Research Article |
Corresponding author: Serguei A. Simutnik ( simutnik@gmail.com ) Academic editor: Petr Janšta
© 2022 Serguei A. Simutnik, Evgeny E. Perkovsky, Dmitry V. Vasilenko.
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:
Simutnik SA, Perkovsky EE, Vasilenko DV (2022) Electronoyesella antiqua Simutnik, gen. et sp. nov. (Chalcidoidea, Encyrtidae) from Rovno amber. Journal of Hymenoptera Research 94: 105-120. https://doi.org/10.3897/jhr.94.94773
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Electronoyesella antiqua Simutnik, gen. et sp. nov., is described and illustrated based on a female specimen from late Eocene Rovno amber. Like most previously described Eocene Encyrtidae, the new taxon differs from the majority of extant ones in a number of features. Sclerotised metasomal structures, similar to the paratergites of extant Tetracneminae, are seen here for the first time in fossils. The new genus is characterized also by the frontovertex with four vertical rows of piliferous punctures and the face also with intricate sculpture; notauli are present as small but distinct depressions, only anteriorly; the apex of metatibia with a peg originating from a round, deep pit; and the unusual setation of the hind wing.
cerci, Eocene, evolution of Encyrtidae, metatibial peg, paratergites
To date, 16 species in 14 extinct genera of Encyrtidae have been described from Rovno, Baltic, and Danish ambers and several undescribed encyrtids have been reported by
One species of the extant genus Copidosoma Ratzeburg, 1844, C. archeodominica Zuparko & Trjapitzin, 2014, has been described from Miocene Dominican amber (
According to the molecular analysis of
The studied specimen is housed in the collection of the
Schmalhausen Institute of Zoology of the National Academy of Sciences of Ukraine, Kiev (
The specimen was examined using the equipment and techniques described in
Terminology and abbreviations follow
Chalcidoidea Latreille, 1817
Encyrtidae Walker, 1837
Electronoyesella antiqua Simutnik, sp. nov.
Type species only.
The new genus is named in honor of John Stuart Noyes, who first saw the presence of the structures similar to paratergites in the new fossil. The name is a combination of “electrum” (Latin: electrum = amber) and “Noyes”. The genus name is a feminine noun.
Female. Body not flattened; frontovertex as long as broad, with four vertical rows of piliferous punctures (Fig.
Male. Unknown.
Placement of Electronoyesella gen. nov. in Tetracneminae is supported by the absence of the filum spinosum of linea calva, the tridentate mandibles with the middle tooth being the longest, the hypopygium reaching a little way past the apex of the syntergum, and the presence of the sclerotized, ribbon-like, separated part of Mt8 along the margin of the syntergum (Figs
The hind wing of the new genus has a single line of long setae alongside the entire costal cell (Fig.
The same line of long setae alongside the costal cell of the hind wing is present in few extant Encyrtinae: Exoristobia Ashmead, 1904 (Simutnik et al. 2021), Rhytidothorax Ashmead, 1900, and some other Bothriothoracini Howard, 1895 (J. S. Noyes, pers. comm. 2022). In Aphycoides Mercet, 1921 these setae are sparser and shorter. Within Tetracneminae, a somewhat similar line of setae is present in Ericydnus Walker, 1837 and Moraviella Hoffer, 1954, but their setae do not vary in length. A line or several lines of setae are present in Aenasius Walker, 1846; Blepyrus Howard, 1898; Monodiscodes Hoffer, 1953, but they are also short.
A line of long setae, but sparser and more or less equal in length originating from the membrane of the costal cell, similar to these of Ericydnus, are also found in the earliest known Sakhalinian amber encyrtids: Sugonjaevia Simutnik, 2015, Encyrtoides Simutnik, 2021, and Sakhalinencyrtus Simutnik, 2021. This character state seems to be a feature of the stem group of Encyrtidae.
The first funicular segment seen in the majority of known Eocene encyrtid females, including the oldest described female from middle Eocene Sakhalinian amber (
The new taxon further differs from most known Encyrtidae by the presence of a peg or spicule originating from the round, deep pit at the apex of metatibia (Fig.
Holotype
,
Nematocera, spider web.
The specific epithet means ancient in Latin.
