Research Article |
Corresponding author: Jonah M. UImer ( jonah.ulmer@gmail.com ) Academic editor: Ankita Gupta
© 2023 Jonah M. UImer, Petr Janšta, Dany Azar, Lars Krogmann.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
UImer JM, Janšta P, Azar D, Krogmann L (2023) At the dawn of megadiversity – Protoitidae, a new family of Chalcidoidea (Hymenoptera) from Lower Cretaceous Lebanese amber. Journal of Hymenoptera Research 96: 879-924. https://doi.org/10.3897/jhr.96.105494
|
The earliest representatives of Chalcidoidea are described from Barremian age Early Cretaceous Lebanese amber and classified in Protoitidae Ulmer & Krogmann, fam. nov. (Hymenoptera: Chalcidoidea). Protoitidae exhibits a high morphological diversity of the terminal metasomal tergum which may indicate a broad spectrum of oviposition capabilities and the ability to occupy a diverse range of ecological niches. Protoitidae comprises two genera, Protoita Ulmer & Krogmann, gen. nov., and Cretaxenomerus Nel & Azar, 2005 based on C. jankotejai Nel & Azar, 2005, which is transferred from Scelionidae (Hymenoptera: Platygastroidea) to Protoitidae. Together, 10 new species, all by Ulmer and Krogmann, are described in the two included genera–Protoita bidentata, P. istvani, P. noyesi, P. petersi, Cretaxenomerus brevis, C. curvus, C. deangelis, C. mirari, C. tenuipenna, and C. vitreus. Keys to the genera and species of Protoitidae are provided. In addition, we examine the postulated plesiomorphies and apomorphies within Chalcidoidea with respect to the fossil record, and provide additional hypotheses on their biogeographic origins.
Barremian age, Paleoentomology, plesiomorphic, taxonomy
Today, chalcid wasps (Hymenoptera: Chalcidoidea) are among the most diverse lineages of life, following a megaradiation event in the Late Cretaceous (
Due to its extreme diversification, Chalcidoidea has been the subject of numerous phylogenetic studies since the end of the last century (e.g.,
The early pattern of evolution of Chalcidoidea is still uncertain, in part because of the low number of fossils (n ≈ 154 species) (from paleobioDB;
Graph of identified Chalcidoidea families along the fossil record. Points are singleton taxa known only within the fossil record from one time period, whereas those with a fossil record extending multiple ages are shown as a line through the ages in which they are represented. Alternating gray and white bands represent geological eras. Extinct families are denoted by †. Bouceklytinae and Distylopinae are noted with an asterisk (*) because their familial placement is uncertain. Taxa in red correspond to the “soft-bodied” clade (Soft-bodied), while taxa in blue correspond to the “hard-bodied” (Hard-bodied) lineages based on
Chalcidoidea is a notoriously difficult group to assess for statements of homology (
While no Chalcidoidea have previously been described from Lebanese amber, several undoubtedly chalcid taxa have been uncovered from mid-Cretaceous amber deposits, which coincides with the diversification of the superfamily (Fig.
This uncertainty of fossil placement is further seen in the description of the putative pteromalid, Parviformosus wohlrabeae
Fossil “true” Chalcidoidea are more prevalent within the Upper Cretaceous (Burmese) deposits, although the sister group Mymarommatoidea is known already from Lebanese amber (
Excluding Bouceklytinae (uncertain subfamily), Diversitinidae was the only valid extinct family of Chalcidoidea described from Cretaceous (Burmese) amber (
The Chalcidoidea fossil record prior to this work consists of approximately 154 described species (Suppl. material
Lebanese amber is one of the oldest fossil sources, dating to the Barremian age of the Lower Cretaceous (~130 MYA) (
Because the most recent paleobiogeographic models suggest a Southern Gondwana origin for chalcids (Cruaud et al. 2022), with multiple northward dispersals between 150 and 100 MYA, the examination of older northeastern Gondwanan fauna can provide novel insights into the earliest range expansions of a fledgling group. Herein, we provide the description of a new family of Chalcidoidea from Lebanese amber, the earliest currently known, based on 15 fossils. The new family is classified as two genera (one described as a new) and 11 species, of which ten are newly described. Postulated plesiomorphies and hypotheses about the early diversification of Chalcidoidea pre-radiation are discussed.
