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<article article-type="research-article" dtd-version="3.0" xml:lang="en" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">
	<front>
		<journal-meta>
			<journal-id journal-id-type="publisher-id">SCIENTIA MARINA</journal-id>
			<journal-title-group>
				<journal-title>Scientia Marina</journal-title>
				<abbrev-journal-title>Sci Mar</abbrev-journal-title>
			</journal-title-group>
			<issn pub-type="epub">0214-8358</issn>
			<publisher>
				<publisher-name>Consejo Superior de Investigaciones Científicas</publisher-name>
			</publisher>
		</journal-meta>
		<article-meta>
			 <article-id pub-id-type="publisher-id">sm4239</article-id>
			 <article-id pub-id-type="doi">10.3989/scimar.04239.08B</article-id>
			 
			
		<title-group>
			  <article-title>Epiphytic flora on <italic>Gelidium corneum</italic> (Rhodophyta: Gelidiales) in relation to wave exposure and depth</article-title>
		<trans-title-group xml:lang="es">
		<trans-title>Flora epífita de <italic>Gelidium corneum</italic> (Rhodophyta: Gelidiales) en relación a la exposición al oleaje y la profundidad</trans-title>
		</trans-title-group>
		<alt-title alt-title-type="running-head">Epiphytes on <italic>G. corneum</italic> in relation to wave exposure and depth</alt-title>
		</title-group>
		
		<contrib-group>
			  <contrib contrib-type="author" corresp="yes"> 
				<name>
				 <surname> Quintano</surname>
				 <given-names>Endika</given-names>
				</name>
				<xref ref-type="aff" rid="U1"/>
				<xref ref-type="corresp" rid="cor1"/>
			  </contrib>
			  <contrib contrib-type="author" corresp="no"> 
				<name>
				 <surname>Díez</surname>
				 <given-names>Isabel</given-names>
				</name>
				<xref ref-type="aff" rid="U1"/>
			  </contrib>
			  <contrib contrib-type="author" corresp="no"> 
				<name>
				 <surname>Muguerza</surname>
				 <given-names>Nahiara</given-names>
				</name>
				<xref ref-type="aff" rid="U1"/>
			  </contrib>
			  <contrib contrib-type="author" corresp="no"> 
				<name>
				 <surname>Santolaria</surname>
				 <given-names>Alberto</given-names>
				</name>
				<xref ref-type="aff" rid="U1"/>
			  </contrib>
			  <contrib contrib-type="author" corresp="no"> 
				<name>
				 <surname>Gorostiaga</surname>
				 <given-names>José María</given-names>
				</name>
				<xref ref-type="aff" rid="U1"/>
			  </contrib>
			  <aff id="U1">Department of Plant Biology and Ecology, Faculty of Science and Technology, University of the Basque Country UPV/EHU, PO Box 644, E-48080 Bilbao, Spain.</aff>
			 </contrib-group>
			 
			 <author-notes>
		<corresp id="cor1">e-mail: <email xlink:href="endika.quintano@ehu.es">endika.quintano@ehu.es</email>
		</corresp>
		</author-notes>
		
<pub-date pub-type="epub">
		<day>30</day>
		<month>12</month>
		<year>2015</year>
		</pub-date>
		<pub-date pub-type="collection">
		<year>2015</year>
		</pub-date>
		
		<volume>79</volume>
		<issue>4</issue>
		<fpage>479</fpage>
		<lpage>486</lpage>
		
		<elocation-id content-type="doi">10.3989/scimar.04239.08B</elocation-id>

		 <history>
		  	<date date-type="received">
				<day>13</day>
				<month>3</month>
				<year>2015</year>
			</date>
			<date date-type="accepted">
				<day>13</day>
				<month>7</month>
				<year>2015</year>
			</date>
			<date date-type="published">
				<day>9</day>
				<month>10</month>
				<year>2015</year>
			</date>
		 </history>
		 
		<permissions>
		<copyright-statement>&#x00A9; 2015 CSIC</copyright-statement>
		<copyright-year>2015</copyright-year>
		<license license-type="open-access" xlink:href="http://creativecommons.org/licenses/by-nc/3.0/">
		<license-p>This is an open-access article distributed under the Creative Commons Attribution-Non Commercial Lisence (by-nc) Spain 3.0.</license-p>
		</license>
		</permissions>
		
