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784 tocWho’s that girl? A singular Tropiduchidae planthopper from the Eocene Baltic amber (Hemiptera: Fulgoromorpha)

Jacek Szwedo and Adam Stroiński

Article number: 20.3.60A
Copyright Palaeontological Association, December 2017

Author biographies
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Submission: 19 May 2017. Acceptance: 21 November 2017

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A new tribe of Tropiduchidae planthoppers is described from the Baltic amber–Gedanotropidini trib. nov., with a new genus and species Gedanotropis sontagae gen. et sp. nov. A key to the tribes and genera of Tropiduchidae from the Eocene Baltic amber is presented. Use of FT-IR spectrophotometry for confirmation of provenance of museum material and its documentation is proposed. The ecoevolutionary consequences of particular morphological characters of the new taxa and ‘flatoidinisation syndrome’ are introduced and discussed.

Jacek Szwedo. Laboratory of Evolutionary Entomology, Department of Invertebrate Zoology and Parasitology, Faculty of Biology, University of Gdańsk, 59, Wita Stwosza St., PL80-308 Gdańsk, Poland.
Adam Stroiński. Museum and Institute of Zoology, Polish Academy of Sciences, 64, Wilcza St., PL00-679 Warszawa, Poland.

Keywords: new tribe; new genus; new species; ‘flatoidinisation syndrome’; Baltic amber

Final citation: Szwedo, Jacek and Stroiński, Adam. 2017. Who’s that girl? A singular Tropiduchidae planthopper from the Eocene Baltic amber (Hemiptera: Fulgoromorpha). Palaeontologia Electronica 20.3.60A: 1-20.

Copyright: December 2017 Palaeontology Association.
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The Tropiduchidae Stål, 1854, the family of planthoppers (Fulgoromorpha) comprising more than 180 genera with over 650 species (Bourgoin, 2017) is currently a highly diversified group morphologically, ecologically and taxonomically. Their size ranges from 5 to 13 mm in length (O’Brien and Wilson, 1985; O’Brien, 2002). Recent Tropiduchidae inhabit a wide range of habitats across the globe, from warm and wet tropical and subtropical forests, to dry and semi-dry deserts and savannahs (Fennah, 1982; Gnezdilov, 2012b; Bourgoin 2017). Some species are known as crop pests, but most species feed on shrubs and trees (Fennah, 1982; Wilson et al., 1994; O’Brien, 2002) and particularly Arecales and Gentianales that represent about 25% of the records (Bourgoin, 2017).

The higher classification of the family was for the first time developed by Melichar (1914). Later, Fennah (1982) proposed a new classification system. The most recent proposal (Gnezdilov, 2013b) divides the family into two subfamilies. During the last few years both fossil and recent Tropiduchidae attracted attention of researchers (Szwedo, 2000; Wang R.R. and Liang, 2006, 2007, 2008, 2011; Shcherbakov, 2006; Gnezdilov, 2007, 2012a, 2013b; Fletcher, 2008; Liang and Wang R.R., 2008a, 2008b; Wang R.R. et al., 2009, 2012a, 2012b, 2013a, 2013b, 2014, 2017; Stroiński and Gnezdilov, 2009; Szwedo and Stroiński, 2010, 2013; Gnezdilov, 2012a, 2012b, 2013b; Chang and Chen, 2014a, 2014b; Constant, 2015; Gnezdilov and Bourgoin, 2015; Junkiert and Walczak, 2015; Stroiński et al., 2015; Wang M.L. et al., 2015; Gnezdilov et al., 2016; Junkiert et al., 2017). As a result of these, the total number of tribes recognised currently raised to 24 (some of them subdivided into subtribes), including four extinct ones (Appendix 1). Finally, after a number of taxonomic changes, shifting of several groups to Tropiduchidae from other families, together with description of extinct tribes, the definition of the family became rather vague (Bartlett et al., 2014, Gnezdilov et al., 2016). As a result we are now without a single autapomorphic character allowing a clear and simple definition of family, which questions its monophyly in current status and content. The phylogenetic investigations on the Tropiduchidae are at their infancy, with the only phylogenetic work done for the tribe Tropiduchini at the moment (Wang et al., 2017).

