Isorthoceras junceum ( Hall, 1847 )

Kröger, Björn, 2013, The cephalopods of the Boda Limestone, Late Ordovician, of Dalarna, Sweden, European Journal of Taxonomy 41, pp. 1-110 : 63-64

publication ID	https://doi.org/ 10.5852/ejt.2013.41
publication LSID	lsid:zoobank.org:pub:A2F1B9ED-870A-466E-B35E-BD5DA782476E
DOI	https://doi.org/10.5281/zenodo.3815139
persistent identifier	https://treatment.plazi.org/id/AD4D9054-CD5A-6A59-F02A-412BFBD2F93D
treatment provided by	Carolina
scientific name	Isorthoceras junceum ( Hall, 1847 )
status

Treatment

Isorthoceras junceum ( Hall, 1847)

Figs 17E View Fig , 23C View Fig

Orthoceras junceum Hall, 1847: 204 , pl. 47; fig. 3a-f.

Geisonoceras junceum – Balashov 1956: 199, pl. 4, fig. 4a-b.

Isorthoceras ? junceum – Kröger et al. 2011: 46, figs 4a, 9h-i (with synonymy).

Diagnosis

Transversally ornamented, straight Isorthoceras with circular cross section and comparatively low angle of expansion of 5°, chamber distance 0.2–0.3 of corresponding cross section; adult size ca. 10–11 mm in cross section; siphuncle subcentral-central with diameter ca. 0.1 of corresponding conch cross section. (Compiled from Hall 1847.)

Type locality and horizon

Watertown, New York, USA; Trenton Formation, early Katian, Late Ordovician.

Material

Two specimens ( PMU 26833, 26834) from Kallholn, Siljan District, Sweden; Boda Limestone, late Katian, Ordovician.

Description

Specimen PMU 26833 is a fragment of a body chamber 40 mm long, with a diameter increasing from 11 to 12.8 mm (angle of expansion 2.6°). At the adoral end of the specimen, the cast possesses a ca. 3 mm wide apertural constriction, which indicates a mature apertural shell thickening. The shell surface is ornamented with ca. ten fine rounded transverse striae per millimetre.

The second specimen is a 44 mm long portion of a phragmocone, with a diameter increasing from 6.2 to 8.8 mm (angle of expansion 3.4°) and a central thin siphuncle ( Figs 17E View Fig , 23C View Fig ).

Remarks

The two specimens are assigned to I. junceum based on the general similarity of the conch dimensions, the low angle of expansion, and the characteristic narrow transverse ornamentation. The adult conch diameter of specimen PMU 26833 is slightly larger than in other specimens of this species, which is interpreted as intraspecific variation.

The species was discussed in detail by Kröger et al. (2011). Herein the question mark that was positioned after the genus name by Kröger et al. (2011) is omitted, because a comparison of known species of Isorthoceras clearly indicates that this genus is characterized by the typical conch features that are listed above. The internal characters of the type of this species are still not known, but the external features are so similar to those of other species of the genus, that it justifies assigning O. junceum to Isorthoceras .

Comparison

Isorthoceras romingeri ( Foerste, 1932) is a finely transversely striated Isorthoceras from the Black River Formation of Minnesota, USA, which differs in having a larger adult size (more than 17 mm in cross section) and a narrower chamber spacing (seven chambers occur per distance similar to corresponding cross section).

Stratigraphic and geographic range

Trenton Limestone, early Katian, from New York, USA ( Hall 1847); Rocklandian-Edenian, mid Katian, from north central USA ( Catalani 1987); Martinsburg Shale, late Katian ( Bassler 1919); Utica Shale, late Katian ( Flower 1946); Anderskyi bed, southern Kazakhstan, late Katian ( Balashov 1956); Boda Limestone, late Katian-Glisstjärn Formation, Hirnantian, Siljan District, Sweden.