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Estuarine, Coastal and Shelf Science
January 2015, Volume 152, Pages 11-22
http://dx.doi.org/10.1016/j.ecss.2014.11.005
http://archimer.ifremer.fr/doc/00226/33747/
© 2014 Elsevier Ltd. All rights reserved.
Achimer
http://archimer.ifremer.fr
Community, Trophic Structure and Functioning in two
contrasting Laminaria hyperborea forests
Leclerc Jean-Charles
1, 2, *
1, 2
3
, Riera Pascal , Laurans Martial , Leroux Cedric
1, 2
Davoult Dominique
1, 4
, Lévêque Laurent
1, 4
,
1
Sorbonne Universités, UPMC Univ Paris 6, Station Biologique de Roscoff, Place Georges Teissier, 29680
Roscoff, France
2
CNRS, UMR 7144 AD2M, Station Biologique de Roscoff, Place Georges Teissier, 29680 Roscoff, France
3
IFREMER, Laboratoire de Biologie Halieutique, Centre Bretagne, BP 70,29280 Plouzané, France
4
CNRS, FR 2424, Station Biologique de Roscoff, Place Georges Teissier,29680 Roscoff, France
* Corresponding author : Jean-Charles Leclerc, email address : leclercjc@gmail.com
Abstract :
Worldwide kelp forests have been the focus of several studies concerning ecosystems dysfunction in the past
decades. Multifactorial kelp threats have been described and include deforestation due to human impact,
cascading effects and climate change. Here, we compared community and trophic structure in two
contrasting kelp forests off the coasts of Brittany. One has been harvested five years before sampling and
shelters abundant omnivorous predators, almost absent from the other, which has been treated as preserved
from kelp harvest. δ15N analyses conducted on the overall communities were linked to the tropho-functional
structure of different strata featuring these forests (stipe and holdfast of canopy kelp and rock). Our results
yielded site-to-site differences of community and tropho-functional structures across kelp strata, particularly
contrasting in terms of biomass on the understorey. Similarly, isotope analyses inferred the top trophic
position of Marthasterias glacialis and Echinus esculentus which may be considered as strong interactors in
the sub-canopy. We interrogate these patterns and propose a series of probable and testable alternative
hypotheses to explain them. For instance, we propose that differences of trophic structure and functioning
result from confounded effects of contrasting wave dissipation depending on kelp size-density structure and
community cascading involving these omnivorous predators. Given the species diversity and complexity of
food web highlighted in these habitats, we call for further comprehensive research about the overall strata
and tropho-functional groups for conservation management in kelp forests.
Keywords : Laminaria hyperborea, Community cascade, Stable isotopes, Biomass, Suspension-feeders,
Omnivorous predators
1. Introduction
Worldwide kelp forests harbour high biodiversity and host complex biological interactions, expected to
promote their stability (see Steneck et al., 2002 and Filbee-Dexter and Scheibling, 2014 for reviews). In
North-eastern Atlantic, kelp forests are dominated by
Please note that this is an author-produced PDF of an article accepted for publication following peer review. The definitive
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Laminaria hyperborea, a species distributed from Portugal to Northern Norway, at depths
ranging from 0 to 30 m (Kain, 1971). In pristine areas, Laminaria hyperborea individuals can
reach up to 3.5 m in length and can be considered as a habitat of their own composed of three
stratified parts: the lamina, the stipe, and the holdfast. Among these strata, associated
communities are particularly diverse and differently distributed (Moore, 1973; Schultze et al.,
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1990; Christie et al., 2003). Community structure and distribution of mobile fauna has often
been linked to the structural complexity of kelp individuals (Jones, 1971; Moore, 1973) and
epiphytic seaweeds (Norderhaug et al., 2002; Christie et al., 2007). Within epiphytes and
holdfasts, environmental factors such as turbidity and wave exposure, interacting with the
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complexity of seaweed forming-habitat, can also influence mobile fauna distribution (Moore,
1973; Norderhaug et al., 2012; Norderhaug et al., 2014).While these strata have been
investigated, understorey communities are still overlooked. The kelp canopy can provide
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favourable conditions for the development of functionally diverse seaweeds on the
surrounding substratum (Norton et al., 1977), expected to shelter complex communities of
sessile and mobile fauna.
Among the multiple threats of kelp (see Steneck et al., 2002 for review), sea urchin
overgrazing can lead to alternative stable states of the ecosystem dominated by encrusting
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coralline algae and urchins, commonly named barrens as a consequence of an extensive
habitat loss. In northern Europe, some L. hyperborea populations have been particularly
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studied in Norway, and overgrazing events were reported owing to the local abundance of the
green sea urchin Strongylocentrotus droebachiensis, co-occurring with the edible sea urchin
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Echinus esculentus (Sivertsen, 1997). While S. droebachiensis feeds either on adult or young
kelp, E. esculentus grazing seems mostly restricted to the understorey kelp recruits and other
algae, and can exercise some control over L. hyperborea forests and associated communities
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(Jones and Kain, 1967; Sjøtun et al., 2006; Norderhaug and Christie, 2009). On the rocky
shores of Brittany, below the southern distribution of S. droebachiensis, only a few grazers,
including E. esculentus, are able to feed directly on kelp. This report has been suggested to
favour their local persistence (Leblanc et al., 2011). Interestingly, E. esculentus has also been
described as an omnivorous (i.e. feeding on several trophic level) and opportunistic predator
(Allen, 1899; Forster, 1959; Comely and Ansell, 1988). Variable foraging behaviour such as
omnivory can be of critical importance in strengthening food web interactions, including
cascading effects (Emmerson and Yearsley, 2004; Bruno and O'Connor, 2005; O'Gorman and
Emmerson, 2010). For instance, it has been proposed, on the base of modelled food webs, that
a stable community should be favoured since omnivorous interactions are weak (Emmerson
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and Yearsley, 2004). In complex coastal mesocosm communities, manipulating the abundance
of strong interactors, such as predator echinoderms, has been shown to skew food web
properties without any impact on species richness (O'Gorman and Emmerson, 2010).
In Brittany, L. hyperborea is harvested for almost two decades, given their quantity of
alginic acid, valuable for stabilizing and suspending properties (Chapman and Chapman,
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1980). The major part of kelp exploitation is localized within the ‘Parc Naturel Marin
d’Iroise’ which was created in 2007 in order to reconcile the environmental management with
the development of human activity, and actually differs from a sanctuary. Within the park, the
net kelp trawling ranged officially between 2,000 and 12,300 tons per year during the last
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decade. With regards to previous studies dealing with kelp dynamics and rate of stipe
production with age (Sjøtun et al., 1993; Sjøtun and Fredriksen, 1995), harvesting has been
zoned on the basis of a five year-rotation system. Up to now, the lack of knowledge about the
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recovery of communities and food web associated with kelp forests indicates the need for
further long-term researches, taking into account their overall components (Sivertsen, 1997;
Christie et al., 1998; Waage-Nielsen et al., 2003; Lorentsen et al., 2010; Smale et al., 2013).
An individual L. hyperborea may reach up about 20 years old and produce a new hapteron
ring around its holdfast during each spring (Kain, 1963; Rinde and Sjøtun, 2005). From one
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year to another, this peripheral growth increases both the structural complexity and the size of
the holdfast forming microhabitat, hence promoting the colonization and the diversity of
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associated assemblages (Jones, 1971; Christie et al., 1998). Studies of microhabitat
complexity should also be improved considering the surrounding substratum, which is mainly
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overlooked in European kelp forests despite its value for local diversity (Waage-Nielsen et al.,
2003). Given the heterogeneous topography and the local cover by functionally diverse and
abundant organisms (Norton et al., 1977), the rock represents a complex biotope important in
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management.
The present study aimed to report biodiversity and trophic structure patterns associated
with two L. hyperborea forests of contrasting conditions and histories. Though comparable
overall kelp densities, one area has been moderately kelp-harvested for almost one decade,
whereas the other has been, to our knowledge, preserved from exploitation. In parallel, the
former has been consistently observed to shelter large echinoderms (sea-urchins and sea-stars)
in important densities, nearly absent from the other. We investigated patterns in diversity and
biomass distribution of macroalgae and macrofauna species across kelp forest strata, and
understory megafauna densities between sites. These patterns are discussed according to
biomass distribution of tropho-functional group and trophic level estimations in order to offer
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alternative hypotheses to explain these stratum-dependent patterns and their potential
implications in future kelp forest conservation management.
2. Material & Methods
2.1. Study sites
The study sites were located near Roscoff and within the Molène archipelago (Fig. 1)
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along the north-western coast of Brittany. These sites, separated by 70 km, are part of the
same well-mixed (throughout the year) water mass at the English Channel entrance (Birrien et
al., 1991). The Roscoff site (48°43.556N, 4°01.415W) is a dense, sheltered boulder field with
some coarse interstitial sediment, lying upon a flat rocky reef, situated 1 km from the shore
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and 2.5 m below chart datum. The kelp forest (≈ 1 km²) is surrounded by mosaic habitats,
represented by offshore infralittoral coarse sand/gravel flats, other kelp forests at comparable
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depth, few Zostera spp. beds on the infralittoral fringe, intertidal rocky reefs dominated by
Fucales, and intertidal fine sand beaches (Joubin, 1909). Unlike in the Molène area, kelp
harvesters started to trawl L. hyperborea in 2007, for an official net crop ranging between 300
and 3,300 tons per year up to now. From diver observations and information provided by local
fishermen, the Roscoff study site was considered to be preserved from kelp-harvesting, but
was frequently exploited for abalones and large decapods. During autumn 2010, L.
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hyperborea densities were measured on the site within 0.25 m² 3-sided quadrats (n = 60), for
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three size classes: 0-10 cm, 10-40 cm, > 40 cm. Densities were estimated at 16.9 ± 11.4
individuals m-2 (± S.D.), largely dominated by adults from the canopy layer (Stipe > 40 cm,
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13.1 ± 6.6 ind. m-2). The Molène site (48°25.089N, 4°54.742W) is located within the ‘Parc
Naturel Marin d’Iroise’. This site is a boulder field with some coarse interstitial sediment,
lying upon a flat rocky reef (‘Helle’ plateau), situated 3.5 km from the nearest shore (Molène
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Island) and 9.0 m below chart datum. The ‘Helle’ plateau (≈ 8 km²) is surrounded by
circalittoral heterogeneous sand flats and infralittoral coarse biogenic gravel and
heterogeneous sand beds (Raffin, 2003). According to fishermen (Ifremer data), L.
hyperborea was not harvested at this site for five years before sampling. During March 2011,
after winter recruitments, kelp densities were estimated within 1 m² quadrats (n = 15) at 18.1
± 9.1 individuals m-2 (± S.D.), dominated by medium individuals (Stipe 10-40 cm, 5.1 ± 2.5
ind. m-2) and adults (6.9 ± 3.2 ind. m-2). Although kelp density displayed site-to-site
differences in the size-canopy structure, any causal link with kelp trawling cannot be
established since initial condition and temporal variability within both sites remains unknown
(Osenberg and Schmitt, 1996).
