Kazakhstania evoluta ( Vöhringer, 1960 )

Korn, Dieter & Weyer, Dieter, 2023, The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany), European Journal of Taxonomy 882, pp. 1-230 : 146-147

publication ID

https://doi.org/ 10.5852/ejt.2023.882.2177

publication LSID

lsid:zoobank.org:pub:67C909E4-C700-4F8D-B8CE-5FD9B2C5D549

DOI

https://doi.org/10.5281/zenodo.8184491

persistent identifier

https://treatment.plazi.org/id/03EA5C14-CA98-85DD-FDE4-FA49FECF81FE

treatment provided by

Felipe

scientific name

Kazakhstania evoluta ( Vöhringer, 1960 )
status

 

Kazakhstania evoluta ( Vöhringer, 1960) View in CoL

Figs 10E View Fig , 87–88 View Fig View Fig ; Tables 83–84 View Table 83 View Table 84

Gattendorfia evoluta Vöhringer, 1960: 159 View in CoL , pl. 5 fig. 4.

Gattendorfia evoluta View in CoL – Korn 1994: 74, text-figs 65i, 66l, 67h, 68f. — Sprey 2002, pl. 4 fig. 3.

non Gattendorfia evoluta View in CoL – Bockwinkel & Ebbighausen 2006: 112, text-figs 29, 30e –h.

Diagnosis

Species of Kazakhstania with a conch reaching 30 mm diameter. Conch at 15 mm dm thinly discoidal, very evolute (ww/dm ~0.40; uw/dm ~0.65). Whorl profile at 15 mm dm moderately depressed (ww/wh ~1.80); coiling rate very low (WER ~1.48). Venter weakly flattened. Growth lines very fine, narrow-standing, with convex course. Without constrictions on the shell surface. Suture line with very narrowly lanceolate external lobe.

Material examined

Holotype

GERMANY • Rhenish Mountains, Oberrödinghausen , railway cutting ; Hangenberg Limestone , loose material; Vöhringer Coll.; illustrated by Vöhringer (1960: pl. 5 fig. 4), Korn (1994: text-fig. 65i) and Sprey (2002: pl. 4 fig. 3); re-illustrated here in Fig. 87 View Fig ; GPIT-PV-63963.

Paratype

GERMANY • Rhenish Mountains , Oberrödinghausen , railway cutting ; Hangenberg Limestone , bed 2 ; Vöhringer Coll.; GPIT-PV-63965 .

Additional material

GERMANY • 2 specimens; Rhenish Mountains , Oese , old quarry ; Hangenberg Limestone , bed 30 ; Weyer & Korn 2000 Coll.; MB.C.5258.1, MB.C.5258.6 .

Description

Holotype GPIT-PV-63963 is a moderately well-preserved specimen with 23 mm conch diameter ( Fig. 87 View Fig ). It displays the characteristic conch geometry with a very wide umbilicus (uw/dm = 0.63) and a depressed rectangular whorl profile (ww/wh = 1.88) with a flattened venter and uniformly convex flanks. Shell remains are present in some places; they show very fine growth lines, standing approximately 0.2 mm apart. They are clearly directed backwards from the umbilicus and form a broad ventral sinus ( Fig. 88C View Fig ). The suture line has a very narrow, lanceolate external lobe ( Fig. 88B View Fig ).

The sectioned paratype GPIT-PV-63965 shows only minor ontogenetic changes in conch geometry up to a conch diameter of 14 mm ( Fig. 88A View Fig ). The whorl profile of all whorls larger than 4 mm conch diameter is rounded trapezoidal with a flattened venter. The ontogenetic trajectories are monophasic ( Fig. 88D– F View Fig ); the umbilical width increases slightly in early ontogeny and remains at a very high value above 0.60 from a conch diameter of 5 mm.

Remarks

Kazakhstania evoluta can be distinguished from almost all other species of the genus by the absence of constrictions. Similar in this respect is only E. kana sp. nov. from the Anti-Atlas of Morocco; this species, however, has a pouched external lobe that is about twice as wide and is thus clearly different from K. evoluta .

Kingdom

Animalia

Phylum

Mollusca

Class

Cephalopoda

Order

Goniatitida

SubOrder

Tornoceratina

SuperFamily

Prionoceratoidea

Family

Gattendorfiidae

SubFamily

Gattendorfiinae

Genus

Kazakhstania

Loc

Kazakhstania evoluta ( Vöhringer, 1960 )

Korn, Dieter & Weyer, Dieter 2023
2023
Loc

Gattendorfia evoluta

Bockwinkel J. & Ebbighausen V. 2006: 112
2006
Loc

Gattendorfia evoluta

Sprey A. M. 2002: 146
Korn D. 1994: 74
1994
Loc

Gattendorfia evoluta Vöhringer, 1960: 159

Vohringer E. 1960: 159
1960
GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF