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Spatial and depth-associated distribution patterns of shallow gorgonians in the Algarve coast (Portugal, NE Atlantic)

Helgoland Marine Research volume 67, pages 521–534 (2013)Cite this article

Abstract

The ecological role of gorgonians for marine rocky bottoms is worldwide recognized, but the information on the distribution patterns of NE Atlantic temperate species is insufficient, considering current global, regional and local threats. To overcome the lack of information on the spatial distribution patterns of gorgonians in south Portugal, in 2009/2010, the occurrence and abundance of gorgonian species in rocky bottoms were quantified over more than 25 km of coast (37.1°N/8.6°W) down to 30 m depth. Eunicella labiata, Eunicella gazella, Eunicella verrucosa and Leptogorgia sarmentosa were abundant and frequent in the studied area, while Leptogorgia lusitanica was less abundant. All species evidenced a similar depth pattern, that is abundance significantly increased with depth below 15 m. At shallower waters (up to 15 m), the distribution of gorgonians may be constrained by abiotic factors and competition with algae. Indeed, the abundance of gorgonians was negatively correlated with the percentage cover of algae along the depth gradient, but gorgonians and sponges coexist. Competition among gorgonian species also seems to be low in this area because of the similarity in the abundance pattern observed for the most abundant species and also their high association. In NE Atlantic shallow temperate rocky bottoms, the distribution of gorgonians seems to be influenced by environmental factors and biological interactions, namely competition (algae) and coexistence (sponges and other gorgonians).

Introduction

Gorgonians (Octocorallia: Alcyonacea) are colonial organisms characterized by a skeleton, slow growth and long life span. Their three-dimensional structure may modify the physical habitat, by reducing current velocity, stabilizing soft substrata, enhancing sedimentation and local accumulation of fine particles, as well as increasing availability of niches similarly to what is found for other marine animals (e.g. Idjadi and Edmunds 2006; Norling and Kautsky 2007). They are habitat formers (foundation species) facilitating the colonization of other species through positive indirect effects (Bruno et al. 2003; Thomsen et al. 2010) creating habitat cascades. The importance of these facilitation processes for the structure of communities in terms of species abundance and diversity is widely accepted (Thomsen et al. 2010). However, the positive effects deriving from habitat cascades depend on the characteristics of the foundation species, such as size, density and longevity (Bruno et al. 2003). In coastal marine communities, gorgonians are commonly the most abundant habitat formers, sometimes the only conspicuous ones, providing the framework for the community. Because gorgonians are long-lived animals, they may extend these modifications for long time, producing significant effects in marine ecosystems, namely by enhancing local diversity (Cerrano et al. 2009). Furthermore, the ecological role of gorgonians in ecosystem functioning has been widely acknowledged (Ballesteros 2006; Coma et al. 2006; Cupido et al. 2008; Linares et al. 2008b), with a strong emphasis on the role of habitat formers in marine conservation (see Wright and Jones 2006).

Over the last decades, many studies reported that gorgonians are affected by drastic, rapid and lasting disturbances either of natural (e.g. Linares et al. 2005; Coma et al. 2006; Garrabou et al. 2009) or human origin (e.g. Bavestrello et al. 1997; Coma et al. 2004; Chiappone et al. 2005; Cerrano and Bavestrello 2008; Linares et al. 2008b). In order to preserve their ecological role as habitat formers, detailed knowledge on the distribution patterns of abundance of gorgonian species is essential to propose adequate conservation and management measures (Benedet-Cecchi et al. 2003; García-Charton et al. 2008; Costello et al. 2010).

The Algarve coast (southern Portugal, north-eastern Atlantic) presents a rich fauna with biogeographic affinities with the Mediterranean Sea, the Lusitanian, the west African Transition, Northern European Seas and Western Atlantic provinces (sensu Spalding et al. 2007; Souto et al. 2010; Levy et al. 2011), because of the proximity to the Strait of Gibraltar (Baus et al. 2005; and references therein) and the confluence of oceanic currents (Cherubin et al. 2000; Pérez et al. 2001; Coelho et al. 2002; Martins et al. 2002). However, the gorgonian populations of southern Portugal are poorly described, especially compared to the Mediterranean, where in the past few years, several studies have been performed in shallow sub-littoral waters, gathering a large amount of biological and ecological information, and building predictive models to be used in conservation plans (Linares et al. 2007, 2008b; Bramanti et al. 2009). In fact, the most recent study concerning the gorgonian fauna of the Algarve coast reported only 10 different species caught as by-catch by bottom gill nets (Vieira 2008). Therefore, significant knowledge gaps still persist, namely on the abundance patterns in the near shore benthic community (0–30 m), spatial and depth distribution.

In this context, the present study aimed to quantify the occurrence and abundance of the main gorgonian species in the shallow rocky bottoms (0–30 m) of the western Algarve coast (≈25 km of coastline). In order to assess the relationship between the distribution of gorgonians and potential competitors for space and food, the percentage cover of erect algae and sponges were also quantified. If population dynamics of those benthic taxa is governed by competition, it is expected that the abundance of gorgonians and both erect algae and sponges would be inversely correlated.

Materials and methods

Study area

The Algarve coast (Fig. 1) is characterized by heterogeneous coastline and sub-littoral areas. The western part of the Algarve coast comprises rocky formations of several types (e.g. underwater spurs, boulders, low relief rocky areas, submerged rock bottoms) and by different sediment dynamics.

Fig. 1
figure1

Location of the sampling sites (filled circle) in Lagos Bay

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The study area is located in the western Algarve coast extending from Lagos to Portimão (Fig. 1), hereafter designated by Lagos Bay. This area has 20.6 km2 of rocky bottoms within a total area of 70 km2 (up to 30 m depth) and covers ≈25 km of the Algarve coast, distancing only ≈30 km to the westernmost continental part of Europe (Cabo São Vicente, Sagres). In particular, the coast between Ponta da Piedade and Armação de Pêra, where this study was conducted, is morphologically complex presenting rocky areas with cliffs forming small beaches, a large bay with extensive sandy beaches and dunes, including a coastal lagoon (Ria de Alvor) and a small estuary (Rio Arade). The shallow continental shelf (down to ≈30 m depth) is generally characterized by rocky outcrops with pockets of rubble and/ or sand (Gonçalves et al. 2010)

In general, the circulation patterns in the Iberian Peninsula are dominated by up-welling (summer) and down-welling (winter) events associated with northerly/southerly winds, coupled to the North Atlantic Oscillation (Sánchez et al. 2007). Sea surface temperature presents marked seasonal variation depending on whether down-welling or up-welling dominates (ranging from 14 to 24 °C, respectively; http://www.hidrografico.pt/), whereas salinity is fairly constant (35.0–36.0).

