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The earliest beetle with mouthparts specialized for feeding on nectar is a parasitoid of mid-Cretaceous Hymenoptera
BMC Ecology and Evolution volume 21, Article number: 207 (2021)
During the Mesozoic, there were many insects in several holometabolous orders (Neuroptera, Mecoptera and Diptera) with elongated mouthparts adapted for feeding on nectar. The evolutionary history of the megadiverse order Coleptera, which has a great diversity of mouthparts and feeding strategies, is well documented since early Permian with a significant peak in diversity in the Triassic. Currently, however, there is no evidence that in the Mesozoic these beetles fed on nectar despite the recorded specializations for pollination of flowering plants in several families since the mid-Cretaceous.
Here we describe a new wedge-shaped beetle Melanosiagon serraticornis gen. et sp. nov. from mid-Cretaceous Burmese amber attributed to Macrosiagonini (Ripiphoridae: Ripiphorinae), which has elongated galea comparable to that in the extant parasitoid genus Macrosiagon, and a well known example of adaptation for nectar feeding in Coleoptera. Furthermore, Salignacicola gen. nov. is established for Macrosiagon ebboi Perrichot, Nel et Néraudeau, 2004, based on the holotype found in mid-Cretaceous amber from France. Systematic positions of both newly established genera are discussed. A list of potential wasp and bee hosts of Ripiphorinae from the Mesozoic is provided.
This study presents evidence of the earliest occurrence of specialized nectar feeding mouthparts in Coleoptera. Melanosiagon serraticornis is closely related to extant Macrosiagonini. In all genera belonging to subfamily Ripiphorinae the primary larvae are adapted for parasitism on aculeate Hymenoptera (bees and wasps) and adults are associated with blossoms of flowering plants, in terms of their specialized morphology. Adults of Macrosiagon visit blossoms of flowering plants to obtain nectar and lay eggs from which the hatching larvae attack visiting wasps and bees. An association with flowers of some tropical trees is already corroborated in some extant species. Interestingly the larvae of Ripiphorinae are also found in Burmese amber. Thus, both life stages of the mid-Cretaceous Ripiphorinae indicate a close association of this lineage with flowering trees.
Co-radiation of insects and seed plants (spermatophytes) is one of the most intriguing phenomena in evolution with the earliest evidence dating back to the late Paleozoic . Various specializations of insect mouthparts, feeding strategies and interactions particularly with pollination played a crucial role in the evolutionary history of both megadiverse groups [2, 3]. While the Cenozoic is clearly dominated by the radiation of angiosperms, the Mesozoic is primarily characterized by the rise of gymnosperms (conifers, Ginkoaceae and Cycadales) and appearance of angiosperms in the Early Cretaceous, which resulted in new associations between insects and plants as well as host shifts in many insect groups (e.g., [4, 5]. Hence, the Cretaceous is one of the most significant periods in respect of plant–insect co-radiation and evidence of these interactions in both groups is preserved in fossilized resin and as compressed fossils [1, 6]. Among the well-known examples of Cretaceous insect radiations are major anthophilous taxa like the bees (Apidae: Meliponini), pollen wasps (Vespidae: Masarinae), brachyceran flies (Acroceridae, Apioceridae, Bombyliidae, Empididae, Nemestrinidae, Stratiomyidae, and Syrphidae) and moths (Lepidoptera: Micropterygidae, Yponomeutoidea) . Further source of important evidence for the co-evolution is documented as plant–insect interactions in form of feeding traces, mines and galls preserved on leaves (e.g., ). While the majority of studies focus on Cretaceous evidence of direct or indirect angiosperm pollinators and/or pollinivores (e.g., [8, 9]) there are only a few on nectivorous insects feeding on floral nectar and pollen of gymnosperms during the Cretaceous (see ). The specialized nectar feeding insects with elongated mouthparts first appeared in the Late Paleozoic and diversified remarkably during the Triassic and Jurassic in orders like Mecoptera, Diptera and Neuroptera .
Currently, beetles are important pollinators and their Cretaceous record of pollination and pollinivory and co-evolution with gymnosperm and angiosperms is being more and more precisely documented for different lineages (e.g., [4, 11,12,13]). In contrast, nectar feeding is scarcely documented for extant species of Coleoptera with elongated (proboscis-like) mouthparts, such as Meloidae (Leptopalpus, Nemognatha, Gnathium and Zonitis), Ripiphoridae: Ripiphorinae (Macrosiagon), Cantharidae (Chauliognathus) and less elongated maxillary structures for nectarivory in addition to pollen-feeding as found in Scarabaeidae (Hopliini from Greater Cape Region) (see [14, 15]). Thus, it is not surprising that fossil evidence for such feeding specialization in Mesozoic Coleoptera is so far unknown, although insects with elongated mouthparts adapted for feeding on nectar at that time were much more diverse than in the Cenozoic.