The oldest fossil record of the family is that from the Turonian, the Upper Cretaceous (Szwedo, 2009; Nicholson et al., 2015), but the formally described taxa comes from the Eocene Baltic amber—extinct tribes Jantaritambini, Austrini and Patollini, and recent tribe Elicini (Szwedo and Stroiński, 1999, 2010, 2013; Szwedo, 2000)—and from the Lutetian (middle Eocene) deposits of the Green River Formation with extinct Emilianini (Shcherbakov, 2006). The fossil described below cannot be placed in any of the currently recognised tribes of Tropiduchidae, and represents another extinct and peculiar group of these planthoppers. This fossil still brings more questions on morphological characters and their disparity within the taxa attributed to the Tropiduchidae—classification, relationships and evolutionary history of the family.


Baltic amber has been a subject of longstanding debates about its botanical origin, formation and age, about its accumulation and origin of its deposits. The biggest concentration of amber in the deposit, in the Gulf of Gdańsk (Sambian Peninsula to Chłapowo), is definitively secondary one; the other deposits, i.e., Górka Lubartowska amber (Lublin Region, Poland), Ukrainian amber (deposits near Klesov, Rovno and Zhitomir; Bogdasarov, 2010; Perkovsky et al., 2010), Bitterfeld amber (Rascher et al., 2008; Wolfe et al., 2016) are variously aged and secondary as well. Absolute dating analyses of glauconites from Sambia Peninsula showed that the “blue earth” formation (amber bearing Prussian Formation) is allocated to the Middle Eocene (Lutetian: 44.1 ± 1.1 Ma) and is thus significantly older than previously assumed (Wappler, 2003, 2005). Limnic sediments of Eckfeld Maar, aged 44.3 ± 0.4 Ma, correlate with K-Ar radiometric data from the Sambia Peninsula and contain insect genera known only from Baltic amber (Wappler 2005). For details and overview of discussions see supplementary information in Szwedo and Drohojowska (2016) and Kosmowska-Ceranowicz (2017).

s figure1The studied specimen is a piece of transparent amber, polished in form of irregular plate; weight 12.66 g, size 50 × 32 × 11 mm. Reference IR curves of the piece numbered as MAI UG 508762 IR are deposited in MAI UG (Museum of Amber Inclusions, University of Gdańsk, Gdańsk, Poland)(Figure 1.1-2). Inclusion of Gedanotropis sontagae gen. et sp. nov. (Figure 1.3-4)—dorsal portion is partly covered with milky veil and some bubbles of gas obscuring the specimen; right tegmen is partly damaged; left tegmen with apical portion missing; ventral surface of the inclusion is partly obscured by milky veil, internal cracks and bubbles of gas. Syninclusions are two specimens of Collembola: Symphypleona: Sminthuridae (one partly damaged) and small particles of detritus.

Amber was cut, grinded and polished prior the study. Observations and documentation were made using stereoscopic microscope Olympus SZH10, Olympus DSX100 free angle wide zoom microscope, and stereoscopic microscope Leica M205A. The photographs were taken using Olympus C-5060 digital camera under QuickPHOTO 2.0 software attached to Olympus SZH10 microscope, Olympus DSX100 microscope, and with Leica DM6000 attached to Leica M205A microscope under control the LAS Montage multifocus. Photographs were readjusted using Adobe Photoshop Elements 6.0 software. Drawings were made with camera lucida attached to Olympus SZH10 and Leica M2015A microscopes.

The number of rostrum segments in Fulgoromorpha varies from 3 to 5 (Brożek et al., 2006); thus, for numbering of rostrum segments we propose the following nomenclature, counting from a base: basal segments 1-3 (there can be one, two or three segments basad of subapical one); subapical segment and apical segment.

Venation of wings is based on Bourgoin et al. (2015), with following abbreviations:

Pc+CA, precosta + costa anterior; CP, costa posterior; ScP, subcosta posterior; R, radius; ScP+R(+MA), common portion of subcosta posterior, radius and media anterior; MA, media anterior is always fused with vein R (apomorphy of the Hemiptera), so we use here abbreviated notion ScP+R denoting this common stem (Bourgoin et al., 2015); ScP+RA, common portion of subcostal posterior and radius anterior; RA, radius anterior; RP, radius posterior (with MA fused); MP, media posterior; CuA, cubitus anterior; CuP, cubitus posterior; Pcu, postcubitus; and A1, first anal vein. The naming and numbering of cells and areas of the tegmina is also based on Bourgoin et al. (2015).

