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Article

Population Genetics Assessment of the Model Coral Species Stylophora pistillata from Eilat, the Red Sea

by
Elad Nehoray Rachmilovitz
1,2,*,
Jacob Douek
1,* and
Baruch Rinkevich
1,*
1
Israel Oceanographic and Limnological Research, National Institute of Oceanography, Tel Shikmona, P.O. Box 2336, Haifa 3102201, Israel
2
Department of Marine Biology, Leon H. Charney School of Marine Sciences, University of Haifa, Mount Carmel, Haifa 3498838, Israel
*
Authors to whom correspondence should be addressed.
J. Mar. Sci. Eng. 2024, 12(2), 315; https://doi.org/10.3390/jmse12020315
Submission received: 11 January 2024 / Revised: 10 February 2024 / Accepted: 11 February 2024 / Published: 12 February 2024
(This article belongs to the Section Marine Biology)

Abstract

:
The successful management of coral reefs necessitates understanding the genetic characteristics of reefs’ populations since levels of genetic diversity play a critical role in their resilience, enabling them to withstand environmental changes with greater efficacy. To assess the genetic diversity and connectivity of the widespread Indo-Pacific coral, Stylophora pistillata, eight microsatellite loci were employed on 380 tissue samples collected from eight sites along the northern Gulf of Eilat, Red Sea. We documented deviations from the Hardy–Weinberg equilibrium and observed low heterozygosity and high values of expected heterozygosity (0.59 and 0.82, respectively). The relatively high FST values and STRUCTURE analysis results showed population fragmentation along the short coastline (<12 km). These results signify isolation by distance, low gene flow between most populations, and possible non-random mating. These results are connected to this species’ sexual reproduction traits, a brooding coral species with planulae that settle shortly upon release with limited connectivity that are most probably further exacerbated by anthropogenic impacts imposed on Eilat’s reefs. This study provides insights into the connectivity and population genetics of S. pistillata residing in an urbanized northern Red Sea reef and reinforces the need for better management of the current MPA, employing future active coral reef restoration in the area.

1. Introduction

Genetic diversity plays a pivotal role in the processes of speciation and adaptation, influencing not only a specie’s resilience but also its ability to withstand catastrophic events and respond to climate change that may otherwise lead to extinction [1,2,3,4]. This principle is also valid for coral reefs, one of the most diverse ecosystems on earth, which host over a quarter of all known marine species [5,6] in less than 0.2% of the earth’s surface [7]. Scleractinian corals are the keystone species in the coral reefs and are further considered as the ecosystem engineers of coral reefs [8,9,10,11]. Corals are extremely sensitive to environmental changes; thus, the continuous anthropogenic impacts and global climate change pressures they face (such as mass bleaching and coral mortality following the heating oceans, decreased levels of calcification due to seawater acidification, habitat degradation, algae/coral phase shifts, overfishing, tourist activities, diseases, and other interacting stressors [12,13]) are leading to the global decline of coral reefs. The ICRE report for 2020 indicates that over half of the world’s coral reefs have already been lost, projecting that the anticipated 2 °C increase in seawater temperatures over the next two decades might lead to the loss of over 99% of coral reefs [14]. As coral reefs decline globally, there is a need for better management tools and improved conservation and restoration protocols [15,16,17]. An important aspect of steering the future of coral reefs involves managing their genetic diversity: the higher the genetic diversity at the commencement of conservation or restoration ventures, the greater the potential for sustained success over the long term [18,19,20]. Hence, to ensure the success of any restoration initiative or conservation plan, it is imperative to first evaluate the genetic diversity prior to any conservation and/or rehabilitation action of the targeted species.
The genetic diversity of a species is primarily shaped by genetic drift, selection, and migration [21,22]. As in other marine ecosystems, scleractinian coral populations are theoretically open to gene exchange with distant reefs. Scleractinian corals are sessile organisms and depend on the planktonic movement of gametes and larvae for gene exchange. Since tracking those gametes and larvae is virtually impossible, the population genetic of scleractinian corals relies on studying adult populations rather than their larvae [22,23,24].
Population genetics studies commonly use the efficient molecular markers of microsatellite loci [25], and this is also the case with corals [26]. To analyze the population genetics of coral species along the Israeli coast of the Gulf of Eilat, northern Red Sea, we employed eight microsatellite markers on the ‘smooth cauliflower’ coral Stylophora pistillata (Esper 1797) (Figure 1). This branching coral is a common and widespread Indo-Pacific species of the family Pocilloporidae [27,28,29]. While S. pistillata’s sexual reproduction traits have been thoroughly studied in the northern Gulf of Eilat [27,28], little is known about its population genetics [30,31]. In this research, we endeavor to explore the population genetics properties of this species by collecting samples from a wide range of sites along the Israeli coast of the Red Sea and, for the first time, also from shallow- and deep-water sites. We hope that this initiative might shed light on the coral population genetics in the gulf, which can then be translated into a better understanding and improved management practices of the urbanized coral reefs in the Gulf of Eilat and used to harness the ecological engineering properties of this species [28,32] for the ‘reef of tomorrow’.

