A new genus and species of octocoral with aragonite calcium-carbonate skeleton (Octocorallia, Helioporacea) from Okinawa, Japan.

A new genus and species of octocoral with a calcium-carbonate skeleton, Naniporakamurai sp. n., is described from a shallow coral reef in Okinawa, Japan. Contrary to most octocorals, the skeleton is composed of crystalline aragonite as in blue coral Heliopora. The results of molecular phylogenetic analyses of sequences of mtMutS, COI, and ITS1-5.8s-ITS2-28S region suggest Nanipora gen. n. specimens should be included in order Helioporacea. Based on morphological results compared with other Helioporacea including the genus Epiphaxum (family Lithotelestidae), we establish the new genus Nanipora within Lithotelestidae. This is the first time that a close molecular phylogenetic relationship between Heliopora and a related genus within Helioporacea has been revealed.

Introduction

Octocorals (class , subclass ) are sessile marine benthic organisms. Most octocorals support their body by sclerites in their tissue, or having a solid axial structure made of calcite calcium-carbonate or of protein, unlike scleractinians PageBreakwith a massive aragonite calcium-carbonate skeleton. The blue coral (Pallas, 1766) (, ) is especially peculiar as it is an octocoral with a massive aragonite calcium-carbonate skeleton similar to scleractinians.

Although was long considered to be the sole member of the order , Bayer and Muzik (1977) described an octocoral with aragonite skeleton from a specimen in the Barbados collection of J. B. Lewis as (Bayer & Muzik, 1977) and placed the species in the family established within . Bayer (1979) reclassified this species as , as Lonsdale (1850: 237–324) had previously described a very similar fossil octocoral as Lonsdale, 1850. In total, two fossil and three extant species, two from the Caribbean and one from the western Indian Ocean (Madagascar) (Bayer 1992; Louzet and Molodtsova 2008), have been recorded. While fossils of have been recovered sporadically but widely from Europe, from a wide range of geological ages (Lozouet and Molodtsova 2008), extant species’ records are very rare and this genus remains enigmatic (Daly et al. 2007; McFadden et al. 2010).

In this study, we report on our examinations of unknown octocoral specimens with a calcium-carbonate skeleton from a shallow reef off Zamami Island, Okinawa, Japan. Morphology and structure of skeleton for these specimens were examined by using SEM and micro-CT. X-ray diffraction was used to determine the calcium-carbonate composition of the skeleton. Three molecular markers; mitochondrial mismatch repair protein (mtMutS), mitochondrial cytochrome c oxidase subunit 1 (COI), and the nuclear ribosomal gene complex of the 3’ end of the 18S subunit, ITS-1, 5.8S subunit, ITS-2, and the 5’ end of the 28S subunit (ITS1-5.8s-ITS2-28S) were sequenced to determine the phylogenetic placement of these specimens. Based on these specimens from Zamami Island, this octocoral is described as gen. et sp. n. within the family .

Methods

Collection of specimens

Specimens were collected by snorkeling using a chisel and a hammer from Ama Beach, Zamami Island, Ryukyu Archipelago, Japan (26°23'N; 127°29'E) at a depth of 1 m in July 2012 (Suppl. material 1). Colonies were attached to the bottoms (=downward facing sides) of carbonate stones. Digital images were also taken in situ to record the appearance of living colonies. Specimens were fixed in 99% ethanol immediately after collection.

