Campanile selandicum ( Lundgren, 1867 )

Hansen, Thomas, 2019, Gastropods from the Cretaceous-Palaeogene boundary in Denmark, Zootaxa 4654 (1), pp. 1-196 : 86-87

publication ID

https://doi.org/ 10.11646/zootaxa.4654.1.1

publication LSID

lsid:zoobank.org:pub:CFD82CC0-3110-472E-972B-7ADC0C523A04

persistent identifier

https://treatment.plazi.org/id/BF18F633-A955-FFB3-2B9C-C58BFDF8FBF0

treatment provided by

Plazi

scientific name

Campanile selandicum ( Lundgren, 1867 )
status

 

Campanile selandicum ( Lundgren, 1867)

Figs 24 View FIGURE 24 B–D

1867 Cerithium selandicum Lundgren : 17, pl. 1, fig. 2.

1902 Cerithium pseudotelescopium n. sp. —Ravn: 219–220, pl. 1, figs 13–14.

1902 Cerithium selandicum Lundgren—Ravn : 220–221, pl. 1, figs 15–16.

1933 Cerithium ( Campanile ?) pseudotelescopium Ravn—Ravn : 45, pl. 4, fig. 8a–b.

1933 Metacerithium ? selandicum Lundgren—Ravn : 46.

2014 Campanile View in CoL ? pseudotelescopium ( Ravn, 1902) —Lauridsen & Schnetler: 48, fig. 32.

Diagnosis. Columella with single strong fold. Teleoconch sculpture on early whorls consisting of two or three distinct spiral rows of tubercles. Suture bordered by two rows, while last row runs on adapical half of whorl, connected by weak transverse rib to adapical tubercle row. Later whorls with fine spiral ribs.

Material from the boundary layers. MGUH 33140, MGUH 33141 and ØSM.10042-129. The old collections at the Natural History Museum of Denmark includes another five uncatalogued moulds.

Type stratum and type locality. The middle Danian Faxekalk at Limhamn, southern Sweden .

Occurrence. From the lower Danian Cerithium Limestone Member and up to the middle Danian Faxe Limestone in Sweden and Denmark. At Stevns Klint it is found in the Cerithium Limestone Member and succeeding Korsnaeb Member. A specimen has been found by C. Heinberg in the contemporaneous ‘dead layer’ at Vokslev, Northern Jutland.

Description of Cerithium Limestone material. Protoconch not known. Teleoconch spire high, slender with low, flat whorls and sharp keel, whorl height corresponding to one third the width. Suture enhanced by spiral ribs on early growth stages, becoming thin and shallow on later growth stages. Last whorls more inflated with keel close to abapical suture. Base nearly perpendicular to whorl side, flat to slightly concave, becoming more convex on last whorl. Aperture subrectangular with short columella carrying single sharp fold centrally, bordered abapically by deep canal.

Teleoconch sculpture variable, on early growth stages consisting of two primary beaded spiral ribs, the typically strongest at adapical suture, the other on keel at abapical suture. Primary spiral ribs separated by several weaker secondary ribs, the adapical one being the strongest; secondary ribs increasing in number on later whorls while becoming fainter. Tubercles, reflecting slightly opisthocyrt growth lines, generally merging into transverse ribs on adapical part of whorl, fading out abapically, often merging with tubercles on abapical primary spiral rib; number of adapical tubercles approximately 15 in a half whorl on second last whorl of MGUH 33141 and 18 in abapical row. Transverse ribs decreasing in strength and length with increasing whorl number. Base with single primary smooth spiral rib located close to keel at transition to flat part of base and axially succeeded by faint secondary spiral ribs. Sculpture on later growth stages changing to one of moderately fine, unbeaded spiral ribs only, the exact rib-configuration varying from specimen to specimen, but tending towards a fainter ribbing centrally on whorl. Base with weak spiral ribs.

Measurements. Most complete specimen, MGUH 33140, 32.7 mm high and 11.4 mm wide, consisting of 12 teleoconch whorls.

Remarks. The taxon is variable with regard to shell sculpture, varying between forms with only spiral ribs to others with two or three stronger spiral rows of tubercles, the adapical two connected by more or less weak transverse ribs. The transverse sculpture is typically most prominent on early teleoconch whorls, fading out on later whorls. The wide variability has led to the erection of the subjective junior synonym Campanile pseudotelescopium ( Ravn, 1902) . It was thought to differ from C. selandicum ( Lundgren, 1867) by having only one subsutural tubercle row and by the whorls being generally slightly higher and with a more abapical location of the columellar fold. An examination of the material stored at the Geological Museum of Copenhagen together with new material figured by Damholt et al. (2010) do not support such a division.

The taxon belongs to Campanile and not Metacerithium due to the well developed columellar fold and the strongly flattened base on early whorls.

MGUH

Museum Geologicum Universitatis Hafniensis

ØSM

Ohio State University Museum

Kingdom

Animalia

Phylum

Mollusca

Class

Gastropoda

Family

Campanilidae

Genus

Campanile

Loc

Campanile selandicum ( Lundgren, 1867 )

Hansen, Thomas 2019
2019
Loc

Campanile

Fischer 1884
1884
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