2. Materials and Methods

2.1. Stylophora Pistillata Sampling

Tissue samples of 380 Stylophora pistillata colonies were collected by SCUBA diving from 8 reef sites along the Israeli coast in the Gulf of Eilat (Figure 2 and Table 1 for site locations, depths, number of samples collected at each site, and collection dates), in accordance with the Israeli Nature and National Parks Protection Authority permits 2016/41540, 2020/42540, and 2021/42878. A single branch tip (about 1 cm3) was clipped off, using electrician clippers, from each sampled large coral colony (>15 cm in diameter) and placed in a 5 mL plastic vial submerged in seawater. Each colony was sampled only once, and the next sampled colony was haphazardly chosen at least 4 m away. The collected samples were brought to the laboratory at the InterUniversity Institute (IUI) for marine sciences in Eilat, and each sample underwent a brief drying process on dry paper towels for less than a minute and was then individually placed in a new 1.5 mL vial containing a solution of 200 µL of lysis buffer (0.25 M Trisborate pH 8.2, 0.1 M EDTA, 2% SDS and 0.1 M NaCl), 40 µL of 5 M sodium perchlorate, and 240 µL of phenol:chloroform:isoamyl alcohol (25:24:1) [33] and stored at 4 °C.

2.2. Genomic DNA Extraction

The samples were transported in a cooler box with ice packs from Eilat to the Israel Oceanographic and Limnological Research Institute (IOLR) in Haifa, Israel. DNA extraction from each coral sample followed the protocols outlined by Graham [34] and Douek et al. [33] of phenol/chloroform extraction and ethanol precipitation. The integrity and the quantity of each genomic DNA were assessed using a NanoDrop 2000 (Thermofisher Scientific, Inc., Pittsburgh, PA, USA). Samples were held at 4 °C until further analyses.

2.3. Microsatellite Amplification and Analysis

Microsatellite alleles (developed for Stylophora sp. from the Red Sea [35]) for each DNA sample were amplified according to [35] in 11 µL of the total volume containing 2 μL of the DNA sample (diluted 1:50 with DDW, 50–100 ng/µL), 0.1 μL of the two primers, forward and reverse mix (different dyes were used for different reactions, Table 2), 3.9 μL of DDW, and 5 μL of ready-to-use commercial Taq polymerase mixture (2× Taq PCR MasterMix (Tiangen Biotech, Beijing, China). The conditions for the PCR cycles (in Mastercycler X50s thermocycler, Eppendorf, Hamburg, Germany) were an initial denaturation step at 95 °C (5 min), followed by 25 cycles at 94 °C (30 s), 55 °C (90 s), and 72 °C (60 s), and a final extension at 60 °C for 30 min [27,35]. The fluorescent-labeled PCR products were examined in an agarose gel (1.5%). Positive PCR products were prepared for analyses by mixing 0.25 μL of each amplification product labeled with VIC, FAM, NED, and PET, and 0.4 μL of LIZ size standard (MapMarker DY632, 50–500 bp, BioVenture Inc. Murfreeboro, TN, USA) was added, as well as 8.6 μL of HiDi Formamide (Thermofisher Scientific, Inc., Pittsburgh, PA, USA). Samples were analyzed off site (ABI PRISM 3100 Genetic Analyzer, Applied Biosystems, Foster City, CA, USA); to the DNA Sequencing Facility, Department of Biochemistry, University of Cambridge, Cambridge UK). The chromatograms of the fluorescent amplification products were scored and binned at the IOLR using the genotyping software Geneious Prime version 2023.2 with the Microsatellites Plugin [36,37].

