Research Article |
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Corresponding author: Alicja Pełczyńska ( alicja.pelczynska@edu.uni.lodz.pl ) Corresponding author: Pawel Korecki ( pawel.korecki@uj.edu.pl ) Academic editor: Mónica M. Solórzano Kraemer
© 2026 Alicja Pełczyńska, Evgeny E. Perkovsky, Brendon E. Boudinot, Adrian Richter, Wiesław Krzemiński, Tomasz Kołodziej, Pawel Korecki, Katarzyna M. Sowa, Agnieszka Soszyńska.
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:
Pełczyńska A, Perkovsky EE, Boudinot BE, Richter A, Krzemiński W, Kołodziej T, Korecki P, Sowa KM, Soszyńska A (2026) The rise and fall of the Eocene fly genus Kelneria (Diptera, Keroplatidae). Arthropod Systematics & Phylogeny 84: 677-703. https://doi.org/10.3897/asp.84.e197461
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Abstract
The extinct Eocene fly genus Kelneria Matile, 1979 is characterized by extreme modification of male genitalia within the family Keroplatidae. However, their morphology has remained poorly understood, as fossil material cannot be examined using traditional entomological techniques. To overcome this limitation, we applied micro-computed tomography (µCT) and synchrotron radiation micro-computed tomography (SRµCT) to reconstruct the genitalia through segmentation of scan data, enabling reassessment of the spatial organization and homology of their structures.
Our analyses indicate that Kelneria was both morphologically distinctive and well represented in Eocene amber assemblages. They also support the synonymization of the Oise amber genus Eokelneria Hebert, Ngô-Muller & Nel, 2025 with Kelneria Matile, 1979, demonstrating that the characters used to establish Eokelneria fall within the range of variation observed in Kelneria. We further demonstrate that the species-level diversity of Kelneria has been underestimated and describe three new species: Kelneria rovnensis Pełczyńska & Perkovsky sp. nov., K. erroris Pełczyńska, Krzemiński & Soszyńska sp. nov. and K. szymoni Pełczyńska, Krzemiński & Soszyńska sp. nov. Additionally, identification of representatives in Rovno and Oise ambers extends the geographic and temporal range of the genus to the early Eocene (c. 53 Ma).
Taken together, these findings show that Kelneria was an abundant, diverse, and widespread genus in the Eocene but has no modern representatives. The reasons for this extinction remain unknown; however, contrasting distribution of Eocene and extant representatives of the tribe Robsonomyiini suggests that this disappearance may reflect a broader faunal turnover in Europe after the Eocene.
Baltic amber, Eocene–Oligocene transition, Eokelneria, fossil insects, micro-CT, new synonymy, Rovno amber, synchrotron radiation micro-CT (SRµCT)
Insect genitalia evolve faster than any other body part, resulting in their extreme structural diversity (
Kelneria belongs to the subfamily Macrocerinae, in which males typically bear well-developed gonostyli terminating in two tooth-like projections, as seen in Macrocera lutea Meigen, 1804. In striking contrast, the gonostyli of Kelneria are drastically reduced, approaching complete loss. The epandrium is likewise highly modified, bearing a pair of unique lateral processes and the aedeagus with associated membranous structures is remarkably strongly sclerotized.
Given that genital morphology is closely associated with reproductive performance and fitness across animals (
In extant Diptera, such analyses rely on genital dissection and KOH maceration, procedures that separate and clear sclerotized structures, thereby removing obscuring tissues and allowing individual elements to be examined, manipulated, and compared under light microscopy in different orientations. This enables accurate assessment of their articulation and spatial relationships (e.g.
However, all known Kelneria species are preserved exclusively as Eocene amber inclusions, precluding the application of these techniques. As a result, investigations of their genitalia have so far been restricted to light-microscopic examination of intact structural complexes, in which individual elements remain overlapped and obscured. Consequently, observations are limited to externally visible features, hindering comprehensive interpretation of their morphology. To overcome these constraints, we applied micro-CT imaging to digitally dissect and reconstruct the male terminalia, enabling examination of their spatial organization and reassessment of structural homologies.
