Tornquistes (Tornquistes) cf. romani (Douvillé, 1912)

Cecca, Fabrizio & Savary, Bérengère, 2007, Palaeontological study of Middle Oxfordian- Early Kimmeridgian (Late Jurassic) ammonites from the Rosso Ammonitico of Monte Inici (north-western Sicily, Italy), Geodiversitas 29 (4), pp. 507-548 : 516-517

publication ID

https://doi.org/ 10.5281/zenodo.4651042

DOI

https://doi.org/10.5281/zenodo.4650763

persistent identifier

https://treatment.plazi.org/id/6A5FC813-3760-BD04-FD4B-FAA0C449FCF1

treatment provided by

Felipe

scientific name

Tornquistes (Tornquistes) cf. romani (Douvillé, 1912)
status

 

Tornquistes (Tornquistes) cf. romani (Douvillé, 1912) ( Fig. 4D View FIG )

MATERIAL EXAMINED. — MI3 9/7.

STRATIGRAPHIC DISTRIBUTION. — Bed 9 of section Castello Inici, which has been assigned to the Middle Oxfordian Plicatilis Zone.

DESCRIPTION

Incomplete specimen corresponding to the body chamber of an individual that reached a diameter of about 60 mm. The shell is globular and rather involute. The whorl section is ovate, with convex flanks converging towards the narrow venter. The umbilical edge is rounded and no umbilical wall is visible. Bundles of two strong, radiate ribs spring from radial umbilical bullae. Single ribs are intercalated between the bundles.

DISCUSSION

The poor preservation of our specimen prevents its precise identification. The morphologically closer species is Tornquistes (T.) romani . It is impossible to state if the specimen studied corresponds to an adult or to an immature individual but its rib density and, apparently, its umbilical width can be compared to immature specimens of similar diameter described by Thierry & Charpy (1982). The preservation does not allow observing whether the umbilical wall is really not developed or if it is simply not observable. Tornquistes (T.) multicostatum Thierry & Charpy, 1982 and T. (T.) helvetiae (Tornquist, 1896) have more evolute shells.

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