2.4. Data Analysis

We used GenAlEx software version 6.5 [38,39] to calculate the number of alleles, frequencies, observed heterozygosity (HO), and expected heterozygosity (HE). The number of private alleles, genetic differentiation among populations (FST), and the fixation index (F) were established and used to investigate the deviation from the Hardy–Weinberg equilibrium (HWE). A Mantel test for pairwise geographic distance between populations versus pairwise genetic distance (FST) was employed to evaluate isolation by distance. To assess the significance of all estimates, we employed an analysis of molecular variance (AMOVA) utilizing 999 random permutations. This approach was used to quantify the proportion of genetic variation between locations. The genotypic structure analysis of the population was conducted using STRUCTURE software version 2.3.4 (July 2012) [40] with the following defining parameters: each run consisted of 100,000 iterations with a burn-in of 100,000 for each value of K, from K = 1–20, and with randomize turned off. The results were entered into STRUCTURE Harvester web version 0.6.94 (July 2014) [41], estimating the most likely value of K. BAPS software version 5.3 (October 2009) [42] was used for a Bayesian analysis of population structure to establish genetic distances and relationships between populations. A factorial analysis of correspondence (FAC) for relationships between populations was carried out with GENETIX software version 4.05 (January 2004) [43]. A dendrogram describing the genetic distances and relationships between the coral populations was generated using POPTREE2 software (December 2013) based on distance (DA) [44] and refined using MEGA11 software version 11.0.13 (June 2022) [45]. CERVUS software version 3.0.7 [46] was used to produce polymorphic information content (PIC) analysis and to calculate the significance of deviation from the Hardy–Weinberg equilibrium.

3. Results

Each of the 380 Stylophora pistillata DNA samples was PCR amplified using eight fluorescent microsatellite markers. Analyses of all PCR products (eight per sample, 380 samples) from all collection sites showed high allelic diversity, ranging from 24 alleles (locus Stylo_72) to 61 (locus Stylo_45). Observed heterozygosity (HO) values for each of the eight loci ranged from 0.43 to 0.73, and the overall value was 0.59 ± 0.02 (mean ± SE; Table 3). Expected heterozygosity (HE) at the eight loci ranged from 0.78 to 0.87, and the overall value was 0.82 ± 0.01 (Table 3). The fixation index (F) for each locus ranged from 0.08 (Stylo_80) to 0.46 (Stylo_48) with a total average of 0.28 ± 0.03 (Table 3. Results further revealed that the S. pistillata populations diverged from the Hardy–Weinberg equilibrium (Table 3). The polymorphic information content (PIC) values ranged from 0.88 to 0.95 for the eight loci. Analyses of the microsatellite data by population (according to their collection sites) revealed that the Dekel beach shallow site had the highest average number of alleles of all loci per site (14.13 ± 1.29), while the Lighthouse beach shallow site had the lowest value of average number of alleles on all loci, 10 ± 0.93 (Table 4). HO ranged from 0.46 ± 0.08 (North beach site) to 0.72 ± 0.06 (Dekel beach shallow), averaging 0.59 ± 0.02 at all sites (Table 4). HE ranged from 0.75 ± 0.03 at the Jorden Border beach to 0.87 ± 0.01 at the Dekel beach shallow site (mean = 0.82 ± 0.01) (Table 4).
Pairwise FST values performed on collection sites ranged from 0.037 between the shallow and deep sites at the Dekel beach to 0.205 between the North Shore beach and the Aqaba Border sites. The average for all pairwise analyses was 0.0998 (Table 5). The variance calculated by AMOVA was 0.38 (10%) among populations and 3.341 (90%) within populations. In total, FST based on the standard permutation across the full dataset was 0.102 and was significantly different among populations (p < 0.001) (Table 6). A Mantel test for pairwise geographic distance between populations versus pairwise genetic distance (FST) was not significant (p ≤ 0.08), with an R2 of 0.0358 (Supplementary Figure S1).
Assessing the likelihood of assigned alleles as originating from the same site population or other populations showed a high chance of ‘self-site’ assignment (87%; Table 7). North Shore beach had 100% ‘self-site’ assignment, while the Egypt Border site had the lowest ‘self-site’ assignment (57%; Figure 3, Table 7).
A 3D factorial analysis of correspondence (FAC) carried out with GENETIX showed three main clusters: one consisting only of the North beach, the second encompassing the two sampling depths at the Dekel beach site, and the third entailing all other sites with some internal differentiation and zonation to each sampling site (Figure 4).
The clustering of individual plots by STRUCTURE suggests the presence of four distinct genetic clusters with a K value of 4, as suggested by Structure Harvester. In this arrangement, JB, KI, UO, and LIS formed one clustered population. Another clustered population encompassed TY, LID, and EB sites, while North Shore beach is considered as a population on its own. Both deep and shallow water samples at the Dekel beach site clustered together as the fourth population (Figure 5, top). BAPS clustering of individual plots showed an optimal K value of seven populations where both sampling depths at the Dekel beach site were clustered together as one population, Kisosky beach and Underwater Observatory beach were clustered together as one population, and Tour Yam beach and Egypt Border beach formed an additional population. JB, NB, LIS, and LID were each considered as a separate population (Figure 5, bottom).
POPTREE2 generated a dendrogram illustrating the genetic distances and relationships among populations through distance (Da) analysis. According to this dendrogram, North Shore beach emerged as a distinct population when compared to all other sampling sites. The shallow- and deep-water sampling depths at Dekel beach represented a separated population from all other sites, which further clustered into two additional groups, the first consisted of Kisoski beach and Underwater Observatory beach together, as compared to the external branch of the Lighthouse beach (both shallow- and deep-water sites) that emerged as an external group. The second group consists of the Egypt Border beach and Tour Yam beach together with Jordan Border beach as a separate population (Supplementary Figure S2).

