Research Article |
Corresponding author: James Davis Reimer ( jreimer@sci.u-ryukyu.ac.jp ) Academic editor: Bert W. Hoeksema
© 2018 Yee Wah Lau, Frank Robert Stokvis, Leendert Pieter van Ofwegen, James Davis Reimer.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Lau Y, Stokvis F, van Ofwegen L, Reimer J (2018) Stolonifera from shallow waters in the north-western Pacific: a description of a new genus and two new species within the Arulidae (Anthozoa, Octocorallia). ZooKeys 790: 1-19. https://doi.org/10.3897/zookeys.790.28875
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A new genus and two new species of stoloniferous octocorals (Alcyonacea) within the family Arulidae are described based on specimens collected from Okinawa (Japan), Palau and Dongsha Atoll (Taiwan). Hana gen. n. is erected within Arulidae. Hana hanagasa sp. n. is characterised by large spindle-like table-radiates and Hana hanataba sp. n. is characterised by having ornamented rods. The distinction of these new taxa is also supported by molecular phylogenetic analyses. The support values resulting from maximum likelihood and Bayesian inference analyses for the genus Hana and new species H. hanagasa and H. hanataba are 82/1.0, 97/1.0 and 61/0.98, respectively. Hana hanagasa sp. n. and Hana hanataba sp. n. are the first arulid records for Okinawa, Palau, and Dongsha Atoll, and represent species of the second genus within the family Arulidae.
Arulidae , COI, molecular phylogeny, mtMutS, north-western Pacific, octocoral, 28S rDNA, Stolonifera , taxonomy
Stolonifera is a subordinal group within Octocorallia, consisting of octocoral families that have been grouped together based mainly on the character of having polyps that arise separately from an encrusting horizontal, branching, ribbon-like stolon, or with polyps arising from broad, encrusting membranes. Stoloniferans are therefore morphologically different from other octocorals, which have their polyps embedded within common coenenchymal tissue. Like soft corals, stoloniferan octocorals are found in various marine ecosystems, such as coral reefs in shallow tropical and temperate seas (
Until 2012, there were six families of Alcyonacea considered to belong to the Stolonifera; Acrossotidae Bourne, 1914, Coelogorgiidae Bourne, 1900, Cornulariidae Dana, 1846, Clavulariidae Hickson, 1894, Pseudogorgiidae Utinomi & Harada, 1973, and Tubiporidae Ehrenberg, 1828. Of these, the family Clavulariidae is the most speciose and most studied, comprising 27 genera and over 60 species (
Recent observations and collections in the north-western Pacific have revealed a similar abundance of stoloniferous octocoral species in coral reefs that are either unrecorded or even undescribed (
A total of 16 arulid specimens were collected, at Okinawa Island, Japan (n=12) from June to August 2017, at Palau (n=2) from December 2017 to January 2018, and at Dongsha Atoll, Taiwan (n=2) from April to May 2018. All specimens were collected at depths between 5–30 m by means of SCUBA. Material was preserved in 99% ethanol. In total eight localities were visited for sampling, Okinawa Island (n = 4), Palau (n = 2), and Dongsha Atoll (n = 2) (Figure
Information on voucher specimens and GenBank accession numbers of stoloniferan octocoral taxa and reference taxa used in phylogenetic analyses in this study. Collection numbers:
Family | Genus/species | Specimen voucher | Location | GPS (DDM) | Genbank AN | ||
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COI | mtMutS | 28S rDNA | |||||
Arulidae | Arula petunia |
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South Africa |
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JX203827 | JX203773 | JX203670 |
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South Africa |
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JX203828 | JX203774 | JX203671 | ||
Hana hanagasa gen. n., sp. n. | OKA170629-01 | Iheya – Iheya Island, Okinawa Island, Japan | 27°5.710’N, 128°1.828’E | MH845559 | n.a. | MH844382 | |
OKA170711-06 | Hedo Dome – Cape Hedo, Okinawa Island, Japan | 26°51.125’N, 128°15.027’E | MH845552 | n.a. | n.a. | ||
