A New Sternorrhynchan Genus and Species from the Triassic Period of China That Is Likely Related to Protopsyllidioid (Insecta, Hemiptera)

Simple Summary The new sternorrhynchan Triassopsyllidiida pectinata gen. et sp. nov. is described from the latest Middle Triassic Tongchuan biota of China. The phylogenetic relationships of the Protopsyllidioidea are discussed. Abstract Triassopsyllidiida pectinata gen. et sp. nov. is described from the latest Middle Triassic Tongchuan biota of China and tentatively attributed to the superfamily Protopsyllidioidea. Its forewing venation is unique among this superfamily in the anteriorly pectinate vein ScP + RA and the presence of a veinlet between R and M + CuA. Its exact position in this group remains uncertain, mainly because of the weak diagnostic value of the wing venation characters in these insects. The phylogenetic relationships of the Protopsyllidioidea are discussed.


Introduction
The Protopsyllidioidea Carpenter, 1931, is a group of extinct Psyllaeformia with fossils ranging between the Late Permian and the Late Cretaceous, and is currently subdivided into four families: Postopsyllidiidae Hakim, Azar & Huang, 2019; Permopsyllidiidae Becker-Migdisova, 1985; Protopsyllidiidae Carpenter, 1931; and Paraprotopsyllidiidae Hakim, Azar, Szwedo, Drohojowska & Huang, 2021. After the morphological phylogenetic hypothesis of Hakim et al. [1], the Protopsyllidioidea would be a grade that leads to the modern clade (Psylloidea + Aleyrodomorpha). This hypothesis does not fit with the molecular phylogeny of the Hemiptera proposed by Song et al. [2], who obtained a clade (Psylloidea (Aleyrodoidea (Coccoidea + Aphidoidea))), instead of two clades (Psylloidea + Aleyrodoidea) and (Coccoidea + Aphidoidea) as in Hakim et al. [1]. These last authors have neglected the important character presence versus absence of the crossvein cua-cup between the veins CuA and CuP', an absence shared by all the extant (Psylloidea (Aleyrodoidea (Coccoidea + Aphidoidea))) while it is present in the fossil Protopsyllidioidea (except the Paraprotopsyllidiidae), Archescytinidae, etc. Thus a new morphological analysis is necessary to resolve this contradiction.
Here, we describe a new Triassic fossil that we tentatively attribute to the Protopsyllidioidea. It greatly differs from all the described representatives of this group. As well, it should be helpful for the future phylogenetic analysis of these insects.

Material and Method
Only one specimen, with a part and counterpart, was preserved in the greenish-grey shale of a lacustrine deposit of the Tongchuan biota. It was collected in the lower parts of the Middle-Upper Triassic Yanchang Formation near Hejiafang Village, Jinsuoguan Township, Yintai District, Tongchuan City, Shaanxi Province, northern China (for detailed location of fossil site, see Fu et al. [3]). This layer is the upper section of Ch7 Member of the formation cited as the Tongchuan Formation in most palaeontological studies. The age of the fossil layers are very close to the Middle-Late Triassic boundary [4] and assigned to the latest Ladinian in this paper.
The specimens were carefully prepared using a sharp blade by removing the rock that was covering part of it. Photographs were taken with a Zeiss AxioZoom V16 stereoscope. All images were optimised and grouped into plates using Adobe Photoshop CS6. Line drawings were drafted with Adobe Illustrator CC 2018. The material studied here is deposited in the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, China.

Systematic palaeontology
Triassopsyllidiida pectinata sp. nov. (Figures 1-3) lidioidea. It greatly differs from all the described representatives of this group. As well, i should be helpful for the future phylogenetic analysis of these insects.

Material and Method
Only one specimen, with a part and counterpart, was preserved in the greenish-grey shale of a lacustrine deposit of the Tongchuan biota. It was collected in the lower parts o the Middle-Upper Triassic Yanchang Formation near Hejiafang Village, Jinsuoguan Township, Yintai District, Tongchuan City, Shaanxi Province, northern China (for de tailed location of fossil site, see Fu et al. [3]). This layer is the upper section of Ch7 Membe of the formation cited as the Tongchuan Formation in most palaeontological studies. Th age of the fossil layers are very close to the Middle-Late Triassic boundary [4] and as signed to the latest Ladinian in this paper.
The specimens were carefully prepared using a sharp blade by removing the rock that was covering part of it. Photographs were taken with a Zeiss AxioZoom V16 stereo scope. All images were optimised and grouped into plates using Adobe Photoshop CS6 Line drawings were drafted with Adobe Illustrator CC 2018. The material studied here i deposited in the Nanjing Institute of Geology and Palaeontology, Chinese Academy o Sciences, Nanjing, China.

