A new species of Ampulicomorpha Ashmead from Eocene French amber, with a list of fossil and extant Embolemidae (Insecta: Hymenoptera) of the world

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Introduction
Embolemidae is one of the smallest and least known families among Chrysidoidea, currently with 62 extant species described in three genera (see list in Supplementary material: Appendix A): the cosmopolitan Embolemus Westwood, 1833 and Ampulicomorpha Ashmead, 1893;and Trogloembolemus Olmi, Mita and Guglielmino, 2014, which is known only from two troglobitic species from Japan (Mita and Olmi, 2018).
Extant embolemid wasps are parasitoids on nymphs of the planthopper families Cixiidae (for Embolemus) and Achilidae (for Ampulicomorpha), but knowledge on their biology remains very limited due to their cryptic behavior and tiny size (varying from 1 to 7 mm), making them difficult to find and observe (Olmi, 1995). Within the superfamily Chrysidoidea, Embolemidae has consistently been retrieved as sister to Dryinidae (Brothers and Carpenter, 1993;Carr et al., 2010;Brothers, 2011;Branstetter et al., 2017), although the group has rarely been incorporated in higher-level phylogenies of Hymenoptera to place it in a broader context.
Morphologically, embolemid wasps are easily discernible from other Chrysidoidea by their 10-segmented antennae that are inserted far from the mouthparts and, in extant genera, on a frontal prominence (but prominence absent in the extinct genera Cretembolemus Olmi, Rasnitsyn, Brothers and Guglielmino, 2014;Baissobius Rasnitsyn, 1975;and Embolemopsis Olmi, Rasnitsyn and Guglielmino, 2010). They are also noticeable for their sexual dimorphism, as several other chrysidoid families, the males being macropterous while females are either micropterous or brachypterous in Embolemus, but macropterous in Ampulicomorpha. The distinction between males of both genera is more challenging, based only on the second cubital cell of the fore wing being closed by distinctly pigmented veins in Ampulicomorpha, and open or closed by weakly pigmented veins in Embolemus. Hence, the synonymy of both genera proposed by van Achterberg and van Kats (2000), which is still controversial as the genera seem to have different hosts and biology and the females are clearly distinct (Olmi et al., 2014c;Contarini et al., 2020). An ongoing molecular analysis of species of both genera will hopefully help clarify this situation (note from M. Olmi in Contarini et al., 2020). Meanwhile, we keep considering Ampulicomorpha as a distinct, valid genus in the present work.
Fossil Embolemidae are known from rock imprints and inclusions in amber but remain infrequent, with only 11 species recognized to date ( Fig. 1: eight species from five Cretaceous deposits, three species from two Eocene deposits). But we are aware of a work in progress by Perkovsky et al. (in prep.), in which all known fossil embolemids are reviewed and several new species are described, including new species of Embolemus from mid-Cretaceous Burmese (Kachin) amber as well as the oldest known embolemid, from the Early Barremian amber of the Isle of Wight (ca. 128 Ma). Interestingly, it belongs to the extinct genus Embolemopsis, which is otherwise known only from an Aptian-aged rock imprint from Siberia (Olmi et al., 2010). So far, this is the only genus found both as a rock imprint and an amber inclusion. Other species in rock imprints similarly belong to extinct genera, namely Baissobius and Cretembolemus, while other amber fossils belong to either Embolemus or Ampulicomorpha. Remarkably, these two extant genera are recorded as early as in the mid-Cretaceous, 100-105 Ma (including undescribed species of Embolemus from Kachin amber, pers. obs.). And these Burmese fossils already display a dimorphism similar to extant ones, indicating a long-term morphological stasis in these lineages.
Here we describe a new fossil species of Ampulicomorpha based on a single female specimen from Early Eocene Oise amber, France. This is the second species of Ampulicomorpha from the Eocene of Europe, and the first fossil record of the family Embolemidae in France.