Among the 450 different outcrops of amber-bearing sediment from the Lower Cretaceous in Lebanon, 29 outcrops provide biological inclusions. In the present study we examined 15 specimens from two outcrops:
Of the examined specimens, all but one, Protoita istvani, sp. nov., are from the Hammana outcrop.
All the material was previously deposited at the National Museum of Natural History, Paris, France (
Relevant material was prepared following (
Fossil data for Chalcidoidea was pulled from the paleobioDB (
Terminology follows the Hymenoptera Anatomy Ontology (HAO) (
Fore wing morphology and terminology A Cretaxenomerus vitreus, sp. nov. B Rotoita sp. (Baeomorphidae). av = anal vein; bc = basal cell; bv = basal vein; cc = costal cell; Cu1 = cubital vein; hb = hyaline break; M+Cu = medio-cubital crossvein; mv = marginal vein; pas = parastigma; pmv = postmarginal vein; smv = submarginal vein; stv = stigmal vein; uncs = uncus.
Some morphological characters are of a continuous or difficult to discretize nature (e.g., clavomere segments) or their physical boundaries are not clearly defined in some taxa (e.g., marginal wing venation). The need for consistency and checkpoints of characters amongst all taxa are critical for their interpretation, especially within paleotaxonomy where structures can be degraded or obscured. Here we provide our rationale for discretizing such characters within Protoitidae.
Marginal vein (mv)–The marginal vein of Chalcidoidea is usually delimited between either the end of the costal cell (cc) proximally or the junction of the hyaline break and the point of intersection of the stigmal vein and postmarginal vein. In several specimens of Protoitidae the costal cell is not visible or folded in a way that it does not provide clear indication of the proximal starting point of the marginal vein. In these specimens we use the presence of a weakening of the wing venation at a junction similar to the hyaline break in higher chalcids, which often has sensilla that mark the beginning of the marginal vein (hb; Fig.
Flagellomere (fl)/ funicle (fu)/ clavomere (cl)
–Within chalcid antennal terminology, flagellomeres are all the antennomeres beyond the pedicel, whereas funicular segments are defined as the flagellomeres located between the anellus or anelli (often ring-like segment(s) directly distal of pedicel that always lack MPS) and clava. Protoitidae lack an anellus, the basal flagellomere being longer than wide and having MPS, so for the sake of clarity when discussing antennal segments “flagellomere” is used for all segments beyond the pedicel including clavomere(s), and funicle for all segments between pedicel and clava. The claval segments of several taxa are often difficult to discern because of a gradual increase in flagellomere width through the entire length of the flagellum. Likewise, many fossil taxa described are based on singletons so shape and closeness of antennal segments are difficult to state as true or as taphonomic artifacts. Within this work, we assign and count claval segments starting at those without a clear ‘gap’ at the joint with the subsequent segment (Fig.
Order Hymenoptera Linnaeus, 1758
Superfamily Chalcidoidea
Protoita, gen. nov.
Antenna 14-segmented (Fig.
1 | Metasoma in dorsal view triangular in shape and broadly attached to mesosoma (Figs |
Protoita gen. nov. |
– | Metasoma in dorsal view ovoid, with distinct constriction between meta- and mesosoma (Figs |
Cretaxenomerus Nel & Azar, 2005 |
Small, less than 1 mm in length. Head transverse in dorsal view, wider than mesosoma and with temple narrow. Metasoma sessile, broadly associated with mesosoma, and in dorsal view triangular in shape; syntergum no longer than preceding tergite; cerci digitiform. Female with exerted ovipositor at most ¼ as long as length of metasoma.