Systematic palaeontology
Type locality. Latest Middle Jurassic at the locality near the Hejiafang village, Jinsuoguan Township, Tongchuan City, Shaanxi Province, North China; Late Ladinian, Middle Triassic. Holotype. NIGP180297 (part and counterpart of fragmental body with a forewing), stored at Nanjing Institute of Geology and Palaeontology, CAS, Nanjing, China.
Type locality. Latest Middle Jurassic at the locality near the Hejiafang village, Jinsuoguan Township, Tongchuan City, Shaanxi Province, North China; Late Ladinian, Middle Triassic.
Description. Head ovoid-shaped; eyes large, ellipse-shaped; protothorax wider than head; mesothorax wide; legs covered with fine setae, middle legs long and slender, hind legs distinctly longer than middle legs, hind femur robust, tibia much longer than femur ( Figure 1). Forewing (Figures 2 and 3), 3.6 mm long, 1.4 mm wide; no trace of coloration visible; ambient vein present but not very thick; all main veins except CuP with large and robust setae regularly spaced in one row, basal part of wing margin armed with one row of small setae, middle and posterior parts of wing margin gradually become armed with setae; C with small setae; ScA long, with large and robust setae, very close to C and reaching C at beginning of pectinate area of RA + ScP; ScP oblique, appressed to stem of R, joining RA at point of separation between RA and RP; a strong convex vein R + M + CuA, M + CuA emerging 0.6 mm from wing base, RP emerging from R 0.4 mm from base of M + CuA, simple and straight, reaching wing apex; ScP + RA slightly curved, pectinated be- Description. Head ovoid-shaped; eyes large, ellipse-shaped; protothorax wider than head; mesothorax wide; legs covered with fine setae, middle legs long and slender, hind legs distinctly longer than middle legs, hind femur robust, tibia much longer than femur ( Figure 1). Forewing (Figures 2 and 3), 3.6 mm long, 1.4 mm wide; no trace of coloration visible; ambient vein present but not very thick; all main veins except CuP with large and robust setae regularly spaced in one row, basal part of wing margin armed with one row of small setae, middle and posterior parts of wing margin gradually become armed with setae; C with small setae; ScA long, with large and robust setae, very close to C and reaching C at beginning of pectinate area of RA + ScP; ScP oblique, appressed to stem of R, joining RA at point of separation between RA and RP; a strong convex vein R + M + CuA, M + CuA emerging 0.6 mm from wing base, RP emerging from R 0.4 mm from base of M + CuA, simple and straight, reaching wing apex; ScP + RA slightly curved, pectinated before mid-wing, with seven branches, all simple except third with one secondary branching, most basal one (possibly ScP) being slightly stronger than more distal ones; distal stem of M + CuA 0.5 mm long; a short veinlet between R and M + Cu; stem of M 0.9 mm long, separating into MA and MP; MA simple, reaching wing apex; MP posteriorly reg-Insects 2022, 13, 592 5 of 8 ularly pectinate with four branches; stem of CuA 0.5 mm long, with two long branches defining a long and narrow areola postica, CuA2 straight, CuA1 curved; we cannot decipher the presence vs. absence of crossvein cua-cup between CuP and M + CuA, slightly arched, without setae; CuP weakly indicated, concave and straight, declined near its apex; two veins in anal area, distally fused and forming an Y-vein.