However, it is not only the extraordinary genital morphology, unknown among extant Keroplatidae, that makes this genus noteworthy. Kelneria is the most abundant keroplatid genus in Baltic amber, but despite this apparent prevalence, only four species have been described to date: K. abundare (Meunier, 1904), K. ciliata (Meunier, 1904), K. filiformis (Meunier, 1904), and K. setosa Matile, 1979. This discrepancy between remarkable abundance and the limited number of described species suggested that the species-level diversity of the genus has been underestimated and prompted its reinvestigation.
Application of μCT and SRμCT enabled detailed reconstruction of the male terminalia and facilitated recognition of morphological differences among the examined specimens. Consequently, in the present study we describe three new Kelneria species, although additional morphotypes were recognized within the examined material. Furthermore, our observations document its occurrence not only in Baltic but also in Rovno and Oise ambers, extending both the geographic and temporal range of the genus.
For the purpose of this study, 682 unsorted keroplatid inclusions from Baltic amber, dated to the early Priabonian (c. 36–35 Ma; Ross et al., 2026) and Rovno amber (c. 36–35 Ma; Chemyreva et al., 2024; Eskov et al., 2026) were examined. Of these, 339 specimens were identified as Kelneria, accounting for 49.7% of all examined Keroplatidae and the vast majority of Macrocerinae. Specifically, Kelneria comprised 152 of 316 keroplatid inclusions from Rovno amber (48.1%) and 187 of 366 inclusions from Baltic amber (51.1%). Additionally, type specimens (all derived from Baltic amber) from the type series of K. abundare (GZG.BST.3081, former Königsberg catalogue no. Z1582; GZG.BST.3077 = Z3063; GZG.BST.3059 = Z620), K. ciliata (GZG.BST.3048 = Z2450), K. filiformis (GZG.BST.3072 = Z2953), and K. setosa (GZG.BST.3079 = Z2680; GZG.BST.3068 = Z1247) were examined.
Photographic documentation was obtained using a Canon EOS 5D Mark IV digital camera equipped with a Canon MP-E 65 mm f/2.8 1–5× macro lens. Image stacks acquired at successive focal planes were combined into extended-depth-of-field images using Helicon Focus 8. Line drawings were prepared in CORELDRAW 2018 based on the photographs, and measurements were taken using IMAGEJ (
Scanning was performed using a customized version of the TOMOSCOPE XS PLUS 200 (Werth Messtechnik, Gießen, Germany). The specimen was scanned using 60 kV voltage, 120 µA current, an exposure time of 1500 ms and 2200 projections while averaging three images of every projection position. The resulting volume had a resolution of 2.46 µm^3 and after contrast adjustment in WINWERTH (Werth Messtechnik, Gießen, Germany) was exported as a 16-bit .rek file.
Data segmentation was performed in DRAGONFLY 3D WORLD version 2024.1 (Comet Technologies Canada Inc.) using a non-commercial license. To segment with a minimum of manual labelling, removing background graininess was the central problem. The fossil reconstruction procedure developed and performed here is as follows: (1) A segmentation threshold was set to highlight the darkest areas, which corresponded to the cavity of the fossil and black noise pixels; (2) a one-click segmentation was made by using “add to new”; (3) standard cleaning was done by using the 3D paintbrush to delete blocks of non-subject pixels and by using the “remove islands” function; (4) the region of interest (ROI) was inverted; (5) the “close” morphological function was used to collapse bright points together; (6) the ROI was re-inverted; (7) remaining noise was deleted using remove islands; (8) the “dilation” function was used until the dilated ROI exceeded the boundary of the amber cavity; (9) the “smooth” function was used with a kernel of 5 a few times as this produced more smoothing than 3; (10) the “erode” function was used a few times until the ROI was slightly inside of the boundary of the body cavity; (11) the ROI was inverted and used to mask following the standard export protocol (e.g.,
Two alternative approaches were taken. (A) At step 10 (erosion), the ROI was over-eroded and the cavity was masked with the ROI using the maximum value (10,000). The ROI was then inverted and used to mask the background at the default value (1). (B) At step 8, instead of dilating, the ROI could be smoothed directly and maximum value cavity filling was run, with subsequent background masking. Combinations of the main workflow and alternative workflows A and B were run to explore the data. The best instance for the genitalia was found when following steps 1–7 of the main workflow was run, then manual segmentation was performed to label pixels known to be part of the genitalia but which had been removed by the less sensitive methods.