1 | Head globular or of about equal dimensions (Figs |
2 |
– | Head narrowed antero-posteriorly in dorsal view (Figs |
3 |
2 | Terminal clavomere equal in length to preceding clavomere (Fig. |
Protoita noyesi sp. nov. |
– | Terminal clavomere ½ length of preceding clavomere (Fig. |
Protoita petersi sp. nov. |
3 | Antenna with clava 3-segmented; funicular segments all about equal in dimensions (Fig. |
Protoita bidentata sp. nov. |
– | Antenna with clava 2-segmented; funicular segments 1–3 4× as long as wide (Fig. |
Protoita istvani sp. nov. |
The female of Protoita noyesi differs from those of other species in the genus by the following combination of characters: occiput impressed relative to vertex (Fig.
Female. Body length 876. Body uniformly brown except legs light brown. Wings with light brown infumation, uniformly setose. Right mesopleuron with bluish metallic tint. Head wedge shaped in lateral view, wider than mesosoma in dorsoventral view (Fig.
Protoita noyesi, holotype A lateral habitus B apical part of antenna C fore leg basitarsus D mesosoma, lateral E head, posterior F fore wing G ovipositor complex and terminal metasomal segments. Scale bars: 500 µm (A); 200 µm (F); 100 µm (D); 50 µm (G). 3v = 3rd valvulae; axl = axillula; btc = basitarsal comb; cal = calcar; cer = cerci; msc = mesoscutum; msct = mesoscutellum; no1 = pronotum; ov = ovipositor; pl2 = mesopleuron; pre = prepectus; prp = propodeum.
Male. Unknown.
Female. Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: 407AB.
Specimen in good condition with slight detachment from amber along the mesopleuron, and bubble formed around propodeal spiracle.
The specific epithet is a patronym in honor of Dr John Noyes for his lifelong contributions to chalcidology.
Protoita bidentata, the only species of the genus known from the male, differs from all other species in the genus by the following combination of characters: Body and antenna bicolored (Fig.
Protoita bidentata, holotype A dorsolateral habitus B male genitalia, ventral C terminal funicular segments and clava D mesosoma, dorsolateral E head, posteroventral. Scale bars: 500 µm (A); 100 µm (C–E). aed = aedeagus; dig = digitus; frn = frenum; hyc = hypostomal carina; lbp = labial palp; md = mandible; msp = mesothoracic spiracle; Mtn = metasomal tergum; mxp = maxillary palp; no3 = metanotum; par = paramere; psp = propodeal spiracle; tsa = transcutal articulation; vol = volsella.
Male. Body length 855. Head, scape, pedicel and fu1–fu4 brown. Mesosoma, metasoma and fu5 to tip of clava dark brown. Legs pale. Sculpture on head, meso- and metasoma alutaceous. Wings hyaline, uniformly pilose, damaged beyond postmarginal vein (Fig.
Female. Unknown.
Holotype : male, Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: 182.
Specimen with distal ⅓ of its wings missing and basal antennomeres damaged.
The specific epithet is derived from the mandibular formula of the species.
Protoita bidentata is the only species in the genus described from a male. While it is the only taxon with two mandibular teeth, sexual dimorphism in this character is very rare in Chalcidoidea, likely the female of P. bidentata is also bidentate. Unlike dentition, antennal shape and claval segments are quite often sexually dimorphic in extant chalcids, and in Cretaxenomerus curvus where the male is known we can see a drastic variation in flagellar shape and claval number. P. bidentata is the only species known within Protoita with 3 claval segments, and within all of Protoitidae only C. deangelis is also known to have 3 claval segments however that species is described from a female.
The female of P. istvani differs from all others in the genus by the following combination of characters: Head flattened antero posteriorly, disc-like (Fig.
Protoita istvani, holotype A lateral habitus B antenna, lateral C mesosoma, lateral D head, posterior E fore wing F ovipositor complex and terminal metasomal segments G head, lateral. Scale bars: 500 µm (A); 250 µm (E); 150 µm (C); 100 µm (D, F, G). 2v = 2nd valvifer; cxn = coxa; occ = occipital carina; pl3 = metapleuron; tor = toruli.
