Asako K Matsumoto1, Leen P van Ofwegen2. 1. Planetary Exploration Research Center (PERC), Chiba Institute of Technology (Chitech), Tsudanuma 2-17-1, Narashino, Chiba 275-0016, Japan. 2. Naturalis Biodiversity Center, Darwinweg 2, P.O. Box 9517, 2300 RA Leiden, The Netherlands.
Abstract
Octocorals with thread-like colony shape have been re-examined, mainly from Japanese waters. The holotypes of Elasmogorgia filiformis and Filigella boninensis and a syntype of Filigella mitsukurii have been studied. Euplexaura arbuscula is identified and Euplexaura yayoii sp. n. described.
Octocorals with thread-like colony shape have been re-examined, mainly from Japanese waters. The holotypes of Elasmogorgia filiformis and Filigella boninensis and a syntype of Filigella mitsukurii have been studied. Euplexaura arbuscula is identified and Euplexaura yayoii sp. n. described.
Entities:
Keywords:
Alcyonacea; Astrogorgia; Challenger Expedition; Indo-Pacific; Plexauridae; Thesea; deep-water octocorals; new species
The octocoral genera , and have been underexplored and their taxonomic position remains confusing. One of the Japanese species of these genera, , is classified with three different genera in WoRMS, as (Ofwegen 2016a), (Ofwegen 2016b), and (Ofwegen 2016c). In this manuscript, a revision is presented of the PageBreakgenera and and their species in Japan, as well as some Japanese species of .The genus Gray, 1868 was established to accommodate from Brazil. Later on Wright and Studer (1899) established the Pacific genus with the remark that their new species could be identical to . Next, Hickson (1905) described from the Maldives, Kinoshita (1909) described from Japan, Nutting (1912) described , also from Japan, and finally Aurivillius (1931) described from the Ogasawara Islands (Bonin Islands), and Thomson and Dean (1931) described from Kalimantan (Indonesia). Both Kinoshita and Aurivillius considered and synonymous and Aurivillius doubted whether of Nutting (1912) belonged to one of these two genera. Kükenthal (1919) first treated them as two separate genera but he synonymized them five years later (Kükenthal 1924).Bayer (1959: 17) was the first to include in the genus Duchassaing & Michelotti, 1860, although he did not directly synonymize the genus with , but much later in his key to the octocoral genera, Bayer (1981: 945). However, he did not re-examine six Pacific species referred to or , and therefore the status of these species has remained doubtful.In the present study, the type material of , , , and , is examined and their previous identifications are discussed. In addition, two specimens identified as by Nutting (1910) and by Thomson and Dean (1931) were examined.
Thomson and Dean (1931) from Kalimantan clearly does not belong to because it has a red colony and also red sclerites. The type specimen of (ZMA 2536) appears to consist of a few branch fragments with disintegrated sclerites. It is considered to represent a species of in the present study.Finally, a new thread-like species is decribed from the Pacific side of northern Japan, sp. n., in addition to Broch, 1935 from off Chishima Is. (Kuril Is.), which previously was reported from the west coast of Kamchatka, Sea of Okhotsk. These two species are both from northern Japan and northeastern Russia (Figure 1).
Figure 1.
Distribution map of (*), (●), (□), and sp. n. (■).
Distribution map of (*), (●), (□), and sp. n. (■).
