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Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 1–60, 2019

True flies (Insecta: Diptera) from the late (Bembridge Marls) of the , , UK Wiesław KRZEMIN´ SKI1*, Vladimir BLAGODEROV2, Dany AZAR3, Elena LUKASHEVICH4, Ryszard SZADZIEWSKI5, Sonja WEDMANN6, Andre´ NEL7, Franc¸ois-Marie COLLOMB7, Alain WALLER7 and David B. NICHOLSON8 1 Institute of Systematics and Evolution of , Polish Academy of Sciences, Ul. Sławkowska 17, 31-016 Krako´w, Poland. Email: [email protected] 2 Department of Natural Sciences, National Museums Scotland, Chambers St., Edinburgh EH1 1JF, UK. 3 Department of Biology, Faculty of Sciences II, Lebanese University, Fanar – Matn, P. O. box 26110217, Lebanon. 4 Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya Str. 123, 117868 Moscow, Russia. 5 Department of Invertebrate Zoology, University of Gdan´sk, Pilsudskiego 46, 81-378 Gdynia, Poland. 6 Senckenberg Research Institute and Museum, Research station Grube Messel, Markstraße 35, D-64409 Messel, Germany. 7 CNRS UMR 5202, Muse´um National d’Histoire Naturelle, CP 50, Entomologie, 45 rue Buffon, F-75005, Paris, France. 8 School of Earth and Environmental Sciences, University of Portsmouth, Burnaby Road, Portsmouth PO1 3QL, UK. *Corresponding author.

ABSTRACT: The Diptera fauna from the late Eocene of the Isle of Wight (Bembridge Marls) is studied including redescriptions of formerly described material. The fauna includes the following taxa: – one ; – 11 species; – one described and two unidentified species; – undetermined species of three ; Culicidae – four species; – one species; – one species; – one described and four unidentified species; Limoniidae – 31 species; – 14 species; – two species; – two species; – three species; Simuliidae – an unnamed species; Tipulidae – nine species. Diptera : – unidentified species; – two species; – two species; – one species; – one species; – unidentified species; – unidentified species; – two species; – unidentified species; – unidentified species; Otitidae – one species; – unidentified species; – two species; – two species; Syrphidae – unidentified species; Tabanidae – one species. Following new taxa are described: Leptotarsus (Longurio) fragmentatus Krzemin´ski, n. sp., Leptotarsus (Longurio) wegiereki Krzemin´ski, n. sp., Tipula (s. lato) anglicana Krzemin´ski, n. sp. (Tipulidae); Cyttaromyia rossi Krzemin´ski, n. sp. (Cylindrotomidae); Gurnardia corami Krzemin´ski, n. gen, n. sp., hooleyi Krzemin´ski, n. sp., Pilaria volodii Krzemin´ski, n. sp., (Cheilotrichia) duplicata Krzemin´ski, n. sp., Cheilotrichia (Empeda) szwedoi Krzemin´ski, n. sp., (Psiloconopa) gurnetensis Krzemin´ski, n. sp., (Orimarga) lenae Krzemin´ski, n. sp., (Dicranomyia) azari Krzemin´ski, n. sp., Dicranomyia (Dicranomyia) fasciata Krzemin´ski, n. sp., (Helius) edmundi Krzemin´ski, n. sp., Helius (Helius) popovi Krzemin´ski, n. sp., staryi Krzemin´ski, n. sp. (Limoniidae); Wightipsychoda Azar, n. gen. (Psychodidae); Dilophus andrewrossi Nel, Colomb & Waller, n. sp., Bibiodes massiliensis Nel, Colomb & Waller, n. sp. (Bibionidae); Azana cockerelli Blagoderov, n. sp., Aglaomyia vectis Blagoderov, n. sp., oligocenica Blagoderov, n. sp., Palaeoempalia saxea Blagoderov, n. sp., hoolei Blagoderov, n. sp., gurnardensis Blagoderov, n. sp. (Mycetophilidae); Regmoclemina haennii Krzemin´ski, n. sp. (Scatopsidae); Sylvicola problematica Krzemin´ski, n. sp. (Anisopodidae); Palaeoberidops barkeri Nicholson, n. gen., n. sp. (Stratiomyidae). The Diptera fauna and palaeohabitat of the Insect Bed is discussed.

KEY WORDS: , new taxa.

The Diptera from the late Eocene of the Isle of Wight are regions. They are a very common and diversified group in the similar to the Recent fauna in generic composition, particu- Insect Bed. Most important information about fossil Diptera larly in containing genera occurring today in subtropical from Isle of Wight were published by Cockerell (1915,

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Table 1 Current taxonomic position of the previously described species fossil Diptera form the Insect Limestone.

