Dzhulfites brevisellatus Korn & Hairapetian, 2021
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.5604747 |
persistent identifier |
https://treatment.plazi.org/id/1FDCA9D7-546A-48FA-94E1-0053EB7F7C23 |
taxon LSID |
lsid:zoobank.org:act:1FDCA9D7-546A-48FA-94E1-0053EB7F7C23 |
treatment provided by |
Felipe |
scientific name |
Dzhulfites brevisellatus Korn & Hairapetian |
status |
sp. nov. |
Dzhulfites brevisellatus Korn & Hairapetian sp. nov.
urn:lsid:zoobank.org:act:1FDCA9D7-546A-48FA-94E1-0053EB7F7C23
Fig. 23 View Fig ; Table 8
Diagnosis
Species of Dzhulfites with conch reaching 160 mm dm. Subadult stage with weakly trapezoidal, moderately depressed whorl profile (ww/wh =1.50–1.80) and broadly rounded venter; 10–13 coarse conical nodes on midflank per volution. Adult stage with numerous weak ribs and small ventrolateral nodes. Prongs of external lobe bifid or trifid; altogether 15–20 notches of E, A and L lobes.
Etymology
From the Latin ‘ brevis ’, meaning ‘low’ and ‘ sella ’, meaning ‘saddle’, after the low amplitude of lobes and saddles in the suture line.
Material examined
Holotype IRAN • Esfahan Province, Baghuk Mountain H section ; Hambast Formation, 5.70 m below top; illustrated in Fig. 23B View Fig ; MB.C.29748 .
Paratypes IRAN • 1 specimen; Esfahan Province, Baghuk Mountain ; Hambast Formation; MB.C.29746 • 1 specimen; Esfahan Province, Baghuk Mountain E section ; Hambast Formation; MB.C.29747 .
Description
The large paratype MB.C.29746 has 125 mm conch diameter, of which half of the last whorl belongs to the strongly weathered body chamber ( Fig. 23A View Fig ). The phragmocone is 90 mm in diameter and is partly crushed; it shows that the whorl profile is trapezoidal with a broadly rounded venter. The sculpture changes dramatically throughout ontogeny. At 40 mm dm there are 13 coarse, spiny ventrolateral nodes per volution; these nodes become weaker and more numerous so that the last 120° of the phragmocone have about 20 weak ventrolateral nodes, which are connected with weak and slightly sinuous radial ribs on the flank. The suture line of the specimen suffered from weathering, but, most probably, the prongs of the very short external lobe are bifid.
Holotype MB.C.29748 is a fairly well-preserved, fully septate specimen with 51 mm conch diameter ( Fig. 23B View Fig ). It has a weakly trapezoidal whorl profile with broadly rounded flanks and venter. The sculpture shows about ten coarse conical nodes, which are positioned on the midflank, on the last preserved volution.
The suture line of the holotype shows an external lobe with subparallel, weakly diverging flanks and weakly asymmetric, trifid prongs. All three saddles of the outer suture line are similar in shape, being inverted U-shaped and broadly rounded. The adventive lobe and the lateral lobe are similar in shape with parallel flanks and many small notches at the base. They differ in their depth; the adventive lobe is much deeper than the external lobe ( Fig. 23C View Fig ).
Remarks
Among the species of Dzhulfites , only D. nodosus is similar in conch shape and sculpture, but this species shows an applanate venter in the adult stage. Dzhulfites brevisellatus sp. nov. differs from D. spinosus and the other species of the genus in the suture line, which in D. brevisellatus sp. nov. shows much wider elements; particularly the saddles are wider than the lobes. In the shape of the suture line, D. brevisellatus sp. nov. has some resemblance to representatives of the family Xenodiscidae .
Stratigraphic range
Upper part of the Hambast Formation; 5.70 to 4.70 m below the extinction horizon ( Dzhulfites spinosus Zone to Shevyrevites shevyrevi 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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