Female. Body length 918. Coloration auburn with dark antennae. Eyes white. Wings hyaline, uniformly setose. Metasoma damaged, tergal segments detached from body (Fig.
Male. Unknown
Holotype : female, Roum – Aazour – Homsiyyeh, Caza Jezzine, Mouhafazet South Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: HAR26.
Specimen with bubbles surrounding MPS on several flagellomeres, mesosoma detached from the amber, and metasomal tergites damaged because they are detached.
The specific epithet is a patronym in honor of István Mikó, the first author’s mentor and close friend who instilled in him his passion for entomology and morphology.
The female of P. petersi differs from others of the genus by the following combination of characters: Head not as transverse as in other species, only about 1.6× as wide as long in dorsal view (Fig.
Female. Body length 913. Body dark brown legs, except coxae, and part of mesepimeron. Head, especially frons, vertex and back of head, base of fu1 light brown to dark yellow. Wings hyaline, uniformly pilose. Head ovular, only 1.6× as wide as long, wider than widest point of meso- or metasoma in dorsal view (Fig.
Male. Unknown
Holotype : female, Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: 874A.
Specimen with right antenna damaged beyond flagellomere 5, right hind leg damaged at midpoint of femur, and right fore wing damaged beyond midpoint of marginal vein.
The specific epithet is a patronym in honor of our friend and colleague Dr Ralph Peters, for his work on the early diversification of Chalcidoidea.
Body larger than 1 mm. Head usually long in dorsal view with temples well developed. Metasoma separated from mesosoma by distinct petiole or constriction, and in dorsal view ovoid; female with an elongate syntergum, longer than preceding tergite (Mt7) (except C. deangelis).
1 | Syntergum longer than 1/2 length of ovipositor (Figs |
2 |
– | Syntergum shorter than or equal to 1/2 length of ovipositor (Figs |
4 |
2 | Syntergum articulating with preceding tergum at an angle (Fig. |
Cretaxenomerus curvus sp. nov. |
– | Terminal tergum not articulating with preceding tergum at an angle (Figs |
3 |
3 | Head at least 2× as broad as long (Fig. |
Cretaxenomerus jankotejai |
– | Head about as broad as long, globular. Terminal tergum of uniform width along entire length (Fig. |
Cretaxenomerus mirari sp. nov. |
4 | Flagellum with 1-segmented clava (Figs |
5 |
– | Flagellum with 2–3 segmented clava (Figs |
6 |
5 | Fore wing spatulate, 2.5× as long as wide (Fig. |
Cretaxenomerus vitreus sp. nov. |
– | Fore wing narrow, 3.5× as long as wide (Fig. |
Cretaxenomerus tenuipenna sp. nov. |
6 | Head longer than wide (Fig. |
Cretaxenomerus deangelis sp. nov. |
– | Head wider than long (Fig. |
Cretaxenomerus brevis sp. nov. |
Female. Females differ from those of all other species within the genus by the following combination of characters: Syntergum hinged at joint with elongated Mt7, reaching more than ¾ length of ovipositor sheath (Fig.
Cretaxenomerus curvus, holotype (874D) A lateral habitus B mesosoma, lateral C antenna, lateral D ovipositor complex and terminal abdominal segments E head, lateroventral F fore wing. Scale bars: 500 µm (A); 150 µm (F); 100 µm (B–E). iap = interantennal process; lcl = lateral clypeal line; Mt8+9 = syntergum.
Female. Body length 1314 (HT) – 1407 (PT). Overall body color black with a blue sheen on the gena of HT when examined at certain angles except tegulae, legs excluding coxae, and second half of ovipositor sheath dark brown, tip of ovipositor sheath light brown, and with legs almost black. Wings hyaline except fore wing slightly brownish in HT (possible artifact) and partly brownish in PT 881B; with sparser pilosity proximally on wing surface. Head, mesosoma and metasoma coriaceous to alutaceous except areolate posterior part of mesoscutellum and propodeum. Head ovate, 1.5× as wide as long (Fig.