Species identification

The identification of gorgonian species was based on the studies by Carpine and Grasshoff (1975), Grasshoff (1988; 1992) and González (1993). In the Algarve coast, underwater identification of gorgonians is difficult because of ambiguities in the taxonomy of Eunicella and Leptogorgia, and therefore, the following criteria were established to identify these species:

  • Eunicella gazella colonies always white with orange polyps; diameter of the ramets noticeably larger than in E. verrucosa; colony surface generally homogeneous with low relief and extensive branching mostly in one dimension.

  • Eunicella verrucosa colonies with colour varying from white to cream, beige or pale orange; polyps varying from white to orange; heterogeneous surface with “bumps” (verrucae), usually larger in size than E. gazella.

  • Eunicella labiata large species; colonies divided in two main branches immediately after the base of the colony, with less branches than E. verrucosa and E. gazella; colours are usually darker than in the previous species, ranging from cream to dark brown; colonies are often broken, loosing one of the main branches; conspicuous verrucae observed all over the colony, usually lighter.

  • Eunicella singularis erect colonies with few long branches always in upright position; colonies always white coloured; colony surface generally smooth with low relief.

  • Leptogorgia lusitanica bush-like colonies growing in only one dimension, perpendicular to dominant currents; terminal branches thinner than the central ones; extremely variable in colour, generally presenting two colours, usually wine red/purple and yellow, sometimes white and blue, and other times uniform in colour (generally white or yellow); the central branches of the colony usually lack polyps in the surface facing the currents.

  • Leptogorgia sarmentosa bush-like colonies growing in one or more dimensions; usually of uniform but variable colour (yellow, red, brick orange, rarely white, rarely green); polyps usually present in all surfaces of the branches.

Underwater photographs of the most common gorgonian species from the study area are presented in Fig. 2.

Fig. 2
figure2

Main gorgonian species found in Lagos Bay. a E. labiata, b E. verrucosa, c E. gazella, d L. sarmentosa, e L. lusitanica. Photos b, c, d, e by Pedro Veiga

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Spatial and depth distribution of the main gorgonian species

In order to describe the patterns of spatial and vertical distribution of gorgonian species, a total of 69 sites were sampled by means of underwater transects by scuba diving 5 × 1 m belt transects (horizontal), 3 replicates at each site (in total 207 sampling units) from May 2009 to June 2010. Sampling sites were randomly selected, but restricted to rocky substrata, explaining the spatial gaps. In this area, gorgonians are rarely found in soft bottoms, therefore sampling effort was directed towards rocky bottoms only. The bathymetric distribution of the gorgonian species was analysed considering the average depth of each sampling unit and estimating the median density at 6 depth levels: 0–5 m, 5–10 m, 10–15 m, 15–20 m, 20–25 m and 25–30 m. The number of transects conducted at each depth level was different (see Table 1). Sampling was restricted to 30 m due to scuba diving safety rules and dive time constraints.

Table 1 Gorgonian presence and frequency of occurrence at the different depth levels for the whole gorgonian assemblage (all gorgonians) and each species separately
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Interaction between gorgonians and other benthic groups

In order to assess interaction effects between gorgonians and potential competitors for space and food, the abundance of erect algae (macroalgae and turf) and sponges was quantified. While conducting the censuses of the gorgonian populations, the number of sponges was counted at each transect, and the percentage cover of erect algae was quantified using quadrats (1 × 1 m, 3 replicates).

Statistical analyses

The distribution of gorgonian species indicated that only five out of seven species were frequent in the study area (see Results). Therefore, the comparison of the density of gorgonians at different depth levels was undertaken for the overall gorgonian assemblage (all gorgonians) and for the most frequent species (L. sarmentosa, L. lusitanica, E. gazella, E. labiata and E. verrucosa) using parametric (one-way ANOVA) or nonparametric methods (Kruskal–Wallis’ H test) whenever ANOVA assumptions were not met. In both cases, pairwise multiple comparisons were used: Tukey Honestly Significant Differences (Tukey HSD) and Behrens-Fisher nonparametric multiple test (Berhens-Fisher) (Munzel and Hothorn 2001), respectively. The number of transects was not constant at each depth level, resulting in an unbalanced design, therefore depth levels with fewer samples (0–5 m and 25–30 m) were discarded to improve the power of the statistical tests. The correlation between depth and density of gorgonians was tested by means of an exponential regression using the log e (1 + y) transformation of the dependent variable.

Non-metric multidimensional scaling was used to analyse differences in the distribution and abundance patterns of gorgonian assemblages using the modified Gower dissimilarity index with transformed data (log2(x) + 1). The modified Gower index excludes joint absences and is able to detect changes in composition, with the advantage of being directly interpretable as the average change in orders of magnitude between two sampling units (Anderson et al. 2006). The choice of the base of the logarithm emphasizes compositional change or changes in abundance. By using log2 transformation, the modified Gower index is weighted towards a compositional change equal to a doubling in abundance (Anderson et al. 2006), which places more emphasis on changes in relative abundance. To analyse the contribution of each species to the discrimination of the compared assemblages, the indicator value (IndVal) was used (Dufrêne and Legendre 1997). On the other hand, the ecological association of gorgonians was quantified using the Ochiai measure based on binary data (presence-absence data) (Janson and Vegelius 1981). This measure presents minimum coexistence values of 0 when the two species are never found together and maximum coexistence values of 1 when both species always occur together (Janson and Vegelius 1981).

The correlation between the abundance of gorgonians and potential competitors was assessed using linear regression. All statistical analyses were performed using the open source software R version 12.1 (R Development Core Team 2010).

Results

Distribution patterns of gorgonian species

Occupancy and abundance

In Lagos Bay, gorgonians were present in 64.7 % of the 207 sampling units, totalling 2481 colonies belonging to seven taxa (Table 1). Four species, E. labiata, E. verrucosa, L. sarmentosa and E. gazella, were responsible for 96.9 % of the total abundance. E. labiata was the most frequent (52.7 % of transects) and abundant species (36.5 % of the total). E. verrucosa, E. gazella, L. sarmentosa, were also were also frequent (39.6–45.9 % of the transects) and abundant (18.5–22.4 % of the total abundance). L. lusitanica was found in 16.9 % of the transects but accounted only for 2.9 % of the abundance. E. singularis was rare as only three colonies were accounted in a single transect.

