1 Running title: Coral identity underpins reef complexity 2 3 Title: Coral identity underpins reef complexity on Caribbean reefs 4 5 6 Lorenzo Alvarez-Filip1,2,*, Nicholas K. Dulvy2, Isabelle M. Côté2, Andrew R. Watkinson3 7 and Jennifer A. Gill1 8 9 10 1 Centre for Ecology, Evolution, and Conservation, School of Biological Sciences, University of East Anglia, Norwich NR4 7TJ, United Kingdom 11 12 13 2 Earth to Ocean Research Group, Department of Biological Sciences, Simon Fraser University, Burnaby BC, V5A 1S6 Canada 14 15 16 3 School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, United Kingdom. 17 18 * Correspondence should be sent to: Lorenzo Alvarez-Filip, Department of Biological 19 Sciences, Simon Fraser University. 8888 University Drive, Burnaby, British Columbia, V5A 20 1S6, Canada. Email address: [email protected] 21 22 23 24 25 26 1 27 Abstract 28 29 The architectural complexity of ecosystems can greatly influence their capacity to support 30 biodiversity and deliver ecosystem services. Understanding the components underlying this 31 complexity can aid the development of effective strategies for ecosystem conservation. 32 Caribbean coral reefs support and protect millions of livelihoods, but recent anthropogenic 33 change is shifting communities towards reefs dominated by stress-resistant coral species, 34 which are often less architecturally complex. With the regionwide decline in reef fish 35 abundance it is becoming increasingly important to understand changes in coral reef 36 community structure and function. We quantify the influence of coral composition, diversity 37 and morpho-functional traits on the architectural complexity of reefs across 91 sites at 38 Cozumel, Mexico. Although reef architectural complexity increases with coral cover and 39 species richness, it is highest on sites that are low in taxonomic evenness and dominated by 40 morpho-functionally important reef-building coral genera, particularly Montastraea. Sites 41 with similar coral community composition also tend to occur on reefs with very similar 42 architectural complexity, suggesting that reef structure tends to be determined by the same 43 key species across sites. Our findings provide support for prioritising and protecting 44 particular reef types, particularly those dominated by key reef-building corals, in order to 45 enhance reef complexity. 46 47 Keywords: biodiversity, dominance, functional groups, habitat complexity, landscape 48 ecology 49 50 51 2 52 INTRODUCTION 53 54 The architectural complexity of ecosystems often underpins the biodiversity and 55 ecosystem services that they support. Architectural complexity is very often defined or 56 provided by foundation taxa (e.g. trees, oysters, stony corals) that have a disproportionate 57 influence on ecosystem structure, function and stability (MacArthur 1984, Bruno and 58 Bertness 2001, Ellison et al. 2005). However, within these broad groups of foundation taxa, 59 different species can contribute disproportionately to architectural complexity. Species 60 identity and dominance have been reported as important determinants of ecosystem functions 61 and processes (e.g. terrestrial grassland, soil ecosystems; Tilman et al. 1997, McLaren and 62 Turkington 2010), however, studies that directly examine the role of the type, rather than the 63 number, of species on habitat facilitation are rare. Understanding the influence of different 64 species and taxa on ecosystem structure and function is not only of fundamental ecological 65 interest but can underpin the development of effective conservation priorities and actions. 66 Coral reefs are among the most rapidly changing and valuable ecosystems in the 67 world. It is estimated that nearly 70 per cent of the world’s coral reefs are threatened by 68 anthropogenic activities (Wilkinson 2008) and are experiencing unprecedented rates of 69 degradation (Veron 2008). In the Caribbean, for instance, the architectural complexity of 70 reefs has declined substantially over the past forty years with the loss of ~80% of the most 71 complex reefs (Alvarez-Filip et al. 2009a). Because of the importance of reef-building corals 72 as foundation species within the diverse reef ecosystem, patterns of degradation and 73 ecological resilience on coral reefs are typically measured through changes in overall coral 74 cover (e.g. Gardner et al. 2003, Bruno and Selig 2007, Mumby et al. 2007). However, 75 changes in coral cover often do not capture the changes in reef architectural complexity 76 (Alvarez-Filip et al. in press) that can underpin a suite of important ecosystem services such 3 77 as the dissipation of wave energy, nutrient recycling and the abundance, diversity and trophic 78 structure of coral reef fishes (Szmant 1997, Lugo-Fernandez et al. 1998, Sheppard et al. 2005, 79 Wilson et al. 2007; 2010). 