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2.2. Community and trophic structure
Sampling was performed by scuba-divers in late March 2011 (early spring). At each
sampling site, L. hyperborea adults (n = 5) were randomly collected in 1 mm mesh bags
(Christie et al., 2003). A substantial part of the within-site variability in the biotic colonisation
of kelp can be explained by age and size of kelp (Whittick, 1983; Anderson et al., 2005);
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therefore only adult kelp from the canopy layer were selected underwater by their total length
(1-2 m) before further biometric analyses in the laboratory. Few mobile species inhabit the
lamina (Norton et al., 1977; Christie et al., 2003); therefore stipe and its adjoining lamina
were collected in the same bag and the holdfast was collected separately. The surrounding
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substratum was sampled in 0.1 m² quadrats (n = 5) using an air pump connected to a 1 mm
mesh collector.
In the laboratory, each bag was carefully rinsed with seawater over a 500 µm mesh
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sieve. Bag contents were fixed in their entirety with a buffered formaldehyde solution (3 %).
Fauna and flora were sorted according to origin (stipe/lamina, holdfast or rock) and their ashfree dry mass (AFDM) determined at the species level, except for pooled measurement of the
Corallinale/Peyssonelia sp. encrusting complex (Kennelly, 1989). In addition to mass
measurement of their different parts, adult kelps were processed for age, size and holdfast
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volume. Individual kelp were aged using the method of Kain (1963), ranging from 3 to 8
years without any difference between sites (Appendix A, t-test, t = – 0.717, P = 0.494).
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While no difference was detected for stipe length (72-128 cm) and mass (21.5-67.7 gAFDM),
the mean diameter (measured from 5 points per stipe) was slightly higher in Molène (2.8 ± 0.5
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cm) than in Roscoff (2.3 ± 0.2, t = – 4.30, P = 0.003) but difference in the calculated surface
area was not significant (P = 0.052). Each holdfast was packed in a thin Ziploc bag and
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pushed in a transparent water jar, allowing to create a vacuum and to measure its total
displacement volume. Holdfast interstitial volume (named 'ecospace' in Jones, 1971) was
determined by the difference between total and hapteron displacement volumes, measured in a
graduated tube once dissected throughout fauna sorting. Neither these volumes nor holdfast
biomass differed significantly between sites (P > 0.05, Appendix A).
Additional random collection conducted for isotopic analyses (see below) and scubadiving observations (≈ 5’) provided wider qualitative information on communities and trophic
structure in spring 2011. These observations were strengthened by a quantitative survey set up
for winter 2013. It should be noted that Molène area was patchily trawled the next day after
the spring 2011 sampling and may have influenced, by modifying the dissimilarity between
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sites, the results of this additional survey. Megafauna (width > 5 cm) densities were estimated
by three scuba-divers in Roscoff (late January) and in Molène (mid-February). Dominant
species (large molluscs, crustaceans, echinoderms) were counted on the evident rock
substratum and below 10 medium boulders (with a diameter of 50-100 cm) randomly turned
over along three parallel 25 × 2 m transects (spaced by 3 m).
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2.3. Sampling and preparation for stable isotope analyses
In late March 2011, at Roscoff and Molène sites, three replicates of seawater (5 L)
were collected with a Niskin bottle below the surface (− 1 m) to assess the suspended
particulate organic matter (POM). Sediment organic matter (SOM) was obtained by scraping
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the first cm of interstitial sediment into 200 mL containers (3 replicates). Small boulders (3
replicates with a volume of approximately 1 L) were collected to sample epilithic biofilms
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(rock organic matter, ROM). Additional kelp holdfasts (3 replicates) were also brought back
to the laboratory to extract the associated organic matter (holdfast organic matter, HOM).
SOM, ROM and HOM were considered as the components of the organic matter pool (called
OM pool hereafter). The most abundant macroalgae and consumer species were collected (1
mm mesh bags) from three stipe/lamina samples, three holdfasts and from the surrounding
substratum. Zooplankton tows (200 µm) were conducted for 10 minutes at approximately 1 m
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below the water surface for copepod isotope analyses.
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In the laboratory, seawater samples (POM) were filtered on pre-combusted Whatman
® GF/F filters (0.7 µm). Sediment samples were shaken in filtered seawater (0.20 µm) to
suspend the SOM. Sampled rock boulders were gently brushed using a smooth brush in
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filtered seawater (0.20 µm) to suspend ROM. HOM was brushed from within the holdfast
base using a similar smooth brush in filtered seawater (0.20 µm). Brushing was brief to
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minimise the release of extracellular polymeric substances (EPS) by the holdfast which could
bias the isotope signature of the HOM. Suspended SOM, ROM, and HOM were sieved
separately on a 63 µm mesh and filtered on 0.7 µm GF/F filters. Although stable isotope
analyses were focused on δ15N for trophic level estimations in the present paper, some
carbonate removal (identical procedures at both sites) was performed for δ13C measurements
which are presented elsewhere (Leclerc et al., 2013b). Each filter was then briefly acidified
(HCL, 1 N), thoroughly rinsed with distilled water, and dried at 60 °C for 48 h.
Macroalgae were sorted by species, washed, and stored in plastic bags at − 30 °C until
preparation and analysis. L. hyperborea samples were separated according to the different
thallus parts, namely old lamina (distal part), young lamina (formed during winter), stipe
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(close to the meristem) and EPS. EPS were extracted from stipe pieces cut longitudinally,
disposed above large glass containers and maintained for 1 h at ambient temperature. EPS
samples were directly dried at 60 °C (48 h) before grinding. Zooplankton samples were
placed in a test tube from which light was excluded except for the top tenth of the tube. A
cold light source was placed at the top and copepods attracted by the light were sorted from
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the living material using a pipette and kept in 0.20 µm filtered seawater for 3 h to allow gut
clearance. Macro-consumers were starved overnight in 0.20 µm filtered seawater to allow
evacuation of their digestive contents. Samples were then stored in glass containers at − 30 °C
until preparation and analysis.
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Macroalgae pieces were scraped with a scalpel, rinsed with freshwater to remove
epiphytes and then briefly acidified (HCL, 1 N). Whenever possible, isotope analyses of
consumers were conducted on muscle tissue to minimise isotope variability and to reflect
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integrative assimilation of sources by the consumers (e.g. Pinnegar and Polunin, 1999). Most
samples were prepared at the individual level. To obtain sufficient material for accurate stable
isotope analyses, a few samples containing several individuals of the same taxa were pooled
(Copepoda, Nematoda, Odontosyllis ctenostoma, Rissoa parva, Barleeia unifasciata, Janira
maculosa, and colonial taxa: Bryozoa and Ascidiacea). Each sample was then briefly acidified
(HCL, 1 N), rinsed with distilled water, and dried at 60 °C for 48 h. In order to cope with
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changes induced by longer acidifications, δ15N measurements were conducted on untreated
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samples for calcareous organisms (Corallina, Sycon, Crisa, Didemnum, Marthasterias,
Asterias and Amphipholis). Once dried, samples were crushed with a mortar and a pestle then
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put in tin capsules before mass-spectrometry analyses.
Nitrogen isotope ratios were determined using a Flash EA CN analyser coupled with a
Finnigan Delta Plus mass spectrometer, via a Finnigan Con-Flo III interface. Data are
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expressed in the standard δ unit.
δ15N = [(15N/14Nsample / 15N/14Nreference) – 1] × 103
These abundances were calculated in relation to the certified reference material atmospheric
dinitrogen (at-air). The at-air scale was obtained using in-house protein standards, calibrated
against IAEA N3 reference material. The standard deviation of repeated measurements of
δ15N values of a laboratory standard was 0.05 ‰ versus at-air.
2.4. Data analyses
Community structures were analysed for macroalgae and macrofauna separately,
according to habitat (stipe/lamina, holdfast and rock) and site (Roscoff, Molène), using
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PRIMER 6 (Plymouth Routine in Multivariate Ecological Research) software. Previously,
species AFDM were standardised by the total biomass per sample (i.e. biomass percentages).
Prior analyses, one outlier sample (rock quadrat from Molène), containing one megafauna
individual (Marthasterias glacialis, 82 % AFDM of the sample) have been excluded.
Similarities among samples were estimated using the Bray-Curtis Similarity Index (Clarke
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and Warwick, 2001). Samples were ordinated using a non-metric Multidimensional Scaling
(nMDS) and differences among sites and habitats (both fixed factors) were analysed using
permutational multivariate analyses of variance (PERMANOVA, Anderson et al., 2008),
allowing testing whether inter-group similarity is greater than within-group. Species biomass
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distributions between sites within each habitat were compared using pair-wise tests,
depending on significant interactions between the two factors. Within each habitat group,
PERMDISP routine revealed that the multivariate dispersion (around the centroid) of biomass
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distribution of seaweeds and fauna was homogeneous between sites (P > 0.15).
For each microhabitat, biomasses of large tropho-functional groups were compared
between sites. For that purpose, different biomass standardisations were conducted, according
to the microhabitat considered, except for rock samples (0.1 m-2). Biomass of seaweed or
consumer groups was standardised either by lamina, stipe or holdfast biomass. In order to
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characterize habitat features that may influence faunal distribution (Christie et al., 2007;
Norderhaug et al., 2014), red, brown and green macroalgae (considered as trophic groups)
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were separated according to their morphology: crustose, smooth leaf-like (poorly branched),
rough leaf-like (coarsely branched), bush-like (densely branched). Consumers were separated
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according to their major feeding mode: grazer, sessile suspension-feeder (including sessile
bivalves), mobile suspension-feeder, deposit-feeder, mobile fauna- and sessile faunapredators. When the homoscedasticity hypothesis was achieved (Fisher tests), the mean
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biomass of tropho-functional groups was compared between sites using one-tailed Student ttests. Otherwise, a Wilcoxon-Mann-Whitney U-test was applied. Megafauna densities in
transects (25 × 2 m, 3 replicates, winter 2013) were considered between Roscoff and Molène
using one-tailed Wilcoxon-Mann-Witney U-test. For biomass and density site-to-site
comparisons, tropho-functional groups of consumers and primary producers were all
considered as independent entities owing to the lack of a priori knowledge on their
interrelationships; therefore multiple site-to-site paired comparisons were chosen. Freeware R
statistical environment was used for all these statistical analyses (R Development Core Team,
2012).
