The Symbiodinium community associated with scleractinian corals is widely considered to be shaped by seawater temperature, as the coral's upper temperature tolerance is largely contingent on the Symbiodinium types harboured. Few studies have challenged this paradigm as knowledge of other environmental drivers on the distribution of Symbiodinium is limited. Here, we examine the influence of a range of environmental variables on the distribution of Symbiodinium associated with Acropora millepora collected from 47 coral reefs spanning 1,400 km on the Great Barrier Reef (GBR), Australia.
The environmental data included Moderate Resolution Imaging Spectroradiometer (MODIS) satellite data at 1 km spatial resolution from which a number of sea surface temperature (SST) and water quality metrics were derived. In addition, the carbonate and mud composition of sediments were incorporated into the analysis along with in situ water quality samples for a subset of locations. Analyses were conducted at three spatio-temporal scales [GBR (regional-scale), Whitsunday Islands (local-scale) and Keppel Islands/Trunk Reef (temporal)] to examine the effects of scale on the distribution patterns. While SST metrics were important drivers of the distribution of Symbiodinium types at regional and temporal scales, our results demonstrate that spatial variability in water quality correlates significantly with Symbiodinium distribution at local scales. Background levels of Symbiodinium types were greatest at turbid inshore locations of the Whitsunday Islands where SST predictors were not as important. This was not the case at regional scales where combinations of mud and carbonate sediment content coupled with SST anomalies and mean summer SST explained 51.3% of the variation in dominant Symbiodinium communities.
Citation: Cooper TF, Berkelmans R, Ulstrup KE, Weeks S, Radford B, Jones AM, et al. (2011) Environmental Factors Controlling the Distribution of Symbiodinium Harboured by the Coral Acropora millepora on the Great Barrier Reef. PLoS ONE 6(10): e25536. https://doi.org/10.1371/journal.pone.0025536
Editor: Terence Evens, US Dept. of Agriculture – Agricultural Research Service (USDA-ARS), United States of America
Received: May 12, 2011; Accepted: September 6, 2011; Published: October 31, 2011
Copyright: © 2011 Cooper et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: This study was supported by the Australian Institute of Marine Science, University of Queensland, DHI Group and the Marine Tropical Science Research Facility through the Reef and Rainforest Research Centre. These funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript. DHI Group supported the time of KU to develop and produce the manuscript.
Competing interests: DHI Group supported the time of KU to develop and produce the manuscript only. This does not alter the authors' adherence to all PLoS ONE policies on sharing data and materials.
Unicellular photosynthetic symbionts (Symbiodinium spp.) play a vital role in the energy budget, metabolism and secretion of the calcium carbonate skeleton of scleractinian corals , . The Symbiodinium community associated with scleractinian corals is widely considered to be influenced by host identity and environmental factors and has been shown to shape the coral's tolerance to environmental extremes , . Symbiodinium is a diverse dinoflagellate genus comprising nine phylogenetic clades (A–I), which are subdivided into numerous types based on ribosomal and chloroplast DNA , . Of the nine known clades, six (A–D, F and G) have been identified from scleractinian corals with clades C and D being dominant in the Indo-Pacific. Functional differences among clades and types are known to confer competitive advantages to their host leading to increased resistance to thermal stress (e.g. , , ) and diversification into low light mesophotic habitats , .
Sea surface temperature (SST) is an important influence on the coral-Symbiodinium association under natural conditions – and as a driver of Symbiodinium community shifts under bleaching conditions  Light is also known to exert important controls on the structure of Symbiodinium communities (e.g. ). Studies conducted throughout the Caribbean and Indo-Pacific have found that while some clade C types occur abundantly under a variety of thermal and light conditions, clade D is generally found in warmer water or turbid environments , , . However, the affinity of clade D to certain environments is host-specific and several studies have found clade D types to be more abundant in both shallow, high light environments , ,  and low light or turbid environments (Great Barrier Reef, GBR; –).
Studies of the genetic diversity of Symbiodinium over large-scale spatial gradients have shown geographically distinct populations that differ with latitude or inshore to offshore conditions (e.g. , ). The general conclusion from these studies is that Symbiodinium diversity is driven by acclimatization to local environments (e.g. latitudinal changes in SST; inshore to offshore conditions). Over smaller spatial scales, variation in Symbiodinium community composition across depth gradients ,  has been shown to be greater than over larger horizontal spatial scales , further suggesting that light is an important driver of Symbiodinium diversity. Thus, local-scale patterns cannot be extrapolated to regional scales given that environmental drivers of coral-Symbiodinium associations operate at different spatial scales . In addition to variability in their spatial distributions, Symbiodinium associations are flexible over temporal scales with evidence of shuffling from thermo-sensitive to tolerant types in adult corals during SST anomalies on time scales of months and reverting to their post-bleaching consortia within months or several years , .
The influence of other environmental drivers such as water quality, nutrient levels and sediment-types on Symbiodinium biogeography remains poorly understood . Nutrient levels may play a role given their importance in symbiont metabolism and biomass dynamics , while sediment type may be important as the free-living stage of Symbiodinium associate predominantly with the benthos . A better understanding of the specific environmental drivers of Symbiodinium biogeography is fundamental for prediction of coral community responses to a changing climate. To achieve this, comprehensive studies that examine the influence of multiple predictors are required.
The scleractinian coral Acropora millepora (Ehrenberg, 1834) has been shown to host a variety of Symbiodinium clades and types including C1, C2, A and D (based on ITS1-SCCP or ITS1-QPCR) either individually or simultaneously , , , , . Symbiont populations may undergo change  in response to transplantation to a different environment  or following a natural bleaching event . The flexibility of A. millepora-Symbiodinium associations makes it an ideal model to test the importance of environmental drivers in shaping the distribution of Symbiodinium. This study reports on the correlation between a range of environmental variables and the distribution of Symbiodinium associated with A. millepora collected at different spatial scales: i) along 13° latitude spanning approximately 1,400 km on the GBR, ii) along a persistent water quality gradient in the Whitsunday Islands spanning approximately 65 km , and iii) on populations sampled repeatedly over a number of years at Davies and Trunk Reefs, and the Keppel Islands. The environmental predictors combine satellite data for the regional-scale analysis with water quality samples collected in the Whitsunday Islands for the local-scale analysis. Our results suggest that Symbiodinium distribution in A. millepora is not always primarily driven by temperature, but that it is dependent on the combination of a variety of environmental variables. Further, depending on the thermal history, the spatial and temporal scales over which a study is conducted are likely to influence the patterns observed.
The most prolific symbiont type that was observed in A. millepora was Symbiodinium C2, which was dominant in 982 of the 1,527 samples and present at 42 of the 47 reefs investigated (Figure 1a, Table S1). Symbiodinium C2* (sensu ) was dominant in 274 samples and present at 14 reef locations. Symbiodinium C1 was dominant in 69 samples and present at nine reef locations. Symbiodinium D1 was dominant in 200 samples and present at 11 reef locations (Figure 1a, Table S1). In the Whitsunday Islands, Symbiodinium C2 was the dominant type at all locations sampled. Symbiodinium C1 and D1 occurred at background levels at three inner locations only (Repulse, Lindeman and Long Islands) (Table S1).
Dominant (a) and (c), and background (b) and (d) levels of Symbiodinium. Underlay for (a) and (b) is long-term mean SST (9-year; °C) and for (c) and (d) long-term mean Secchi depth (7-year; m). * indicate local-scale data points, † indicate samples included in temporal analysis. Background levels of Symbiodinium, determined based on co-occurring lower intensity bands, was detected in only 12% of samples; hence the (b) and (d) represent a smaller sample size.
More than one Symbiodinium type was detected in 12% of the samples. There were 83 samples with background levels of Symbiodinium C1 at 10 different reef locations (dominant Symbiodinium C2 although a sample from Miall Island had D1 as its dominant community in 2006) (Figures 1b and d, Table S1). A further 57 samples had background levels of Symbiodinium C2 at eight different reef locations (dominant Symbiodinium C1, and to a lesser extent dominant D1), while 42 samples had background levels of Symbiodinium D1 at eight different reef locations (dominant Symbiodinium C2, and to a lesser extent dominant C1) (Figures 1b and d, Table S1). Finally, two individual samples originating from Whitsunday and Calder Islands hosted background levels of a type belonging to Symbiodinium clade A (Figures 1b and d, Table S1).
Regional-scale patterns, Great Barrier Reef
The Symbiodinium community differed among regions on the GBR (Table 1) although the pairwise comparisons following a Bonferroni correction were unable to discriminate where those differences occurred. Notwithstanding, a multidimensional scaling (MDS) ordination showed that the Symbiodinium communities in regions adjacent to each other at either end of the spatial gradient, i.e. Far Northern and Northern; and Whitsundays and Southern GBR, are more similar to each other and tended to group together (Figure 2).