OKA170711-07 | Hedo Dome – Cape Hedo, Okinawa Island, Japan | 26°51.125’N, 128°15.027’E | n.a. | n.a. | n.a. | ||
OKA170711-08 | Hedo Dome – Cape Hedo, Okinawa Island, Japan | 26°51.125’N, 128°15.027’E | MH845553 | n.a. | n.a. | ||
OKA170711-10 | Hedo Dome – Cape Hedo, Okinawa Island, Japan | 26°51.125’N, 128°15.027’E | MH845554 | MH845544 | n.a. | ||
OKA170711-16 | Hedo Dome – Cape Hedo, Okinawa Island, Japan | 26°51.125’N, 128°15.027’E | n.a. | n.a. | n.a. | ||
OKA170711-15 | Canyon – Cape Hedo, Okinawa Island, Japan | 26°52.326’N, 128°15.995’E | MH845555 | MH845545 | n.a. | ||
OKA170711-17 | Canyon – Cape Hedo, Okinawa Island, Japan | 26°52.326’N, 128°15.995’E | n.a. | MH845546 | n.a. | ||
OKA170711-20 | Hedo Dome – Cape Hedo, Okinawa Island, Japan | 26°51.125’N, 128°15.027’E | MH845556 | MH845547 | MH844383 | ||
OKA170818-03 | Futagami-iwa – Cape Hedo, Okinawa Island, Japan | 26°52.177’N, 128°14.847’E | MH845557 | n.a. | MH844384 | ||
OKA170818-05 | Futagami-iwa – Cape Hedo, Okinawa Island, Japan | 26°52.177’N, 128°14.847’E | n.a. | n.a. | n.a. | ||
OKA170818-11 | Canyon – Cape Hedo, Okinawa Island, Japan | 26°52.326’N, 128°15.995’E | MH845558 | n.a. | n.a. | ||
ROR171225-01 | Blue Corner – Ngemelis Island, Palau | 7°8.400’N, 134°13.200’E | MH845550 | n.a. | MH844386 | ||
ROR171226-03 | Peleliu PICRC monitoring site – Peleliu, Palau | 7°0.400’N, 134°13.060’E | MH845551 | MH845543 | MH844387 | ||
DSX180420-1-01 | North spur & grooves – Dongsha Atoll, Taiwan | 20°46.291’N, 116°46.057’E | MH845548 | n.a. | n.a. | ||
DSX180424-3-15 | North – Dongsha Atoll, Taiwan | 20°46.677’N, 116°50.090’E | MH845549 | MH845542 | MH844385 | ||
Clavulariidae | Paratelesto sp. |
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Mcfadden & Ofwegen, 2012 |
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GQ342411 | GQ342489 | JX203693 |
Rhodelinda sp. |
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Mcfadden & Ofwegen, 2012 |
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JX203845 | n.a. | JX203695 |
Sclerites were isolated by dissolving entire polyps and stolons in 4% hypochlorite (household bleach). Sclerites were rinsed at least seven times with de-ionised water, dried, and initially studied by embedding the sclerites in Euparal on glass slides. In addition, for more detailed morphological studies, sclerites were mounted on scanning electron microscope (SEM) stubs and coated with Pd/Au for imaging on a JEOL JSM6490LV SEM operated at high vacuum at 15kV.
DNA was extracted from polyps, using a DNeasy Blood and Tissue kit (Qiagen, Tokyo). PCR was performed for two mitochondrial markers, cytochrome c oxidase subunit I (COI) and the MSH homologue mtMutS. The nuclear ribosomal marker, 28S rDNA, was amplified as well. The ~900 bp fragment of COI was amplified using the primers COII8068xF 5’-CCATAACAGGACTAGCAGCATC-3’ and COIOCTr 5’-TCATAGCATAGACCATACC-3’ (
Multiple sequence alignments were performed using MAFFT 7 (
Arula McFadden & Ofwegen, 2012
(after
Hana hanagasa, sp. n., by original designation.
Colony with polyps connected through flat and thin ribbon-like stolons. Anthocodiae (retractile portion of polyp) retract into cylindrical to clavate calyces. Tentacles are fused proximally, forming a broad, circular oral membrane. The oral membrane has eight deep furrows, which run from the intertentacular margin to the mouth of the polyp, giving it a plump appearance. Sclerites of anthocodia are rods. Sclerites of calyx are 6-radiates and table-radiates. The main difference between Hana and Arula is in sclerites found in the type species Hana hanagasa sp. n. and Arula petunia in the stolon. Sclerites of the stolon are fused sheets that form a flattened network of table-radiates in H. hanagasa, while in A. petunia they are similar to the separate table-radiates found in the calyx. Additionally, there is a difference in sizes of the table-radiates, being longer in H. hanagasa than in A. petunia. Sclerites colourless. Zooxanthellate.
From the Japanese language ‘hana’ (花), meaning flower; denoting the shape of the polyps, which resemble flowers. Gender: feminine.
