Planorbarius cf. cornu ( Brongniart, 1810 )

Harzhauser, Mathias, Neubauer, Thomas A. & Hoşgör, İzzet, 2018, Oligocene-Miocene freshwater gastropods from the Oltu-Narman Basin in eastern Turkey, Acta Palaeontologica Polonica 63 (2), pp. 357-369 : 364-366

publication ID

https://doi.org/ 10.4202/app.00469.2018

publication LSID

lsid:zoobank.org:pub:153CB896-6EE8-48F1-A330-80FCD3B1ED94

persistent identifier

https://treatment.plazi.org/id/03C387DC-7819-9362-FCCC-F91F51A993F0

treatment provided by

Felipe

scientific name

Planorbarius cf. cornu ( Brongniart, 1810 )
status

 

Planorbarius cf. cornu ( Brongniart, 1810) View in CoL

Fig. 5C–E View Fig .

cf. 1810 Planorbis Cornu ; Brongniart 1810: 371, pl. 22: 6.

Material.— Seven specimens: NHMW 2018 View Materials /0019/0022 ( Fig. 5C View Fig ); NHMW 2018 View Materials /0019/0023 ( Fig. 5D View Fig ); NHMW 2018 View Materials / 0019/0024 ( Fig. 5E View Fig ); NHMW 2018 View Materials /0019/0024a (4 specimens) from the upper Susuz Formation ( upper Oligocene or lower Miocene ) at Kömürlü, Oltu-Narman Basin, northeastern Turkey .

Remarks.—Only fragmentary specimens consisting of few whorls are available showing a shell with strongly convex whorls and deep suture ( Table 5). The protoconch displays traces of spiral rows of pits, which are replaced by delicate spiral cords on the first teleoconch whorl whereas the later whorls are smooth. These features correspond fully to specimens of Planorbarius cornu as described by Harzhauser et al. (2014b) from the early Miocene of the Czech Republic. Although the very high whorls support the identification, a separation from the early to late Miocene Planorbarius mantelli ( Dunker, 1848) is difficult based on fragments only see Harzhauser et al. 2014a, b). Moreover, the status of Planorbarius cornu is problematic and would need revision based on topotypic specimens from the Meulières de Montmorency in France (see Kadolsky 2015 for discussion). Therefore, we discuss the Turkish species in open nomenclature.

Planorbarius cornu was originally described from the Rupelian of the Paris Basin and is frequently recorded in Europe from Oligocene and lower Miocene deposits ( Wenz 1923).

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