		<abstract xml:lang="en">
		<title>SUMMARY</title>
		<p>The canopy-forming macroalga <italic>Gelidium corneum</italic> (Hudson) J.V. Lamouroux plays a major role in the functioning of the subtidal ecosystem of the Cantabrian Sea (northern Spain). Despite its importance, little is known about the factors that may potentially affect the distribution pattern of its epiphytic flora. Here we examine two indirect factors: coastal orientation (N and NW) and depth (3 and 7 m), as proxies for wave exposure and light availability, respectively. We test their effects on the total epiphytic load, alpha diversity (species richness, Shannon, Simpson and evenness measures) and multivariate structure of the epiphytic flora growing on <italic>G. corneum</italic> in subtidal waters off the Basque coast. <italic>Plocamium cartilagineum</italic>, <italic>Dictyota dichotoma</italic> and <italic>Acrosorium ciliolatum</italic> were found to be the most common epiphytes. Significant interactive effect of coastal orientation and depth were observed for species composition and abundance of epiphytic flora. Increased wave exposure resulted in a lower epiphyte load and a less diverse community, suggesting that under high hydrodynamic conditions epiphytes were more likely to become dislodged from hosts. However, light availability only had a significant effect on the distribution of epiphytes below a certain threshold of wave action, with the epiphytic load being 30-40% greater on shallow bottoms. </p>
		</abstract>
		<trans-abstract xml:lang="es">
		<title>RESUMEN</title>
		<p>El alga formadora de copa <italic>Gelidium corneum</italic> (Hudson) J.V. Lamouroux tiene un papel fundamental en el funcionamiento de los ecosistemas submareales del mar Cantábrico (norte de España). A pesar de su importancia, se sabe poco sobre los factores que afectan a la distribución de su flora epífita. En este estudio, examinamos dos factores indirectos: la orientación de la costa (N y NO) y la profundidad (3 y 7 m), como factores representativos de la exposición al oleaje y la disponibilidad de luz, respectivamente. Este estudio testa sus efectos sobre la carga total de epífitos, la alfa-diversidad (riqueza de especies, Shannon, Simpson y equitatividad) y la estructura multivariable de la flora epífita que crece sobre <italic>G. corneum</italic> en las aguas submareales de la costa vasca. Los epífitos más comunes fueron <italic>Plocamium cartilagineum</italic>, <italic>Dictyota dichotoma</italic> y <italic>Acrosorium ciliolatum</italic>. Se observó un efecto interactivo de la orientación de la costa y la profundidad para la composición de especies y la abundancia de la flora epífita. En las localidades con mayor exposición al oleaje la carga epífita era menor y la comunidad menos diversa, sugiriendo que bajo condiciones de un elevado hidrodinamismo los epífitos eran más susceptibles de ser desprendidos de su hospedador. Sin embargo, la disponibilidad de luz solo tuvo un efecto significativo en la distribución de los epífitos por debajo de ciertos umbrales de la acción del oleaje, siendo la carga de epifitos un 30-40% mayor en los fondos someros.</p>
		</trans-abstract>
		<kwd-group xml:lang="en">
			<title>KEYWORDS</title>
			<kwd>epibionts</kwd>
			<kwd>host frond</kwd>
			<kwd>light availability</kwd>
			<kwd>spatial variability</kwd>
			<kwd>macroalgae</kwd>
			<kwd>wave action</kwd>			
		</kwd-group>
		<kwd-group xml:lang="es">
			<title>PALABRAS CLAVE</title>
			<kwd>acción del oleaje</kwd>
			<kwd>disponibilidad de luz</kwd>
			<kwd>epibiontes</kwd>
			<kwd>fronde hospedador</kwd>
			<kwd>macroalgas</kwd>
			<kwd>variabilidad espacial</kwd>
		</kwd-group>
	 </article-meta>
	</front>
			<body>
<sec id="S1">
<title>INTRODUCTION</title>
			
			<p>Epiphytism is a widespread strategy in marine benthic communities on rocky bottoms where the competition for space is high (<xref ref-type="bibr" rid="CIT43">Rindi and Guiry 2004</xref>, <xref ref-type="bibr" rid="CIT05">Belegratis et al. 1999</xref>). Macroalgae provide an ideal primary substratum for the growth of epiphytic algae (<xref ref-type="bibr" rid="CIT28">Lutz et al. 2010</xref>), which significantly contribute to primary productivity (<xref ref-type="bibr" rid="CIT05">Belegratis et al. 1999</xref>) and, in turn, provide habitat for other organisms (<xref ref-type="bibr" rid="CIT22">Karez et al. 2000</xref>). Epiphytism entails both benefits and disadvantages for the host plant (<xref ref-type="bibr" rid="CIT49">Wahl 1989</xref>). In general, the detrimental effects of epiphytes are indirect (<xref ref-type="bibr" rid="CIT13">Fricke et al. 2011</xref>). They increase drag on hosts, increasing their risk of breakage and dislodgement, particularly in hydrodynamically stressful environments (<xref ref-type="bibr" rid="CIT02">Anderson and Martone 2014</xref>). Furthermore, growth rates and reproductive output of heavily epiphytized hosts may decrease as a result of the reduction in irradiance reaching the frond (<xref ref-type="bibr" rid="CIT45">Sand-Jensen 1977</xref>) and the partial nutrient depletion of water after its passage through the epiphytic layer (<xref ref-type="bibr" rid="CIT33">Muñoz et al. 1991</xref>). Favourable consequences of epiphytism have also been postulated, including herbivore avoidance and protection against desiccation for intertidal hosts (<xref ref-type="bibr" rid="CIT02">Anderson and Martone 2014</xref>).</p>
			<p><italic>Gelidium corneum</italic> (Hudson) J.V. Lamouroux (formerly <italic>G. sesquipedale</italic>) is a very important benthic primary producer in the Cantabrian Sea (<xref ref-type="bibr" rid="CIT42">Rico and Fredriksen 1996</xref>, <xref ref-type="bibr" rid="CIT19">Gorostiaga et al. 1998</xref>, <xref ref-type="bibr" rid="CIT11">Díez et al. 2003</xref>) and forms extensive stands at depths down to 9-15 m in the subtidal zone off the Basque coast (<xref ref-type="bibr" rid="CIT18">Gorostiaga 1995</xref>, <xref ref-type="bibr" rid="CIT06">Borja et al. 2004</xref>). This canopy-forming species plays an important ecological role by providing habitat and shelter for many other organisms (<xref ref-type="bibr" rid="CIT06">Borja et al. 2004</xref>, <xref ref-type="bibr" rid="CIT08">Bustamante et al. 2014</xref>). The algae <italic>Dictyota dichotoma</italic>, <italic>Plocamium cartilagineum</italic> and <italic>Asparagopsis armata</italic> (<xref ref-type="bibr" rid="CIT46">Santos 1994</xref>) and the bryozoans <italic>Electra pilosa</italic> and <italic>Scrupocellaria</italic> spp. (<xref ref-type="bibr" rid="CIT08">Bustamante et al. 2014</xref>) have been reported as its main epibionts. The seasonal pattern of <italic>G. corneum</italic> growth substantially influences the development of the epiphytic load. This perennial species with apical growth (about 7-8 cm yr<sup>–1</sup>) reaches its maximum frond elongation rate in late spring and summer (<xref ref-type="bibr" rid="CIT17">Gorostiaga 1994</xref>). Under the high light availability of this period, <italic>G. corneum</italic> forms a dense canopy as a result of the fast process of frond branching, which favours the settlement and growth of epiphytes (<xref ref-type="bibr" rid="CIT17">Gorostiaga 1994</xref>, <xref ref-type="bibr" rid="CIT46">Santos 1994</xref>). In autumn and winter a considerable loss of branches occurs due to the effect of storms, resulting in a decrease in the standing stock of <italic>G. corneum</italic> (<xref ref-type="bibr" rid="CIT17">Gorostiaga 1994</xref>) and in its epiphytic load.</p>
			<p><italic>G. corneum</italic> used to be the main raw material for agar extraction along the Atlantic shores of Spain, Portugal and Morocco, providing these countries with almost 50% of the world harvest in the 1980s (<xref ref-type="bibr" rid="CIT30">McHugh 1991</xref>). In the particular case of the Basque coast, <italic>G. corneum</italic> was only exploited by scuba diving in the 1970s and between 1992 and 1999 (<xref ref-type="bibr" rid="CIT07">Borja et al. 2013</xref>). However, since the turn of the 21<sup>st</sup> century many <italic>G. corneum</italic> beds have suffered a significant decline on several coastal stretches of the Basque coast (<xref ref-type="bibr" rid="CIT12">Díez et al. 2012</xref>, <xref ref-type="bibr" rid="CIT07">Borja et al. 2013</xref>), where this macrophyte exhibits morphological (<xref ref-type="bibr" rid="CIT12">Díez et al. 2012</xref>) and biochemical (<xref ref-type="bibr" rid="CIT41">Quintano et al. 2013</xref>) symptoms of stress. It has been suggested that climate-driven factors such as increased seawater temperature in combination with changes in local factors that include light and nutrients availability and wave energy are involved in the declines of <italic>G. corneum</italic> beds (<xref ref-type="bibr" rid="CIT12">Díez et al. 2012</xref>, <xref ref-type="bibr" rid="CIT07">Borja et al. 2013</xref>). Since epiphytism potentially affects the growth and survival of <italic>G. corneum</italic> and may interact with other stressors, information about factors affecting epiphyte development is valuable. Likewise, epiphyte composition and abundance on <italic>G. corneum</italic> are liable to change according to environmental conditions, and thus this particular flora can play a greater role as a bioindicator (i.e. stress symptoms), as has been reported for other macrophytes (<xref ref-type="bibr" rid="CIT44">Russell et al. 2005</xref>, <xref ref-type="bibr" rid="CIT15">Giovannetti et al. 2010</xref>).</p>
			<p>Wave exposure and irradiance have long been recognized as major factors in regulating the distribution of algae (<xref ref-type="bibr" rid="CIT27">Lüning 1990</xref>). In this regard, epiphyte growth and colonization are generally negatively affected by increased wave energy, whereas increased light favours epiphyte development (<xref ref-type="bibr" rid="CIT31">Michael et al. 2008</xref>). In this study we examine two indirect factors, coastal orientation (north and northwest; N and NW) and depth (3 and 7 m), as proxies for wave exposure and light availability, respectively. We test the effects of these two factors and their interaction on the total epiphytic load, alpha diversity (species richness, Shannon, Simpson and evenness measures) and multivariate structure of the epiphytic flora growing on the red alga <italic>G. corneum</italic> in subtidal waters off the Basque coast. We expected the abundance and diversity of epiphytes to be negatively correlated with wave exposure (higher loads in north facing coastal stretches) and positively correlated with light intensity (higher loads on shallow bottoms).</p>
			
