Pharciceras beyrichi, Korn & Bockwinkel, 2021

Korn, Dieter & Bockwinkel, Jürgen, 2021, The pharciceratid ammonoids from the Roteisenstein Formation of Dillenburg (Cephalopoda, Ammonoidea), European Journal of Taxonomy 771, pp. 1-79 : 13-15

publication ID

https://doi.org/ 10.5852/ejt.2021.771.1503

publication LSID

lsid:zoobank.org:pub:9FAB6919-E4AC-44A6-89AB-2E236F55FDB5

DOI

https://doi.org/10.5281/zenodo.5552698

persistent identifier

https://treatment.plazi.org/id/6E860B7E-D08C-4491-9649-B94A153C0191

taxon LSID

lsid:zoobank.org:act:6E860B7E-D08C-4491-9649-B94A153C0191

treatment provided by

Felipe

scientific name

Pharciceras beyrichi
status

sp. nov.

Pharciceras beyrichi sp. nov.

urn:lsid:zoobank.org:act:6E860B7E-D08C-4491-9649-B94A153C0191

Figs 8–9 View Fig View Fig ; Table 3 View Table 3

Diagnosis

Species of Pharciceras with thickly discoidal, subevolute conch at 35 mm dm (ww / dm ~ 0.55; uw/ dm ~ 0.38). Whorl profile depressed, crescent-shaped at 35 mm dm (ww / wh ~1.75); whorl expansion rate low (WER ~1.55). Whorl profile with broadly convex flanks continuing to the very broadly rounded venter. Growth lines coarse, strongly biconvex; ventrolateral shoulder with two spiral grooves. Outer suture line with symmetric, V-shaped prongs of the external lobe, a lancolate, blunt lateral lobe and very small rounded U 2 and U 4 lobes.

Etymology

Named after Heinrich Ernst Beyrich (1815–1896), one of the pioneers of studying fossils from the Red Ironstone.

Material examined

Holotype GERMANY • Rhenish Mountains , Oberscheld; late Givetian (Red Ironstone); Koch Coll.; MB.C.22174 . ( Fig. 8 View Fig )

Paratype GERMANY • 1 specimen; Rhenish Mountains , probably from Oberscheld; late Givetian (Red Ironstone); MB.C. 30231 .

Description

Holotype MB.C.22174 is laterally slightly deformed, completely chambered specimen with 34 mm conch diameter in haematitic limestone; small parts of the specimen are covered with shell, the phragmocone is filled with sparry calcite ( Fig. 8 View Fig ). The specimen has a thickly discoidal and subevolute conch shape with a low coiling rate at 34 mm diameter; the whorl profile is depressed with steep umbilical wall and broadly rounded flanks and venter. Two faint ventrolateral spiral grooves on each side separate the flanks from the venter, which is broadly rounded at the largest diameter of the specimen but flattened up to the last volution ( Fig. 9B View Fig ). The ornament shows lamellar growth lines. The suture line has a very wide external lobe with nearly parallel flanks and lanceolate prongs. Two lobes are located on the flank: the asymmetric lateral lobe that is larger than the prongs of the external lobe and the small, rounded U 2 lobe ( Fig. 9A View Fig ). A very small U 4 lobe is located on the umbilical wall.

Remarks

The two specimens, of which only the holotype is rather well-preserved, are described here as a new species because a conch morphology cannot be attributed to any other species of Pharciceras . Its conch is stouter (ww / dm ~ 0.55 at 35 mm conch diameter) than in most of the other species of Pharciceras . Juveniles of P. kruegeri sp. nov. are also stout, but they possess a narrower umbilicus (uw / dm ~0.33) than P. beyrichi sp. nov. (uw / dm ~ 0.38) and much weaker ventrolateral grooves.

Pharciceras tridens is a similar form, but is slenderer with a ww / dm ratio of ~ 0.45 at 35 mm conch diameter. In smaller stages at 25 mm diameter, the venter is broadly rounded in P. tridens , in contrast to the slightly flattened venter in P. beyrichi sp. nov.

Table 3. Conch dimensions and ratios of selected specimen of Pharciceras beyrichi sp. nov.

Specimen dm ww wh uw ah ww / dm ww / wh uw / dm WER IZR
MB.C.22174 34.7 18.7 10.8 13.2 6.8 0.54 1.73 0.38 1.55 0.37
MB

Universidade de Lisboa, Museu Bocage

Kingdom

Animalia

Phylum

Mollusca

Class

Cephalopoda

SubClass

Ammonoidea

Order

Ammonoidea

SubOrder

Pharciceratina

Family

Pharciceratidae

SubFamily

Pharciceratinae

Genus

Pharciceras

GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF