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Article

The Imitation Game: In Search for Brachycera in the Triassic

by
Elena D. Lukashevich
1,* and
Mike B. Mostovski
2,3
1
Borissiak Paleontological Institute, Russian Academy of Sciences, Moscow 117647, Russia
2
The Steinhardt Museum of Natural History, Tel Aviv University, Tel Aviv 69978, Israel
3
School of Agricultural, Earth and Environmental Sciences, University of KwaZulu-Natal, Private Bag X54001, Durban 4000, South Africa
*
Author to whom correspondence should be addressed.
Submission received: 17 July 2023 / Revised: 28 August 2023 / Accepted: 29 August 2023 / Published: 2 September 2023
(This article belongs to the Special Issue Diversity of Fossil and Recent Insect Faunae)

Abstract

:
The richest assemblage of the Triassic Diptera has been described from the famous Konservat-Lagerstätte Grès à Voltzia (Upper Buntsandstein) in the northern Vosges Mountains in France, dated as Early Anisian. A re-examination of the holotypes and additional material from the type locality allows for the establishment of Vogerhyphus gen. nov. and erection of the Vogerhyphinae subfam. nov. for Vymrhyphus blagoderovi Krzemiński and Krzemińska, 2003 and Vogerhyphus krzeminskorum sp. nov. (Protorhyphidae), and a new monotypic family Galliidae fam. nov. for Gallia alsatica Krzemiński and Krzemińska, 2003, originally described as Rhagionidae based on its wing venation. Galliidae fam. nov. is characterized by its closed cua cell and long moniliform antenna with 14-segmented flagellum and is hypothesized to belong to the stem-group Brachycera, along with the Late Triassic Prosechamyiidae. The process of brachycerization in the Diptera evolution is briefly discussed.

1. Introduction

The oldest fossil Diptera come from the Anisian deposits in Spain, Germany and France [1,2,3]. The richest Triassic assemblage of Diptera has been described from the famous Konservat-Lagerstätte Grès à Voltzia (Upper Buntsandstein) of the northern Vosges Mountains in France (hereinafter referred to as the Vosges), dated as Bithynian, about 245 Ma. For outcrops of the Vosges, a deltaic area is reconstructed, a transitional environment ranging from nearshore to terrestrial, with unstable and occasionally hash conditions, and numerous shallow drying pools [4,5]. The assemblage from the Vosges comprises about 70 adults, 30 pupae and 3 larvae [6] representing Nematocera of the infraorders Tipulomorpha, Psychodomorpha sensu Hennig, Culicomorpha and Bibionomorpha, as well as Brachycera. The very first dipteran described from these beds was Grauvogelia arzvilleriana Krzemiński, Krzemińska and Papier 1994, based on numerous well-preserved isolated wings [1]. Krzemiński and Krzemińska [7] added another five species (four of them in new genera), each based on a single adult specimen: Louisa nova Krzemiński and Krzemińska, 2003 (Grauvogeliidae), Tanus triassicus Krzemiński and Krzemińska, 2003 (Nadipteridae), Archilimonia vogesiana Krzemiński and Krzemińska, 2003 (Archilimoniidae), Vymrhyphus blagoderovi Krzemiński and Krzemińska, 2003 (Protorhyphidae), and Gallia alsatica Krzemiński and Krzemińska, 2003 (Rhagionidae). The type of A. vogesiana was revised as a member of the Limoniidae and a second species, A. grauvogeliana Lukashevich and Ribeiro, 2019, was described from the Vosges [8]. Recently, the holotype of T. triassicus was re-examined, some details of the wing venation were clarified, and photographs were published for the first time [2].
The present paper deals with some undescribed adult Diptera from the Vosges, also collected by Louis Grauvogel in the middle of the 20th century [9]. The holotypes of Vymrhyphus blagoderovi and Gallia alsatica were re-examined by EDL in 2008, and their photographs are published herein for the first time.
It was already suggested that Vymrhyphus blagoderovi from the Vosges belongs in a separate genus, although no new name was proposed at the time [10]. In a key to the genera of the Protorhyphidae [11], this species was also separated from its congeners. A re-examination of the holotype and additional material from the type locality allows us to establish a new genus in a new subfamily for this peculiar taxon.
For twenty years after the description of Gallia alsatica, no additional Rhagionidae and only one other brachyceran genus was described as a member of the monotypic Pro-sechamyiidae [10] from Triassic deposits. Thus, Brachycera have been (expectedly) extremely rare in the Triassic fossil record, with only the three described specimens. Additional Gallia specimens from the Vosges and re-examination of the holotype of G. alsatica prompts the erection of a new family for this unusual genus based on characteristics other than wing venation.

2. Material and Methods

Several thousands of insects are known from 13 localities in the northern Vosges from the lowermost unit of ‘Grès à Voltzia’ Formation, which is part of the Upper Buntsandstein, dating to the early Anisian [12]. All the specimens discussed below were found in Arzviller (Moselle department), as well as some other 80 dipterans from the Vosges, from the same lens 118b, intercalated within fluviatile sandstones [13]. The material had been housed in the private collection of Léa Grauvogel-Stamm, Strasbourg, France, for many years, until 2017, when these fossils were transferred to the Staatliches Museum für Naturkunde, Stuttgart, Germany (SMNS). In our paper, SMNS accession numbers are used. In earlier publications dealing with this material [2,7,8], accession numbers from different collections (where material was housed previously) were published—herein, they are given in brackets, e.g., SMNS-P-75643-1 (No. 9077). Parts and counterparts are specified with a slash, e.g., SMNS-P-7543-2/3, unless otherwise stated.
The specimens were photographed using a Leica MZ9.5 stereomicroscope with a Leica DFC420 digital camera, and the images were edited using Adobe Photoshop CS 9.0 software. The orientation of the published photographs reflects the actual position of the specimens, whereas line drawings are flipped for ease of comparison.
The wing vein terminology used in this study follows that of Shcherbakov et al. [14] and Mostovski et al. [15]. The anal cell auct. is accepted here as cua.

