Smittoidea cancellata, Hayward & Winston, 2011
publication ID |
https://doi.org/ 10.1080/00222933.2011.574922 |
persistent identifier |
https://treatment.plazi.org/id/03F93214-964B-D208-FE47-FBC89245FDBE |
treatment provided by |
Felipe |
scientific name |
Smittoidea cancellata |
status |
sp. nov. |
Smittoidea cancellata sp. nov.
( Figure 23 View Figure 23 )
Material
Holotype. NMNH 1154053 View Materials : Eltanin cruise 9, station 740, 56 ◦ 06’ to 56 ◦ 07’ S, 66 ◦ 19’ to 66 ◦ 30’ W, 494– 384 m, 18 September 1963; one fragment. GoogleMaps
Paratypes. VMNH 01367.200 View Materials : same data as holotype; seven fragments GoogleMaps .
Description
Colony architecture unknown; type material consists of flat or curled, unilaminar flakes, with no evidence of substratum, basal walls of autozooids clean. Autozooids hexagonal, flat; frontal shield flat, or just convex medially, with thin, dimpled calcification, bordered by projecting vertical walls, and large, closely spaced marginal pores. Primary orifice wider than long, proximal edge with broad, straight-edged lyrula, occupying two-thirds of total width; condyles conspicuous, sharply pointed, down-curved. No oral spines. Peristome thin, low, with medio-proximal notch, above a small, oval suboral avicularium, with semi-elliptical mandible, parallel to frontal plane, directed proximally, crossbar slender with thin median columella. Sporadically, the avicularium is dimorphic, with scaphoid rostrum, ca 0.4 mm long, proximally directed. Ovicell recumbent on frontal shield of distally succeeding autozooid, hemispherical, ectooecium with large, uncalcified frontal area, the exposed entooecium pierced by numerous, irregularly shaped pores.
Measurements
For all measurements n = 20, mean ± SD: autozooid length 1.24 ± 0.11 mm; autozooid width 0.18 ± 0.01 mm; orifice width 0.25 ± 0.01.
Etymology
Latin, cancellatus: latticed, with reference to the dimpled calcification. Remarks
Species of Smittoidea have been described from shelf-sea environments worldwide, including Antarctica and the subantarctic southwest Atlantic. In its distinctive frontal calcification and small, oval, suboral avicularium S. cancellata sp. nov. is most similar to S. malleata Hayward and Thorpe, 1989 , reported from the South Shetland Islands, Graham Land and the Ross Sea, and S. albula Hayward and Taylor, 1984 , known only from the Ross Sea. However, both of these species have elongate oval ovicells, much larger than that of S. cancellata and more densely perforated. Smittoidea malleata is further distinguished in lacking a peristome, and in its lyrula, which is simply a short projection from the distal edge of the avicularium. The lyrula of S. albula is a conspicuous square structure, and a thin, raised peristome extends along the lateral borders of the orifice, and proximally incorporates the avicularium. In both of the described species the condyles are thick and angular, quite unlike the slender, pointed condyles of S. cancellata .
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