Rendering was performed in DRAGONFLY on the best model, with lighting and shadows enabled and the dataset set to maximum solidity and cubic interpolation.
The X-ray µCT scans were performed at the PolyX beamline (
Fourier transform infrared spectroscopy (FTIR) was used to obtain IR spectra of the investigated amber specimens. The analyses were performed with a Nicolet iS5 FTIR spectrometer equipped with a diamond crystal attenuated total reflectance (ATR) attachment at the Institute of Systematics and Evolution of Animals, Polish Academy of Sciences in Kraków, Poland (ISEA PAS). The obtained spectra have been archived in the institutional database, in accordance with the guidelines proposed by
Nomenclature used in this study primarily follows
Original schematic illustration of the hypothetical ground plan of the Kelneria wing, showing individual sections of the radial and medial sectors. Wing vein nomenclature follows
Order Diptera Linnaeus, 1758
Infraorder Bibionomorpha Hennig, 1948
Superfamily Sciaroidea Billberg, 1820
Family Keroplatidae Rondani, 1856
Subfamily Macrocerinae Rondani, 1856
Tribe Robsonomyiini Matile, 1990
2025 †Eokelneria Hebert, Ngô-Muller & Nel: 53, figs 1, 2 [syn. nov.]
†Kelneria setosa Matile, 1979 by original designation.
Relatively small Macrocerinae with head bearing three closely grouped ocelli forming a triangle; antennae medium-sized, in males exceeding the length of the thorax but shorter than the wing; apical flagellomere ending in an apiculus; anepisternum bearing a few anterodorsal setae, rest of thoracic pleura bare; wings relatively short and broad; vein R1 short, not reaching the mid-length of the wing; basal cell small, not exceeding one-fourth of the wing length; radiomedial fusion and stem of the medial fork short; tibial spurs longer than the tibial diameter; pretarsus with well-developed empodium exceeding the claws; pulvilli small; male genitalia with strongly reduced gonostyli, appearing as small lobes at the outer angles of the gonocoxites; epandrium notched, bearing a pair of lateral processes.
†Kelneria abundare (Meunier, 1904); †Kelneria ciliata (Meunier, 1904); †Kelneria filiformis (Meunier, 1904); †Kelneria setosa Matile, 1979; †Kelneria rovnensis sp. nov.; †Kelneria erroris sp. nov.; †Kelneria szymoni sp. nov.; Kelneria oisensis (Hebert, Ngô-Muller & Nel, 2025)
The two fossil genera, Kelneria and Eokelneria, both occurred in the Eocene of Europe and share numerous morphological similarities. The general habitus of Eokelneria closely resembles that of Kelneria. Both taxa are similar in antennae (length and presence of an apiculus on the apical flagellomere), length of tibial spurs (exceeding the width of the apical tip of the tibia), overall wing venation (Fig.
Comparison of wing venation in Kelneria setosa and Kelneria oisensis comb. nov. Blue dots indicate: 1 apical margin of the basal cell; 2 termination of frm; 3 fork of M1+2; 4 fork of R2+3+4+5. The shape of the basal cell is highlighted in yellow. The wing of Kelneria oisensis comb. nov. is redrawn based on the photographic documentation provided in the original description by
The principal character used by
Holotype: MALE, preserved in an 11 × 10 × 4 mm piece of Rovno amber (
Late Eocene (Priabonian, c. 36–35 Ma), Rovno amber (Volhynian Uplift), Pugach quarry, Klesov, Rovno Oblast, Ukraine.
Antennae approx. 0.8× wing length, with distinctly separated flagellomeres densely covered with relatively long microtrichia; pedicel subequal in length to scape; palpus very large, with apical palpomere distinctly elongated, longer than subsequent one and longer than first flagellomere; Sc ending in C approx. at level of rb cell tip; m–cu joining cubital vein before level of Rs base; R2+3 approx. 0.4 length of R2+3+4+5 fork stem; epandrium deeply and broadly notched, bearing long, slender, spinulose lateral processes extending slightly beyond apices of gonopods. Female unknown.
Body (Fig.