3. Results

Infraorder Bibionomorpha.
Family Protorhyphidae Handlirsch, 1906.
Subfamily Protorhyphinae Handlirsch, 1906.
Type genus: Protorhyphus Handlirsch, 1906 (Dobbertin, Germany, J1).
Diagnosis: Sc moderate or short with apex near or before wing midlength; crossvein r-m connecting R4+5 and M1+2 stems; basal part of M thin, desclerotized; discal cell near wing midlength; M1+2 fork longer than M3+4 fork; Rs origin at 0.17–0.33, M forking at 0.33–0.44, CuA apex at 0.44–0.56 wing length; A1 short.
Composition: In addition to the type genus, Archirhyphus Handlirsch, 1939, Vymrhyphus Blagoderov, 1995, Brachyrhyphus Blagoderov and Grimaldi, 2007, and Austrorhyphus Martin, 2008 from the Mesozoic of Eurasia, North America and Australia.
Subfamily Vogerhyphinae subfam. nov.
LSID: urn:lsid:zoobank.org:act:79A864ED-5560-46B6-9EB8-B65214B53568.
Type genus: Vogerhyphus gen. nov. (Vosges, France, Tr2).
Diagnosis: Sc long, with apex beyond wing midlength; crossvein r-m connecting M1+2 stem with R5 base; basal part of M obvious; discal cell beyond wing midlength; M3+4 fork longer than M1+2 fork; Rs origin at 0.4, M forking at 0.5, CuA apex at 0.65 of wing length; A1 relatively long and wavy, not reaching wing margin.
Comparison: The new subfamily differs from Protorhyphinae in having a longer Sc, the position of r-m connecting M1+2 stem with the R5 base, the position of the discal cell in the distal half of the wing, and a relatively shorter M1+2 fork.
Composition: The type genus.
Vogerhyphus gen. nov.
Vymrhyphus Blagoderov, 1995 (partim).
LSID: urn:lsid:zoobank.org:act:B3C86E29-69DF-40EE-A7F9-55C463118ADC.
Type species: Vymrhyphus blagoderovi Krzemiński and Krzemińska, 2003 (Vosges, France, Tr2).
Etymology: From Vosges Mountains.
Diagnosis: Wing elongated, 3× longer than wide. Sc long, extending beyond wing midlength, with its apex near or beyond r-m level. C ending slightly beyond R5 apex; all radial veins nearly straight and subparallell for most of their length. R1 straight and long (0.75–0.85 of total wing length). R4+5 forking level to discal cell midlength. R4+5 stem short, Rs stem 2–2.5× as long as R4+5 stem, R4 5–8× as long as R4+5 stem. R5 not arched forwards, ending at wing apex, R4+5 fork 1.7–1.8× as long as M1+2 fork, r-m connecting R5 near base and discal cell midlength. Basal part of M sclerotized, aligned with M1+2; M3+4 forking near ⅓ discal cell length, bas M4 (before m-cu) extremely short. CuA subparallel to CuP or converging but not meeting. Anal lobe developed.
Remarks: Vogerhyphus gen. nov. has a long R1 (0.75–0.85 of total wing length). In most previously known protorhyphid genera, R1 is shorter (0.55–0.65 of total wing length), with the exception of Vymrhyphus (0.67–0.76, EDL unpubl. data) and Austrorhyphus (0.8) [11].
Species included: In addition to the type species, Vogerhyphus krzeminskorum sp. nov. (Vosges, France, Tr2).
Vogerhyphus blagoderovi (Krzemiński and Krzemińska, 2003) comb. nov.
Vymrhyphus blagoderovi Krzemiński and Krzemińska, 2003 [7] (p. 173, Figure 11).
Holotype: SMNS-P-75643-1± (No. 9077±), part and counterpart of isolated wing; Arzviller (lens 118b), Grès à Voltzia (Upper Buntsandstein; Bithynian, Anisian), Vosges Mountains, France.
Description: Wing length 4.2 mm. Sc 0.65 of total wing length; R1 about 0.85 of total wing length, with apex level with M2 apex; Rs stem almost straight, twice as long as R4+5 stem; R4 5× as long as R4+5 stem; discal cell 0.2 of total wing length; CuA with bend at m-cu, CuA and CuP converging but not meeting.
Remarks: The wing between CuA and CuP apices is crumpled, so the degree of vein proximity can be exaggerated.
Vogerhyphus krzeminskorum sp. nov.
(Figure 1b,c and Figure 2b).
LSID: urn:lsid:zoobank.org:act:2ADDE176-6FA9-41FB-ABCB-88AC50EB61CD.
Etymology: After Ewa and Wieslaw Krzemińskis, authors of numerous taxa from the Vosges.
Figure 1. Vogerhyphus, gen. nov., photograps. (a) V. blagoderovi (Krzemiński and Krzemińska, 2003) comb. nov., holotype; (b,c) V. krzeminskorum sp. nov., holotype: wing, part; total habitus, counterpart. Scale bars 0.5 mm.
Figure 1. Vogerhyphus, gen. nov., photograps. (a) V. blagoderovi (Krzemiński and Krzemińska, 2003) comb. nov., holotype; (b,c) V. krzeminskorum sp. nov., holotype: wing, part; total habitus, counterpart. Scale bars 0.5 mm.
Diversity 15 00989 g001
Holotype: SMNS-P-75643-2/3 (No. 5914/5915), part and counterpart of incomplete imago (thorax and both wings preserved); Arzviller (lens 118b), Grès à Voltzia (Upper Buntsandstein; Bithynian, Anisian), Vosges Mountains, France.
Figure 2. Wings of Vogerhyphus, gen. nov., line figures. (a) V. blagoderovi (Krzemiński and Krzemińska, 2003) comb. nov., holotype; (b) V. krzeminskorum sp. nov., holotype. Scale bars 1 mm.
Figure 2. Wings of Vogerhyphus, gen. nov., line figures. (a) V. blagoderovi (Krzemiński and Krzemińska, 2003) comb. nov., holotype; (b) V. krzeminskorum sp. nov., holotype. Scale bars 1 mm.
Diversity 15 00989 g002
Description: Wing length 2.7 mm. Sc 0.58 of total wing length; R1 about 0.75 of total wing length, with apex level with M3 apex; Rs stem curved, 2.5× as long as R4+5 stem; R4 8× length of R4+5 stem; discal cell 0.17 of total wing length. CuA and CuP subparallel.
Remarks: The new species differs from the type species in the pattern of the cubital veins. The difference in the wing size is considered insignificant. A similar degree of variation has been noted in species of other genera based on numerous isolated wings (Protorhyphus simplex Handlirsch, 1906, P. rohdendorphi Lukashevich, 2012, and Archirhyphus asiaticus Rohdendorf, 1964) [16,17].
The thorax may bear a V-suture, but the state of the material preservation does not allow us to claim this with certainty.
Stem-group Brachycera.
Family Galliidae fam. nov.
LSID: urn:lsid:zoobank.org:act:97047E36-9C8F-47C6-8FA0-99351508F70D.
Type genus: Gallia Krzemiński and Krzemińska, 2003 (Vosges, France, Tr2).
Composition: The type genus.
Diagnosis: Antenna long, moniliform, with over 10 more or less uniform segments; short scape and pedicel subequal; first flagellomere likely to be rounded in cross-section, not differing from subsequent flagellomeres; all flagellomeres roughly as long as wide except for 4 apical ones that are slightly elongated. Rs forking beyond M fork, before r-m and before or level with Sc apex; R1 and R2+3 not converging or diverging at wing margin; R4+5 forking noticeably proximad of R1 apex and of distal end of discal cell; R4+5 fork much longer than R4+5 stem; R4+5 fork fairly symmetrical, so Rs, R4+5 and R5 do not form a straight line; R4 nearly straight at base and straight apically; R5 ending near wing tip; M3 reaching wing margin; M3 after im and M4 (sub)parallel; m-cu joining CuA well beyond its midlength; CuA angled at m-cu; CuA and CuP meeting at wing margin or cell cua with very short petiole.