	</sec>
<sec id="S2">
<title>MATERIALS AND METHODS</title>
			
<sec id="S2.1">
<title> Study area</title>
			
		  <p>The Basque coast is situated in the southernmost part of the Bay of Biscay (northern Spain). The study was carried out on the coast of Bizkaia (western Basque coast) (<xref ref-type="fig" rid="F1">Fig. 1</xref>), which is 108 km long (<xref ref-type="bibr" rid="CIT11">Díez et al. 2003</xref>) and is dominated by rocky substrata (<xref ref-type="bibr" rid="CIT09">Chust et al. 2011</xref>). The Basque coast is exposed to large fetches where swell mainly comes from the WNW and NW (<xref ref-type="bibr" rid="CIT16">González et al. 2004</xref>), with mean significant wave heights (Hs) of 1.5 and 2.5 m during summer and winter, respectively (<xref ref-type="bibr" rid="CIT26">Liria et al. 2009</xref>). </p>
		  			<fig id="F1">
				<label>Fig. 1</label>
				<caption>
				<title>Study area. Layout of the six transects along the coast of Bizkaia (western Basque coast). North-facing locations: Armintza (N1); Gaviota (N2); Ondarroa (N3). Northwest facing locations: Bakio (NW1); Cape Ogoño (NW2); Cape Lekeitio (NW3).</title>
				</caption>
				<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="../sm79n4-4239-web-resources/image/sm4239fig1_fmt.jpeg"/>
			</fig>

</sec>
<sec id="S2.2">
<title>Data collection</title>
			
		  <p>As a consequence of the prevailing NW swell in the study area, coastal stretches facing this direction are more exposed than those facing N, which are in turn more exposed than those facing NE. <italic>G. corneum </italic>thrives mainly in exposed (N) to very exposed (NW) coastal stretches (<xref ref-type="bibr" rid="CIT06">Borja et al. 2004</xref>). Therefore, in order to represent two hydrodynamical conditions, three locations were randomly selected with the two coastal orientations where <italic>G. corneum</italic> was present: north (N) and northwest (NW) (<xref ref-type="fig" rid="F1">Fig. 1</xref>). The classification of the sampling locations into two degrees of wave exposure was supported by the type of canopy vegetation found there, which acts as a good indicator of hydrodynamics in the study area (<xref ref-type="bibr" rid="CIT11">Díez et al. 2003</xref>). Bottoms at very exposed locations were dominated by a monospecific canopy of <italic>G. corneum</italic>, whereas in exposed sites <italic>Cystoseira baccata</italic> was co-dominant (<xref ref-type="bibr" rid="CIT11">Díez et al. 2003</xref>). The N-facing locations were Armintza (N1) (43°26’39”N, 2°54’53”W), Gaviota (N2) (43°25’88”N, 2°50’07”W) and Ondarroa (N3) (43°19’80”N, 2°25’28”W). The NW-facing locations were Bakio (NW1) (43°26’74”N, 2°47’33”W), Cape Ogoño (NW2) (43°26’20”N, 2°56’85”W) and Cape Lekeitio (NW3) (43°22’62”N, 2°36’93”W). </p>
			<p>In order to test the influence of light availability on the distribution of epiphytic flora, two depths (3 and 7 m) were selected as representative of two different conditions of light intensity. We assumed depth to be a good proxy for light because we only focused on vegetation growing on reefs with slight to moderate slopes (0-30°), thus avoiding the influence of topography at each sampling depth. These two depths were selected according to <xref ref-type="bibr" rid="CIT11">Díez et al. (2003)</xref> who reported that <italic>G. corneum</italic> stands exhibited the highest coverage up to 8 m depth for our study area. </p>
			<p>The sampling was conducted in summer 2008. At each depth three replicates of 50×50 cm quadrats were randomly sampled. Those <italic>G. corneum</italic> fronds and their epiphytes inside the quadrats were removed by carefully scraping the substrate; fronds were placed in labelled cotton bags and transferred later to the laboratory in wet conditions. </p>
			<p>Once in the laboratory, samples were kept frozen. For the analysis, samples were thawed and the epiphytic flora was separated and identified. Algal taxonomy was updated following AlgaeBase (<xref ref-type="bibr" rid="CIT21">Guiry and Guiry 2014</xref>). Subsequently, the dry weight values (100-110°C, 24 h) were obtained for <italic>G. corneum</italic> and its epiphytes.</p>
			</sec>
<sec id="S2.3">
<title>Statistical analysis</title>
			