Spatial and depth distribution

Generally, gorgonians were present in the entire study area, without any evidence of spatial segregation (Fig. 3).

Fig. 3
figure3

Spatial distribution of gorgonian species in Lagos Bay. The size of the bubbles reflects the abundance of the gorgonians at each transect. Density is presented as colonies per 5 square metres

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In Lagos Bay, gorgonians were found from 7.5 to 27 m (the maximum depth sampled). The depth range of all species presented similar upper limits, with L. sarmentosa occurring from 7.5 m, E. verrucosa from 8.0 m, E. labiata and L. lusitanica from 8.7 m and E. gazella from 11.6 m. The increase of gorgonians’ abundance with depth was evident and common to the most frequent and abundant species (Fig. 4). Up to 15 m, gorgonians were rare or presented very low abundance. At depths deeper than 15 m, all species increased in abundance and showed similar trends. At 20–25 m, more than  colonies per 5 square metres were found in Lagos Bay. All species showed large variation in abundance at 15–20 m and 20–25 m, especially the most abundant and frequent ones (Fig. 4).

Fig. 4
figure4

Depth distribution of gorgonian species’ abundance in Lagos Bay. Data correspond to transects grouped into depth levels. The black square represents the median; the box indicates the first and third quartiles; and the line denotes the range. Total number of colonies (n) and samples (t) are indicated for each species

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Significant differences were found in the abundance of all species at different depth levels (Table 2). For the most abundant and frequent species, E. labiata, significant differences were found between depth levels below and above 15 m (Table 2). The second most abundant species, E. verrucosa, showed significant differences between 10–15 m and 20–25 m, whereas L. sarmentosa showed differences between 20–25 m (its highest abundance) and the shallower depth levels (up to 15 m). E. gazella was absent above 10 m and rare at 10–15 m, increasing significantly its abundance with depth. L. lusitanica exhibited low abundance but still the same increasing pattern with depth. Its abundance was significantly higher at depths below 15 m, even though apparently decreasing at 25–30 m.

Table 2 Results of Kruskal–Wallis’ H (H) for the abundance of gorgonians at each depth level
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An exponential trend was detected between depth and gorgonian’s abundance for the bathymetric range of this study (Fig. 5). All regressions were highly significant (P < 0.001) and presented high coefficients of determination (r 2 = 0.438–0.787, except for L. lusitanica with 0.221). The increase of 1 m in depth is associated with a 10.3–11.0 % increase in the number of colonies of L. sarmentosa, E. gazella and E. verrucosa, with E. labiata showing the highest percentage (15.5 %) and L. lusitanica presenting a much lower value (3.0 %). The rates of increase in the two latter species were significantly different from the remaining (L. lusitanica, ANCOVA, P < 0.001; E. labiata, ANCOVA, P < 0.05).

Fig. 5
figure5

Relationship between depth and abundance of gorgonians in Lagos Bay. The regression equation is presented for each species. The axes of the graphs were rotated for improving the visualization of the depth gradient

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The non-metric multidimensional scaling diagram (Fig. 6) shows a depth gradient from left to right, reflecting differences in abundance within each depth level. The composition and structure of the gorgonian assemblages in Lagos Bay presented significant differences (Permanova, Pseudo F = 4.07, P < 0.001), due to higher abundances at deeper sites. However, the generally low indicator values (IndVal 0.31–0.44; P > 0.05) showed that the composition of the assemblages was similar at all depth levels and most species (except E. singularis) occurred in several depth levels. The assemblage was characterized by a dynamic alternation in species rankings with E. labiata being in the top two ranks along the studied depth range and L. sarmentosa alternating from first to fourth in rank. The low abundance of L. lusitanica was reflected in its rank position, fifth at all depth levels.

Fig. 6
figure6

Non-metric multidimensional scaling plot of the gorgonian assemblage data from Lagos Bay (modified Gower index of dissimilarity using log2(x) + 1 transformed data)

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Four species were highly associated, coexisting in a large number of the samples. E. labiata, E. verrucosa, E. gazella and L. sarmentosa presented high values of the Ochiai measure (0.68–0.85), whereas L. lusitanica showed lower values (0.46–0.58) and E. singularis presented extremely low levels of association with the remaining gorgonian species (0–0.19).

Interactions between gorgonians and other biota

The distribution of erect algae (mainly Chlorophyta and Phaeophyta) and sponges in Lagos Bay is also depth-dependent. The abundance of erect algae (dominated by Dictyota dichotoma, Asparagopsis armata, Halopteris filicina, Gelidium latifolium and Peyssonnelia rubra) declined along the depth gradient. On the other hand, sponges clearly increased their abundance with depth (Fig. 7). This group was dominated by encrusting forms such as Phorbas fictitius, Scopalina lophyropoda, Cliona viridis, Axinella damicornis and Chondrosia reniformis and massive erect forms such as Crella elegans and Axinella polypoides. A significant negative correlation (linear regression, r 2 = 0.439, F 1,11 = 8.605, P < 0.05) between the percentage cover of erect algae, and the number of gorgonian colonies was found in Lagos Bay, whereas a positive correlation (linear regression, r 2 = 0.769, F 1,11 = 36.67, P < 0.05) was detected between sponges and gorgonians (Fig. 7).

Fig. 7
figure7

Percentage cover of erect algae and abundance of sponges along the depth gradient (a and b, respectively) and linear regressions between these faunal groups and the number of gorgonian colonies in Lagos Bay (c and d). N-abundance

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Discussion

The present study detected a clear depth pattern in the distribution of all gorgonian species in Lagos Bay. According to Weinberg (1978), the two main factors affecting the octocorallia communities are irradiance and presence of sediment in the substrate. The amount of light reaching an underwater surface is related to depth, even though it depends on several factors, namely transparency and suspended particles (Gili et al. 1989). Depth, slope and the interaction of these two factors have been reported as presenting a marked positive effect in Anthozoa species distribution (Gili et al. 1989). Indeed, many studies highlighted major variations of physical (e.g. currents, sedimentation) and chemical variables (organic matter content) along the depth gradient, with consequences for the distribution of marine communities (e.g. Garrabou et al. 2002; McArthur et al. 2010).