Symbols: ▵ Far Northern, + Northern, ▪ Whitsundays, ○ Southern GBR. For symbiont types, bold indicates a dominant type and italics are those occurring at background levels.
Results of the marginal tests show that there were several environmental predictors that each explained a significant proportion of the variation in the Symbiodinium community, when considered alone (Table 2). The mud and carbonate content of the sediment explained 27.3% and 18.5%, respectively, of the variation in the Symbiodinium community while anomalies in Secchi depth (1.8%) had the least influence on Symbiodinium communities at regional scales (Table 2). The step-wise model selection eliminated Secchi depth anomalies from the model and the conditional tests associated with the sequential addition of the other predictors were significant for mud content, carbonate content, SST anomaly and mean summer SST (P<0.05; Table 2). Whilst the addition of long-term SST and Secchi depth contributed to the selection of the best model they did not explain significantly more of the variation in the Symbiodinium community (Table 2). Together these environmental predictors explained 51.3% of the regional variation in the Symbiodinium community on the GBR.
The distance-based redundancy ordination (dbRDA) indicated that the first two axes explain 66% of the variability of the fitted model (Figure 3). The first axis was related to both the mud and carbonate content of the sediment while the second axis was strongly related to long-term mean SST and represented the spatial structure in the data with the warmer regions, i.e. Far Northern and Northern, located near the top of the plot while the cooler regions were generally situated in the lower half of the plot.
Symbols: ▵ Far Northern, + Northern, ▪ Whitsundays, ○ Southern GBR.
The distribution of the different Symbiodinium types occurring at regional scales on the GBR was influenced by all of the environmental predictors examined (Table 3). The distribution of Symbiodinium C2 showed non-linear responses to most of the environmental predictors. For example, Symbiodinium C2 occurred in lowest relative abundances at locations with mean summer SST of around 25.5°C and increasing in relative abundance at higher and lower temperatures (Figure 4). Similarly, this symbiont type occurred in greatest relative abundance at locations where the sediments were characterised as having transitional carbonate content, and at locations with a long-term Secchi depth of approximately 13 m (Figure 4).
Solid line shows the model and grey area is the 95% confidence interval. Y-axis is scaled to abundance, values around zero indicate absent symbiont type, negative units are included as they represent the range of confidence limit boundaries.
There was a significant relationship between the distribution of Symbiodinium C2* and mean summer temperature. The greatest abundance of Symbiodinium C2* occurred at locations where the SST values were around 28°C. In addition, there was a greater abundance of Symbiodinium C2* at locations with relatively low carbonate and mud content in the sediments (Figure 4).
The distribution of Symbiodinium D1 was strongly influenced by several environmental predictors (Table 3). This symbiont type showed greatest abundance at locations with high carbonate content of the sediment and with the warmest mean summer SST. Additionally, there was a significant relationship between Symbiodinium D1 and 3-month Secchi depth. Symbiodinium D1 was more abundant at turbid, inner locations with low Secchi depth than at outer locations near the GBR shelf edge (Figure 4).
Symbiodinium C1 generally occurred in low relative abundances throughout the GBR. Nevertheless, the relative abundance of this type tended to be greater at turbid, inner locations with lower Secchi depth than at the outer locations near the GBR shelf edge (Figure 4).
Local-scale patterns, Whitsunday Islands
The Symbiodinium community differed between inner and outer zones in the Whitsunday Islands (Table 4) and the MDS plot showed a clear separation of the Symbiodinium communities between the two zones (Figure 5). Differences between zones were due to background levels of Symbiodinium C1 and D1 at inner locations, which were absent at locations in the outer zone. These two Symbiodinium types together accounted for over 92% of the dissimilarity between zones in the Whitsunday Islands (Table 4).
Symbols: ▾ inner zone, ▴ outer zone. For symbiont types, bold indicates a dominant type and italics are those occurring at background levels. Locations defined as occurring in inner and outer zones of water quality using thresholds described by De'ath and Fabricius (2010) .
Results of the marginal tests show that there were several environmental predictors that individually explained a significant proportion of the variation in the Symbiodinium community (Table 5). The mud content of the sediment, long-term SST and the water quality index (WQI) each explained 80.3%, 39.1% and 37.6% of the variation in the Symbiodinium community, respectively whereas anomalies in Secchi depth (2.5%) had the least influence (Table 5). The step-wise model selection eliminated three of the predictors from the model and the conditional tests associated with the sequential addition was significant for mud content and long-term SST (P<0.05; Table 5). Although the addition of long-term SST, mean summer SST and WQI contributed to the selection of the best model they did not explain significantly more of the variation in the Symbiodinium community. Together these environmental predictors explained 99.9% of the local-scale variation in the Symbiodinium community in the Whitsunday Islands.