Morphological analyses

Digital images were utilized to examine the color and shape of living colonies and polyps (Fig. 1). Skeletons were soaked in household bleach containing sodium hypochlorite PageBreakfor 15–20 min, followed by rinsing with distilled water and air-drying, to remove soft tissues. Skeletal specimens were stuck to aluminum specimen mounts by carbon double-faced tape, then examined and imaged with a scanning electron microscope (SEM) VE-8800 (Keyence, Osaka, Japan). CT images of ethanol-preserved specimens were taken with micro CT (in vivo micro X-ray CT system R_mCT2, Rigaku, Tokyo, Japan) and examined with the DICOM imaging application OsiriX v. 5.9 32-bit (Rosset et al. 2004) to investigate the structure of the skeleton in a non-invasive manner. By using this application, areas of particular CT-value in organisms can be visualized: e.g. showing skeleton (high CT-value) and hiding soft tissue (low CT-value), or vice versa. To check for the presence of sclerites, small pieces of EtOH preserved colonies were dissolved with household bleach on a well-slide and examined with an optical microscope. Additionally, several polyps were dissolved on carbon double-faced tape. Deposits from washing solution of whole colonies were retrieved and carefully rinsed, followed by mounting on carbon double-faced tape. These specimens were examined by SEM. X-ray diffraction analyses were performed with an X-ray diffractometer RINT Ultima/PC (Rigaku, Tokyo, Japan) at the Instrumental Research Center, University of the Ryukyus, to examine the crystal forms of calcium carbonate (aragonite/calcite) of the skeleton. Skeletal specimens were smashed to powder, mounted on well-washed glass slides and analyzed using Cu Kα radiation (40 kV, 30 mA), scanning between a 2θ angle ranging from 25° to 37° at 0.02° steps. The calcite/aragonite component (%) of samples was determined by comparing with data of standard samples of 100% calcite/aragonite. For comparison, a sample skeleton of the blue coral was prepared and analyzed in the same manner.

Figure 1.

Living colony of attached to the bottoms (=downward facing side) of calcium-carbonate stone at Ama Beach, Zamami Island, Okinawa, Japan, 16 July 2012. Scale bar: approximately 5 mm.

DNA extraction and PCR amplification

DNA was extracted from tentacles and anthocodial tissue of ethanol-preserved samples by a guanidine extraction protocol following Sinniger et al. (2009). PCR amplifications were performed using HotStarTaq DNA polymerase (Qiagen, Tokyo, Japan) according to the manufacturer’s instructions. The mitochondrial mismatch repair protein (mtMutS) was amplified by semi-nested PCR following the procedure of McFadden et al. (2006), as no visible PCR product was yielded by a single PCR reaction. First, primers ND42599F (5’-GCCATTATGGTTAACTATTAC-3’) (France and Hoover 2002) and Mut-3458R (5’-TSGAGCAAAAGCCACTCC-3’) (Sánchez et al. 2003) were used to amplify the 5’ end of mtMutS, and then a second PCR reaction was run using internal forward primer ND42625F (5’-TACGTG GYACAATTGCTG-3’) (Lepard 2003) and reverse primer Mut-3458R. Both PCR reactions were performed under the following conditions: 15 min at 94 °C; 35 cycles of 1.5 min at 94 °C, 1.5 min at 58 °C, and 1 min at 72 °C; and a final extension of 5 min at 72 °C. Mitochondrial cytochrome oxidase subunit I (COI) was amplified by the primers COII-8068 (5’-CCATAACAGGACTAGCAGCATC-3’) (McFadden et al. 2004) and COI-OCTr (5’-ATCATAGCATAGACCATACC-3’) (France and Hoover 2002) under the following conditions: PageBreak5 min at 95 °C; 35 cycles of 1 min at 94 °C, 1 min at 40 °C, and 1.5 min at 72 °C; and then a final extension of 7 min at 72 °C. The nuclear ribosomal gene complex of the 3’ end of the 18S subunit, internal transcribed spacer 1 (ITS-1), 5.8S subunit, ITS-2, and the 5’ end of the 28S subunit was amplified by the primers 1s (5’-GGTACCCTTTGTACACACCGCCCGTCGCT-3’) and 2ss (5’-GCTTTGGGCTGCAGTCCCAAGCAACCCGACTC-3’) (Chen et al. 1996) under the following conditions: 15 min at 95 °C; 35 cycles of 0.5 min at 94 °C, 1 min at 52 °C, and 1.5 min at 72 °C; and a final extension of 5 min at 72 °C. Amplified products were visualized with 1.0% agarose gel electrophoresis. Positive PCR products were cleaned up by Exonuclease I and Shrimp Alkaline Phosphatase (Takara, Shiga, Japan) before sequencing.