Name and taxonomic placement as described Valid name and current taxonomic placement simplex Cockerell, 1921; Mycetophilidae Mycetophilidae: : Acnemia simplex Cockerell, 1921 disjunctula Cockerell & Haines, 1921, p. 83; Limoniidae: Limnophilidae: (Pseudolimnophila) disjunctula Limoniidae (Cockerell & Haines, 1921) gurnetensis Cockerell, 1921; Asilidae Not revised vectensis Cockerell, 1915; Limoniidae Limoniidae: : Helius (Helius) vectensis (Cockerell, 1915) Bibio extremus Cockerell, 1921; Bibionidae Bibionidae: ?Bibio extremus Cockerell, 1921 Bibio gurnetensis Cockerell, 1917a; Bibionidae Bibionidae: ?Bibio gurnetensis Cockerell, 1917a Bibio oblitus Cockerell, 1921; Bibionidae Bibionidae: ?Bibio gurnetensis Cockerell, 1917a Bibio oligocenus Cockerell, 1917a; Bibionidae Bibionidae: ?Bibio oligocenus Cockerell, 1917a Bibiodites confluens Cockerell, 1915; Bibionidae Bibionidae: Bibiodes confluens (Cockerell, 1915) anglicus Cockerell, 1921; Rhagionidae Not revised Chrysopilus stigmaticus Cockerell, 1921; Rhagionidae Not revised Chrysops vectensis Cockerell, 1921; Tabanidae Not revised Culex petrifactellus Cockerell, 1915; Culicidae Culicidae: Ochlerotatus protolepis (Cockerell, 1915) Culex protolepis Cockerell, 1915; Culicidae Culicidae: Ochlerotatus protolepis (Cockerell, 1915) Culex protorhinus Cockerell, 1915; Culicidae Culicidae: Culex protorhinus Cockerell, 1915 Culex vectensis Edwards, 1923; Culicidae Culicidae: Culex vectensis Edwards, 1923 Dicranomyia excavata Cockerell & Haines, 1921; Limoniidae Limoniidae: Limoniinae: Dicranomyia (Dicranomyia) excavata Cockerell & Haines, 1921 Dicranomyia exhumata Cockerell, 1922; Limoniidae Limoniidae: Limoniinae: Dicranomyia (Dicranomyia) excavata Cockerell & Haines, 1921 Dicranomyia undulata Cockerell & Haines, 1921; Limoniidae Limoniidae: Limoniinae: undulata (Cockerell & Haines, 1921) priscula Cockerell, 1921; Dixidae Dixidae: priscula (Cockerell, 1921) Empeda ferruginea Cockerell, 1921; Limoniidae Limoniidae: : Cheilotrichia (Empeda) ferruginea (Cockerell, 1921) Empeda hyalina Cockerell, 1921; Limoniidae Limoniidae: Chioneinae: Cheilotrichia (Empeda) hyalina (Cockerell, 1921) oligocena Cockerell, 1915; Ephydridae Anthomyzidae indet. Ephydra sepulta Cockerell, 1915; Ephydridae Anthomyzidae indet. spilopterum Cockerell, 1921; Limoniidae Limoniidae: Dactyolabinae: (Dactylolabis) spiloptera (Cockerell, 1921) ferrea Cockerell, 1921; Limoniidae Limoniidae: Chioneinae: Gonomyia (Gonomyia) indecisa Cockerell & Haines, 1921 Gonomyia grisea Cockerell, 1921; Limoniidae Limoniidae: Chioneinae: Cheilotrichia (Empeda) hyalina (Cockerell, 1921) Gonomyia indecisa Cockerell & Haines, 1921; Limoniidae Limoniidae: Chioneinae: Gonomyia (Gonomyia) indecisa Cockerell & Haines, 1921 Gonomyia lutescens Cockerell, 1921; Limoniidae Limoniidae: Chioneinae: Gonomyia (Gonomyia) indecisa Cockerell & Haines, 1921 fasciatipennis Cockerell, 1921; Limoniidae Limoniidae: Chioneinae: Gymnastes (Paragymnastes) fasciatipennis Cockerell, 1921 brodiei Cockerell, 1915; Chloropidae Chloropidae: Hippelates brodiei Cockerell, 1915 Holorusia vasifera Cockerell & Haines, 1921, Tipulidae Tipulidae: Ischnotoma (Ischnotoma) vasifera (Cockerell & Haines, 1921) Limnobia spilota Cockerell, 1921; Limoniidae Limoniidae: Limoniinae: spilota (Cockerell, 1921) aliena Cockerell, 1921; Limoniidae Limoniidae: Limoniinae: Dicranomyia (Dicranomyia) aliena (Cockerell, 1921) Limnophila cyclospila Cockerell & Haines, 1921; Limoniidae Limoniidae: : Limnophila (Limnophila) cyclospila Cockerell & Haines, 1921 Limnophila deleta Cockerell, 1921; Limoniidae Limoniidae: Limnophilinae: Limnophila (Limnophila) deleta Cockerell, 1921 Limnophila incognita Cockerell, 1921; Limoniidae Limoniidae: Chioneinae: (Lunaria) incognita (Cockerell, 1921) Macromastix cladoptera Cockerell & Haines, 1921; Tipulidae Tipulidae: Leptotarsus (Macromastix) cladoptera (Cockerell & Haines, 1921) Megistocera gurnetensis Cockerell, 1921; Tipulidae Tipulidae: Brachypremna gurnetensis (Cockerell, 1921) Mesomyites concinna Cockerell, 1917a; Limoniidae Limoniidae: Chioneinae: concinna (Cockerell, 1917a) Mongoma cruciferella Cockerell, 1917a; Limoniidae Limoniidae: Limoniinae: (Mongoma) cruciferella (Cockerell, 1917a) Mongoma pallescens Cockerell, 1921; Limoniidae Limoniidae: Limoniinae: Trentepohlia (Mongoma) pallescens (Cockerell, 1921) vectensis Cockerell, 1915; Mycetophilidae Mycetophilidae: indet. Mycomya oblita Cockerell, 1921; Mycetophilidae Mycetophilidae: Mycomya oblita Cockerell, 1921 edwardsi Cockerell, 1921; Ceratopogonidae Ceratopogonidae: Palpomyia edwardsi Cockerell, 1921 Paltostomopsis ciliata Cockerell, 1915; indet. Phronia virgata Cockerell, 1921; Mycetophilidae Mycetophilidae: : ? virgata (Cockerell, 1921)

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Table 1 (Continued)