FT-IR spectrum (Figure 1.1-2) was obtained in the Laboratory of the International Amber Association, Gdańsk, Poland with Nicolet iS10 Spectrometer with an ATR (Attenuated Total Reflectance; diamond crystal) accessory. Spectra were registered with resolution 4 cm-1, baseline correction and advanced ATR correction were applied. Reference curve numbers in the collection archives are stored as registration number of the specimen, with suffix ‘IR’. This procedure must be regarded now as obligatory for the museum material, especially holotypes, for various reasons. First, there are numerous fakes offered in the market (Grimaldi et al., 1994), and the type of amber or fossil resin must be examined to receive confirmation of its kind. The fakes could be made in various ways, e.g., by autoclaving the more recent resins rich in inclusions, such as Colombian copal. Second, Baltic amber and other resins are altered due to process of autoclaving (treatment with heat and pressure), which sometimes gives the benefits for investigations removing the “milky veil” often present on the inclusions, on the other hand it could heavily alter the inclusion, its dimensions or shape of important taxonomic features (Szwedo and Sontag, 2009). Such treatment is to be identified with use of FT-IR spectrum (Wang Y. et al., 2014; Kosmowska-Ceranowicz, 2015). The knowledge about the treatment is important for curatorial purposes, as treated amber could deteriorate much faster than the raw, polished-only one (Bisulca et al., 2012).


Class INSECTA Linnaeus, 1758
Order HEMIPTERA Linnaeus, 1758
Family TROPIDUCHIDAE Stål, 1866
Subfamily ELICINAE Melichar, 1915
Tribe GEDANOTROPIDINI trib. nov.

Type genus. Gedanotropis gen. nov., designated herein.

Etymology. The generic name is derived from the Ancient Greek stem ‘trop-‘ (nominativus), ‘tropid-‘ (genetivus), of the word ‘τρόπισ; τρόπιδος’ - trópis, trópidos (keel of the ship), i.e. according with ICZN (2000) Article 29.3.1, the stem ‘tropid-‘ must be used for creation family-group taxon name.

Diagnosis. Vertex, disc of pronotum and disc of mesonotum in ascending, stepwise planes. Tegmen macropterous with full venation developed; costal area present, with transverse veinlets; nodal line absent. Gonoplac rounded, its median, membranous part without denticles.

Description. Frons with median carina; clypeus with median carina and without lateral carinae. Antennal plate organs present in apical and dorsal portion to half of pedicel length. Mesonotum without median carina, lateral carinae converging anteriad. Vertex, disc of pronotum and disc of mesonotum in ascending, stepwise planes. Mesonotum elevated, with intercarinal median disc flattened. Tegmen wide, costal area with transverse veinlets; anterior margin strongly curved at base, clavus long, with apex exceeding ¾ of tegmen length; tornus absent. Stem ScP+R and stem RP(+MA) leaving basal cell at a single point; stem MP short, branch MP1+2 forked basad of branch MP3+4 forking. Clavus with transverse veinlets. Metatibia with lateral spines. Gonoplac rounded; posterior margin without teeth; membranous part medially without denticles (Figure 2, Figure 3, Figure 4).

s figure2Remarks. The tribes of Tropiduchidae, as understood nowadays, are defined by combination of various characters. Vertex, disc of pronotum and mesonotum of Tropiduchidae are placed in a single plane, making the stepwise planes in the newly described tribe exceptional and apomorphic. Representatives of the family vary in length and structure of tegmina, with costal area present or absent, with or without transverse veinlets. In ‘typical’ Tropiduchinae, the nodal line is present and developed variously, however in Elicinae the nodal line could be absent or partly developed. The variability is observed also in presence or absence and degree of development of transverse veinlets on clavus. Also the armature of metatibia vary strongly among tribes of Tropiduchidae. In Fennah’s 1982 classification scheme a combination of male gonostyli and female gonoplac is an important character at the tribal level. Unfortunately, only female characters are available here. Rounded gonoplac is characteristic for the Elicinae, but lack of any teeth or denticles and membranous median portion are apomorphic character states for the new tribe.

Type horizon. Middle Eocene.

Genus GEDANOTROPIS gen. nov.

Type species. Gedanotropis sontagae sp. nov., designated herein and by monotypy.