The oldest known representatives of wedge-shaped beetles (Ripiphoridae) are larvae and adults from various mid-Cretaceous deposits of amber in the Northern Hemisphere . Perrichot et al.  describe males of two species of Ripiphoridae from the uppermost Albian respective Cenomanian of France as members of Ripiphorinae, however, both these species do not belong to this subfamily. The monotypic genus Paleoripiphorus Perrichot, Nel et Néraudeau, 2004 belongs to the Ripidiinae [18, 19], whereas the exact systematic placement of “Macrosiagon” ebboi Perrichot, Nel et Néraudeau, 2004, within or even outside of the family is debateable [16, 19]. Grimaldi et al.  report a syninclusion of five triungulinids as possible Ripiphoridae in Cretaceous Burmese amber. The diagnostic characters of the larvae are the same as those of extant Ripiphorinae and are placed in this subfamily by Batelka et al.  with uncertain tribal placement as the only known representatives of this subfamily from the Mesozoic.
Inclusions in Burmese amber in combination with fossils available from other Cretaceous amber deposits is an important source of taxonomic, bionomic, systematic and biogeographic data for Cretaceous Ripiphoridae and other groups of insects (e.g. [21, 22]. Here we report a new genus and species of wedge-shaped beetle from Burmese amber and the first definite adult of a Cretaceous Ripiphorinae with elongated mouthparts adapted for feeding on nectar. We also erect a new genus for mid-Cretaceous “Macrosiagon” ebboi from France, because this species cannot be attributed to Ripiphorinae as currently defined. Systematic positions of both newly established genera are discussed. In addition, a list of Mesozoic wasps and bees is provided to illustrate the availability of possible hosts for larvae of Cretaceous ripiphorine beetles.
Specimens, locality and geological setting
The holotype of Melanosiagon serraticornis gen. et sp. nov. was obtained from amber from the Hukawng Valley, Kachin State, northern Myanmar. Burmese amber, or burmite is dated to the mid-Cretaceous (lower most Cenomanian) age based on U–Pb dating of zircon crystals from the volcaniclastic matrix . The holotype is deposited in the collection of Charles University, Faculty of Science, Department of Zoology, Prague (prefix PřFUK).
The holotype of Salignacicola ebboi (Perrichot, Nel et Néraudeau, 2004) is described from amber from Salignac, near Sisteron, Alpes-de-Haute-Provence (France). The dating of this amber is uncertain, probably Cenomanian. The holotype (No. Sis 2.1) is deposited in the Laboratoire de Paléontologie, Muséum National d’Histoire Naturelle, Paris (France).
The plant material was not used in this study.
Both specimens were studied using an Olympus BX40 microscope, Olympus IX81 inverted fluorescence microscope with UIS2 objectives, Zeiss Lumar V12, Nikon SMZ745T and Leica S9D stereomicroscopes, and photographed using Canon EOS 90D digital camera attached to the microscope or a Leica S9D stereomicroscope. Olympus IX81 was equipped with an ORCA-AG monochromatic 12-bit charge coupled device camera (Hammatsu, Japan). Images taken using the inverse microscope are mirrored. For this, we used the imagej (64-bit) software (Rasband, W.S., ImageJ, U.S. National Institutes of Health, Bethesda, MD, U.S.A.). The original photographs were processed using Adobe Photoshop CS4. Some images were prepared as series of focal layers, which were then combined using the focus-stacking software Helicon Focus (Helicon Soft) or Zerene Stacker (Zerene Systems LLC).
Taxonomy and terminology
The authorship of the family Ripiphoridae and subfamily Ripiphorinae follows changes proposed by Bouchard and Bousquet .
List of abbreviations
Abbreviations for morphological structures are as follows: ml, median lobe of pronotal disc; ga, galea; md, mandible; pe, posterior edge of pronotal disc; lg, ligula; lbp, labial palpus; mxp, maxillary palpus; and RP, radius posterior.
This publication and the nomenclatural acts it contain are registered in ZooBank, the proposed online registration system for the International Code of Zoological Nomenclature (ICZN). The ZooBank LSIDs (Life Science Identifiers) can be obained and the associated information viewed using any standard web browser by appending LSID to the prefix ‘http://zoobank.org/’. The LSIDs for this publication are: urn:lsid:zoobank.org:pub:04D6E8E8-54D7-46D8-AFD6-6A57AF96A514.
Order Coleoptera Linnaeus, 1758
Superfamily Tenebrionoidea Latreille, 1802
Family Ripiphoridae Laporte, 1840
Subfamily Ripiphorinae Laporte, 1840
Tribe Macrosiagonini Heyden, 1908.
Melanosiagon gen. nov.
Type species. Melanosiagon serraticornis sp. nov.
Etymology. Generic name is a combination of the black appearance of the specimen (Greek μελάνω) and the generic name Macrosiagon . Feminine in gender. The name is registered under ZooBank LSID urn:lsid:zoobank.org:act:46B9D135-5214-4999-9F2B-0BF4133F5F7F.
Diagnosis. This genus is characterized by having a long and slender body, long elytra, acute, convex and partially dehiscent, small head, strongly flattened antero-posteriorly with vertex transversely planar, specialized mouthparts with elongated galea, bilobed ligula covered by bristles, prominent tibial spurs, tibial spur formula 2-2-2, antennae 11-segmented, mesonotal and metanotal legs with erect stiff spiniform setae, pretarsal claws serrate, abdominal segments laterally compressed, apical fields on hind wings with secondary “ghost” branches (sensu : 186) and apices of hind wings asymmetrically overlapping in resting position.
Melanosiagon serraticornis sp. nov.
Etymology. This species epithet refers to the characteristic shape of antennomeres III–X. This species name is registered under ZooBank LSID urn:lsid:zoobank.org:act:9D3499A6-664B-4073-A550-32F96AE5C1B7.
Material. Holotype: PřFUK056 (Figs. 1, 2); lowermost Cenomanian; Myanmar, Kachin, Hukawng Valley; preserved in a polished, transparent yellow piece of amber (14.4 × 10.1 × 0.53 mm). Almost completely preserved female except for four distal pro- and mesotarsomeres and distal half of antennomere XI on the right side (lost during preparation and polishing of the amber). Overall body, especially head capsule and pronotal disc show signs of desiccation of the cuticle and apices of projections on antennomeres VI, VII and XI of the left antenna were broken-off and lost before the body was entrapped in resin.
Description. Female. Body dull, black. Head capsule, orthognathous, compressed antero-posteriorly; eyes small, lenticular, prominent in lateral view; vertex transversely planar, slightly elevated above anterior margin of pronotal disc; antennae serrate, inserted in front of eyes; scapus about 2 × as long as pedicel, subcylindrical and slightly curved; pedicel short, about 2 × as long as wide, slightly narrower than scapus; antennomeres III–X distinctly serrate, flattened dorso-ventrally; projections triangular with more or less rounded apices; surface of antennomeres III–XI covered with sparse semi erect sensilla; antennomeres XI similar to preceding ones, albeit not completely preserved; ?labrum dorsally covered by erect setae, mandibles sickle-shaped, ventrally directed, with row of erect setae on their outer lateral edge; labial palpi slightly extending beyond the ligula with terminal palpomere fusiform, apices covered by erect setae; ligula in form of two lobes densely covered by bristles; maxillary palpi 4-segmented; palpomere I not fully discernible, palpomere II longest and widest at apex; palpomere III and IV equal in length; palpomere IV with acute apex; galea distinctly prolonged with surface microstructures probably microtrichia.
Pronotum convex, long, widest at base, distinctly narrower towards apex, covered with sparse semi erect setae; posterior margin of pronotum trilobate; median lobe with shallowly convex ridge reaching from base to 2/3 along length of pronotal disc; elevated process at base of median lobe absent; ventral part of prothorax dark and poorly visible.
Meso- and metathorax wedge-shaped, only poorly visible ventrally; elytra convex from base to tip, dehiscent, blade-shaped, with sharp apices; surface covered with sparse, backward-leaning semi erect setae; outer borders of elytra nearly straight, inner borders of the last quarter curved outwards.
Hind wings dark brown, folded in resting position with asymmetrically overlapping apices, reaching well beyond apices of elytra; apical fields of vein RP with dense longitudinal secondary “ghost” branches.
Legs very long and slender; tarsal formula 5-5-4; pretarsal claws straight, with comb of five short teeth and one longer apical curved tooth; prothoracic legs quite different from meso- and metathoracic legs; claws on pretarsus almost as long as protarsomere V, claws on meso- and metatarsomeres much shorter than respective ultimate tarsomere; each leg with two tibial spurs; tibial spurs short on protibia, long on meso- and metatibia; protarsomeres without distinct apical setal fringe, meso- and metatarsomeres with distinct apical setal fringe except on last tarsomere; protibia and protarsomeres covered with fine setae; meso- and metatibia covered with dense fine setae and sparse longer spiniform setae; meso- and metatarsomeres covered dorsally with fine and dense short setae, but ventrally they are covered with sparse and longer spiniform setae.