For most species, the general pattern found indicated increasing abundances with depth within the analysed depth range. The present study also revealed that the 15 m bathymetric seems to be an important turning point in the distribution of most gorgonian species in Lagos Bay, which can be related to higher irradiance above this depth but also to higher surf impact. Indeed, in the Algarve, the lower beach profile limit (closure depth), where wave action is able to disturb the sea bottom, is around 10 m below mean sea level (Dolbeth et al. 2007; Almeida et al. 2011), which is known to influence the patterns of benthic communities (Dolbeth et al. 2007; Carvalho et al. 2011). The turbulence from surf can detach gorgonians but also increase the rates of contact with substrate or neighbouring conspicuous fauna and flora, leading to colony tissue damage due to abrasion. The upper depth distribution limit of the dominant gorgonians in Lagos Bay was very similar suggesting that they are determined by abiotic conditions as observed elsewhere (Zabala and Ballesteros 1989; Linares et al. 2008a), especially the high water motion of shallower coastal areas. The combination of both factors (strong irradiance and surf) was already reported as being determinant in the distribution of western Mediterranean gorgonian species (Weinberg 1978).

Depth distribution in tropical shallow water gorgonians is also mainly governed by light (Sánchez et al. 1998) and other environmental factors affecting light (e.g. bed load, Yoshioka and Yoshioka 1989), mainly because most species are zooxanthellate (Dahlgren 1989; Sánchez et al. 1998). In opposition, shallow water gorgonian assemblages in the Algarve are dominated by azooxanthelate octocorals, with the zooxanthelate gorgonian E. singularis being rarely sampled (and the presence of zooxanthelae in the few colonies found in the Algarve was not confirmed). Besides, in the present study, erect algae dominated the biocenoses at low depth but rapidly decreased their abundance when light intensity is reduced, and their abundance was inversely correlated to the abundance of gorgonians. In shallow water, algal-dominated benthic communities present species that favour out-competition processes being continuously replaced (Garrabou et al. 2002). In contrast, animal-dominating deeper communities tend to present slow-growth species avoiding competition displacement and enhancing the maintenance of diversity and complexity (Garrabou et al. 2002). However, there is a depth range (12–20 m) where the abiotic conditions seem suitable both for erect algae and gorgonians where competition for space occurs, explaining the negative correlation between the two groups. In fact, anthozoans are unable to compete with large algae where light intensity is high (Zabala and Ballesteros 1989; Gili et al. 1989) supporting the idea that the bathymetric behaviour of gorgonian species in Lagos Bay may be only indirectly linked to light intensity. The present observations are in agreement with the model proposed for the Mediterranean, consisting of three zones: a superficial zone (0–10 m) dominated by erect algae, a mixed zone (10–15 m) co-dominated by erect algae, crustose algae and suspension feeders and a third zone (15–42 m) dominated by suspension feeders (Zabala and Ballesteros 1989).

Sponges and gorgonians in Lagos Bay presented similar distribution patterns with depth and were positively correlated, suggesting that the species belonging to these groups coexist. Massive erect sponges such as C. elegans and A. polypoides may compete for space with gorgonians, but these are only a part of the sponges assemblage (percentage cover of sponges was not assessed) dominated by encrusting forms that use the available space below erect forms efficiently. Sponges mainly feed on very small particles, such as suspended particles, free-living bacteria and colloidal organic matter (Ruppert and Barnes 1994; Riisgård and Larsen 2010). On the other hand, gorgonians mainly feed on larger particles such as zooplankton and particulate organic carbon. Therefore, passive (gorgonians) and active (sponges) suspension feeders can co-exist (Gili and Coma 1998) as observed in Lagos Bay.

The similarity in depth distribution patterns of gorgonian species and the high association of the most abundant species suggest the coexistence of these slow-growth species. The lower coexistence of L. lusitanica with the more abundant species may be due to its lower abundance in Lagos Bay being absent in a high number of samples. In fact, the only case of competition between gorgonians reported for nearby areas concerns the mutual exclusion of Eunicella cavolinii and E. verrucosa in Mediterranean coralligenous habitats (Carpine and Grasshoff 1975). However, until now, E. cavolinii has not been found in the Algarve, and there is no evidence that E. verrucosa distribution is being constrained by competition. It is important to notice that the strong associations found between the gorgonian species that are more representative of Lagos Bay should be addressed with care as competition may take place at lower scales (<5 m).

Concerning the gorgonian assemblage composition, four species are well represented in the area, with E. labiata being the most abundant and E. verrucosa, E. gazella and L. sarmentosa presenting similar abundance. The mentioned Eunicella species are poorly represented in the Mediterranean, where shallow water gorgonian assemblages are dominated by Paramuricea clavata, E. singularis and L. sarmentosa (e.g. Ballesteros 2006; Gori et al. 2010). However, the abundance of each dominant species in the Mediterranean is clearly associated with habitat characteristics such as vertical facies, soft bottoms, maerl, pebbles and rocks (Gori et al. 2010), suggesting different ecological requirements. On the contrary, in Lagos Bay, the distributions of the dominant gorgonian species were all well correlated (species occurring at the same sites) suggesting that the rocky areas are relatively homogeneous with respect to available niches for several gorgonian species. However, because the study was restricted to rocky areas, the environmental gradients in several topographic and environmental factors that can affect the distribution of gorgonians are relatively short, minimizing the influence of those factors in the distribution of some species.

The most frequent and abundant species found, E. labiata, is relatively common in coralligenous habitats near the Strait of Gibraltar (González 1993), but to the authors’ best knowledge, this species has only been reported recently for the Algarve coast (Gonçalves et al. 2007; Vieira 2008), probably resulting from erroneous identifications in the past. Another recent study also reported its occurrence in the Professor Luiz Saldanha Marine Park (Arrábida, Center Portugal) (Rodrigues 2008), where it was frequent but not dominant. Another abundant Eunicella species in Lagos Bay, E. verrucosa has been described as an Atlantic species with a wide vertical range. In the current study, this species was found from 8 to 27 m, which agrees with data from the Strait of Gibraltar, where it occurs from 6 to 87 m (González 1993). However, in the Mediterranean, this species is only found at deeper waters (35–200 m) because of the competition with E. cavolinii, which occurs mainly between 10 and 30 m (Carpine and Grasshoff 1975). The wider bathymetric range observed both in Lagos Bay and the Strait of Gibraltar may be due to the lack of competitive exclusion by E. cavolinii, which was not observed in both areas but is common in the Mediterranean. The other species dominating the assemblages in Lagos Bay, E. gazella, presented a distribution positively correlated to that of E. verrucosa, which once more is in agreement with the findings by González (1993) in the Strait of Gibraltar, where they are also commonly found together.