80 There is considerable potential for taxon identity and the composition of reef-building 81 corals to influence the architectural complexity of reefs, because hard scleractinian corals are 82 a taxonomically and morphologically diverse group (Veron and Stafford-Smith 2002, Dullo 83 2005). While qualitative differences in the relative contribution of different coral species to 84 reef complexity are readily apparent, the contribution of coral identity and community 85 composition to architectural complexity has yet to be quantified at the larger reef scales. 86 Quantifying the relative contribution of different coral species to the architectural complexity 87 of the reefscape is therefore particularly important in order to understand the trajectory of 88 coral reefs under changing environmental conditions. 89 Disturbances commonly favour a few species that are able to competitively dominate 90 the landscape (Tilman & Lehman 2001; Seabloom et al. 2003). Although the Caribbean 91 underwent rapid losses of the structurally important Acroporid corals in the late-1970s, many 92 reefs remained dominated by healthy populations of the other major-reef building coral 93 Montastraea (e.g. McClanahan et al. 1998), suggesting that reef complexity could be 94 maintained to some degree in reefs across the region. Since then, the spread of several 95 recently emerged diseases, combined with recent bleaching events and other biotic 96 disturbances, are now fostering high rates of mortality of Montastraea and other coral species 97 previously thought to be more resistant to disturbance (Weil 2004; Bruckner & Bruckner 98 2006). Throughout the Caribbean, the loss of these main reef-building coral species 99 (Acropora and Montastraea) has been accompanied by an increase in the relative abundance 100 (often leading to eventual dominance) of stress-tolerant, early-colonizing corals that form 101 smaller and less-architecturally complex colonies such as Porites and Agaricia (Lirman and 4 102 Manzello 2009, Jackson 2001, Aronson et al. 2002, Green et al. 2008). This shift towards 103 weedy coral species may constrain reefs into a state of lower potential architectural 104 complexity (Steneck et al. 2009), even if overall coral cover remains stable. 105 Here we explore the contribution of coral community composition to reef 106 architectural complexity across a broad range of sites in Cozumel, Mexico. First, we quantify 107 whether sites with similar coral community composition also tend to be similar in terms of 108 architectural complexity. Second, we test whether greater coral species diversity is related to 109 greater architectural complexity. Finally, we explore how the taxonomic and functional 110 attributes of coral dominance influence the relationship between coral cover and architectural 111 complexity. 112 113 MATERIALS AND METHODS 114 115 Study area 116 Cozumel is a continental island 18 km off the north-eastern coast of the Mexican 117 Peninsula of Yucatan. The island is surrounded by coral reefs. The most developed 118 formations are in the western shelf, where three terraces can be found between 5 m below sea 119 level and the shelf edge (~20 m). Unlike many other Caribbean reefs where reefs originally 120 comprised Acroporid species, in Cozumel the reefs close to the shore have been built mainly 121 by Montastraea (Muckelbauer 1990). The south-western coast of Cozumel has been under 122 official protection since 1980 (figure 1, Alvarez-Filip et al. 2009b) and, while visitation and 123 tourist activities are permitted, fishing is banned on the western coast of the marine reserve. 