Eoscartoides bryani

Lambkin, Kevin J., 2016, Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2, Zootaxa 4092 (2), pp. 207-218 : 213

publication ID

https://doi.org/ 10.11646/zootaxa.4092.2.4

publication LSID

lsid:zoobank.org:pub:56072014-E67D-4866-A131-6693C2836B5E

DOI

https://doi.org/10.5281/zenodo.6074529

persistent identifier

https://treatment.plazi.org/id/03CD8786-FF89-FF8C-FF3F-F8B43D4FF95D

treatment provided by

Plazi

scientific name

Eoscartoides bryani
status

 

Eoscarterella media Evans, 1956

( Figs 10–12 View FIGURES 10 – 12 )

Eoscarterella media Evans, 1956: 20, fig. 18C; Evans 1961: 19.

Prosbolopsites tillyardi Bekker-Migdisova, 1960: 90 (synonymy by Evans 1961).

Material. Holotype right tegmen UQG C1110/1111+, Mount Crosby Locality A. Two additional tegmina, Mount Crosby Locality A: QM F58593 View Materials + (listed by Evans (1961) as UQE S8/8A), F58596 View Materials + (listed by Evans (1961) as UQE S13/13A and identified as Eoscartoides bryani ).

Description. Length 10.3 mm, width 4.5–4.7 mm (holotype 4.7), length/width 2.2-2.3; R without costal veinlets; RA without or with 1 oblique costal veinlet; no colour pattern detected (the darkened costal margin in Fig. 12 View FIGURES 10 – 12 is a lighting effect of the merged photographs).

Notes. The crossvein between RA2 and RP could not be detected in the holotype or QM F58593 View Materials , neither of which are all that clearly preserved, especially in this area of the tegmen. It is, however, present in QM F58596 View Materials which although more fragmentary is much better preserved.

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