Abdomen short with 5 visible segments (sternites III–VII), much shorter than elytra, laterally compressed; abdominal segments tapering posteriorly, each partially the overlapping succeeding one; sternite VII almost acute at apex.
Measurements. Total body length as preserved approx. 430 µm; length of antennae approx. 150 µm.
Remarks. Melanosiagon serraticornis gen. et sp. nov. is easily distinguishable from other Ripiphoridae by the following combination of characters:
Head compressed antero-posteriorly with vertex transversely planar and not elevated. This character is present only in some Macrosiagonini: genus Metoecus Dejean, 1833 and Macrosiagon vittata species group sensu Falin .
Tibial spur formula 2-2-2. Complete spur formula is preserved only in basal Ptilophorinae (all genera), in Ivierhipidius  (a highly derived genus of uncertain placement , in Ripiphorinae in the genus Ripiphorus Bosc, 1791 and Macrosiagon vittata species group, and in most New Zealand Pelecotominae (whereas in most of the genera of this subfamily and in all Hemirhipidiinae there is a strong tendency for fewer tibial spurs on all legs [31, 32]).
Antennomeres III–X with distinct triangular projections. Serrate or pectinate antennae are common in females of most Ripiphoridae (with some exceptions at the species level). However, in the Macrosiagon vittata species group (see above paragraphs 1 and 2) antennal projections are thread-like, as in males of the Macrosiagon limbata species group sensu Batelka .
Elytra convex, dehiscent and covering the whole abdomen. Complete but dehiscent elytra are typical for most of the Macrosiagonini, but they are usually flattened dorsally. Convex elytra are typical for species in the Macrosiagon limbata and vittata species groups.
Apical fields on hind wings with dense longitudinal secondary “ghost” branches. A character occurring only among Ripiphoridae in Macrosiagon (e.g., : Fig. A139, : Figs. 1, 2) including the Eocene species M. deuvei Batelka, Collomb et Nel, 2006 : Figs. 1–3.
Hind wings folded in resting position with asymmetrically overlapping apices extending beyond apices of elytra. This character occurs in Ripiphoridae only in Macrosiagon. Numerous examples are available for Macrosiagon, e.g., [34: Figs. 2, 3], [29: Figs. 1, 2], [18: Figs. 1–3], [33: Figs. 2, 6, 14, 16, 19, 30, 36, 37, 39, 43, 44; [56: Figs. 1, 4, 6, 7] and others. This typical manner of hind wing folding is likely to be due to the narrow width of the wings with reduced venation, ‘compensated’ by secondary “ghost” branches in the apical field, and by a short abdomen and variably dehiscent elytra which usually do not completely cover the hind wings.
Meso- and metatibia with spiniform setae. Present also in some Ptilophorinae, but legs in this subfamily are much shorter and stronger, and the apices of tibia are much wider.
Long and prominent tibial spurs. Character occurring only in Ptilophorinae and Ripiphorinae, in all other subfamilies there is strong tendency for them to be shorter. In Pelecotominae and Hemirhipidiinae they are even partially hidden in the tibial cavity so they are hardly noticeable under low magnification using a binocular microscope (e.g., [31, 32].
Serrate pretarsal claws. Pretarsus with series of distinct teeth are present in Ptilophorinae (their number depends on the size of the specimen (Batelka, pers. obs.)), in Ripiphorus, in which the number and size of teeth is a sexual characteristic , and in Pelecotominae of South America (formerly Micholaeminae), in which all teeth are very strong and robust (Batelka, unpublished). As the teeth in all the above-mentioned groups differ in shape and number we consider this character as homoplastic, depending possibly on the surface conditions and locomotive requirements of adults. In Cenozoic Macrosiagonini the pretarsal claws are smooth and distinctly bidentate at apex.
Traits of Melanosiagon gen. nov. very convincingly place it among Macrosiagonini (see above under characters 1, 4–6); at least characters 4–6 are undoubtedly shared with Macrosiagon. Unfortunately, the metathorax in Melanosiagon gen. nov. is not discernible so it cannot be compared with Cenozoic Macrosiagonini in which the posterior half of the metepimeron is greatly expanded ventrally above the metacoxa, while the anterior half of the metepimeron evenly tapers towards the mesepimeron. Despite some characters being absent in Cenozoic Macrosiagonini (i.e., serrate pretarsal claws and meso- and metatibia with spiniform setae) we consider Melanosiagon gen. nov. to be a member of the Macrosiagonini. Falin  doubts the monophyly of Macrosiagon in respect to M. vittata species group and genus Metoecus. The phylogenetic analysis of Ripiphoridae based on molecular markers  indeed recovered Metoecus nested inside Macrosiagon (members of M. vittata species group were not available for this analysis). More data are needed to reveal which species group(s) of Macrosiagon should eventually be raised to generic status, equal to Melanosiagon gen. nov. and Metoecus. If it is accepted that bidentate pretarsal claws are synapomorphy within Cenozoic Macrosiagonini, it seems unlikely that genera in this lineage are descendants of Melanosiagon gen. nov.
