Chrispaulia wrightorum, Gale & Jagt, 2021
publication ID |
https://doi.org/10.5852/ejt.2021.755.1405 |
publication LSID |
lsid:zoobank.org:pub:F9105E33-3E8B-4B3C-88B3-0316207B70F6 |
DOI |
https://doi.org/10.5281/zenodo.5036886 |
persistent identifier |
https://treatment.plazi.org/id/DC13434F-62E3-47A9-9F62-327F77141670 |
taxon LSID |
lsid:zoobank.org:act:DC13434F-62E3-47A9-9F62-327F77141670 |
treatment provided by |
Felipe (2021-06-25 17:52:39, last updated 2024-11-24 22:51:15) |
scientific name |
Chrispaulia wrightorum |
status |
sp. nov. |
Chrispaulia wrightorum sp. nov.
urn:lsid:zoobank.org:act:DC13434F-62E3-47A9-9F62-327F77141670
Fig. 13F–G View Fig
? Benthopecten sp. – Spencer & Wright in Moore 1966: U48.
Diagnosis
Chrispaulia with smooth marginal ossicles, in which the distal superomarginals possess a single large spine pit close to their distal, abactinolateral border.
Etymology
After the late brothers C.W. and E.V. Wright, who collected the specimen.
Material examined
The arm fragment ( NHMUK PI EE 17997 ) from the Albian Red Chalk (Hunstanton Formation) at Speeton, Yorkshire (United Kingdom) is the holotype and single specimen known to date. The specimen was originally articulated; it was subsequently reconstructed on plasticene by the Wright brothers.
Description
Arm elongated, narrow; supero- and inferomarginals opposed, shortening rapidly distally ( Fig. 13F–G View Fig ). Superomarginals bearing single, distally directed, crater-like spine base on distal, abactinolateral margin. Supero- and inferomarginals smooth, grooves for cribriform organs between infero-/superomarginal pairs poorly defined.
Remarks
Chrispaulia wrightorum sp. nov. differs from all congeners in the smooth marginal ossicles, lacking rugosities.
Fig. 7 (next page). A–J. Jurapecten infrajurensis sp. nov., various ossicle types (paratypes). A, H. Ambulacrals, in lateral and actinal aspects, respectively (SNSB-BGSP2020XLV 21,SNSB- BGSP2020XLV 28). B, E–F. Adambulacrals, in actinal and abactinal views (SNSB-BGSP2020XLV 22, SNSB-BGSP2020XLV 25–26). C, G, J. Superomarginals, in lateral views (SNSB-BGSP2020XLV 23, SNSB-BGSP2020XLV 27, SNSB-BGSP2020XLV 30). D, I. Inferomarginals, in lateral views (SNSB-BGSP2020XLV 24, SNSB-BGSP2020XLV 29). — K–Y. Jurapecten hessi Gale, 2011. K, P, U. Adambulacral ossicles. K. Abactinal view (NHMUK PI EE 17996). P. NHMUK EE 13598 (the original of Gale 2011a: pl. 19 fig. 11). U. NHMUK EE 13599, the original of Gale (2011a: pl. 20 fig. 12). L. Circumoral ossicle (NHMUK EE 13605, the original of Gale 2011a: pl. 20 fig. 13). M–N. Ambulacral ossicles, in actinal and abactinal views, respectively (NHMUK EE 13595–13596, the originals of Gale 2011a: pl. 19 figs 8–9). O. Ambulacral, in proximal/distal view (NHMUK 13597). Q–S. Superomarginal ossicles (NHMUK EE 13601–13602; the originals of Gale 2011a: pl. 20 figs 6–7). T, V–W. Inferomarginals (NHMUK EE 13600, EE 13603–13604, EE 13608, the originals of Gale 2011a: pl. 20 figs 5, 8, 16). X–Y. Oral ossicles (NHMUK EE 13606– 13607, the originals of Gale 2011a: pl. 20 figs 10, 14). Provenance: A–J. Upper Toarcian–lower Aalenian (possibly aalensis ammonite Zone), Quedlinburg (Landkreis Harz, northern Germany; see Hess 2014). K–Y. Upper Oxfordian (Couches d’Effingen, bifurcatus ammonite Zone, stenocycloides ammonite Subzone), Savigna, near Orgelet, Département du Jura, France (Gale 2011b). Abbreviations: d = distal; p = proximal. See Fig. 3 for detailed morphological terminology. Scale bars: A–J = 0.2 mm; K–Y = 0.5 mm.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Neoasteroidea |
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