Holotype : female, Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: 874D. Locality information and depository of paratypes same as for holotype (Female–881B,146U; Male–1614FA).
Right antenna of holotype with terminal 3 segments missing. The amber piece of the holotype included a single inclusion of a Ceratopogonidae (Diptera).
The specific epithet is derived from the Latin ‘curvus’ meaning curved or bent, in regards to the articulation of the syntergum of the species.
The metasoma of paratype specimen 146U is damaged, preventing examination of the syntergum, however the wing venation and head shape place it as C. curvus. This is the only species described based on both sexes which provides some insight into the putative sexual dimorphisms within the genus. Notably, the variation in antennal shape and claval size which is a prolific form of dimorphism within extant chalcids. The female of C. curvus has a clear clava with multiple claval segments relative to the male which has all flagellar segments relatively stout and uniform with only the partial fusion of the terminal segments indicating a clava.
Female. Cretaxenomerus brevis differs from all other species in the genus by the following combination of characters: scape laterally flattened, only 2.25× as long as broad; antenna with at least fu1–fu4 conspicuously longer than broad, fl1 about 3.75× as long as broad. Anterolateral margin of mesoscutum flanged. Arolium elongated and extending beyond tip of tarsal claws. Syntergum relatively short, extending about ⅓ length of ovipositor sheath.
Female. Body length 1145. Uniformly dark brown, legs light brown, eyes white (likely an artifact of amber deposition) (Fig.
Male. Unknown.
Holotype : female, Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: 1228.
A large bubble obscures the posterior of the propodeum and petiole. The head is damaged at the lateral clypeal line.
The specific epithet is derived from the Latin word for ‘short’, referring to the comparatively short syntergum relative to the other species in the genus.
Cretaxenomerus vitreus differs from all other species in the genus by the following combination of characters: fore wings broadly spatulate, with postmarginal vein about 2× as long as stigmal vein (Fig.
Female. Body length 1381. Body bilaterally damaged with some internal sclerite structures visible (Fig.
Male. Unknown.
Holotype : female, Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: 534C.
Face and mandibles absent from specimen. Mesosoma bisected and cleared with scleritic components visible on left side, internal components visible on right. Metasoma with first few terga present, and marginal setal line of other segments still present to indicate placement. Right hind leg with only distal tarsomeres remaining.
The specific epithet is the Latin word for ‘glassy’ or ‘transparent’ in regards to the unique taphonomy of the specimen that appears as though it were cleared.
Damage to the specimen provides for a unique examination of both external and internal scleritic structures; however, damage to the abdomen has resulted in the loss of the terminal segments and syntergum. The lack of a multi-segmented clava is shared with Cretaxenomerus tenuipenna sp. nov.; however, the distinct difference in wing shape and venation separates these two specimens into distinct species.
Cretaxenomerus mirari differs from all other species in the genus by the following combination of characters: Head very transverse in dorsal view. Clypeus not as inflexed. Mesoscutum broader than long. Hind basitarsus with dense comb-like setation (Fig.
Female. Body length 1212. Coloration dark brown to black, slight metallic coloration on abdomen may be an artifact. Scape, legs and ovipositor sheaths dark brown, tip of ovipositor sheaths light brown. Wings lightly brownish infumated, wing venation brown. Head. Unusually long and low, about 1.5× as wide as long and low, about 0.5× as high as broad (Fig.
Male. Unknown.
Holotype : female, Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: 157G.
Specimen complete, but terminal segments of the right antenna fragmented, and tarsal segments of the left fore leg longitudinally split; partial detachment from the amber along the right side of thorax and eye margin. Streaks in the amber make it difficult to clearly assess some characters.
The specific epithet is derived from the Latin ‘mirari’, which is the origin of the English ‘mirage’ in regards to the haziness of the specimen within the amber from the taphonomic process.
