Ebiscothyris bellonensis, Bitner & Cohen, 2015, Bitner & Cohen, 2015

Bitner, Maria Aleksandra & Cohen, Bernard L., 2015, Congruence and conflict: case studies of morphotaxonomy versus rDNA gene tree phylogeny among articulate brachiopods (Brachiopoda: Rhynchonelliformea), with description of a new genus, Zoological Journal of the Linnean Society 173 (2), pp. 486-504 : 494-495

publication ID

https://doi.org/ 10.1111/zoj.12217

DOI

https://doi.org/10.5281/zenodo.10543024

persistent identifier

https://treatment.plazi.org/id/03F5D923-FFBD-1A77-097C-FF76FEF07C06

treatment provided by

Felipe

scientific name

Ebiscothyris bellonensis
status

gen. et sp. nov.

EBISCOTHYRIS BELLONENSIS View in CoL GEN. ET SP. NOV.

( FIGS 7A–I View Figure 7 , 8A–F View Figure 8 , 9A–D View Figure 9 )

Diagnosis

As for the genus.

Etymology

Referring to the Bellona Plateau, where part of the material was collected.

Holotype

The specimen illustrated in Figure 7E–H View Figure 7 , IB-2013-1, was collected at station CP 2616 on the Chesterfield Plateau.

Paratypes

The specimens illustrated in Figures 7A–D, I View Figure 7 and 8A– F View Figure 8 , IB-2013-2 to IB-2013-6, were collected at stations CP 2557 and CP 2616.

Type locality

Cruise EBISCO, station CP 2616, Coral Sea, Chesterfield Plateau, 19°35.08′S, 158°49.83′E, 786–836 m depth.

Material examined

Coral Sea , cruise EBISCO, western Bellona Plateau: station DW 2544, 21°09.91′S, 158°38.15′E, 650– 723 m depth, five specimens GoogleMaps ; station CP 2545, 21°10.04′S, 158°37.40′E, 765–778 m depth, three specimens; station CP 2556, 21°05.29′S, 158°33.72′E, 741– 791 m depth, nine specimens; station CP 2557, 21°06.05′S, 158°31.66′E, 800–923 m depth, three specimens. Chesterfield Plateau : station CP 2616, 19°35.08′S, 158°49.83′E, 786–836 m depth, 28 specimens GoogleMaps .

Depth range

650–923 m.

Measurements (station, length, width, and thickness, all in mm)

CP 2616 (holotype), 13.1, 12.0, 8.1; CP 2616 (paratype), 13.1, 12.3, 7.1. Measurements of all currently available specimens of E. bellonensis gen. et sp. nov. are given in Appendix S7.

Description

Shell of medium size, white, thin to translucent anteriorly, elongate oval to subpentagonal in outline, with maximum width at about mid valve. Shell surface smooth, with weakly defined growth lines; lateral and anterior valve margins slightly incurved, thickened ( Fig. 7C, D, G, H View Figure 7 ). Shell biconvex, ventral valve more convex. Lateral commissures dorsally curved, anteri- or commissure strongly and broadly unisulcate. Beak short, suberect to erect. Foramen of medium size, circular, permesothyrid. Deltidial plates conjunct, forming a well-exposed symphytium with only a weak median line of junction in some specimens (cf. Fig. 8A View Figure 8 ). Pedicle variable, may be as much as ten times as long as the shell ( Fig. 7I View Figure 7 ). The long pedicle differentiates E. bellonensis gen. et sp. nov. from Abyssothyris and other terebratulids. Ventral valve interior with welldeveloped tubular, excavate pedicle collar ( Fig. 8F View Figure 8 ). Teeth small, short ( Fig. 8A View Figure 8 ). Dorsal valve interior with long and medially inclined inner socket ridges that bound wide sockets; fulcral plates well developed. Cardinal process prominent, semi-elliptical ( Fig. 8D, F View Figure 8 ). Outer hinge plates narrow, triangular; crural bases ill defined. Loop short, occupying about 25% of dorsal valve length, with blunt, short, crural processes directed ventrally ( Fig. 8B–E View Figure 8 ). Descending branches subparallel, very wide; transverse band broad, medially folded. Muscle scars strongly impressed on both valves, elongate oval in outline.

Ultrastructural analysis shows three shell layers ( Fig. 9A–D View Figure 9 ). The microgranular primary layer is 5.2– 7.8 μm thick, the secondary layer is very thin (3.2– 5.6 μm), and its fibres are wide, implying that mantle epithelial cells are large, and/or that the angle between the fibres and the primary layer is small. In transverse section, the secondary layer shows only two overlapping layers of fibres ( Fig. 9B View Figure 9 ), a feature that has only been reported before in the dyscoliid Xenobrochus norfolkensis Bitner, 2011 ( Bitner, 2011: fig. 4E, F); however, the incurved, thickened valve margins are built of several, densely arranged sheets of secondary fibres (see Fig. 9C View Figure 9 ). The tertiary layer of E. bellonensis gen. et sp. nov. is thick (85–152 μm), with its internal surface showing clear traces of large, irregularly interlocking prisms ( Fig. 9C, D View Figure 9 ). The total shell thickness is 96–160 μm. In Kanakythyris ( Fig. 9E, F View Figure 9 ) the shell is also composed of three layers; however, the secondary layer is much thicker, and the prisms are more irregular on the internal surface, and display delicate ornamentation ( Fig. 9F View Figure 9 ), whereas in E. bellonensis gen. et sp. nov. they are smooth (see Fig. 9D View Figure 9 ).

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