Dowlingoceras kallholnense Frye, 1987
publication ID |
https://doi.org/10.5852/ejt.2025.978.2801 |
publication LSID |
lsid:zoobank.org:pub:422E6F06-B4C8-4840-854C-811145D88B32 |
persistent identifier |
https://treatment.plazi.org/id/93268783-9633-7060-FDDB-F991FD57FB6B |
treatment provided by |
Plazi (2025-03-07 10:46:31, last updated by GgImagineBatch 2025-03-07 11:20:26) |
scientific name |
Dowlingoceras kallholnense Frye, 1987 |
status |
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Dowlingoceras kallholnense Frye, 1987 View in CoL
Figs 16E, 27A
Dowlingoceras kallholnense Frye, 1987: 95–96 View in CoL , figs 6a–b, 7.
Dowlingoceras kallholnense View in CoL – Kröger 2013: tab.2.
Diagnosis
Dowlingoceras with a slightly compressed cross section (CHI = 1.1); oval cross section, venter narrower than dorsum; mature body chamber is more gibbous than those of the other species of the genus, ca 40 mm high at its base, and with marked constriction near the peristome. (Compiled from Frye 1987.)
Material examined
ESTONIA • Vormsi Island, Hosholm shore; Adila Formation, Pirgu Regional Stage; GIT 878-247.
Type locality and horizon
Kallholn, Dalarna, Sweden; Boda Formation, latest Katian.
Description
Specimen GIT 878-247 preserves parts of the mature body chamber and the phragmocone with a conch height and width of 39 mm and 32 mm, respectively (CHI = 1.2) The conch cross section is oval with a narrower curvature on the ventral compared to the dorsal side. The conch height increases from 36– 37 mm at a length of 17 mm (angle of expansion 8°). The body chamber is only partly preserved, had a length of more than 38 mm and decreases in conch height from its base with a convex outline in lateral view toward ca 35 mm in height. The sutures form a wide lateral lobe and are ca 6 mm apart where the conch height is 39 mm (RCL = 0.15). The siphuncular segments are elongated (7 mm long, 4 mm high, SCR = 0.57) fusiform, wider adorally and adnate to the adoral septal surfaces. The septal necks are poorly preserved, apparently cyrtochoanitic.
Remarks
The Swedish types of D. kallholnense have conch dimensions (maximum height of mature body chamber = 40 mm; CHI = 1.1, and a low angle of expansion in the adoral parts of the phragmocone) ( Frye 1987) which are nearly identical to the specimen described herein. The differences in the connecting ring shape (presence of an adnate area in specimen GIT 878-247 are interpreted as taphonomic or the effects of orientation of the cut. (See also Turek & Aubrechtová 2024, and Pohle et al. 2024, on this topic.) The view is oblique to the dorso-ventral body axis, in Frye (1987: fig. 7), it is apparently perpendicular to that axis in specimen GIT 878-247 (Fig. 16E).
Frye M. W. 1987. Upper Ordovocian (Harjuan) oncoceratid nautiloids from Boda Limestone, Siljan District, Sweden. Geologiska Foreningens i Stockholm Forhandlingar 109: 83-99. https://doi.org/10.1080/11035898709454748
Kroger B. 2013. The cephalopods of the Boda Limestone, Late Ordovician, of Dalarna, Sweden. European Journal of Taxonomy 41: 1-110. https://doi.org/10.5852/ejt.2013.41
Pohle A., Jell P. & Klug C. 2024. Plectronoceratids (Cephalopoda) from the latest Cambrian at Black Mountain, Queensland, reveal complex three-dimensional siphuncle morphology, with major taxonomic implications. PeerJ 12: e 17003. https://doi.org/10.7717/peerj.17003
Turek V. & Aubrechtova M. 2024. Micro-CT reveals 3 D endosiphuncular structure in Late Ordovician actinoceratid cephalopod from the Prague Basin (Czech Republic). Bulletin of Geoscience s 99 (3): 1-21. https://doi.org/10.3140/bull.geosci.1901
GIT |
Institute of Geology at Tallinn University of Technology |
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Dowlingoceras kallholnense Frye, 1987
Kröger, Björn 2025 |
Dowlingoceras kallholnense
Frye M. W. 1987: 96 |