The output of the model selection of the dbRDA ordination indicates that the first two axes explained over 95% of the variability of the fitted model (Figure 6). Indeed, the first axis was strongly and positively related to the WQI and negatively related to sediment with dominant mud (60–80%).
Symbols: ▾ inner zone, ▴ outer zone.
In the Whitsunday Islands, Symbiodinium C2 was the dominant type at all locations sampled. Although long-term Secchi depth was the best single predictor model of the environmental variables that were examined, the analyses did not identify any significant environmental predictors of Symbiodinium C2 distribution (Table 6). This was not the case for background levels of Symbiodinium where the WQI had a significant influence on their distribution in the Whitsunday Islands (Table 6). The background levels of Symbiodinium occurred in greatest relative abundance at turbid locations with high WQI, which corresponded to the inner Whitsunday Islands of Repulse, Lindeman and Long Islands.
Temporal changes in distribution of Symbiodinium
Shifts in the Symbiodinium community occurred at four of the six locations sampled as part of the temporal analysis (Table 7). Trunk Reef was sampled in February 2005 and in March 2009. In 2005, Symbiodinium C1 was dominant but changed to Symbiodinium C2* as the dominant type in 2009 (Table S2). North Keppel Island was sampled on five occasions between 2001 and 2009. Symbiodinium C2 was dominant in all colonies sampled in 2001, but changed to a mix of C2 and D1 in July 2002 following a bleaching event in early 2002, followed by a mix of C1, C2 and D in October 2003 reverting back to 100% Symbiodinium C2 dominance by 2009 (Table S2). Miall Island was sampled on three occasions in 2004, 2006 and 2008. In 2004, Symbiodinium C2 was the dominant type but there was a shift to Symbiodinium D1 and mixtures of C1, C2 and D1 after a bleaching in 2006 followed by a change back to predominantly Symbiodinium C2 in 2008 (Table S2). Halfway Island was sampled on seven occasions between 2002 and 2006. Symbiodinium C2 was dominant in all years at this location except 2006 when Symbiodinium D1 was dominant in 40% of samples (Table S2). There were no changes in the assemblage at either Davies Reef or Magnetic Island where the dominant types were Symbiodinium C2* and D1, respectively, over the time period examined.
Each symbiont type associated with the different environmental predictors in contrasting ways over time (Figure 7). As expected, Symbiodinium D1 associated strongly with SST anomalies and mean summer SST. However, the other dominant symbiont types associated more strongly with Secchi depth. Symbiodinium C1 and C2* were associated with mean Secchi depth over the 3-months prior to sampling while Symbiodinium C2 in the Keppel Islands were associated with anomalies in Secchi depth (Figure 7).
Symbols: + Trunk Reef, ▴ North Keppel Is., ▪ Miall Is., • Halfway Is. Colours: red 2001, green 2002, black 2003, navy blue 2004, light blue 2005, pink 2006, yellow 2008, grey 2009. For symbiont types, bold indicates a dominant type and italics are those occurring in background levels.
One of the fundamental gaps underlying studies of Symbiodinium biogeography is the lack of highly resolved spatial and temporal biological and environmental data. A combination of meta-analysis and field data for coral samples, coupled with large-scale satellite data as well as in situ water quality and sediment data provided a high resolution spatio-temporal dataset for this study. This has deepened our understanding of environmental controls of the patterns of Symbiodinium diversity and distribution in A. millepora by establishing that factors other than SST influence Symbiodinium biogeography and local- and regional-scale patterns are influenced by a variety of factors.
Regional-scale drivers of symbiont communities
Our results show that spatial and temporal scales are important for determining the environmental drivers that have the strongest influence on Symbiodinium associations in A. millepora on the GBR. At regional scales, the patterns of variability in Symbiodinium distribution were best explained by a combination of mud and carbonate content as well as SST anomalies and mean summer SST. Sediment types can influence the level of resuspension in the water column and therefore light levels but may also act as a reservoir of Symbiodinium for uptake by corals such as A. millepora that acquire new symbionts from their environment every generation. It is unknown how sediments influence the symbiont community in corals, but since the free-living stage of Symbiodinium is predominantly sediment-associated , it is conceivable that sediment type and particle size could influence the ecology of the free-living symbionts. While the spatial distribution of mud and carbonate broadly co-vary with distance from shore and water clarity (as a proxy for light), our data show that water clarity per se (here measured as Secchi depth) correlates weakly with symbiont type suggesting that factors other than distance from shore are implicated.