Name and taxonomic placement as described Valid name and current taxonomic placement Platyura obliqua Cockerell, 1921; Mycetophilidae Keroplatidae: Macrocerinae: obliqua (Cockerell, 1921) Plecia acourti Cockerell, 1921; Bibionidae Bibionidae: Plecia acourti Cockerell, 1921 fractus Cockerell, 1921; Asilidae Not revised Protoberis obliterata Cockerell, 1915; Stratiomyidae Bibionidae: Bibio obliteratus (Cockerell, 1915) Protoscinis perparvus Cockerell, 1917a; Chloropidae Ephydridae: : Scatellini: Protoscinis perparvus Cockerell, 1917a Psychoda leucospila Cockerell, 1921; Psychodidae Psychodidae: Wightipsychoda leucospila (Cockerell, 1921) Psychoda primaeva Cockerell, 1915; Psychodidae Psychodidae: Pericoma primaeva (Cockerell, 1915) brodiei Cockerell, 1917a; Limoniidae Limoniidae: Limoniinae: Dicranomyia (Dicranomyia) brodiei (Cockerell, 1917a) Rhyphys hooleyi Cockerell, 1921; Anisopodidae. Anisopodidae: Sylvicola hooleyi (Cockerell, 1921) ‘Rymosia’ edwardsi Cockerell, 1921; Mycetophilidae Mycetophilidae: Mycetophilinae: Mycetophilini indet. ‘Rymosia’ ferruginea Cockerell, 1921; Mycetophilidae Mycetophilidae: Mycetophilinae Mycetophilini indet. Rymosia grisea Cockerell, 1921; Mycetophilidae Mycetophilidae: Mycetophilinae indet. ‘Rymosia’ rufescens Cockerell, 1921; Mycetophilidae Mycetophilidae: Mycetophilinae: Mycetophilini indet. gurnetensis Cockerell, 1915; Sciaridae Not revised Sciara lacoei Cockerell, 1915; Sciaridae Not revised Sciara protoberidis Cockerell, 1915; Sciaridae Not revised Sphaerocera sepultula Cockerell, 1915; Borboridae Ephydridae indet. Stenomyites fuscipennis Cockerell, 1915; Otitidae Otitidae Stenomyites fuscipennis Cockerell, 1915 brodiei Cockerell, 1915; Stratiomyidae Stratiomyidae: brodiei (Cockerell, 1915) Styringomyia extensa Cockerell & Haines, 1921; Limoniidae Limoniidae: Chioneinae: Styringomyia concinna (Cockerell, 1917a) acourti Cockerell, 1921; Bombyliidae Not revised Taeniorhynchus cockerelli Edwards, 1923; Culicidae Culicidae: Coquillettidia cockerelli (Edwards, 1923) Tipula acourti Cockerell, 1921; Tipulidae Tipula (s. lato) acourti Cockerell, 1921 Tipula callarche Cockerell, 1921; Tipulidae Leptotarsus (Macromastix) cladoptera (Cockerell & Haines, 1921) Tipula gardneri Cockerell, 1917a; Tipulidae Tipula (s. lato) gardneri Cockerell, 1917a Tipula hooleyi Cockerell & Haines, 1921; Tipulidae Tipula (s. lato) limiformis Cockerell, 1915 Tipula limiformis Cockerell, 1915; Tipulidae Tipula (s. lato) limiformis Cockerell, 1915

1917a, b, 1921); Cockerell & Haines (1921); Edwards (1923); Insect Bed, which lies towards the base of the Bembridge Jarzembowski (1976); Krzemin´ski (1996); Vane-Wright (1967). Marls Member (: ) (Gale In 2005–2007 thanks to financial support of et al. 2006; Ross & Self 2014). INTAS (Project no. 03-51-4367) an international group of The largest collection is housed in Natural History Museum dipterologists, including Wiesław Krzemin´ski (Poland) – (NHM), London. Most of the specimens at this museum team leader, Dany Azar (Lebanon), Vladimir Blagoderow belong to the A’Court Smith (purchased 1877, 1883), P.B. (Russia), Elena Lukashevich (Russia), Andre Nel (France), Brodie (purchased 1898) and R.W. Hooley (purchased 1924) Ryszard Szadziewski (Poland), Sonja Wedmann (Germany), collections. They are labelled ‘Gurnard Bay’ (which is an old Vladimir Zlobin (Russia), had undertaken the task of deter- name for Gurnet Bay); however, Smith collected specimens mination and revision of dipteran materials from the Isle of all the way from West Cowes to Newtown River on the NW Wight. Later Francis-Marie Collomb (France), David B. side of the Isle of Wight (Jarzembowski 1980). Most of the Nicholson (UK) and Alain Waller (France) also joined the specimens probably came from Thorness Bay (Jarzembowski project. 1976). Brodie and Hooley acquired parts of Smith’s collection, Our study on old and new collections housed in UK and so that parts and counterparts of individual insects have USA museums and materials collected during field trips re- turned up in the three collections. The parts and counterparts vealed over 1,700 fossil specimens, belonging to 32 families of often have different numbers because they were registered at the Diptera; however, only around 800 specimens were studied different times. An additional collection was discovered at the for this paper. Taxonomic results of study on higher flies Sedgwick Museum, Cambridge by A.J. Ross. This collection from the Insect Bed are published elsewhere (Zlobin 2007). A has also yielded counterparts of specimens at the NHM, which summary of current taxonomic position of previously described indicates that this is another part of the Smith collection. A species is presented in Table 1. label with ‘1883’ on it suggests that the Sedgwick Museum acquired this collection in 1883, the same that the NHM purchased specimens from Smith. Prefixes I. and In. preceding the numerals of specimens indi- 1. Material and methods cate that they come from different series. The fossil insects of the Isle of Wight originate from the late Eocene concretions or tabular bands of very fine-grained 1.1. Number of specimens studied micrite, identified as Insect Limestone of the Isle of Wight. Diptera : Anisopodidae – five specimens; Bibioni- The unit where these concretions/bands occur is known as the dae – 19 specimens; Ceratopogonidae – nine specimens;