Material and methods
Abbreviations
BMNHBritish , London, UKNBC (RMNH)Naturalis Biodiversity Center, formerly Rijksmuseum van Natuurlijke Historie, Leiden, The NetherlandsUMUTZUniversity
Museum of , Tokyo, JapanUUZM (UPSZTY)Museum of Evolution, Uppsala, SwedenZMUCZoological
, Copenhagen, DenmarkZINMuseum of the Zoological Institute of the Russian Academy of Sciences St. Petersburg, RussiaZMAZoological Amsterdam (ZMA), now part of NBC
Material
Material was collected from depths between 38 and 366 m by dredging, trawling or fishing net onboard RV Tansei-maru, and Japan Agency for Marine-earth Science and Technology and RV Yayoi, the , during the years 1975–2010. Type specimens and other historical museum material was examined in collections of the BMNH, NBC, UMUTZ, UUZM, ZIN, and ZMUC.From each specimen a small piece of the distal part of a branch was dissolved in a solution of household bleach (4% hypochlorite) to isolate sclerites. The sclerites were washed with demineralised water, dried on a hot plate, mounted on SEM stubs, and coated with Pd/Au for SEM imaging. For this, either a JEOL JSM6490LV scanning electron microscope was operated at high vacuum at 10 kV, or a JEOL JSM6510LA scanning electron microscope with a Quick Carbon Coater SC-701C, SANYU ELECTRON was used. For terminology, see Bayer et al. (1983).Descriptions of old Japanese material collected by Japanese used “hiro” (Japanese fathom) as the depth unit. One Japanese fathom (hiro) is usually 1.43 m, occasionally 1.51 m, whereas, it is 1.818 m for the length unit on land. The old depth unit fathom PageBreakis also converted to 1.8288 m. When it was not clear whether the collector used fathom or hiro, the converted depth has wider ranges.
Holotype BMNH 1889.5.27.77, Arafura Sea, South of Papua, 28 fms, Challenger st. 188, 10 September 1874; ZMA Coel. 2537, Siboga st. 213, Saleyer anchorage, Sulawesi, Indonesia, 38 m, 26 September 1899 (= ); ZMA Coel. 2538, Timor, 112 m, Siboga st. 289, (= ).Colony thread-like (Figure 2a). Calyces dome-shaped, arranged all around the branches (Figure 2a). Coenenchyme with spindles up to 0.45 mm long, with simple tubercles (Figures 3–4). Colony white with colourless spindles.a
Wright & Studer, 1889, holotype BMNH 1889.5.27.77 b
Broch, 1935, ZIN 11667 c
(Aurivillius, 1931), holotype UPSZTY2165 (UUZM 68) d
(Kinoshita, 1909), syntype UMUTZ-CnidG-222 e
sp. n., holotype RMNH 42104.Wright & Studer, 1889, holotype BMNH 1889.5.27.77, a spindles from surface layer of coenenchyme b capstan.Wright & Studer, 1889, holotype BMNH 1889.5.27.77, a spindles from interior of coenenchyme b possible collaret spindle c rod.
Remarks.
One somewhat flattened spindle was found, 0.35 mm long, maybe referable to a collaret (Figure 4b), and one capstan (Figure 3b). As the microscope slide that was made only shows heavily oxidized black sclerites it could not be really ascertained where different types of sclerites came from. The little fragment available was not sufficient for more extensive examination. Wright and Studer (1889) mentioned spindles up to 0.62 mm long. They also mentioned the basal portion of the tentacles has spindle-shaped sclerites of up to 0.18 mm long. mostly resembles a species of but differs in not having polyp body sclerites and PageBreakPageBreakPageBreakextremely weak ornamentation of spindles. Until new material becomes available for a more thorough examination the genus is retained.ZMA 2537 of Thomson and Dean (1931) is a thread-like colony fragment containing colourless disintegrated sclerites, which were sufficiently recognizable to identify it as a species of . In a comparison with Ofwegen and Hoeksema, 2001, from Sulawesi, the latter species appears to have shorter spindles, up to 0.5 mm long, whereas Thomson and Dean's (1931) specimen has spindles of over 1 mm long. Because of the disintegrated state of its sclerites, no more differences could be ascertained.ZMA 2538 of Nutting (1910) was also re-examined; it has characters of the genus . of Nutting (1912) is also unlikely an .Verrill, 1869Verrill, 1869: 75;with colonies branched in one plane. Calyces may be present but are mostly absent. Polyps with collaret and points, only point sclerites, or no sclerites at all. The surface of the coenenchyme with robust ovals or spindles with complex tubercles; sometimes with one side that is less tuberculate. The interior with rods or small spindles with simple tubercles. All sclerites colourless.Broch, 1935Figures 1
, 2b
, 5
Figure 5.