Family Ripiphoridae Laporte, 1840
Subfamily incertae sedis.
Salignacicola gen. nov.
Type species. Macrosiagon ebboi Perrichot, Nel et Néraudeau, 2004.
Etymology. Combination of the name of the type locality and the Latin suffix –cola (meaning inhabitant(s)). Masculine in gender. The name is registered under ZooBank LSID urn:lsid:zoobank.org:act:D5E1D0C3-0B1C-4FA6-B2FB-1968308E3B6A.
Material. Male holotype preserved as an amber inclusion found in Salignac, near Sisteron (France), Cretaceous (Cenomanian) .
Remarks. This species is interpreted not to belong to the subfamily Ripiphorinae (to which the genus Macrosiagon belongs) by Batelka et al. . After re-examination of the male holotype, this species was tentatively excluded from Ripiphoridae, because of an unusual combination of characters: tibial spur formula 1-2-2; serrate pretarsal claws; putative biflabellate antennae (regarded as uniflabellate by [16: Fig. S3a]) with greatly prolonged thread-like antennal rami covered densely by long hair-like sensilla,reduced venation on hind wings; abdomen long, eight segmented with apex of ninth segment visible (sic), ultimate abdominal segment tapering posteriorly; very long hind legs; and very long metatibial spurs [16: Fig. S3, 17]. Its similarities in terms of characters with other Ripiphoridae considering the description of Melanosiagon gen. nov. are updated and discussed below.
Description of Salignacicola ebboi (Perrichot, Nel et Néraudeau, 2004), a species originally placed within Macrosiagonini, cannot be compared with other ripiphorids because of absence of some important information. Several of the most prominent characters of this fossil can be, however, preliminarily reconsidered in the context of certain ripiphorid lineages or genera as follows:
Tibial spur formula 1-2-2. Reduction in the number of tibial spurs is common in various lineages of Ripiphoridae (see above comments for character 2 under Melanosiagon gen. nov.) and occurs also in most Macrosiagonini.
Antennomeres III–XI (X) in males with single long projection. Character present in all Ptilophorinae, Pelecotominae and Hemirhipidiinae, and most Ripidiinae (except for several genera with filiform antennomeres and Paleoripiphorus with biflabellate antennae). In males of Ripiphorinae antennomeres III–X (IX) always have two long rami.
Thread-like antennal rami. Present in some species of Macrosiagon (see above comments for character 3 under Melanosiagon gen. nov.).
Long hair-like sensilla on antennal rami. Similar sensilla occur in several species of Ptilophorus Dejean, 1834 inhabiting Socotra, Central Asia and USA . Homology of this character in Salignacicola gen. nov. and the modern offshoot Ptilophorus, is unlikely.
Abdomen is 9-segmented. Ripiphoridae (except for Ripidiinae) have a 5-segmented abdomen. Up to seven visible segments are discernible in some fossil Ripidiinae with VIIIth and IXth segment visible as internal structures . In Salignacicola gen. nov. the reported number may be incorrect: five translucent telescopically overlapping segments would appear to be nine units. This character should be reinvestigated.
Legs long and slender with apical setal fringes on tibia and tarsomeres. Typical for Macrosiagonini (like Metoecus), Pelecotominae and Hemirhipidiinae. In Ptilophorinae they are much shorter and stronger, in Ripidiinae distinct tibial and tarsal setal fringes are absent.
Long meta(tibial) spurs. Present only in Ptilophorinae and Ripiphorinae (see above comments for character 9 under Melanosiagon gen. nov.).
Serrate pretarsal claws. Now known in both Ripiphorinae tribes, Ptilophorinae, and South American Pelecotominae (see above comments for character 10 under Melanosiagon gen. nov.).
Salignacicola gen. nov. shares characters 1, 3, 5, 8 and 9 with Ripiphorinae as the subfamily is now understood (i.e., including Melanosiagon gen. nov.), but uniflabellate antennae (character 2) excludes Salignacicola gen. nov. from Ripiphorinae more basally or it might require (depending on the shape of the sclerites on the metathorax) redefinition of this character in this subfamily. Long hair-like sensilla on antennal rami (character 4) can be interpreted as an apomorphy of the genus, but not as synapomorphy with certain recent species of Ptilophorus bearing similar sensilla. Salignacicola gen. nov. thus, may represent a stem lineage of Ripiphorinae (retaining the uniflabellate antennae of its ancestors), which went extinct at the end of Cretaceous, but its exact phylogenetic position within the subfamily will remain unclear until the critical characters of the holotype are reinvestigated using micro-CT and redescribed in accordance with the high standard of the descriptions of most of the Ripiphoridae entrapped in very transparent Burmese amber.