All specimens are from Okinawa Island, Okinawa, Japan. Holotype: OKA170711-15, Canyon, Cape Hedo (26°52.326'N, 128°15.995'E), 17 m depth, coll. YW Lau, 11 July 2017 (MH845555; MH845545). Paratype 1: OKA170629-01, Iheya, Iheya Island (27°5.710'N, 128° 1.828'E), coll. R Janssen, 29 June 2017 (MH845559; MH844382). Paratype 2: OKA170711-06, Hedo Dome, Cape Hedo (26°51.125'N, 128°15.027'E), 6 m depth, coll. YW Lau, 11 July 2017 (MH845552). Paratype 3: OKA170711-07, Hedo Dome, Cape Hedo (26°51.125'N, 128°15.027'E), 6 m depth, coll. YW Lau, 11 July 2017. Paratype 4: OKA170711-08, Hedo Dome, Cape Hedo (26°51.125'N, 128°15.027'E), 10 m depth, coll. YW Lau, 11 July 2017 (MH845553). Paratype 5: OKA170711-10, Hedo Dome, Cape Hedo (26°51.125'N, 128°15.027'E), 11 m depth, coll. YW Lau, 11 July 2017 (MH845554; MH845544). Paratype 6: OKA170711-16, Hedo Dome, Cape Hedo (26°51.125'N, 128°15.027'E), 7 m depth, coll. FR Stokvis, 11 July 2017. Paratype 7: OKA170711-17, Canyon, Cape Hedo (26°52.326'N, 128°15.995'E), 16 m depth, coll. FR Stokvis, 11 July 2017 (MH845546). Paratype 8: OKA170711-20, Hedo Dome, Cape Hedo (26°51.125'N, 128°15.027'E), coll. JD Reimer, 11 July 2017 (MH845556; MH845547; MH844383). Paratype 9: OKA170818-11, Canyon, Cape Hedo (26°52.326'N, 128°15.995'E), collected by JD Reimer, 18 August 2017 (MH845558). Paratype 10: OKA170818-03, Futagami-iwa, Cape Hedo (26°52.177'N, 128°14.847'E), 22 m depth, coll. YW Lau, 18 August 2017 (MH845557; MH844384). Paratype 11: OKA170818-05, Futagami-iwa, Cape Hedo (26°52.177'N, 128°14.847'E), 11 m depth, coll. JD Reimer, 18 August 2017.
The colony consists of numerous small polyps (~50) growing on hard coral rock. Polyps are spaced apart irregularly (0.3–2.5 mm), connected by stolons that are 0.5 mm in diameter and flat thin ribbon-like in cross-section. Polyps have anthocodia fully retracted into calyces of 2.5–3 mm tall and up to 1.0 mm diameter at the widest point; calyces are slightly club-shaped or barrel shaped, wider near the distal end than at the proximal point of attachment to the stolon.
The oral disk expands into a broad circular membrane by fusion of the proximal regions of the adjacent tentacles. The margin of the oral membrane has eight broad lobes, with eight deep furrows, which run from the intertentacular margin to the mouth of the polyp, giving a plump appearance (Figure
In situ photographs of examined Hana specimens from Okinawa, a Hana hanagasa, holotype, OKA170711-15 and b Hana hanagasa, paratype, OKA170711-06; Palau c Hana hanataba holotype, ROR171225-01 and d Hana hanataba, paratype, ROR171226-03; Dongsha e Hana hanataba, paratype, DSX180320-1-01 and f Hana hanataba, paratype, DSX180324-3-15 g specimen BKI180320-2-10, an arulid photographed in Tunku Abdul Rahman Park, Sabah, Malaysia h Hana hanagasa, holotype, OKA170711-15, colony preserved in ethanol. Scale bar: 1 mm.
Anthocodial sclerites are small rods with simple tubercles around margins 0.10–0.18 mm long (Figure
The oral disk is white and the tentacles are brown in life (Figure
Paratypes are colonies consisting of 50–100 polyps, growing on hard substrates and sponges. Colonies show variations in number of pinnules, having 8–10 pairs lining either side of the rachis.
Northwest coast of Okinawa Island and southeast coast of Iheya Island in the East China Sea.
Arula and Hana are the only two genera within the family Arulidae. Arula petunia and H. hanagasa have very similar polyp morphologies with only a clear difference in polyp colour. Oral disk and tentacles of A. petunia are blue in life and white and brown in H. hanagasa, respectively. This would suggest assignment to the same genus, however, the combination of differences in genetic data and sclerite morphology indicate that they should be separate from each other at the generic level. The possibility that there are similar species or previous descriptions and reports on arulid species has previously been discussed (
From the Japanese language ‘hanagasa’ (花笠), the traditional Okinawan ceremonial dance headpiece worn by female performers; denoting the shape of the polyps, which resembles the flower headpiece.
Holotype: ROR171225-01, Blue Corner, Ngemelis Island, Palau (7°8.400'N, 134°13.200'E), 23 m depth, coll. YW Lau, 25 July 2017 (MH845550; MH844386). Paratype 1: ROR171226-03, Peleliu PICRC monitoring site, Peleliu, Palau (7°0.400'N, 134°13.060'E), 28 m depth, coll. GY Soong, 26 December 2017 (MH845551; MH845543; MH844387). Paratype 2: DXS180420-1-01, North spur & grooves, Dongsha Atoll, Taiwan (20°46.291'N, 116°46.057'E), 7 m depth, coll. YW Lau, 20 April 2018 (MH845548). Paratype 3: DSX180424-3-15, North, Dongsha Atoll, Taiwan (20°46.677'N, 116°50.090'E), 8 m depth, coll. JD Reimer, 24 April 2018 (MH845549; MH845542; MH844385).