124 125 Field surveys 5 126 In total, 91 sites along the south-west coast of Cozumel, all separated by at least 200 127 m (figure 1), were surveyed between October 2007 and February 2008. At each site, one 30 128 m transect was haphazardly located on the top of the reef crest (between 10 and 15 m depth) 129 and parallel to the coast. Reef attributes such as coral cover or reef architecture were not used 130 to determine the position of transects. To evaluate coral abundance, we used the point 131 intercept method to record the occurrence of corals every 25 cm along each transect (120 132 counts per transect). This method is widely used in the Caribbean and elsewhere to describe 133 reef benthic composition, and it has been shown to provide comparable information to 134 measuring benthic composition along the entire length of transects (Hill and Wilkinson 135 2004). All corals were identified in the field at species level according to Veron and Stafford- 136 Smith 2002. 137 Reef architectural complexity was quantified using the rugosity index (Risk 1972), 138 which was obtained by fitting a fine, three metre chain (0.7 cm link-length) to the reef. While 139 laying the chain, care was taken to follow the detailed contour of corals and other reef 140 attributes (rock crevices, sponges) by lining up individual branches and fitting the chain 141 between coral ramets. To calculate the index, the contoured distance is divided by the linear 142 distance between its start and end point. A perfectly flat surface has a rugosity index of one, 143 with larger numbers indicating more complex surfaces. Rugosity measures were taken in five 144 equally spaced points along the same 30 m transect, which were then averaged to give 145 transect-level rugosity. 146 147 148 149 150 Data Analyses To examine whether transects with similar coral community composition also tended to have similar architectural complexity, we constructed matrices of site community 6 151 composition and site rugosity for all pairs of sites. The similarity matrix for coral community 152 composition was constructed using all coral species and their relative cover in each site, and 153 computed using the Bray-Curtis similarity coefficient. The architectural complexity matrix 154 was constructed by calculating the relative percentage similarity in rugosity between each 155 pair of sites using the following formula: 156 % similarity = (│Ri - Rj│/ MD) x 100 157 where │Ri - Rj│is the absolute difference between the values of rugosity in sitei and sitej for 158 each pair of sites, and MD is the maximum observed difference between all the pairwise 159 comparisons. We evaluated whether architectural complexity among sites is a function of 160 coral community composition among sites using a Mantel test (Mantel 1967). This test 161 measures the correlation between two matrices and assesses the significance of the 162 correlation by randomizing one of the matrices and calculating a null distribution of values 163 from the randomly generated associations. In this study, the Mantel test was calculated using 164 the package Vegan in R (R 2009), with 10,000 random matrix permutations used to assess 165 significance levels. 166 To test whether greater coral species diversity is related to greater architectural 167 complexity, we quantified coral diversity using three univariate dimensions of diversity: coral 168 species richness (number of species recorded at each site), evenness in species abundance 169 (the Pielou index of percentage areal cover of each species) and taxonomic diversity. For the 170 last dimension, we calculated the average taxonomic distinctness (Δ+) and the variation in 171 taxonomic distinctness (Λ+) using a widely-used and accepted coral taxonomy (Veron and 172 Stafford-Smith 2002). Average taxonomic distinctness measures average evolutionary 173 relatedness as the mean path (or branch) length of the local community and the variation in 174 taxonomic distinctness is the variance in path (or branch) lengths of the local community 175 (Clarke and Warwick 2001). We also calculated richness and evenness of the morpho- 7 176 functional groups. We then used linear regressions to explore the strength and nature of the 177 associations between each of these measures of coral diversity and reef architectural 178 complexity. 179 To explore the influence of species identity and morpho-functional attributes on reef 180 structure, we grouped coral species by genus and by morphology. Morpho-functional groups 181 were constructed from the maximum size and colony shape of each coral species (table 1). 182 Following Reyes-Bonilla (2004), three shape categories (massive or nodular; branching, 183 ramose or phaceloid; platy, foliaceous or encrusting) and three size categories (small (<10 184 cm); medium (10 to 30 cm); large (>30 cm)) were used. Combining shape and size categories 185 resulted in seven different morpho-functional groups (table 1). 