Isotopic analyses helped to estimate consumer trophic levels (TLconsumer) as follows:
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TLconsumer = 2 + (δ15Nconsumer– δ15Nbaseline) / 2.5
where δ15Nbaseline corresponds to the mean δ15N of strict primary consumers (TL = 2.0). Only
the species sampled at both sites were used as baseline in order to strengthen TL site-to-site
comparisons, regardless of the trophic enrichment factor (TEF) choice. The latter was chosen
according to Caut et al. (2009) who reported a mean δ15N-TEF value of 2.5 ‰ for invertebrate
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whole body. With regard to the large variability of TEF within this group (Caut et al., 2009),
the corresponding uncertainty in TL estimation was 0.9 (S.D.). Since δ15N fractionation
depends, among other factors, on the protein content of the mixed food source (Perga and
Grey, 2010), considering this variability in estimations is essential when considering strong
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omnivory occurring in food webs. It should be noted that the TL was estimated from species
mean δ15N; hence the intraspecific variability of TL was not taken into account in results.
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3. Results
3.1. Community structure
Among the 65 macroalgal taxa identified across sites (Table 1, Appendix B), 9 were
found on lamina, 34 on stipe, 43 on holdfast, 53 on the surrounding substratum. These taxa
were differently distributed among microhabitats, within each site (Fig. 2A, Table 2A). The
canopy (lamina and stipe) epiphytic relative composition did not differ between Roscoff and
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Molène (pair-wise tests), and was characterised on its own. On lamina, the seaweed species
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richness (Table 1) and tropho-functional group biomass (Fig. 3A) were similar between sites.
Brown algae (on average 20 mgAFDM gAFDMLamina−1) were largely dominated by the
filamentous Ectocarpus sp. while red algae (≈ 10 mgAFDM gAFDMLamina−1) were dominated
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by the rough leaf like Cryptopleura ramosa. On stipe, biomass of epiphytic seaweeds was
dominated (Fig. 3B) by smooth leaf-like (Palmaria palmata and Rhodymenia pseudopalmata)
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and rough leaf-like red algae (Phycodrys rubens, Cryptopleura ramosa). Although the
biomasses of these two dominant groups and biomass distribution of the overall species were
similar between sites, Roscoff stipes were represented by twofold higher species richness
(Table 1) and higher biomass for crustose and bush-like red algae. On holdfast, the species
richness did not differ (Table 1), whereas species relative abundances differed significantly
between sites (Pair-wise test, Table 2A), as observed at the tropho-functional group level (Fig.
3C). Highly variable on holdfasts, red algae biomass did not differ significantly between sites,
except for the crustose corresponding to Corallinale/Peyssoniella sp., absent in Molène and
abundant in Roscoff). On the surrounding substratum (Table 1), obvious differences were
highlighted between sites (Fig. 2A, Table 2A). In Molène, the biomass associated with the
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rock substratum was dominated by smooth leaf-like brown algae (Fig. 3D), i.e. Saccorhiza
polyschides and Laminaria hyperborea recruits. In Roscoff, red algae, distributed among
diverse functional groups, dominated the biomass. Compared to Molène, greater biomasses
were found for smooth leaf-like (e.g. Dilsea carnosa and Callophyllis laciniata), rough leaflike (e.g. Delesseria sanguinea, Phyllophora crispa), and bushy red algae (e.g. Corallina
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elongata and Heterosiphonia plumosa).
Among the 279 macrofauna taxa identified on total across sites and habitats (Appendix
C), 145 were found on stipe, 191 on and within holdfast and 204 on the rock. Irrespective of
the strata analysed, the species richness of sessile fauna (Bivalvia included) was comparable
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between Roscoff and Molène (Table 1). Mobile fauna richness was comparable on kelp
individuals between site, with numerical abundance of 151 to 407 individuals in Molène, and
92 to 360 in Roscoff. On the rocky substratum, mobile fauna species richness was
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significantly greater in Roscoff (Table 1) and represented by 145-398 ind. 0.1 m-2 against 4097 ind. 0.1 m-2 in Molène. Each microhabitat was characterised by its own macrofauna
species biomass distribution and differed between sites. (Fig. 2B, Table 2B). These species
were largely dominated by sessile suspension-feeders which represented on average 53 to 99
% of the consumer biomass according to microhabitat and site (Fig. 4). On stipe + lamina
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(Fig. 4A), the biomass of sessile suspension-feeders in Molène (44 mgAFDM gAFDMStipe−1)
was double that in Roscoff (16), mainly due to species growing on the stipe itself. In Molène,
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this group was dominated by the ascidian Distomus variolosus (62 %), and the bryozoan
Celleporina calciformis (12.8) whereas Roscoff stipes were mostly encrusted by the sponge
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Ophlitaspongia papilla and the bryozoan Phaeostachys spinifera. Higher grazer biomass was
observed in Roscoff (4 mgAFDM gAFDMStipe−1), mostly due to the gastropod Gibbula
cineraria (67 %). Within holdfast, the macrofauna biomass (Fig. 4B) was higher in Roscoff,
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particularly for sessile suspension-feeders and deposit-feeders (e.g. Rissoa parva, Eupolymnia
nesidensis). In Roscoff, sessile suspension-feeders were dominated by sponges (Amphilectus
fucorum, Myxilla incrustans, Ophlitaspongia papilla, Halisarca dujardini) and didemnid
ascidian (Didemnum maculosum). In Molène, this group was dominated by polyclinid
ascidians (Aplidium glabrum and Morchelium argus) and the bryozoan Celleporina
calciformis. Between sites, the rocky substratum largely contrasted in biomass distribution of
either macrofauna species or trophic group (Table 2B, Fig. 4C). The Roscoff rocky
substratum yielded substantial biomass of consumers compared to Molène, except for grazers
and mobile fauna-predators (Fig. 4C). The biomass of sessile suspension-feeder was eightfold higher in Roscoff (0.7 gAFDM 0.1m−2) than in Molène, dominated by sponges as
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Phorbas plumosum, Amphilectus fucorum, Dysidea fragilis, Myxilla incrustans, Halichondria
sp., the ascidians Polyclinum aurantium and the bryozoan Microporella ciliata. The biomass
of mobile suspension-feeders was six-fold higher in Roscoff (0.01 gAFDM 0.1 m−2), and was
dominated by the echinoderm Antedon bifida, and the sabellid Branchomma bombyx. Depositfeeder biomass was three-fold higher (0.1 mgAFDM 0.1 m−2) in Roscoff, mostly represented
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by terebellids such as Pista elongata or Eupolymnia nesidensis, echinoderms as Amphipholis
squamata, and many gastropods such as Bittium reticulatum, Barleeia unifasciata, Rissoa
parva. The biomass of sessile fauna-predators was treble in Roscoff (0.1 mgAFDM 0.1 m−2)
than in Molène, and was dominated by the echinoderm Asterina gibbosa and several
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gastropods (e.g. Trivia arctica) and annelids (e.g. Haplosyllis spongicola).
Megafauna species were differently distributed between sites (Fig. 5). In Roscoff, the
rocky substratum and sub-boulders were dominated by grazing gastropods and predatory
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decapods, whereas in Molène, these habitats were dominated by echinoderms (mostly
predators). The abalone Haliotis tuberculata was found in ten-fold greater density in Roscoff
compared to Molène. Among crustaceans, the edible and swimming crabs Cancer pagurus
and Necora puber were significantly more abundant in Roscoff, where large echinoderms
were almost absent except for Henricia sanguinolenta. Important sea cucumber densities
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(Cucumaria frondosa and Holothuria forskali) were observed in Molène, significantly higher
compared to Roscoff for Holothuria forskali. Predatory echinoderms displayed important
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densities in Molène, especially for Echinus esculentus (6.7 ± 3.2 ind. 50 m−2) and
Marthasterias glacialis (18.3 ± 8.4).
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3.2. δ15N of the main sources and consumers
Sources showed important δ15N variations in both sites (Fig. 6). Brown algae δ15N
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values ranged from 2.1 to 6.1 ‰ in Roscoff and from 1.2 to 8.1 ‰ in Molène, for Laminaria
hyperborea young lamina and EPS respectively (Table 3). Red algae δ15N ranged from 3.4
(Phycodrys rubens) to 5.8 ‰ (Rhodymenia pseudopalmata) in Roscoff and from 4.2
(Callophyllis laciniata) to 6.4 ‰ (Delesseria sanguinea) in Molène. The OM pool (POM,
SOM, HOM, ROM) δ15N ranged from 4.6 (POM) to 8.9 ‰ (HOM) in Roscoff and from 5.3
(HOM) to 6.7 ‰ (ROM) in Molène.
As for primary sources, primary consumers displayed large intra-group variability in
δ15N (Fig. 6, Table 3). This variability in the baseline (strict primary consumers) induced
uncertainty in the trophic level estimation of consumers. Considering fifteen species, the
δ15N-baseline was 6.9 ± 1.3 (SD) in Roscoff and 6.7 ± 1.2 in Molène. For grazer group, the
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δ15N values ranged from 6.4 (Gammaropsis maculata) to 9.7 ‰ (Gibbula cineraria) in
Roscoff and from 6.5 (Patella pellucida) to 9.0 ‰ (Gibbula cineraria) in Molène. Among
suspension-feeders, the δ15N ranged from 4.7 (Musculus subpictus) to 8.2 ‰ (Ophlitaspongia
papilla) in Roscoff and from 4.7 (Alcyonidium gelatinosum) to 7.6 ‰ (Ophlitaspongia
papilla) in Molène. Among mobile suspension-feeder species, δ15N ranged from 5.9 (Jassa
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falcata) to 8.2 ‰ (Branchiomma bombyx) in Roscoff and from 6.4 (Branchiomma bombyx) to
7.6 ‰ (Jassa falcata) in Molène. The δ15N of deposit-feeders (including omnivores) ranged
from 6.8 (Rissoa parva) to 8.8 ‰ (Maera inaequipes, TL = 2.8) in Roscoff and from 4.7
(Apseudes talpa) to 9.1 ‰ (Leucothoe spinicarpa, TL = 3.0). Sessile fauna-predator δ15N
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ranged from 8.8 (Ocinebrina aciculata, TL = 2.8) to 11.8 ‰ (Calliostoma zizyphinum, TL =
4.0) in Roscoff and from 8.3 (Odontosyllis ctenostoma, TL = 2.6) to 11.7 ‰ (Echinus
esculentus, TL = 4.0) in Molène. Mobile fauna-predator δ15N ranged from 11.1 (Gnathia
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dentata, TL = 3.7) to 14.4 ‰ (Homarus gammarus, TL = 5.0) in Roscoff and from 10.9
(Harmothoe impar, TL = 2.6) to 11.9 ‰ (Eualus occultus, TL = 4.1) in Molène.
