Unturella truncata Shcherbakov, 2022

Shcherbakov, D. E., 2022, New Dysmorphoptilidae (Cicadomorpha) from the end-Permian and Middle Jurassic of Siberia: earliest evidence of acoustic communication in Hemiptera and the latest find of the family, Russian Entomological Journal 31 (2), pp. 108-113 : 110

publication ID

https://doi.org/ 10.15298/rusentj.31.2.02

DOI

https://doi.org/10.5281/zenodo.13179526

persistent identifier

https://treatment.plazi.org/id/03DE87A3-C52B-FFEB-D856-A62DFAEAC781

treatment provided by

Felipe

scientific name

Unturella truncata Shcherbakov
status

sp. nov.

Unturella truncata Shcherbakov View in CoL , sp.n.

Figs 1–8 View Figs 1–8 .

Unturella truncata Shcherb. View in CoL : Kazakov et al., 2002: 160 (nomen nudum)

Unturella truncata Shcherb. View in CoL : Varganov et al., 2015: 127 (nomen nudum)

MATERIAL. Holotype PIN 2989 View Materials /1±, complete tegmen (clavus separated; M-CuA area crumpled, so that apical margin seems oblique), Untuun-2, left bank of Untuun R. (left tributary of Kochechumo R.) against mouth of Khoktokon R., Evenkiysky District, Krasnoyarsk Krai; Bugarikta, Nidym or lower Kochechumo Formation (Agitkan Horizon), terminal Permian (Changhsingian) or basal Triassic; paratypes PIN 5382 View Materials /98±, 100±, 101±, 104±, incomplete tegmina (clavus missing), Khungtukun-2, right bank of Nizhnyaya Tunguska R. 4.9 km ESE from mouth of Khungtukun R., Evenkiysky District , Krasnoyarsk Krai; Bugarikta Formation (Khungtukun Horizon [ Sadovnikov, 2015]), terminal Permian (Changhsingian).

DESCRIPTION. Tegmen 12.0– 13.5 mm long, elongate (2.7:1), transversely truncate apically, with distinct apex and tornus (posterior apical angle). Costal margin convex near base, nearly straight (not concave) distally; precostal carina narrow except near base; CP long, strong; bSc long, low arched. R stem arched forwards proximally, as long as RA to dSc. dSc very long, slanting, continuing proximal RA. RA with 2–3 postnodal branches less oblique than dSc; prenodal branches barely visible or absent. RP with small fork. M forked distal to CuA, pectinate backwards, with 3 main branches, M1 with small fork. Basal cell long, closed with arculus. CuA fork long, CuA1 arched forwards, CuA2 joining margin distant from claval apex. Three crossveins. Claval veins widely separated, nearer to sides of clavus; Pcu gently curved, joining margin about 2/3 clavus length. Tegmen entirely covered with fine punctures on upperside (coarser on clavus) and stub-like microtrichia on underside (apparently forming plastron). In costal area near base these microtrichia merge into closely packed microscopic ridges covering elongate oval fingerprint-like area (strigil) about 1.3 x 0.6 mm; ridges more dense in proximal part of strigil (10 per 100 µm) than in its distal part (6.5 per 100 µm) Ambient vein not corrugated; marginal membrane narrow. Tegmen brownish, more so towards base, especially in costal area and on clavus; precostal carina dark brown.

ETYMOLOGY. Latin truncatus (truncated).

R

Departamento de Geologia, Universidad de Chile

Kingdom

Animalia

Phylum

Arthropoda

Class

Insecta

Order

Hemiptera

Family

Dysmorphoptilidae

Genus

Unturella

Loc

Unturella truncata Shcherbakov

Shcherbakov, D. E. 2022
2022
Loc

Unturella truncata Shcherb.

Varganov A. S. & Popova N. N. & Sosnovskaya A. V. & Smokotina I. V. & Glushkov V. M. & Kazhaeva O. D. & Mikryukova L. N. 2015: 127
2015
Loc

Unturella truncata Shcherb.

Kazakov A. M. & Konstantinov A. G. & Kurushin N. I. & Mogutcheva N. K. & Sobolev E. S. & Fradkina A. F. & Yadryonkin A. V. & Devyatov V. P. & Smirnov L. V. 2002: 160
2002
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