Coleoptera with maxillae specialized for feeding on nectar
Maxillae (and partially also the labium) in Coleoptera that feed on nectar have attracted the attention of scientists for almost two centuries. The first account of these structures in certain floricolous beetles was presented by Nicholas M. Hentz in 1828 to members of the American Philosophical Society in Philadelphia and published shortly after . He established two new genera, Chauliognathus (Cantharidae) and Macrosiagon (Ripiphoridae), in which he describes setiferous and penicillate galea, much longer than the maxillary palpus in certain species. However, Hentz also reminds readers of another well-known example of this modification of galea in the meloid genus Nemognatha Illiger, 1807. Wilhelmi and Krenn  state that proboscis-like mouth parts for feeding on nectar in beetles are found in certain genera of Meloidae, Ripiphoridae and Cantharidae. Another family, which must be added to the list, is Mordellidae, in which several species of anthophilous genera have prolonged galea. The South African genus Ctenidia Laporte, 1840 (originally placed in Ripiphoridae) has two segmented, setose and extremely thin galea, longer than half of the length of the head and almost as long as the maxillary palpus . Because males have flabellate and females’ pectinate antennae and both sexes have greatly prolonged galea, a new subfamily, Ctenidiinae was established solely for this genus . Styletous galea also occur in the Palaearctic Galeimorda , a subgenus of Variimorda Méquignon, 1946 established especially because of this peculiar structure . Similar prolonged and acute galea are also described in certain Palaearctic species of Mordella Linnaeus, 1758  and Mordellistena Costa, 1854 . While the anatomy of maxillae (especially the maxillary palpus) suitable for feeding on nectar was thoroughly investigated in three genera of Meloidae , and mouthparts of monotypic Ctenidia are described in detail by Franciscolo , analyses of the labio-maxillary complex in the speciose genera Chauliognathus and Macrosiagon are still scattered in the literature and have not been summarized or evaluated. Another specialized pollen and/or nectar feeder are the monkey beetles (Scarabaeidae: Hopliini) characteristic of the floristic hotspot in the Greater Cape Region in South Africa. In this group the mandibles and maxillae are densely bristled and the lacinia mobilis is often toothed and there are bristled galea on the maxillae [14, 44].
Labio-maxillary complex of Macrosiagonini
The tribe Macrosiagonini contains two extant genera: Metoecus and Macrosiagon. Yablokov-Khnzoryan  figures the maxillae of Metoecus with atrophied one-segmented galea, miniaturized lacinia and labium without ligula, which appear to be unsuitable for feeding on plant liquids. This is supported by the experiments and observations of Zahradník , that the adults of M. paradoxus did not consume either pollen grains or nectar, or water with sugar or animal proteins. According to this author, adults only live for 3–4 days and depend exclusively on their body fat.
The situation in Macrosiagon is quite different. Mouthparts are specialized for feeding on nectar, although the shapes of the labium and maxilla differ in the different species. Sometimes the representations of these structures in the same species by different authors differ, reflecting either incorrect identification or observation/interpretation errors, or a combination of these errors (Table 1). Hentz  established his genus Macrosiagon based on the shape of the galea in M. dimidiatum (Fabricius). The same species was supposedly investigated also by Williams  and Falin  (but see below). Gerstaecker  figures the maxillae of M. spinipennis (Gerstaecker) and maxillae and labium of M. bimaculatum (Fabricius). The last species was also studied by Yablokov-Khnzoryan . Manfrini de Brewer [50, 51] figures the maxillae and labium of M. flavipennis (Leconte) and M. excavatum (Champion). Maxillae with reduced palpus are figured for M. caffrum (Fåhraeus) and an unidentified specimen from Zanzibar by Franciscolo . The SEM photomicrographs of mouthparts of an unidentified specimen from USA (which judging from the shape of the head may be M. cruentum (Germar)) are provided by Großmann .