Anomalies in SST and mean summer SST that exceed the thermal tolerance of corals are conducive to bleaching conditions and may drive the shuffling of Symbiodinium types as observed by  and  for A. millepora. The GBR-wide distribution of the most abundant symbiont type, Symbiodinium C2, appears to be driven by long-term SST, mean summer SST as well as long-term and 3-month Secchi depth and mud content of the sediment, suggesting that it is adapted to a broad range of mean, non-anomalous, temperature regimes and water quality conditions. The fact that the remaining Symbiodinium types associated strongly with the optical properties of the water column and sediment composition suggests that water clarity and possibly nutrient levels may play a role in less abundant Symbiodinium consortia, with anomalous thermal regimes an important co-driver.
The distribution of Symbiodinium D1 was strongly related to many of the environmental predictors that were examined. Previous studies have focused predominantly on temperature and have found a strong association between temperature extremes and D1 prevalence , . However, our results suggest that water clarity and sediment type may also be important factors governing the distribution of D1. Although the association of D1 with water clarity is generally consistent with the conclusion of LaJeunesse et al. (2010) , we suggest that caution be applied in interpreting results where the standard chlorophyll-a concentration algorithm  is used as a measure of water clarity in shallow coral reef waters, especially at low (e.g. 24 sq km) resolution. The empirical chlorophyll-a concentration algorithm was developed for open ocean Case-1 waters  and is unable to correct for bottom reflectance or the presence of scattering particles resulting in significant contamination of the signal in shallow or turbid (Case 2) waters.
Symbiodinium clade D is pandemic but uncommon on a global-scale, occurring predominantly on reefs that are subjected to periodic stress or that have a history of bleaching. As such, clade D types have been described as opportunistic endosymbionts that are able to out-compete other types in health-compromised corals . This view is inconsistent with the observation of stable D1 symbiont communities in A. millepora at locations such as Magnetic Island, which is difficult to classify as “health-compromised” in the context of coral cover, juvenile coral recruitment, or coral species diversity . Here, D1 prevalence has been shown to be governed by a combination of environmental predictors, hence it is unlikely that stress conditions alone drive their abundance. Rather, responses to environmental conditions coupled with possible local adaptation operate in concert to fulfil their physiological requirements , , .
Influence of local-scale variation in environmental drivers (water quality) on Symbiodinium distribution
Aside from SST and light levels, environmental variables such as water quality have generally not been considered previously as environmental controls on the distribution of Symbiodinium, despite having known effects on symbiont density (e.g. , ) and photo-physiology , . The environmental gradients observed across the Whitsunday Island region are stronger and more persistent than those observed along the GBR ,  and have been linked to changes in photo-physiology and coral assemblages with increasing distance away from the discharge of two local rivers , , . The pattern of variability of Symbiodinium types was best explained by the mud content of sediment, the gradient of which is particularly strong in the Whitsunday Islands. Our local-scale results also show that the distribution of Symbiodinium C2 was best explained by long-term Secchi depth, highlighting again that water quality, and possibly nutrient levels, are important drivers of Symbiodinium distribution. Further, Secchi depth has previously been shown to correlate with large-scale differences in Mesoamerican symbiont communities . As such, water clarity can exert strong local structuring on the marine environment due to terrestrial runoff , and wind driven resuspension of sediments , that in turn can drive changes at all trophic levels on coral reefs.
It is unclear why Secchi depth related more strongly to Symbiodinium C2 at a local-scale compared to the regional GBR-scale. It may simply be a function of higher local-scale sampling intensity of the environmental gradients, which could produce stronger statistical associations. On the other hand, Oliver and Palumbi (2009)  also found that regional-scale thermal correlates could not be demonstrated in the west Pacific. They attributed their findings to other factors such as host responses, other environmental drivers, or within-type physiological diversity. Given the high potential for local adaptation of Symbiodinium as a result of large population sizes, significant existing heritable genetic variation in physiological performance , , and restricted gene flow among GBR populations , it should not be surprising that responses differ between regional and local scales. The possibility that local-scale environmental conditions may structure Symbiodinium associations in contrasting ways to those observed at larger spatial scales warrants further investigation.