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 4 WIESŁAW KRZEMIN´ SKI ET AL. Chironomidae – 170 specimens; Culicidae – 140 specimens; Haines (1921). Revision of some of these materials was made Cylindrotomidae – one specimen; Dixidae – six specimens; by Vane-Wright (1967) and Krzemin´ski (1996); the latter Keroplatidae – 17 specimens; Limoniidae – 135 specimens; demonstrated that Megistocera gurnetensis Cockerell, 1921 Mycetophilidae – 55 specimens; Psychodidae – 39 specimens; belonged to the Brachypremna Osten Sacken, while Scatopsidae – two specimens; Simuliidae – one specimen; Holorusia vasifera Cockerell & Haines 1921 belongs to the Tipulidae – 32 specimens. Diptera Brachycera: Agromyzidae – genus Ischnotoma Skuse. two specimens; Anthomyzidae – 18 specimens; Chloropidae – In the present paper further misinterpretations are dealt three specimens; Dolichopodidae – 23 specimens; Empididae – with: Tipula callarche Cockerell, 1921 and Macromastix two specimens; Ephydridae – four specimens; Heleomyzidae – 11 cladoptera Cockerell & Haines, 1921 were described on the ba- specimens; Lauxaniidae – 12 specimens; Otitidae – six specimens; sis of part and counterpart of the same specimen. Also, no Phoridae – two specimens; Stratiomyidae – 41 specimens; difference can be found between Tipula limiformis Cockerell, Syrphidae – four specimens. Cyclorrhaphous diptera were 1915 and Tipula hooleyi Cockerell & Haines, 1921. Therefore described in a separate publication (Zlobin 2007). Also, Cockerell T. hooleyi is a younger synonym of T. limiformis.Incon- (1915, 1921) described species of Asilidae, Blephariceridae (see clusion, there are now six valid species described from the below), Bombyliidae, Rhagionidae, Sciaridae and Tabanidae. Bembridge Marls. Additionally, among undetermined mate- Fine-grained limestone often enables exceptional preserva- rial three additional species belonging to the genus Leptotarsus tion of delicate structures, although many isolated wings and Guerin-Meneville and one to the genus Tipula Linnaeus were fragments of the body are preserved in the material. When found. They are described below. taxonomically important structures like antennae, palps, legs, Today Tipulidae form a large of Diptera Nematocera, genitalia are missing or destroyed, not all families of the with about 4000 species of worldwide distribution. Larvae live Diptera can be studied and determined on the same level. in freshwater, semi-aquatic and terrestrial habitats. It has not been possible to re-describe all of Cockerell’s The oldest Tipulidae were described from the Lower Creta- types, which when originally described were only figured with ceous (Krzemin´ski 1992). They are common in fossil materials a line drawing. However, all of his holotypes and other specimens from the Palaeogene and Neogene of Europa, Asia and North that provide new family level records have been listed and America. imaged for completeness. Classification of Diptera follows Pape et al. (2011). For Genus: Brachypremna Osten Sacken, 1887 an explanation of general morphological terminology of Culicidae and abbreviations see Dahl (1997) and Szadziewski Type species. Tipula dispellens Walker, 1861, p. 334, (1998). For an explanation of general morphological terminology (designated by Coquillett 1910) of Ceratopogonidae and abbreviations see Szadziewski (1988, Remarks. Recently the genus Brachypremna is represented 1996). Nomenclature of radial and medial veins of Scatopsidae by 37 species distributed only in tropical and subtropical re- follows Cook (1981). gions of the world; most (34 sp.) known from the Neotropical Fossil Diptera from the Isle of Wight are deposited in: Region, one from Nearctic and two from the Australian Re- gion. Only three fossil species are known: from Eocene Baltic BMB – Booth Museum of Natural History, Brighton (Eocene), from the Dominican amber () and CAMSM – Sedgwick Museum of Earth Sciences, University from the early Isle of Wight (Cockerell 1921; of Cambridge Alexander 1931; Krzemin´ski 1996). IWCMS – Isle of Wight County Museum Service Brachypremna gurnetensis (Cockerell, 1921) NHMUK – Natural History Museum, London, Department (Fig. 1, Pl. 1a) of Palaeontology 1921 Megistocera gurnetensis Cockerell, p. 456, fig. 3 MNEMG – Maidstone Museum & Bentlif Art Gallery 1931 Brachypremna gurnetensis Alexander, p. 8 USNM – Department of Paleobiology, National Museum 1994 Brachypremna gurnetensis Evenhuis, p. 57 of Natural History, Smithsonian Institution, Washington 1996 Brachypremna gurnetensis Krzemin´ski, pp. 275–76, DC fig. 3

Holotype. NHMUK In.17090/In.17492 (part and counter- part), Smith Collection; Insect Bed; late Eocene; NW Isle of 2. Systematic palaeontology Wight, UK. Diptera Linnaeus, 1758 Remarks. Revision and redescription of this species was given by Krzemin´ski (1996). Suborder Nematocera Dumeril, 1805 Genus: Leptotarsus Guerin-Meneville, 1831 Superfamily Latreille, 1802 by Wieslaw Krzemin´ski Type species. Leptotarsus macquartii Guerin-Meneville, 1831: Atlas: pl. 20, fig. 1 (by monotypy) Family Tipulidae Latreille, 1802 Subgenus: Macromastix Osten Sacken, 1887 TIPULIDAE (Diptera Nematocera) are rather common and well preserved in Bembridge Marls of the Isle of Wight when Type species. Macrothorax ornatus Jaennicke, 1867, p. 320 compared to other contemporary faunas. These large Diptera Remarks. The subgenus Macromastix is represented in fossil are represented mostly by isolated wings or some wing frag- state by two fossil species, from the Oligocene of France and ments. Bodies are rare and mostly poorly preserved. In the from late Eocene Isle of Wight, England. Recently the sub- collections from the Bembridge Marls eight species were genus comprises 94 species living in tropical and subtropical described by Cockerell (1915, 1917a, 1921) and Cockerell & regions.

