A new species of Crypthelia, C. kelleyi, is described from a seamount in the Northwestern Hawaiian Islands, making it the fifth species of stylasterid known from the Hawaiian Islands. Collected at 2,116 m, it is the fourth-deepest stylasterid species known.
Once thought to be absent from Hawaiian waters (Boschma 1959), four stylasterid species have been reported from this archipelago, primarily on seamounts and off small islands in the Northwestern Hawaiian Islands at depths of 293–583 m (Cairns 2005). This is consistent with the theory of Cairns (1992) that stylasterids are insular in occurrence, usually being found on seamounts and off small volcanic islands. Cairns (1978) reported the first Hawaiian species, Distichopora anceps, from off Laysan, and he described three more species in 2005, the latter in the genera Distichopora and Stylaster. Herein a fifth species is reported, also from the Northwestern Hawaiian Islands, but at a much greater depth, 2,116 m, making it the fourth-deepest stylasterid ever collected among the 316 known species. The three deeper species are Crypthelia affinis Moseley, 1879 (2,789 m); Crypthelia medioatlantica Zibrowius & Cairns, 1992 (2,644 m); and Conopora verrucosa (Studer, 1878) (2,355 m).
materials and methods
The specimen was collected on the Okeanos Explorer expedition to the Northwestern Hawaiian Islands, which took place in August 2015. The benthic Cnidaria from this expedition were preserved in 70% ethanol and subsequently deposited at the nmnh. The scanning electron photomicrographs were taken by the author using a Zeiss EVO MA15 scanning electron microscope.
The following abbreviations are used in the text: BPBM, Bernice P. Bishop Museum, Honolulu; D2, Deep Discover remotely operated vehicle; EX, Okeanos Explorer; L2, Leg 2 of cruise; NMNH, National Museum of Natural History, Washington, D.C.; SEM, Scanning Electron Microscope (prefacing stub number of Cairns series); usnm, United States National Museum (now the National Museum of Natural History), Washington, D.C.
results and discussion
Corallum usually uniplanar, but may also be biplanar or monopodial; commensal calcareous worm living in calcareous tubes often present. Coenosteal texture usually linear-imbricate; nematopores common. Gastro- and dactylopores arranged in cyclo-systems, which usually occur unilinearly on anterior face, but may also occur on posterior [End Page 77] face. Gastropore tube double-chambered, the upper chamber separated from the lower by a circular ring constriction; gastrostyles absent. Gastropores covered by a fixed lid of variable size and inclination. Both male and female ampullae usually superficial, occurring in a variety of positions on the corallum; efferent pores also variable in placement, but often occur beneath the cyclosystem lid.
Cosmopolitan, except for off continental Antarctica and the Arctic, 85–2,789 m.
Including the new species described herein, the genus Crypthelia contains 47 Recent species (Cairns 2016), making it the second-most species-rich genus in the family, following Stylaster with 88 Recent species. Almost half of these species were recently redescribed and figured by Cairns (2015) from the New Caledonian region. As he pointed out, the species can be segregated as to whether they harbor commensal polynoid polychaetes or not, as well as by their ampullar formula (i.e., the location of the female and male ampullae and their respective efferent pores) (Cairns 2015:Table 9).
Crypthelia kelleyi Cairns, n. sp
Figures 1A–F, 2A–D
Holotype: one female colony and numerous small fragments preserved in 70% ethanol, SEM C2347–2349, usnm 1294083; fragments (part of holotype) bpbm D2339.
Okeanos Explorer EX1504L2_D2_Dive 11: 27° 07′ 51″ N, 175° 34′ 15″ W (north rift zone ridge of Bank 9 North, south of Pearl and Hermes Atoll, Northwestern Hawaiian Islands), 2,116 m, 12 August 2015.