In the species studied the labial palpi are always short, three-segmented, ligula very prolonged (but surprisingly absent in M. flavipennis), always bilobed at apex, with both lobes greatly prolonged (tongue-like) in M. excavatum. Maxillary palpus of Macrosiagon is four-segmented (three-segmented palpus in M. bimaculatum sensu Yablokov-Khnzoryan  is likely an observation error). Lacinia is short, densely covered by setae. Lacinia is not figured as a free (separate) structure in M. dimidiatum sensu Williams  and Falin , and is more prolonged than the galea in M. excavatum sensu Manfrini de Brewer  (an observation error?). In the unidentified species from Zanzibar it is figured as atrophied (broken off?) or a knob-like process. Galea is usually acute or narrow at apex, but it is figured clavate in unidentified species from Zanzibar and sub clavate in M. caffrum.
Number and interpretation of galeomeres vary greatly among authors. Großmann  notes that her observation differs from the interpretation of Williams . Großmann  shows basal galeomere extremely prolonged and densely covered with setae, and distal galeomere short (only 100 μm long) and smooth with only a few sensilla. She stresses that Williams  considers that the basal galeomere is shorter than the distal one, which also ends in a smooth tip. Consequently, Großmann  considers Williams  observation to be a possible misinterpretation. Falin  also interprets the smooth apex of the galea as a “sclerotized tip”, not a separate structure, possibly because the suture between both segments is only visible at a high magnification using SEM. Based on the comparison of all three representatives of M. dimidiatum summarized in Table 1, there are marked differences in the measurements of particular structures of the maxilla. Despite the possible misinterpretations mentioned above, misidentification of some the specimens should also be considered. Rivnay  indicates that M. dimidiatum is often confused in collections with M. flavipennis and M. pectinatum (Fabricius), and sometimes even with M. cruentum. Thus, future studies on the mouthparts of Macrosiagon must pay particular attention to the correct identification of the material examined.
Ecology and lifestyle of primary larvae and adults of Cretaceous Ripiphorinae
It is likely that the larvae of Ripiphorinae reported by Grimaldi et al.  were trapped alive on a tree (because these weakly sclerotized creatures show no signs of desiccation), in contrast, the female of Melanosiagon serraticornis gen. et sp. nov. is slightly damaged and desiccated, with its hind wings in a resting position and, therefore, was certainly dead when entrapped in resin (not accidentally flying around a tree and caught by a chance). Both events indicate a close association of the mid-Cretaceous Ripiphorinae with trees producing resin in the area that is nowadays known as northern Myanmar. Albeit many extant species of Ripiphorus and Macrosiagon lay eggs in blossoms of certain herbaceous plants in semi-desert or desert habitats [33, 54, 55], some species of Macrosiagon occur in tropical forests (e.g., [56, 57] and are associated with inflorescences of trees, e.g., Castanopsis sp. in Laos . Their role as pollinators should also be considered because they have modified mouthparts with prolonged galea and ligula.
The specialized morphology of triungulinid larvae of Ripiphorinae in Burmese amber indicates a close parasitic relationship with their hosts, possible aculeate Hymenoptera, notably wasps, which are hosts (together with certain lineages of bees) of the extant members of this subfamily. Various groups of wasps (and maybe some bees), which are known as hosts of recent Ripiphorinae, were abundant and diverse around the World during the Cretaceous. Apoidea are recorded in amber, as compressed fossils and there are also nests of Halictidae bees in Lower and Upper Cretaceous deposits. The following families of Apoidea, Scolioidea, Tiphioidea and Vespoidea are recorded: †Angarosphecidae (15 gen., 50 spp.), †Melittosphecidae (1 gen. et sp.), †Discoscapidae (1 gen. et sp.), Sphecidae (8 gen., 9 spp.), †Cirrosphecidae (1 gen. et sp.), Crabronidae (1 gen. et sp.), Scoliidae (6 gen., 13 spp.), Pompilidae (1 gen. et sp. indet.), Tiphiidae (2 gen., 2 spp.), Vespidae (8 gen., 20 spp.) and Rhopalosomatidae (2 gen., 3 spp.). Except for the last-mentioned family, all the above-mentioned extant families are known to be hosts of extant Ripiphorinae . Thus, Cretaceous wasps and bees may have facilitated the evolution of Ripiphorinae. For detailed list of all the species recorded see Additional file 1.
Diversity of Cretaceous Ripiphoridae
In addition to the rarely seen Cretaceous Ripiphorinae and Salignacicola gen. nov., a genus of uncertain position established herein, the Cretaceous record of other Ripiphoridae is quite rich. In total, five Ripidiinae genera and seven species (including one species of Paleoripiphorus indistinguishable from the one found in France) are described from Burmese amber [11, 12, 16, 38, 59]. Unidentified longipede holometabolous primary larvae from Turonian amber of New Jersey, USA reported by Grimaldi et al.  are also abundantly recorded in Burmese amber and identified as triungulinids of Ripidiinae . This larval morphotype was later attributed to the genus Paleoripiphorus based on the conspecific syninclusion of 28 males, one female (first fossil female of Ripidiinae ever discovered) and two longipede larvae of this genus in Burmese amber .