Material and methods
The description below is based on a single individual found in amber from the Le Quesnoy outcrop, near Houdancourt in the Oise Department of the Paris Basin, France. The outcrop, dated as Ypresian in age ('Sparnacian', Early Eocene, ca. 53 Ma), has yielded a copious amount of fossiliferous amber associated with abundant plant remains and a diverse vertebrate fauna. Further details on the geology, biodiversity, and paleoenvironment can be found in Nel et al. (1999Nel et al. ( , 2004, Cavagnetto (2000), Brasero et al. (2009), or Nel andBrasero (2010).
The wasp was found preserved in an automorph, cylindrical piece of orange amber approximately 4.0 mm in diameter. The piece was partly polished to remove the opaque weathered surface using Buehler CarbiMet silicon carbide papers on a Buehler Metaserv 3000 polisher. Then, it was immersed in Canada balsam between cover slips for optimal views. Observations, measurements, and photographs were made using a Leica MZ APO stereomicroscope equipped with an ocular micrometer and a Canon 5D Mark II SLR camera. Helicon Focus 6.7 software was used to build composite images from a series of photographs taken at different focal planes. The resulting images and figures were processed using Adobe CC (Photoshop, Illustrator), which was also used to compose the map in Figure 1.
The specimen is preserved without apparent distortion and is mostly complete, missing the tarsomeres of right mid leg, the femoro-tibial articulation of the right hind leg, the left hind leg beyond the femur, the posterodorsal portion of the mesosoma, and most of the wings except basal portions and the apical portion of the right fore and hind wings. The wings and mesosomal structures were apparently lost in an amber splintering that likely occurred during the field collecting or the washing of the amber material.
The terminology used in this study generally follows that of Lanes et al. (2020) pertaining to Bethylidae, with additions of Olmi (1995) or Olmi et al. (2014c) for all the ocellar measurements, which are detailed below with other measurements and indices, and illustrated in Figure 2.   (Feugueur, 1963;Nel et al., 1999;Cavagnetto, 2000) Etymology. The specific epithet is derived from the Le Quesnoy outcrop, the type locality from which the new species originates.
Description. Female, macropterous ( Fig. 3C: basal portions of all wings and apicalmost portions of the right fore and hind wings are the only preserved parts; but the fore wing reaches the second gastral segment, thus indicating macroptery). Body length 3.15 mm as visible dorsally (but gaster curved ventrally and anteriorly, total length in lateral view 4.30 mm). Head pyriform, slightly longer than high, 0.60 mm long; eye rather large, higher than long, slightly less than half as long as head (0.25 mm long). Antennae filiform, inserted on two contiguous frontal projections; scape elongate, 1.7Â as long as first flagellomere; first flagellomere approximately 2.5Â as long as broad, following flagellomeres gradually shortening except apical one which is longest, with rounded tip; length of antennomeres (in mm): 0.65, 0.12, 0.38, 0.35, 0.30, 0.28, 0.26, 0.26, 0.20, 0.24; distance between antennal sockets and clypeus 0.25 mm; ocelli conspicuous, OL = 0.08, OOL = 0.18, OPL = 0.24, POL = 0.09; occipital carina distinct in dorsal and lateral views; mandible tridentate, subrectangular, about twice as long as broad, outer surface slightly convex; maxillary palps with five visible segments, basal segment widest; labial palps not visible.
Metasoma. First gastral segment with anterior petiole approximately as long as metatrochanter (ca. 0.16 mm); first segment distinctly widening posteriorly, about as long as apical width; second gastral segment largest of metasomal segments; following segments progressively smaller, curved downward, nearly at right angle from first two segments.

Discussion
Female embolemid wasps typically have the antennal scape elongate, much longer than the third antennal segment (Olmi, 1995), which clearly is the case of the newly described specimen (Figs. 3A-C). The new species, being a macropterous female with the antennae inserted on two contiguous frontal projections, is thus assignable to Ampulicomorpha according to Olmi (1995) or Olmi et al. (2014a). Additionally, the rather large eyes of the new fossil also suggest this genus

Conclusion
The newly described species of Ampulicomorpha adds to the scant knowledge of the evolutionary history of embolemid wasps. The current fossil record shows that the genus occurred in territories that today belong to the western Palaearctic region from, at least, the late Early Cretaceous (A. perialla from the Albian of Spain) until the Late Eocene (A. succinalis from the Priabonian of the 'Baltic amber forest'). Today, the Palaearctic species of Ampulicomorpha are almost exclusively restricted to its eastern part (Olmi, 1995;Xu et al., 2012;Olmi et al., 2014a;Kim and Lee, 2016;Mita et al., 2017), with the exception of A. thauma Rasnitsyn and Matveev, 1989 in the southwest of Russia (Rasnistyn and Matveev, 1989;Olmi et al., 2014a) and A. reticulata (van Achterberg and van Kats, 2000) in the Netherlands (originally described as Embolemus reticulatus but from a macropterous female, so it has been transferred in Ampulicomorpha by Olmi et al. (2014c) who rejected the synonymy of both genera). In contrast, the only genus broadly distributed today in the western Palaearctic region is Embolemus (Olmi, 1994;Hansen and Olmi, 1996) (Fig. 1).