The dominance of L. sarmentosa in the study area may be related to the presence of sediment particles in the rocky bottom. Indeed, this species is clearly associated with areas with frequent but moderate disturbance, where sediment re-suspension is high (Gori et al. 2010), and has been pointed as an indicator of silt (Weinberg 1978; reported as Leptogorgia ceratophita). Although it has been reported to inhabit different substrates, namely rocky areas, shells on biodetritic sediments and sandy muddy areas (González 1993), it shows a high correlation with soft bottoms or surfaces where sediments tend to accumulate (Gori et al. 2010). The preferential distribution of L. sarmentosa within areas of high sedimentation rates may be related to its feeding requirements, as it is known that re-suspended particles are particularly important for this species’ diet (Ribes et al. 2003; Rossi et al. 2004). According to our observations, sediment transport (bed load) is high in the Lagos Bay area, probably because this area is near the Rio Arade estuary, Ria de Alvor (coastal lagoon) and Ribeira de Bensafrim (creek). The habitat conditions in Lagos Bay clearly favour this species as the area is mainly characterized by low relief rocky plateaus with a thick layer of fine sediments that are easily re-suspended (submerged rock bottoms). In the Mediterranean, this species is abundant in sheltered areas with turbulent circulation but without strong near-bottom currents (Gori et al. 2010). Regarding L. lusitanica, even though its ecological requirements are still poorly understood, it has been described as preferring habitats with weak to moderate hydrodynamics but clear waters (González 1993). In fact, in other areas of the Algarve coast where sedimentation and turbidity is lower, this species presents higher abundance at similar depths (e.g. Pedra da Greta and Pedra do Barril, authors’ unpublished data).

The low abundance and frequency of occurrence of E. singularis was already expected, as it is a Mediterranean species with limited distribution outside this area. This species is one of the dominant taxa in the coralligenous communities in the Mediterranean Sea (Ballesteros 2006; Gori et al. 2010) and dominant in light-rich areas (photophilic communities) where it can be found on horizontal or slightly sloped surfaces, having a marked dependence on light. Indeed, this is the only gorgonian species in the Mediterranean area presenting zooxanthellae, but has been reported from 6 to 67 m. The preferential habitat described for this species is frequent in the study area, but the species was rarely found in Lagos Bay. We hypothesize that the colonies found in the study area are colonizers from Mediterranean populations that under favourable conditions were able to reach and settle in suitable rocky areas of the Algarve coast.

The gorgonian community in Lagos Bay is co-dominated by different species contrasting greatly to what has been reported from the Mediterranean characterized by mono-specific communities. This co-dominance extends beyond the depth limits explored in this study, as recent surveys suggest that gorgonian fauna is abundant and diverse in the south Portugal continental shelf (JG, unpublished data). Studies dealing with gorgonian species distribution on the Mediterranean rarely focused on comparative studies, probably because communities are so strongly dominated by the typical Mediterranean species P. clavata, E. singularis and L. sarmentosa. The distribution of these species with small overlap due to different habitat requirements and traits (Gori et al. 2010) probably reflects their evolutionary history. The distribution of weaker competitors may be constrained due to density-dependent traits leading to the high dominance by locally adapted species. On the other hand, in Lagos Bay, the co-dominance of several gorgonian species of different origin may reflect not only the confluence of recruits to the area promoted by physical factors but also the complex interactions between species that enhance coexistence. Multi-species coexistence (gorgonians and sponges, in the present study) may be encouraged by neighbourhood interactions (http://www.rensub.com) and local dispersal which increase intra-specific competition relative to inter-specific (Tilman 1994). What is more, gorgonians facilitate the colonization of other species (Bruno et al. 2003; Idjadi and Edmunds 2006; Thomsen et al. 2010) promoting biodiversity, biomass increase and ecological complexity. Reciprocal facilitation can enhance the positive effects and the persistence of foundation species in marine benthic communities (Bozec et al. 2012) with relevance on ecosystem functioning and conservation (Halpern et al. 2007).

Final remarks

The present study provides invaluable information on the spatial and depth distribution of gorgonian species in shallow rocky bottoms near the westernmost part of continental Europe. The key role of gorgonians in the infralittoral rocky communities poses another challenge, the capacity of these animals to cope with both thermal stress but also pathogens under a climate change scenario, an important issue for the future management of coastal marine ecosystems. The present data are also relevant for the establishment and management of future MPAs in southern Portugal, a common management tool in several areas of the world, namely in the Mediterranean, where gorgonians are used as ecological indicators. What is more, “coral gardens”, including gorgonian dominated biocenoses in south Portugal and Spain have been recently proposed for the OSPAR (Convention for the Protection of the marine Environment of the North-East Atlantic) list of protected habitats (Anonymous 2011). Therefore, reference data like the one provided by this study may be relevant for future monitoring programmes. In Lagos Bay, the abundance of all gorgonian species increases with depth, showing a strong association to another suspension feeding benthic taxa, the sponges (Porifera). The specific ecological requirements regarding space and food of the two taxonomical groups probably present low overlap, thus competition levels shall be low. However, at shallower depths, gorgonians seem to be out-competed by algae for space, even though the upper limit in the distribution of gorgonians in Lagos Bay is probably mostly related to abiotic factors such as high water movement. Further multidisciplinary studies, with broader spatial and temporal scales but also wider depth ranges, supported by modern technology (e.g. ROVs and remote sensors) should be undertaken in order to elucidate on the abiotic and biotic factors that might be affecting the distribution of these octocorals in the Algarve coast.

References

  1. Almeida LP, Ferreira Ó, Pacheco A (2011) Thresholds for morphological changes on an exposed sandy beach as a function of wave height. Earth Surf Proc Land 36(4):523–532. doi:10.1002/esp.2072

    Article  Google Scholar 

  2. Anderson MJ, Ellingsen KE, McArdle BH (2006) Multivariate dispersion as a measure of beta diversity. Ecol Lett 9(6):683–693. doi:10.1111/j.1461-0248.2006.00926.x

    PubMed  Article  Google Scholar 

  3. Anonymous (2011) OSPAR workshop on the improvement of the definitions of habitats on the OSPAR list. background document for discussion: “coral gardens”, “deep sea sponge aggregations” and “seapen and burrowing megafauna communities”. Tech. rep., OCEANA, http://eu.oceana.org/en/eu/media-reports/publications/ospar-workshop-on-the-improvement-of-the-definitions-of-habitats-on-the-ospar-list, 20–21 October 2011, Bergen, Norway