4. Discussion

In this study, we analyzed 380 tissue samples of adult Stylophora pistillata colonies collected from eight locations along the whole Israeli coastal reef in the northern Gulf of Eilat, Red Sea (a 12 km coastline from the Jordanian border to the Egyptian border, a highly urbanized coral reef area). DNA samples were amplified for eight microsatellite loci to create a dataset that characterizes the basic population genetics of S. pistillata in the region. While focusing only on the Israeli reefs at the Gulf of Eilat, analyzing the dataset revealed relatively low observed heterozygosity (HO) against high expected heterozygosity (HE), implying a non-stable distribution of genetic variation in all studied S. pistillata populations over generations, some of which are probably related to non-random mating. Clearly, additional work is needed for the whole Gulf of Eilat evaluations, including sites from Jordan, Egypt, and Saudi Arabia, to increase the dataset and improve and strengthen the conclusions.
Our results revealed that the entire studied S. pistillata populations along the 12 km of the coastal contour of the Israeli coast are sub-divided into several isolated populations. This surprising outcome is further supported by the positive F values, indicating low gene flow between most populations, further bolstering isolation by short distances of several hundred meters to a few kilometers, and also by the results supporting high levels of inbreeding within each studied site. The above conclusion is in line with Zvuloni et al.’s [30] outcomes, showing significant genetic differences in the rDNA ITS among two S. pistillata populations in the northern gulf, separated by ≤10 km. Yet, the above population structure of S. pistillata from the most northern part of the Red Sea does not corroborate with other populations of this widely distributed coral species. For example, Takabayashi et al. [47] have documented panmixia between S. pistillata populations in the Western Pacific separated by distances over thousands of kilometers. In addition, Monroe [31] showed no distinctive population structure across the length of the Red Sea (spanning approximately 2000 km of the Saudi Arabian reefs between Maqnah in the north and the Farasan Islands in the south) but showed a greater population structure on a fine scale, suggesting genetic selection based on fine-scale environmental variations.
S. pistillata is a hermaphroditic and brooding coral species, where oocytes are fertilized by sperm originating from neighboring colonies. In many marine invertebrates with such internal fertilization, sperm usually travel limited distances, estimated at a few meters and up to a few hundreds of meters [48,49,50,51], increasing the possibility of within site inbreeding. Gravid S. pistillata colonies release mature planula larvae almost 8 months/year [27,52,53]. These larvae are short-term swimmers with a limited planktonic phase, where >28% settle within 12 h from release, and the vast majority of settlers (60–80% of released larvae) are recorded within the first 48 h after their release [54,55]. While under laboratory conditions, larvae continue to swim for over a month; only a few larvae continue to settle after the first 2–3 days and within the first week upon release. These biological features lead to a considerable number of planulae that settle near their maternal colonies within the source site and restrict the actual dispersal into a short geographical range, further supporting the significant genetic differences recorded between the sites studied over a short coastline of about 12 km long, and enhanced inbreeding. While modeling larval connectivity and their dispersal in the northern Gulf of Eilat, Berenshtein et al. [56] concluded that the majority of larval supply is within closely situated sites, allowing only a limited flow from north to south trajectory. Berenshtein et al. [56] showed that the movement of planulae was greatly reduced over 20 km of distance, further suggesting the existence of physical barriers that isolate distant sites, a notion further supported by an additional model for coral larvae dispersal [57]. This model further predicts connections between the two sides of the gulf (not studied here) and the possible contributions of reef sites located further to the south [56].
Pairwise FST analyses showed that the three most northern sites, JB, NB, and KI, which are close to each other, about 0.8–1.2 km apart, significantly differentiate. This result may reflect physical parameters, such as water currents and bathymetry of the area, on top of the continued anthropogenic pressures. The northern part of the Gulf of Eilat depicts a relatively closed water system that is supplied through the straights of Tiran at the south by a chain of eddies along the south-to-north axis [58], creating a relatively mixed sea on an annual scale, and these eddies might trap planula in the direction of a certain areas or cast them out to either into the open sea or toward sandy flats where they cannot settle [59,60]. The bathymetry at the northern tip of the gulf is relatively uniform, composed of relatively sandy flats with very patchy reef modules, which do not offer many settlement