identifier	taxonID	type	CVterm	format	language	title	description	additionalInformationURL	UsageTerms	rights	Owner	contributor	creator	bibliographicCitation
03CD8786FF8EFF8BFF3FF8FD3CBDFB11.text	03CD8786FF8EFF8BFF3FF8FD3CBDFB11.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Dysmorphoptilidae Handlirsch 1906	<div><p>Family Dysmorphoptilidae Handlirsch, 1906</p></div>	https://treatment.plazi.org/id/03CD8786FF8EFF8BFF3FF8FD3CBDFB11	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Lambkin, Kevin J.	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.text	03CD8786FF8EFF88FF3FF8B03A9EFD92.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Eoscartoides Evans 1956	<div><p>Eoscartoides Evans, 1956</p><p>Eoscartoides Evans, 1956: 220 .</p><p>Type species. Eoscartoides bryani Evans, 1956, by original designation.</p><p>Mesonirvana Evans, 1956: 191–192. Syn. nov.</p><p>Type species. Mesonirvana abrupta Evans, 1956: 192, fig. 5E, by original designation.</p><p>Mesocixiodes Tillyard, 1922: 462 (partim).</p><p>Type species. Mesocixiodes termioneura Tillyard, 1922: 462, text fig. 82, plate 53, fig. 34, by original designation.</p><p>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 RA1 directed anteriorly in line with stem of RA, entering costal margin well before tegmen apex, with at least 2 anterior branches; RA2 extensive, occupying a large area antero-apically, with at least 3 anterior branches; RA2 and RP joined by a crossvein; M1+2 deeply forked; M3+4 simple, or with a terminal fork only; M and CuA joined basally by a short crossvein (the “arculus”); apical m-cu inclined; CuA1 gently concave; CuA2 straight.</p><p>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).</p><p>The large and distinctly shaped strigil, the very short stem of RA, and the basic pattern of forking of M (M1+2 deep, M3+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 F3697a/b, GSQ 318a, QM F58592), 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).</p></div>	https://treatment.plazi.org/id/03CD8786FF8EFF88FF3FF8B03A9EFD92	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Lambkin, Kevin J.	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.text	03CD8786FF8DFF88FF3FFEC93DFFFAC2.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Eoscartoides bryani Evans 1956	<div><p>Eoscartoides bryani Evans, 1956</p><p>(Figs 1–3)</p><p>Eoscartoides bryani Evans, 1956: 221, fig. 18A; Evans 1961: 20, figs 4A–4C. Mesonirvana abrupta Evans, 1956: 192, fig. 5E. Syn. nov.</p><p>Material. Holotype left tegmen UQG C172, paratype tegmina UQG C677/680+, C933/934+, holotype tegmen of Mesonirvana abrupta, UQG C1652, all Mount Crosby Locality A. 12 additional tegmina, Mount Crosby: Locality A: QM: F3693a/b+, F3695a/b+, F3697a/b+, F58584, F58585 +, F58586 +, F58587 +, F58588 +, F58589 +, F58590 + (the latter seven listed by Evans (1961) as UQE S4, S5/5A, S9, S10/10A, S15, S17/17A and S19/19A); Locality B: ACC I.2 a/b+, I.120.</p><p>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 RA1 enters costal margin at about ⅔ tegmen length, with 1-3 anterior branches, one sometimes with an end-twig; RA2 with 3-5 branches, sometimes with an end-twig; RP simple, more or less straight, or at most very slightly up-curved apically; M1 simple or with a terminal fork; M3+4 simple, in one specimen only with a terminal fork; CuA2 only slightly shorter than CuA1; tegmen surface apparently somewhat darkly suffused, noticeably darker in extreme basal costal space and narrowly along costal margin.</p><p>Notes. The species demonstrates a degree of intraspecific variation in tegmen size and proportions, and in the form, spacing and number of branches of RA1 and RA2 (Figs 1,3).</p></div>	https://treatment.plazi.org/id/03CD8786FF8DFF88FF3FFEC93DFFFAC2	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Lambkin, Kevin J.	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.text	03CD8786FF8DFF88FF3FF9993CCFF841.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Eoscartoides orthocladus (Tillyard 1922) Tillyard	<div><p>Eoscartoides orthocladus (Tillyard) 1922, comb. nov.</p><p>(Figs 4–6)</p><p>Mesocixiodes orthoclada Tillyard, 1922: 463, text-fig. 83.</p><p>Material. Holotype left tegmen, GSQ 318a, Denmark Hill. Three additional tegmina, Denmark Hill: GSQ 91a/b+, 193a, 324a/b+.</p><p>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.</p><p>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.</p></div>	https://treatment.plazi.org/id/03CD8786FF8DFF88FF3FF9993CCFF841	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Lambkin, Kevin J.	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.text	03CD8786FF8BFF8CFF3FFAFD3D85FEB2.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Eoscartoides dmitryi	<div><p>Eoscartoides dmitryi sp. nov.</p><p>(Figs 7–9)</p><p>Material. Holotype right tegmen QM F58591, Dinmore, collected by Robert Knezour. Three paratype tegmina, Dinmore: QM F13625; ACC I.36 +; RKC: QM F58592.</p><p>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 RA1 enters costal margin at about ½ tegmen length, with 2 anterior branches; RA2 with 4–5 branches, sometimes with an endtwig; RP simple or with an up-curved terminal fork; M1 and M3+4 with deep terminal forks; CuA2 much shorter than CuA1; 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).</p><p>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 CuA2. 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.</p></div>	https://treatment.plazi.org/id/03CD8786FF8BFF8CFF3FFAFD3D85FEB2	Public Domain	No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.		MagnoliaPress via Plazi	Lambkin, Kevin J.	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