  4. Ballesteros E (2006) Mediterranean coralligenous assemblages: a synthesis of present knowledge. Oceanogr MarBiol Ann Rev 44:123–195

    Google Scholar 

  5. Baus E, Darrock DJ, Bruford MW (2005) Gene-flow patterns in Atlantic and Mediterranean populations of the Lusitanian sea star Asterina gibbosa. Mol Ecol 14:3373–3382. doi:10.1111/j.1365-294X.2005.02681.x

    PubMed  Article  CAS  Google Scholar 

  6. Bavestrello G, Cerrano C, Zanzi D, Cattaneo-Vietti R (1997) Damage by fishing activities to the gorgonian coral Paramuricea clavata in the Ligurian Sea. Aquat Conserv Mar Freshw Ecosyst 7(3):253–262. doi:10.1002/(SICI)1099-0755(199709)7:3<253::AID-AQC243>3.0.CO;2-1

  7. Benedetti-Cecchi L, Bertocci I, Micheli F, Maggi E, Fosella T, Vaselli S (2003) Implications of spatial heterogeneity for management of marine protected areas (MPAs): examples from assemblages of rocky coasts in the northwest Mediterranean. Mar Environ Res 55(5):429–458. doi:10.1016/S0141-1136(02)00310-0

    PubMed  Article  CAS  Google Scholar 

  8. Bozec YM, Yakob L, Bejarano S, Mumby PJ (2012) Reciprocal facilitation and non-linearity maintain habitat engineering on coral reefs. Oikos. doi:10.1111/j.1600-0706.2012.20576.x (in publication)

  9. Bramanti L, Iannelli M, Santangelo G (2009) Mathematical modelling for conservation and management of gorgonians corals: youngs and olds, could they coexist. Ecol Model 220(21):2851–2856. doi:10.1016/j.ecolmodel.2009.01.031

    Article  Google Scholar 

  10. Bruno JF, Stachowicz JJ, Bertness MD (2003) Inclusion of facilitation into ecological theory. Trends Ecol Evol 18(3):119–125

    Article  Google Scholar 

  11. Carpine C, Grasshoff M (1975) Les gorgonaires de la Méditerranée. Bull Inst Océanogr Monaco 71(1430):140, 62 fig., 1 pl

    Google Scholar 

  12. Carvalho S, Cunha MR, Pereira F, Pousão-Ferreira P, Santos MN, Gaspar MB (2011) The effect of depth and sediment type on the spatial distribution of shallow soft-bottom amphipods along the southern Portuguese coast. Helgol Mar Res. doi:10.1007/s10152-011-0285-9

  13. Cerrano C, Bavestrello G (2008) Medium-term effects of die-off of rocky benthos in the Ligurian Sea. What can we learn from gorgonians? Chem Ecol 24(Supplement 1):73–82. doi:10.1080/02757540801979648

    Article  Google Scholar 

  14. Cerrano C, Danovaro R, Gambi C, Pusceddu A, Riva A, Schiaparelli S (2009) Gold coral (Savalia savaglia) and gorgonian forests enhance benthic biodiversity and ecosystem functioning in the mesophotic zone. Biodivers Conserv 19(1):153–167. doi:10.1007/s10531-009-9712-5

    Article  Google Scholar 

  15. Cherubin L, Carton X, Paillet J, Morel Y, Serpette A (2000) Instability of the Mediterranean Water undercurrents southwest of Portugal: effects of baroclinicity and of topography. Oceanol Acta 23(5):551–573. doi:10.1016/S0399-1784(00)01105-1

    Article  Google Scholar 

  16. Chiappone M, Dienes H, W DS, Miller SL (2005) Impacts of lost fishing gear on coral reef sessile invertebrates in the Florida Keys National Marine Sanctuary. Biol Cons 121:221–230. doi:10.1016/j.biocon.2004.04.023

    Google Scholar 

  17. Coelho HS, Neves RJJ, White M, ao PCL, Santos AJ (2002) A model for ocean circulation on the Iberian coast. J Mar Syst 32(1-3):153–179. doi:10.1016/S0924-7963(02)00032-5

  18. Coma R, Pola E, Ribes M, Zabala M (2004) Long-term assessment of temperate octocoral mortality patterns, protected vs. unprotected areas. Ecol Appl 14(5):1466–1478. doi:10.1890/03-5176

    Article  Google Scholar 

  19. Coma R, Linares C, Ribes M, Díaz D, Garrabou J, Ballesteros E (2006) Consequences of a mass mortality in populations of Eunicella singularis (Cnidaria: Octocorallia) in Menorca (NW Mediterranean). Mar Ecol Prog Ser 327:51–60. doi:10.3354/meps327051

    Article  Google Scholar 

  20. Costello C, Rassweiler A, Siegel D, Leo GD, Micheli F, Rosenberg A (2010) The value of spatial information in MPA network design. Proc Natl Acad Sci USA 107(43):18,294–18,299. doi:10.1073/pnas.0908057107

    Article  CAS  Google Scholar 

  21. Cupido R, Cocito S, Sgorbini S, Bordone A, Santangelo G (2008) Response of a gorgonian (Paramuricea clavata) population to mortality events: recovery or loss. Aquat Conserv Mar Freshw Ecosyst 18(6):984–992. doi:10.1002/aqc.904

    Article  Google Scholar 

  22. Dahlgren EJ (1989) Gorgonian community structure and reef zonation patterns on Yucatan coral reefs. Bull Mar Sci 45(3):678–696

    Google Scholar 

  23. Dolbeth M, Óscar Ferreira, Teixeira H, Marques JC, Dias JA, Pardal MA (2007) Beach morphodynamic impact on a macrobenthic community along a subtidal depth gradient. Mar Ecol Prog Ser 352:113–124. doi:10.3354/meps07040

    Article  Google Scholar 

  24. Dufrêne M, Legendre P (1997) Species assemblages and indicator species:the need for a flexible asymmetrical approach. Ecol Monograph 67(3):345–366. doi:10.1890/0012-9615(1997)067[0345:SAAIST]2.0.CO;2

    Google Scholar 

  25. García-Charton JA, Pérez-Ruzafa A, Marcos C, Claudet J, Badalamenti F, Benedetti-Cecchi L, Falcón JM, Milazzo M, Schembri PJ, Stobart B, Vandeperre F, Brito A, Chemello R, Dimech M, Domenici P, Guala I, Diréach LL, Maggi E, Planes S (2008) Effectiveness of European Atlanto-Mediterranean MPAs: do they accomplish the expected effects on populations, communities and ecosystems. J Nat Conserv 16(4):193–221. doi:10.1016/j.jnc.2008.09.007