The corallum is flabellate, the holotype (Figure 1A) measuring 64 mm in height and 53 mm in width. Branch anastomosis is common, especially in the basal region of the corallum; there is no polychaete commensalism. The coenosteal texture is linear-imbricate (Figure 1C, E) to reticulate-imbricate, the latter condition common around the cyclosystems, the former on the branches. The coenosteal strips are slightly convex and 0.06–0.085 mm in width; each platelet is highly corrugated (Figure 1E), approximately 6–9 longitudinal ridges occurring on the surface, giving each platelet a rough texture. Nematopores occur on the edge of the cyclosystem lid (Figure 2B), on the female ampullae, on the upper and outer edges of the pseudosepta (Figures 2A, D), and on the sides of the cyclosystems (Figure 1F), but rarely on the branch coenosteum. There is no regularity in placement of the nematopores, less than 10 occurring on the lid and associated ampullae, and usually less than 10 on the pseudosepta and adjacent regions, again not in any fixed order. The nematopores are usually raised on a small (0.05 mm tall and 0.08–0.09 mm in basal diameter) cone, the aperture diameter being about 0.04–0.045 mm. The corallum is uniformly white.
The cyclosystems are unifacially arranged on the corallum and are elliptical to slightly irregular in outline (Figures 1B, D, 2B), the greater diameter ranging from 1.4 to 1.6 mm. Based on 50 cyclosystems, the range of dactylopores per cyclosystem is 12–21, average 17.06 (σ = 1.81), and mode of 17.
The upper gastropore chamber is spherical, about 0.65 mm in diameter, opening to the lower chamber through a gastropore ring constriction of about 0.4 mm in diameter (Figure 2C). The lower chamber is quite compressed (about 0.1 mm deep) and only slightly wider than the upper chamber, about 0.75 mm in diameter (Figure 2C). The cyclo-system lid is tongue-shaped (Figures 1B, D, F, 2B), obliquely oriented, and covers 30%–50% of the cyclosystem; the edges of the lid are turned slightly upward. Rarely a smaller accessory lid is present on the opposite side of the cyclosystem, usually fusing with the larger lid. The dactylotomes are uniformly 0.08–0.09 mm in width, separated by pseudosepta 0.08–0.15 mm in basal width (Figure 2D). The upper surface of the pseudo-septa is slightly concave and quite porous; pseudosepta are of equal length (Figure 2D).
The female ampullae occur in the cyclo-system lid, 1–3 occurring per cyclosystem (Figures 1B, D, F, 2A), usually in a linear [End Page 78]
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order [female arrangement A sensu Cairns (2015:Table 9)]. They form prominent hemispherical mounds 0.55–0.65 mm in diameter. Their efferent pores occur beneath the lid and are about 0.11 mm in diameter (Figure 1F). Male ampullae are unknown.
Among the 47 species of Crypthelia (Cairns 2016), 33 lack a commensal relationship with polynoid polychaetes and the attendant calcareous tubes they form to modify the coral’s corallum. Of these 33 species, 17 occur in the Indo-West Pacific region. Of these only three have their female ampullae restricted to the cyclosystem lid [female arrangement A sensu Cairns (2015:Table 9)]: C. kelleyi, n. sp.; C. clausa Broch, 1947; and C. pudica Milne Edwards & Haime, 1849. Crypthelia kelleyi is easily distinguished from C. clausa (Maldive Islands, 609–915 m) by its much smaller cyclosystems, lower number of dactylopores per cyclosystem, and presence of nematopores. It is, however, similar to C. pudica, the type species of the genus, which is widely distributed from the Philippines, western Australia, and Japan at 368–1,633 m. Crypthelia kelleyi differs largely in degree, having smaller female ampullae, smaller inclined lids, and slightly larger cyclosystems. Crypthelia kelleyi also tends to have a reticulate branching pattern with branch anastomosis, [End Page 80] whereas that of C. pudica is open branched. Crypthelia pudica was most recently re-described and illustrated by Cairns (1983).
Known only from the type locality.
Named in honor of Christopher Kelley, deep-sea biologist specializing in Hawaiian fauna.
I am grateful for the opportunity to examine corals collected by the Okeanos Explorer expedition to the Northwestern Hawaiian Islands in 2015, and particularly to Chris Kelley, who made this specimen available. I thank Robert Ford for constructing the Photoshop figures.
1. Manuscript accepted 9 June 2016.