Comparison: The new family differs from almost all other dipteran families with the closed cua cell (anal cell in older terminology) in having a long moniliform antenna with more than eight-segmented flagellum; from the Prosechamyiidae (also with moniliform antenna) in R4+5 forking distad of r-m, in having all four branches of vein M, closed discal cell and cell cua at most with short petiole; and from the Rachiceridae (with more than eight-segmented flagellum) in having non-converging R1 and R2+3, R4+5 fork proximad of R1 apex and (sub)parallel M3 and M4.
Remarks: The thorax may bear a V-suture, but the state of the material preservation does not allow us to claim this with certainty.
Gallia Krzemiński and Krzemińska, 2003.
Diagnosis: Small flies (wing length about 3 mm). Antenna with 16 segments. Sc ending beyond wing midlength; R1 long, ending far beyond M1+2 furcation; Rs stem as long as or noticeably longer than R4+5; R2+3 noticable longer than Rs stem, R4+5 fork much longer than its stem; M1+2 forking beyond im; m-cu at or just after M3+4 furcation. Abdomen elongate, longer than wing at least in presumptive female, male terminalia not wider than preceding abdominal tergite (Figure 3, Figure 4d,e, Figure 5c and Figure 6a,d).
Gallia alsatica Krzemiński and Krzemińska, 2003.
Gallia alsatica Krzemiński and Krzemińska, 2003 [7] (p. 177, Figure 14).
Holotype. SMNS-P-75643-8/9 (No 6170/6171), part and counterpart of male; Arzviller (lens 118b), Grès à Voltzia (Upper Buntsandstein; Bithynian, Anisian), Vosges Mountains, France.
Figure 4. Details of Gallia alsatica Krzemiński and Krzemińska, 2003, holotype, male, photographs. (a) Right wing, counterpart; (b) left wing, part; (c) head with eye and antenna; (d,e) abdominal apex, part and counterpart. Scale bars 0.5 mm.
Figure 4. Details of Gallia alsatica Krzemiński and Krzemińska, 2003, holotype, male, photographs. (a) Right wing, counterpart; (b) left wing, part; (c) head with eye and antenna; (d,e) abdominal apex, part and counterpart. Scale bars 0.5 mm.
Diversity 15 00989 g004
Figure 5. Details of Gallia alsatica Krzemiński and Krzemińska, 2003, holotype, male, line figures. (a,b) Right and left wings; (c) abdominal apex; (d) eye and antenna. Scale bars 0.5 mm.
Figure 5. Details of Gallia alsatica Krzemiński and Krzemińska, 2003, holotype, male, line figures. (a,b) Right and left wings; (c) abdominal apex; (d) eye and antenna. Scale bars 0.5 mm.
Diversity 15 00989 g005
Additional material: SMNS-P-75643-4/5a (No. 6176a/6177a), possibly female, part and counterpart; SMNS-P-75643-4/5b (No. 6176b/6177b), thorax with two wings, part and counterpart, on one slab with SMNS-P-75643-4/5a; SMNS-P-75643-6/7 (No. 6178/6179), possibly female, part and counterpart; probably from the same slab as SMNS-P-75643-4/5 (the rock is glued on one piece of paper). All additional specimens are from the same lens as holotype.
Description: Head wider than thorax (Figure 6b,d and Figure 7c,d). Eyes large, dichoptic in male, not flattened dorsally, without conspicuous microsetae, facets of male evenly distributed and of equal size (Figure 4c and Figure 5d). Antenna 1.7× longer than head width, with short scape and pedicel of approximately the same size and elongate flagellum, with 14 ovoid flagellomeres, gradually slightly tapered toward apex (Figure 6b–e and Figure 7c,d). Wing moderately long, without distinct colour pattern. Wing venation (Figure 4a,b, Figure 5a,b and Figure 7a,b,c,e): Sc exceeding 0.54–0.57 wing length; arculus present; R1 exceeding 0.75–0.77 wing length; Rs origin at 0.39–0.4 wing length; costal section Sc–R1 clearly longer than R1–R2+3; Rs stem 2.2–3.1× as long as R4+5 stem in holotype and subequal or 1.5× in other specimens; R2+3 nearly straight, ending at C not near R1, 2.0–2.6× in holotype as long as Rs stem and 2.5–3.3× in other specimens; r-m dividing R4+5 stem as 1:1–2; discal cell 0.17–0.20 of wing length; basal portion of M1+2 4.5–5.2× as long as M1+2 after im in holotype and 6–10× in other specimens; M3+4 fork subequal or 1.2–1.3× as long as M1+2 fork; m-cu 3–4× as long as basal portion of M4 or basal portion absent. Abdomen about as wide as thorax, anterior five tergites virtually parallel-sided, posterior tergites slightly conically tapered; abdomen and male terminalia pubescent (Figure 3, Figure 4e and Figure 6a,d); aedeagal sheath probably with two stout curved apical hooks (Figure 4d and Figure 5c).
Measurements, mm: Holotype, male: body length 4.4; wing length 3.0, wing width 1.0; head width 0.7; preserved part of antenna 0.5. Additional specimens: body length, 3.8–3.9; wing length 1.9–2.4, wing width 0.7–0.9; head width 0.5–0.6; antenna length 0.9.
Remarks: In the holotype, only a short proximal portion of the antenna is visible—six more or less uniform flagellomeres—but its distal portion is poorly traceable, being obscured by a conchostracan carapace, so its complete length and the exact number and shape of flagellomeres are unknown (Figure 4c and Figure 5d). The variability in the wing venation of male is recorded based on the two wings of the holotype (Figure 3, Figure 4a,b and Figure 5a,b). Variability in the wing venation of additional specimens—m-cu position at or just behind M3+4 furcation, as well as ratio of the Rs stem/R4+5 stem 1.0–1.5× and the basal portion of M1+2 6–10× as long as petiole—are found in two wings of one specimen SMNS-P-75643-4/5b (Figure 6f and Figure 7a,b).
Figure 6. Gallia alsatica Krzemiński and Krzemińska, 2003, photographs. (ac) SMNS-P-75643-4/5a, possibly female, total habitus, part and counterpart, head with antenna; (d,e) SMNS-P-75643-7, possibly female, total habitus, head with antennae; (f) SMNS-P-75643-4/5b, thorax with wings. Scale bars (a,b,d) 1 mm; (c,e,f) 0.5 mm.
Figure 6. Gallia alsatica Krzemiński and Krzemińska, 2003, photographs. (ac) SMNS-P-75643-4/5a, possibly female, total habitus, part and counterpart, head with antenna; (d,e) SMNS-P-75643-7, possibly female, total habitus, head with antennae; (f) SMNS-P-75643-4/5b, thorax with wings. Scale bars (a,b,d) 1 mm; (c,e,f) 0.5 mm.
Diversity 15 00989 g006
Figure 7. Gallia alsatica Krzemiński and Krzemińska, 2003, line figures. (a,b) SMNS-P-75643-4b, left and right wings; (c) SMNS-P-75643-7, possibly female, head with antennae, thorax and wing; (d,e) SMNS-P-75643-4a, possibly female, head with antenna and thorax, wing. Scale bars 0.5 mm.
Figure 7. Gallia alsatica Krzemiński and Krzemińska, 2003, line figures. (a,b) SMNS-P-75643-4b, left and right wings; (c) SMNS-P-75643-7, possibly female, head with antennae, thorax and wing; (d,e) SMNS-P-75643-4a, possibly female, head with antenna and thorax, wing. Scale bars 0.5 mm.
Diversity 15 00989 g007