Female. Habitus as in Figs
Coloration. Head, thorax, gaster dorsally, tegula, and all femora black; antenna uniformly dark brown; gaster ventrally dark brown; venation brown; mesotibial spur and tarsi pale yellow; surface of frontovertex, thorax, legs shiny due to presence of a thin layer of air, without metallic shine.
Sculpture.
Head, pronotum and mesoscutum rough reticulate, but surface of head only sparsely punctate – frontovertex with 4 vertical rows of large but shallow piliferous punctures (Fig.
Head.
Lenticular, slightly wider than thorax in dorsal view; occipital margin sharp, but not carinate (Fig.
Antenna. Geniculate, 11-segmented, without differentiated anelli, with 6 funicular segments and 3-segmented clava; radicle short, about 2× as long as broad (Fig.
Mesosoma. Pronotum short, not conspicuously narrower than mesoscutum, almost vertical (in lateral view), with posterior edge only slightly emarginate (Fig.
Wings. Fully developed, hyaline. Forewing 2.5× as long as broad; linea calva not interrupted but closed on posterior margin, without filum spinosum, with well-developed line of long setae alongside basal margin of dorsal surface (Figs
Legs. Mid tibial spur about as long as basal mid tarsal segment or slightly shorter, both relatively long; mesotibia with row of pegs along anteroapical edge (Figs
Metasoma. As long as head and mesosoma together; cerci situated in apical third of metasoma, with long vertical setae (or bristles) (Figs
Electronoyesella antiqua gen. et sp. nov., holotype female A metasoma, part of mesosoma, posterodorsal (cers – cercal seta, hyp – hypopygium, osh – ovipositor sheaths, ost – ovipositor stylet, ptrg? – paratergite?, spr – spiracle, syn – syntergum, vr2 – second valvifer) B metasoma, part of mesosoma, posterolateral (cer – cercus, fc – filamentous connection, muc – mucro, opo? – possible, outer plate of the ovipositor, spv – hyaline spur vein; osh(v3) – ovipositor sheaths).
A, B Ericydnus sp., female A metasoma, dorsal (opo – outer plates of ovipositor, ptrg – paratergite) B apex of metasoma, lateral (spr – spiracle on the lateral lobe of the Mt7, v3 – ovipositor sheaths) C Electronoyesella antiqua gen. et sp. nov., holotype female, apex of metasoma, lateral (fc – filamentous connection). Scale bars: 0.2 mm.
Male. Unknown.
Type species only.
Electronoyesella antiqua gen. et sp. nov. from Rovno amber is the 23th non-ant hymenopteran genus (from 57, 40.4%) and 50th non-ant hymenopteran species (from 73, 68.5%), unknown from Baltic amber (Olmi 2022a, b).
Late Eocene and extant encyrtid faunas differ (
One of the most intriguing things in the evolution of encyrtids is what happens to the connection of tergite IX of the abdomen (Mt8) and the outer plates of the ovipositor (OPO) (J. S. Noyes, pers. comm. 2022). The OPO are completely separated from the syntergum behind the cercal plate in Encyrtinae. In Tetracneminae they are connected by the paratergite. Both features almost certainly result from advancement of cerci (
Cerci of the earliest known middle Eocene Encyrtidae from Sakhalinian amber are close to each other, located at the very top of the gaster, similar to the ground plan state for Chalcidoidea. Then, tentatively in late Eocene, they began to shift towards the base of the gaster and the distance between them began to increase (figs 12–14 in
The process of cercus advancement in both Encyrtinae and Tetracneminae occurred independently and in parallel, and it began precisely in the late Eocene, since the cerci still remain in the apical or subapical position in most encyrtids from European ambers. Cerci extremely advanced to the base of the metasoma, as in many extant taxa, have not been found in known Eocene Encyrtidae.
The elongate sclerotized strip (paratergite) in Tetracneminae apparently separated from the lateral margin of the syntergum when the latter became long enough and the cercal plates advanced significantly towards the base of the gaster. The true paratergite must directly maintain a connection to tergite IX (Mt8). This connection is traceable in many species of extant Ericydnus around the side and anterior of the cercal plate (Fig.
We are sincerely grateful to John S. Noyes, S. Bruce Archibald, Aleksandr P. Rasnitsyn, and Petr Janšta for their help and valuable comments, and to Anatoly P. Vlaskin (