		  <p>The surface that could be epiphytized differed in each sample according to the variation in abundance of the host <italic>G. corneum</italic> (<xref ref-type="table" rid="T1">Table 1</xref>). Therefore, a standardization was performed to compare epiphyte abundances from different samples. This was achieved by obtaining the epiphyte/<italic>G. corneum</italic> biomass ratio for every taxon at each sampling unit.</p>
		  	<table-wrap id="T1">
			<label>Table 1</label>
		<caption>
			<title>Biomass of <italic>G. corneum</italic> (mean±se, g dry weight 0.25 m<sup>–2</sup>) in relation to coastal orientation (N, north; NW, northwest), location and depth.</title>
		</caption>
		<table frame="hsides" rules="groups">
  <thead>
		        <tr>
		          <th></th>
		          <th colspan="3">N-facing locations</th>
		          <th colspan="3">NW-facing locations</th>
	            </tr>
		        <tr>
		          <th>(depth)</th>
		          <th>N1</th>
		          <th>N2</th>
		          <th>N3</th>
		          <th>NW1</th>
		          <th>NW2</th>
		          <th>NW3</th>
	            </tr>
	          </thead>
		      <tbody>
		        <tr>
		          <td>3 m</td>
		          <td>5.67±0.26</td>
		          <td>4.65±0.41</td>
		          <td>3.68±0.64</td>
		          <td>24.13±3.67</td>
		          <td>16.75±3.86</td>
		          <td>31.68±2.99</td>
	            </tr>
		        <tr>
		          <td>7 m</td>
		          <td>13.15±1.64</td>
		          <td>15.64±1.12</td>
		          <td>11.49±1.81</td>
		          <td>180.53±18.99</td>
		          <td>60.72±3.75</td>
		          <td>70.32±2.66</td>
	            </tr>
	          </tbody>
	        </table>
	      </table-wrap>
			<p>Univariate and multivariate analyses were conducted using the PERMANOVA+ for PRIMER6 package (<xref ref-type="bibr" rid="CIT03">Anderson et al. 2008</xref>). For each sampling unit, community measures including species richness (S), Shannon diversity (H’, log<sub>e</sub>), Simpson (1-λ) diversity and Pielou J’ evenness were calculated. Spatial differences in community measures and multivariate structure (i.e. quali-quantitative taxa composition) of epiphytic flora on <italic>G. corneum</italic> were tested with an a priori chosen significance level of α=0.05. The experimental design consisted of three factors: coastal orientation (OR; 2 levels, fixed), location (LO; 6 levels, random) and depth (DE; 2 levels, fixed, crossed with coastal orientation and location). Univariate analyses were based on Euclidean distance, whereas multivariate analyses were based on the Bray-Curtis similarity matrix calculated from fourth root transformed data. After relevant terms, post hoc pairwise comparisons were performed using PERMANOVA t statistics and 9999 permutations. Homogeneity within each factor was explored by applying the permutational test for homogeneity of multivariate dispersions (PERMDISP). A principal coordinate analysis (PCO) was conducted to visualize the sample grouping in two-dimensional space and to calculate how much of the variability in taxa composition and abundance was explained by the first two axes. The vectors of the taxa abundances were overlaid onto the PCO using Spearman correlation. The contribution of each epiphytic taxon to the separation of the three groups detected in the pairwise comparisons was examined using the similarity percentage procedure (SIMPER).</p>
			</sec>
		  </sec>
<sec id="S3">
<title>RESULTS</title>
			
		  <p>A total of 12 macroalgae taxa were recorded growing over <italic>G. corneum</italic>, most of them being morphologically simple forms belonging to the Ceramiaceae, Callithamniaceae and Bonnemaisoniaceae families (<xref ref-type="table" rid="T2">Table 2</xref>). The total epiphytes/<italic>G. corneum</italic> biomass ratio was higher at N-facing locations than at NW-facing locations (<xref ref-type="fig" rid="F2">Fig. 2</xref>). However, differences in relation to depth were only found at N-facing locations, with the total epiphytes/<italic>G. corneum</italic> biomass ratio being higher at 3 m depth (<xref ref-type="fig" rid="F2">Fig. 2</xref>). In this regard, univariate PERMANOVA analyses detected a significant interaction between coastal orientation and depth (Pseudo-F<sub>1,4</sub>=42.31, p=0.004). With respect to species richness (<xref ref-type="fig" rid="F3">Fig. 3A</xref>), the number of taxa in N-facing locations was significantly higher than in NW-facing locations (Pseudo-F<sub>1,4</sub>=18.89, p=0.013). Diversity also differed from one coastal orientation to the other. Both Shannon (<xref ref-type="fig" rid="F3">Fig. 3B</xref>) and Simpson (<xref ref-type="fig" rid="F3">Fig. 3C</xref>) diversities were significantly higher at N-facing locations (Pseudo-F<sub>1,4</sub>=87.43, p=0.001 and Pseudo-F<sub>1,4</sub>=96.09, p=0.001, respectively). Finally, Pielou J’ evenness (<xref ref-type="fig" rid="F3">Fig. 3D</xref>) was also higher at N-facing locations (Pseudo-F<sub>1,4</sub>=13.79, p=0.027). In all cases depth showed no effect on community measures. </p>
		  	<table-wrap id="T2">
			<label>Table 2</label>
		<caption>
			<title> Epiphytic taxa and their families recorded growing on <italic>G. corneum</italic> during the study period (2008). Taxa are arranged by abundances.</title>
		</caption>
		<table frame="hsides" rules="groups">
  <thead>
		        <tr>
		          <th>Taxa</th>
		          <th> Family </th>
	            </tr>
	          </thead>
		      <tbody>
		        <tr>
		          <td><italic>Plocamium cartilagineum</italic> (Linnaeus) P.S. Dixon </td>
		          <td>Plocamiaceae</td>
	            </tr>
		        <tr>
		          <td><italic>Dictyota dichotoma</italic> (Hudson) J.V. Lamouroux </td>
		          <td>Dictyotaceae</td>
	            </tr>
		        <tr>
		          <td><italic>Acrosorium ciliolatum</italic> (Harvey) H. Kylin </td>
		          <td>Delesseriaceae</td>
	            </tr>
		        <tr>
		          <td><italic>Falkenbergia rufolanosa</italic> (Harvey) F. Schmitz (tetrasporic phase of <italic>Asparagopsis armata</italic>) </td>
		          <td>Bonnemaisoniaceae</td>
	            </tr>
		        <tr>
		          <td><italic>Bonnemaisonia hamifera</italic> P. Hariot </td>
		          <td>Bonnemaisoniaceae</td>
	            </tr>
		        <tr>
		          <td><italic>Aglaothamnion tripinnatum</italic> (Agardh) G. Feldmann-Mazoyer </td>
		          <td> Callithamniaceae </td>
	            </tr>
		        <tr>
		          <td><italic>Aglaothamnion tenuissimum</italic> (Bonnemaison) G. Feldmann-Mazoyer </td>
		          <td> Callithamniaceae</td>
	            </tr>
		        <tr>
		          <td><italic>Gayliella flaccida</italic> (Harveyex Kützing) T.O. Cho and L.J. McIvor </td>
		          <td>Ceramiaceae </td>
	            </tr>
		        <tr>
		          <td><italic>Trailliella intricata</italic> (tetrasporic phase of <italic>B. hamifera</italic>) </td>
		          <td>Bonnemaisoniaceae</td>
	            </tr>
		        <tr>
		          <td><italic>Antithamnionella ternifolia</italic> (Hooker andHarvey) L. Lyle </td>
		          <td>Ceramiaceae </td>
	            </tr>
		        <tr>
		          <td><italic>Callithamnion tetragonum</italic> (Withering) S.F. Gray </td>
		          <td> Callithamniaceae </td>
	            </tr>
		        <tr>
		          <td><italic>Antithamnion nipponicum</italic> Y. Yamada and K. Inagaki </td>
		          <td>Ceramiaceae </td>
	            </tr>
	          </tbody>
	        </table>
		  </table-wrap>
		  			<fig id="F2">
				<label>Fig. 2</label>
				<caption>
				<title>Plot showing the interactive effect of coastal orientation (North: N1, N2, N3; Northwest: NW1, NW2, NW3) and depth (3 and 7 m) on total epiphytes/<italic>Gelidium</italic> biomass ratio (0.25 m<sup>2</sup>). Bars represent means±se (n=3).</title>
				</caption>
				<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="../sm79n4-4239-web-resources/image/sm4239fig2_fmt.jpeg"/>
			</fig>

			<fig id="F3">
				<label>Fig. 3</label>
				<caption>
				<title>Species richness (A), Shannon diversity (B) Simpson diversity (C) and Pielou J’ evenness (D) of epiphytic flora in relation to coastal orientation (North: N1, N2, N3; Northwest: NW1, NW2, NW3) and depth (3 and 7 m). Bars represent means±se (n=3).</title>
				</caption>
				<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="../sm79n4-4239-web-resources/image/sm4239fig3_fmt.jpeg"/>
			</fig>
          
          <p>Principal coordinates analysis (PCO) relates the pattern of distribution of samples to the macroalgae taxa recorded as <italic>G. corneum</italic> epiphytes (<xref ref-type="fig" rid="F4">Fig. 4</xref>). PCO axis 1, which explained 72.2% of the total variation, mainly reflected differences related to the interaction between coastal orientation and depth. The points for the samples collected at NW-facing locations, at depths of both 3 and 7 m, are located towards the left of the plot, whereas the samples collected at N-facing locations are placed towards the right, where samples collected at 3 and 7 m are separated. Indeed, PERMANOVA analyses on multivariate data detected a significant interaction between coastal orientation and depth (<xref ref-type="table" rid="T3">Table 3</xref>). Pairwise comparisons indicated that epiphytic abundance and composition at 3 and 7 m was significantly different within N-facing locations, whereas no differences were found between epiphytes from the two depths at NW-facing locations. Therefore, three different groups were distinguished: Group 1 (N; 3 m), Group 2 (N; 7 m) and Group 3 (NW). The two-dimensional projection is highly representative of the full data cloud since it explains 80.5% of the total variation. Spearman correlations show that <italic>P. cartilagineum, D. dichotoma, Acrosorium ciliolatum</italic> and <italic>Falkenbergia rufolanosa</italic> are positively correlated with PCO axis 1, whereas <italic>Callithamnion tetragonum</italic> has a negative relationship (<xref ref-type="fig" rid="F4">Fig. 4</xref>).</p>
		  
		  			<fig id="F4">
				<label>Fig. 4</label>
				<caption>
				<title>PCO diagram based on Bray-Curtis dissimilarities showing sample distribution in relation to the interaction between coastal orientation (triangles: N; circles: NW) and depth (white, 3 m; black, 7 m). Variables were fourth-root transformed and the vector overlay (Spearman rank correlation &gt;0.5) indicates the relationship between taxa and PCO axes.</title>
				</caption>
				<graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="../sm79n4-4239-web-resources/image/sm4239fig4_fmt.jpeg"/>
			</fig>