4. Discussion
4.1. Patterns of community, trophic structure and functioning
Overall, observed patterns in diversity and species distribution were dependent on the
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taxonomic/functional group (e.g. seaweed, macrofauna, megafauna), as well as on the stratum
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considered (lamina, stipe, holdfast of canopy plants and rock). Molène and Roscoff Laminaria
hyperborea canopy plants (lamina, stipe) hosted similar macroalgal biomass distribution,
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represented by 37 species in total. In both sites, algal epiphytes were dominated by
filamentous Ectocarpus sp. on lamina, smooth leaf-like Palmaria palmata on uppermost part
of stipe, rough leaf-like Phycodrys rubens on the middle part, and smooth leaf-like
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Rhodymenia pseudopalmata, on the lower level of stipe and on holdfast. Across European
kelp forests, Palmaria palmata occurs in shallow waters, its lower distribution being limited
by light (Norton, 1968; Norton et al., 1977; Whittick, 1983; Castric-Fey, 1996), therefore its
abundance as an epiphyte on the same part of stipe in both sites suggests that the irradiance
reaching the canopy layer is somewhat comparable in spite of difference in depth (Whittick,
1983). Compared to their well-studied Norwegian counterparts, Brittany Laminaria
hyperborea stipes were almost devoid of boreal bushy algae species such as Rhodomela
confervoides and Ptilota gunneri (Christie et al., 2007). In lieu of [check if text missing] (see
discussion in Whittick, 1983), in Brittany, the split leaf-like Cryptopleura ramosa was found
either on the mid-level of stipe, on lamina or on holdfast. Despite similar macroalgae taxa and
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morphologic group biomass distribution between sites, the macrofauna associated with the
canopy significantly differed (see also Appendix C) but was mostly due to differences in
sessile taxa growing on stipe itself. The absence of Phaeostachys spinifera on Molène stipes
can be attributed to its southern limit of distribution in Roscoff, and may explain the
development of competitive species such as Distomus variolosus and Celleporina calciformis.
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The lower abundance of mobile fauna among abundant macroalgal epiphytes in Molène is
more difficult to explain since most species are currently reported in European kelp forests
(Jones, 1973; Norton et al., 1977; Schultze et al., 1990; Christie et al., 2003; 2014) and may
result from patterns observed on the overall forest. While an important dissimilarity in species
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composition was found among strata, a substantial connectivity exists horizontally among
kelp plants and vertically among strata for several mobile taxa (Norderhaug et al., 2002;
Waage-Nielsen et al., 2003). The abundance of mobile fauna in kelp epiphytes may therefore
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interfere with habitat complexity on the understorey and kelp size-density structure (density
of adults hosting abundant epiphytes), factors interacting with wave force dissipation
(Eckman et al., 1989; Norderhaug et al., 2014). In Norway, Norderhaug et al. (2014) showed
higher richness and abundance of mobile fauna associated to kelp epiphytes in intermediate
wave-exposed sites. Although contrasting with our findings, this study was performed among
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sites displaying equivalent kelp densities in the canopy layer, therefore limiting any
generalisation to heterogeneous kelp forests.
TE
At the holdfast level, taxonomic and trophic structures differed between sites. Biomass
of deposit- and suspension-feeders was higher in Roscoff, and could result from higher
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particulate organic matter retention (Jones, 1971; Edwards, 1980) in this more sheltered site.
Disregarding local hydrodynamics, such retention can be due to contrasting canopy structures
(size-density, Eckman et al., 1989) and structural complexity near the bottom. Despite similar
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interstitial volumes between sites, holdfast from Roscoff hosted important biomass of
structurally
diverse
red
algae.
For
instance,
important
encrusting
by
the
Corallinale/Peyssonelia sp. complex forms a hard substratum and enhances habitat size for
sessile fauna as sponges (e.g. Amphilectus fucorum, Myxilla incrustans) and ascidians (e.g.
Didemnum maculosum), and for other red algae species (dominated by smooth and split leaflike species). The seaweed structural complexity (Gee and Warwick, 1994), in addition to the
active selective suspension-feeding of ascidians and sponges (Levinton, 1972; Bell, 2008)
may favour holdfast organic matter retention (Moore, 1972; Dixon and Moore, 1997), hence
amplifying site-to-site differences. Biomass of mobile fauna such as the dominant deposit
feeders, Rissoa parva and Eupolymnia nesidensis, considered as ‘Turbidity indifferent
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species’ by Moore (1973) can benefit from habitat size/complexity and resource availability.
Site-to-site differences in holdfast organic matter retention can also be suggested from isotope
composition of HOM, more
15
N-enriched in Roscoff than the other sources of the OM pool,
suggesting a higher bacterial activity (Thornton and McManus, 1994).
On the rocky substratum, taxonomic and functional composition contrasted between
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the two sites. The biomass of functionally diverse epilithic red algae was higher in Roscoff
compared to Molène. Among the dominant red algae inhabiting Roscoff understorey, the
bushy Corallina elongata and the smooth leaf-like Dilsea carnosa are generally restricted to
shallow waters (Norton, 1968; Norton et al., 1977) and was not expected to be abundant in
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Molène. Conversely, the deep species (Norton, 1968) Phyllophora crispa and Calliblepharis
ciliata represented 37 % of red algae biomass in Roscoff but were nearly absent in Molène.
While epiphytic algal composition may be similar on canopy kelp in areas of contrasting
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histories (Christie et al., 1998), patterns in epilithic structure remain overlooked. Particularly
abundant in Roscoff samples, the perennial species Phyllophora crispa has a rigid and rough
leaf-like habit, favourable to host diverse red algae, sessile (sponges, bryozoans, ascidians)
and mobile fauna, as already reported (Kostylev et al., 2010). Phyllophora crispa and
associated epiphytes form a habitat quite comparable to adult kelp holdfasts in terms of
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complexity and OM retention (unpubl. obs.). Between sites, the rock habitat was thus
profoundly different between sites in term of algal composition and resulting feature. Nearby
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the bare bottom in Molène, the large variability of brown algae biomass observed on holdfast
and rock (Fig. 3C, D) suggests patchy and opportunistic winter settlement of the annual kelp
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s.l. Saccorhiza polyschides (Norton, 1978; Engelen et al., 2011) and Laminaria hyperborea
recruits (Sjøtun et al., 2006).
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4.2. Hypotheses about processes involved in observed patterns
While the present sampling framework does not allow a complete interpretation of the
observed patterns, a series of probable and testable hypotheses can be formulated as thoughts
for future research. Differences in habitat structure on the bottom (holdfast and surrounding
substratum) between Molène and Roscoff may result from confounding physical and biotic
effects. Kennelly (1989) found that subcanopy scouring by the small kelp Ecklonia radiata
(C.Agardh) J.Agardh decreases as the stipe length increases. While Laminaria hyperborea
adults have an erect and rigid stipe which reduces contacts between the blades and the bottom,
young short-stiped forms are more flexible and could have a wider sweeping area and a more
intensive scouring, as reported for kelp of comparable habit, e.g. L. pallida Greville
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(Velimirov and Griffiths, 1979) and Pterygophora californica (Reed and Foster, 1984).
Consequently, kelp abrasion of understorey turfs (Irving and Connell, 2006) and sessile fauna
(Connell, 2003) may be greater within a kelp forest dominated by young plants. Whether such
effect occurs during the kelp growth, especially during the recovery of kelp-harvested areas,
may be of interest for future research. As explained above, the epiphytic composition
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suggested that incident light was comparable on upper stratum. However, contrasting kelp
size-density structure and turbidity may affect the light reaching the bottom. While adults
dominated the Roscoff kelp forest (November 2010), kelp size classes were more evenly
distributed in Molène (March 2011). While the negative shading effect of high kelp density on
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understorey algae is a well-known phenomenon (e.g. Norton et al., 1977; Reed and Foster,
1984; Wernberg et al., 2005), the effect of evenness in multi-layered kelp forests on these
parameters remains, to our knowledge, unexplored. Since kelp are known to interfere with
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turbulence (e.g. Eckman et al., 1989), it would be worth exploring whether this turbulence
vary with evenness in size and flexibility and, in turn with light resource partitioning
(Middelboe et al., 2006). Nonetheless, the lower abundance of both sciaphilic and photophilic
red algae, combined importance of S. polyschides in Molène on the rock indicates that
additional factors are involved in these patterns. The lower red algae and sessile fauna cover
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on Molène subcanopy may also partially result from a cascading effect, which includes
indirect and direct interactions involving large echinoderms. Although megafauna densities
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were measured two years after macrofauna sampling, these estimations reflected the survey
observations and isotopic random collections, highlighting the rarity of large echinoderms at
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Roscoff and their commonness at Molène site. Often reported as a kelp grazer (Jones and
Kain, 1967; Fredriksen, 2003), the edible sea urchin Echinus esculentus has also been
described as a browsing opportunistic predator (Allen, 1899; Forster, 1959; Comely and
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Ansell, 1988). Within the Molène benthic community, E. esculentus exhibited one of the
highest δ15N (measured on Aristotle lantern), corresponding to a mean trophic level of 4.0 (±
0.9 considering the variability in TEF for invertebrate whole body, Caut et al., 2009). This
estimation is consistent with our observations of digestive contents conducted on individuals
that have been sampled for stable isotope analyses. Guts contained some seaweed fragments
but were dominated by sessile fauna (bivalves, cirripeds, sponges, bryozoans, and ascidians)
and associated poorly mobile organisms (e.g. nematodes, TL = 3.9), of higher fitness interest
compared to macroalgal based diet (e.g. Hughes et al., 2005; Vanderklift et al., 2006). Given
the sea urchin densities in Molène, this omnivorous species may be partly responsible of the
lower biomass of sessile fauna and seaweed. When E. esculentus has been described as an
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important kelp recruit grazer, its density exceeded 3-4 ind. m−2 (in summer, Jones and Kain,
1967; Sjøtun et al., 2006), substantially higher compared to Molène (0.1-0.2 ind. m−2 in
winter). Hence, any density-dependant feeding behaviour of E. esculentus according to food
availability should be of interest for future research. In the present study, a greater effect can
be expected from the spiny sea-star Marthasterias glacialis (TL = 3.8) which shows greater
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density (0.3-0.6 ind. m−2 in winter). This voracious species feeds opportunistically either on
macroalgae, sessile or mobile macrofauna, and can be considered as a key predator in
communities of coastal rocky shores (Frid, 1992; Verling et al., 2003; Bonaviri et al., 2009;
Tuya and Duarte, 2012). Furthermore, M. glacialis is one of the main predators of the abalone
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Haliotis tuberculata (Forster, 1962), poorly represented in Molène. While the spiny sea-star
can influence the ormer distribution, other controls should be tested. Haliotis spp. require
diverse seaweeds in their diet, including fresh red algae of the understorey (Guest et al., 2008;
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Leclerc et al., 2013a).