Etymology. Generic name is derived from old Latin name of City of Gdańsk, Gedanum, and Ancient Greek noun τρόπ-ις; τρόπιδ-ος (tróp-is, trópid-os) meaning keel of the ship, and being the core for generic name Tropiduchus (from Ancient Greek τρόπ-ις (trop-is) and ἔχω (ékhō): have, hold, possess, of property). Gender: masculine; 3rd declension.

s figure3Diagnosis. Head with compound eyes narrower than pronotum. Vertex wider than long in mid line, with all margins carinate. Frons with lateral margin elevated. Mesonotum with lateral carinae connected at base. Base of tegmen strongly curved; costal area reaching half of tegmen length, wide at base, tapered apicad, with regular transverse veinlets; postcostal cell distinctly narrower than costal area; main stems forked in following sequence: ScP+R(+MA) forks first very shortly after the basal cell; MP forks later but very early in the first fifth on the tegmen separating a very long C3; CuA forks at mid length of clavus; all stems forked again in basal ⅓ of tegmen length; single apical line of transverse veinlets present. Hind wing with two transverse veinlets rp-mp and mp-cua present. Metatibia with 5 lateral spines and 8 apical teeth. Apex of anal tube exceeding posterior margin of gonoplac. Lateral portions of female pregenital sternite narrower than median portion, tapering laterad.

Description. Head with compound eyes about as wide as mesonotum; vertex wider than long in mid line, with all margins distinctly carinate; anterior margin widely quoin-shaped, posterior margin arcuately incised, lateral margins merely longer than length at midline, parallel; disc of vertex without median carina (Figure 2.2, Figure 4.1, 4.3). Vertex and frons connected at right angle. Frons with lateral margins elevated, median carina keel-shaped. Disc of frons between median carina and lateral margins with parallel ledges, not reaching dorsal margin nor frontoclypeal suture. Compound eyes bulging, higher than wide in lateral view, with small posteroventral callus. Ocellus present, at cross of anterior and lower margins lines. Antennal fovea elevated, placed under the compound eye, close to it ventral margin, scapus as long as wide, pedicel about twice as long as wide, a bit wider apically than at base, antennal plate organs present in apical and dorsal portion to half of pedicel length (Figure 2.1-2, Figure 4.1-2, 4.5).

s figure4Frontoclypeal suture angulate. Clypeus with elevated median carina and without lateral carinae; median portion, below frontoclypeal suture, slightly convex (Figure 2.2, Figure 4.2, 4.5).

Rostrum (Figure 4.5) 4-segmented, all segments well sclerotised; 1st basal segment longer than wide, 2nd basal segment the shortest, with triangular membranous part at base, subapical segment the longest, apical segment distinctly longer than wide, shorter than subapical one; apex of rostrum reaching base of hind coxae.

Pronotum (Figure 2.1, Figure 4.1, 4.3) longer than vertex in mid line, anterior margin angulately incised, with apex reaching half of compound eyes length; posterior margin widely arcuate; disc of pronotum delimited by strongly elevated, carinate anterior margin, not stepping on paradiscal field of pronotum, posterior margin distinctly elevated, disc of pronotum lacking median carina; plane of disc of pronotum above plane of disc of vertex.

Mesonotum (Figure 2.1, Figure 4.1, 4.3) longer in mid line than cumulative length of vertex and pronotum, anterior margin rounded, posterior margin angulate; disc of mesonotum with plane area distinctly elevated above plane area of pronotum, flat, delimited by lateral carinae connected at base; disc of mesonotum distinctly shifted from anterior margin, lateral margins widely diverging posterolaterad to the level of lateral angles of mesonotum, then angulately curved, converging posteromediad at short distance and not reaching posterior margin of mesonotum.

Tegula huge, without carina.

Profemur (Figure 4.5) slightly laterally compressed, subpentagonal in cross section, dorsal margin with row of short setae, anteroventral ridge with row of short thorns apically; protibia subtriangular in cross section; basitarsomere short, midtarsomere and apical tarsomere subequal in length, tarsal claws huge, arolium wide.

Mesofemur (Figure 4.5) slightly longer than profemur, subpentagonal in cross section, dorsal margin with row of short setae, anteroventral ridge with row of short thorns apically; mesotibia longer than protibia, subtriangular in cross section; basitarsomere short, midtarsomere and apical tarsomere subequal in length, tarsal claws huge, arolium wide.

Metacoxa large, metacoxal process invisible.

Metafemur (Figure 2.5) slightly flattened, ventral margins ridged; metatibia long, with 5 lateral spines (the basal one not clear on left metatibia) and a row of 8 apical teeth; basitarsomere longer than cumulative length of mid- and apical tarsomeres, with row of 7 apical teeth; midtarsomere short, with lateral teeth distinct, median lobe distinct, with apical margin extending apices of lateral teeth, covered with dense and strong setae; apical tarsomere shorter than basitarsomere, tarsal claws distinct with subbasal teeth with two setae, arolium wide.