	<table-wrap id="T3">
			<label>Table 3</label>
		<caption>
			<title>Summary of PERMANOVA results testing for the effect of coastal orientation (OR), location (LO) and depth (DE) on the composition and abundance (biomass ratios) of the epiphytic taxa growing on <italic>G. corneum</italic> (ns=non significant, *&lt;0.05, **&lt;0.01, ***&lt;0.001). Pairwise comparisons for the OR×DE interaction are shown.</title>
		</caption>
		<table frame="hsides" rules="groups">
  <thead>
                <tr>
                  <th colspan="5">PERMANOVA results</th>
                </tr>
                <tr>
                  <th></th>
                  <th>df</th>
                  <th>MS</th>
                  <th>Pseudo-F</th>
                  <th> p</th>
                </tr>
              </thead>
              <tbody>
                <tr>
                  <td> OR</td>
                  <td>1</td>
                  <td>11233.02</td>
                  <td>47.96</td>
                  <td>***</td>
                </tr>
                <tr>
                  <td> DE</td>
                  <td>1</td>
                  <td>1145.41</td>
                  <td>4.83</td>
                  <td>*</td>
                </tr>
                <tr>
                  <td> LO (OR) </td>
                  <td>4</td>
                  <td>234.17</td>
                  <td>1.14</td>
                  <td>ns</td>
                </tr>
                <tr>
                  <td> OR×DE </td>
                  <td>1</td>
                  <td>680.48</td>
                  <td>3.62</td>
                  <td>*</td>
                </tr>
                <tr>
                  <td> LO (OR)×DE </td>
                  <td>4</td>
                  <td>237.11</td>
                  <td>1.16</td>
                  <td>ns</td>
                </tr>
                <tr>
                  <td> Error </td>
                  <td>24</td>
                  <td>204.08</td>
                  <td></td>
                  <td></td>
                </tr>
                <tr>
                  <th colspan="5">Pairwise comparisons:</th>
                </tr>
                <tr>
                  <td></td>
                  <td colspan="4">N3m&gt;N7m&gt;NW3m=NW7m</td>
                </tr>
              </tbody>
            </table>
          </table-wrap>
          <p>The SIMPER routine identified Group 3 (NW) as the most distinctive group, with average dissimilarities of 31.11% and 24.35% with respect to Group 1 (N; 3 m) and Group 2 (N; 7 m), respectively (<xref ref-type="table" rid="T4">Table 4</xref>). This procedure identified <italic>P. cartilagineum, D. dichotoma, A. ciliolatum</italic> and <italic>F. rufolanosa</italic> as the species which contributed most to the dissimilarities between Group 3 and the other two groups (<xref ref-type="table" rid="T4">Table 4</xref>). In the case of the dissimilarity between Group 1 and Group 2, the contribution of <italic>A. tenuissimum</italic> and <italic>A. tripinnatum</italic> was also relevant. Regarding the abundance of different taxa, <italic>P. cartilagineum, D. dichotoma</italic>, and <italic>A. ciliolatum</italic> showed the highest biomass ratios in all the groups whereas other taxa only appeared in one group: <italic>Trailliella intricata</italic> (Group 1), <italic>Antithamnionella ternifolia</italic> (Group 2), <italic>C. tetragonum</italic> and <italic>Antithamnion nipponicum</italic> (Group 3) (<xref ref-type="table" rid="T5">Table 5</xref>). Group 1 registered the highest biomass ratios for most taxa, which decreased gradually towards Groups 2 and 3. </p>
		  	<table-wrap id="T4">
			<label>Table 4</label>
		<caption>
			<title>Summary of SIMPER procedure indicating the dissimilarity between Group 1 (N; 3 m), Group 2 (N; 7 m) and Group 3 (NW), and the contribution (%) of each taxon.</title>
		</caption>
		<table frame="hsides" rules="groups">
  <thead>
                <tr>
                  <th colspan="2">Group 1 and Group 2 </th>
                  <th colspan="2"> Group 1 and Group 3 </th>
                  <th colspan="2">Group 2 and Group 3 </th>
                </tr>
                <tr>
                  <th colspan="2">(Av. Dissimilarity=14.97%)</th>
                  <th colspan="2"> (Av. Dissimilarity=31.11%) </th>
                  <th colspan="2"> (Av. Dissimilarity=24.35%) </th>
                </tr>
                <tr>
                  <th>Taxa</th>
                  <th>Contr. (%)</th>
                  <th>Taxa</th>
                  <th>Contr. (%)</th>
                  <th>Taxa</th>
                  <th>Contr. (%)</th>
                </tr>
              </thead>
              <tbody>
                <tr>
                  <td><italic>A. ciliolatum</italic></td>
                  <td>19.0</td>
                  <td><italic>F. rufolanosa</italic></td>
                  <td>21.8</td>
                  <td><italic>F. rufolanosa</italic></td>
                  <td>25.6</td>
                </tr>
                <tr>
                  <td><italic>P. cartilagineum</italic></td>
                  <td>13.7</td>
                  <td><italic>A. ciliolatum</italic></td>
                  <td>20.1</td>
                  <td><italic>D. dichotoma</italic></td>
                  <td>17.5</td>
                </tr>
                <tr>
                  <td><italic>A. tenuissimum</italic></td>
                  <td>12.3</td>
                  <td><italic>D. dichotoma</italic></td>
                  <td>19.0</td>
                  <td><italic>A. ciliolatum</italic></td>
                  <td>14.0</td>
                </tr>
                <tr>
                  <td><italic>D. dichotoma</italic></td>
                  <td>12.0</td>
                  <td><italic>P. cartilagineum</italic></td>
                  <td>13.8</td>
                  <td><italic>P. cartilagineum</italic></td>
                  <td>8.6</td>
                </tr>
                <tr>
                  <td><italic>A. tripinnatum </italic></td>
                  <td>11.5</td>
                  <td><italic>A. tenuissimum</italic></td>
                  <td>6.5</td>
                  <td><italic>A. tripinnatum </italic></td>
                  <td>7.6</td>
                </tr>
                <tr>
                  <td><italic>A. ternifolia</italic></td>
                  <td>8.6</td>
                  <td><italic>C. tetragonum</italic></td>
                  <td>4.7</td>
                  <td><italic>A. ternifolia</italic></td>
                  <td>7.2</td>
                </tr>
                <tr>
                  <td><italic>G. flaccida</italic></td>
                  <td>7.8</td>
                  <td><italic>G. flaccida</italic></td>
                  <td>3.5</td>
                  <td><italic>C. tetragonum</italic></td>
                  <td>6.7</td>
                </tr>
              </tbody>
            </table>
          </table-wrap>
		  