186 To explore how the taxonomic and functional attributes of coral dominance influence 187 the relationship between coral cover and architectural complexity, we compare the slopes of 188 these relationships among (a) the three most abundant genera (Agaricia, Porites and 189 Montastraea) and (b) the three most abundant morpho-functional groups (figure 2b). The 91 190 transects were categorised depending on the single most dominant (highest relative 191 abundance on the site) genus and morpho-functional group. Differences between each pair of 192 linear models were explored by dividing the difference between both regression coefficients 193 by the square root of the sum of the squared standard errors. Assuming normally distributed 194 residuals, this estimate follows a t-distribution with n-2 degrees of freedom (Zar 1999). 195 196 RESULTS 197 198 A total of 33 species of reef-building corals were recorded in Cozumel during this study 199 (table 1). The dominant genera included Agaricia, Montastraea and Porites (primarily P. 200 astreoides), and hence corals with large, massive and foliaceous colonies were the most 8 201 abundant morpho-functional groups (figure 2a,b). Both coral cover and reef architectural 202 complexity vary greatly across the study area, from flat sites with low coral cover to highly 203 complex areas of reef. Average coral cover for the 91 sites was 16% (± 1.32 SE, range: 0 - 204 52%) while rugosity averaged 1.49 (± 0.04 SE, range: 1.02 - 2.77). 205 Pairs of sites with similar coral community composition tend to also have similar 206 levels of architectural complexity (Mantel test, rm = 0.18; p < 0.001).Very high similarity in 207 coral community composition (> 70% similarity) only occurred in reefs with similar 208 architectural complexity (> 50% similarity in rugosity), regardless of whether the sites were 209 similarly complex or similarly flat (figure 3). 210 Architectural complexity is positively associated with the number of coral species; 211 sites with fewer than five coral species tend to be relatively flat while more diverse sites, with 212 between 8 and 13 species, had the greatest complexity (figure 4a). However, the evenness in 213 coral cover among coral species declined with increasing coral species richness (r = -0.40; P 214 < 0.001), and consequently sites with greater architectural complexity tended to be species- 215 rich but dominated by one or few coral species (figure 4b). The flat reefs primarily comprise 216 bare rock and/or algae rather than monotypic patches of relatively flat corals (e.g. Millepora 217 or Siderastrea), as indicated by the lack of any sites with high coral cover and low rugosity 218 (figure 4a). The relationship between taxonomic distinctness among coral species and 219 architectural complexity is highly non-linear (R2 = 0.01; P = 0.22), with a small number of 220 flat reefs tending to be either particularly distinct or particularly related (figure 3c). The 221 variation in taxonomic distinctness was not significantly related to architectural complexity 222 (figure 4d). From the morphological and functional perspective, greatest complexity is found 223 on reefs with higher morpho-functional diversity (figure 4e), but dominated by relatively few 224 morpho-functional types (figure 4f). 225 9 226 Reefs with greater coral cover tend to have greater architectural complexity but the 227 228 variance in architectural complexity also increases with coral cover (figure 5a). Much of 229 variance in architectural complexity at high levels of coral cover is the result of dominance 230 by a particular coral genus. Sites dominated by species from the genus Montastraea have 231 greater architectural complexity for a given coral cover, followed by Agaricia then Porites 232 (figure 5b). On Montastraea-dominated sites, architectural complexity increased more 233 rapidly with increasing coral cover than on Porites-dominated sites (T24 = -2.23; P = 0.03). 