(Symbiodinium) in Scleractinian Corals from Tropical Reefs in Southern Hainan
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Journal of Systematics and Evolution 49 (6): 598–605 (2011) doi: 10.1111/j.1759-6831.2011.00161.x Research Article Low genetic diversity of symbiotic dinoflagellates (Symbiodinium) in scleractinian corals from tropical reefs in southern Hainan Island, China 1,2Guo-Wei ZHOU 1,2Hui HUANG∗ 1(Key Laboratory of Marine Bio-resources Sustainable Utilization, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China) 2(Tropical Marine Biological Research Station in Hainan, Chinese Academy of Sciences, Sanya 572000, China) Abstract Endosymbiotic dinoflagellates in the genus Symbiodinium are among the most abundant and important group of photosynthetic protists found in coral reef ecosystems. In order to further characterize this diversity and compare with other regions of the Pacific, samples from 44 species of scleractinian corals representing 20 genera and 9 families, were collected from tropical reefs in southern Hainan Island, China. Denaturing gradient gel electrophoresis fingerprinting of the ribosomal internal transcribed spacer 2 identified 11 genetically distinct Symbiodinium types that have been reported previously. The majority of reef-building coral species (88.6%) harbored only one subcladal type of symbiont, dominated by host-generalist C1 and C3, and was influenced little by the host’s apparent mode of symbiont acquisition. Some species harbored more than one clade of Symbiodinium (clades C, D) concurrently. Although geographically isolated from the rest of the Pacific, the symbiont diversity in southern Hainan Island was relatively low and similar to both the Great Barrier Reef and Hawaii symbiont assemblages (dominated by clade C Symbiodinium). These results indicate that a specialist symbiont is not a prerequisite for existence in remote and isolated areas, but additional work in other geographic regions is necessary to test this idea. Key words coral, dinoflagellate, diversity, South China Sea, Symbiodinium. Dinoflagellates in the genus Symbiodinium (also An increasing number of studies have focussed on called zooxanthellae) are found in symbiosis with a di- the biogeographic distribution of Symbiodinium (e.g. verse range of marine invertebrate taxa and some pro- LaJeunesse, 2002; LaJeunesse et al., 2003, 2004a; Chen tists (reviewed in Baker, 2003; Finney et al., 2010). Al- et al., 2005; van Oppen et al., 2005). This understanding though originally thought to be a single dinoflagellate may provide insights into the future responses of reef species, Symbiodinium microadriaticum (Freudenthal, corals to environmental change (Buddemeier & Fautin, 1962), studies based on biochemical, morphological, 1993; Baker et al., 2004; LaJeunesse et al., 2010a). physiological, and molecular data have gradually es- As environmental factors may vary enormously from tablished that the genus Symbiodinium is a diverse as- spatial and temporal scales, regional differences in Sym- semblage (Rowan, 2004; LaJeunesse et al., 2010a). The biodinium diversity within a single host or among mul- genus Symbiodinium is now recognized to comprise nine tiple species are therefore important (LaJeunesse et al., divergent lineages (clades A–I) based on analyses of nu- 2010a). For example, Symbiodinium A and B are much clear ribosomal DNA (LaJeunesse, 2002; LaJeunesse more common in Caribbean scleractinians compared to et al., 2004a; Pochon & Gates, 2010) and chloroplast the Indo-Pacific, where clade C Symbiodinium prevail. 23S rDNA (Santos et al., 2002). Six of these clades (A– Moreover, the Symbiodinium in the same host species D, F, and G) are known to form associations with scler- are varied among different environments. For example, actinian corals, but predominantly with those of clades the Indo-Pacific coral Plesiastrea versipora (Lamarck, A–D (Baker, 2003). Each of these clades contains mul- 1816) hosts clade C at low latitudes and clade B at tiple subcladal lineages or types that show geographic the latitudinal margins of its distribution (Rodriguez- and host specificity using by more variable molecular Lanetty et al., 2001). It is believed that more research markers such as ITS rDNA (Sampayo et al., 2009). into regions of the Indo-Pacific will uncover more sym- biont diversity (Baker & Rowan, 1997; LaJeunesse et al., 2003). Received: 30 March 2011 Accepted: 5 July 2011 ∗ Author for correspondence. E-mail: [email protected]; Tel./Fax: 86- Considerable research on Symbiodinium diversity 20-84460294. and distribution has been carried out in the Caribbean C 2011 Institute of Botany, Chinese Academy of Sciences ZHOU & HUANG: Low genetic diversity of Symbiodinium in corals 599 and Central and Eastern Pacific (LaJeunesse, 2002; La- northern SCS. Luhuitou Bay (LHT), Ximao