    Article  Google Scholar 

  26. Garrabou J, Ballesteros E, Zabala M (2002) Structure and dynamics of North-western Mediterranean rocky benthic communities along a depth gradient. Estuar Coast Shelf S 55:493–508. doi:10.1006/ecss.2001.0920

    Article  Google Scholar 

  27. Garrabou J, Coma R, Bensoussan N, Bally M, Chevaldonn P, Cigliano M, Díaz D, Harmelin JG, Gambi MC, Kersting DK, Ledoux JB, Lejeusne C, Linares C, Marschal C, Pérez T, Ribes M, Romano JC, Serrano E, Teixido N, Torrents O (2009) Mass mortality in Northwestern Mediterranean rocky benthic communities: effects of the 2003 heat wave. Global Change Biol 15(5):1090–1103. doi:10.1111/j.1365-2486.2008.01823.x

    Article  Google Scholar 

  28. Gili J, Coma R (1998) Benthic suspension feeders: their paramount role in littoral marine food webs. Trends Ecol Evol 13(8):316–321. doi:10.1016/S0169-5347(98)01365-2

    PubMed  Article  CAS  Google Scholar 

  29. Gili J, Murillo J, Ros J (1989) The distribution pattern of benthic Cnidarians in the Western Mediterranean. Sci Mar 53:19–35

    Google Scholar 

  30. Gonçalves JMS, Monteiro P, Coelho R, Afonso CML, Almeida C, Veiga P, Machado M, Machado D, Oliveira F, Ribeiro J, Abecasis D, Primo L, Tavares D, Fernández-Carvalho J, Abreu S, Fonseca L, Erzini K, Bentes L (2007) Cartography and characterization of the marine communities off the national underwater ecological reserve between Galé and Ancão. Final report, CCDR Algarve, Faro, 242 pp. + Annexes (In portuguese)

  31. Gonçalves JMS, Monteiro P, Afonso CML, Oliveira F, Rangel M, Machado M, Veiga P, Leite L, Sousa I, Bentes L, Fonseca L, Erzini K (2010) Cartography and characterization of the marine communities off the national underwater ecological reserve between the Arade river and Ponta da Piedade. Final report, ARH Algarve, Faro, 122 pp. + Annexes. http://fcma.ualg.pt/cfrg/documents/RenIV_NET.pdf

  32. González PJL (1993) Taxonomia y zoogeografia de los antozoos del Estrecho de Gibraltar y areas proximas. PhD thesis, Universidad Sevilla

  33. Gori A, Rossi S, Berganzo E, Pretus J, Dale M, Gili J (2010) Spatial distribution patterns of the gorgonians Eunicella singularis, Paramuricea clavata, and Leptogorgia sarmentosa (Cape of Creus, Northwestern Mediterranean Sea). Mar Biol 151(4):1–16. doi:10.1007/s00227-010-1548-8

    Google Scholar 

  34. Grasshoff M (1988) The genus Leptogorgia (Octocorallia: Gorgoniidae) in West Africa. Atlantide Rep14:91–147

    Google Scholar 

  35. Grasshoff M (1992) Die flachwasser-gorgonarien von Europa und Westafrika (Cnidaria, Anthozoa). Courier Forschunginstitut Senckenberg 149:1–135

    Google Scholar 

  36. Halpern BS, Silliman BR, Olden JD, Bruno JP, Bertness MD (2007) Incorporating positive interactions in aquatic restoration and conservation. Front Ecol Environ 5(3):153–160

    Article  Google Scholar 

  37. Idjadi JA, Edmunds PJ (2006) Scleractinian corals as facilitators for other invertebrates on a Caribbean reef. Mar Ecol Prog Ser 319:117–127. doi:10.3354/meps319117

    Article  Google Scholar 

  38. Janson S, Vegelius J (1981) Measures of ecological association. Oecologia 49:371–376. doi:10.1007/BF00347601

    Article  Google Scholar 

  39. Levy A, Wirtz P, Floeter SR, Almada VC (2011) The Lusitania Province as a center of diversification: the phylogeny of the genus Microlipophrys (Pisces: Blenniidae). Mol Phylogenet Evol 58(2):409–413. doi:10.1016/j.ympev.2010.12.008

    PubMed  Article  CAS  Google Scholar 

  40. Linares C, Coma R, Díaz D, Zabala M, Hereu B, Dantart L (2005) Immediate and delayed effects of a mass mortality event on gorgonian population dynamics and benthic community structure in the NW Mediterranean Sea. Mar Ecol Prog Ser 305:127–137. doi:10.3354/meps305127

    Article  Google Scholar 

  41. Linares C, Doak DF, Coma R, Díaz D, Zabala M (2007) Life history and viability of a long-lived marine invertebrate: the octocoral Paramuricea clavata. Ecology 88(4):918–928. doi:10.1890/05-1931

    PubMed  Article  Google Scholar 

  42. Linares C, Coma R, Garrabou J, Díaz D, Zabala M (2008) Size distribution, density and disturbance in two Mediterranean gorgonians: Paramuricea clavata and Eunicella singularis. J Appl Ecol 45:688–699. doi:10.1111/j.1365-2664.2007.01419.x

    Article  Google Scholar 

  43. Linares C, Coma R, Zabala M (2008) Restoration of threatened red gorgonian populations: An experimental and modelling approach. Biol Cons 141(2):427–437. doi:10.1016/j.biocon.2007.10.012

    Article  Google Scholar 

  44. Martins CS, Hamann M, Fiúza AFG (2002) Surface circulation in the eastern North Atlantic, from drifters and altimetry. J Geophys Res 107:3217–3228. doi:200210.1029/2000JC000345

    Article  Google Scholar 

  45. McArthur M, Brooke B, Przeslawski R, Ryan D, Lucieer V, Nichol S, McCallum A, Mellin C, Cresswell I, Radke L (2010) On the use of abiotic surrogates to describe marine benthic biodiversity. Estuar Coast Shelf S 88(1):21–32. doi:10.1016/j.ecss.2010.03.003

    Article  Google Scholar 

  46. Munzel U, Hothorn LA (2001) A unified approach to simultaneous rank test procedures in the unbalanced one-waylayout. Biometrical J 43(5):553–569. doi:10.1002/1521-4036(200109)43:5<553::AID-BIMJ553>3.0.CO;2-N