Temporal variability & acclimatization
The occurrence of temporally variable symbiont communities at some locations and not at others is an issue that remains poorly understood. Three of the four sites where substantial temporal changes took place occurred in the Keppel Island group. Symbiont shuffling in this area has been documented following a natural bleaching event in early 2006  but has clearly also taken place previously as a result of bleaching in 2002 . Similarly, A. millepora at Trunk Reef in the central GBR underwent a shift from Symbiodinium C1 towards the end of a warm summer in 2005 to Symbiodinium C2 in 2009. This is the first documented case of temporal symbiont variability on an offshore reef on the GBR indicating that shuffling is not restricted to the more environmentally variable inshore reefs. It is worth noting that all of the temporal changes in symbiont communities presented can be directly correlated to thermal stress (Keppels: 2002 and 2006 bleaching events; Trunk Reef: 2005). This highlights the importance of thermal stress as the driver of symbiont change and the need for standardizing data to non-stressful periods prior to undertaking large-scale analyses to avoid extra sources of variation. The stronger association of Symbiodinium C1 with Secchi depth than with temperature is probably an artefact of the data since it is influenced substantially by a successional change in symbiont types at North Keppel and Miall Islands after bleaching. At these sites symbiont communities changed from Symbiodinium C2 to Symbiodinium D1 and C1 dominance during and after bleaching, and remained as a mix of predominantly Symbiodinium C1 and Symbiodinium D1 over following months, eventually drifting back to C2 dominance over a period of 1–2 years. Symbiodinium C1 is considered thermo-tolerant  with a photo-physiology that allows it to out-compete Symbiodinium D1 over a period of time until it is itself out-competed by Symbiodinium C2 –. Conversely, symbiont communities remained stable during, and following, the 2002 bleaching event at Magnetic Island (100% D1 dominant) and Davies Reef (100% C2* dominant). These results highlight our limited understanding, not only of the factor(s) that influence symbiont shuffling, but also of the prerequisite symbiont makeup and densities that are required for shuffling to take place.
In summary, given the importance of Symbiodinium for holobiont metabolism and health, understanding the environmental controls on the distribution of symbiont types is crucial if we are to manage the resilience of coral reefs in an era of rapid environmental change. Modelling of Symbiodinium community structure as well as accumulation of large-scale data in space and time through meta-analysis and satellite imagery is important to allow reliable predictions of biological responses to environmental changes. Our findings highlight that drivers of specific associations between Symbiodinium and A. millepora are multiple and varied depending on the spatial and temporal scale at which investigations took place. At larger scales, SST variables are important drivers whereas local-scale patterns can be explained by variables that are affected by environmental gradients caused by local events. Importantly, this study is unique among other large-scale studies in that the samples all come from the same coral species, which avoids possible confounding of patterns due to host identity, thus reducing the risk of spurious environmental correlations.
Materials and Methods
Sampling of A. millepora was divided into two studies based on spatial scales. The first component focused on a regional scale incorporating 47 inner and outer coral reefs across 13° latitude (11°–24°S) of the GBR (Figure 1). In total, dominant and background levels of Symbiodinium in 1,527 coral samples were analysed with sampling undertaken between 2001 and 2009 and within-reef replication of 1–79 colonies (mode = 10). The second component focused on 8 of the 47 coral reefs situated in the Whitsunday Islands region (20°00′–30′S and 148°45′–149°15′E) of the GBR. This region is characterised by a persistent environmental gradient with significant changes in irradiance, sediments and water column nutrients from inner to outer locations with increasing distance away from the discharge of two rivers . In total, 79 Symbiodinium samples were analysed from eight locations in the Whitsunday Islands with sampling done in January 2007 and within-reef replication of 10 colonies (mode = 10).
To investigate the temporal variability in Symbiodinium communities, six locations (Davies Reef, Magnetic Island, Miall Island, North Keppel Island, Trunk Reef, Halfway Island) were sampled repeatedly (n = 2–7 times) between 2001 and 2009 and within-reef replication of 7–79 colonies (mode = 10).
For all collections at each location, branches (∼3–5 cm long) of A. millepora were collected from adult colonies occurring at a depth of 1–7 m below lowest astronomical tide (LAT), generally on the leeward side of the reef. Acropora millepora generally occurs on the mid- to upper reef slope, including the reef flat on inshore sites, but not on offshore sites where its close congener, A. spathulata, is more common. To avoid biasing our collections with respect to water clarity, collections deliberately covered the full depth range of A. millepora with collections at 32% of sites including a minimum depth of >2 m and 62% with a maximum depth of >4 m.