Cretaxenomerus mirari shares several characters with P. curvus, namely the presence of 3 claval segments and a syntergal protrusion which is roughly ¾ of length of the ovipositor. While it is possible that P. mirari has an articulating syntergum which is simply not observable due to taphonomic processes, a postmarginal vein that is longer than the stigmal vein and a clear costal cell, would suggest that P. mirari is a distinct species for the sake of identification and until more specimens are discovered which may contradict its current placement.
Cretaxenomerus tenuipenna can be differentiated from all other species in the genus by the following combination of characters: scape conspicuously long, about as long as eye height, fu1-2 about 2× as long as wide, especially fu1 much narrower than pedicel, at least fu4 only slightly longer than wide and wider than pedicel, terminal claval segments loosely associated, without distinct fusion between cl1 and fl11. Fore wing slender, 3.5× longer than wide. Foretibia without basitarsal comb. Propodeum not strongly sloped.
Female. Body length 1256. Body dark brown, appendages light brown, may be taphonomic artifact. Wings hyaline with some slight brown infumation distally from basal vein, uniformly pilose. Right fore leg tarsal segments except about half of basitarsus and left hind tarsal segments 25 are missing, left antenna after pedicel and ovipositor broken on several places, both antennae with some cracks on scape and pedicel. Head. Globular, approximately equal in length and width (Fig.
Male. Unknown.
Holotype : female, Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: 623I.
Specimen relatively complete; antennal segments partly fragmented and separated from taphonomic process; syntergum and ovipositor complex also fragmented; tarsal segments missing beyond basitarsus on left fore- and hind leg. Streaks and ripples in the amber obscured some characters during imaging.
The specific epithet is a portmanteau of the Latin ‘tenuis’ for narrow and ‘penna’ for feather in regards to its slender wings.
Cretaxenomerus tenuipenna has several similarities with C. brevis, most pronounced being the shortened syntergum as well as C. vitreus in antennal structure. However, the wing shape would indicate it is likely a closely associated but distinct species.
Cretaxenomerus deangelis differs from all other species in the genus by the following combination of characters: shape of its head capsule, longer than wide in dorsal view. Mesoscutum with notauli. Fore wing basal cell narrow and marginal setation short. Syntergum short.
Female. Body length 1179. Head capsule light-brown, body and appendages dark brown, aside from first two flagellomeres. Wing venation dark brown. Wing’s damaged just distal to junction of smv and bv, first 2 flagellomeres damaged. Wings with slight brown infumation, uniform pilosity. Head elongate, about 1.3× as long as wide, wider than mesosoma in dorsal view (Fig.
Male. Unknown.
Holotype : female, Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number 810H.
Due to the taphonomic process both antennae are detached from the head and both scapes, pedicels and first two flagellomeres are broken; the mesosoma is slightly deformed dorsolaterally; both wings are broken, the left wing just before the basal vein and the right wing beyond the basal vein, and with some additional ruptures on the disc of both wings.
The specific epithet is a patronym in honor of Eric Deangelo, an early mentor and professor of one of the authors (JU) who introduced him to biology and research.
Due to the orientation of the specimen in the amber, the tip of the metasoma is obscured, so the syntergum could not be clearly examined, but there does not appear to be an elongate syntergum. Because C. deangelis apparently lacks an elongate syntergum, similar to Protoita but unlike other Cretaxenomerus females, this feature might support it’s placement into a third genus, although it shares more similarities with Cretaxenomerus species than Protoita. Without additional specimens to examine, we consider it premature to erect a third genus for the specimen due to its damaged state and obscured syntergum and place it tentatively in Cretaxenomerus. Even though the lack of an elongate syntergum is shared with Protoita, this lack of an apomorphy does not justify placement within Protoita as it shares more diagnostic features with Cretaxenomerus such as body length, a petiolar constriction at the waist and a head which is not wider than long in dorsal view.
Cretaxenomerus jankotejai can be differentiated from all other species in the genus by the following combination of characters: large body length, broad head, which is nearly 2× as wide as long (Fig.
Female. Body length 1490, uniformly dark brown in coloration, eyes white, wings hyaline with dense pilosity along wing disc, sparser at speculum. Head globulose, length 160, 2× as wide as long (Fig.
