Shevyrevites nodosus ( Shevyrev, 1965 )

Korn, Dieter, Hairapetian, Vachik, Ghaderi, Abbas, Leda, Lucyna, Schobben, Martin & Akbari, Amir, 2021, The Changhsingian (Late Permian) ammonoids from Baghuk Mountain (Central Iran), European Journal of Taxonomy 776, pp. 1-106 : 21-22

publication ID

https://doi.org/ 10.5852/ejt.2021.776.1559

publication LSID

lsid:zoobank.org:pub:226B6C59-8620-4A29-9BEF-359BE67A1A2C

DOI

https://doi.org/10.5281/zenodo.5633946

persistent identifier

https://treatment.plazi.org/id/03CC87BF-FFD9-FFC2-FDB8-FE68FAC1FBCC

treatment provided by

Felipe

scientific name

Shevyrevites nodosus ( Shevyrev, 1965 )
status

 

Shevyrevites nodosus ( Shevyrev, 1965) View in CoL

Fig. 18 View Fig ; Table 3

Bernhardites nodosus Shevyrev, 1965: 171 , pl. 21 fig. 8.

Bernhardites nodosus – Shevyrev 1968: 87, pl. 2 fig. 2.

Shevyrevites nodosus View in CoL – Korn et al. 2019: 46, text-fig. 13.

non Shevyrevites nodosus View in CoL – Korn in Ghaderi et al. 2014: text-fig. 7d.

Diagnosis

Species of Shevyrevites with conch reaching 80 mm dm. Subadult stage with circular, slightly compressed whorl profile (ww/wh =0.60–0.75) and rounded venter; 10 coarse lateral nodes per volution. Adult stage with parallel-sided, slightly compressed whorl profile (ww/wh =0.60–0.75), flattened venter and subangular ventrolateral shoulder; radial plications. Prongs of external lobe simple or bifid; altogether about 15 notches of E, A and L lobes.

Type material

Holotype ARMENIA • Ogbin ; Late Permian; illustrated by Shevyrev (1965: pl. 24 fig. 1); PIN 1478/31 .

Material examined

IRAN • 1 specimen; Esfahan Province, Baghuk Mountain C section ; Hambast Formation; MB.C.29713 1 specimen; Esfahan Province, Baghuk Mountain E section ; Hambast Formation; MB.C.29714 1 specimen; Esfahan Province, Baghuk Mountain G section ; Hambast Formation; MB.C.29715 2 specimens; Esfahan Province, Baghuk Mountain ; Hambast Formation; MB.C.29716 to MB.C.29717 .

Description

Specimen MB.C.29713 has 53 mm diameter and shows the partly crushed phragmocone and less than half a volution of the terminal body chamber ( Fig. 18 View Fig ). The whorl profile of the body chamber is subtrapezoidal with weakly converging flanks, a subangular ventrolateral shoulder and a flattened venter. The sculpture of the phragmocone differs significantly from the body chamber; while the phragmocone bears coarse conical nodes (10 per volution) and later elongate sharp ribs on the midflank, the body chamber has weak and blunt radial ribs. Only portions of the suture line can be seen on the flank; they show a finely serrated adventive lobe.

Remarks

Shevyrevites nodous differs in the coarse lateral nodes of the subadult stage from S. shevyrevi and S. corrugatus sp. nov.

Stratigraphic range

Upper part of the Hambast Formation; 4.45 m below the extinction horizon ( Shevyrevites nodosus Zone ).

Kingdom

Animalia

Phylum

Mollusca

Class

Cephalopoda

Order

Ceratitida

Family

Xenodiscidae

Genus

Shevyrevites

Loc

Shevyrevites nodosus ( Shevyrev, 1965 )

Korn, Dieter, Hairapetian, Vachik, Ghaderi, Abbas, Leda, Lucyna, Schobben, Martin & Akbari, Amir 2021
2021
Loc

Shevyrevites nodosus

Korn et al. 2019: 46
2019
Loc

Bernhardites nodosus

Shevyrev A. A. 1968: 87
1968
Loc

Bernhardites nodosus

Shevyrev A. A. 1965: 171
1965
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