		  	<table-wrap id="T5">
			<label>Table 5</label>
		<caption>
			<title>Average abundance (epiphytes/<italic>G. corneum</italic> biomass ratios) of each taxon in the different groups (Group 1, Group 2, Group 3). Taxa are arranged by abundances.</title>
		</caption>
		<table frame="hsides" rules="groups">
  <thead>
                <tr>
                  <th></th>
                  <th>Group 1 (N3m)</th>
                  <th>Group 2 (N7m)</th>
                  <th>Group 3 (NW)</th>
                </tr>
                <tr>
                  <th>Taxa</th>
                  <th>Av. Abund.</th>
                  <th>Av. Abund.</th>
                  <th> Av. Abund. </th>
                </tr>
              </thead>
              <tbody>
                <tr>
                  <td><italic>P. cartilagineum</italic></td>
                  <td>0.230012</td>
                  <td>0.142005</td>
                  <td> 0.093562 </td>
                </tr>
                <tr>
                  <td><italic>D. dichotoma</italic></td>
                  <td>0.077107</td>
                  <td>0.044609</td>
                  <td> 0.012694 </td>
                </tr>
                <tr>
                  <td><italic>A. ciliolatum</italic></td>
                  <td>0.040558</td>
                  <td>0.011547</td>
                  <td> 0.007273 </td>
                </tr>
                <tr>
                  <td><italic>F. rufolanosa</italic></td>
                  <td>0.003253</td>
                  <td>0.001696</td>
                  <td> 0.000151 </td>
                </tr>
                <tr>
                  <td><italic>B. hamifera</italic></td>
                  <td>0.000973</td>
                  <td>0</td>
                  <td> 0.000287 </td>
                </tr>
                <tr>
                  <td><italic>A. tripinnatum</italic></td>
                  <td>0.000702</td>
                  <td>0.000304</td>
                  <td> 0.000048 </td>
                </tr>
                <tr>
                  <td><italic>A. tenuissimum</italic></td>
                  <td>0.000561</td>
                  <td>0.000186</td>
                  <td> 0 </td>
                </tr>
                <tr>
                  <td><italic>G. flaccida</italic></td>
                  <td>0.000344</td>
                  <td>0.000255</td>
                  <td> 0 </td>
                </tr>
                <tr>
                  <td><italic>T. intricata</italic></td>
                  <td>0.000341</td>
                  <td>0</td>
                  <td> 0 </td>
                </tr>
                <tr>
                  <td><italic>A. ternifolia</italic></td>
                  <td>0</td>
                  <td>0.000221</td>
                  <td> 0 </td>
                </tr>
                <tr>
                  <td><italic>C. tetragonum</italic></td>
                  <td>0</td>
                  <td>0</td>
                  <td> 0.000178 </td>
                </tr>
                <tr>
                  <td><italic>A. nipponicum</italic></td>
                  <td>0</td>
                  <td>0</td>
                  <td> 0.000052 </td>
                </tr>
              </tbody>
            </table>
          </table-wrap>
    </sec>
<sec id="S4">
<title>DISCUSSION</title>
			
