Hungaroleberis, Tóth & Cséfán, 2018

Tóth, Emőke & Cséfán, Tünde, 2018, Rare myodocopid ostracods from Mesozoic sections of Hungary: summary, revision and description of new taxa, Zootaxa 4374 (3), pp. 350-374 : 362

publication ID

https://doi.org/ 10.11646/zootaxa.4374.3.2

publication LSID

lsid:zoobank.org:pub:DD41141A-212F-4502-84AA-C2ABD2254A3C

DOI

https://doi.org/10.5281/zenodo.5967888

persistent identifier

https://treatment.plazi.org/id/53BDBC1D-2646-4A23-AE71-799AA2F8893C

taxon LSID

lsid:zoobank.org:act:53BDBC1D-2646-4A23-AE71-799AA2F8893C

treatment provided by

Plazi

scientific name

Hungaroleberis
status

gen. nov.

Genus Hungaroleberis View in CoL n. gen.

Etymology. referring to the country of its type locality and with reference to the extant genus Cylindroleberis . Type species: Hungaroleberis retiferus n. sp.

Other species:

? Myodocopida gen. nov. sp. nov. (Crasquin et al. 2010, figs. 23. D’, E’, F’)

Cypridina gussevaae Crasquin-Soleau, 1998 (Crasquin-Soleau & Baud 1998, pl. 7, figs. 3–4.) Hungaroleberis sp. (this study, figs. 6/4–6.)

Type locality. Somhegy , Bakony Hills, Hungary.

Type level. Bajocian, Humphresianum Zone, Bed 3.

Diagnosis. Cylindroleberididae with valves ovoid in lateral view; rostrum and rostral incisure weakly developed; posterior margin arched without caudal process; valve surface reticulate or smooth.

Remarks. Compared to the Cretaceous species Mesoleberis hollandica Kornicker, van Bakel, Fraaije & Jagt, 2006 , Hungaroleberis lacks the linear indentation below the incisure and is smaller in size. According to Kornicker and Sohn (2000) the poorly-developed rostrum and incisure is characteristic for the superfamily Cylindroleberidoidea. These features can be observed on Hungaroleberis . Unfortunately, the specimens are complete, closed carapaces, and the muscle scar pattern cannot be examined.

Occurrences. Hydra Island , Greece: Wordian to Wuchiapingian, Upper Permian (Crasquin-Soleau & Baud 1998) ; Zhejiang Province, South China: Changhsingian, Upper Permian (Crasquin et al. 2010); Somhegy, Bakony Hills , Hungary: Bajocian, Middle Jurassic (this paper); Csurgókút, Tata, Hungary: Toarcian, Lower Jurassic (this study).

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