net importers of energy. With one exception,
grazer biomass always exceeded algal biomass, emphasizing
the importance of subsidies to maintain primary consumers.
As recorded elsewhere in South Africa (McQuaid et al., 1985),
algal biomass tended to increase with exposure, as the biomass
of grazers declined (Figure 6(f)), so that reliance on imported
materials increases as wave action declines—contrary to
Hartnoll’s (1983) observation that sheltered shores are
normally net exporters and exposed shores net importers.
Test-driving the process
For the classification of rocky shores into three habitats to be
useful, it needs to be applicable elsewhere. A previous analysis
by Emanuel et al. (1992) indicates this is the case, at least
within the limits of the Namaqua biogeographic province.
Across the 1200 km Namaqua coast, they demonstrated that
sites with comparable wave action had greater similarities in
community composition than were evident between sites that
were closely situated but experienced different intensities of
wave action. One can therefore be confident that wave action
does act as a useful means of identifying distinct habitats with
quantifiably different communities.
HABITAT DIVERSITY RELATIVE TO WAVE ACTION ON ROCKY SHORES 653
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
These conclusions were verified by sampling five sites
250 km to the south of the study area but still within the same
biogeographic region. The classification of all five concurred
with the division of habitats into three levels of wave action.
This increased confidence both in the classification and in
the ability to estimated wave intensity from simple measures
of topography and prevailing wave direction. This has
important implications. It suggests that not only can
community composition be estimated from wave intensity,
but that the latter can be estimated from easily obtainable
indirect measures. If it is possible to estimate wave forces
consistently from topographic maps or orthophotographs and
data on prevailing wind and wave directions, then entire
regions can be mapped from remote data to determine the
position and extent of rocky-shore habitats.
It is still necessary to fully test the validity of such physical
surrogates, and to do so across biogeographic boundaries, to
explore their generality.
Application
The first level of decision-making in the hierarchy advocated
by Hockey and Branch (1997) and Roberts et al. (2003a,b) is
that conservation be accorded to all biogeographic provinces.
The first steps of determining biogeographic patterns around
the coast of southern Africa were taken early (Stephenson,
1939; summarized in Stephenson and Stephenson, 1972), and
since refined by Emanuel et al. (1992) and Sink et al. (2005).
Five distinct biogeographic provinces are now recognized.
These are well defined for the intertidal and shallow subtidal
zones, but with increasingly less precision as one moves
offshore, where information on the distribution of species is
deficient. Lombard et al. (2004) provisionally dealt with this by
recognizing ‘bioregions’ that incorporate both along-shore
biogeographic patterns and likely changes in community
composition that will occur as one moves offshore, and
employed these bioregions when recommending possible
locations of future MPAs.
Within bioregions, all habitats need protection. This is the
second tier in the hierarchy of conservation goals. Based on the
current data, at a minimum, rocky-shore habitats with three
grades of wave action are sufficiently distinct to require
independent protection: sheltered, semi-exposed to exposed,
and very exposed. Although quantitatively distinguishable in
terms of their maximum wave forces (0–5, 5–15 and
415� 103Nm�2), they could also be recognized from simple
estimates based on topography and wave orientation. The
three habitats also constitute functionally different entities: (i)
sheltered shores dominated by Cymbula granatina and
dependent on drift kelp; (ii) moderately exposed shores
dominated by Scutellastra argenvillei and Mytilus
galloprovincialis, dependent on attached kelp and particulate
fragments; (iii) very exposed shores that are physically-driven
and where algae such as Plocamium cornutum and Corallina
spp. reach their primacy.
In this context, a comparison with sandy beaches is
instructive. Sandy beaches can be classified on a continuum
from reflective (steep, coarse-grained, with oncoming waves
directed at the face of the beach) to dissipative (shallow, fine-
grained, with strong offshore wave action that is dissipated
over the flat beach). Species richness rises from reflective to
dissipative conditions (McLachlan et al., 1993). Importantly,
this involves the addition of species, not the substitution of one
set of species by another. Thus, reflective beaches contain a
subset of the species found on dissipative beaches, and
conservation of representative dissipative beaches will protect
more species and will cover all those species found on reflective
beaches. Dissipative beaches therefore assume priority over
reflective ones in terms of conservation value. This situation
contrasts with that on rocky shores, where different suites of
species are involved at different intensities of wave action, and
protection of one type of habitat would not offer protection to
assemblages in other habitats.
