taxonID	type	description	language	source
03CD8786FF8EFF88FF3FF8B03A9EFD92.taxon	materials_examined	Type species. Eoscartoides bryani Evans, 1956, by original designation. Mesonirvana Evans, 1956: 191 – 192. Syn. nov. Type species. Mesonirvana abrupta Evans, 1956: 192, fig. 5 E, by original designation. Mesocixiodes Tillyard, 1922: 462 (partim). Type species. Mesocixiodes termioneura Tillyard, 1922: 462, text fig. 82, plate 53, fig. 34, by original designation. Diagnostic characters. Tegmen over 11 mm long, lobate; precostal carina and marginal membrane distinct; hypocostal carina short; punctation very fine, somewhat coarser basally and posterior to Pcu; hyposubcostal carina long, only very slightly concave; strigil in basal costal space large and well developed, quite coarsely rugose, extending in an arc from just above R to costal margin; no swellings detected on hind margin of clavus, its proximal corner strongly bent downwards; stem of RA very short, its primary fork just beyond clavus ½ length, proximal to level of CuA fork; stem of RA 1 directed anteriorly in line with stem of RA, entering costal margin well before tegmen apex, with at least 2 anterior branches; RA 2 extensive, occupying a large area antero-apically, with at least 3 anterior branches; RA 2 and RP joined by a crossvein; M 1 + 2 deeply forked; M 3 + 4 simple, or with a terminal fork only; M and CuA joined basally by a short crossvein (the “ arculus ”); apical m-cu inclined; CuA 1 gently concave; CuA 2 straight.	en	Lambkin, Kevin J. (2016): Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2. Zootaxa 4092 (2): 207-218, DOI: 10.11646/zootaxa.4092.2.4
03CD8786FF8EFF88FF3FF8B03A9EFD92.taxon	description	Notes. The type species of Eoscartoides and Mesonirvana are synonyms. As both generic names were established in the same paper, as first reviser (ICZN Article 24), I have chosen Eoscartoides as the senior synonym on the grounds that its type specimen is better preserved and that all subsequent published specimens (Evans 1961) have been identified as Eoscartoides bryani. The type specimen of the type species, Mesonirvana abrupta Evans, preserves only the apical region of the tegmen and is somewhat distorted, whereas that of E. bryani is almost complete, and in particular shows the characteristic strigil in the basal costal space (see photographs at pages 44 and 56 of Jell 2004). The large and distinctly shaped strigil, the very short stem of RA, and the basic pattern of forking of M (M 1 + 2 deep, M 3 + 4 simple) are considered as the apomorphies for Eoscartoides. The structure and shape of the strigil is apparently the same as that of the unnamed Triassic sspecies from the Madygen Formation of Kyrgyzstan illustrated by Shcherbakov and Popov (2002, fig. 184) which also appears to have similar venation to Eoscartoides. Even though only one specimen of each of the three species of Eoscartoides preserves a substantial part of the clavus (QM F 3697 a / b, GSQ 318 a, QM F 58592), the peculiar bend at the proximal corner is present in all three and is probably the basal part of the commissural carina (Dmitry Shcherbakov, pers com.) (Figs 3,4,9).	en	Lambkin, Kevin J. (2016): Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2. Zootaxa 4092 (2): 207-218, DOI: 10.11646/zootaxa.4092.2.4
03CD8786FF8DFF88FF3FFEC93DFFFAC2.taxon	materials_examined	Material. Holotype left tegmen UQG C 172, paratype tegmina UQG C 677 / 680 +, C 933 / 934 +, holotype tegmen of Mesonirvana abrupta, UQG C 1652, all Mount Crosby Locality A. 12 additional tegmina, Mount Crosby: Locality A: QM: F 3693 a / b +, F 3695 a / b +, F 3697 a / b +, F 58584, F 58585 +, F 58586 +, F 58587 +, F 58588 +, F 58589 +, F 58590 + (the latter seven listed by Evans (1961) as UQE S 4, S 5 / 5 A, S 9, S 10 / 10 A, S 15, S 17 / 17 A and S 19 / 19 A); Locality B: ACC I. 2 a / b +, I. 120.	en	Lambkin, Kevin J. (2016): Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2. Zootaxa 4092 (2): 207-218, DOI: 10.11646/zootaxa.4092.2.4