Sequence analyses

Sequencing was performed by Fasmac (Kanagawa, Japan). Cycle sequencing was performed in both directions using the forward and reverse primers separately with BigDye® Terminator v3.1 Cycle Sequencing Kit (Applied Biosystems) under reaction conditions according to the manufacturer’s instructions. Reaction products were analyzed on an ABI PRISM 3700 DNA Analyzer (Applied Biosystems). The sequences were analyzed by 4Peaks Version 1.7.2 software (mekentosj.com, Amsterdam, Netherlands).

By using Se-AL v2.0a11 software (Rambaut 2002), the nucleotide sequences of mtMutS, COI, and ITS1-5.8s-ITS2-28S from specimens obtained in the present study were separately aligned with sequences of and other octocoral species retrieved from GenBank (Suppl. material). The alignments were checked by eye and manually edited to remove any ambiguous sites (e.g. double peaks) before phylogenetic analyses. For each alignment, none or only one to two base pairs were edited in this manner. Consequently, three aligned data sets were generated: 1) 861 sites of 33 sequences (mtMutS), 2) 735 sites of 12 sequences (COI), and 3) 697 sites of 5 sequences (ITS1-5.8s-ITS2-28S). The alignment data are available on request from the corresponding author. Additional octocoral sequences retrieved from GenBank are shown in Supplementary Table 2.

Phylogenetic analyses

Maximum-likelihood (ML) analyses with PhyML Online (Guindon and Gascuel 2003) of these datasets were independently performed using input trees generated by BIONJ (Gascuel 1997) with the general time reversible (GTR) model. PhyML bootstrap trees (1000 replicates) were constructed using the same parameters as the individual ML trees. Genetic distances were calculated using Kimura’s two-parameter model (Kimura 1980).

Bayesian trees were reconstructed by running the program MrBayes 3.1.2 (Ronquist and Huelsenbeck 2003) within the program Geneious version 8.0.4 (Restricted) created by Biomatters (available from http://www.geneious.com/). One cold and three PageBreakheated Markov chain Monte Carlo (MCMC) chains with default-chain temperatures were run for 1,000,000 generations, sampling log-likelihoods (InLs), and trees at 1000-generation intervals (1,000 InLs and trees were saved during MCMC). The first 100,000 generations of all runs were discarded as “burn-in” for the dataset and remaining 900 trees were used to obtain posterior probabilities and branch-length estimates, respectively. Neighbor-joining (NJ) trees were also reconstructed by using CLC Free Workbench 4 software (CLCbio.com, Aarhus North, Denmark) (1000 replicates).

Systematics

Class Ehrenberg, 1831 Subclass Haeckel, 1866 Order Bock, 1938

Bayer & Muzik, 1977

Type genus.

Bayer & Muzik, 1977 (junior synonym of Lonsdale, 1850).

Diagnosis

(after Bayer and Muzik 1977; Lozouet and Molodtsova 2008, revised). Helioporacean octocoral with growth form of encrusting, stoloniferous or upright sparsely branched stems. Whole colony rigid with internal skeleton of crystalline aragonite. Polyps fully retractile. Sclerites may be present or absent; if present, capstans and crosses in form, composed of calcite.

gen. n.

http://zoobank.org/283000C2-355E-4302-A44F-94CB19202538

Type species.

sp. n., here designated.

Diagnosis.