4. Discussion and Conclusions

4.1. Affinities of Vogerhyphus

As demonstrated previously [8,14], Rs and M forks are usually shorter (with Rs origin and discal cell in the distal half of the wing) in the Triassic Tipulomorpha, so some characteristics of Vogerhyphus gen. nov. are tipulomorph. However, it is clear now that such tipulomorph proportions were common in Triassic members of Psychodomorpha, and no single proportion is sufficient to separate infraorders of Nematocera [2,18]. Therefore, the new subfamily possesses some peculiarities shared with Tipulomorpha and Psychodomorpha but it is attributed to the Mesozoic bibionomorph Prothorhyphidae based on the combination of the long but incomplete A1, Rs pattern, M stem aligned with M1+2, and m-cu position, whereas in extinct and living Anisopodidae, only the Rs pattern with three branches is distinct [19]. The M4 bend on m-cu with an extremely short basal portion of M4 is also known in extinct Hennigmatidae and extinct and extant Tanyderidae (Psychodomorpha sensu Hennig [20]), as well as r-m connecting the R5 base; however, the combination of three Rs veins (with long unbranched R2+3 not forming a stalk with R4) and m-cu position is known only in the Prothorhyphidae.
In V. blagoderovi, CuA and CuP are clearly converging (but not meeting), so its brachyceran affinity cannot be entirely ruled out. In Brachycera, a similar pattern of media has been well-known to occur since the Triassic (Gallia alsatica); sometimes, the long A1 is incomplete and cell cua is open. However, if CuA and CuP are converging but not meeting, as in some Rhagionidae and Bombyliidae, then the cross-vein r-m never connects at the R5 base.
It is worth mentioning that in the Triassic stem-group of Brachycera, Prosechamyia Blagoderov and Grimaldi, 2007 from the Norian Cow Branch Formation of North America, veins of the radial sector are nearly straight and subparallel for most of their length. In addition, the R4+5 stem is short and r-m connects the M1+2 stem with the R5 base, while the basal part of M is obvious and M is forking in the distal half of the wing [10], as in Vogerhyphus gen. nov. However, other characters of Prosechamyia are apomorphic: Sc and R1 are shorter, the discal cell is absent, at least one or even two medial branches are lacking and cell cua is petiolate. Therefore, the protorhyphid affinity of Vogerhyphus gen. nov. seems to be more plausible at present.