Holotype of Kelneria rovnensis Pełczyńska & Perkovsky sp. nov. (
Holotype of Kelneria rovnensis Pełczyńska & Perkovsky sp. nov. (specimen K-32069). A Male genitalia, lateral view; B fore leg; C mid and hind legs. Volumetric renders of the genitalia (SRµCT); D ventral view; E lateral view; F dorsal view; G right quarter profile. — Abbreviations: t VIII = tergite VIII; st VIII = sternite VIII; epand = epandrium; cerc = cercus; gc = gonocoxite; gs = gonostylus; tb II–III = tibiae II–III; ta I–V = tarsomeres I–V. Remarks: spurs are indicated by yellow arrows; the empodium is indicated by a blue arrow; a row of more robust setae is indicated by white arrows.
Comparison of homologous structures of the male terminalia in Macrocera lutea Meigen, 1804, and Kelneria rovnensis sp. nov. The drawing of M. lutea is redrawn from
The species epithet rovnensis refers to Rovno region of Ukraine, from which the holotype originates.
The specimen was found in the clear piece of amber with weight 4 g and size 38 × 10 × 25mm; distinction between gonostyli and gonocoxites is unclear; shape of the anal angle of the wing is hypothesized and indicated by a dashed line, as the anal field of the wing of the holotype is folded.
Holotype: MALE, preserved in a 15 × 10 × 3 mm piece of Baltic amber (GZG.BST.03049) housed in the Geowissenschaftliches Zentrum, Universität Göttingen, Göttingen, Germany (
Holotype of Kelneria erroris Pełczyńska, Krzemiński & Soszyńska sp. nov. (specimen GZG.BST.03049). A Close-up of the head and thorax, lateral view; B wing; C interpretative drawing of wing venation. — Abbreviations: flg I = flagellomere I; scp = scape; ped = pedicel; plp III–IV = palpomeres III–IV; la = labellum; oc = ocellus; sct = scutum; anepst = anepisternum; anepm = anepimeron; kepst = katepisternum; ltg = laterotergite; med = mediotergite; h = humeral crossvein; Rb = radiobasal vein; Sc = subcostal vein; Rs = radial sector; R1 = anterior branch of radius; R2+3 = second branch of radius; R3+4 = third branch of radius; frm = radio-medial fusion; M1 = first branch of media; M2 = second branch of media; M3+4 = fourth branch of media; m–cu = medio-cubital crossvein; Cu = cubital vein; A1 = first anal vein.
Holotype of Kelneria erroris Pełczyńska, Krzemiński & Soszyńska sp. nov. (specimen GZG.BST.03049). A Male genitalia, lateral view; B volumetric render of the genitalia in lateral view (SRµCT); C interpretative drawing of genitalia, lateral view; D volumetric render of the genitalia in dorsal view (SRµCT); E fore leg; F mid leg; G hind leg; H apex of tarsus, mid leg. — Abbreviations: t VIII = tergite VIII; st VIII = sternite VIII; epand = epandrium; aed = aedeagus; gc = gonocoxite; gs = gonostylus; tb I–III = tibiae I–III; ta IV = tarsomere IV; claw = pretarsal claw. Remarks: spurs are indicated by yellow arrows; the empodium is indicated by a blue arrow; the colour coding of the genital structures is consistent with that used in Figure
Antennae approx. 0.7× wing length, with distinctly separated flagellomeres densely covered with very short microtrichia; palpus small, with apical palpomere subequal in length to the preceding one and shorter than first flagellomere; Sc ending in C distinctly before level rb cell tip; m–cu joining cubital after level of Rs base; R2+3 short, approx. 0.2 length of R2+3+4+5 fork stem; epandrium with deep, triangular notch, bearing large, triangular lateral processes with very short, dense apical setation, terminating approx. at the level of gonopods apices. Female unknown.
Late Eocene (Priabonian, c. 36–35 Ma), Baltic amber (Sambian Peninsula), Kaliningrad Oblast, Russia.
Body (Fig.
The species epithet erroris refers to a taxonomic error whereby the holotype of this species was previously included in the type series of K. abundare.