Tegmen (Figure 2.3, Figure 3, Figure 4.3, 4.4) about 2.5 times as long as wide, membranous, with dense and distinct venation. Costal margin strongly curved at base, then almost straight, parallel to posterior margin; anteroapical angle widely rounded, apical margin round, with breaking point at about median axis of tegmen, posteroapical angle widely angulate, tornus (postclaval margin) absent, apex of clavus exceeding ¾ of tegmen length, clavus closed, acute. Costal area well developed, very wide at base, tapering toward apex, intersected with slightly oblique veinlets, slightly exceeding half of tegmen length. Postcostal cell narrower than costal area, tapering distad, with a few transverse veinlets. Basal cell longer than wide. Stem ScP+RA and stem RP(+MA) leaving basal cell with a very short stalk, stem ScP+RA distinctly curved at base, forked distad of stem RP(+MA) forking, reaching anterior margin basad of anteroapical angle with 8 terminals; stem RP(+MA) forked at level of branch MP1+2 forking, then both branches forked again on corium, slightly basad of end of costal area; branches reaching anteroapical angle with 10 terminals. Stem MP short, forked at distance of basal cell length; branch MP1+2 forked basad of branch MP3+4 forking, branch MP3+4 forked slightly apicad of stem CuA forking; branch MP1 forked on corium, slightly basad of branch MP2 forking, then forked basad of apical line of veinlets, reaching margin with 3 terminals; branch MP2 forked on corium, then on membrane, basad of apical line of veinlets, reaching margin with 5 terminals; branch MP3 forked on corium and membrane, reaching margin with 5 terminals; branch MP4 forked on corium, apical of first forking of branch MP3, reaching margin with 2 terminals; stem MP reaching apical margin with 15 terminals. Stem CuA forked slightly basad of branch MP3+4 forking, branch CuA1 forked on corium and membrane, reaching margin with 3 terminals; branch CuA2 single. Claval veins Pcu and A1 fused at about ½ of tegmen length, fused stem Pcu+A1 reaching posterior margin of clavus slightly basad of apex of clavus.

Cell C1 longer than cell C3, closed posteriorly with transverse veinlet placed apicad of ScP+R and RP1 (+MA) forkings. Cell C2 shorter than cell C1, closed with transverse veinlet 1r-mp apicad of RP(+MA) and MP1+2 forkings. Cell C3 about 1.5 times as long as cell C2, closed with transverse veinlet 1im placed apicad of stem MP2 first forking. Cell C4 longer than cell C2, closed by transverse veinlet mp-cua placed slightly apicad of branch MP3+4 and CuA forkings. Cell C5 the shortest, closed with icua veinlet basad of claval veins junction.

Several not regularly dispersed veinlets on remigium present, and arcuate apical line of veinlets present. Clavus with four transverse veinlets between CuP and Pcu, two transverse veinlets between Pcu and A1 basad of junction.

Functional nodal line of transverse veinlets absent; corium with sparse transverse veinlets; membrane with dense and irregular net of transverse veinlets, apical line of veinlets distinctly developed. Apical cells longer than wide.

Hind wing (Figure 2.4, Figure 4.3-4) slightly shorter than forewing, wide, without costal area, with angulate anteroapical angle and only 2 transverse veinlets rp-mp, and mp-cua. Stem ScP+R(+MA) forked basad of wing coupling lobe, ScP+RA1 short, oblique, reaching margin at level of transverse veinlets rp-mp and mp-cua; terminal RA2 reaching margin distinctly basad of anterior angle of hind wing with single terminal. Branch RP(+MA) forked from ScP+R(+MA) distinctly basad of rp-mp veinlet, at level of branch CuA1 first forking forked distinctly apicad of rp-mp veinlet; branch RP1+2 forked slightly apicad of rp-mp veinlet, with two terminals reaching margin basad of anteroapical angle; terminal RP3 (+MA) reaching margin at anteroapical margin. Stem MP forked apicad of stem ScP+R forking, at level of branch CuA1 first forking; branch MP1+2 forked slightly apicad of transverse veinlet rp-mp, basad of branch MP3+4 forking, reaching margin with four terminals MP1a and MP1b, forking basad of terminals MP2a and MP2b forking; branch MP3+4 forked apicad of branch MP1+2 forking, terminal MP3 single, terminal MP4 forked just before apex; stem M reaching margin with 7 terminals in total. Stem CuA multiforked, first furcation slightly basad of stem ScP+R forking; branch CuA1 forked again at level of stem MP furcation, branch CuA1a reaching margin as single terminal, branch CuA1b forked again distinctly basad of mp-cua veinlet, reaching margin with two terminals; branch CuA2 forked sequentially downwards, first terminal, CuA2c forked slightly apicad of branch CuA1b forking, at level of branch ScP+RA forking, second terminal, CuA2b forked at level of transverse veinlets rp-mp and mp-cua, terminal CuA2a parallel to CuA1b2, terminals CuA2b and CuA2c parallel, shifted to end of CuP. Stem CuP single, reaching margin basad of end of RA2 terminal.