sites for planulae [59] when compared to the southern areas that have more pronounced and uniform reef formations [61]. It is evident that the whole northern tip of the Gulf of Eilat is heavily impacted by anthropogenic stressors, such as continuous municipal development, municipal sewage, marine constructions, and other diverse maritime activities (commercial ports, phosphate and nitrogen loading docks, oil platforms, and ship anchoring) and recreational diving pressure [30,62,63,64,65,66,67,68,69]. These anthropogenic impacts cause continuous degradation of the reef [70,71], creating a fragmented urbanized reef [72,73] with high possible impacts on coral population genetics. These proposed anthropogenic and physical conditions at the North Shore beach site might have extreme effects of isolating coral populations in this area from other surrounding populations. At the southern sites (TY, UO, LI, and EB), the S. pistillata populations, while still differentiating from each other, exhibit elevated connectivity among them. These results reveal heightened genetic mixing at the more southern sites (TY, UO, LIS, LID, and EB) as compared to the northern sites (JB, NB, KI, DES, and DED; Table 7, Figure 3), which are further mirrored by the lower FST values between most southern sites (Table 5).
The deep and shallow sites at Dekel beach revealed the lowest pairwise FST value in this research, which might indicate that these sites are acting as a single population and together are experiencing differentiating forces from the other areas in the region, creating an isolated larger Dekel beach population. On the contrary, when examining the deep and shallow Lighthouse beach sites, the FST values reveal a significant genetic distinction between these two closely located sampling depths (>100 m apart), indicating restricted gene flow between them. This outcome may be attributed to local currents and reef geomorphology that reduce genetic connectivity between the shallow and the deep sites or to other, undisclosed factors [74], like those linked to distinct symbiont clades harbored in shallow vs. deep water S. pistillata corals [75]. Several studies in other reef locations have found that depth, while serving as a divider between deep and shallow reefs, not always cause population genetics differences [24,76,77]. Yet, depth may constitute a barrier to gene flow, and our results may question the assumed roles of mesophotic habitats as refuges [78,79,80]. While the deep area of the Dekel beach site may contribute larval recruitment to shallower depths, the deep area of the Lighthouse beach site may not, but this requires further research.
Here, we studied one of the most common and widely distributed coral species in the Gulf of Eilat, emphasizing the necessity for comparing its population genetics properties with other common coral species in the region. This should include species with different reproduction strategies (such as broadcasters) in order to clarify spatial scales for conservation and restoration efforts. The results further underscore the importance of gaining a better understanding of the population genetic structures of key species in this urbanized reef. Situated in proximity to the city of Eilat and near Aqaba, Jordan, another major city the coral reef in Eilat has experienced a gradual decline over nearly four decades due to human activities (resulting from heedless development of the city of Eilat, intermittent municipal sewage outflow, industrial and maritime installations, tourism and others [30,62,63,64,65,66,67,68,69]). This degradation of the reef has continued despite the implementation of best practices, such as the creation of an MPA, including a small zone (ca. 350 m of coastline) of a limited access area within it, which has been enforced since 1992 in hopes of creating a refuge area. Some of the assumptions for this conservation strategy are grounded on unrealistic expectations that do not have clear long-term positive impacts in preventing ongoing degradation [62,70,71,81,82]. Now, when considering the broader impacts of global climate change, there is a growing necessity for innovative management approaches, such as active reef restoration [15,83], which can be aided by monitoring the genetic properties of key species [18]. The results of the present study that elucidate a surprisingly fragmented population of one of the most abundant coral species in the gulf offer insights into various ecological engineering approaches to counteract the genetic decline. These approaches may involve initiatives, like the seeding of isolated reef sites with coral planulae using floating nurseries [84], the transplantation of gravid nursery-farmed colonies [85], or the establishment of floating devices to restore biological connectivity through stepping-stone connections [32].
Through our findings, we aspire to contribute to a more profound comprehension of the population genetics dynamics of S. pistillata and, consequently, the entire coral reef in the region. Such knowledge may prove instrumental [86] in enhancing management practices for the coral reef in the area, offering potential benefits for innovative strategies toward climate change and anthropogenic adaptation.