Crossvein sc–r is not illustrated in the wing drawing, as its likely positioned close to the wing base and cannot be discerned in the holotype; shape of the anal angle of the wing and apical tip of vein A1 is hypothesized and indicated by a dashed line, as anal field of the wing of the holotype is folded; specimen designated herein as the holotype originates from the type series of K. abundare as defined by Meunier (1904); this misinterpretation was subsequently retained in the generic revision by
Holotype: MALE, preserved in a 29 × 19 × 5 mm piece of Baltic amber (specimen MP/5375a). Paratype: FEMALE, preserved in the same piece of amber (specimen MP/5375b) deposited in the Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Kraków, Poland (ISEA PAS) (Figs
Antennae approx. 0.7× wing length in male, 0.5× wing length in male, with distinctly separated flagellomeres densely covered with very short microtrichia; palpus small, with apical palpomere longer than the preceding one and shorter than first flagellomere; Sc ending in C distinctly before level rb cell tip; m–cu joining cubital before level of Rs base; R2+3, approx. 0.4 length of R2+3+4+5 fork stem; epandrium with deep, triangular notch, bearing long and narrow triangular processes, terminating approx. at the level of gonopods apices.
Late Eocene (Priabonian, c. 36–35 Ma), Baltic amber, exact locality unknown.
Body (Fig.
Holotype (male, specimen MP/5375a) and paratype (female specimen, MP/5375b) of Kelneria szymoni Pełczyńska, Krzemiński & Soszyńska sp. nov. A: Male wing; B female wing, C interpretative drawing of male wing venation; D interpretative drawing of female wing venation. — Abbreviations: h = humeral crossvein; Sc = subcostal vein; sc–r = subcostal–radial crossvein; Rs = radial sector; R1 = anterior branch of radius; R2+3 = second branch of radius; R4+5 = third branch of radius; frm = radio-medial fusion; M1 = first branch of media; M2 = second branch of media; M3+4 = fourth branch of media; m–cu = medio-cubital crossvein; Cu = cubital vein; A1 = first anal vein.
Holotype (male, specimen MP/5375a) of Kelneria szymoni Pełczyńska, Krzemiński & Soszyńska sp. nov. A Close-up of the head and thorax, lateral view; B fore leg; C hind leg; D tip of the tarsus, hind leg; female. — Remarks: spurs indicated by yellow arrows; empodium indicated by blue arrow. — Abbreviations: flg I = flagellomere I; scp = scape; ped = pedicel; plp = palpus; la = labellum; oc = ocellus; sct = scutum; sctl = scutellum; anepst = anepisternum; anepm = anepimeron; kepst = katepisternum; ltg = laterotergite; med = mediotergite; t VIII = tergite VIII; t X = tergite X; st VIII = sternite VIII; epand = epandrium; aed = aedeagus; gc = gonocoxite; gs = gonostylus; cerc I–II = cerci I–II; tb I–II = tibiae I–II; ta IV = tarsomere IV; claw = pretarsal claw.
Holotype (male, specimen MP/5375a) and paratype (male, specimen MP/5375b) of Kelneria szymoni Pełczyńska, Krzemiński & Soszyńska sp. nov. A Male genitalia, lateral view; B volumetric render of male genitalia in lateral view (SRµCT); C drawing of male genitalia, lateral view; D female genitalia; E volumetric render of male genitalia in dorsal view (SRµCT); F drawing of male genitalia, dorsal view; G drawing of female genitalia, lateral view; H volumetric render of male genitalia in ventral view (SRµCT); I drawing of male genitalia, ventral view. — Abbreviations: t VIII = tergite VIII; t X = tergite X; st VIII = sternite VIII; epand = epandrium; aed = aedeagus; gc = gonocoxite; gs = gonostylus; cerc I–II = cerci I–II. Remarks: the colour coding of the genital structures is consistent with that used in Figure
The species epithet szymoni is derived from the name Szymon and is honoring Szymon Kaczmarek (University of Lodz, Poland), who provided the holotype specimen.
The two specimens are interpreted as conspecific because the position of the male relative to the female strongly suggests that they were caught in resin either while in copula (and subsequently separated by a flow of resin), during the initiation of copulation, or immediately after copulation. Sexual dimorphism is evident in overall body proportions, with the female being larger and more robust, the antennae of the female are markedly shorter (approx. 0.5× wing length), than those of the male (approx. 0.7× wing length), slight differences are also observable in wing venation R1 terminates slightly before the mid-length of the wing in the male (ending approximately at the level of Cu termination), whereas in the female it reaches approximately the mid-length of the wing (ending distinctly distal to the level of Cu termination), as shown in Fig.