		  <p>We expected the abundance and diversity of epiphytes to be negatively correlated with wave exposure (coastal orientation) and positively correlated with light intensity (negatively with depth). Our results partially support this hypothesis. Significant interactive effect of these two factors was observed for species composition and abundance of epiphytic flora. <italic>G. corneum</italic> populations living at the most exposed locations had the lowest epiphyte load and the least diverse community. However, depth only had a significant effect on the distribution of epiphytes below a certain threshold of wave action, with the epiphytic load being 30-40% greater on shallow bottoms. This pattern suggests that in shallow waters hydrodynamic pressure on epiphytic flora could be a more determinant factor in regulating epiphytes than light availability. </p>
			<p>The composition of epiphytes on <italic>G. corneum</italic> is found to be dominated by <italic>P. cartilagineum, D. dichotoma</italic> and <italic>A. ciliolatum</italic>. The first two of these taxa have been described as common annual epiphytes accompanying <italic>G. corneum</italic> (<xref ref-type="bibr" rid="CIT46">Santos 1994</xref>, <xref ref-type="bibr" rid="CIT18">Gorostiaga 1995</xref>). Furthermore, hydrodynamism appeared to have a significant influence on the distribution of some morphologically simple taxa, whereas <italic>F. rufolanosa, A. tenuissimum</italic><italic>, A. tripinnatum, A. ternifolia</italic>, and <italic>G. flaccida</italic> showed a preference for relatively lower-energy conditions, <italic>C. tetragonum</italic> and the alien species <italic>A. nipponicum</italic> were more abundant at the most exposed locations. It is also noteworthy that the epiphytic community on <italic>G. corneum</italic> found in this study was extraordinary low, especially compared with that found in northwestern Spain (Galicia) for other canopy-forming species thriving in semi-exposed to exposed areas (<xref ref-type="bibr" rid="CIT37">Otero-Schmitt and Pérez-Cirera 1996</xref>). The latter authors found 30 to 70 different species of epiphytic flora, mainly rhodophytes, growing in four different species from the genus <italic>Cystoseira</italic>. In this sense, the frondose morphology and cartilaginous texture of <italic>G. corneum</italic> contrasts with the tree-like morphology and leathery texture of the species of the genus <italic>Cystoseira</italic>, which might enhance the notable differences found in the diversity of epiphytic flora between the two macrophytes. Differences in epiphytic loads regarding morphological features and longevity of the host have been reported in the case of seagrass species (<xref ref-type="bibr" rid="CIT25">Lavery and Vanderklift 2002</xref>).</p>
			<p>With respect to the epiphytic loads in the present study, very exposed (NW) areas showed significantly lower epiphytic abundances than exposed (N) areas. This pattern is consistent with other studies from northwestern Spain (Galicia) (<xref ref-type="bibr" rid="CIT39">Peteiro and Freire 2013</xref>) and northern Europe (<xref ref-type="bibr" rid="CIT38">Pedersen et al. 2012</xref>, <xref ref-type="bibr" rid="CIT04">Baer and Stengel 2014</xref>), which found the epiphytic loads on canopy-forming species to be lower on more exposed coastal stretches. Moreover, very exposed locations (NW) in our study showed lower species richness and diversity, coinciding with that found for epiphytic flora (<xref ref-type="bibr" rid="CIT23">Kersen et al. 2011</xref>) and fauna growing on canopy-forming macrophytes (<xref ref-type="bibr" rid="CIT35">Norderhaug et al. 2012</xref>, <xref ref-type="bibr" rid="CIT36">2014</xref>), according to whom lower species diversities are found under frequent or even rare ecological disturbances (e.g. wave action). Indeed, wave exposure is one of the major factors directly or indirectly influencing the structure of algal assemblages (<xref ref-type="bibr" rid="CIT43">Rindi and Guiry 2004</xref>, <xref ref-type="bibr" rid="CIT34">Nishihara and Terada 2010</xref>, <xref ref-type="bibr" rid="CIT07">Borja et al. 2013</xref>). Although increasing wave action is a key factor in supplying nutrients for macroalgae (<xref ref-type="bibr" rid="CIT29">Martins et al. 2013</xref>), hydrodynamic pressure can also remove epibionts and prevent them from settling (<xref ref-type="bibr" rid="CIT23">Kersen et al. 2011</xref>). The mechanical stress produced by higher wave-action (<xref ref-type="bibr" rid="CIT24">Kraufvelin 2007</xref>) could favour the removal of epiphytes at NW oriented locations in our study, whereas at N oriented locations lower hydrodynamic levels could favour their development. Similarly, the lower species richness and diversity and the smaller quantities of morphologically simple forms found at NW-facing locations in this study might be explained by the higher sensitivity of some taxa to the effects of wave action (<xref ref-type="bibr" rid="CIT34">Nishihara and Terada 2010</xref>). However, there are some exceptions, such as <italic>C. tetragonum</italic> and <italic>A. nipponicum</italic>, which showed affinity to more exposed coastal stretches, as also reported by <xref ref-type="bibr" rid="CIT47">Secilla (2009)</xref>.</p>
			<p>Light is a prime factor regulating the distribution of algae since the survival and productivity of photosynthetic organisms are closely linked to light intensity and quality (<xref ref-type="bibr" rid="CIT40">Prado et al. 2007</xref>, <xref ref-type="bibr" rid="CIT31">Michael et al. 2008</xref>). Increasing irradiance levels usually favour algal development and growth (<xref ref-type="bibr" rid="CIT01">Altamirano et al. 2000</xref>, <xref ref-type="bibr" rid="CIT10">Colombo-Pallotta et al. 2006</xref>). Therefore, due to the exponential decay of light intensity with increasing depth (<xref ref-type="bibr" rid="CIT20">Gross et al. 2003</xref>, <xref ref-type="bibr" rid="CIT29">Martins et al. 2013</xref>), shallower waters may be expected to contain higher epiphyte loads (<xref ref-type="bibr" rid="CIT32">Muñoz and Fotedar 2010</xref>, <xref ref-type="bibr" rid="CIT48">Tsirika et al. 2007</xref>). Our findings partially support this hypothesis. At the N-facing locations (with less wave energy) the epiphytic load was significantly greater in shallow waters than in deeper waters. However, our results do not show this pattern in the NW-facing locations, where the potentially greater epiphytic growth under high light conditions may be mitigated by the higher wave action (<xref ref-type="bibr" rid="CIT26">Liria et al. 2009</xref>, <xref ref-type="bibr" rid="CIT14">Galparsoro et al. 2010</xref>). Nevertheless, it should be noted that factors other than light, such as water movement, temperature, sedimentation and nutrient availability, may vary with depth. Therefore, experimental field and laboratory studies should be conducted in order to separate the effect of light availability on the distributional patterns of epiphytes from other depth-related factors.</p>
			<p>In conclusion, our findings suggest that the interactive effects of wave action and light availability seem to be involved in the diversity, abundance and composition patterns of the epiphytes growing on <italic>G. corneum</italic>. Since epiphytes may cause some damage to their hosts, future field and laboratory experiments should be carried out to assess the effects of these assemblages on <italic>G. corneum</italic> populations. Furthermore, considering the significant decline undergone by <italic>G. corneum</italic> in pristine coastal stretches of the Basque coast (<xref ref-type="bibr" rid="CIT12">Díez et al. 2012</xref>, <xref ref-type="bibr" rid="CIT07">Borja et al. 2013</xref>), the combined effects of epiphytism and potential environmental stressors on this canopy-forming species would need to be separated to generate better predictive models of the distribution of <italic>G. corneum</italic> under hypothetical climate change scenarios.</p>
		</sec>	
		  </body>
		  <back>
<ack>
<title>ACKNOWLEDGEMENTS</title>
			
		  <p>This study was supported by the projects ‘ECOLIFE-CAN: Monitoring the Effects of Climate Change on Benthic Marine Communities along the Basque Coast: a First Evaluation of Biological (CGL08-0547) and Ecological Changes and Stress Factors’ (Ministry of Science and Innovation, MICIIN) and ‘K-EGOKITZEN: Climate Change: Impact and Adaptation’ (Department of Industry, Trade and Tourism of the Basque Government). We are also indebted to the University of the Basque Country (UPV/EHU) for grant PIF09/2009/PIF09048, which partially supported this work.</p>
			
	</ack>
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</ref-list>
</back>
</article>