Supplementary Materials

The following supporting information can be downloaded at https://www.mdpi.com/article/10.3390/jmse12020315/s1, Supplementary Figure S1. Mantel test for the pairwise geographic distances between populations (x-axis) and the pairwise genetic distances (FST) (y-axis) for the sampling sites of Stylophora pistillata in the Gulf of Eilat created by GenAlEx software version 6.5. Supplementary Figure S2. The genetic distances and relationships between the Stylophora pistillata populations (sites) in Eilat created by POPTREE2. Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB). Values at the nodes represent bootstrap values.

Author Contributions

Conceptualization, E.N.R. and B.R.; sample collection, E.N.R.; DNA extraction, PCR amplification, and sequencing, E.N.R.; data analysis, E.N.R. and J.D.; writing—original draft preparation, E.N.R., B.R. and J.D.; writing—review and editing, E.N.R., J.D. and B.R.; supervision, B.R.; project administration, B.R.; funding acquisition, B.R. All authors have read and agreed to the published version of the manuscript.

Funding

This study was funded by the ISF (number 3511/21), NSFC (number 42161144006), Joint Scientific Research Program, and the Horizon Europe OCEAN CITIZEN project (No. 101093910; marine forest coastal restoration: an underwater gardening socio-ecological plan), HORIZON-MISS-2021-OCEAN-02-01 (to B.R.).

Institutional Review Board Statement

The research was conducted under a permit from the Israel Nature and Parks Authority, numbers 2016/41540, 2020/42540, and 2021/42878.

Informed Consent Statement

Not applicable.

Data Availability Statement

The DNA samples are kept at 4 °C at the IOLR.

Acknowledgments

We appreciate the continued support and help of all our lab members in Haifa and Eilat, as well as the staff and members of the IOLR (Haifa and NCM) and the IUI. In particular, we thank G. Paz for figure construction, E. Reem for statistical advice, R. Sosnowski for proofreading, and A. Oren for assisting with sample collection.

Conflicts of Interest

The authors declare no conflicts of interest.

