Piersaloceras (?) sp., Teichert, 1930

Kröger, Björn, 2025, The Lyckholm acme of cephalopods - Review of the late Katian (Vormsi-Pirgu regional stages) Ordovician cephalopods of Estonia, European Journal of Taxonomy 978, pp. 1-169 : 76-77

publication ID

https://doi.org/10.5852/ejt.2025.978.2801

publication LSID

lsid:zoobank.org:pub:422E6F06-B4C8-4840-854C-811145D88B32

DOI

https://doi.org/10.5281/zenodo.15150609

persistent identifier

https://treatment.plazi.org/id/93268783-963D-706A-FD50-FCF1FB82FC68

treatment provided by

Plazi

scientific name

Piersaloceras (?) sp.
status

 

Piersaloceras (?) sp.

Figs 30C View Fig , 31A View Fig

Material examined

ESTONIA • Sutlema old quarry; Kõrgessaare Formation , Vormsi Regional Stage; TUG 1827-163 .

Description

The specimen is a fragment of a curved body chamber, preserved in its total length but lateral parts of the body chamber are missing ( Fig. 30C View Fig ). The outer shell is well-preserved, it is ornamented with narrowly spaced (ca 15–20 per 10 mm) imbricated frills ( Fig. 31A View Fig ), which are directly transverse, and parallel to the peristome. No hyponomic sinus occurs. In lateral view, both margins are curved. The curvature of the concave margin is wider than that of the convex margin, which results in a gibbous outline of the body chamber. The greatest conch height of 50 mm is located at ca mid-length of the body chamber. At its base, the height is 48 mm and at the aperture 43 mm. The suture, reconstructed from the base of the body chamber, forms a narrow lateral lobe. No traces of the siphuncle and of the septal foramen are preserved.

Remarks

The characteristically frilled ornamentation of this fragment is most similar to that of P. gageli Teichert, 1930 , which, in turn, is known only from a single, immature specimen. It differs from the type specimen (and, to date, only known specimen of this genus) in lacking the longitudinal furrows on the impression of the mold, which could be an effect of the typical oncoceratid longitudinal ridges, and which is present in more apical conch parts of many oncocerids (see discussion in Frye 1987: 92). Because details of the siphuncle and parts of the phragmocone are unknown from the specimen described above, a definite determination is not possible. The general shape of the body chamber is similar to that of Redpathoceras saxbyense sp. nov., and to Uranoceratidae , such as Deckeroceras Foerste, 1935b . The mature body chamber of the former is however longer (68 mm) and at its base less high (45 mm). More complete, better-preserved material is needed to evaluate the relationship of this specimen to Redpathoceras , or whether Piersaloceras might belong to the Uranoceratidae or Probillingsitidae Flower, 1941 .

Notably, some oncoceratids, such as Beloitoceras or Neumatoceras also have similarly shaped body chambers, but are more strongly compressed and have a hyponomic sinus. This could link oncoceratids and uranoceratids, as suggested by the phylogeny in Pohle et al. (2022).

Kingdom

Animalia

Phylum

Mollusca

Class

Cephalopoda

SubClass

Multiceratoidea

Family

Graciloceratidae

Genus

Piersaloceras

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