    Google Scholar 

  47. Norling P, Kautsky N (2007) Structural and functional effects of Mytilus edulis on diversity of associated species and ecosystem functioning. Mar Ecol Prog Ser 351:163–175. doi:10.3354/meps07033

    Article  Google Scholar 

  48. Pérez FF, Castro CG, Álvarez-Salgado XA, Ríos AF (2001) Coupling between the iberian basin—scale circulation and the Portugal boundary current system: a chemical study. Deep-Sea Res Pt I 48(6):1519–1533. doi:10.1016/S0967-0637(00)00101-1

    Article  Google Scholar 

  49. R Development Core Team (2010) R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria, url http://www.R-project.org, ISBN 3-900051-07-0

  50. Ribes M, Coma R, Rossi S (2003) Natural feeding of the temperate asymbiotic octocoral-gorgonian Leptogorgia sarmentosa (Cnidaria: Octocorallia). Mar Ecol Prog Ser 254:141–150. doi:10.3354/meps254141

    Article  CAS  Google Scholar 

  51. Riisgård HU, Larsen PS (2010) Particle capture mechanisms in suspension-feeding invertebrates. Mar Ecol Prog Ser 418:255–293. doi:10.3354/meps08755

    Article  Google Scholar 

  52. Rodrigues SCM (2008) Dados ecológicos de gorgónias (octocorallia: Alcyonacea) - contributo para a conservação e gestão de actividades subaquáticas no parque marinho professor Luiz Saldanha (Portugal). Master’s thesis, Universidade de Lisboa

  53. Rossi S, Ribes M, Coma R, Gili J (2004) Temporal variability in zooplankton prey capture rate of the passive suspension feeder L. sarmentosa (Cnidaria: Octocorallia), a case study. Mar Biol 144(1):89–99. doi:10.1007/s00227-003-1168-7

    Article  Google Scholar 

  54. Ruppert EE, Barnes RD (1994) Invertebrate zoology, 6th edn. Saunders College Publishing, New York

    Google Scholar 

  55. Sánchez JA, Zea S, Diáz JM (1998) Patterns of octocoral and black coral distribution in the oceanic barrier reef-complex of Providencia Island, southwestern Caribbean. Caribbean J Sci 34(3–4):250–264

    Google Scholar 

  56. Sánchez RF, Relvas P, Delgado M (2007) Coupled ocean wind and sea surface temperature patterns off the western Iberian Peninsula. J Mar Syst 68(1–2):103–127. doi:10.1016/j.jmarsys.2006.11.003

    Article  Google Scholar 

  57. Souto J, Reverter-Gil O, Fernández-Pulpeiro E (2010) Gymnolaemate bryozoans from the Algarve (southern Portugal): new species and biogeographical considerations. J Mar Biol Assoc UK 90(7):1417–1439. doi:10.1017/S0025315409991640

    Article  Google Scholar 

  58. Spalding MD, Fox HE, Allen GR, Davidson N, na ZAF, Finlayson M, Halpern BS, Jorge MA, Lombana A, Lourie SA, Martin KD, McManus E, Molnar J, Recchia CA, Robertson J (2007) Marine ecoregions of the world: a bioregionalization of coastal and shelf areas. Bioscience 57(7):573–583. doi:10.1126/science.1067728

  59. Thomsen MS, Wernberg T, Altieri A, Tuya F, Gulbransen D, McGlathery KJ, Holmer M, Silliman BR (2010) Habitat cascades: the conceptual context and global relevance of facilitation cascades via habitat formation and modification. Integr Comp Biol 50(2):158–175. doi:10.1093/icb/icq042

    PubMed  Article  Google Scholar 

  60. Tilman D (1994) Competition and biodiversity in spatially structured habitats. Ecology 75(1):2–16

    Article  Google Scholar 

  61. Vieira P (2008) Caracterização de espécies de gorgónias (Cnidaria; Gorgonacea) da costa Algarvia. Master’s thesis, Universidade do Algarve

  62. Weinberg S (1978) Mediterranean octocorallian communities and the abiotic environment. Mar Biol 49(1):41–57. doi:10.1007/BF00390729

    Article  Google Scholar 

  63. Wright JR, Jones CG (2006) The concept of organisms as ecosystem engineers ten years on: progress, limitations, and challenges. Bioscience 56(3):203–210. doi:10.1641/0006-3568(2006)056[0203:TCOOAE]2.0.CO;2

    Google Scholar 

  64. Yoshioka PM, Yoshioka BB (1989) Effects of wave energy, topographic relief and sediment transport on the distribution of shallow-water gorgonians of Puerto Rico. Coral Reefs 8:145–152. doi:10.1007/BF00338270

    Article  Google Scholar 

  65. Zabala M, Ballesteros E (1989) Surface-dependent strategies ane energy flux in benthic marine communities or, why corals do not exist in the mediterranean. Sci Mar 53(1):3–17

    Google Scholar 

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Acknowledgements

J.C. (SFRH/BD/29491/2006) benefits from a PhD grant awarded by “Fundação para a Ciência e a Tecnologia” (FCT)’. The authors would like to acknowledge the contribution of two anonymous reviewers that substantially improved this paper. The authors also acknowledge Pedro Veiga for providing some of the underwater photographs used in this publication. This study was performed in the framework of the research project Rensub (http://www.rensub.com), funded by ARH Algarve and POVT.

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  1. Instituto Português do Mar e da Atmosfera (IPMA), Av. 5 Outubro, s/n, 8700–305, Olhão, Portugal

    João Cúrdia & Miguel N. Santos

  2. Centre of Marine Sciences (CCMAR/CIMAR), Universidade do Algarve, Campus de Gambelas, 8005–139, Faro, Portugal

    Pedro Monteiro, Carlos M. L. Afonso & Jorge M. S. Gonçalves

  3. CESAM & Departamento de Biologia, Universidade de Aveiro, Campus Universitário de Santiago, 3810–193, Aveiro, Portugal

    João Cúrdia & Marina R. Cunha

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Cúrdia, J., Monteiro, P., Afonso, C.M.L. et al. Spatial and depth-associated distribution patterns of shallow gorgonians in the Algarve coast (Portugal, NE Atlantic). Helgol Mar Res 67, 521–534 (2013). https://doi.org/10.1007/s10152-012-0340-1

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Keywords

  • Gorgonians
  • Leptogorgia
  • Eunicella
  • Spatial distribution
  • Rocky bottoms
  • Biological interactions

Helgoland Marine Research

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