Witchellia companyi, Sandoval, 2022
publication ID |
https://doi.org/ 10.5252/geodiversitas2022v44a27 |
publication LSID |
urn:lsid:zoobank.org:pub:E4896081-9312-4EA6-AE33-AAC44201748E |
DOI |
https://doi.org/10.5281/zenodo.7149036 |
persistent identifier |
https://treatment.plazi.org/id/A30DAB70-2DED-4484-8755-90D94C4825A5 |
taxon LSID |
lsid:zoobank.org:act:A30DAB70-2DED-4484-8755-90D94C4825A5 |
treatment provided by |
Admin |
scientific name |
Witchellia companyi |
status |
sp. nov. |
Witchellia companyi n. sp. [M]
( Figs 8 View FIG D-E; 11C; 13D-F)
urn:lsid:zoobank.org:act:A30DAB70-2DED-4484-8755-90D94C4825A5
DIAGNOSIS. — Macroconch planulate and evolute with wide and shallow umbilicus, rectangular compressed section, fine keel, ribbing varying throughout ontogeny with the BC end becoming smooth or finely striate, very simple septal suture.
TYPE MATERIAL. — Holotype: Specimen JAC11.8.16 (HT), Department of Stratigraphy and Palaeontology, Faculty of Sciences, University of Granada ( Spain) . — Paratypes: specimens JAC11.8.14 , JAC11.8.15 , JAC11.8.17 , JAC11.8.18 , and JAC11.8.19 ( PT).
TYPE LOCALITY AND OCCURRENCE. — Sierra Alta Coloma (JAC11 section, Jaén Province, central sector of the Median Subbetic, Betic Cordillera , Spain), Lower Bajocian (Propinquans Zone, Patella Subzone ).
DERIVATION OF NAME. — In honour of my colleague Miguel Company, professor of Palaeontology at the University of Granada, Spain.
MATERIAL EXAMINED. — JAC11.8.14 , JAC11.8.15 , JAC11.8.16 , JAC11.8.17 , JAC11.8.18 , JAC11.8.19 , JAC11.8.23 , JAC11.8.31 , JAC22.54.6 and JAC22.54.7 .
MEASUREMENTS. — See Table 19.
DESCRIPTION
Medium-sized planulate macroconchs, evolute (U/D varying between 0.39 and 0.42 in complete adult specimens) with moderate whorl expansion and a relatively wide and shallow umbilicus. The whorl section ( Fig. 11C View FIG ) is almost rectangular, with flat and inclined (at times almost vertical) umbilical wall, a rounded umbilical edge, flattened flanks, and a narrow, tabulated ventral region, with a thin and relatively high keel lacking lateral grooves. It has a simple opening with little ventral expansion. The ornamentation is reminiscent of that of W. romanoides . The innermost whorls are not detectable in any of the available specimens and have no tuberculate stage. The inner and intermediate whorls present weak flexuous, subradial ribs, strongly projecting forward in the ventral region, which during ontogenetic development are usually successively simple, divided, fasciculate, grouped at the umbilical border, and again simple. The outer whorls may become almost smooth, with flexuous growth striae arranged in bundles. The septal suture ( Fig. 8 View FIG D-E) is relatively simple; E is as deep as L, the saddle E-L is wide and strongly asymmetrical, L is tripartite, L-U 2 is narrow and high, and the umbilical lobes are slightly retracted.
REMARKS
The most similar species are W. romanoides ( Douvillé, 1885) and W. pseudoromanoides Dietze, Chandler & Schweigert 2003 , but both are more involute and the former is also usually less ornamented whereas the latter is more strongly ribbed and has a broader whorl expansion. W. companyi n. sp. could possibly be a direct descendant of latest W. romanoides .
DISTRIBUTION
Lower Bajocian, Laeviuscula Zone (Laeviuscula Subzone)– Propinquans Zone (Patella Subzone). The species has been recorded only in the Sierra de Alta Coloma area ( Granada and Jaén Provinces).
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.
Kingdom |
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Phylum |
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Class |
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Order |
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SubOrder |
Ammonitina |
SuperFamily |
Hildoceratoidea |
Family |
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SubFamily |
Soninniinae |
Genus |