In European kelp forests, the dominant starfish predators are the edible and the
swimming crabs: Cancer pagurus and Necora puber (Ramsay et al., 2000). In Roscoff, these
species and the lobster Hommarus gammarus were the highest benthic predators according to
their estimated trophic levels (4.2-5.0). Both Cancer spp. and Necora spp., more abundant in
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Roscoff, can forage significantly on large echinoderms and play a key role in their regulation
(Freire and Gonzalez-Gurriaran, 1995; Ramsay et al., 2000; Steneck et al., 2004; Fagerli et al.,
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2014). However, given the absence of E. esculentus and M. glacialis in Roscoff, any
contribution to the decapod diets cannot be inferred. Since these predators are not echinoderm
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specialists, it seems improbable that their densities are sufficient to control, even collapse,
large echinoderm populations at Roscoff site (Miller, 1985; Sivertsen, 2006), but information
about echinoderm recruitments and predation-rate on young stages (Fagerli et al., 2014) is
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lacking in the area. Multi-scale spatio-temporal variability of large echinoderms population
can be altered, at different life history stages, by several crossed factors including the nature
of the substratum (Laur et al., 1986; Hamel and Mercier, 1996; Balch and Scheibling, 2000),
the depth (Reid, 1935; Jones and Kain, 1967; Comely and Ansell, 1988; Verling et al., 2003),
the food availability (Laur et al., 1986; Tuya and Duarte, 2012), the predation pressure
(Steneck et al., 2004; Estes et al., 2011), the temperature and epizootics (Scheibling and
Stephenson, 1984). In the English Channel, the stochastic repartition of large echinoderm taxa
has intrigued several authors for decades (Allen, 1899; de Beauchamp, 1914; Holme, 1966;
Ellis and Rogers, 2000). For example, Marthasterias glacialis from shallow waters seems to
16
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decrease in abundance from the West to the East, but to our knowledge, this issue remains
unexplored.
4.3. Ecological and management implications
Omnivorous species can be of critical importance for stability and emergent ecosystem
properties which strongly depend on the interaction strength (Emmerson and Yearsley, 2004;
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Bascompte et al., 2005). In the present study, adult E. esculentus and M. glacialis sampled in
Molène were estimated to operate from the fourth trophic level, feeding upon a range of three
trophic levels. While the diversity of interaction strengths linking these opportunist species to
the associated community remains unclear, our results highlighted direct interactions that
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were concentrated upon the overall sessile suspension-feeder group. Owing to their large
body-size and their energetic requirement (O'Gorman and Emmerson, 2010), these species
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may thus be considered as collectively strong interactors (sensu Berlow, 1999). Their
collective effect may be of critical importance for the associated trophic structure and
functioning, through community cascading effects, by reducing the morphological diversity
toward the bottom, seemingly affecting habitat structure and organic matter retention. In
addition to affecting habitat complexity, sessile suspension-feeders composition and
abundance can have dramatic influence on ecosystem properties (Gili and Coma, 1998). In
D
kelp forests, many suspension- and deposit-feeders (e.g. Ophiothrix fragilis and Maera
TE
inaequipes for ubiquitous examples) are able to select kelp-derived particles (including
propagules) among the organic matter pool (e.g. Beviss-Challinor and Field, 1982), and one
can wonder whether this function affect kelp recruitments and survival (Dayton, 1985). While
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experimental manipulations involving direct grazer provide substantial insights on cascading
effects, manipulating particle-consumers faces to the difficulty of quantifying particulate basal
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resource in marine reproduction (O'Gorman and Emmerson, 2010) and limit understanding of
their interactions with other species. In the present study, we found more abundant kelp
recruits and reduced biomass of suspension-feeder and red algae simultaneously. If
omnivorous predators are involved in the observed patterns, these results provides new
insights about the sustainability of kelp primary production in Brittany, often attributed to the
local rarity of direct kelp consumers (Arzel, 1998; Leblanc et al., 2011). However, Echinus
esculentus and Marthasterias glacialis behave opportunistically, so comprehensive analyses
of seasonal and density-dependant variations of their diet are required to state on this indirect
interaction. Apart from contrasting structure and functioning nearby the bottom, our results
highlighted that kelp canopy individuals are major refuges for the development of diverse and
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abundant sessile organisms, in spite of contrasting size structure and kelp forest histories.
Alternatively, these results are strong arguments in favour of further comprehensive analyses
of the overall kelp forest strata, including the water column (e.g. Lorentsen et al., 2010) for
conservative management and understanding of resilience in structure and functioning in kelp
forests.
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Acknowledgements
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We would like to thank F Gentil and C Broudin for help with animal identification.
We are grateful to the marine operations staff at the Roscoff Biological Station “Service Mer
& Observation SBR”, especially Y Fontana, W Thomas, M Camusat & N Guidal for the
sampling set-up. This work benefited from the support of the “Parc Naturel Marin d’Iroise”,
the Brittany Regional Council and the French Government through the National Research
Agency with regards to an investment expenditure programme IDEALG which reference is
stated as ANR-10-BTBR-04.
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Fig. 1 Location of the two study sites in the Molène archipelago and Roscoff, Brittany
(France). Intertidal areas are in clear grey.
Fig. 2 Non-metric Multidimensional Scaling conducted from the Bray Curtis similarities
among relative ash free dry mass (standardized by sample total) of macroalgae (A) and
macrofauna (B) species in Roscoff (full symbols) and in Molène (empty symbols).
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Fig. 3 Macroalgae biomass (AFDM ± SD) according to microhabitats (A: lamina, B: stipe, C:
holdfast, D: rock) and sites (Roscoff: full bars, Molène: empty bars) in early spring 2011.
Significance of mean difference is indicated: *** (P < 0.001), ** (P < 0.01), * (P < 0.05), NS
(P > 0.05), as determined Student or Mann-Whitney tests, according to the homoscedasticity
of the data. GA: green algae, BA: brown algae, RA: red algae, Cr: crustose, SmL : smooth
leaf-like, RoL: Rough leaf-like, Bu: bush-like.
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Fig. 4 Trophic group biomass (AFDM ± SD) according to microhabitats (A: stipe + lamina,
B: holdfast, C: rock) and sites (Roscoff: full bars, Molène: empty bars) in early spring 2011.
Significance of mean difference is indicated: *** (P < 0.001), ** (P < 0.01), * (P < 0.05), NS
(P > 0.05), as determined Student or Mann-Whitney tests, according to the homoscedasticity
of the data. G: grazers, SSF: sessile suspension-feeders, MSF: mobile suspension-feeders, DF:
deposit-feeders, sf-P: sessile fauna-predators, mf-P: mobile fauna-predators.
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Fig. 5 Megafauna densities (± SD) per transects (50 m²) measured on the rocky substratum
and above 10 boulders in winter 2013 at Roscoff (full bars) and at Molène (empty bars) sites.
Significance of mean difference is indicated: *** (P < 0.001), ** (P < 0.01), * (P < 0.05), NS
(P > 0.05), as determined Student or Mann-Whitney tests, according to the homoscedasticity
of the data. Trophic groups (G: grazers, MSF: mobile suspension-feeders, DF: depositfeeders, sf-P: sessile fauna-predators, mf-P: mobile fauna-predators) and Phyla (Moll:
Mollusca, Crus: Crustacea, Echi: Echinodermata) are indicated above. Hal: Haliotis
tuberculata, Hen: Henrica sanguinolenta, Cuc: Cucumaria frondosa, Hol: Holothuria
forskali, Mar: Marthasterias glacialis, Ech: Echinus esculentus, Ast: Asterias rubens, Lui:
Luidia ciliaris, Can: Cancer pagurus, Maj: Maja squinado, Nec: Necora puber, Lop:
Lophozozymus incisus, Gal: Galathea spp.
AC
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Fig. 6 Individual δ15N (‰) values of the main sources of organic matter and consumers
according to their dominant trophic group (brown algae (BA), red algae (RA), deposited POM
(DPOM), suspended POM (SPOM), grazers (G), sessile suspension-feeders (SSF), mobile
suspension-feeders (MSF), deposit-feeders (DF), sessile fauna-predators (sf-P), mobile faunapredator (mf-P) within Roscoff (full dots) and Molène (empty dots) Laminaria hyperborea
forests in early spring 2011.
24
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Table 1 Species richness (Mean ± S.D. [total]) of macroalgae, mobile fauna and sessile fauna,
according to habitat and site. Mean richness were considered between seasons by two-tailed
Student t-test depending on homoscedasticity of the data. Otherwise a Mann-Whitney U-test
(marked M.W.) was applied. Significant P-values are in bold.
RI
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Table 2 Results of PERMANOVA and pair-wise tests conducted from the Bray Curtis
similarities of macroalgal (A, 65 species) and macrofauna (B, 279 species) species ash free
dry mass (standardized by sample total). Site (Roscoff, Molène), Habitat (Lamina, Stipe,
Holdfast, Rock), and their interaction were tested. Significant P (perm) are in bold.
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Table 3 δ15N (‰, ± SD) of the main primary sources and consumers of the Laminaria
hyperborea forests in Roscoff and in Molène, according to their microhabitat (Hab) : stipe
(S), holdfast (H), rock (R). Trophic groups (TG) are indicated for consumers: grazers (G),
sessile suspension-feeders (SSF), mobile suspension-feeders (MSF), deposit-feeders (DF),
sessile fauna-predators (sf-P), mobile fauna-predator (mf-P). Consumer trophic levels (TL ±
0.9 SDTEF) were estimated according to the mean species δ15N, or set at the lowest threshold
2.0.
Electronic Supplementary Materials
Appendix A Morphometric parameters measured on kelp canopy individuals collected in
Roscoff and in Molène. Parameters are compared between sites by Student t-tests according
to the achievement of homoscedasticity hypothesis.
TE
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Appendix B Macroalgal species found at Roscoff and Molène sites during the survey
(samples and observations). Relative occurrence is indicated: x: 1-10 % in samples, xx: 20-40
%, xxx 40-100% according to diversity sampling; °: species found in 1transect, °°: in 2
transects, °°°: in 3 transects during the megafauna survey.
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Appendix C Animal species found at Roscoff and Molène sites during the survey (samples
and observations). Relative occurrence is indicated: x: 1-10 % in samples, xx: 20-40 %, xxx
40-100% for diversity samples; °: species found in 1transect, °°: in 2 transects, °°°: in 3
transects during the megafauna survey.
25
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ROSCOFF
Two-tailed
comparison (P -value)
MOLENE
Richness
4.6
17.0
14.4
25.8
±
±
±
±
1.5 [9]
3.6 [31]
3.4 [33]
2.5 [42]
3
8.8
11.6
20.8
±
±
±
±
0.8 [6]
2.2 [14]
3.6 [26]
7.7 [37]
SESSILE FAUNA (Total = 99)
Stipe
Holdfast
Rock
25.8
22.2
28.8
±
±
±
4.4 [41]
5.4 [54]
5.4 [57]
22.2
31.2
26
±
±
±
5.4 [39]
8.6 [52]
5 [55]
0.841M.W.