Island Jeunesse et al., 2003, 2004a, 2004b), but little has been (XD), Xipai Island (XP), and Xiaodonghai Bay (XDH) done in the South China Sea (SCS), Western Pacific, are part of Sanya National Coral Reefs Nature Reserve, one of the largest marginal seas. The SCS is rich in established in 1990. Small fragments (approximately coral cover and diversity and has recently been shown 5cm2) of reef corals were collected at a depth of 1– in decline (Huang, 2005). Several studies have reported 10 m with hammer and chisel using scuba diving at the Symbiodinium diversity in reef-building corals in four locations in Sanya in October 2008 (Fig. 1). All the SCS (Huang et al., 2006, 2011; Dong et al., 2009). specimens were preserved in 100% EtOH until further Dong et al. (2008) reported the diversity of Symbio- processing. dinium in Luhuitou Bay (Sanya, China) by polymerase chain reaction (PCR) restriction fragment length poly- morphism. Unfortunately, the method mainly used in 1.2 DNA extraction and ITS2-DGGE previous studies was only at the cladal level and could fingerprinting not provide more details about the ecological aspects Total DNA was extracted using the protocol de- (Sampayo et al., 2009). Additionally, it is not known scribed in Huang et al. (2006). The Symbiodinium ITS2 whether the Symbiodinium communities in this isolated region was analyzed using DGGE in combination with area are different from other regions of the Pacific. DNA sequencing of dominant bands. The ITS2 was am- In the present study, denaturing gradient gel elec- plified using the primers ITS2 clamp (5 -CGCCCGCCG trophoresis (DGGE) and sequencing of the internal tran- CGCCCCGCGCCCGTCCCGCCGCCCCCGCCCGG scribed spacer 2 (ITS2) region were used to determine GGATCCATATGCTTAAGTTCAGCGGGT-3 )and the diversity and community structure of Symbiodinium ITSintfor2 (5 -GAATTGCAGAACTCCGTG-3 ) with associated with reef-building corals from four reefs in a touch-down PCR protocol following LaJeunesse southern Hainan Island, SCS. We also compared our (2002). The PCR products were loaded on 8% findings to the data available for these coral species in polyacrylamide gels (acrylamide : N, N -methylenebis- other parts of the Pacific, including the Great Barrier acrylamide 37:1) with a denaturant gradient of 30%– Reef (GBR), Okinawa, and Hawaii (LaJeunesse et al., 60% (where 100% is defined as 7 mol/L urea and 40% 2003, 2004a, 2004b), to corroborate hypothesized bio- V/V formamide). Electrophoresis was carried out with geographic patterns in the distribution of Symbiodinium the DCode System (Bio-Rad, Hercules, CA, USA) ◦ diversity, and to determine whether or not an exception using 0.5 × Tris-Acetate-EDTA (TAE) buffer at 60 C occurred. for 14 h at 100 V. Gels were stained for 30 min in SYBR Green nucleic acid gel stain (Molecular Probes, 1 Material and methods Eugene, OR, USA) and photographed with ultraviolet transillumination. 1.1 Sample collection Distinct ITS2-DGGE profiles (fingerprints) were The sampling for this study was carried out at characterized by sequencing of the dominant bands. Sanya, on the southernmost coast of Hainan Island, The most prominent DGGE bands were excised from Fig. 1. Maps of coral reefs sampled in this study, downloaded from http://www.ngdc.noaa.gov/mgg/shorelines/gshhs.html and produced using Surfer 9. HI, Hainan Island; LHT, Luhuitou Bay; XD, Ximao Island; XDH, Xiaodonghai Bay; XP, Xipai Island. C 2011 Institute of Botany, Chinese Academy of Sciences 600 Journal of Systematics and Evolution Vol. 49 No. 6 2011 the gel, eluted in DNAase free water overnight, and other regions of the Pacific including the GBR, Ok- re-amplified with a reverse primer lacking the GC- inawa, and Hawaii (LaJeunesse et al., 2003, 2004a, clamp under the conditions described above. Sequenc- 2004b). Figure 2 shows the typical band profiles ob- ing was carried out using an ABI3730 DNA Sequencer tained, labelled with their ITS2 type (LaJeunesse, 2002; (Applied Biosystems, Carlsbad, CA, USA). The DGGE LaJeunesse et al., 2003). Heteroduplexes were usu- fingerprints and their corresponding sequences were ally produced from the DGGE analysis due to mis- compared against a reference database from diversity matching of variants during the PCR process (La- analyses carried out at other Indo-Pacific locations; Jeunesse et al., 2003). The ITS2 phylogeny inferred Symbiodinium ITS2 sequences were named as in pre- from MP is shown for Symbiodinium types in clade vious studies (LaJeunesse et al., 2003, 2004a, 2004b). C, as there was divergence among clade C symbionts The capital letter of these taxonomic designators refers (Fig. 3). Maximum parsimony, NJ, and Bayesian in- to the particular clade of Symbiodinium and the num- ference methods yielded very similar trees (data not bers and lowercase letters refer to bands diagnostic shown).