Discussion
Among the Permian-Triassic hemipteran groups, only the sternorrhynchan Protopsyllidioidea have all the following characteristics of Triassopsyllidiida gen. nov.: area between C and ScP + R rather narrow; no or very few crossveins, especially in distal half of wing; RP simple; a long stem M + CuA emerging from R + M + CuA; presence of strong setae on all main veins [1].
Drohojowska et al. [6] proposed the following synapomorphies for the Sternorrhyncha: 'rostrum placed in sternal depression', 'mesonotum strongly raised', 'mesoscutum forming two humps', 'veinlet cua-cup at basal cell absent'. The last character state is erroneous because the crossvein cua-cup is clearly present in the Protopsyllidioidea (see [1] Some other fossil families show similarities with Triassopsyllidiida gen. nov., namely the Liadopsyllidae Martynov, 1926, but these have no strong setae on their veins and their vein M has only two distal branches, unlike Triassopsyllidiida gen. nov. [7][8][9]. The Archescytinidae Tillyard, 1926, and the Pincombeidae Tillyard, 1922, have a simple RP, but their M and CuA separate at their common base on R + M + CuA [10,11]. The Dysmorphoptilidae Handlirsch, 1906, also has a simple RP, or it is weakly forked, and a common stem of M with CuA, but they have a broader area between C and ScP + R and a tegmen that is abruptly narrowed distally. None of these groups have strong macrotrichia on their veins [12][13][14][15]. The Permian genus Orthoscytina Tillyard, 1926 (in Prosboloidea, a 'problematic paraphyletic group' in Cicadomorpha, after Szwedo et al. [16]), shares with Triassopsyllidiida gen. nov. the simple RP, M with several branches, and CuA with at least two branches. Even an unnamed specimen figured by Evans [17] has the very particular anteriorly pectinate ScP + RA of Triassopsyllidiida gen. nov., but Orthoscytina strongly differs from Triassopsyllidiida gen. nov. in the very broad area between C and ScP + R, where ScP and R are basally separated and there is the absence of a stem of M + CuA re-emerging from R + M + CuA.
Hakim et al. [1] proposed the following wing venation characters for the Protopsyllidioidea: forewing with stem R branched, ScP developed variously, in some taxa delimiting pterostigma posteriorly (closed pterostigma), or weakened (opened pterostigma); RA and RP always present; stem M fused with stem CuA at base for at least a short distance, M two-, three-, rarely four-branched; CuA forked, areola postica present [but reduced in some taxa, e.g., Angustipsyllidium minutum Hakim, Azar et Huang, 2021], branch CuA2 sometimes weakened; clavus triangular, shortened with two claval veins, or A2 fused with margin. All these characters are present in Triassopsyllidiida gen. nov.
Hakim et al. [1] characterized the venation of the Mesozoic Postopsyllidiidae as follows: forewings setose; pterostigma greatly reduced (sometimes pigmented); vein M three-branched; A1 and A2 present and well developed. Triassopsyllidiida gen. nov. has a M Insects 2022, 13, 592 6 of 8 with five branches, excluding it from this family. Hakim et al. (2019) also gave the following characteristics in their diagnosis of the Protopsyllidiidae: forewing with pterostigma absent (while present in Triassopsyllidiida gen. nov., but also in at least the type genus Protopsyllidium, see Tillyard (1926)), basal cell normally absent; vein M two-branched (unlike Triassopsyllidiida gen. nov., but this difference is more of generic importance than sufficient to discriminate families), vein CuA forked, rarely simple; crossvein rp-m normally absent.
Hakim et al. [1] also proposed the following diagnostic characters for the Permopsyllidiidae: forewings wide and round near apex, narrower at base, no setae on veins or wing margin; when present, vein ScA (?) short; vein R normally branches around mid-length of wing; vein RP arcuate or slightly curved, rarely straight; pterostigma wide, triangular and sometimes darkened; vein M with three or four branches; one or two crossveins rp-m visible; basal cell present in several taxa; anal area wide; veins A1 and A2 connected distally into a Y-shape vein. The Permopsyllidiidae differ from Triassopsyllidiida gen. nov. in the absence of setae on veins and the presence of crossvein(s) between RP and M. The absence versus presence of setae on veins is sometimes hard to determine on fossils, as demonstrated by their bases, which are clearly visible on the imprint of the holotype of Triassopsyllidiida pectinata sp. nov., while they are not detectable on its counter-imprint. Thus, this character remains uncertain. The presence versus absence of crossvein rp-m can be more diagnostic, at least at the genus level, but it is hard to determine its value at the family level and it is not stable in the family.
Triassopsyllidiida gen. nov. differs from all the genera currently in the Protopsyllidioidea in the presence of a series of straight, parallel veinlets between ScP + RA in the distal half of forewing, and the presence of a short veinlet between R and M + CuA [1,[19][20][21][22][23][24][25][26][27][28][29]. Only Triassopsylla Tillyard, 1917, has a ScP re-emerging distally from RA and a distal fork of RA, which is very different from the series of eight veinlets emerging from ScP + RA as in Triassopsyllidiida gen. nov. [30]. One would be tempted to create a new family for Triassopsyllidiida gen. nov. on the basis of this curious character, but such veinlets distally emerging from ScP + RA are also present in some extant species of Psylloidea, e.g., Euphyllura pakistanica Loginova, 1973, while the other representatives of Euphyllura have only two branches of ScP + RA [31]. Thus, this character alone is not sufficient to support a family. Nevertheless, Triassopsyllidiida gen. nov. strongly differs from all genera of the Protopsyllidioidea. The second character, 'presence of a short veinlet between R and M + CuA', is also very unusual among the Protopsyllidioidea, but it would be necessary to find it on further specimens of Triassopsyllidiida gen. nov. to determine if it is stable or not before erecting a new family for Triassopsyllidiida gen. nov.
After the phylogenetic hypothesis of Hakim et al. [29], Triassopsyllidiida gen. nov. would fall in the clade (Postopsyllidiidae (Protopsyllidiidae (Psylloidea + Aleyrodomorpha))) on the basis of the absence of the crossvein rp-m, which is a homoplastic character. These authors did not consider the presence of robust setae on the veins in their analysis, a character present in the Postopsyllidiidae, the Protopsyllidiidae, and the Paraprotopsyllidiidae [1]. It would be necessary to verify the absence of these setae in all the previously described Permopsyllidiidae. These setae are sometimes hardly visible in fossils. The character, 'presence of strong setae on main veins', could be a potential synapomorphy for the clade Protopsyllidioidea.
The exact position of Triassopsyllidiida gen. nov. remains somewhat uncertain because it does not have the putative apomorphy of the Postopsyllidiidae (absence of pterostigma), and neither that of the Protopsyllidiidae (vein M reduced to two branches). The Paraprotopsyllidiidae have a simple median vein. Hakim et al. [29] did not propose any synapomorphy for the Permopsyllidiidae. Triassopsyllidiida gen. nov. does not fit with the diagnoses of the four families Postopsyllidiidae, Protopsyllidiidae, Paraprotopsyllidiidae, and Permop-syllidiidae. The differences in forewing venation between all these families are relatively weak characteristics, rendering their definitions and limits somewhat uncertain, especially for the Permopsyllidiidae that are only based on forewing characters.

