Published August 31, 2017 | Version v1
Taxonomic treatment Open

Bathycyclopora vibraculata Berning & Harmelin & Bader & Cibio 2017, gen. et comb. nov.

  • 1. Oberösterreichisches Landesmuseum, Geowissenschaftliche Sammlungen, 4060 Leonding, Austria. & CIBIO, Centro de Investigação em Biodiversidade e Recursos Genéticos, InBIO Laboratório Associado, Pólo dos Açores, 9501 - 801 Ponta Delgada, Açores, Portugal. & urn: lsid: zoobank. org: author: 30 D 7 D 0 DB-F 379 - 4006 - B 727 - E 75 A 0720 BD 93 & Corresponding author: b. berning @ landesmuseum. at
  • 2. Aix-Marseille University, Mediterranean Institute of Oceanography, OSU Pytheas, Station Marine d'Endoume, 13007 Marseille, France. & Email: jean-georges. harmelin @ univ-amu. fr & urn: lsid: zoobank. org: author: D 11 AE 07 A-CFD 9 - 41 EE-B 3 F 9 - 6 E 0472150300
  • 3. Institut für Geowissenschaften, Christian-Albrechts-Universität, 24118 Kiel, Germany. & Email: bbader @ online. no & urn: lsid: zoobank. org: author: AA 3 BCFDC- 524 D- 4648 - 9268 - F 0 F 1 C 94 B 9 A 68

Description

Bathycyclopora vibraculata (Calvet, 1931) gen. et comb. nov.

Fig. 11 A–F, Table 11

? Phylactella vibraculata Calvet, 1931: 113, pl. 2, figs 17–18.

Material examined

Lectotype (here designated)

AZORES: 2 ovicellate colonies on a coral fragment, the larger one with an ancestrula is the lectotype (MOM INV-22480 a), the smaller one a paralectotype (MOM INV-22480 b), dry, Stn 2.

Paralectotypes

AZORES: 1 colony on coral fragment, dry, Stn 2 (MOM INV- 22679); 1 colony on coral fragment, dry, Stn 2 (MOM INV- 22680); 1 colony fragment, dry, on slide, severely affected by Bynesian decay, Stn 2 (MOM INV- 22479).

Description

Colony encrusting, unilaminar, multiserial, forming small patches (Fig. 11A). Zooids relatively large, hexagonal or polygonal, separated by grooves (Fig. 11 B–C); lateral walls well developed, becoming more extensive distally, gently sloping, with a single basal pore chamber connecting each neighbouring zooid (Fig. 11C), round septular pore surrounded by a large area of cryptocyst with a surface similar to that of frontal shield, framed by a narrow and slightly raised ridge of gymnocystal calcification, separated from neighbouring pore chamber by a suture, pore in distal pore chamber slightly raised with respect to lateral ones. Frontal shield convex, imperforate except for a single row of numerous conspicuous marginal pores, gently rising distally towards a suboral crest with a blunt or occasionally triangular central umbo that is laterally sloping towards proximal pair of spines (Fig. 11D); surface rugose and with irregular wrinkles, superimposed by fine granules.

Orifice about as wide as long, distal half rounded and with a conspicuous immersed shelf along entire distal margin, lateral margins parallel, proximal edge slightly concave; condyles conspicuous, rectangular or roughly triangular, distinctly set off from orifice margins (Fig. 11F); distolateral orifice margin with seven or rarely six evenly spaced spines, six spines with a distinct distal gap in potentially maternal zooids.

Ovicell hyperstomial, ooecium resting on or slightly immersed in distal zooid’s frontal shield (Fig. 11D), globular, in general wider than long, with a very short tubular peristome wedged in between distalmost pair of spines and terminating at distal orifice margin; smooth ectooecium a narrow band around base of ooecium, broadening proximally to frame ooecial aperture (Fig. 11E); exposed endooecium imperforate, surface topography similar to that of frontal shield; ooecial aperture suborbicular, not closed by operculum.

Adventitious avicularia paired, small, oval, lateral to orifice near distolateral zooidal corners (Fig. 11 D– E); rostrum short, semicircular to semielliptical, slightly raised distally, directing laterally or distolaterally, palate an immersed distolateral shelf framing a suborbicular opesia; crossbar incomplete, composed of two short inwardly curved triangular condyles, proximal uncalcified area reduced, semicircular. Interzooidal avicularia frequent in late astogenetic parts of colony, emplaced on a polygonal cystid with variably developed cryptocyst-type granular frontal shield and a row of marginal pores as in autozooids (Fig. 11 C–D); rostrum slightly to distinctly spatulate, slightly raised distally, of variable size and pointing in various directions, most of palate occupied by a broad flat shelf with a V-shaped proximal edge caused by indentation of distal uncalcified area; crossbar broad laterally and much thinner towards centre when complete, or reduced to a pair of short triangular condyles; proximal uncalcified area reduced, semicircular.

Ancestrula tatiform, oval (ca 500 µm long, 350 µm wide), smooth gymnocyst presumably narrow all around, cryptocyst absent; opesia large (ca 380 µm long, 260 µm wide), oval, slightly constricted in distal fifth; 11 spines, with five proximal ones widely spaced and six distal ones situated closer together (Fig. 11B).

Remarks

As Calvet (1931) did not explicitly mention a holotype, we here designate as lectotype the specimen that was presumably depicted on pl. 2, figs 17–18. The species epithet stems from a misinterpretation of the small adventitious avicularia, which Calvet (1931: 114) thought were vibracula. The mandible is, however, confined to the rostrum, moves in one plane only, and is therefore a normal avicularium (Fig. 11E). Bathycyclopora vibraculata gen. et comb. nov. has never been reported again after its discovery.

Ecology

All available colonies encrust dead coral skeletons at ca 600 m depth, forming small patches.

Distribution

Bathycyclopora vibraculata gen. et comb. nov. was found at a single station off NW Terceira Island (Azores).

Notes

Published as part of Berning, Björn, Harmelin, Jean-Georges & Bader, Beate, 2017, New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism, pp. 1-51 in European Journal of Taxonomy 347 on pages 32-34, DOI: 10.5852/ejt.2017.347, http://zenodo.org/record/3832630

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Additional details

References

  • Calvet L. 1931. Bryozoaires provenant des campagnes scientifiques du Prince Albert 1 er de Monaco. Resultats des Campagnes Scientifiques du Prince Albert 1 er de Monaco 83: 1 - 152.