Broch, 1935, ZIN 11667 a spindles and blunt ellipsoids from surface layer of coenenchyme b–d sclerites from interior of coenenchyme b spindles c capstans d cross.
Broch, 1935: 20, fig. 12.
Material.
ZIN 11667(ZIN110824-018-040), Skaly Lovushki I., off Chishima Is. (= Kuril Is.), , depth 140 m, Bottom: gravel with stones, Ship Odissey, Grab “Ocean” 50 cm2 (bottom sampler), coll. Boris Sirenko and Mikhail Kolesnikov, 3 August 1984.Branches thread-like. Calyces dome-shaped, arranged all around the branches (Figure 2b). Polyps without sclerites. The surface layer of the coenenchyme has spindles and blunt ellipsoids (Figure 5a), up to 0.15 mm long, with complex tubercles. The interior has small spindles, capstans, and a few crosses, up to 0.15 mm long (Figures 5b-d), all with simple tubercles.Broch, 1935, ZIN 11667 a spindles and blunt ellipsoids from surface layer of coenenchyme b–d sclerites from interior of coenenchyme b spindles c capstans d cross.The material examined was fragmentary (Figure 2b) and therefore it resembles a species of .Kukenthal, 1909 resembles regarding its sclerites, but it differs in having polyp spindles.Since its original description, the species was not found again and its type material could not be retraced, hence some doubts remain about the identification of this species. Broch (1935) described the species only from one specimen. It is not present in the , and ZIN.
Distribution.
Kamchatka, Sea of Okhotsk, off Chishima Is. (= Kuril Is.).(Aurivillius, 1931)Figures 1
, 2c
, 6
, 7
Figure 6.
(Aurivillius, 1931), holotype UPSZTY2165 (UUZM 68), a tentacle scales b point spindles c collaret spindles d spindles from surface layer of coenenchyme e blunt ellipsoids from surface layer of coenenchyme.
Figure 7.
(Aurivillius, 1931), holotype UPSZTY2165 (UUZM 68), sclerites of interior of coenenchyme.
Aurivillius, 1931: 139 (Bonin Islands).;Holotype UPSZTY2165 (UUZM 68), East of Chichijima I., Ogasawara Is. (= Bonin Is.), Japan, depth 100 m, in formalin, Dr. Sixten Bock's, Japan Expedition, coll. Dr. Sixten Bock, 1 August 1914.Branches thread-like, 6 cm in length. Calyces dome-shaped, arranged all around the branches (Figure 2c). The polyps have points with flattened spindles, up to 0.15 mm long (Figure 6b), with simple tubercles and spiny distal end. Collaret present, with slightly bent, flattened spindles, up to 0.25 mm long, with simple tubercles (Figure 6c). Tentacles with small scales, up to 0.10 mm long (Figure 6a).(Aurivillius, 1931), holotype UPSZTY2165 (UUZM 68), a tentacle scales b point spindles c collaret spindles d spindles from surface layer of coenenchyme e blunt ellipsoids from surface layer of coenenchyme.The surface layer of the coenenchyme has spindles (Figure 6d) and blunt ellipsoids (Figure 6e), up to 0.65 mm long, with complex tubercles. Several of them with one side less tuberculate. The interior has small spindles and rods, up to 0.25 mm long (Figure 7), with simple tubercles.(Aurivillius, 1931), holotype UPSZTY2165 (UUZM 68), sclerites of interior of coenenchyme.Because the sclerites of this species are spindles and ellipsoids with complex tubercles it actually represents an species. It is the only species of with thread-like colony shape which has many sclerites with one side that is less tuberculate.(Kinoshita, 1909)Figures 1
, 2d
, 8
, 9
Figure 8.
(Kinoshita, 1909), syntype UMUTZ-CnidG-222 a tentacle scales b point spindles c collaret spindles d–e spindles from surface layer of coenenchyme. Scale at d only applies to d.
Figure 9.
(Kinoshita, 1909), syntype UMUTZ-CnidG-222 sclerites of interior of coenenchyme.