234 However, the slopes of relationships between coral cover and architectural complexity for 235 Agaricia and each of the other two genera did not differ significantly (Agaricia vs 236 Montastraea: T49 = 1.65, P= 0.10; Agaricia vs Porites: T47 = -1.23, P = 0.22). The differences in architectural complexity for given levels of coral cover are also 237 238 strongly related to the morpho-functional attributes of the dominant species. Sites dominated 239 by massive and large coral species have greater architectural complexity for a given coral 240 cover, followed by sites dominated by large platy, foliaceous or encrusting (PL) and then 241 medium size massive corals (figure 5c). Architectural complexity on sites dominated by 242 massive and large coral species also increased significantly more rapidly with increasing 243 coral cover than on reefs dominated by medium size massive corals (T34 = -2.72, P = 0.01). 244 However, the slope of the relationship between architectural complexity and coral cover on 245 large platy, foliaceous or encrusting -dominated reefs did not differ significantly from the 246 other two morphological groups (PL vs ML: T54 = 1.56, P = 0.13; PL vs MM: T30 = -0.81; P = 247 0.43). 248 249 250 10 251 252 DISCUSSION 253 254 Our findings suggest that the type and dominance of foundation species can be just as 255 important as their overall abundance in providing architectural complexity to their 256 ecosystems. Reef complexity increases with increasing coral cover, but the rate of increase in 257 complexity depends on coral community composition and, in particular, the identity of the 258 dominant species and their associated morphological and functional traits. The most 259 architecturally complex sites are dominated by few coral species (and morpho-functional 260 groups) and the identity of these corals largely explains the differences in the architecture of 261 these sites. These findings underscore the importance of considering coral species 262 composition and shifts in coral dominance on Caribbean reefs in order to understand the 263 implications of changes in these ecosystems on the associated biodiversity and ecosystem 264 services. 265 Generally, species diversity is considered a fundamental feature of ecosystem 266 structure and function (Loreau et al. 2001, Hooper et al. 2005) and, in coral reefs, greater 267 species diversity might be expected to increase reef complexity simply because of the large 268 variety of coral forms and shapes (e.g. Chabanet et al. 1997, Bruno and Bertness 2001). 269 However, positive relationships between the number of coral species and architectural 270 complexity may in fact be a consequence of the positive relationship between coral cover and 271 architectural complexity, as species diversity can also be positively associated with the extent 272 of coral cover (this study: r = 0.83, P < 0.001; Bell and Galzin 1984). Moreover, taxonomic 273 relatedness indices show that most sites shared a very similar species composition and that 274 there is no clear effect of increasing taxonomic composition on reef architectural complexity. 275 By contrast, the distribution of species relative abundances (percent cover) clearly shows that 11 276 predominance by one or few species increases the complexity of the reef structure. 277 Historically, Caribbean reefs have comprised small numbers of abundant species rather than a 278 high diversity of coral species (Johnson et al. 2008), supporting the importance of coral 279 dominance in structuring Caribbean reefs. In addition, Caribbean corals have relatively low 280 diversity and redundancy in comparison with other regions of the world. For example, there 281 are 120 massive coral species in the Great Barrier Reef, Australia while the Caribbean 282 harbours fewer than 25 (Bellwood et al. 2004). This lack of functional diversity might explain 283 why Caribbean reef architectural complexity relies more on the presence and identity of 284 dominant species than on the combined structural attributes of a wider range of species. 285 We found that the strength of the positive effect of foundation species in providing 286 structure to the habitat largely depends on the identity of the dominant taxa. At the reefscape 287 scale, architectural complexity increased faster in sites dominated by large-massive species, 288 such as Montastraea, than in sites dominated by short-lived and stress-resistant species. 289 Branching corals are a relatively uncommon in Cozumel, for example, branching species of 290 the genus Porites (P. porites) occur at much lower relative abundance than the sister massive 291 species (P. astreoides; table 1), and the main differences in reef complexity found in this 292 study are therefore primarily a consequence of the large and massive nature of Montastraea 293 corals. Among Caribbean reef-building corals, Montastraea species play critical roles in reef 294 construction and community ecology (Harborne et al. 2008, Harborne 2009). The relative 295 abundance of such massive species is declining in the Caribbean (Edmunds and Elahi 2007). 