Female terminalia (Figure 2.6, Figure 4.6). Pregenital sternite with distinct transverse bulbosity at base, and two eminences; lateral portions tapering laterad, directed posterolaterally; posterior margin strongly deflected, basally of this deflection two rounded cavities, transversely striated, incised deeply at margin deflection, separated by triangular ridge. Anal tube elongate, oval, with apex exceeding posterior margin of gonoplacs. Gonoplac rounded, with obtusely rounded pyramidal eminence medially; posterior margin with narrow, elongate, membranous part, placed below half of gonoplac height, without denticles (smooth).

Type horizon. Middle Eocene.

Gedanotropis sontagae sp. nov.
Figure 2, Figure 3, Figure 4

Type material. Holotype: female, Baltic amber inclusion, MAI UG 508762; deposited in Museum of Amber Inclusions, University of Gdańsk, Gdańsk, Poland.

Etymology. The specific name is dedicated to our great friend, Dr. Elżbieta Sontag, eminent specialist on fossil and recent Diptera: Ceratopogonidae, Curator of Museum of Amber Inclusions, University of Gdańsk, Gdańsk, Poland.

Type horizon. Middle Eocene (Lutetian).

Type locality. Baltic amber (secondary deposit, Gulf of Gdańsk area).

Diagnosis. Lateral margins of vertex about 1.3 times as long as vertex in mid line. Tegmen with 9 terminals of branch ScP+RA, 10 terminals of branch RP, 15 terminals of branch MP. Cell C1a shorter than cell C1b; cell C3a slightly shorter than cell C3b, cell C5’ open to the margin; cells C2 and C4 closed, with transverse veinlets well anteriad of half of tegmen length. Combined length of hind leg mid- and apical tarsomere exceeding length of basitarsomere.

Description. Plane of vertex at right angle to plane of frons. Metatibio-tarsal formula 8 : 7 : 2[+ setiferous lobe]. Hind wing with stem MP reaching margin with 7 terminals, branch CuA1 with 3 terminals, branch CuA2 with 3 terminals. Female anal tube slightly longer than broad.

Measurements (measurements could be slightly biased due to optical properties of amber): Total length 16.5 mm, length of body 12.8 mm. Head with compound eyes 3.3 mm; vertex at anterior margin 18.75 mm, at posterior margin 2.0 mm, 0.48 mm long at mid line, 0.62 mm long measured at lateral margin. Frons at mid line 2.35 mm long, at lateral margin 2.7 mm long; clypeus 0.96 mm long. Rostrum 2 mm long, subapical segment 1.05 mm, apical segment 0.6 mm long. Pronotum 0.75 mm long at mid line, 3.85 mm wide. Mesonotum 3.5 mm long at mid line, 3.2 mm wide. Tegmen 14.7 mm long, 6.8 mm wide at widest point. Profemur 2.5 mm long, protibia 3.0 mm long, protarsus 1.15 mm long, basitarsomere 0.3 mm, mid tarsomere 0.35 mm, apical tarsomere with claws 0.75 mm; Mesofemur 2.7 mm long, mesotibia 3.4 mm long, mesotarsus 1 mm long, basitarsomere 0.35 mm, mid tarsomere 0.35 mm, apical tarsomere with tarsal claws 0.75 mm. Metafemur 2.55 mm long, metatibia 4.6 mm long, metatarsus 1.5 mm long, basitarsomere 0.85 mm long, midtarsomere 1.25 mm long, apical tarsomere 1.25 mm long, combined length of basi- and mitarsomeres 1 mm.


Classification and Morphological Characters

Some Tropiduchidae superficially resemble Dictyopharidae but the small second metatarsus bearing a distinct spine on each side allows an easy distinction. However, the “classic” two characters differentiating Tropiduchidae from other Fulgoroidea families (Brues et al., 1954; O’Brien and Wilson, 1985; Naumann et al., 1991; O’Brien, 2002),—i.e., 1) presence of the groove or fine line separating the apex of the mesonotum (mesoscutellum) from the rest of the mesonotal disc and 2) apex of tegmina bearing more numerous veinlets set off by the nodal line (in most representatives)—appeared to be of limited value. Moreover, no clear idea about the relationships of the recognised tribes within the family has ever been presented, and no strong evidences for monophyly of these taxonomic units are available.