Male. Unknown.
Holotype : female, Hammana / Mdeyrij, Caza Baabda, Mouhafazet Mount Lebanon; lower Barremian. In amber mounted in Canada Balsam. Deposited at Natural History Museum of the Lebanese University, accession/specimen number: 972A.
Specimen complete; dorsum of head partially detached; a large transverse crack in the amber obscures portions of the metasoma distally.
The classification of Protoitidae within Chalcidoidea is based on at least two of three putative external synapomorphies for the superfamily, with the most conspicuous being the specialized morphology and placement of MPS along all flagellar segments. Although multiporous plate sensilla occur within several lineages of Proctotrupomorpha, Chalcidoidea are unique in having the MPS raised, ridge-like, along the flagellomere and with the apical end of the sensilla raised above and often projecting beyond the apical margin of the flagellomere (Figs
It should be noted that the prepectus is free, external and triangular in Diversinitidae, which represents the condition in most larger “hard-bodied chalcids” (
Within Chalcidoidea, Protoitidae cannot be included in Mymaridae, which are regarded as the earliest extant lineage of Chalcidoidea, morphologically by the structure of the ovipositor (
Protoitidae do share some features with Baeomorphidae and some Mymaridae, namely the shape of the prepectus, which is comparatively narrow, dorsoventrally elongated and anteriorly overlapped by the lateral panel of the pronotum (Fig.
All species of Protoitidae, aside from P. bidentata, have tridentate mandibles. Although there has been no formal investigation of the character polarity of mandibular dentition for Chalcidoidea, variation in the mandibular formula amongst the most basal lineages, Mymaridae and Baeomorphidae, makes it a structure difficult to assess for phylogenetic significance. The extinct genera of Mymaridae have no consistent pattern in dentition, varying from 2–4 teeth (
Both the basal and cubital veins of Protoitidae are sclerotized or at least pigmented, unlike for most other Chalcidoidea. Within Chalcidoidea, basal and cubital fore wing veins are also pigmented in Baeomorphidae, a few Pteromalidae (Miscogasterinae, Trigonoderinae), a few Melanosomellidae, Leucospidae, some Megastigmidae and sporadically in many other groups (
All protoitids are characterized by a syntergum which results from the fusion of Mt8 and Mt9. This is a derived feature found also in most extant Chalcidoidea, but which likely evolved convergently multiple times (
We observed in several Cretaxenomerus females six distinct metasomal tergal sclerites preceding the syntergum, with Mt7 being slightly elongate to articulate with the syntergum (Mt8+9). The point of fusion between Mt8+9 is likely at about the posterior ⅓ of the elongated tergum where there is a pair of lateral notches before the structure abruptly narrows slightly again, corresponding to the position of the cerci (Fig.
The syntergum is sexually dimorphic, being elongate only in females, and likely functioning as a dorsal protection for the elongate ovipositor sheaths. In several females, such as a paratype of P. curvus, where the ovipositor is extended, the syntergum is shifted up, articulating with the base of the ovipositor, and terminal tergite (Mt7). The membranous anal tube can be seen projecting from the apex of the syntergum, suggesting it to be the true distal point of the abdomen (Figs
Within Cretaxenomerus there is continuous variation in the structure of the syntergum. Within the “short-syntergum” species, consisting of C. brevis and C. tenuipenna, the ovipositor sheaths are continuous in width along their entire length (Figs
There is a clear divide in the Chalcidoidea fossil record between the Cretaceous and Eocene, corresponding with the division of early “soft-bodied” chalcids and the larger “hard-bodied” lineages (Fig.
The most recent biogeographic theories on the origin of Chalcidoidea suggest an Eastern Gondwanan origin for the group with the rapid radiation of the group occurring in Southern Gondwana (
The authors would like to thank André Nel for providing the initial specimens for this study and for hosting several research stays of LK at
Fossil Chalcidoidea occurence data
Data type: csv
Explanation note: Curated occurence and metadata of fossil Chalcidoidea taxa used for generating time series plots.