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Figure 1. Stylophora pistillata (Esper 1797) colonies in the Gulf of Eilat.
Figure 1. Stylophora pistillata (Esper 1797) colonies in the Gulf of Eilat.
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Figure 2. Sampling sites along the Gulf of Eilat’s coastline: Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB). *—Study area.
Figure 2. Sampling sites along the Gulf of Eilat’s coastline: Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB). *—Study area.
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Figure 3. Gene flow trajectories for each sampling site [%], assessing the likelihood of the gene pool (microsatellite alleles) to be the ‘self-site’ or ‘other-site’ population. Arrows indicate gene flow from one site to the others. Numbers are percentage [%] of contribution. Values for all 10 sampling sites of Stylophora pistillata in the Gulf of Eilat, Israel: Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
Figure 3. Gene flow trajectories for each sampling site [%], assessing the likelihood of the gene pool (microsatellite alleles) to be the ‘self-site’ or ‘other-site’ population. Arrows indicate gene flow from one site to the others. Numbers are percentage [%] of contribution. Values for all 10 sampling sites of Stylophora pistillata in the Gulf of Eilat, Israel: Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
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Figure 4. A 3D factorial analysis of correspondence (FAC) of Stylophora pistillata populations in the Gulf of Eilat, Israel, generated by GENETIX on the sampled individuals per site. Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
Figure 4. A 3D factorial analysis of correspondence (FAC) of Stylophora pistillata populations in the Gulf of Eilat, Israel, generated by GENETIX on the sampled individuals per site. Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
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Figure 5. Cluster analysis for all 10 Stylophora pistillata sampling sites in Eilat, Israel. (Top panel) was created by STRUCTURE (optimal K = 4) and (bottom panel) BAPS (optimal K = 7). The y-axis indicates the allocation probability of each sampling site into a distinct cluster, as indicated by the assigned colors. Sampling sites are shown on the x-axis. Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
Figure 5. Cluster analysis for all 10 Stylophora pistillata sampling sites in Eilat, Israel. (Top panel) was created by STRUCTURE (optimal K = 4) and (bottom panel) BAPS (optimal K = 7). The y-axis indicates the allocation probability of each sampling site into a distinct cluster, as indicated by the assigned colors. Sampling sites are shown on the x-axis. Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
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Table 1. Collection sites in the Gulf of Eilat (site I.D., name of site, geographic location, and depth), collection dates, and the number of coral fragments collected at each site.
Table 1. Collection sites in the Gulf of Eilat (site I.D., name of site, geographic location, and depth), collection dates, and the number of coral fragments collected at each site.
Site I.D.Site NameSite LocationDepth
(Meters)
Collection DatesNumber of
Samples Collected
JBJordan Border
beach
29°32′34.08″ N 34°58′25.02″ E8–12 27–28 February 202230
NBNorth Shore
beach
29°32′46.89″ N 34°57′59.31″ E8–121–2 March 202240
KIKisoski beach29°32′49.85″ N 34°57′13.72″ E8–121–2 March 202240
DESDekel beach
shallow
29°32′18.97″ N 34°56′46.30″ E8–123 March 202240
DEDDekel beach
deep
29°32′18.97″ N 34°56′46.30″ E26–403 March 202240
TYTour Yam
beach
29°31′0.03″ N 34°55′36.45″ E8–1227–28 February 202230
UOUnderwater
Observatory beach
29°30′12.57″ N 34°55′7.55″ E8–1227–28 February 202240
LISLighthouse beach
shallow
29°30′2.76″ N 34°54′58.89″ E8–129 November 202244
LIDLighthouse beach
deep
29°30′2.76″ N 34°54′58.89″ E26–409 November 202246
EBEgypt Border
beach
29°29′38.07″ N 34°54′23.52″ E8–1227–28 February 202230
Table 2. Chosen microsatellite loci from [35], their fluorescence labels used, and size range for the Israeli Stylophora pistillata populations.
Table 2. Chosen microsatellite loci from [35], their fluorescence labels used, and size range for the Israeli Stylophora pistillata populations.
LocusFluorescent LabelSize Range–Eilat
Stylo_176-FAM110–230
Stylo_45PET210–340
Stylo_48PET210–340
Stylo_55VIC220–360
Stylo_726-FAM30–165
Stylo_73NED110–280
Stylo_80VIC140–270
Stylo_82NED170–300
Table 3. Stylophora pistillata population statistics per locus (from [35]) and for all sampling sites. N—number of individuals tagged by the locus, Na—number of different alleles, HO—observed heterozygosity, HE—expected heterozygosity, F —fixation index, PIC—polymorphic information content, and significance of the deviation from the Hardy–Weinberg equilibrium: *** = p < 0.001.