A preliminary analysis of conservation on the west coast of
South Africa has already been undertaken, revealing that (1)
there is inadequate protection granted to the Namaqua
biogeographic province; (2) the coast is subject to intense
fishing and diamond-mining that conflict with conservation
goals; and (3) the region between the Groen and Spoeg Rivers
that constituted the study area contains a high diversity of
habitats and is a priority area for future conservation
(Emanuel et al., 1992).
Recognition of the role of MPAs
‘No-take’ Marine Protected Areas (MPAs) are now well
established as a ‘necessary but not sufficient’ tool for marine
conservation (Allison et al., 1998) and have repeatedly been
proven to increase average size, density and biomass of
individual species and the diversity of communities (Bennett
and Attwood, 1991; Polunin and Roberts, 1993; Allison et al.,
1998; Halpern, 2003). However, to reach their full potential,
MPAs must be selected on sound ecological criteria that
maximize their planned goals (Hockey and Branch, 1994;
1997; Allison et al., 1998; Carr et al., 2003; Halpern, 2003;
Roberts et al., 2003a,b). But how should we best select and
design MPAs?
Rival merits of different approaches to identifying
conservation priorities
There are two distinct aspects to the challenge of selecting
MPAs. The first is whether species or habitats serve as the
most useful units for decisions. Actions based on species do
ensure that all species are considered, but usually ignore the
relative abundance of species and require detailed information
that seldom exists for all taxa. Attempts have been made to test
whether higher taxa can be employed instead of species, or if
well-known taxonomic groups can be used as a surrogate for
all species. The results have been mixed. Gladstone (2002)
showed that molluscs are an effective indicator group but
macroalgae are not; and Beger et al. (2003) argued that groups
that are spatially heterogeneous such as fish are better
indicators than those that are not, such as corals. By
comparison with analyses based on species, habitats are
easier to map, require less demanding information, and are
better at incorporating the structure and functioning of
ecosystems and communities (Sladek Nowlis and
Friedlander, 2004).
The second issue is the rival merits of ‘hotspot’,
biogeographic and complementarity approaches. The
‘hotspot’ approach focuses on species richness and endemism
(Myers, 1990; Myers et al., 2000), favouring conservation of
regions with high levels of richness and endemism. The
L.K. BLAMEY AND G.M. BRANCH654
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
underlying philosophy is that such areas yield maximal gains
by protecting the greatest number of species and/or endemics
relative to investment, a strategy adopted by Conservation
International (Mittermeier, 2000). The approach is at its best
in identifying entire regions most worthy of conservation, and
in rating comparable systems, as Roberts et al. (2002) have
done in identifying conservation priorities for tropical reefs.
But even then, Lourie and Vincent (2004) argue that it is only
applicable within biogeographic regions. It certainly cannot
usefully compare different types of ecosystems or habitats even
within a region—say sandy beaches (which have low diversity)
with tropical coral reefs (with high diversity)—because there is
no intrinsic reason why high-diversity ecosystems should
warrant greater conservation than low-diversity ones. For
this reason, the hotspot approach risks overlooking low-
diversity habitats, areas or regions.
Hotspot identification requires detailed information on
species distribution. In contrast, once habitats are defined, they
can be rapidly mapped with minimal expertise. They are also
amenable to identification with remote sensing or via simple
proxies such coastal topography and prevailing winds.
The biogeographic approach dictates that selection of
conservation areas must first be based on identification and
coverage of all biogeographic regions, and that within each
biogeographic region, adequate protection be afforded to all
habitats (Hockey and Branch, 1994; Roberts et al., 2003a,b).
In its infancy, this approach advocated selection of protected
areas at the edges and centres of biogeographic regions
(Hockey and Branch, 1997), but with development of
algorithms based on iterative, optimizing or simulated
annealing approaches, it is now possible to identify the most
efficient complementary combinations of areas within
biogeographic regions that will provide desired levels of
protection for habitats or species (Leslie et al., 2003).
Pressey and Nicholls (1989), Turpie et al. (2000), Awad
et al. (2002), Beger et al. (2003), and Fox and Beckley
(2005) have compared hotspots, biogeographic and comple-
mentarity approaches in terms of their efficiency in achieving
representative conservation. Biogeographic and comple-
mentarity approaches had fairly similar efficiencies. Using
hotspots proved least efficient because attention falls on sites
with high species richness or endemism, which are often closely
situated and therefore contain similar suites of species.
Moreover, species richness hotspots often failed to coincide
with endemism hotspots, so that species-rich localities did not
protect many endemics and vice versa.
Thus it is argued, first, that using habitats rather than (or in
addition to) species as the units of conservation is superior in
several respects, and essential when detailed data on species
distributions are lacking. Second, it is necessary to combine
biogeographic and complementarity analyses of habitats (or
species) in a hierarchical manner, with biogeographic analyses
defining the first step, and complementarity analyses of
habitats taking place within each biogeographical region to
efficiently preserve all habitats (Hockey and Branch, 1997;
Roberts et al., 2003a,b).
In conclusion, rocky shores on the west coast of South
Africa constitute at least three discrete habitats. Failure to
protect all three habitats would mean that the full spectrum of
community types occupying rocky shores would not gain
protection. It would have been inappropriate to apply the
‘hotspot’ concept to the data to decide conservation priorities
among habitats: highest diversity would have favoured
protection of shores with intermediate levels of wave action,
ignoring the fact that different suites of species and different
functional attributes exist for each habitat. It is believed that
habitat diversity is a better measure of the conservation value
of an area than can be derived from a consideration of species
richness and endemism.
ACKNOWLEDGEMENTS
We thank Nina Steffani, Tammy Robinson, Paula de Coito,
Matthew Bird, and Evie Wieters for help in the field, and
Hedley Grantham and an anonymous reviewer for their
helpful comments. Funding was received from the University
of Cape Town, the National Research Foundation and the
Andrew Mellon Foundation.
REFERENCES
Andrew NL, Viejo RM. 1998. Effects of wave exposure andintraspecific density on the growth and survivorship ofSargassum muticum (Sargassaceae: Phaeophyta). EuropeanJournal of Phycology 33: 251–258.
Allison GW, Lubchenco J, Carr MH. 1998. Marine reservesare necessary but not sufficient for marine conservation.Ecological Applications 8: S79–S92.
Avery RP. 2003. Marine and terrestrial conservationplanning—how different are they? In Conservation ofMarine Environments: Out of Sight, Out of Mind,Hutchings P, Lunney D. (eds). Royal Zoological Society ofNew South Wales: Mosman, New South Wales.
Awad AA, Griffiths CL, Turpie JK. 2002. Distribution ofSouth African marine benthic invertebrates applied to theselection of priority conservation areas. Diversity andDistributions 8: 129–145.
Ballantine WJ. 1961. A biologically-defined exposure scale forthe comparative description of rocky shores. Field Studies 1:1–19.
Banks SA, Skilleter GA. 2007. The importance ofincorporating fine-scale habitat data into the design of anintertidal marine reserve. Biological Conservation 138: 13–29.
Beger M, Jones GJ, Munday PL. 2003. Conservation of coralreef biodiversity: a comparison of reserve selectionprocedures for corals and fish. Biological Conservation 111:53–62.
Bennett BA, Attwood CG. 1991. Evidence for recovery of asurf-zone fish assemblage following the establishment of amarine reserve on the southern coast of South Africa.Marine Ecology Progress Series 75: 173–181.
Bertness MD, Gaines SD, Bermudez D, Sanford E. 1991.Extreme spatial variation in the growth and reproductiveoutput of the acorn barnacle Semibalanus balanoides.MarineEcology Progress Series 75: 91–100.
Blanchette CA. 1997. Size and survival of intertidal plants inresponse to wave action: a case study with Fucus gardneri.Ecology 78: 1563–1578.
Branch GM, Marsh AC. 1978. Tenacity and shell shape in sixPatella species: adaptive features. Journal of ExperimentalMarine Biology and Ecology 34: 111–130.
Branch GM, Odendaal F. 2003. Marine protected areas andwave action: impacts on a South African limpet, Cymbulaoculus. Biological Conservation 114: 255–269.
HABITAT DIVERSITY RELATIVE TO WAVE ACTION ON ROCKY SHORES 655
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
Branch GM, Steffani CN. 2004. Can we predict the effects ofalien species? A case-history of the invasion of South Africaby Mytilus galloprovincialis (Lamarck). Journal ofExperimental Marine Biology and Ecology 300: 189–215.
Brown JM, Quinn JF. 1988. The effect of wave action ongrowth in three species of intertidal gastropods. Oceologia75: 420–425.
Bustamante RH, Branch GM. 1996a. Large scale patterns andtrophic structure of southern African rocky shores: the rolesof geographic variation and wave exposure. Journal ofBiogeography 23: 339–351.
Bustamante RH, Branch GM. 1996b. The dependence ofintertidal consumers on kelp-derived organic matter on thewest coast of South Africa. Journal of Experimental MarineBiology and Ecology 196: 1–28.
Bustamante RH, Branch GM, Eekhout S, Robertson B,Zoutendyk Z, Schleyer M, Dye A, Hanekom N, Keats D,Jurd M, McQuaid C. 1995a. Gradients of intertidal primaryproductivity around the coast of South Africa and theirrelationships with consumer biomass. Oecologia 102:189–201.
Bustamante RH, Branch GM, Eekhout S. 1995b. Maintenanceof an exceptional intertidal grazer biomass in South Africa:subsidy by subtidal kelps. Ecology 76: 2314–2329.
Bustamante RH, Branch GM, Eekhout S. 1997. The influencesof physical factors on the distribution and zonation patternsof South African rocky-shore communities. South AfricanJournal of Marine Science 18: 119–136.
Carr MH, Neigel JE, Estes JA, Andelman S, Warner RR,Largier JL. 2003. Comparing marine and terrestrialecosystems: implications for the design of coastal marinereserves. Ecological Applications 13: S90–S107.
Carrington E. 1990. Drag and dislodgement of an intertidalmacroalga: consequences of morphological variation inMastocarpus papillatus Keutzing. Journal of ExperimentalMarine Biology and Ecology 139: 185–200.
Connell JH. 1978. Diversity in tropical rain forests and coralreefs: high diversity of trees and corals is maintained only ina non-equilibrium state. Science 199: 1302–1310.
Connolly SR, Menge BA, Roughgarden J. 2001. A latitudinalgradient in recruitment of intertidal invertebrates in thenortheast Pacific Ocean. Ecology 82: 1799–1813.
Cowling RM, Heijnis CJ. 2001. The identification of BroadHabitat Units as biodiversity entities for systematicconservation planning in the Cape Floristic Region. SouthAfrican Journal of Botany 67: 15–38.
Davenport J, Davenport JL. 2005. Effects of shore height,wave exposure and geographical distance on thermal nichewidth of intertidal fauna. Marine Ecology Progress Series292: 41–50.
Dayton PK. 1971. Competition, disturbance and communityorganization: the provision and subsequent utilization ofspace in a rocky intertidal community. EcologicalMonographs 41: 351–389.
Denny MW. 1985. Wave forces on intertidal organisms: a casestudy. Limnology and Oceanography 30: 1171–1187.
Denny MW. 1987. Lift as a mechanism of patch initiation inmussel beds. Journal of Experimental Marine Biology andEcology 113: 231–245.
Denny MW, Daniel TL, Koehl MAR. 1985. Mechanical limitsto size in wave-swept organisms. Ecological Monographs 55:69–102.
Emanuel BP, Bustamante RH, Branch GM, Eekhout S,Odendaal FJ. 1992. A zoogeographic and functionalapproach to the selection of marine reserves on the westcoast of South Africa. South African Journal of MarineScience 12: 341–354.
Fox NJ, Beckley LE. 2005. Priority areas for conservation ofWestern Australian coastal fishes: a comparison of hotspot,biogeographical and complementarity approaches.Biological Conservation 125: 399–410.
Friedlander A, Sladek Nowlis J, Sanchez JA, Appeldoorn R,Usseglio P, McCormick C, Bejerano S, Mitchell-Chui A.2003. Designing effective marine protected areas inSeaflower Biosphere Reserve, Colombia, based onbiological and sociological information. ConservationBiology 17: 1769–1784.
Gaylord B, Blanchette CA, Denny MW. 1994. Mechanicalconsequences of size in wave-swept algae. EcologicalMonographs 64: 287–313.
Gladstone W. 2002. The potential value of indicator groups inthe selection of marine reserves. Biological Conservation 104:211–220.