Concluding Remarks
The Permopsyllidiidae are currently restricted to the Upper Permian Period of Australia and the Russian Federation, while the Postopsyllidiidae and Paraprotopsyllidiidae are Cretaceous, and the Protopsyllidiidae are known in the Permian of Australia, France, the Russian Federation, and South Africa; the Triassic of South America, Australia, and South Africa; the Jurassic of China, Europe, and Central Asia; and the Cretaceous on nearly all the paleo-continents. These families seem to be very ancient and were probably very widely distributed during the period between the late Permian and the late Cretaceous. While the Protopsyllidioidea survived the Permian-Triassic episode, known as the 'mother of all extinctions', the causes and exact period(s) of their extinctions remain obscure. It is probably not due to competition with some other acercarian groups because they co-habited with the stem groups of the modern sternorrhynchan clades for a long time. A link with the floristic changes of the early Late Cretaceous could also be unlikely, as the youngest representatives are known in the Raritan amber (Turonian). They possibly became extinct during the period between the Turonian and the Maastrichtian, when the 'Angiosperm Terrestrial Revolution' was at its maximum [32], or at the very end of the Cretaceous, as for the Odonata Aeschnidiidae, which was very recently described from the latest Maastrichtian [33]. Unfortunately, the current knowledge on the entomofaunas from this crucial period is very fragmentary.

Data Availability Statement:
The data presented in this study are available in the article.