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Subgenus Longurio Loew, 1869

Type species. Longurio testaceus Loew, 1869 (by monotypy) Remarks. Recently subgenus Longurio comprises 112 species living in tropical and subtropical regions and two fossil species from the Lower from Russia and (Shih et al. 2015).

Leptotarsus (Longurio) fragmentatus Krzemin´ski, n. sp. (Fig. 3, Pl. 1c)

Holotype. NHMUK In.25379, Hooley Collection; Insect Bed; late Eocene; NW Isle of Wight, UK. Diagnosis. Sc ending in Costa, opposite proximal third portion of R2 þ 3 þ 4; R3 strongly curved to costal wing margin; cross-vein m-cu about 1.25 times longer than d cell. Description. Only a portion of the wing is preserved, but characteristic venation of radial sector allows to separate it from other Tipulidae from the Isle of Wight. Wing clear, 18– 19 mm long. Venation: Sc long, ending in the costal vein, opposite 1/3 of R2 þ 3 þ 4; cross-vein sc-r at its three lengths before tip of Sc; R3 short, and strongly curved to costal wing Figures 1–4 Tipulidae, wing venation. (1) Brachypremna gurnetensis margin; Rs 1.5 times longer than R2 þ 3 þ 4; d cell long and (Cockerell, 1921), holotype NHMUK In.17090. (2) Leptotarsus narrow; petiole (distal section of M1 þ 2) very short; upper Macromastix cladoptera ( ) (Cockerell & Haines, 1921), holotype margin of d cell four times longer than petiole; M1 about five NHMUK I.10379. (3) Leptotarsus (Longurio) fragmentatus Krzemin´ski, n. sp., holotype NHMUK In.25379. (4) Leptotarsus (Longurio) times longer than petiole; cross-vein m-cu very long and about wegiereki Krzemin´ski, n. sp., holotype NHMUK In.17493. 1.25 times longer than d cell.

Leptotarsus (Longurio) wegiereki Krzemin´ski, n. sp. (Fig. 4, Pl. 7a) Leptotarsus (Macromastix) cladoptera (Cockerell & Haines, 1921) Etymology. A new species is dedicated to Piotr We˛gierek (Fig. 2, Pl. 1b) (Silesian University, Katowice, Poland) a paleoentomologist, specialist of Homoptera. 1921 Macromastix cladoptera Cockerell & Haines, p. 111– Holotype. NHMUK In.17493, Smith Collection; Insect 112, fig. I10397 (published May 1921) Bed; late Eocene; NW Isle of Wight, UK. 1921 Tipula callarche Cockerell p. 455, fig. 1 (published June Other material. CAMSM X.50140 (TN 76), CAMSM 1921), syn. nov. X.50140.89a (TN 141), Smith Collection; NHMUK In.25207, 1994 Leptotarsus (Macromastix) cladoptera Evenhuis, p. 56 Hooley Collection. 1994 Tipula callarche Evenhuis, p. 58 Diagnosis. Sc ending in Costa, opposite Rs fork; d cell very small; cross-vein m-cu long, about three times longer than Holotype. NHMUK I.10397(part), Brodie Collection, de- width of d cell. scribed as Macromastix cladoptera Cockerell & Haines, 1921 Description. Wing length 18–19 mm, without pattern, but and NHMUK In.17381(counterpart), Smith Collection (de- anal part is destroyed in all specimens. Venation: Sc ending scribed as Tipula callarche Cockerell, 1921); Insect Bed; late in Costal vein, opposite to fork of Rs; cross-vein sc-r at its Eocene; NW Isle of Wight, UK. three lengths before tip of Sc; R2 þ 3 þ 4 1.5 times shorter Diagnosis. Wing wide, narrowing to petiolate basally, anal than Rs; R4 twice longer than R2 þ 3 þ 4; d cell very small; lobe very narrow; A2 very close and parallel to anal wing petiole of M1 þ 2 twice longer than preceding section between margin; colour pattern on wing membrane. cross-veins r-m and m-m; M1 about twice longer than M1 þ 2; Redescription. Two wings (one incomplete) and small cross-vein m-cu 2.5 times longer than width of d cell. portion of thorax are preserved. Wing about 9.5 mm long, Remarks. Venation pattern in this new species is unique by with a well visible colour pattern. Venation: tip of Sc lost, Sc being complete (tip not atrophied) and ending in the Costa, and this vein together with sc-r terminates in Rl, opposite small d cell, and long cross-vein m-cu. All these characters are mid of Rs; R3 0.5 times length of R3 þ 4; Rs little shorter only exceptionally met in the Tipulidae, such as some Recent than R3 þ 4; petiole (most distal section) of Ml þ 2 as long as species of the genus Leptotarsus. M2 and equal preceding section between cross-veins r-m and m-m; cross-vein m-cu in fork of M3 þ 4; A2 close and parallel Genus: Tipula Linnaeus, 1758 to anal wing margin; part of wing is narrow and almost without anal lobe. Type species. Linnaeus, 1758, p. 585 Remarks. Macromastix cladoptera was described by Cockerell (designated by Latreille 1810) & Haines in May 1921 from one part of the specimen. One Remarks. The genus Tipula (Diptera Nematocera) is very month later, in the same year, Cockerell described another diverse; currently about 1,200 Recent species in 34 subgenera

