Published March 25, 2026 | Version v1

Caneycycloceras Niko & Mapes 2011

  • 1. Museum für Naturkunde, Leibniz-Institut für Evolutions-und Biodiversitätsforschung, Invalidenstrasse 43, 10115 Berlin, Germany.
  • 2. Institute of Geology, Czech Academy of Sciences, Rozvojová 269, Prague, 16500, Czech Republic. & University of Tartu, Faculty of Science and Technology, Institute of Ecology and Earth Sciences, Department of Geology, Ravila 14 a, 50411 Tartu, Estonia.

Description

Genus Caneycycloceras Niko & Mapes, 2011

Type species

Caneycycloceras girtyi Niko & Mapes, 2011.

Diagnosis

Genus of the family Brachycycloceratidae with an exogastric, rapidly expanding, weakly cyrtoconic juvenile conch and a strongly inflated adult conch. Juvenile conch with circular conch profile. Juvenile conch strongly annulate, shell surface with fine growth lines; adult conch weakly non-annulate. Siphuncle nearly central, septal necks questionably suborthochoanitic.

Species included

Arkansas (Niko & Mapes 2011): Caneycycloceras girtyi Niko & Mapes, 2011.

Rhenish Mountains (this paper): Caneycycloceras rotersorum sp. nov.; Caneycycloceras fuerstenbergorum sp. nov.

Remarks

Niko & Mapes (2011: 293) gave a diagnosis to separate their new genus from Brachycycloceras: “Shell characterized by more rapid expansion (28° to 30° in angle) and slightly stronger endogastric curvature (radius of curvature = ca 8 cm) of immature shell than Brachycycloceras that is assigned to the same family; siphuncle supracentral with a nearly central position; mature shell indicates slightly contracting tendency to aperture; periodic transverse constrictions are developed in adoral part of mature shell.” They also stated that the position of the siphuncle is the most distinctive feature: “In the new genus, the siphuncle is located near the conch axis with position ratios (distance of central axis of septal foramen from internal shell wall of venter to corresponding dorsoventral internal shell diameter) approximately 0.53, whereas the siphuncle position of Brachycycloceras is near midway between the conch axis and the dorsal margin, whose ratios of the siphuncular position are approximately 0.7–0.8.” Besides this, the expansion angle is larger in Caneycycloceras (28°–30°) than in Brachycycloceras (13°–15°).

Two additional new species are assigned here to Caneycycloceras. Unfortunately, both are known only from their juvenile conchs, so it remains uncertain whether they also developed the bulbous adult stage characteristic of the type species. However, the morphology of the annulate portion of the conch supports their placement within the genus Caneycycloceras.

Notes

Published as part of Korn, Dieter & Aubrechtová, Martina, 2026, New annulate Carboniferous orthoconic and cyrtoconic cephalopods of the family Brachycycloceratidae Furnish, Glenister & Hartman, 1962, pp. 1-39 in European Journal of Taxonomy 1048 on pages 23-24, DOI: 10.5852/ejt.2026.1048.3231, http://zenodo.org/record/19335382

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Linked records

Additional details

Biodiversity

Scientific name authorship
Niko & Mapes
Kingdom
Animalia
Phylum
Mollusca
Order
Orthocerida
Family
Brachycycloceratidae
Genus
Caneycycloceras
Taxon rank
genus
Taxonomic concept label
Caneycycloceras Niko, 2011 sec. Korn & Aubrechtová, 2026

References

  • Niko S. & Mapes R. H. 2011. Caneycycloceras, a new brachycycloceratid cephalopod genus from the Early Carboniferous in Oklahoma, Midcontinent North America. Paleontological Research 15: 292-295. https://doi.org/10.2517/1342-8144-15.4.292