Micro-CT reconstruction of the male terminalia of K. rovnensis sp. nov. (Fig.
| 1 | Epandrial notch broad and rounded, with lateral processes arising along the lateral margins of the epandrium; processes slender, spinulose in lateral view (Fig. |
2 |
| 1’ | Epandrial notch deep and triangular; lateral processes appearing triangular in lateral view (Fig. |
4 |
| 2 | Antennal flagellomeres indistinctly separated, flagellum filiform, setation of flagellomeres very short (Fig. |
K. filiformis |
| 2’ | Antennal flagellomeres distinctly separated, flagellomeres covered with long setation (Fig. |
3 |
| 3 | Maxillary palpi large, apical palpomere longer than first flagellomere (Fig. |
K. rovnensis sp. nov. |
| 3’ | Maxillary palpi small, apical palpomere shorter than first flagellomere (Fig. |
K. ciliata |
| 4 | Epandrial processes narrow, distinctly incised along the ventral margin of the epandrium, reaching gonopodal apices (Fig. |
K. szymoni sp. nov. |
| 4’ | Epandrial processes broad, ventral margin not distinctly incised (Fig. |
5 |
| 5 | Gonocoxite about as long as wide (Fig. |
K. abundare |
| 5’ | Gonocoxite distinctly longer than wide (Fig. |
K. erroris sp. nov. |
The FTIR spectra of the examined specimens display a doublet of peaks in the 1260–1160 cm–1 range, with the strongest absorption peak at approximately 1150 cm–1 (Fig.
Kelneria is remarkably abundant in Baltic and Rovno ambers; in contrast, the genus is known from a single specimen in Oise amber. However, the implications of this striking disparity in relative abundance among those deposits are difficult to assess. Baltic and Rovno ambers originated from amber forests distributed across broad geographic regions, effectively capturing multiple microhabitats and reflecting large-scale palaeoenvironments (
Our observations of Kelneria in Baltic, Rovno and Oise ambers indicate that the genus dates back at least to the earliest Eocene (c. 55–53 Ma) and was widespread and common in Eocene Europe (
Distribution of extant and fossil representatives of the tribe Robsonomyiini (yellow = extant; red = fossil). Numbers indicate different Eocene amber deposits: 1 Oise amber; 2 Baltic amber; 3 Rovno amber. Map created using the SimpleMappr online generator (simplemappr.net) and modified in CorelDRAW 2018 (coreldraw.com/en/product/coreldraw).
Comparable disjunct distributional patterns have been documented in other insect groups known from Eocene ambers. For example, in Coleoptera, the genus Dysanabatium was abundant in Eocene Europe but is today restricted to Southeast Asia (
Notably, more species of Robsonomyiini are known from Baltic amber alone than from all extant zoogeographic regions combined (Table
Species distribution of the extant and fossil representatives of the tribe Robsonomyiini. Abbreviations: Af, Afrotropical; Pa, Palearctic; Ne, Nearctic; Or, Oriental.
| Genus | Extant distribution | Fossil record | |||||
| Af | Pa | Ne | Or | Baltic amber | Rovno amber | Oise amber | |
| Kelneria | — | — | — | — | 6 | 1 | 1 |
| Calusamyia | — | — | 1 | — | — | — | — |
| Langkawiana | — | — | — | 1 | — | — | — |
| Micrepimera | 1 | — | — | 2 | 2 | — | — |
| Robsonomyia | — | 1 | 1 | — | 2 | — | — |
| Srilankana | — | — | — | 1 | — | — | — |
| Total: | 1 | 1 | 2 | 4 | 10 | 1 | 1 |
This pattern suggests that the tribe may have reached its peak diversity in the European amber forests. Consequently, the post-Eocene climatic transition, which led to the replacement of those warm, mixed evergreen forests by more temperate and increasingly seasonal vegetation in Europe, may have contributed to their disappearance from the region (
However, unlike Robsonomyia and Micrepimera, which persisted outside the continent, Kelneria is entirely absent from the extant fauna. This may reflect a more geographically restricted distribution of the genus, potentially lacking access to southeastern climatic refugia during the late Eocene cooling (
Data from the Paleobiology Database (PBDB 2025) show that a total of 545 dipteran genera are known from the Eocene of Europe, of which as many as 241 are regarded as extinct (approx. 44%). Because many fossil insect species were described before modern concepts to separate genera were established, it is possible that many may require reassignment to possibly extinct genera. If this expectation were borne out, the real scale of their extinction may be even higher. Yet, the possibility that Kelneria survived into the present day was previously hypothesised by
Although the general habitus, including body proportions, and the wing venation pattern are relatively uniform in Kelneria, pronounced interspecific variation is observed in the male genitalia, which remain the primary basis for species-level identification within the genus. Although the gonostyli are strongly reduced in all species and appear as small lobes at the outer angles of the gonocoxites, the remaining genital structures differ markedly. The biggest variation concerns the shape of the epandrium, particularly the shape of the epandrial notch. This notch may be broad, shallow and rounded, as in K. rovnensis sp. nov. (Fig.