Gray JS. 2000. The measurement of marine species diversity,with an application to the benthic fauna of the Norwegiancontinental shelf. Journal of Experimental Marine Biologyand Ecology 250: 23–49.
Halpern BS. 2003. The impact of marine reserves: do reserveswork and does reserve size matter? Ecological Applications13: S117–S137.
Harley CDG, Helmuth BST. 2003. Local- and regional-scaleeffects of wave exposure, thermal stress and absolute versuseffective shore level on patterns of intertidal zonation.Limnology and Oceanography 48: 1498–1508.
Hartnoll RG. 1983. Bioenergetics of a limpet-grazed intertidalcommunity. South African Journal of Science 79: 166–167.
Hockey PAR, Branch GM. 1994. Conserving marinebiodiversity on the African coast: implications of aterrestrial perspective. Aquatic Conservation: Marine andFreshwater Ecosystems 4: 345–362.
Hockey PAR, Branch GM. 1997. Criteria, objectives andmethodology for evaluating marine protected areas inSouth Africa. South African Journal of Marine Science 18:369–383.
Jenkins SR, Hartnoll RG. 2001. Food supply, grazing activityand growth rate in the limpet Patella vulgata L.: acomparison between exposed and sheltered shores. Journalof Experimental Marine Biology and Ecology 258: 123–139.
Kelleher G, Kenchington RA. 1990. Political and socialdynamics for establishing marine protected areas. Natureand Resources 26(2): 31–38.
Leslie H, Ruckelhaus M, Ball IR, Andelman S,Possingham HP. 2003. Using siting algorithms in thedesign of marine reserve networks. Ecological Applications13: S185–S195.
Lewis JR. 1964. The Ecology of Rocky Shores. EnglishUniversity Press: London.
Lombard AT, Cowling RM, Pressey RL, Rebelo AG. 2003.Effectiveness of land classes as surrogates for species inconservation planning for the Cape Floristic Region.Biological Conservation 112: 45–63.
Lombard AT, Strauss T, Harris J, Sink K, Attwood C,Hutchings L. 2004. South African National SpatialBiodiversity Assessment 2004: Technical Report. Volume 4:Marine Component. Pretoria: South African NationalBiodiversity Institute.
Lourie SA, Vincent ACT. 2004. Using biogeography to helpset priorities in marine conservation. Conservation Biology18: 1004–1020.
Margules CR, Pressey RL. 2000. Systematic conservationplanning. Nature 405: 243–253.
McGuinness KA. 1987a. Disturbance and organisms onboulders I. Patterns in the environment and thecommunity. Oecologia 71: 409–419.
L.K. BLAMEY AND G.M. BRANCH656
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc
McGuinness KA. 1987b. Disturbance and organisms onboulders II. Cause of patterns in diversity and abundances.Oecologia 71: 420–430.
McLachlan A, Jaramillo E, Donn TE, Wessels F. 1993. Sandybeach macrofauna communities and their control by thephysical environment: a geographic comparison. Journal ofCoastal Research 15: 27–38.
McQuaid CD, Branch GM. 1984. The influence of seatemperature, substratum and wave exposure on rockyintertidal communities: an analysis of faunal and floralbiomass. Marine Ecology Progress Series 19: 145–151.
McQuaid CD, Branch GM, Crowe CC. 1985. Biotic andabiotic influences on rocky intertidal biomass and richness inthe southern Benguela region. South African Journal ofZoology 20: 115–122.
Menge BA, Sutherland JP. 1987. Community regulation:variation in disturbance, competition and predation inrelation to environmental stress and recruitment. AmericanNaturalist 130: 730–757.
Mittermeier RA. 2000. Conservation International andbiodiversity conservation. Nature 405: 255.
Myers N. 1990. The biodiversity challenge: expanded hotspotanalysis. Environmentalist 10: 243–256.
Myers N, Mittermeier RA, Mittermeier CG, Da FonsecaGAB, Kent J. 2000. Biodiversity hotspots for conservationpriorities. Nature 403: 853–858.
Navarrete SA, Wieters EA, Broitman BR, Castilla JC. 2005.Scales of benthic-pelagic coupling and the intensity ofspecies interactions: from recruitment limitation to topdown control. Proceedings of the National Academy ofSciences USA 102: 18046–18051.