All samples were preserved in absolute ethanol. DNA extraction was carried out using Wayne's method  and PCR amplification was conducted following . Genetic identification of Symbiodinium types hosted by A. millepora colonies was performed using single-stranded conformation polymorphism (SSCP) of the ITS1 region of the nuclear rDNA , which has a lower detection limit of 5–10% relative abundance but does not rule out the presence of symbionts below the detection limits . This technique was used because it allowed us to include the results of a relatively large body of literature of A. millepora samples that have been genotyped using SSCP with newly genotyped samples. Samples were identified against known Symbiodinium SSCP profiles with dominant and background levels identified based on band intensity on the SSCP gel as per the example in Figure 8. PCR products giving distinct SSCP profiles were cloned and sequenced to confirm genotypes (Symbiodinium C1: Gen Bank Accession numbers AF380551, EU189440 –1, EU189444 – 7; Symbiodinium C2: AF380552, EU189442 – 3, EU189448 – 9; Symbiodinium C2*: AY643495 – AY643498; and Symbiodinium D1: EU02479, EU189450 – 5).
The image illustrates the link between band intensity and how relative abundance (dominant or background) of Symbiodinium strains was determined for individual samples. Samples in Bold = dominant, Bold/Normal = dominant/background, Normal/Normal = equal band intensities, Bold Italics/Normal = slight dominance/significant background.
SST and Secchi Depth.
The environmental data used in the analysis included Moderate Resolution Imaging Spectroradiometer (MODIS) satellite data from which a number of temperature and Secchi depth (as a measure of water quality) metrics were derived. Daily MODIS data were acquired directly from the NASA Ocean Biology Processing Group (oceancolor.gsfc.nasa.gov) for the period 2000 to 2009 and various time series generated at 1 km spatial resolution. The SST metrics included the long-term (9-year) mean SST, mean summer SST (01-Dec to 28-Feb) and summer SST anomalies, which were determined as the difference between the previous 3-month summer mean and the long-term summer mean. Both day- and night-time SST data were used.
Recent developments in remote sensing application include the development of an operational algorithm to determine the euphotic zone depth (Zeu%), a direct measure of water clarity . The quasi-analytical (QAA) algorithm is based on the inherent optical properties of the water column, a function of absorption and backscattering , to determine Zeu% in eutrophic coastal and complex waters. For this study, we used a GBR-validated Secchi depth algorithm, generated by matching the 10% euphotic depth level (Zeu10%) against GBR Secchi data (1997–2010) as follows: MODIS and SeaWiFS Level-1 (oceancolor.gsfc.nasa.gov) satellite/in situ data matchups were rigorously selected to ensure optimal accuracy. The matched in situ Secchi data were further regressed against the QAA 10% light level (Zeu10%) algorithm and a Type II linear regression (RMA) of log-transformed satellite and in situ data used to fine-tune the Secchi depth (Zsd) returned from the QAA algorithm, to generate a GBR-validated Zsd algorithm . The algorithm was implemented and applied to the full regional time series of MODIS Aqua data (2002–2010). Daily, monthly and climatological means were generated at 1 km resolution for further analyses.
The Secchi depth metrics included the long-term (7-year; 2002–2009) mean Secchi depth, mean Secchi depth for 3 months prior to sampling date, and Secchi depth anomalies. The Secchi depth anomalies were determined as the difference between the means of the 3-months prior to coral sampling and the 3-month long-term means (2002–2009) for that same period. The long-term means were calculated for the 3-month periods over the 7-year Secchi depth data series.
To maintain consistency between data points, Secchi depth data were extracted from the same locations used for extracting the SST values. However, to avoid any potential bottom contamination, particularly at the inshore locations, we compared the physical depth at each location with the 7-year long-term Secchi mean. Where the physical depth was shallower than the long-term mean Secchi depth, an alternative pixel location was manually selected by adjusting the station location to the closest pixel with a physical depth that exceeded the 7-year long-term Secchi mean.
Mud and carbonate sediment data were obtained from . Carbonate content was derived by measurement of the amount of acid-soluble material and divided in the following categories: i) Pure carbonate facies (>90%), ii) High carbonate facies (80–90%), iii) Impure carbonate facies (60–80%), iv) Transitional facies (40–60%), v) Terrigenous facies (20–40%), and vi) High terrigenous facies (<20%). Terrigenous mud content is divided into the following categories based on the content of mud: i) Pure mud (>80%), ii) Dominant mud (60–80%, iii) Very high mud (40–60%), iv) High mud (20–40%), v) Moderate mud (10–20%), vi) Low mud (1–10%), and vii) Non-mud facies, composed predominantly of sand (<1%).