In addition to genital morphology, important diagnostic information is provided by the mouthparts and antennae. Regarding morphology of the mouthparts, among the currently recognised species, Kelneria rovnensis sp. nov., described from Rovno amber, is the most distinctive. This species differs from other representatives of the genus in possessing large and well-developed palpi (Fig.
The evolutionary history of Kelneria presents a striking combination of morphological distinctiveness, numerical abundance, and ultimate disappearance. During the Eocene, the genus was not only geographically widespread, occurring in Oise, Baltic, and Rovno ambers, but also numerically dominant within Keroplatidae. Such abundance in Baltic and Rovno amber inclusions, even when accounting for taphonomic bias, suggests that Kelneria constituted a substantial component of forest-associated dipteran communities. Its disappearance, therefore, cannot be interpreted as the loss of a rare or ecologically insignificant taxon. Kelneria appears to represent a lineage that flourished in the equable microthermal climate of warm-temperate, humid amber forests but possibly failed to persist under middle-latitude climate with much colder winters following the Eocene–Oligocene Transition (EOT) and the restructuring of European forest ecosystems (
Taken together, these findings demonstrate that Kelneria was a distinctive, abundant, diverse, and geographically widespread Eocene genus with no known extant representatives. The reasons for its disappearance remain unknown. However, the distributional contrast between Eocene and extant representatives of the tribe Robsonomyiini suggests that this loss may have been part of a broader faunal turnover in Europe after the Eocene.
Authors’ contributions. A.P. took the lead in writing the manuscript and was responsible for material preparation, photography, and graphic illustrations. A.P. and W.K. were responsible for taxonomic decisions. B.B. and A.R. performed the laboratory micro-CT scanning, prepared the 3D reconstructions and conducted the morphological analyses. T.K. performed the synchrotron radiation micro-computed tomography (SRµCT) measurements. K.M.S. and P.K. designed and implemented the synchrotron imaging methodology and performed the 3D reconstructions. E.P. provided the examined specimen and assisted in the interpretation of the results. A.S. and W.K. contributed to the research concept and design, provided access to material, supervised the project, and secured funding. All authors critically revised the manuscript and approved the final version.
Funding. This research was funded by the National Science Center, Poland (grant no. 2020/37/B/NZ8/03042). We also thank HMWK (Hessian Ministry of Science and Arts) through the IWB-EFRE program, project number: 20009100, and SOSA (Senckenberg Ocean Species Alliance) for financing the Werth micro-CT scanner under the project title “3D-Forschung mittels hochauflösender µCT für den digitalen Zwilling von Objekten”. Research at the National Synchrotron Radiation Centre SOLARIS is supported by the Ministry of Science and Higher Education, Poland, under contract no. 1/SOL/2021/2. Evgeny Perkovsky was supported by Scholars at Risk Ukraine (SARU) program for 2026 funded by Orient’s Fond.
Conflict of interests. The authors declare that they have no conflict of interests
Use of AI. The authors acknowledge the use of ChatGPT (OpenAI, GPT-5.3; accessed April 2026) for stylistic and language improvement of the manuscript.
The authors thank Katarzyna Kopeć (Institute of Systematics and Evolution of Animals, Polish Academy of Sciences) for performing the spectroscopy analyses.