296 For example, Cozumel reefs were largely dominated by Montastraea species in the 1980s 297 (Muckelbauer 1990) but more recently they have been increasingly dominated by Agaricia 298 and Porites (Alvarez-Filip et al. 2009b; figure 2). Cozumel reefs may therefore no longer be 299 providing the structural benefits that they were in recent decades. Similar shifts from 300 assemblages dominated by physically large and long-lived coral species toward assemblages 12 301 dominated by weedy corals are being recorded throughout the Caribbean (Lirman and 302 Manzello 2009, Jackson 2001, Aronson et al. 2002, Green et al. 2008, Steneck et al. 2009), 303 highlighting the large-scale consequences that these changes in coral community composition 304 may have for the architectural complexity of Caribbean reefs. 305 On sites with relatively low coral cover (≤ 20 %), architectural complexity varies 306 little, even across sites dominated by different coral species and types (figures 5 b,c), 307 probably because dominant species are not abundant enough (high evenness; figure 5a) to 308 contribute significantly to the reef framework. Assuming that this also applies elsewhere in 309 the Caribbean, our findings may help to explain the rapid structural homogenization towards 310 relatively flat reefs reported in recent decades (Alvarez-Filip et al. 2009a). Most Caribbean 311 reefs have been near or below 20% coral cover since the early 2000s (Gardner et al. 2003, 312 Bruno et al. 2009, Schutte et al. 2010), which may suggest that the abundance of previously 313 dominant corals in most reefs is now too low to contribute significantly to reef architectural 314 complexity. It is likely that the high frequency of disturbances or chronic mortality that 315 Caribbean reefs are facing may prevent some structurally-important species from dominating 316 (Hughes and Connell 1999), and these reefs are therefore likely to remain in the current low- 317 complexity and high evenness state. 318 More complex reefs tend to have greater numbers of individuals, biomass or richness 319 of reef-associated fishes and invertebrates (Dulvy et al. 2002, Idjadi and Edmunds 2006, 320 Wilson et al. 2007). Consequently, our findings suggest that assemblages with dominant reef- 321 building species such as Montastraea spp. would be expected to facilitate more biodiverse 322 and functionally-important coral reefs in the Caribbean. Montastraea historically ranked high 323 in importance along with Acropora palmata and A. cervicornis in their overall contribution to 324 Western Atlantic reef structure. Acroporids have now almost vanished from Caribbean reefs 325 and the unique structural role (i.e. large-branching colonies) of these corals is likely no longer 13 326 filled by any other species (Bruckner 2003; Aronson & Precht 2006). In the Caribbean 327 therefore it is likely that halting rates of architectural complexity loss will require a major 328 emphasis on facilitating the maintenance and endurance of healthy populations of 329 Montastraea corals, and promoting the recovery of Acroporids, rather than just focussing 330 efforts on restoring the overall abundance of scleractinian corals. This seems to be 331 particularly important for those reefs that have relatively high coral cover (> 20%), where the 332 presence of healthy populations of these key coral species may considerably increase the reef 333 architectural complexity. Important regional differences in the species richness and functional 334 composition of reef systems (Bellwood et al. 2004) also highlight the need to explore the 335 generality of these findings. Assessing whether similar patterns occur in regions with 336 considerably higher diversity of coral forms and functional redundancy, such as in the Indo- 337 West Pacific, would enrich our understanding of the role of coral species composition in the 338 provision of ecological and ecosystem services. 339 340 341 Acknowledgements 342 This study was carried out with the permission and support of the Parque Nacional Arrecifes 343 de Cozumel and the Comisión Nacional de Áreas Naturales Protegidas of México. We thank 344 M. Millet-Encalada, R. Hernandez-Landa, A. Brito-Bermudez, and the staff of the PNAC for 345 their invaluable help during the surveys. This research was founded by the Mexican 346 scholarships from the CONACYT (171864) and SEP to L.A-F. 