The colony consists of small polyps (~30) growing on rock. Polyps are spaced apart irregularly (0.5–2.5 mm), connected by stolons that are 0.5 mm in diameter and flat thin ribbon-like in cross-section. Polyps have anthocodia retracted into calyces of 2.5–3.0 mm tall and up to 1.0 mm diameter at the widest point; calyces are slightly club-shaped or barrel shaped, wider near the distal end than at the proximal point of attachment to the stolon.
The oral disk expands into a broad circular membrane by fusion of the proximal regions of the adjacent tentacles (Figure
Anthocodial sclerites are rods with sparse simple tubercles around margins 0.07–0.24 mm long and rods ornamented with clustered tubercles on one end, giving it a club-shaped appearance, size 0.10–0.18 mm (Figure
The oral disk and tentacles are white in life with brown in the proximal part of tentacle (Figure
Paratypes consist of colonies with 30–100 polyps, growing on hard substrates. Colonies show variations in the tentacles, sometimes having ten pairs of pinnules.
The south-east of Palau in the Philippine Sea and the north to north-east reef of Dongsha Atoll, Taiwan in the South China Sea.
Hana hanagasa and Hana hanataba have very similar polyp morphology, with minor colour differences, which could be due to differing abundances of zooxanthellae. Genetic data and sclerite morphology indicate that H. hanagasa and H. hanataba should be separated from each other at the species level. Sclerites found in H. hanataba are different from those in H. hanagasa in the presence of ornamented rods, which are lacking in H. hanagasa. It is noteworthy that both H. hanagasa and H. hanataba were found in environments with the presence of a comparatively strong current.
From the Japanese language ‘hanataba’ (花束), meaning bouquet; denoting the multitude of polyps resembling arranged flowers.
This study has added 24 sequences to the reference database, representing two species for which no barcodes have been sequenced before. The phylograms resulting from the ML analyses of the separate markers were highly congruent with those from the analysis of the combined markers (Figure
Phylogenetic reconstruction for arulid specimens from Okinawa Island (OKA), Palau (ROR), Dongsha Atoll (DSX), arulid reference taxa (Arula petunia) and outgroup sister taxa (Paratelesto sp. and Rhodelinda sp.) using the combined COI+mtMutS+28S rDNA dataset. The best maximum likelihood tree is shown, with values at branches representing bootstrap probabilities (>50%) and posterior probabilities from the Bayesian inference analysis (>0.50), respectively. Sclerites unique to Hana hanagasa and Hana hanataba are shown and typical table radiates found in the family Arulidae are shown for the genus Arula.
Sequences of H. hanagasa, gen. n., sp. n., from Okinawa Island and H. hanataba, gen. n., sp. n., from Palau and Dongsha Atoll, Taiwan, grouped together in a well-supported clade within the Arulidae. The sequences formed a separate clade from sequences of Arula petunia (Figure
The separation of H. hanagasa and H. hanataba was confirmed by molecular analyses and through the investigation of the sclerites. The genetic distances (uncorrected p, expressed as percentage) within the genus Hana between H. hanagasa and H. hanataba were 0.8% and 0.67% for COI and mtMutS, respectively [Suppl. material
The new species H. hanagasa and H. hanataba bring the total number of species within the Arulidae to three and represent the first confirmed records of arulids for the north-western Pacific. Arulids so far have been recorded only in South Africa with informal reports of other possible congeners occurring in Sabah, Malaysia (Figure
Even though all new arulid specimens were amplified for four markers, here we used only three of the gene regions, 28S rDNA, COI and mtMutS, in the analyses. ND6 was excluded from the analyses, as the outgroup sequences lacked available ND6 sequences. There were no differences in results when including or excluding this region when performing analyses with concatenated datasets. However, utilising four region sequences resulted in better resolution. Therefore, for future analyses, it is recommended to include ND6 to obtain better resolution.
It has been made clear in previous studies that the subordinal group Stolonifera is polyphyletic (
Fieldwork in Palau was part of the SATREPS P-CoRIE Project “Sustainable management of coral reef and island ecosystem: responding to the threat of climate change”, funded by the Japan Science and Technology Agency (JST) and the Japan International Cooperation Agency (JICA) in cooperation with Palau International Coral Reef Center and Palau Community College. We thank H Kise and J Oruetamor for logistics in Palau. We thank GY Soong for providing a specimen and corresponding photograph (Palau; ROR171226-03 Hana hanataba; Figure
Supplemental figures 1–3
Supplemental tables 1, 2