Acanthoclymenia planorbis (Sandberger & Sandberger, 1851)

Korn, Dieter & Bockwinkel, Jürgen, 2022, The early gephuroceratid ammonoids from the Roteisenstein Formation of Dillenburg (Cephalopoda, Ammonoidea), European Journal of Taxonomy 823, pp. 10-47 : 42-44

publication ID

https://doi.org/ 10.5852/ejt.2022.823.1811

publication LSID

lsid:zoobank.org:pub:D5AC626B-4A10-4CD9-B77B-6D7EFE8D180E

DOI

https://doi.org/10.5281/zenodo.6930226

persistent identifier

https://treatment.plazi.org/id/C9186647-4227-897D-FE46-5D61FE55C436

treatment provided by

Felipe

scientific name

Acanthoclymenia planorbis (Sandberger & Sandberger, 1851)
status

 

Acanthoclymenia planorbis (Sandberger & Sandberger, 1851) View in CoL

Figs 21–22 View Fig View Fig

Goniatites planorbis Sandberger & Sandberger, 1851: 96 , pl. 9 fig. 3.

Gephyroceras planorbis – Wedekind 1918: 122.

Ponticeras planorbis – Matern 1931: 83.

Acanthoclymenia planorbis View in CoL – Korn & Klug 2002: 119, text-fig. 123h.

Diagnosis

Species of Acanthoclymenia reaching about 30 mm conch diameter with small, extremely discoidal, evolute conch between12 and 32 dm (uw/dm decreasing from ~ 0.50 to ~ 0.45). Whorl profile compressed; umbilical wall shallow and rounded, whorl profile pear-shaped, ventrolateral margin angular, venter flat. Growth lines very fine, strongly biconvex.

Material examined

Lectotype GERMANY • Rhenish Mountains, Oberscheld ; middle Frasnian (Red Ironstone); Wiesb. 46a. Illustrated by Sandberger & Sandberger (1850 –1856: pl. 9 fig. 3a); re-illustrated here ( Fig. 21A View Fig ).

Paralectotype GERMANY • 1 specimen; Rhenish Mountains , Oberscheld ; middle Frasnian (Red Ironstone); Wiesb. 46b. Illustrated by Sandberger & Sandberger (1850 –1856: pl. 9 fig. 3) re-illustrated here ( Fig. 21B View Fig ) .

Additional material

GERMANY • 1 specimen; Rhenish Mountains , Oberscheld (Grube Königszug); middle Frasnian (Red Ironstone); Kauth Coll.; MB.C.30438 1 specimen; Rhenish Mountains , Oberscheld; middle Frasnian (Red Ironstone); Koch Coll.; MB.C.30439 .

Description

Four specimens are selected for description and illustration:

Lectotype Wiesb. 46a: incomplete specimen with 32 mm conch diameter in haematitic ironstone ( Fig. 21A View Fig ).

Paralectotype Wiesb. 46b: incomplete specimen with 22 mm conch diameter in haematitic ironstone ( Fig. 21B View Fig ).

MB.C.30438: slab and counterslab with two specimens (13 and 7 mm conch diameter) co-occuring with Mesobeloceras kayseri in haematite ore ( Fig. 22A View Fig ).

MB.C.30439: moderately well-preserved specimen with 12 mm conch diameter in haematitic iron ore ( Fig. 22B View Fig ).

The specimens contribute only little to our knowledge of the species. All are embedded on rock slabs ( Fig. 22 View Fig ), which prevents precise measurement of the whorl width, but it is clear that the conch is extremely discoidal. It is also clear that the whorl profile is pear-shaped with a rounded umbilical wall, convex flanks, a subangular ventrolateral shoulder and a flattened venter. The umbilicus has nearly exactly half the value of the conch diameter.

Remarks

Acanthoclymenia planorbis differs from the other species of the genus from Oberscheld, A. forcipifera , in the much wider umbilicus at 12 mm conch diameter (uw/dm ~ 0.50 in A. planorbis but ~ 0.30 in A. forcipifera ).

Kingdom

Animalia

Phylum

Mollusca

Class

Cephalopoda

Order

Ammonoidea

Family

Acanthoclymeniidae

Genus

Acanthoclymenia

Loc

Acanthoclymenia planorbis (Sandberger & Sandberger, 1851)

Korn, Dieter & Bockwinkel, Jürgen 2022
2022
Loc

Acanthoclymenia planorbis

Korn D. & Klug C. 2002: 119
2002
Loc

Ponticeras planorbis

Matern H. 1931: 83
1931
Loc

Gephyroceras planorbis

Wedekind R. 1918: 122
1918
Loc

Goniatites planorbis

Sandberger & Sandberger 1851: 96
1851
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