Classification and subdivisions of the family have been proposed several times, since pioneering works by Melichar (1914) and Muir (1923), to the most recent higher classification proposed by Fennah (1982), who listed 120 genera discriminated into 15 tribes. Up to date183 genera, distributed within 24 tribes separated within 2 subfamilies, are known (Gnezdilov, 2013b, Bourgoin, 2017). The subfamily Tropiduchinae Stål, 1866 to which all tribes listed by Fennah (1982) belong, represents the so-called “typical tropiduchid” with an elongate ovipositor and elongate gonoplacs with marginal teeth (except the genus Durium Stål, 1861) and with a triangular (in shape of isosceles triangle) posterior connective lamina of gonapophyses IX (Gnezdilov, 2003, fig. 35). The subfamily Elicinae Melichar, 1915 (senior synonym of Gaetuliina Fennah, 1978) can be distinguished by rounded (hemispheric in Elicini Melichar, 1915 or flat in Parathisciini; Gnezdilov, 2013b) gonoplacs without teeth or with small denticles and by elongate (not triangular) posterior connective lamina of gonapophyses IX (Gnezdilov, 2013b).

One important and particularly noticeable feature of Gedanotropis gen. nov. is absence of the metacoxal process. In modern Fulgoroidea it is always present as a spine-like, sometimes sulcate or spatulate.

Disparity in Extinct and Extant Tropiduchid

As for modern tropiduchids, diversity and disparity of Tropiduchidae in the Eocene Baltic amber remain unexplained. However, the fossils from Baltic amber in majority of cases belong to separate and different lineages from the present tribes. This could result from several reasons. First, it could be the real indication of particular diversity and disparity of Tropiduchidae in the habitats of the Baltic amber forests. Tropiduchinae are represented among Baltic amber inclusions only by Jantaritambini while all other taxa belong to Elicinae: Elicini, Austrini, Patollini and Gedanotropidini trib. nov. described above. Except for Elicini ( Tritophania patruelis Jacobi, 1938) all tribes recorded from Baltic amber are exclusive for this resin (Appendix 2). Second, the fossil record of the other Tropiduchidae tribes is scarce and most of them have not been recognised and reported. Third, the evolution and adaptation of many of Tropiduchidae taxa were related with host plants lineages rapidly evolving during the Palaeogene and these fossils had low fossilisation potential.

Issidisation and Flatidinisation Syndromes

It must be noted that similarly to modern Tropiduchinae and Elicinae, among Baltic amber inclusions, the forms with ‘issidisation syndrome’ (Gnezdilov, 2013a), are present, i.e., Austrini and Patollini. Such kind of body constitution, i.e., stocky, almost ovoid shape, with brachypterous wings, were already explained by Fennah (1967) as factors allowing to save water by reducing the body surface, facilitating cold resistance and female fecundity, and enhancing the hopping ability, whereas brachyptery would also facilitate mobility in the dense and coarse fynbos vegetation which would hinder flight. Denser integument and a more compact body were also regarded as morphological adaptations to arid climate in planthoppers of the subfamily Orgeriinae Fieber, 1872 of the family Dictyopharidae Spinola, 1839 (Emeljanov, 1980). Brachyptery in true bugs of the family Nabidae Costa, 1852 was noted as characteristic of species living in low and sparse vegetation (Kerzhner, 1981). Among fossils from the Baltic amber brachypterous forms were recorded also among Cicadellidae leafhoppers (Szwedo, 2002; Dietrich and Gonçalves, 2014).

The newly described genus Gedanotropis represents the tribe with fully developed wings, and lack the “issidisation syndrome”, similarly to the early described genus Tritophania Jacobi, 1938, representing also fully winged Elicini. In reverse, the new fossil expresses a particular characteristic tegmina shape: subquadrate shape of tegmen, anterior portion of costal margin strongly curved and shifted anteriad, costal margin undulate, polymerization of longitudinal veins and tegmina tent-like fashioned or hold flat (horizontally). Such constitution is known in various other planthopper families (Fulgoridae, Ricaniidae, Flatidae) and is quite common among other representatives of the family Flatidae Spinola, 1839, e.g., subfamily Flatoidinae Melichar, 1901. As for ‘issidisation’ we recognise here a special morphological trend that we call ‘flatoidinisation’. It could be assumed per analogiam to habitats of modern representatives of Flatoidinae, that Gedanotropidini inhabited forests and “flatoidinisation” would indicate their analogous mimetic abilities (O’Brien, 2002) to hide on tree-trunks or lichens covering the bark.

