Eoscartoides orthocladus (Tillyard) 1922

Lambkin, Kevin J., 2016, Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2, Zootaxa 4092 (2), pp. 207-218 : 209

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.6074523

persistent identifier

https://treatment.plazi.org/id/03CD8786-FF8D-FF88-FF3F-F9993CCFF841

treatment provided by

Plazi

scientific name

Eoscartoides orthocladus (Tillyard) 1922
status

 

Eoscartoides orthocladus (Tillyard) 1922 , comb. nov.

( Figs 4–6 View FIGURES 4 – 6 )

Mesocixiodes orthoclada Tillyard, 1922: 463, text-fig. 83.

Material. Holotype left tegmen, GSQ 318a, Denmark Hill. Three additional tegmina, Denmark Hill: GSQ 91a/b+, 193a, 324a/b+.

Description. Tegmen long and narrow, 13.6 mm long, 4.8 mm wide (measurements from holotype only), length/width 2.8, anterior margin almost straight; stem of R shorter than in M. bryani , its primary fork before clavus ½ length; stems of R and RA with 0 or 1 simple costal veinlet; stem of RA1 enters costal margin at about ⅔ tegmen length, with 3 anterior branches; RA2 with 4–5 branches; RP simple, slightly up-curved apically; M1 with a terminal fork, M3+4 simple; CuA2 only slightly shorter than CuA1; no colour pattern detected.

Notes. All four specimens are poorly preserved. Even though the venation of E. orthocladus is similar to that of E. bryani , the different wing shape and the fact that it is from the younger Blackstone Formation at Denmark Hill are considered as sufficient to justify its status as a distinct species. The specific name has been changed to masculine in accord with ICZN Article 30.1.4.4.

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