4.2. Affinities of Gallia

The genus Gallia was described as the oldest member of the Rhagionidae based only on its wing venation [7], with other features being left out of the discussion due to their unsatisfactory state of preservation in the only holotype.
The Rhagionidae are accepted as the basalmost—in both their morphology and their appearance in the fossil record—members of the Brachycera, with very few reliable adult synapomorphies [21,22]. Grimaldi and Cumming [23] suggested that the position of the R4+5 fork is at the same level as the distal end of discal cell (and not distal to it) and the shape of R4 (with a sharp bend at its base) and R5 (straight) may work as synapomorphies for the majority of the Rhagionidae, but these characters demonstrate inter- and intrageneric variations [22]. Stuckenberg [21] considered R2+3 with a distinct albeit moderate curvature beneath the stigma as one of autopomorphies of the Rhagionidae s.str. (i.e., after the exclusion of Austroleptidae and Spaniidae); other autapomorphies are in the female postabdomen and are generally unobservable in fossils. He also mentioned R4 and R5 enclosing the wing apex as an additional character for the family, but this also occurs in the Athericidae and Tabanidae. Shcherbakov et al. [14] used another set of characters for the Rhagionidae and Xylophagidae s.l. (including Protobrachyceron Handlirsch, 1920) when they discussed the systematic position of the Late Triassic Alinkidae: (1) Rs originating well before the M fork; (2) Rs forking level with the M fork; (3) Rs not aligned with R4+5 and bent at r-m; (4) cell r3 at least as broad as r5; and (5) m-cu joining CuA far beyond its midlength and M3+4 close to M3+4 fork, or M4. However, these characters cannot be considered autapomorphies or synapomorphies of the Rhagionidae and Xylophagidae, for they are also found, either isolated or in combination, in the Protorhyphidae or other nematoceran taxa.
Although the inclusion of Gallia in the Rhagionidae was somewhat acceptable at the time of its original description, its actual existence among the snipe flies seems contentious in light of information derived from the wing venation. In this Triassic genus (Figure 5a,b), R2+3 has no curvature beneath R4, the R4+5 fork is noticeably proximal to the distal end of discal cell, R4 has no sharp bend at its base but is instead gently curved, and R5 does not actually form a continuous line with the R4+5 stem (and Rs). Thus, none of the presumed rhagionid apomorphies are found in the wing venation of Gallia. It should be noted that some Early Jurassic genera described from isolated wings were attributed to the Rhagionidae despite having a straight R2+3. These are Grimmyia Ansorge, 1996 [16], Liassobrachyceron Krzemiński and Ansorge, 2005 [24] and Taschigatra Mostovski and Jarzembowski, 2000 [25]. The last genus was placed into the Rhagionidae not without some doubt, and all three may actually belong in the Xylophagidae, along with Early–Late Jurassic Protobrachyceron, whose species are known from both wings (Germany, J1 [26,27]) and complete bodies (China, J2 [28]), including stylate antennae (Kazakhstan, J2–J3; MBM unpubl. data).
The genus displays another peculiarity by having the im crossvein proximal of the M1+2 fork. A similarly stalked M1+2 fork crops out in several extant and extinct genera of the Rhagionoidea sensu Kerr [22]—Alloleptis Nagatomi and Saigusa, 1982 (Recent), Omphalophora Becker, 1900 (Recent), Paleochrysopilus Grimaldi and Cumming, 1999 (Lebanese amber, K1 [23]) and Ptiolinites Kovalev, 1986 (Mongolia, Russia, Spain, UK, K1 [29,30])—as well as in quite a few extinct and extant representatives of nematoceran and brachyceran families, e.g., Apystomyiidae, Cramptonomyiidae, Empididae, Limoniidae, Nadipteridae, Protorhyphidae, Ptychopteridae, Rhagionemestriidae, Uranorhagionidae etc., so this character is not unique to the snipe flies.
A re-examination of the holotype and the discovery of additional specimens of G. alsatica in the Grauvogel’s collection further complicated the conundrum of the systematic position of the genus Gallia. The holotype of G. alsatica demonstrated structures adjacent to the head that can be interpreted as six subequal segments of the flagellum, which distal part is hidden under a conchostracan carapace (Figure 3a, Figure 4c and Figure 5d). Two additional specimens (possibly females) with nearly identical wing venation compared to the holotype, have long moniliform antennae with 16 almost uniform segments preserved in one of them (Figure 6b–e and Figure 7c,d). Such antennae with a small and subequal scape and pedicel and 14 more or less uniform flagellomeres are unknown in virtually any Brachycera, whose fundamental distinguishing characteristic is an antenna with a maximum of eight flagellomeres [31].