There are also four described genera of Pelecotominae in Burmese amber (for key see ), and other morphotypes of triungulinids differing from the longipede morphotype. Grimaldi et al.  report a single conicocephalate triungulinid from the Campanian amber of Manitoba (Canada) as a possible strepsipteran larva. Another larva belonging to that conicocephalate morphotype was described subsequently by Beutel et al.  from Burmese amber as an early instar of Ripiphoridae without proposing its systematic placement. Kathirithamby et al.  reject the conclusions presented in Beutel et al.  and his colleagues, and report a third specimen of a conicocephalate larva (again belonging to a different species or even genus) from the Upper Cretaceous amber of Taimyr (Russia) as likely to be a strepsipteran larva. The Cretaceous Strepsiptera in Burmese amber are possibly a monophyletic lineage with four genera . The general morphology of their larvae is identical with that of extant lineages and thus all three conicocephalate morphotypes are considered to be Ripiphoridae [22, 63].
This study presents evidence of the earliest occurrence of specialized nectar feeding mouthparts in Coleoptera in the mid-Cretaceous ripiphorid Melanosiagon serraticornis gen. et sp. nov. in Burmese amber from the Hukawng Valley, Kachin State, northern Myanmar. The mouthparts of which are similar to the 4-segmented maxillary palpi and elongated galea, short labial palpi and bilobed ligula covered by bristles in the extant species of the parasitoid genus Macrosiagon . In addition to the structure of the mouthparts M. serraticornis has other diagnostic traits of Macrosiagonini, such as the triangular projections on the antennal flagellomeres, long elytra dehiscent posteriorly, tibial spur formula 2-2-2, erect stiff spiniform setae on meso- and metathoracic legs, pretarsal claws serrate, hind wing apices with secondary “ghost” branches and the apices asymmetrically overlap in resting position. Thus, its attribution is well supported. Salignacicola gen. nov. is newly established for Macrosiagon ebboi Perrichot, Nel et Néraudeau, 2004, based on the holotype found in mid-Cretaceous amber (Cenomanian) from Salignac, Alpes-de-Haute-Provence (France). Inclusion of Salignacicola gen. nov. in Ripiphorinae is not supported.
Microstructures like olfactory hair-like sensilla on antennae of Salignacicola gen. nov. or microscopic teeth on pretarsal claws and shape of the galea of monotypic Melanosiagon gen. nov. are decisive characters for the systematic placement of both new genera. This study demonstrates that fossils must be treated as much as possible in a similar way as their extant relatives if the researcher wants to obtain relevant data about the evolutionary significance and palaeobiology of a particular lineage. Paleoentomology must not rely on superficial similarities of habitus or terminalia, but on a rigorous discussion of the results of investigations of sensory and locomotive microstructures.
The mid-Cretaceous Burmese amber provides exceptionally well-preserved fossils of arthropods and other organisms, which offer excellent insights into the evolutionary history of particular insect groups (for review see, e.g., . The representatives of Ripiphoridae found in Burmese amber are usually very well preserved and can be compared in great detail with their extant relatives. The differences in morphology of these fossil taxa provide a mosaic of important events in the evolution of Ripiphoridae. Based on the extent and increasing quality of the research on Cretaceous specimens over the last two decades, Ripiphoridae could become one of the best represented and studied family of Mesozoic beetles. The present contribution is a small but exciting step towards this objective.
Availability of data and materials
All data generated or analysed during this study are included in this published article and its supplementary information file. Specimens investigated are accessible from public institutional collections as specified in “Methods”. New nomenclatural acts were registered in The Official Registry of Zoological Nomenclature open database—ZooBank (http://zoobank.org/).
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The authors thank Ondřej Šebesta (Charles University) for his help with setting up the Olympus IX81microscope. The authors are grateful to Anthony F. G. Dixon (University of East Anglia, Norwich, United Kingdom) for improving the English. The authors thank Mario Schadel and two anonymous reviewers for their comments and suggestions on an version of this manuscript. This study is a contribution to a project funded by the Grant Agency of the Czech Republic (No. 21-05216S).
Both authors acknowledge the financial support of the Grant Agency of the Czech Republic (No. 21-05216S).
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Batelka, J., Prokop, J. The earliest beetle with mouthparts specialized for feeding on nectar is a parasitoid of mid-Cretaceous Hymenoptera. BMC Ecol Evo 21, 207 (2021). https://doi.org/10.1186/s12862-021-01930-6
- Nectar feeding mouthparts