Encrusting, partly stoloniferous colony with cylindrical calyces up to 5 mm tall, attached to hard substratum. Polyps monomorphic and retractile. Coenenchyme and calyces rigid with internal skeleton, not composed with fused sclerites but of unitary crystalline aragonite. Reticulate pattern on whole colony’s surface, made of tiny pores on the surface. Top of the calyx serrated, with 16–20 indentations. Longitudinal cavities in the calicular wall, connecting to solenial canals in the base of the colony. Interior of calyx smooth, lacking septae. Surface of calyces occasionally wrinkled. Completely lacks sclerites. Living colonies ivory or pale brown. Skeleton colourless. Azooxanthellate.

Etymology.

Named from the Japanese ‘nani’ plus latin ‘pora’: ‘nani’ means ‘what is this?’, as the genus is highly unusual in having an aragonitic skeleton; ‘pora’ is originally meaning of ‘pore’, name used for many anthozoan (especially scleractinian) species with porous skeleton. Gender is feminine.

sp. n.

http://zoobank.org/98A4C103-57A8-469B-A157-81B088EDC717

Figs 1 , 2 , 3 , 4 , 5 , 6 , 7 , 8 , 9 , 10 , 11

Figure 2.

In situ colony of with expanded polyps at Ama Beach, Zamami Island, Okinawa, Japan, 16 July 2012. A growing edge of the colony B middle portion of the colony. Scale bar: approximately 5 mm.

Figure 3.

Scanning electro-microscope (SEM) image for skeleton of colony. Scale bar: 0.5 mm.

Figure 4.

Calyx of . Reticulate pattern and wrinkles are shown. Scale bar: 0.2 mm.

Figure 5.

Surface of the calyx. Reticulate pattern made by numerous tiny pores. Scale bar: 0.04 mm.

Figure 6.

Indentations seen on the top of the calyx of . Scale bar: 0.1 mm.

Figure 7.

Calyx of seen from above. Cavities extend in a longitudinal direction down through the calyx are shown. Scale bar: 0.2 mm.

Figure 8.

Surface calcium carbonate of the darker portions. Beneath, large holes (up to 200 μm) are shown. Scale bar: 0.02 mm.

Figure 9.

A–C Different surface calcium carbonate coverage of three calyces (A>B>C) D Skeleton of younger and marginal part of the colony, partly lacks surface cover. Scale bar: 0.2 mm (A), 0.5 mm (B).

Figure 10.

Cavities seen in cross sectioned coenenchymal skeleton. Scale bar: 0.1 mm.

Figure 11.

3D CT image of soft tissue. Solenial tubes forming network are shown. Scale bar: 0.5 mm.

Type material.

Holotype: NSMT-Co1562, Ama Beach, Zamami, Okinawa, JAPAN (26°13.31'N; 127°17.28'E), 1 m depth, collected by Yu Miyazaki (Y.M.), 16 July 2012, fixed in 99% EtOH, deposited in National Museum of Nature and Science, Tokyo, Japan (NSMT). GenBank accession numbers: mtMutS, KP195280; mt COI, KP195281; ITS1-5.8s-ITS2-28S, KP195282; Paratype 1: Specimen number RMNH 41731. Ama Beach, Zamami, Okinawa, JAPAN (26°23'N; 127°29'E), 1 m depth, collected by Yu Miyazaki (Y.M.), 16 July 2012, fixed in 99% EtOH, deposited in Naturalis Biodiversity Center, Leiden, the Netherlands (RMNH). Paratype 2: USNM 1231377, Ama Beach, Zamami, Okinawa, JAPAN (26°23'N; 127°29'E), 1 m depth, collected by Yu Miyazaki (Y.M.), 16 July 2012, fixed in 99% EtOH, deposited in National Museum of Natural History, Smithsonian Institution, Washington, D.C., USA (USNM); Other materials. Specimen number MISE-MY-120715. Ama Beach, Zamami, Okinawa, JAPAN (26°23'N; 127°29'E), 1 m depth, collected by Yu Miyazaki (Y.M.), 15 July 2012, fixed in 99% EtOH.

Description.