Oliver I, Holmes A, Dangerfield JM, Gillings M, Pik AJ,Britton DR, Holley M, Raison M, Logan V, Pressey RL,Beattie AJ. 2004. Land systems as surrogates for biodiversityin conservation planning. Ecological Applications 14:485–503.
Polunin NVC, Roberts CM. 1993. Greater biomass and valueof target coral-reef fishes in two small Caribbean marinereserves. Marine Ecology Progress Series 100: 167–176.
Pressey RL, Nicholls AO. 1989. Efficiency in conservationevaluation: scoring versus iterative approaches. BiologicalConservation 50: 199–218.
Roberts CM, McClean CJ, Veron JEN, Hawkins JP,Allen GR, McAllister DE, Mittermeier CG, Schueler FW,Spalding M, Wells F, et al. 2002. Marine biodiversityhotspots and conservation priorities for tropical reefs.Science 295: 1280–1284.
Roberts CM, Andelman S, Branch GM, Bustamante RH,Castilla JC, Dugan J, Halpern BS, Lafferty KD, Leslie H,Lubchenco J, et al. 2003a. Ecological criteria for evaluatingcandidate sites for marine reserves. Ecological Applications13: S199–S214.
Roberts CM, Branch GM, Bustamante RH, Castilla JC,Dugan J, Halpern BS, Lafferty KD, Leslie H, Lubchenco J,McArdle D, et al. 2003b. Application of ecological criteria inselecting marine reserves and developing reserve networks.Ecological Applications 13: S215–S228.
Sink KJ, Branch GM, Harris JM. 2005. Biogeographicpatterns in rocky intertidal communities in KwaZulu-Natal, South Africa. African Journal of Marine Science 27:81–96.
Sladek Nowlis J, Friedlander A. 2004. Design and designationof marine reserves. In Marine Reserves, a Guide to Science,Design and Use, Sobel J, Dahlgren C (eds). Island Press:Washington.
Soetaert K, Heip C. 1990. Sample-size dependence of diversityindices and the determination of sufficient sample size in ahigh-diversity deep-sea environment. Marine EcologyProgress Series 59: 305–307.
Sousa WP. 1979. Disturbance in marine intertidal boulderfields: the non-equilibrium maintenance of species diversity.Ecology 60: 1225–1239.
Steffani CN, Branch GM. 2003a. Growth rate, condition andshell shape of Mytilus galloprovincialis: responses to waveexposure. Marine Ecology Progress Series 246: 197–209.
Steffani CN, Branch GM. 2003b. Temporal changes in aninteraction between an indigenous limpet Scutellastraargenvillei and an alien mussel Mytilus galloprovincialis:effects of wave exposure. African Journal of Marine Science25: 195–212.
Steffani CN, Branch GM. 2003c. Spatial comparisons ofpopulations of an indigenous limpet Scutellastra argenvilleiand an alien musselMytilus galloprovincialis. African Journalof Marine Science 25: 213–229.
Stephenson TA. 1939. The constitution of the intertidal faunaand flora of South Africa. Part I. Journal of the LinneanSociety (Zoological ) 40: 487–536.
Stephenson TA, Stephenson A. 1972. Life Between Tidemarkson Rocky Shores. Freeman: San Francisco, CA.
Stevens T, Connolly RM. 2004. Testing the utility of abioticsurrogates for marine habitat mapping at scales relevant tomanagement. Biological Conservation 119: 351–362.
Turpie JK, Beckley LE, Katua SM. 2000. Biogeographyand the selection of priority areas for conservation ofSouth African coastal fishes. Biological Conservation 92:59–72.
Van Erkom Schurink C, Griffiths CL. 1990. Marine mussels ofSouthern Africa— their distribution patterns, standingstocks, exploitation and culture. Journal of ShellfishResearch 9: 75–85.
Ward TJ, Vanderklift MM, Nicholls AO, Kenchington RA.1999. Selecting marine reserves using habitats and speciesassemblages as surrogates for biological diversity. EcologicalApplications 9: 691–698.
HABITAT DIVERSITY RELATIVE TO WAVE ACTION ON ROCKY SHORES 657
Copyright r 2008 John Wiley & Sons, Ltd. Aquatic Conserv: Mar. Freshw. Ecosyst. 19: 645–657 (2009)
DOI: 10.1002/aqc