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Plate 1 Tipulidae and Cylindrotomidae. (a) Brachypremna gurnetensis (Cockerell, 1921) holotype part NHMUK In.17090. (b) Leptotarsus (Macromastix) cladoptera (Cockerell & Haines, 1921), holotype part NHMUK I.10397. (c) Leptotarsus (Longurio) fragmentatus Krzemin´ski, n. sp., holotype NHMUK In.25379. (d) Tipula (s. lato) acourti Cockerell, 1921, holotype part NHMUK I.8901. (e) Tipula (s. lato) anglicana Krzemin´ski, n. sp., holotype NHMUK In.64117. (f ) Tipula (s. lato) gardneri Cockerell, 1917a holotype NHMUK I.8663. (g, h) Tipula (s. lato) limiformis Cockerell, 1915: (g) (type of Tipula hooleyi Cockerell & Haines, 1921 syn. nov.), NHMUK In.24353; (h) holotype USNM 61438. (i) Ischnotoma (Ischnotoma) vasifera (Cockerell & Haines, 1921), holotype NHMUK In.24352. (j) Cyttaromyia rossi Krzemin´ski, n. sp., holotype CAMSM X.50140.14.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 7 are known, distributed worldwide. Most of the species within Diagnosis. Wing membrane little darkened but without the subgenera are uniform in body structure and wing venation pattern; tip of Sc lost, Sc terminally fused with sc-r and ending pattern. Some species and groups of species however are charac- in Rl, much before fork of Rs; distal M1 þ 2veryshort;pre- teristic by having infuscated wings and by the proportions and ceding section between cross-veins r-m and mm about twice shape of the veins and cells, which allows us to determine fossil longer than distal M1 þ 2; mcu cell distinctly more narrow in species by wings only. One new species from the Isle of Wight distal part. is described below and three are redescribed. Redescription. The species is represented by two separate wings of two specimens; wings are in good condition, only Tipula (s. lato) acourti Cockerell, 1921 short basal part is missing. Wing length 20–22 mm without (Fig. 5, Pl. 1d) dark pattern on wing membrane. Venation: tip of Sc lost, Sc terminally fused with sc-r and ending in Rl, well before fork 1921 Tipula acourti Cockerell, pp. 455–456, fig. 2 of Rs; R2 þ 3 þ 4 twice shorter than Rs; d cell rather long 1994 Tipula acourti Evenhuis, p. 57 and narrow; distal M1 þ 2 very short, less than half as long as mid M1 þ 2; Ml four times longer than distal M1 þ 2; Holotype. NHMUK I.8901/In.25471 (part and counterpart), cross-vein m-cu in fork of M3 þ 4; mcu cell in distal part Brodie/Hooley Collections; Insect Bed; late Eocene; NW Isle of narrowed. Wight, UK. Other material. NHMUK I.8667, Brodie Collection; Tipula (s. lato) limiformis Cockerell, 1915 In.64102, In.64103, In.64109, In.64116, In.64118, In.25338, (Figs 8, 9, Pl. 1g, h) In.25471/In.64126 (part and counterpart), Hooley Collection. 1915 Tipula limiformis Cockerell, p. 492, 499, pl. 61, fig. 11 Diagnosis. Wing venation very strong and additionally 1921 Tipula hooleyi Cockerell & Haines, p. 82, fig. H49, underlined by dark clouds accompanying veins. Sc ending in syn. nov. Rl opposite and near Rs fork; d cell large and broad; cu cell 1994 Tipula limiformis Evenhuis, p. 58 of same width in basal and distal part. 1994 Tipula hooleyi Evenhuis, p. 59 Redescription. Wing about 18–20 mm, with strong veins and with dark clouds close to veins. Venation: tip of Sc lost, Sc Holotype. USNM 61438 (Lacoe Collection No. 7523, Fig. 9, terminally fused with sc-r and ending in Rl; Rs twice longer Pl. 1h); Insect Bed; late Eocene; NW Isle of Wight, UK. than R3 þ 4 and as long as R4; d cell rather large and broad; Other material. In.24353 (Hooley Collection No. 49, Fig. 8, petiole short, twice shorter than upper margin of d cell Pl. 1g) was described as Tipula hooleyi by Cockerell & Haines between cross-veins r-m and mm; Ml about three times longer (1921), and In.25208. than petiole; medial cells very broad; cross-vein m-cu in fork Diagnosis. Tip of Sc lost, Sc terminally fused with sc-r and of M3 þ 4; cell m-cu equally wide in basal and distal part. ending in Rl, well before fork of Rs; distal M1 þ 2 very short, half as long as mid M1 þ 2; mcu cell at anal margin narrowed (about 1/3). Tipula (s. lato) anglicana Krzemin´ski, n. sp. Redescription. Wing 21–22 mm long, without dark pattern. (Fig. 6, Pl. 1e) Venation: tip of Sc lost, Sc terminally fused with sc-r and ending in Rl, well before fork of Rs; R2 þ 3 þ 4halfaslong Holotype. NHMUK In.64117, Hooley Collection; Insect as Rs; R4 rather long, little wavy and twice longer than Bed; late Eocene; NW Isle of Wight, UK. R2 þ 3 þ 4; d cell rather short and broad; distal M1 þ 2very Other material. NHMUK In.25206/In.64100 (part and short, only half of mid M1 þ 2; cross-vein m-cu in fork of counterpart), Hooley Collection. M3 þ 4; mcu cell about 1/3 narrower at anal margin than Diagnosis. Cell d very narrow; cu cell rectangular. vein m-cu; anal part of wing in all specimens is missing. Description. Wing length 19 mm, membrane little darkened Remarks. Tipula hooleyi described by Cockerell & Haines but without colour pattern. All veins are very good visible. (1921) does not differ by a single character from the preserved Venation: tip of Sc lost, Sc terminally fused with sc-r and wing fragment of Tipula limiformis, described some years ending in Rl, much before fork of Rs; R2 þ 3 þ 4aslongas earlier by Cockerell (1915); therefore this species is made a R3; Rs about 1.5 times longer than distal M1 þ 2; upper younger synonym of T. limiformis. margin of d cell between cross-veins r-m and m-m about three times longer than petiole; d cell very narrow and rather small; Genus Ischnotoma Skuse, 1890 cross-vein m-cu in fork of M3 þ 4; mcu cell rectangular, Type species. Tipula serricornis Macquart, 1846 (designated equally wide over entire length. by Alexander 1920) Remarks. Venation T. (s. lato) anglicana n. sp differs from Remarks. Recently the genus comprises about 50 species of remaining species of Tipula from the Isle of Wight by the d Australian and Neotropical Regions. cell and mcu cell shape. It is noteworthy that most tipulid species from early Oligo- cene Isle of Wight belong to the genera and subgenera recently Tipula (s. lato) gardneri Cockerell, 1917a living in the tropical and subtropical regions. (Fig. 7, Pl. 1f ) Ischnotoma (Ischnotoma) vasifera (Cockerell & Haines, 1921) 1917a Tipula gardneri Cockerell, pp. 374, 384, pl. 31, fig. 1 (Fig. 10, Pl. 1i) 1994 Tipula gardneri Evenhuis, 1994, p. 58 1921 Holorusia vasifera Cockerell and Haines, pp. 82–83, Holotype. NHMUK I.8663, Brodie Collection; Insect Bed; fig. H9 late Eocene; NW Isle of Wight, UK. 1967 Ischnotoma (Ischnotoma) vasifera Vane-Wright, pp. 529, Other material. NHMUK In.17429 (part and counterpart), 539–540 Smith Collection; In.25205, Hooley Collection. 1994 Ischnotoma (Ischnotoma) vasifera Evenhuis, p. 56