Higher Fulgoroidea Radiation

The ancestral forms of higher fulgoroid planthoppers are difficult to determine since their fossil record is scarce (Shcherbakov, 2006). According to the results of molecular analyses (Urban and Cryan, 2007), families of the issidoid group are young (advanced) taxa. Indeed, fossil representatives of Nogodinidae have been known only since the late Palaeocene (Shcherbakov, 2006), those of Tropiduchidae, since the Late Cretaceous (Szwedo, 2009; Nicholson et al., 2015), those of Issidae, since the Eocene (Gnezdilov and Bourgoin, 2016), Caliscelidae since the Miocene (Bourgoin et al., 2016) whereas no fossil data are available for Acanaloniidae Amyot and Audinet-Serville, 1843 (Szwedo, 2002; Shcherbakov, 2006). According to Szwedo (2002), families of the issidoid group must have originated at the Cretaceous-Palaeogene boundary (66 Mya) and diverged widely during the Eocene to Miocene, while Shcherbakov (2006) placed the latest radiation of higher fulgoroid families, after the Cretaceous-Palaeogene crisis. However, these fossils attest only for the minimum age of the respective lineage. Moreover, insects inhabiting mountain and desert regions have minimal chances to be preserved as fossils (Zherikhin, 1980). Besides, Wang M.L. and Bourgoin (2017, pers. comm., under preparation) place the origin of Issidae at least before 70 Mya.


The forests, in which resin transformed into Baltic amber, have been spreading on the vast area for about 10 million years (Wolfe et al., 2009, 2016; Szwedo, 2012). The differentiation of the forests was influenced by number of factors: geographic and topographic position, soils and water, temperature, insolation, seasonality, climate changes, etc. (Archibald and Farrell, 2003; Archibald et al. 2013; Szwedo, 2012; Szwedo and Kania, 2015; Wolfe et al., 2016). Palaeoclimatic and palaeoecological interpretations result in many questions regarding the variability of Baltic amber forest(s) habitats and environments (e.g., Alexeev and Alexeev, 2016; Perkovsky, 2016; Sadowski et al., 2016a, 2016b; Schmidt et al., 2016; Alexeev, 2017). However, it is probable that dry and open habitats, as e.g., sparse and open forests or low vegetation areas with a few resiniferous trees or at least on borderland with amber producing trees, were present in the area and at time of the Baltic amber deposit alimentation (Kohlmann-Adamska 2001; Szwedo, 2012; Szwedo and Drohojowska, 2015).

The observed high diversity of Tropiduchidae lineages, also reflected in the Baltic amber inclusions with separated fossil lineages, is interesting to note. If it confirms an early radiation of the family, it probably also reflects taphonomic factors linked to a diverse origin of the Baltic amber inclusions. Indeed, thanatocoenosis of Baltic amber is a a result of long, complicated and still little understood processes (Zherikhin, 2002; Martínez-Delclòs et al., 2004; Szwedo and Sontag, 2009) and yield fossil assemblage belonging to various ecosystems and different time-slices. Better understanding of these taphonomic factors remains essential for determining the exact palaeoenvironments of these fossils, their interactions and role in these ancient ecosystems, and particularly with plants which are at the origin of amber inclusions. Nevertheless, further studies on Tropiduchidae from Baltic amber as well as fossils from other contemporaneous deposits, are needed. Phylogenetic analysis based on morphological, palaeoentomological and molecular studies is urgently needed to solve the questions of features, definition and content of Tropiduchidae and its subordinate taxa.


We wish to thank cordially J. Damzen (MB Amber Inclusions, Vilnus, Lithuania) for bringing the specimen to our attention and E. Sontag (Museum of Amber Inclusions, University of Gdańsk, Gdańsk, Poland) for her help during the study of the material. Also we thank A. Klikowicz, M.Sc. Eng. (Amber Laboratory of International Amber Association, Gdańsk, Poland) for the help with FT-IR analysis. We express our sincere thanks to reviewers for their comments and suggestions. We are deeply indebted to T. Bourgoin (MNHN, Paris, France) and D. Świerczewski (Jan Długosz Academy, Częstochowa, Poland) for valuable discussions and comments on earlier drafts of this paper. We wish to thank also M. Hyžný, Handling Editor of PE, for all the comments and suggestions improving this paper.


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