Kinoshita, 1909: 1(Sagami Bay);;;sp.Syntypes UMUTZ-CnidG-222, off Jogashima I., Sagami Bay, Japan, depth 70 Japanese fathoms (100-106 m), secured with Hydra dredge, 26 August 1901; UMUTZ-CnidG-223, Japanese 2 nautical miles (5 km in Kinoshita, 1909) of West South off Jogashima I., Sagami Bay, Japan, saba-nawa line, 31 July 1892. Identified museum material UMUTZ-CnidG-122, off Torishima I., Japan, East China Sea, - , depth 64 fms (117 m), trawl, coll. N. Yanaghi, 22 June 1913, det. F.M. Bayer, ca.1950, as ; UMUTZ-CnidG-126 same data as UMUTZ-CnidG-122, as . Unidentified museum material. ZMUC ANT-000611 (ZMUC120604-09), East China Sea, , depth 75 fms (137 m), sand, Hyateri maru, trawl, coll. Dr. Th. Mortensen, 17 May 1914; ZMUC ANT-000616 (ZMUC120604-16), East China Sea, , depth 90 fms (165 m), hard bottom, Hyateri maru, coll. Dr. Th. Mortensen, 15 May 1914; ZMUC ANT-000664 (ZMUC120604-59), , depth 60 fms (110 m), sand, coll. Dr. Th. Mortensen, 18 May 1914; ZMUC ANT-000655 (ZMUC120604-67), off Misaki Biological Station, Sagami Bay, Japan, depth 200 fms (366 m), sand, coll. Dr. Th. Mortensen, 30 June 1914; AKM1630, Sukumo Bay, Bungo Channel, Japan, ca.-30'E, depth 144-150 m, RV Tansei-maru, KT86-16, st.A-8, 1 m ORI biological dredge, coll. S. Ohta, 1 November 1986; AKM1631, off Kashima, Kashima Sea, Japan, , depth 63-71 m, RV Tansei-maru, KT79-13, st. KB2, 2 m Beam trawl, coll. S. Ohta, 7 August 1979; AKM1632, off Toi, Suruga Bay, Japan, depth 192-207 m, - , RV Tansei-maru, KT75-15, st. 02, 2 m Beam Trawl, coll. S.Ohta, 24 November 1975; AKM1566, South East off Taito-saki Cape, Boso Peninsula, Japan, - , depth 104-105 m, RV Tansei-maru, KT01-08, st. TZ-7, 1 m ORI biological dredge, coll. S. Ohta, 22 June 2001; AKM 1644, off Hitachi, Kashima sea, Japan, - , depth 79–82 m, RV Tansei-maru, KT79-13, st. KB14, 2 m Beam trawl, coll. S. Ohta, 9 August 1979.Branches thread-like. The examined syntype has two branches arising from the main stem with a length of 19 cm and 28.5 cm, respectively; the main stem is 9 cm long. Calyces dome-shaped, arranged all around the branches (Figure 2d). The polyps have points with flattened spindles, up to 0.20 mm long (Figure 8b), with simple tubercles. Collaret present, with slightly bent, flattened spindles, up to 0.30 mm long, with sparse, simple tubercles (Figure 8c). Tentacles with small scales, up to 0.10 mm long (Figure 8a).(Kinoshita, 1909), syntype UMUTZ-CnidG-222 a tentacle scales b point spindles c collaret spindles d–e spindles from surface layer of coenenchyme. Scale at d only applies to d.The surface layer of the coenenchyme has spindles (Figure 8d–e), up to 0.35 mm long, with complex tubercles. Some of them with one side that is less tuberculate. The interior has small spindles and rods, up to 0.25 mm long (Figure 9), with simple tubercles.(Kinoshita, 1909), syntype UMUTZ-CnidG-222 sclerites of interior of coenenchyme.Because the sclerites of this species are spindles with complex tubercles this is actually a species of .Kinoshita (1909) mentioned 13 specimens of and three of them were complete. He used two specimens for his original description. Nowadays PageBreaktwo specimens are present in UMUT and the data fit Kinoshita's, two specimens in his description.The locality name “Jogaschima, Pagamibai” of this species in Kükenthal (1924) is a mistyping of “Jogashima, Sagamibai (Sagami Bay)”.Sagami Bay, off Boso Peninsula, Kashima Sea, Suruga Bay, Bungo Channel, East China Sea, Japan.