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Figures 5–13 Tipulidae and Cylindrotomidae, wing venation. (5) Tipula (s. lato) acourti Cockerell, 1921, holotype NHMUK I.8901. (6) Tipula (s. lato) anglicana Krzemin´ski, n. sp. holotype NHMUK In.64117. (7) Tipula (s. lato) gardneri Cockerell, 1917a, holotype NHMUK I.8663. (8), (9) Tipula (s. lato) limiformis Cockerell, 1915: (8) – (type of Tipula hooleyi Cockerell & Haines, 1921 syn. nov.), NHMUK In.24353; (9) Holotype of Tipula limiformis USNM 61438. (10) Ischnotoma (Ischnotoma) vasifera (Cockerell & Haines, 1921), holotype NHMUK In.24352. (11)–(13) Cyttaromyia rossi Krzemin´ski, n. sp. – wing venation; holotype CAMSM X.50140.14 (TN 63): (11) left wing; (12) right wing; (13) reconstruction based on both wings.

Holotype. NHMUK In.24352/I.8852 (part and counterpart), known only from nine fossil species from the Palaeogene of Hooley/Brodie Collections; Insect Bed; late Eocene; NW Isle of (Scudder 1877, 1894; Cockerell 1924, 1925), Wight, UK. (Freiwald 1991), France (Seguy 1934) and Russia Other material. Besides holotype, specimens NHMUK (Freiwald & Krzemin´ski 1991) and one species from Baltic In.25210, In.25260/In.25493 (part and counterpart). amber (Krzemin´ski 1998). Diagnosis. Vein R4 strongly curved to upper wing margin; Recent Cylindrotomidae are a small family comprising 72 m-cu placed between fork of Mb and fork M3 þ 4. species inhabiting mainly Holartic and Oriental Regions. In Redescription. Wing large, about 23 mm long. Venation: Sc the Afrotropical Region the family is not represented. ending in C; sc-r at its two lengths before tip of Sc; R2 þ 3 þ 4 In the fossil state only 14 fossil species of the family have as long as R3; Rs 1.5 times longer than R2 þ 3 þ 4; R4 in been described so far (Cockerell 1920; Freiwald & Krzemin´ski distal part strongly curved to upper wing margin; d cell rather 1991; Evenhuis 1994; Krzemin´ski 1998). small; distal M1 þ 2 very short; mid section of M1 þ 2is2.5 times longer than distal; cross-vein m-cu placed between fork Genus Cyttaromyia Scudder, 1877 of Mb and fork M3 þ 4. Remarks. Holorusia vasifera described by Cockerell & Type species. Cyttaromyia fenestrata Scudder, 1877, by Haines (1921) was transferred by Vane-Wright (1967) to the monotypy genus and subgenus Ischnotoma Skuse, 1890 on the basis of similarity in wing venation. The species is particularly very similar to the Australian Ischnotoma (Ischnotoma) par (Walker Cyttaromyia rossi Krzemin´ski, n. sp. 1856). (Figs 11–13, Pl. 1j) Conclusion. Generally Tipulidae from the Isle of Wight are indicative of typical warm climate. Recent species from genera Derivation of name. The name of species is dedicated to Brachypremna, Macromastix, Leptotarsus and Ischnotoma live Andrew Ross, with many thanks for his efficient help during in tropical and subtropical regions. all stages of our project. Holotype. CAMSM X.50140.14 (TN 63) Smith Collection; Insect Bed; late Eocene; NW Isle of Wight, UK. Family: Cylindrotomidae Schiner, 1863 Diagnosis. R1 terminating in R3 þ 4 (a generic character); R1 fused with r-r (R2) and terminating in R3 þ 4 in 1/3 of its Cylindrotomidae were until now unknown in the fossil material length; M3 as long as d cell; cross-vein m-cu distinctly before from the late Eocene of the Isle of Wight. There is one specimen fork of Mb. belonging to the fossil genus Cyttaromyia Scudder. This genus Description. Only two wings of the holotype are preserved; has a characteristic wing venation and until now has been body absent. Wing length about 9 mm, with distinct pterostigma.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 9 Venation. Sc long, reaching beyond fork of Rs and terminat- three radial veins ending in C (R3 fused with R4); four medial ing in the Costa; cross-vein sc-r at its four lengths before end vein present; cross-vein m-cu close to 1/3 of d cell. of Sc; R1 terminating in R3 þ 4 (diagnostic character of the Type species. Gurnardia corami n. sp. from the Insect Bed, genus); R1 fused with cross-vein r-r (R2) and terminating in NW Isle of Wight, late Eocene. proximal 1/3 of R3 þ 4; addition cross-vein r0-m0 in mid of Derivation of name. The new genus is named after Gurnard R5; d cell large , almost rectangular; four medial veins present; Bay. M3 as long as d cell length; cross-vein m-cu distinctly before Description. Because only the type species is known, the fork of Mb; A2 rather long; anal lobe small. description of the genus is the same as that of the species. Remarks. The new species Cyttaromyia rossi is most similar to Cyttaromyia frelloi Krzemin´ski, 1998 from the Eocene Gurnardia corami Krzemin´ski, n. sp. Baltic amber. The differences concern the length of R1 and (Fig. 14, Pl. 2a) M3; the former being shorter in C. rossi, while M3 is longer (of the length of d cell). Holotype. NHMUK In.64104, Hooley Collection; Insect Conclusions. The presence of Cyttaromyia intheIsleof Bed; late Eocene; NW Isle of Wight, UK. Wight