Hennig [32] proposed that a distinct separation of the first flagellomere from the rest of the flagellum could be a synapomorphy for the Rhagionidae, whereas Stuckenberg [31] saw the progressive fusion of flagellomeres into an enlarged flagellar base as a synapomorphy of all Brachycera. In the Stratiomyidae, the unfused basal segments of the flagellum may form a morphologically compact unit that looks like a single stoutly rounded segment [33]. However, there is no rule without an exception. The members of the family Rachiceridae possess from 14 to up to over 30 flagellomeres in a pectinate, serrate or moniliform antenna [34], but the Rachiceridae have a far more advanced wing venation compared to Galliidae, with a strongly curved R1, much shorter fork R4+5 and closed m3 cell. On the other hand, similar antennal structures appear in some Nematocera. The antenna of the bibionomorph Burmazelmira aristica Grimaldi, Amorim and Blagoderov, 2003 (Archizelmiridae; Myanmar, K2) has a 12-segmented structure [35] (p. 379, Figures 10-2, 10-3) that superficially resembles the enlarged first segment of the postpedicel in the Stratiomyidae. The differentiation of flagellomeres in this and two other genera of the Archizelmiridae was one of the reasons why they were placed in a separate subfamily Burmazelmirinae [36]. Further examples of brachycera-type antenna are provided by Burmahesperinus Ševčík, Skartveit, Krzemiński and Skibińska, 2021 (Bibionidae [37]), also from the Cretaceous amber of Myanmar. Two species of this bibionid genus have 10–12-segmented flagella with enlarged basal flagellomeres, one species has a 12-segmented flagellum with a slightly enlarged basal segment but greatly swollen pedicel, and the fourth species has a 6-segmented flagellum with a terminal bristle and an enlarged basal part formed by two closely attached but unfused segments. The Late Triassic Alinka cara Krzemiński, 1992—originally described as Brachycera in a family of its own [38]—has a 10-segmented antenna, but its submoniliform flagellum is more consistent with nematoceran affinities of the genus, and it is now considered a member of Procramptonomyiidae [10,14,31].
With its moniliform antenna comprising 14 practically uniform flagellomeres, G. alsatica not only completely ruins the feeble integrity of the Rhagionidae if added to the family, but also does not fit into the Brachycera altogether. The only taxa with a brachycera-type wing venation (i.e., closed cua cell) that might have antennae resembling those of G. alsatica are Prosechamyia dimedia Blagoderov and Grimaldi, 2007 and, to some extent, Prosechamyia trimedia Blagoderov and Grimaldi, 2007 (Prosechamyiidae) from the Norian of the USA [10]. Regrettably, the antennae are incompletely preserved in both prosechamyiids, which were left unassigned as the stem-group for all Brachycera based on a unique combination of wing and antennal characters. We are tempted to follow suit, but would like to emphasize the possible affinity of the Galliidae with Protorhyphidae, with the latter being thought of as ancestral to the Brachycera [14,39]. Veins CuA and CuP demonstrate a trend towards convergence in some Protorhyphidae, e.g., in Vogerhyphus gen. nov., yet cell cua remains open in protorhyphids.
The progressive changes in the dipteran antenna towards a reduction in the number of segments and, more importantly, towards the differentiation of flagellomeres bearing chemo- and mechanoreceptors, is a pivotal point in the evolution of the order during the Triassic and Jurassic [31], probably more important than the closure of the cua cell, which may be linked to the geometry of the wing. Stuckenberg [31] hypothesized that the origin of the Brachycera was prompted by a new feeding mode, which manifested in the concomitant appearance of the modified antenna and enlarged labella, like those in, for example, Jurassic Paleobrachyceron Kovalev, 1981 (Russia, J1–J2 [40]), Palaeoarthroteles mesozoicus Kovalev and Mostovski, 1997 (Russia, J3 [41]), Protorhagio karataviensis Mostovski, 2008 and Protorhagio ponomarenkoi Mostovski, 2008 (Kazakhstan, J2–J3 [42]). A discovery of two archizelmirids [35]—Zelmiarcha lebanensis Grimaldi, Amorim and Blagoderov, 2003 (Lebanon, K1), with unmodified flagellum and small labella, and Burmazelmira aristica Grimaldi, Amorim and Blagoderov, 2003 (Myanmar, K2), with heavily modified flagellum and enlarged labella (see above)—supports Stuckenberg’s hypothesis of the concurrent appearance of the two characters, but also shows that such a trait might have appeared in a group unrelated to the Brachycera. Labandeira [43,44] noted that the early Mesozoic was the time when one of the major diversifications of insect—and Diptera in particular—mouthparts happened.
Budd and Jensen [45] and Stuckenberg [21] highlighted that the last common ancestor of any two clades cannot have the body plan of either of them and may not be readily recognizable in the palaeontological record. In other words, the clades split before they could be recorded as fossils. The two characters—the closed cua cell and the eight-segmented antennal flagellum with differentiated basal flagellomeres—that unite the Brachycera, did not appear simultaneously in the stem group comprising Prosechamyiidae and Galliidae, but developed separately in time. Moreover, other ‘attempts’ to develop ‘brachyceran’ lineages based on a similar modification of the antennae cropped out in the Cretaceous members of the families Archizelmiridae [35] and Bibionidae [37]. This process can be called brachycerization, akin to other ‘-izations’ (e.g., arthropodization, tetrapodization, reptilization, ornithization, angiospermization, etc.), which resulted in major evolutionary changes [46].
Both Prosechamyiidae and Galliidae probably belonged to a group that can be jokingly (and oxymoronically) dubbed nematocerous brachycerans, whose representatives with eight-segmented flagellum and differentiated basal flagellomeres will never be found, for they would be seen as the true Brachycera.