sp. n.
http://zoobank.org/65B660AC-70D9-4697-8411-A1F3116FFD47Figures 1
, 2e
, 10
, 11
Figure 10.
sp. n., holotype RMNH 42104 a tentacle scales b point spindles c collaret spindles d–e sclerites of interior of coenenchyme d spindles e crosses.
Figure 11.
sp. n., holotype RMNH 42104 sclerites from surface layer of coenenchyme.
Holotype RMNH 42104 (AKM1551), Off Ohako-zaki cape, Otsuchi Bay, Iwate Prefecture, Japan. , depth 77.0 m, RV Yayoi, st. 4-1, coll. A.K. Matsumoto, 27 April 2010; paratypes RMNH 42105 (AKM592), entrance of Otsuchi Bay, Iwate Prefecture, Japan, , depth 65.6 m, RV Yayoi, st. 1, coll. A.K. Matsumoto, 12 September 2005; RMNH 42106 (AKM597), same data as AKM 592; RMNH 42107 (AKM623), off Ohako-zaki cape, Otsuchi Bay, Iwate Prefecture, Japan, , depth 63 m, RV Yayoi, st. 2, coll. A.K. Matsumoto, 12 September 2005.
Description.
The holotype is 2.5 cm high and 5.5 cm wide (Figure 2e). The colony is branched only once, 1 cm above the base. The two branches are very slender, only 1 mm thick; the calyces are low, dome-shaped, arranged spirally around the branches.The polyps have points with slightly bent, flattened spindles, up to 0.30 mm long, with a few tubercles and a slightly spiny distal end (Figure 10b). The collaret has bent, flattened spindles, up to 0.30 mm long, with simple tubercles, the largest tubercles present in the middle (Figure 10c). The tentacles have flattened rods, up to 0.15 mm long, with hardly any tubercles (Figure 10a). The surface layer of the branches has spindles and blunt ellipsoids, up to 0.15 mm long, with complex tubercles (Figure 11). The deeper layer has short spindles, up to 0.10 mm long, and a few crosses (Figure 10d-e); all with simple tubercles.sp. n., holotype RMNH 42104 a tentacle scales b point spindles c collaret spindles d–e sclerites of interior of coenenchyme d spindles e crosses.sp. n., holotype RMNH 42104 sclerites from surface layer of coenenchyme.
Etymology.
Named after the research vessel that was used to collect the specimens.The live colony has blue-coloured polyps. differs from the two other Japanese species with thread-like branches, and , by its very small sclerites.Otsuchi Bay, Iwate Prefecture, Japan.
Discussion
Originally, there were four species of : Wright & Studer, 1889,
Thomson and Dean 1931, Hickson, 1905, and Nutting, 1912. Based on the present re-examination, it is obvious that PageBreakPageBreakPageBreak, with spindles covered by simple tubercles, is not a species of . Corals of this genus have coarse rugose plates, sometimes tuberculate spindles and double heads (Bayer 1981). Therefore the genus is reinstated here. The only two species from Japan previously recognized as , i.e., and , were re-examined and both proved to belong to the genus . from Kalimantan is a species of . This leaves and unexamined. was collected by the Steamer Albatross at Satamisaki Light, south of Kyushu I., Kagoshima prefecture, Japan, 103 fms (188 m), and from the Maldives. From the descriptions of these two species it is obvious that , with a heavily branched colony, is not a or . , with spindles with complex tubercles probably is a species of , and therefore the genus is considered here monotypic with as its only member. mostly resembles a species of . Following Bayer (1981) we also consider a synonym of . All Japanese species previously included in are assigned to in this study.All Japanese thread-like plexaurid material South of Kashima Sea was previously identified as and it clearly is the most common thread-like plexaurid species of Japan.