The holotype colony is encrusting (Fig. 1A), attached to the bottom (=downward facing side) of carbonate stone of dimensions 80 × 50 × 50 mm. Colony occasionally with thin stolons (2–3 mm in width, less than 1 mm thick) growing over irregular surface (Fig. 1B, arrow). The polyps of holotype colony are completely withdrawn into calyces after fixation.

Tentacles are 3–4 mm long, with fine but distinct pinnules (Fig. 2A and B). Anthocodiae are fully retractile within calyces. Coenenchyme is thin (up to 3 mm, less than 1 mm in most portions). Both coenenchyme and calyces are rigid with internal skeletons.

Overall shape of the skeleton is virtually the same as the external shape of living colonies (Fig. 3). Calyces are cylindrical, up to 1 mm across; up to 5 mm in height, perforated by randomly distributed pores up to 50 μm in diameter (Fig. 4). The surface of the skeletal calyx is occasionally wrinkled (Fig. 4, 5). The top of the calyces are serrated, with usually 16, but as many as 20 indentations (Fig. 6). Inside of the calyces is simple and tubular, lacking any structures such as septae. Calicular walls are 0.08–0.1 mm thick at the apical end and gradually became thicker going down towards the proximal portion, where thicknesses reached up to 0.2 mm. In the calicular walls, from distal to proximal portions, 12–20 cavities up to 0.05 mm diameter pass through (Fig. 7). These cavities are often discontinuous, converged or branched.

The whole skeleton has a reticulate pattern on the surface (Fig. 3, 4). This pattern is made by numerous tiny pores (up to 5 μm in diameter, Fig. 5); darker parts with pores, and lighter parts without pores. The surface calcium carbonate of the darker portions is very thin like a sheet, compared to the part without pores (Fig. 8). Growing edges of colonies and tops of calyces tend to lack such calcium-carbonate sheets and therefore the surface of these regions has holes (up to 200 μm, Fig. 9A–D). In the cross sections of the coenenchymal skeleton, cavities 0.1–0.2 mm in diameter are observed (Fig. 10). PageBreakThese cavities house solenia, connecting the gastric cavities of polyps and composing solenial network (Fig. 11, 3-dimensional CT images of soft tissue). Lacks sclerites. Azooxanthellate.

Colour. Living colony is pale brown or ivory (Fig. 1A and B). Whole polyps are pale brown, but shrunken tentacles appear dark brown (Fig. 1B). Skeleton is colourless.

Named after Hidefumi Kamura, a great jazz pianist who has continued playing classic style be-bop jazz from when Okinawa was under the rule of U.S. forces, and who can now be considered as a ‘relict’ classical be-bop jazz musician.

Habitat.

colonies are found on the bottoms (=downward facing sides) of carbonate stones on a sandy shallow beach at 1–1.5 m depths with very clear water. For now known only from Ama Beach, Zamami Island, Okinawa, Japan.

Comparison with other species.

General morphology of is quite similar to Lonsdale, 1850. Unlike species, presence of sclerites not observed by any means in any portion of specimen in this study. Secondary daughter calyces, such as seen in Nielsen, 1925 (=) and Verrill’s original drawing of Bayer & Muzik, PageBreakPageBreakPageBreakPageBreakPageBreak1977 (=), are not observed. Pores perforating calicular walls of are distributed irregularly, not aligned in a line or in a row as seen in species (Bayer and Muzik 1977; Bayer 1992; Lozouet and Molodtsova 2008). Neither an octagonal outline in the cross sections of calyces, such as seen in Bayer, 1992, nor sclerosepta as seen in , are observed.

Skeleton.

Examination of SEM images clearly showed the rigid skeleton of this species was not formed by fused sclerites as in , but made of unitary calcium carbonate as in . X-ray diffraction analyses revealed this skeleton was composed of 96% aragonite and 4% low-Mg calcite. Inclusion of traces of calcite may be contamination from calcareous algae attached to the surface of the colony. The skeleton of blue coral , analyzed for comparison, was 100% aragonite.