Author Contributions

Conceptualization, E.D.L.; methodology, E.D.L.; analysis of data, E.D.L. and M.B.M.; writing—original draft preparation E.D.L. and M.B.M.; graphics, E.D.L.; writing—review and editing, E.D.L. and M.B.M.; funding acquisition, E.D.L. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by the Russian Science Foundation, grant number 21-14-00284.

Institutional Review Board Statement

Not applicable.

Data Availability Statement

No shareable research data were generated in this research.

Acknowledgments

EDL is deeply indebted to Léa Grauvogel-Stamm for the great opportunity to work with material collected by her father Louis Grauvogel and for the hospitality during EDL’s visit to Strasbourg in 2008. The late Francine Marshal-Papier helped to work with the Vosges collection. EDL is grateful to Dmitry Shcherbakov (Borissiak Paleontological Institute RAS, Moscow) for taking photographs of the Vosges specimens and informal support during their visit to Strasbourg in 2008. We thank two anonymous reviewers for providing constructive comments.

Conflicts of Interest

The authors declare no conflict of interest.

References

  1. Krzemiński, W.; Krzemińska, E.; Papier, F. Grauvogelia arzvilleriana sp. n.—The oldest Diptera species (Lower/Middle Triassic of France). Acta Zool. Cracov. 1994, 37, 95–99. [Google Scholar]
  2. Lukashevich, E.D. The oldest Diptera (Insecta) from the Upper Buntsandstein (early Middle Triassic) of Europe. Zootaxa 2021, 5067, 135–143. [Google Scholar] [CrossRef] [PubMed]
  3. Peñalver, E.; Matamales-Andreu, R.; Nel, A.; Pérez-de la Fuente, R. Early adaptation of true flies (Diptera) to moist and continental environments. Pap. Palaeontol. 2022, 8, e1472. [Google Scholar] [CrossRef]
  4. Gall, J.C. Faunes et paysages du Grès à Voltzia du Nord des Vosges. Essai paléoécologique sur le Buntsandstein supérieur. Mém. Serv. Cart. Geol. Als. Lorr. 1971, 34, 1–318. Available online: https://www.persee.fr/doc/sgeol_0080-9020_1971_mon_34_1 (accessed on 1 September 2023).
  5. Selden, P.; Nudds, J. Evolution of Fossil Ecosystems, 2nd ed.; Elsevier: Amsterdam, The Netherlands, 2012; 288p. [Google Scholar]
  6. Lukashevich, E.D. Where the immatures of Triassic Diptera developed. Diversity 2023, 15, 582. [Google Scholar] [CrossRef]
  7. Krzemiński, W.; Krzemińska, E. Triassic Diptera: Descriptions, revisions and phylogenetic relations. Acta Zool. Cracov. 2003, 46, 153–184. [Google Scholar]
  8. Lukashevich, E.D.; Ribeiro, G.C. Mesozoic fossils and the phylogeny of Tipulomorpha (Insecta: Diptera). J. Syst. Paleontol. 2019, 17, 635–652. [Google Scholar] [CrossRef]
  9. Grauvogel, L. Note préliminaire sur la faune du Grès à Voltzia. Bull. Soc. Géol. Fr. 1947, 5, 91–92. [Google Scholar]
  10. Blagoderov, V.; Grimaldi, D.A.; Fraser, N.C. How time flies for flies: Diverse Diptera from the Triassic of Virginia and early radiation of the order. Am. Mus. Novit. 2007, 3572, 1–39. [Google Scholar] [CrossRef]
  11. Martin, S.K. A new protorhyphid fly (Insecta: Diptera: Protorhyphidae) from the Lower Jurassic of the Perth Basin, Western Australia. Alavesia 2008, 2, 253–257. [Google Scholar]
  12. Gall, J.-C.; Grauvogel-Stamm, L. The early Middle Triassic ‘Grès a‘ Voltzia’ Formation of eastern France: A model of environmental refugium. C. R. Palevol. 2005, 4, 637–652. [Google Scholar] [CrossRef]
  13. Lukashevich, E.D.; Przhiboro, A.A.; Marchal-Papier, F.; Grauvogel-Stamm, L. The oldest occurrence of immature Diptera (Insecta), Middle Triassic, France. Ann. Soc. Entomol. Fr. 2010, 46, 4–22. [Google Scholar] [CrossRef]
  14. Shcherbakov, D.E.; Lukashevich, E.D.; Blagoderov, V.A. Triassic Diptera and initial radiation of the order. Int. J. Dipterol. Res. 1995, 6, 75–115. [Google Scholar]
  15. Mostovski, M.B.; Ross, A.J.; Szadziewski, R.; Krzemiński, W. Redescription of Simulidium priscum Westwood and Pseudosimulium humidum (Brodie) (Insecta: Diptera; Rhagionidae) from the Purbeck Limestone Group (Lower Cretaceous) of England. J. Syst. Palaeontol. 2003, 1, 59–64. [Google Scholar] [CrossRef]
  16. Ansorge, J. Insekten aus dem oberen Lias von Grimmen (Vorpommern, Norddeutschland). Neue Paläont. Abh. 1996, 2, 1–132. [Google Scholar]
  17. Lukashevich, E.D. New Bibionomorpha (Insecta: Diptera) from the Jurassic of Asia. Paleontol. J. 2012, 46, 273–287. [Google Scholar] [CrossRef]
  18. Lukashevich, E.D.; Shcherbakov, D.E. A new Triassic family of Diptera from Australia. In Proceedings of the First International Palaeoentomological Conference, Moscow, Russia, 30 August–4 September 1998; Bratislava, 1999. pp. 81–89. [Google Scholar]
  19. Kania, I.; Woiton, M.; Lukashevich, E.; Stanek-Tarkowska, J.; Wang, B.; Krzemiński, W. Anisopodidae (Insecta: Diptera) from Upper Cretaceous amber of northern Myanmar. Cret. Res. 2019, 94, 190–206. [Google Scholar] [CrossRef]
  20. Hennig, W. Kritische Bemerkungen über den Bau der Flügelwurzel bei den Dipteren und die Frage nach der Monophylie der Nematocera. Stuttg. Beitr. Naturk. 1968, 193, 1–23. [Google Scholar]
  21. Stuckenberg, B.R. Pruning the tree: A critical review of classifications of the Homeodactyla (Diptera, Brachycera), with new perspectives and an alternative classification. Stud. Dipterol. 2001, 8, 3–41. [Google Scholar]
  22. Kerr, P.H. Phylogeny and classification of Rhagionidae, with implications for Tabanomorpha (Diptera: Brachycera). Zootaxa 2010, 2592, 1–133. [Google Scholar] [CrossRef]