Data were collected for thirteen irradiance and water-column nutrient variables at each of the coral sampling locations in the Whitsunday Islands during water quality sampling undertaken from August 2004 to January 2007 . The irradiance measurements included Secchi- and optical depth, while surface water was collected for measurements of chlorophyll a, phaeophytin, particulate nitrogen (PN), particulate phosphorus (PP), particulate organic carbon (POC), dissolved inorganic nitrogen (DIN: NH4, NO2, NO3), dissolved inorganic phosphorus (DIP: PO4), total dissolved nutrients (total dissolved nitrogen [TDN], total dissolved phosphorus [TDP]) and dissolved organic nutrients (dissolved organic nitrogen [DON] and dissolved organic phosphorus [DOP]). Analysis of the water samples followed standard analytical procedures described in . Since many of these variables are known to be highly correlated with each other, a water quality index (WQI; further details see , ) was calculated for use as an environmental predictor in the analyses using the sum of a z-score transformation for the irradiance and water-column nutrient variables.
Differences in communities of Symbiodinium among regions on the GBR (regional-scale study) and along a persistent water quality gradient in the Whitsunday Islands (local-scale study) were examined with multivariate procedures. For each study, spatial variation among communities of Symbiodinium was examined graphically using multidimensional scaling (MDS) ordination. The adequacy of the two-dimensional representation was assessed by examining the stress value. Stress <0.1 indicates that the ordination has accurately represented the relationships among the samples, but values greater than 0.25 indicate that the ordination may have misrepresented the data .Variation in Symbiodinium communities among four regions on the GBR (Far Northern, Northern, Whitsundays and Southern GBR; regional-scale study) and between inner and outer zones of the Whitsunday Islands (local-scale study) were analysed with one-way analyses of similarities (ANOSIM) using the Bray-Curtis similarity measure. Pairwise comparisons were used to test for differences between pairs of samples when ANOSIM was significant and a Bonferroni correction was used to control the probability of Type I error. Where differences in Symbiodinium communities were detected, the type contributing the most to the dissimilarity was identified using similarity of percentages (SIMPER) analyses. The zones of water quality were based on the thresholds described by ; inner locations with levels of water column chlorophyll-a >0.45 µg l−1, outer locations with <0.45 µg l−1. The MDS and ANOSIM tests were done using dominant and background levels of Symbiodinium, each specified separately, in PRIMER6 with PERMANOVA+, as described by , .
Modelling of the relationship between the Symbiodinium community and the environmental predictor variables was done using distance-based redundancy analysis (dbRDA) following techniques described by , . The importance of each environmental predictor was first assessed individually in marginal tests. A stepwise procedure with variable selection based on adjusted R2 was then used to identify the model of environmental predictors that best explained the dissimilarity among Symbiodinium types in their patterns of abundance. The predictors were fitted sequentially by either adding or subtracting from the model and the results presented are sequential tests for the inclusion of each successive predictor based on the selection of those preceding them in the output. Co-linearity among the environmental predictors was tested prior to analysis and variables that were highly correlated were omitted from the analysis. The sediment data (categorical) were treated as binary in the environmental dataset. The dbRDAs were done using DISTLM in PRIMER6 with PERMANOVA+, as described by , .
The influence of the environmental predictors on the distribution of the dominant Symbiodinium types (e.g. C1, C2, C2* and D1) was then examined using generalized additive models (GAMs). Given the low number of samples where background levels of Symbiodinium were detected, individual analyses for each background type was not possible and hence the analyses focused on dominant Symbiodinium types and a pooled background type.
For the temporal component of the study, a Pearson Chi-squared test was used to determine shuffling between dominant Symbiodinium types at six locations (Magnetic, Halfway, Miall and North Keppel Islands, and Davies and Trunk Reefs) where sufficient samples had been collected on multiple occasions through time (2002–2006). The GAMs and temporal analyses were done using the statistical package R .
Summary of sampling locations and date, Symbiodinium types, number of replicates and source of data.
This project was conducted under the following Great Barrier Reef Marine Park Authority permits: G02/4011.1, G05/12807.1, G06/15571.1, G06/19473.1, G07/26114.1, G08/26994.1, G09/29833.1, G09/31654.1. We gratefully acknowledge the NASA Ocean Biology Processing Group for provision of MODIS satellite data.
Conceived and designed the experiments: TC RB KU MvO. Performed the experiments: TC RB KU AMJ JD SW MC. Analyzed the data: TC KU BR RO. Contributed reagents/materials/analysis tools: RB SW MvO. Wrote the paper: TC RB KU SW MvO.
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