03CD8786FF8DFF88FF3FFEC93DFFFAC2.taxon	description	Description. Tegmen 11.4 – 12.4 mm long, 5.0 – 6.0 mm wide (holotype 5.9), length / width 2.1 - 2.4, anterior margin convex except at base which is somewhat truncate; R with 0 or 1 simple costal veinlet; primary fork of R at about clavus ½ length; stem of RA with 0, 1 or 2 simple costal veinlets; stem of RA 1 enters costal margin at about ⅔ tegmen length, with 1 - 3 anterior branches, one sometimes with an end-twig; RA 2 with 3 - 5 branches, sometimes with an end-twig; RP simple, more or less straight, or at most very slightly up-curved apically; M 1 simple or with a terminal fork; M 3 + 4 simple, in one specimen only with a terminal fork; CuA 2 only slightly shorter than CuA 1; tegmen surface apparently somewhat darkly suffused, noticeably darker in extreme basal costal space and narrowly along costal margin. Notes. The species demonstrates a degree of intraspecific variation in tegmen size and proportions, and in the form, spacing and number of branches of RA 1 and RA 2 (Figs 1,3).	en	Lambkin, Kevin J. (2016): Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2. Zootaxa 4092 (2): 207-218, DOI: 10.11646/zootaxa.4092.2.4
03CD8786FF8DFF88FF3FF9993CCFF841.taxon	materials_examined	Material. Holotype left tegmen, GSQ 318 a, Denmark Hill. Three additional tegmina, Denmark Hill: GSQ 91 a / b +, 193 a, 324 a / b +.	en	Lambkin, Kevin J. (2016): Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2. Zootaxa 4092 (2): 207-218, DOI: 10.11646/zootaxa.4092.2.4
03CD8786FF8DFF88FF3FF9993CCFF841.taxon	description	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 RA 1 enters costal margin at about ⅔ tegmen length, with 3 anterior branches; RA 2 with 4 – 5 branches; RP simple, slightly up-curved apically; M 1 with a terminal fork, M 3 + 4 simple; CuA 2 only slightly shorter than CuA 1; 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.	en	Lambkin, Kevin J. (2016): Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2. Zootaxa 4092 (2): 207-218, DOI: 10.11646/zootaxa.4092.2.4
03CD8786FF8BFF8CFF3FFAFD3D85FEB2.taxon	materials_examined	Material. Holotype right tegmen QM F 58591, Dinmore, collected by Robert Knezour. Three paratype tegmina, Dinmore: QM F 13625; ACC I. 36 +; RKC: QM F 58592.	en	Lambkin, Kevin J. (2016): Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2. Zootaxa 4092 (2): 207-218, DOI: 10.11646/zootaxa.4092.2.4
03CD8786FF8BFF8CFF3FFAFD3D85FEB2.taxon	description	Description. Tegmen c. 18 – 19 mm long (holotype c. 18 mm), 7.5 mm wide, length / width 2.5, anterior margin convex except at base which is somewhat truncate; stem of R shorter than in M. bryani, its primary fork before clavus ½ length, with 0 or 1 simple costal veinlet; stem of RA with 1 simple costal veinlet; stem of RA 1 enters costal margin at about ½ tegmen length, with 2 anterior branches; RA 2 with 4 – 5 branches, sometimes with an endtwig; RP simple or with an up-curved terminal fork; M 1 and M 3 + 4 with deep terminal forks; CuA 2 much shorter than CuA 1; tegmen surface somewhat darkly suffused, noticeably darker in basal costal space, along costal margin, in punctate area of clavus, and along the veins (Fig. 9). Notes. Eoscartoides dmitryi, from the Dinmore site of the Blackstone Formation, is distinguished from its congeners by its larger size, stronger terminal forking of RP and M, and the shorter CuA 2. The specific name honours Dmitry Shcherbakov of the Russian Academy of Sciences. It is only through his ground-breaking work on the classification of fossil Hemiptera that the present study has been possible.	en	Lambkin, Kevin J. (2016): Revision of the Dysmorphoptilidae (Hemiptera: Cicadomorpha: Prosboloidea) of the Queensland Triassic — Part 2. Zootaxa 4092 (2): 207-218, DOI: 10.11646/zootaxa.4092.2.4
