Stipilepas molerensis Carriol, 2016
publication ID |
https://doi.org/ 10.5252/g2016n1a2 |
publication LSID |
urn:lsid:zoobank.org:pub:1102C358-61B2-4CF1-8F06-5B241DC04175 |
persistent identifier |
https://treatment.plazi.org/id/5E4A81D5-2A96-43FE-98D0-CC2747273BF9 |
taxon LSID |
lsid:zoobank.org:act:5E4A81D5-2A96-43FE-98D0-CC2747273BF9 |
treatment provided by |
Felipe |
scientific name |
Stipilepas molerensis Carriol |
status |
sp. nov. |
Stipilepas molerensis Carriol , n. sp.
( Figs 1 View FIG B-D, 2, 3; Table 1)
DIAGNOSIS. — As for genus.
ETYMOLOGY. — After the Mo Clay Formation, ‘moler’ in Danish.
TYPE LOCALITY AND HORIZON. — Mors , northwest Jutland, Denmark ; Mo Clay Formation.
ENVIRONMENTAL SETTING. — Recent species of the Neolepadinae are restricted to hydrothermal vents and seeps in the Pacific and Indian oceans, occurring bathyal and upper abyssal waters. In contrast, Stipilepas molerensis Carriol n. gen., n. sp. occurred in an ‘ordinary’ North Sea habitat, on logs.
TYPE MATERIAL. — The holotype is MGUH 30522 View Materials ( Fig. 2C View FIG ) ; paratypes are MGUH 30523 View Materials ( Fig. 2D View FIG ), MGUH 30524 View Materials ( Fig. 2A View FIG ), MGUH 30525 View Materials ( Fig. 2B View FIG ), MGUH 30526 View Materials ( Figs 1B View FIG [26], 3A), MGUH 30527 View Materials ( Figs 1B View FIG [27], 3B), MGUH 30528 View Materials ( Figs 1B View FIG [28], 3E), MGUH 30529 View Materials ( Figs 1D View FIG [29], 3D), MGUH 30530 View Materials ( Figs 1C View FIG [30], 3F), MGUH 30531 View Materials ( Fig. 1C View FIG [31]), MGUH 30532 View Materials ( Fig. 1C View FIG [32]) and MGUH 30533 View Materials ( Fig. 3C View FIG ) .
DESCRIPTION
Tergum ( Fig.3F View FIG ) wide, subquadrangular.Apico-basal ridge thin, very low, situated less than half the valve width from the carinal margin.Occludent margin straight.Scutal margin sinuous. Upper carinal margin longer than the others, straight.Lower carinal margin convex to straight.Valve rounded and protuberant along occludent margin, this rounded margin is followed by a depression extending from the apex to about the middle of the scutal margin, a faint secondary ridge, extending from tergal apex to scutal margin,marking the limit of the depression.Outer surface ornamented with major and minor, thin transverse growth ridges and thin longitudinal ridges radiating from the apex.
Median latus ( Figs 2C View FIG , 3A View FIG ) short, an isosceles triangle, wider than high, with convex scutal and tergal margins, overlapping scutum and tergum. Outer surface ornamented with major and minor, thin transverse growth ridges.
Scutum ( Figs 1C View FIG ; 3A, D View FIG ) subrhomboidal in outline and, similar to tergum, ornamented with major and minor, thin transverse growth ridges and some thin longitudinal ridges radiating from the apex. The scutum is bent along a line extending from the apex to the baso-lateral angle and, less strongly, along a second line extending from the apex to a point of the basal margin distant, from the rostral angle, of two-thirds the length of this margin. In the part included between these two lines the growth ridges are curved downwards. There is no distinct ridge associated with the change in direction of the growth ridges along the apico-basal axis. Occludent, tergal and lateral margins convex to straight, basal margin sinuous.
Carina ( Fig. 3E View FIG ) and rostrum have the same shape and are difficult to tell apart when found isolated. Carina (or rostrum) strongly convex transversely, widening from the apex to the basal margin, not carinate, ornamented externally with major and minor growth lines.
Peduncle with scales ( Figs 2B, C View FIG , 3C View FIG ), wider than high, externally marked by thin growth lines, with apex rounded. These scales are difficult to count; nevertheless, it is possible to consider their number of tiers by whorl about six. Peduncle length equal to or shorter than that of capitulum.
REMARKS
Stipilepas molerensis Carriol n. gen., n. sp. is the first extinct taxon that is attributable to the Ashinkailepadini and, in addition to? Neolepas augurata Buckeridge & Grant-Mackie, 1985 from the Lower Jurassic of New Caledonia, the second known fossil taxon that is referable to the Neolepadinae .
Superorder SESSILIA Lamarck, 1818 Suborder BRACHYLEPADOMORPHA Withers, 1923 Family BRACHYLEPADIDAE Woodward, 1901
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