Shevyrevites nodosus ( Shevyrev, 1965 )
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 |
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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 ).
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Shevyrevites nodosus ( Shevyrev, 1965 )
Korn, Dieter, Hairapetian, Vachik, Ghaderi, Abbas, Leda, Lucyna, Schobben, Martin & Akbari, Amir 2021 |
Shevyrevites nodosus
Korn et al. 2019: 46 |
Bernhardites nodosus
Shevyrev A. A. 1968: 87 |
Bernhardites nodosus
Shevyrev A. A. 1965: 171 |