0.389
MOBILE FAUNA (Total = 180)
Stipe
Holdfast
Rock
26.8
31.8
40.0
±
±
±
3.9 [55]
12.2 [77]
7.8 [94]
28.6
42
25.5
±
±
±
9.4 [65]
11.8 [93]
4.4 [72]
0.701
0.215
0.007
MOBILE FAUNA (Total = 4531)
Kelp individual 184.2
Stipe 81.2
Holdfast 103.0
Rock 243.2
±
±
±
±
0.281
TE
D
M
AN
US
CR
0.104
0.004
0.253
0.050
244.6
82.4
162.2
76.0
AC
C
109.3
32.5
80.8
58.6
EP
Density
±
±
±
±
102.9
32.2
77.1
27.3
IP
T
MACROALGAE (Total = 65)
Lamina
Stipe
Holdfast
Rock
0.394
0.955
0.050
<0.001
ACCEPTED MANUSCRIPT
AC
C
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SC
M
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B. Macrofauna Structure
Source d.f. Pseudo-F P (perm)
Site
9.1935
1
<0.001
Habitat
10.219
2
<0.001
Site × Habitat
3.673
2
<0.001
Residual
23
Total
28
Pairwise tests between Sites
within levels of Factor "Habitat"
P (perm)
Levels
t
0.008
Stipe
2.6752
0.007
Holdfast
2.1784
0.01
Rock
2.1859
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PT
A. Macroalgae Structure
Source d.f. Pseudo-F P (perm)
Site
2.0577
1
0.028
Habitat
10.68
3
<0.001
Site × Habitat
1.835
3
0.004
Residual
32
Total
39
Pairwise tests between Sites
within levels of Factor "Habitat"
P (perm)
Levels
t
0.751
Lamina
0.4479
0.199
Stipe
1.3542
0.049
Holdfast
1.2778
0.016
Rock
1.6934
ACCEPTED MANUSCRIPT
TG
Roscoff
δ15N ± SD
TL
n
R
R
R
R
R
S
S
R
S
5.4
3.8
5.3
5.3
±
±
±
±
0.4
0.6
0.3
0.3
3
3
3
3
3.9
3.4
5.2
5.8
±
±
±
±
0.8
0.4
0.9
0.4
5
5
3
3
R
S
R
S
S
3
3.1
±
±
2.2
4.7 ±
6.1 ±
1.5
0.1
3
3
1
3
3
Hab.
Molène
δ15N ± SD
TL n
Sources
S
D
H
W
R
R
AC
C
± 0.1
3
6.4
± 0.3
3
6.1
4.6
4.4
± 0.3
± 0.2
± 0.3
5
5
5.7
± 0.5
3
3.6
3.2
5.4
8.1
±
±
±
±
0.4
0.1
0.3
0.1
3
3
5
3
SC
RI
PT
4.2
4.9
± 0.7
3
3.6
± 0.4
6
2.1
2.7
± 0.6
± 0.7
5
3
1.2
2.8
± 0.1
± 0.2
5
3
4.3
± 0.1
3
8.9
4.6
7.8
6.5
±
±
±
±
3
3
3
3
5.3
5.5
6.7
6.1
±
±
±
±
3
3
3
3
5.5
± 0.3
2
3
8.2
7.6
± 0.2
± 0.3
2.5
2.3
3
3
6.7
6.7
7.5
± 0.2
± 0.2
± 0.2
2
2
2.3
3
3
5
5.4
± 0.2
2
3
3.9
1
0.1
0.6
0.2
0.1
SSF
SSF
SSF
SSF
SSF
H
R
S
S
S
sf-P
S
11.2
3.7
1
P
H
13.2
4.5
1
MSF
DF
DF
DF
DF
mf-P
sf-P
sf-P
G
sf-P
H
S+H
H
R
R
H
H
H
S+H
S
2.5
2.7
2.6
2.2
2.1
4.4
3
10
5
3
1
1
2.8
3.2
10
1
EP
Porifera
Amphilectus fucorum
Halichondria panicea
Ophlitaspongia papilla
Phorbas plumosum
Sycon ciliatum
S
R
TE
Consumers
S
0.4
0.5
M
AN
U
Rhodophyceae
Callophyllis laciniata
Corallina elongata
Delesseria sanguinea
Dilsea carnosa
Heterosiphonia plumosa
Palmaria palmata
Phycodrys rubens
Plocamium cartilagineum
Rhodymenia pseudopalmata
Phaeophyceae
Cystoseira sp.
Ectocarpus sp.
Laminaria hyperborea Juvenile
Laminaria hyeperborea Stipe
Laminaria hyperborea EPS
Laminaria hyperborea Old
Lamina
Laminaria hyperborea Young Lamina
Saccorhiza polyschides
Ulvophyceae
Ulva rigida
OM pool
HOM
POM
ROM
SOM
0.1
0.3
0.6
0.1
Nematoda
Nematoda spp.
11.4
Nemertea
Lineus longissimus
Annelida
Branchiomma bombyx
Eupolymnia nesidensis
Nicolea venustula
Nicolea zostericola
Pista elongata
Harmothoe impar
Leonnates glauca
Odontosyllis ctenostoma
Platynereis dumerilii
Syllis columbretensis
8.2
8.7
8.3
7.3
9
±
±
±
±
7.2
12.8
0.6
1.3
0.1
0.4
± 0.6
9.9
6.4
± 0.4
2
3
8.4
± 0.2
2.7
3
10.9
9.7
8.3
± 0.3
± 0.2
± 0.3
3.7
3.2
2.6
5
3
5
ACCEPTED MANUSCRIPT
Syllis variegata
Trypanosyllis zebra
sf-P
sf-P
H
S
MSF
mf-P
DF
DF
G
G
P
MSF
DF
DF
mf-P
mf-P
DF
mf-P
MSF
MSF
W
S
H
H
H
H
R
S
R
H
R
R
R
R
H
H
sf-P
DF
DF
sf-P
G
G
sf-P
sf-P
G
DF
G
sf-P
SSF
SSF
SSF
H
R
H
R
S
R
R
R
S
H+R
R
R
S
H
S+R
11
11.5
± 0.1
± 0.2
3.6
3.8
3
2
2.2
3.7
1
1
9.6
3.2
1
± 0.2
2.2
3
7.9
3.7
8.7 ± 0.4
2.5
2
2.8
1
1
3
± 0.3
± 0.1
2.4
3
5
3
11.9
11.4
6.8 ± 0.3
4.1
3.9
2
1
1
3
7.3
± 0.5
2.2
3
10.8
± 0.2
3.6
3
3.7
2.9
2
1
1
1
Crustacea
EP
TE
D
Mollusca
Acanthochitona crinita
Barleeia unifasciata
Bittium reticulatum
Calliostoma zizyphinum
Gibbula cineraria
Haliotis tuberculata
Ocenebra erinacea
Ocinebrina aciculata
Patella pellucida
Rissoa parva
Tricolia pullus
Trivia arctica
Anomia ephippium
Hiatella arctica
Musculus subpictus
7.6
8.8
6.4 ± 0.3
14.4
5.9 ± 0.3
2.3
2.8
2
5
2
1
1
3
1
5
8.8
2.8
3
± 0.5
± 0.1
4.7
12.3
7.2
± 0.1
± 0.9
7.4
4.2
2.1
2.2
8.6
8.7
11.8 ±
9.7 ±
7.8 ±
9.9
8.8
6.9 ±
6.8
7.8 ±
11.7 ±
6.4 ±
6.4 ±
4.7
0
0.1
0.4
0.3
0.3
0.2
0.7
0.2
5
SC
13.7
7.1
RI
PT
7.5
11.1
M
AN
U
Copepoda spp.
Gnathia dentata
Janira maculosa
Apseudes talpa
Elasmopus rapax
Gammaropsis maculata
Hommarus gammarus
Jassa falcata
Leucothoe spinicarpa
Maera inaequipes
Eualus occultus
Cancer pagurus
Galathea squamifera
Necora puber
Pisidia longicornis
Porcellana platycheles
3
3
1
2.7
2.7
4
3.1
2.4
3.2
2.8
2
2
2.4
3.9
2
2
2
1
1
3
3
5
1
1
5
1
3
3
3
3
1
7.6
9.1
11
9
6.5
10
6.5
5.7
± 0.1
± 0.3
± 0.9
3.3
2
2
2
5
3
9.9
6.5
6.6
6.1
±
±
±
±
3.3
2
2
2
3
5
3
4
4.7
4.4
5.4
± 0
± 0.2
± 0.2
2
2
2
3
3
3
0.1
0.3
0.4
0.7
Bryozoa
AC
C
Alcyonidium gelatinosum
Crisia eburnea
Electra pilosa
Echinodermata
Amphipholis squamata
Asterias rubens
Asterina gibbosa
Echinus esculentus
Marthasterias glacialis
Psammechinus milliaris
Chordata
Botryllus schlosseri
Didemnum maculosum
Distomus variolosus
Polyclinum aurantium
SSF
SSF
SSF
S
S
S
5.5
± 0.2
2
3
5.5
± 0.7
2
3
DF
sf-P
sf-P
sf-P
sf-P
sf-P
S
R
S+R
R
R
R
7.7
± 0.4
2.3
3
10.5
± 0.2
3.4
3
SSF
SSF
SSF
SSF
S
H
S
R
6
6.1
± 0.8
± 0.2
2
2
3
3
7.1
± 0.1
2.1
3
9
9.5
9.4
11.7
11.1
±
±
±
±
±
9.5
0.1
0.3
0.1
0.2
0.1
2.9
3.1
3.1
4
3.8
3.1
3
3
5
3
3
1
5.2
6.4
7
7.2
±
±
±
±
0.3
0.5
0.3
0.4
2
2
2.1
2.2
3
3
5
3
AC
C
EP
TE
D
M
AN
U
SC
RI
PT
ACCEPTED MANUSCRIPT
AC
C
EP
TE
D
M
AN
U
SC
RI
PT
ACCEPTED MANUSCRIPT
AC
C
EP
TE
D
M
AN
US
CR
IP
T
ACCEPTED MANUSCRIPT
AC
C
EP
TE
D
M
AN
U
SC
RI
PT
ACCEPTED MANUSCRIPT
AC
C
EP
TE
D
M
AN
U
SC
RI
PT
ACCEPTED MANUSCRIPT
AC
C
EP
TE
D
M
AN
U
SC
RI
PT
ACCEPTED MANUSCRIPT
ACCEPTED MANUSCRIPT
ROSCOFF
Two-tailed
comparison (P -value)
MOLENE
KELP plants
Age (y)
Biomass (gAFDM)
5.7
89.8
±
±
1.5
20.9
5.3
106.7
±
±
1.1
25.6
0.494
0.285
Biomass (gAFDM)
43.3
±
14.5
3
±
0.8
0.815
Length (cm) 89.0
Biomass (gAFDM) 32.0
Mean diameter (mm) 22.8
Total volume (mL) 203.5
Surface area (cm²) 368.7
±
±
±
±
±
9.3
9.5
2.4
35.0
98.5
92.9
41.5
28.2
264.1
590.74
±
±
±
±
±
21.8
15.8
1.5
74.1
193.83
±
±
±
4.8
338.2
267.7
19.6
597.0
390.0
±
±
±
4.1
202.3
159.8
AC
C
EP
TE
D
Biomass (gAFDM) 14.5
Total volume (mL) 511.2
Interstitial volume (mL) 356.2
M
AN
U
HOLDFAST
SC
STIPE
RI
PT
LAMINA
0.725
0.283
0.003
0.137
0.052
0.108
0.639
0.815
ACCEPTED MANUSCRIPT
Roscoff
Molène
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Rhodophyceae
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AC
C
EP
TE
D
M
AN
U
SC
RI
PT
Acrosorium ciliolatum (Harvey) Kylin, 1924
Aglaothamnion bipinnatum (P.L.Crouan & H.M.Crouan) Feldmann & G.Feldmann, 1948
Aglaothamnion gallicum (Nägeli) Halos ex Ardré, 1970
Aglaothamnion priceanum Maggs, Guiry & Rueness, 1991
Aglaothamnion sp. Feldmann-Mazoyer, 1941
Aglaothamnion tenuissimum (Bonnemaison) Feldmann-Mazoyer, 1941
Antithamnionella sp. Lyle, 1922
Apoglossum ruscifolium (Turner) J.Agardh, 1898
Asparagopsis armata Harvey, 1855 (Falkenbergia rufolanosa Stage (Harvey) F.Schmitz, 1897)
Bonnemaisonia asparagoides (Woodward) C.Agardh, 1822
Brongniartella byssoides (Goodenough & Woodward) F.Schmitz, 1893
Calliblepharis ciliata (Hudson) Kützing, 1843
Callithamnion tetragonum (Withering) S.F.Gray, 1821
Callophyllis laciniata (Hudson) Kützing, 1843
Ceramium pallidum (Nägeli ex Kützing) Maggs & Hommersand, 1993
Chondria dasyphylla (Woodward) C.Agardh, 1817
Corallina elongata J.Ellis & Solander, 1786
Corallinale sp. / Peyssoniella sp. Complex
Cryptopleura ramosa (Hudson) L.Newton, 1931
Dasya sp. C.Agardh, 1824
Delesseria sanguinea (Hudson) J.V.Lamouroux, 1813
Dilsea carnosa (Schmidel) Kuntze, 1898
Gracilaria sp. Greville, 1830
Halurus flosculosus (J.Ellis) Maggs & Hommersand, 1993
Haraldiophyllum bonnemaisonii (Kylin) A.D.Zinova, 1981
Heterosiphonia plumosa (J.Ellis) Batters, 1902
Hypoglossum hypoglossoides (Stackhouse) F.S.Collins & Hervey, 1917
Kallymenia reniformis (Turner) J.Agardh, 1842
Lomentaria articulata (Hudson) Lyngbye, 1819
Lomentaria clavellosa (Lightfoot ex Turner) Gaillon, 1828
Membranoptera alata (Hudson) Stackhouse, 1809
Palmaria palmata (Linnaeus) Weber & Mohr, 1805
Phycodrys rubens (Linnaeus) Batters, 1902
Phyllophora crispa (Hudson) P.S.Dixon, 1964
Plocamium cartilagineum (Linnaeus) P.S.Dixon, 1967
Plumaria plumosa (Hudson) Kuntze, 1891
Polyneura bonnemaisonii (C.Agardh) Maggs & Hommersand, 1993
Polysiphonia brodiaei (Dillwyn) Sprengel, 1827
Polysiphonia elongata (Hudson) Sprengel, 1827
Polysiphonia sp. Greville, 1823
Pterosiphonia parasitica (Hudson) Falkenberg, 1901
Pterothamnion crispum (Ducluzeau) Nägeli, 1862
Ptilothamnion pluma (Dillwyn) Thuret, 1863
Ptilothamnion sphaericum (P.L.Crouan & H.M.Crouan ex J.Agardh) Maggs & Hommersand, 1993
Pyllophoraceae sp.
Rhodochorton purpureum (Lightfoot) Rosenvinge, 1900
Rhodophyllis divaricata (Stackhouse) Papenfuss, 1950
Rhodymenia pseudopalmata (J.V.Lamouroux) P.C.Silva, 1952
Sphaerococcus coronopifolius Stackhouse, 1797
Sphondylothamnion multifidum (Hudson) Nägeli, 1862
Phaeophyceae
Chaetopteris plumosa (Lyngbye) Kützing, 1843
Cutleria multifida (Turner) Greville, 1830
Cystoseira sp. C.Agardh, 1820
Dictyota dichotoma (Hudson) J.V.Lamouroux, 1809
Ectocarpus fasciculatus Harvey, 1841
Ectocarpus sp. Lyngbye, 1819 / Hincksia hincksiae (Harvey) P.C.Silva, 1987
Halopteris filicina (Grateloup) Kützing, 1843
Laminaria digitata (Hudson) J.V.Lamouroux, 1813
Laminaria hyperborea (Gunnerus) Foslie, 1884
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Saccorhiza polyschides (Lightfoot) Batters, 1902ACCEPTED
MANUSCRIPT
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Ulvophyceae
AC
C
EP
TE
D
M
AN
U
SC
RI
PT
Cladophora sp.1 Kützing, 1843
Cladophora sp.2 Kützing, 1844
Ulva sp. (compressa ) Linnaeus, 1753
Ulva rigida C.Agardh, 1823
Umbraulva sp. E.H.Bae & I.K.Lee, 2001
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ACCEPTED MANUSCRIPT
Roscoff
Molène
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Porifera
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Cnidaria
Amphisbetia operculata (Linnaeus, 1758)
Anemonia viridis (Forskål, 1775)
Diphasia attenuata (Hincks, 1866)
Dynamena pumila (Linnaeus, 1758)
Dyphasia (Agassiz, 1862) sp.
Kirchenpaueria pinnata (Linnaeus, 1758)
Lucernariopsis cruxmelitensis (Corbin, 1978)
Orthopyxis integra (MacGillivray, 1842)
Sertularella polyzonias (Linnaeus, 1758)
Urticina felina (Linnaeus, 1761)
TE
x
ο
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ο
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ο
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x
xx
ο
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ο
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EP
AC
C
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M
AN
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Amphilectus fucorum (Esper, 1794)
Axinella (Schmidt, 1862) sp.
Clathrina (Gray, 1867) sp.
Dysidea fragilis (Montagu, 1818)
Grantia compressa (Fabricius, 1780)
Guancha lacunosa (Johnston, 1842)
Halichondria (Fleming, 1828) sp.
Halichondria (Halichondria) panicea (Pallas, 1766)
Haliclona (Grant, 1836) spp.
Halisarca dujardinii (Johnston, 1842)
Hymeniacidon perlevis (Montagu, 1818)
Leucandra gossei (Bowerbank, 1862)
Leuconia johnstonii (Carter, 1871)
Leuconia nivea (Grant, 1826)
Myxilla (Myxilla) incrustans (Johnston, 1842)
Myxilla (Myxilla) rosacea (Lieberkühn, 1859)
Ophlitaspongia papilla (Bowerbank, 1866)
Phorbas plumosus (Montagu, 1818)
Porifera sp.
Suberitidae sp.
Sycon ciliatum (Fabricius, 1780)
Tethya aurantium (Pallas, 1766)
Tethya citrina (Sarà & Melone, 1965)
Entoprocta
Pedicellina nutans (Dalyell, 1848)
Nemertea
Cyanophthalma cordiceps (Friedrich, 1933)
Lineus (Sowerby, 1806) sp. (ruber/sanguineus )
Micrura (Ehrenberg, 1871) sp.
Nemertea sp.
Oerstedia dorsalis (Abildgaard, 1806)
Tubulanus linearis (McIntosh, 1874)
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Mollusca
Polyplacophora
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M
AN
U
D
TE
EP
AC
C
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PT
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ACCEPTED MANUSCRIPT
Acanthochitona crinita (Pennant, 1777)
Callochiton septemvalvis (Montagu, 1803)
Gastropoda
Alvania cancellata (da Costa, 1778)
Barleeia unifasciata (Montagu, 1803)
Bittium reticulatum (da Costa, 1778)
Calliostoma zizyphinum (Linnaeus, 1758)
Cerithiopsis barleei (Jeffreys, 1867)
Cerithiopsis tubercularis (Montagu, 1803)
Chauvetia brunnea (Donovan, 1804)
Crisilla semistriata (Montagu, 1808)
Gibbula cineraria (Linnaeus, 1758)
Gibbula umbilicalis (da Costa, 1778)
Haliotis tuberculata (Linnaeus, 1758)
Jujubinus (Monterosato, 1884) sp.
Lacuna pallidula (da Costa, 1778)
Lacuna parva (da Costa, 1778)
Lamellaria latens (Müller O.F., 1776)
Manzonia crassa (Kanmacher, 1798)
Marshallora adversa (Montagu, 1803)
Nassarius incrassatus (Strøm, 1768)
Ocenebra erinaceus (Linnaeus, 1758)
Ocinebrina aciculata (Lamarck, 1822)
Odostomia unidentata (Montagu, 1803)
Onoba aculeus (Gould, 1841)
Onoba semicostata (Montagu, 1803)
Patella pellucida (Linnaeus, 1758)
Pleurobranchus membranaceus (Montagu, 1815)
Pusillina inconspicua (Alder, 1844)
Raphitoma linearis (Montagu, 1803)
Raphitoma purpurea (Montagu, 1803)
Retusa truncatula (Bruguière, 1792)
Rissoa lilacina (Récluz, 1843)
Rissoa membranacea (J. Adams, 1800)
Rissoa parva (da Costa, 1778)
Tectura virginea (O.F. Müller, 1776)
Tricolia pullus (Linnaeus, 1758)
Trivia arctica (Pulteney, 1799)
Bivalvia
Aequipecten opercularis (Linnaeus, 1758)
Anomia ephippium (Linnaeus, 1758)
Rhomboidella prideauxi (Leach, 1815)
Mimachlamys varia (Linnaeus, 1758)
Hiatella arctica (Linnaeus, 1767)
Kellia suborbicularis (Montagu, 1803)
Modiolula phaseolina (Philippi, 1844)
Musculus discors (Linnaeus, 1767)
Musculus subpictus (Cantraine, 1835)
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ACCEPTED MANUSCRIPT
Sipuncula
Nephasoma (Nephasoma) minutum (Keferstein, 1862a)
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Bryozoa
Aetea anguina (Linnaeus, 1758)
Alcyonidium gelatinosum (Linnaeus, 1761)
Alcyonidium hirsutum (Fleming, 1828)
Amathia lendigera (Linnaeus, 1758)
Bicellariella ciliata (Linnaeus, 1758)
Caberea boryi (Audouin, 1826)
Callopora lineata (Linnaeus, 1767)
Cellepora pumicosa ( Pallas, 1766)
Celleporella hyalina (Linnaeus, 1767)
Celleporina caliciformis (Lamouroux, 1816)
Crisia aculeata (Hassall, 1841)
Crisia denticulata (Lamarck, 1816)
Crisia eburnea (Linnaeus, 1758)
Crisidia cornuta (Linnaeus, 1758)
Electra pilosa (Linnaeus, 1767)
Escharella (Gray, 1848) spp.
Escharoides coccinea (Abildgaard, 1806)
Filicrisia geniculata (Milne Edwards, 1838)
Flustrellidra hispida (O. Fabricius, 1780)
Haplopoma impressum (Audouin, 1826)
Lichenopora verrucaria (O. Fabricius, 1780)
Membranipora membranacea (Linnaeus, 1767)
Membraniporella nitida (Johnston, 1838)
Microporella ciliata (Pallas, 1766)
Oshurkovia littoralis (Hastings, 1944)
Phaeostachys spinifera (Johnston, 1847)
Plagioecia sarniensis (Norman, 1864)
Plesiothoa gigerium (Ryland & Gordon, 1977)
Ramphonotus minax (Busk, 1860)
Schizomavella auriculata (Hassall, 1842)
Schizomavella hastata (Hincks, 1862)
Schizomavella linearis (Hassall, 1841)
Scruparia chelata (Linnaeus, 1758)
Scrupocellaria reptans (Linnaeus, 1758)
Scrupocellaria scabra (van Beneden, 1848)
Scrupocellaria scruposa (Linnaeus, 1758)
Tubulipora plumosa (Thompson in Harmer, 1898)
Turbicellepora magnicostata (Barroso, 1919)
Vesicularia spinosa (Linnaeus, 1758)
TE
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AC
C
EP
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Annelida
Ctenodrilidae
Ctenodrilidae sp. (Kennell, 1882)
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Eunicidae
Eunicidae (Berthold, 1827) indet.
Lumbrineris funchalensis (Kinberg, 1865)
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EP
AC
C
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ACCEPTED
Lysidice ninetta (Audouin & Milne-Edwards,
1833) MANUSCRIPT
Nereidae
Leonnates glauca (Claparède, 1870)
Nereis pelagica (Linnaeus, 1758)
Platynereis dumerilii (Audouin & Milne Edwards, 1834)
Syllidae
Amblyosyllis formosa (Claparède, 1863)
Autolytinae (Langherans, 1879) indet.
Eurysyllis tuberculata (Ehlers, 1864)
Eusyllis assimilis (Marenzeller, 1875)
Eusyllis blomstrandi (Malmgren, 1867)
Exogone (Exogone) naidina (Örsted, 1845)
Exogone (Örsted, 1845) sp.
Haplosyllis spongicola (Grube, 1855)
Myrianida prolifera (O.F. Müller, 1788)
Odontosyllis ctenostoma (Claparède, 1868)
Pionosyllis lamelligera (Saint Joseph, 1887)
Sphaerosyllis hystrix (Claparède, 1863)
Syllis (Lamarck, 1818) sp.
Syllis armillaris (O.F. Müller, 1776)
Syllis columbretensis (Campoy, 1982)
Syllis gracilis (Grube, 1840)
Syllis hyalina (Grube, 1863)
Syllis variegata (Grube, 1860)
Trypanosyllis (Trypanosyllis) coeliaca (Claparède, 1868)
Trypanosyllis zebra (Grube, 1840)
Phyllodocidae
Eumida sanguinea (Örsted, 1843)
Nereiphylla rubiginosa (Saint-Joseph, 1888)
Phyllodoce ( Lamarck, 1818 ) sp.
Polynoidae
Harmothoe extenuata (Grube, 1840)
Harmothoe impar (Johnston, 1839)
Harmothoe spinifera (Ehlers, 1864)
Lepidonotus clava (Montagu, 1808)
Pholoe inornata (Johnston, 1839)
Subadyte pellucida (Ehlers, 1864)
Orbiniidae
Proscoloplos cygnochaetus (Day, 1954)
Maldanidae
Nichomache (Malmgren, 1865) spp.
Arenicolidae
Arenicolides ecaudata (Johnston, 1835)
Spionidae
Aonides oxycephala (Sars, 1862)
Dipolydora (Verrill, 1881) sp.
Pseudopolydora (Czerniavsky, 1881) sp.
Scolelepis tridentata (Southern, 1914)
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Sabellidae
Amphiglena mediterranea (Leydig, 1851)
Branchiomma bombyx (Dalyell, 1853)
Branchiomma lucullanum (Delle Chiaje, 1828)
Fabricia sabella (Ehrenberg, 1836)
Jasmineira elegans (Saint-Joseph, 1894)
Oridia armandi (Claparède, 1864)
Parasabella langerhansi (Knight-Jones, 1983)
Pseudopotamilla reniformis (Bruguière, 1789)
Sabella discifera (Grube, 1874)
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Sabellariidae
Sabellaria spinulosa (Leuckart, 1849)
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Serpudidae
Protula tubularia (Montagu, 1803)
Salmacina (Claparède, 1870) sp.
Spirorbis corrugatus (Montagu, 1803)
Spirorbis (Daudin, 1800) sp.
Spirobranchus triqueter (Linnaeus, 1758)
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Terebellidae
Spadella (Langerhans, 1880) sp.
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Amphitrite johnstoni (Malmgren, 1865)
Eupolymnia nebulosa (Montagu, 1818)
Eupolymnia nesidensis (Delle Chiaje, 1828)
Nicolea venustula (Montagu, 1818)
Nicolea zostericola (Örsted, 1844)
Pista elongata (Moore, 1909)
Polycirrus medusa (Grube, 1850)
Trichobranchus glacialis (Malmgren, 1866)
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Chaetognatha
Platyhelminthes
Cycloporus papillosus (Sars in Jensen, 1878) Lang, 1884
Stylochoplana maculata (Quatrefage, 1845)
Nematoda
Nematoda spp.
Pycnogonida
Achelia echinata (Hodge, 1864)
Achelia hispida (Hodge, 1864)
Ammothella longipes (Hodge, 1864)
Anoplodactylus angulatus (Dohrn, 1881)
Callipallene brevirostris (Johnston, 1837)
Endeis spinosa (Montagu, 1808)
Nymphon gracile (Leach, 1814)
Nymphon brevirostre (Hodge, 1863)
Crustacea
Cirripedia
Verruca stroemia (O.F. Müller, 1776)
Isopoda
Astacilla danmoniensis (Stebbing, 1874)
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Calathura norvegica (Sars, 1872) ACCEPTED MANUSCRIPT
Dynamene bidentata (Adams, 1800)
Dynamene magnitorata (Holdich, 1968)
Gnathia dentata (G. O. Sars, 1872)
Gnathia maxillaris (Montagu, 1804)
Janira maculosa (Leach, 1814)
Stenosoma lancifer (Miers, 1881)
Isopoda sp.
Leptostraca
Nebalia bipes (Fabricius, 1780)
Mysida
Praunus inermis (Rathke, 1843)
Tanaidacea
Apseudes talpa (Montagu, 1808)
Apseudopsis latreillii (Milne-Edwards, 1828)
Amphipoda
Aora spinicornis (Afonso, 1976)
Ampithoe gammaroides (Bate, 1856)
Ampithoe ramondi (Audouin, 1826)
Ampithoe rubricata (Montagu, 1818)
Apherusa bispinosa (Bate, 1857)
Apherusa cirrus (Bate, 1862)
Apherusa jurinei (Milne-Edwards, 1830)
Caprella acanthifera (Leach, 1814)
Caprella fretensis (Stebbing, 1878)
Crassicorophium bonellii (Milne Edwards, 1830)
Dexamine spinosa (Montagu, 1813)
Dexamine thea (Boeck, 1861)
Elasmopus (Costa, 1853)
Gammaropsis maculata (Johnston, 1828)
Iphimedia obesa (Rathke, 1843)
Jassa falcata (Montagu, 1808)
Lembos websteri (Bate, 1857 )
Leucothoe spinicarpa (Abildgaard, 1789)
Lysianassa ceratina (Walker, 1889)
Maera grossimana (Montagu, 1808)
Maera inaequipes (Costa, 1857)
Melita hergensis (Reid, 1939)
Microprotopus (Norman, 1867 sp.
Nannonyx spinimanus (Walker, 1895)
Orchomene humilis (Costa, 1853)
Phtisica marina (Slabber, 1769)
Sunamphitoe pelagica (Milne-Edwards, 1830)
Triphosella (Bonnier, 1893) sp.
Tritaeta gibbosa (Bate, 1862)
Decapoda
Anapagurus hyndmanni (Bell, 1846)
Cancer pagurus (Linnaeus, 1758 )
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ACCEPTED MANUSCRIPT
Eualus occultus (Lebour, 1936)
Eualus pusiolus (Krøyer, 1841)
Eurynome spinosa (Hailstone, 1835)
Galathea squamifera (Leach, 1814 )
Galathea strigosa (Linnaeus, 1761)
Homarus gammarus (Linnaeus, 1758)
Lophozozymus incisus (H. Milne Edwards, 1834)
Maja squinado (Herbst, 1788)
Necora puber (Linnaeus, 1767)
Pagurus bernhardus (Linnaeus, 1758)
Philocheras fasciatus (Risso, 1816)
Pilumnus hirtellus (Linnaeus, 1761)
Pisidia longicornis (Linnaeus, 1767)
Porcellana platycheles (Pennant, 1777)
Xantho pilipes ( A. Milne-Edwards, 1867)
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Echinodermata
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Amphipholis squamata (Delle Chiaje, 1828)
Antedon bifida (Pennant, 1777)
Aslia lefevrii (Barrois, 1882)
Asterias rubens (Linnaeus, 1758)
Asterina gibbosa (Pennant, 1777)
Cucumaria frondosa (Gunnerus, 1767)
Echinus esculentus (Linnaeus, 1758)
Henricia sanguinolenta (O.F. Müller, 1776)
Holothuria (Panningothuria) forskali (Delle Chiaje, 1823)
Luidia ciliaris (Philippi, 1837)
Marthasterias glacialis (Linnaeus, 1758)
Ocnus lacteus (Forbes & Goodsir, 1839)
Ophiothrix fragilis (Abildgaard, in O.F. Müller, 1789)
Pawsonia saxicola (Brady & Robertson, 1871)
Psammechinus miliaris (P.L.S. Müller, 1771)
Chordata
Aplidium pallidum (Verrill, 1871)
Aplidium punctum (Giard, 1873)
Aplidium glabrum (Verrill, 1871)
Aplidium (Savigny, 1816) spp.
Ascidia mentula (Müller, 1776)
Botryllus schlosseri (Pallas, 1766)
Clavelinidae [Archidistoma aggregatum (Garstang, 1891)]
Dendrodoa grossularia (Van Beneden, 1846)
Didemnum maculosum (Milne-Edwards, 1841)
Distomus variolosus (Gaertner, 1774)
Lissoclinum perforatum (Giard, 1872)
Molgula crinita (Sluiter, 1904)
Morchellium argus (Milne-Edwards, 1841)
Polycarpa (Heller, 1877) sp.
Polyclinum aurantium (Milne-Edwards, 1841)
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ACCEPTED MANUSCRIPT
Pyura (Molina, 1782) sp.
Styela (Fleming, 1822) sp.
Trididemnum (Della Valle, 1881) sp.