  23. Grimaldi, D.; Cumming, J. Brachyceran Diptera in Cretaceous ambers and Mesozoic diversification of the Eremoneura. Bul. Am. Mus. Natur. Hist. 1999, 239, 1–124. Available online: http://hdl.handle.net/2246/1583 (accessed on 1 September 2023).
  24. Krzemiński, W.; Ansorge, J. A new rhagionid fly from the Lower Jurassic of Germany. Pol. J. Entom. 2005, 74, 369–372. [Google Scholar]
  25. Mostovski, M.B.; Jarzembowski, E.A. The first brachycerous flies (Diptera: Rhagionidae) from the Lower Jurassic of Gondwana. Paleontol. J. 2000, 34 (Suppl. 3), 367–369. [Google Scholar]
  26. Handlirsch, A. 1920-21. Kapitel 7. Palaeontologie. In Handbuch der Entomologie; Schröder, C., Ed.; G. Fisher: Jena, Germany, 1920; Volume III, pp. 117–304. [Google Scholar]
  27. Krzemiński, W.; Ansorge, J. On Protobrachyceron Handlirsch, 1920 (Diptera: Brachycera) from the Lower Jurassic of Germany. Pol. J. Entom. 2000, 69, 231–237. [Google Scholar]
  28. Zhang, K.; Yang, D.; Ren, D. The first Middle Jurassic Protobrachyceron Handlirsch fly (Diptera: Brachycera: Protobrachyceridae) from Inner Mongolia (China). Zootaxa 2008, 1879, 61–64. [Google Scholar] [CrossRef]
  29. Kovalev, V.G. Bibionomorpha et Asilomorpha. Trans. Jt. Sov.–Mong. Palaeont. Exp. 1986, 28, 127–154. [Google Scholar]
  30. Mostovski, M.B.; Jarzembowski, E.A.; Coram, R.; Ansorge, J. Curious snipe-flies (Diptera, Rhagionidae) from the Purbeck of Dorset, the Wealden of the Weald and the Lower Cretaceous of Spain and Transbaikalia. Proc. Geol. Assoc. 2000, 111, 153–160. [Google Scholar] [CrossRef]
  31. Stuckenberg, B.R. Antennal evolution in the Brachycera (Diptera), with a reassessment of terminology relating to the flagellum. Stud. Dipterol. 1999, 6, 33–48. [Google Scholar]
  32. Hennig, W. Eine neue Art der Rhagionidengattung Litoleptis aus Chile, mit Bemerkungen über Fühlerbildung und Verwandtschaftsbexiebungen einiger Brachycerenfamilien (Diptera: Brachycera). Stutt. Beitr. Naturk. 1972, 174, 1–51. [Google Scholar]
  33. McAlpine, D.K. Observations on atennal morphology in Diptera, with particular reference to the articular surfaces between Segments 2 and 3 in the Cyclorrhapha. Rec. Austr. Mus. 2011, 63, 113–166. [Google Scholar] [CrossRef]
  34. Webb, D.W. A revision of the Nearctic species of Rachicerus (Diptera: Rachiceridae). J. Kans. Entomol. Soc. 1984, 57, 298–315. Available online: http://0-www-jstor-org.brum.beds.ac.uk/stable/25084513 (accessed on 1 September 2023).
  35. Grimaldi, D.A.; Amorim, D.S.; Blagoderov, V.A. The Mesozoic family Archizelmiridae (Diptera: Insecta). J. Paleontol. 2003, 77, 368–381. [Google Scholar] [CrossRef]
  36. Lukashevich, E.D. Revision of Archizelmira Rohdendorf, 1962 (Diptera, Archizelmiridae). Palaeoentomology 2022, 5, 254–261. [Google Scholar] [CrossRef]
  37. Ševčík, J.; Skartveit, J.; Krzemiński, W.; Skibińska, K.A. Peculiar new genus of Bibionomorpha (Diptera) with Brachycera-like modification of antennae from Mid-Cretaceous amber of Myanmar. Insects 2021, 12, 364. [Google Scholar] [CrossRef] [PubMed]
  38. Krzemiński, W. Triassic and Lower Jurassic stage of Diptera evolution. Mitt. Schweiz. Ent. Ges. 1992, 65, 39–59. [Google Scholar]
  39. Séguy, E. Ordre des Diptères. Trait. Zool. 1951, 10, 449–744. [Google Scholar]
  40. Kovalev, V.G. The oldest representatives of the Diptera with short antennae from the Jurassic of Siberia. Paleontol. J. 1981, 3, 85–101. [Google Scholar]
  41. Kovalev, V.G.; Mostovski, M.B. A new genus of the snipe-flies (Diptera, Rhagionidae) from the Mesozoic of Eastern Transbaikalia. Paleontol. J. 1997, 31, 523–527. [Google Scholar]
  42. Mostovski, M.B. Contributions to the study of fossil snipe flies (Diptera: Rhagionidae): The genus Protorhagio. Paleontol. J. 2008, 42, 75–80. [Google Scholar] [CrossRef]
  43. Labandeira, C.C. Insect mouthparts: Ascertaining the paleobiology of insect feeding strategies. Annu. Rev. Ecol. Syst. 1997, 28, 153–193. [Google Scholar] [CrossRef]
  44. Labandeira, C.C. The fossil record of insect mouthparts: Innovation, functional convergence, and associations with other organisms. In Insect Mouthparts: Form, Function, Development and Performance; Zoological Monographs; Krenn, H.W., Ed.; Springer: Cham, Switzerland, 2019; Volume 5, pp. 567–671. [Google Scholar] [CrossRef]
  45. Budd, G.E.; Jensen, S. A critical reappraisal of the fossil record of the bilaterian phyla. Biol. Rev. 2000, 75, 253–295. [Google Scholar] [CrossRef] [PubMed]
  46. Ponomarenko, A.G. Paleobiology of angiospermization. Paleontol. J. 1998, 32, 325–331. [Google Scholar]
Figure 3. Gallia alsatica Krzemiński and Krzemińska, 2003, holotype, male, total habitus. (a) Part and (b) counterpart. Scale bars 1 mm.
Figure 3. Gallia alsatica Krzemiński and Krzemińska, 2003, holotype, male, total habitus. (a) Part and (b) counterpart. Scale bars 1 mm.
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Lukashevich, E.D.; Mostovski, M.B. The Imitation Game: In Search for Brachycera in the Triassic. Diversity 2023, 15, 989. https://0-doi-org.brum.beds.ac.uk/10.3390/d15090989

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Lukashevich ED, Mostovski MB. The Imitation Game: In Search for Brachycera in the Triassic. Diversity. 2023; 15(9):989. https://0-doi-org.brum.beds.ac.uk/10.3390/d15090989

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Lukashevich, Elena D., and Mike B. Mostovski. 2023. "The Imitation Game: In Search for Brachycera in the Triassic" Diversity 15, no. 9: 989. https://0-doi-org.brum.beds.ac.uk/10.3390/d15090989

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