Table 3. Stylophora pistillata population statistics per locus (from [35]) and for all sampling sites. N—number of individuals tagged by the locus, Na—number of different alleles, HO—observed heterozygosity, HE—expected heterozygosity, F —fixation index, PIC—polymorphic information content, and significance of the deviation from the Hardy–Weinberg equilibrium: *** = p < 0.001.
LocusNNaHOHEFPICSignificance
Stylo_17379490.540.860.370.94***
Stylo_55379280.470.790.410.88***
Stylo_82379280.670.830.20.88***
Stylo_48379290.430.790.460.85***
Stylo_72380240.630.780.180.85***
Stylo_80380340.730.790.080.91***
Stylo_73363480.660.850.250.95***
Stylo_45379610.650.860.250.94***
Mean ± SE377.25 ± 2.0437.63 ± 4.710.59 ± 0.020.82 ± 0.010.28 ± 0.030.9 ± 0.01
Table 4. Population statistics per sampling site (mean ± SE) for all loci per site. N—number of individuals collected per site, Na—average number of different alleles from all loci per site, I—information index, HO—observed heterozygosity, HE—expected heterozygosity, F —fixation index. Jordan border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
Table 4. Population statistics per sampling site (mean ± SE) for all loci per site. N—number of individuals collected per site, Na—average number of different alleles from all loci per site, I—information index, HO—observed heterozygosity, HE—expected heterozygosity, F —fixation index. Jordan border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
PopNNaIHOHEF
JB308.5 ± 0.571.68 ± 0.090.65 ± 0.060.75 ± 0.030.13 ± 0.06
NB4011.75 ± 1.671.98 ± 0.180.46 ± 0.080.81 ± 0.040.46 ± 0.09
KI4012.25 ± 1.242.02 ± 0.120.6 ± 0.080.81 ± 0.030.27 ± 0.1
DES4014.13 ± 1.292.28 ± 0.090.72 ± 0.060.87 ± 0.010.18 ± 0.06
DED4013 ± 1.272.23 ± 0.130.66 ± 0.050.86 ± 0.020.23 ± 0.05
TY3011.88 ± 1.112.13 ± 0.10.66 ± 0.040.85 ± 0.020.22 ± 0.05
UO4012.5 ± 1.212.14 ± 0.110.54 ± 0.080.84 ± 0.020.36 ± 0.09
LIS4410 ± 0.931.79 ± 0.110.52 ± 0.110.78 ± 0.030.3 ± 0.17
LID4612.38 ± 0.892.15 ± 0.090.48 ± 0.090.85 ± 0.020.44 ± 0.1
EB3011.63 ± 0.842.05 ± 0.110.68 ± 0.040.82 ± 0.030.18 ± 0.04
Total37.7 ± 0.6111.8 ± 0.382.05 ± 0.040.59 ± 0.020.82 ± 0.010.28 ± 0.03
Table 5. Pairwise population FST values for the 10 Eilat sampling sites. Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
Table 5. Pairwise population FST values for the 10 Eilat sampling sites. Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
JBNBKIDESDEDTYUOLISLIDEB
JB0.000
NB0.2050.000
KI0.0930.1800.000
DES0.0890.1400.0820.000
DED0.1080.1520.1040.0370.000
TY0.1180.1580.1080.0470.0610.000
UO0.0960.1650.0390.0660.0850.0680.000
LIS0.1060.1950.0740.1050.1210.1170.0660.000
LID0.1350.1580.1000.0840.0730.0610.0690.1000.000
EB0.0800.1700.0950.0520.0690.0460.0520.0760.0860.000
Table 6. AMOVA results performed on all Stylophora pistillata populations. SS—sum of squares, Est. Var.—estimated variance, %—percentage of total variance. FST based on the standard permutation across the full dataset was 0.102, p < 0.001.
Table 6. AMOVA results performed on all Stylophora pistillata populations. SS—sum of squares, Est. Var.—estimated variance, %—percentage of total variance. FST based on the standard permutation across the full dataset was 0.102, p < 0.001.
SourcedfSSMSEst. Var.%
Among Pops9289.69832.1890.3810
Within Pops7502505.6213.3413.34190
Total7592795.318 3.721100
Table 7. Summary of population assignment outcomes to the ‘Self-site’ or ‘Other sites’ population employed on the 10 sampling sites: Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
Table 7. Summary of population assignment outcomes to the ‘Self-site’ or ‘Other sites’ population employed on the 10 sampling sites: Jordan Border beach (JB), North Shore beach (NB), Kisoski beach (KI), Dekel beach shallow (DES), Dekel beach deep (DED), Tour Yam beach (TY), Underwater Observatory beach (UO), Lighthouse beach shallow (LIS), Lighthouse beach deep (LID), and Egypt Border beach (EB).
Population‘Self’‘Other’
JB291
NB40
KI337
DES355
DED382
TY273
UO2713
LIS413
LID442
EB1713
Total33149
Percent87%13%
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MDPI and ACS Style

Rachmilovitz, E.N.; Douek, J.; Rinkevich, B. Population Genetics Assessment of the Model Coral Species Stylophora pistillata from Eilat, the Red Sea. J. Mar. Sci. Eng. 2024, 12, 315. https://doi.org/10.3390/jmse12020315

AMA Style

Rachmilovitz EN, Douek J, Rinkevich B. Population Genetics Assessment of the Model Coral Species Stylophora pistillata from Eilat, the Red Sea. Journal of Marine Science and Engineering. 2024; 12(2):315. https://doi.org/10.3390/jmse12020315

Chicago/Turabian Style

Rachmilovitz, Elad Nehoray, Jacob Douek, and Baruch Rinkevich. 2024. "Population Genetics Assessment of the Model Coral Species Stylophora pistillata from Eilat, the Red Sea" Journal of Marine Science and Engineering 12, no. 2: 315. https://doi.org/10.3390/jmse12020315

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