Molecular phylogeny.

The four specimens of in this study had completely identical mtMutS, COI and ITS1-5.8s-ITS2-28S sequences. In the ML trees for mtMutS (Fig. 12) and COI (not shown) alignments, the sequences of in this study and formed a strongly supported clade (ML=99% for mtMutS; ML=90% for COI) to the exclusion of all other octocoral sequences, and sequences of the new specimens formed a subclade clearly different from (ML=100% in mtMutS, ML=100% in COI). p-distances between and were 0.053 (mtMutS) and 0.034 (COI), while distances between and other soft corals included in phylogenetic analyses were at least >0.061 (mtMutS) and >0.042 (COI). ITS1-5.8s-ITS2-28S sequences of the unknown octocoral and could be aligned together, but they could not be accurately aligned with any PageBreakother known octocoral ITS1-5.8s-ITS2-28S sequences due to sequence divergence. The nuclear ITS1-5.8s-ITS2-28S region sequence of had 94 nucleotide differences from sequences over 697 nucleotides (=13.5% variation).

Figure 12.

Maximum likelihood tree for mtMutS sequences. Values at branches represent ML and NJ bootstrap probabilities, respectively (>50%). Bold lines represent branches with very high support in Bayesian analyses (>0.95). Sequences without accession numbers were newly obtained in this study.

Remarks.

The distribution of gen. n. is currently known from only one site in Okinawa. Although the lack of reports may result from their tiny size and cryptic habitat, considering the sporadic distribution and extraordinary rarity of related spp., may also be a relict species surviving with a very limited distribution. This species is one of the few exceptional species with an aragonite calcium-carbonate skeleton among .

Common Japanese name.

Zamami-ishi-hanagoke.

Discussion

Phylogenetic status of in

Results of phylogenetic analyses apparently show that is more closely related to than to other groups of octocorals. The genetic distance between and as shown in branch lengths in the mtMutS tree (Fig. 12) is comparable to what is typically seen among different families of octocorals (e.g. McFadden et al. 2006) (see also Suppl. materials 3, 4). This is the first time the existence of an extant relative of has been confirmed using molecular phylogenetic analyses, as no phylogenetic research on spp. has yet been conducted.

Taxonomic relationship between and

Lonsdale (1850), who described the fossil genus from Chalk (Upper Cretaceous) in Sussex, United Kingdom, felt that was not related to any extant family. According to Lozouet and Molodtsova (2008), was later placed by Voigt (1958) into , which had been defined by the presence of cylindrical anthosteles and connecting stolons. Finally, Bayer and Muzik (1977) placed this genus in the order by examining the type of calcium-carbonate present in skeletons.

The general colony shape of closely resembles encrusting and stoloniferous species of (Bayer, 1992). As well, the basic structure of the skeleton (simple and tubular calyx, indentations on the top of the calyx) is common among and spp. However, longitudinal grooves on the surface of calyces’ skeleton, common to every spp. (see Bayer and Muzik 1977; Bayer 1992; Lozouet and Molodtsova 2008), were not observed in . Instead, the entire surface of the skeleton is covered by a reticulate pattern (Fig. 4). The various descriptions of genus mention possession of calcite calcium-carbonate sclerites (Bayer and Muzik 1977; Bayer 1992; Lozouet and Molodtsova 2008), although actually in some species of the presence of sclerites has not been confirmed due to the absence of soft-tissue in the holotype specimen ( Bayer, 1992), or due to the type specimen being fossilized ( Bayer, 1992) (Bayer 1992; PageBreakLozouet and Molodtsova 2008). The stoloniferous colony is one of the simplest colony morphologies in and is found among many unrelated groups of octocorals, but many other morphological characters apparently suggest the close relatedness of and . In particular, considering the complete lack of sclerites, PageBreakplacement of in a new genus inside is much more appropriate than a major modification of genus and inclusion of within . Molecular phylogenetic data for spp. are necessary to construct the complete phylogeny of .