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Average percentage Colony Colony Morphology shapea sizeb groupc Genus Species cover (± SE) Acropora A. cervicornis 0.03 (0.03) B L BL A. palmata 0.16 (0.1) B L BL M. decactis 0.16 (0.04) M M MM M. formosa 0.02 (0.01) B M BM Stephanocoenia S. intersepta 0.24 (0.05) M M MM Eusmilia E. fastigiata 0.39 (0.07) B M BM Colpophyllia C. natans 0.06 (0.04) M L ML Diploria D. clivosa 0.03 (0.02) M L ML D. labyrinthiformis 0.05 (0.02) M M MM D. strigosa 0.07 (0.04) M M MM M. annularis 1.43 (0.39) M L ML M. cavernosa 0.97 (0.12) M L ML M. faveolata 1.68 (0.26) M L ML M. franksi 0.09 (0.03) M M MM Favia F. fragum 0.02 (0.01) M S MS Dendrogyra D. cylindrus 0.01 (0.01) M L ML Dichocoenia D. stokesii 0.04 (0.02) M M MM Meandrina M. meandrites 0.13 (0.04) M M MM Isophyllastrea I. rigida 0.02 (0.01) M M MM Mycetophyllia M. lamarckiana 0.15 (0.04) P M PM Madracis Montastraea 21 Agaricia Siderastrea Porites Millepora A. agaricites 4.56 (0.41) P L PL A. humilis 0.03 (0.02) M L ML A. lamarcki 0.02 (0.01) P L PL A. tenuifolia 0.43 (0.13) P L PL S. radians 0.02 (0.01) M S MS S. siderea 1.45 (0.16) M L ML P. astreoides 2.45 (0.3) M M MM P. colonensis 0.03 (0.02) P M PM P. divaricata 0.02 (0.01) B L BL P. furcata 0.10 (0.04) B L BL P. porites 0.82 (0.13) B L BL M. alcicornis 0.27 (0.06) B M BM M. complanta 0.06 (0.02) P L PL 499 500 501 502 503 a M = massive or nodular; B = branching, ramose or phaceloid; P = platy, foliaceous or encrusting. b S = small (<10 cm); M = medium (10 to 30 cm); L = large (>30cm). c Morphological group is the combination of shape and size. 22 504 Figure legends 505 506 Figure 1. Map of Cozumel Island and (inset) the location within the Caribbean Sea. The 507 continuous line delimits the polygon of the Marine Protected Area (Parque Nacional 508 Arrecifes de Cozumel) and the bold dotted line represents the area surveyed in this study. 509 510 511 Figure 2. Mean percent cover (± standard error) of hard corals on Cozumel reefs, grouped by 512 (a) genus and (b) morphology (see table 1 for definitions of morpho-functional groups). For 513 (b) the total number of species included in each morpho-functional group is given in 514 parentheses. 515 516 Figure 3. Similarities in coral community composition (Bray-Curtis similarity coefficient) 517 and reef architecture (% similarity in rugosity indices) for 4095 different pairs of sites from 518 91 sites in Cozumel. Circle colour indicates pairs of sites which both have rugosity values > 519 1.5 (black), both < 1.5 (grey) or one from each category (white). 520 521 522 Figure 4. The relationships between reef architectural complexity on 91 sites in Cozumel and 523 (A) total number of coral species (y = 1.06 + 0.08x; R2 = 0.34; P < 0.001); (B) Pielou index 524 of coral species evenness (y = 3.99 - 2.79 x; R2 = 0.30; P < 0.001); (C) average taxonomic 525 distinctness of coral species; (D) variation in taxonomic distinctness of coral species; (E) total 526 number of coral morpho-functional groups (y = 0.79 + 0.19x; R2 = 0.33; p < 0.001); and (F) 527 Pielou index of morpho-functional groups evenness (y = 4.08 – 2.90x; R2 = 0.32; p < 0.001). 528 23 529 Figure 5. The relationship between coral cover and architectural complexity indices across 91 530 sites in Cozumel (R2 = 0.61; slope = 0.024; P < 0.001) for (A) sites dominated by 531 Montastraea (black), Agaricia (dark grey), Porites (pale grey) or no dominant species 532 (white), and the linear regression and 95% confidence intervals for sites dominated by the 533 three most common (B) coral genera: Montastraea (y = 1.02 + 0.04x; R2 = 0.61; P < 0.001); 534 Agaricia (y = 1.12 + 0.02x; R2 = 0.55; P < 0.001) and Porites (y = 1.05 + 0.02x; R2 = 0.84; P 535 < 0.001) and (C) morphological groups: ML (y = 1.05 + 0.03x; R2 = 0.62; P < 0.001); PL (y = 536 1.16 + 0.02x; R2 = 0.50; P < 0.001) and MM (y = 1.02 + 0.02x; R2 = 0.93; P < 0.001). See 537 table 1 for details of morphological groups. In (A) increasing point size represents increasing 538 evenness (Pielou index) of coral community composition. 539 540 24 541 Figure 1 542 543 544 545 546 547 25 548 Figure 2 549 550 551 552 553 26 554 Figure 3 555 556 557 558 559 560 27 561 Figure 4 562 563 564 28 565 Figure 5 566 567 29
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