Taxonomic status of order

The blue coral , the sole member of , has been considered to be extraordinarily distinct among octocorals. When Bayer (1981) reorganized the entire subclass into only three orders, one order was . However, McFadden et al. (2006) showed that sequences were placed within a large – clade. In this study, similar to McFadden et al. (2006), and sequences fell into the same sub-major clade of . However, although no recent molecular study supports the phylogenetic distinctiveness of as an order within subclass , the order is still used. The taxonomic status of this order needs to be re-examined with careful morphological and molecular phylogenetic comparisons. The discovery and confirmation of the phylogenetic relationship of to in this study should contribute to this reassessment.

Geographic distribution and the origin of

Extant is restricted to the Indo-Pacific, and extant species of are found from the Caribbean and the western Indian Ocean (Madagascar), while fossil species of both genera have been found sporadically but widely from Europe. So far, has only been found in Zamami Island, Okinawa, Japan, although surveys are needed to confirm its exact distribution. As indicated in Lozouet and Molodtsova (2008), recent is considered to be a relict of fossil species distributed throughout the Tethys Ocean. Considering the morphological characters of these genera, we can hypothesize that branched first from a common ancestor, subsequently followed by the division of and , although the geographical timing of this split is unknown. As pointed out by Lozouet and Molodtsova (2008), the discontinuous distribution of across the Pacific and the Atlantic implies that at least already existed before the closure of the Tethyan connection. Additionally, the morphological distinctiveness of strongly supports the hypothesis that and radiated before the disjunction of the Atlantic and the Pacific, rather than radiating from Indo-West Pacific . Molecular phylogenetic analyses of Atlantic and Pacific and corroborated studies with paleontology should help confirm the evolutionary history of this unique group.

Cryptic habitat of and

Detailed habitat information of extant species of is unknown as all known living specimens were obtained by dredging or trawling (Bayer and Muzik 1977; Bayer 1992). Lozouet and Molodtsova (2008) indicted fossil species of () were strongly related to submarine canyons, which also included fossil fauna found in muddy sea-floor at depths corresponding to the outer continental shelf or upper slope, submarine cave environments, and rocky circa-littoral cliffs. Considering this information together with the cryptic habitat of (bottom side of carbonate stones), and appear to not reside in shallow well-lit subtropical and tropical environments like , but instead in shaded or cryptic environments. Detailed surveys of such cryptic environments may lead to the discovery of other unknown or species.

Importance of cryptic fauna in

It is astonishing that a unique, relict species such as was found from shallow waters. Generally, relict species are thought to be most commonly found in stable and undisturbed environments, such as abyssal waters, as demonstrated by the discovery of in Africa and Indonesia (Smith 1939; Erdmann et al. 1998). Although not from abyssal depths, extant spp. were also found from quite deep habitats (: 50–400 m, : 183 m, : 200–360 m). The discovery of in this study demonstrates the importance of the study of cryptic anthozoan fauna in shallow coral reef areas (see also Fujii and Reimer 2011), not only for a more correct understanding of coral reef biodiversity, but also to make progress in clarifying the phylogeny and taxonomy of octocorals.

Conclusions

The aragonite calcium-carbonate skeleton is considered to be a synapomorphy among , although only three genera including are currently known from this order. Considering the close phylogenetic relationship between and , and the morphological affinity between and , Bayer and Muzik’s (1977) placement of within based only on small surface structure and aragonite calcium-carbonate skeleton appears appropriate. In this study the phylogenetic position of specimens was suggested by using a molecular phylogenetic approach. mtMutS works well in determining phylogenetic position of such unknown, unclassified species among subclass . Surveying cryptic environments and utilizing proper molecular markers with detailed morphological examinations are an effective way to reveal the true diversity of octocorals.