suggests a rather warm climate of this taphocoenosis. Additional material. NHMUK I.8982/I.9308 (female, part All representatives of this fossil genus were known from sub- and counterpart), I.9491, I.9966, Brodie Collection; I.9188/ tropical climate (ex. Baltic amber), but generally Cyttaromyia In.25422 (part and counterpart), Brodie/Hooley Collections; are very rare in fossil materials (Freiwald & Krzemin´ski 1991; In.25446, Hooley Collection. Krzemin´ski 1991, 1998). Derivation of name. A new species is dedicated to Robert Coram (UK), collector and specialist of fossil insects. Family Limoniidae Speiser, 1909 Diagnosis. The same as that of the genus. Description. Wing clear 5.0–5.8 mm long. LIMONIIDAE (Diptera Nematocera) are common and very Venation. Sc short, only little longer than half wing length, diverse among late Eocene insects from Bembridge Marls of ending somewhat before fork of Rs into R2 þ 3 þ 4 and R5; the Isle of Wight. Most species are represented by isolated cross-vein sc-r at its length before end of Sc; only three radial wings or some wing fragments, but the bodies are rather veins ending in C (R3 fused with R4); R1 long; cross-vein r-r rare and poorly preserved. Fortunately, the patterns of wing (R2) at its length before end of R1; Rs rather short, about 1/4 venation are usually very stable within the genera and with shorter than R2 þ 3 þ 4 and as long as length as R3 þ 4; four numerous minor differences between species. In the Recent medial vein present; M2 short, about half as long as d Limoniidae even small differences in the venation can accom- cell; petiole of m1 cell three times longer than M2; d cell pany gross and important differences in the structure of geni- narrow; cross-vein m-cu about 1/3 of d cell; A2 rather long talia, especially in the male. and wavy. Cockerell (1915, 1917a, b, 1921) and Cockerell & Haines Remarks. The new genus is different from all other genera (1921) described 23 fossil species, but some of them were of the Limoniidae by the presence of three long radial and incorrectly identified. The present revision includes all earlier four medial veins. This composition of characters is unique described species. Between undetermined old collection and among crane flies (Tipulomorpha). Unfortunately, in all collections newly made during the present excavations there specimens, legs are missing; hence, the presence of tibial spurs are representatives of one new genus and 12 species, described cannot be confirmed, which does not allow safe placement below. Together 30 species of Limoniidae are known from the of the new genus Gunardia in the Limnophilinae. Isle of Wight. Although this character is very important to make the decision Recently Limoniidae are one of the largest family of the about the systematic position between Limoniidae on the sub- Diptera, with about 12,000 described species of worldwide family level, the presence of four medial veins and position of distribution. Larvae usually live in running water, ponds and cross-vein m-cu suggest that this new genus should be ascribed ; some are semiaquatic or terrestrial. to the subfamily Limnophilinae. The oldest Limoniidae were described from the Middle and Upper of Asia and North America (Krzemin´ski 1992; Genus Limnophila Macquart, 1834 Krzemin´ski et al. 1994; Shcherbakov et al. 1995; Krzemin´ski & Evenhuis 2000; Krzemin´ski & Krzemin´ska 2003). They are Type species. Limnobia pictipennis Meigen, 1818, p. 119 common in most deposits with insects from the Lower (designated by Westwood 1840) until the Neogene of Europe, Asia and North America. The Subgenus Limnophila Macquart, 1834 oldest true limoniid is the Upper Triassic Architipula youngi Krzemin´ski (1992) (about 210 Ma) but from the Lower/ Type species. As for genus. Middle Triassic of Europe and from Middle Triassic of Asia Remarks. One hundred and forty-six recent species of the flies have been described that are very similar to Limoniidae, subgenus Limnophila are known from Australian (87 sp.), which are probable ancestors of the Limoniidae (Shcherbakov Neotropic (39 sp.), Afrotropic (8 sp.) and Palaearctic (12 sp.) et al. 1995; Krzemin´ski & Evenhuis 2000; Krzemin´ski & Regions. Fifteen fossil species are known from the Eocene and Krzemin´ska 2003). Oligocene of Europe (three from the Baltic amber) and four species from Palaeocene and Oligocene of North America. Subfamily Limnophilinae Bigot, 1854 Limnophila (Limnophila) cyclospila Cockerell & Haines, 1921 Genus Gurnardia Krzemin´ski, n. gen. (Fig. 15, Pl. 2b) 1921 Limnophila cyclospila Cockerell & Haines, pp. 109–10, Diagnosis. Sc short, only little longer than half wing length, fig. I9213 ending little before fork of Rs into R2 þ 3 þ 4 and R5; only 1994 Limnophila cyclospila Evenhuis, p. 75

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Figures 14–25 Limoniidae, wing venation. (14) Gurnardia corami Krzemin´ski, n. sp., holotype NHMUK In.64104. (15) Limnophila (Limnophila) cyclospila Cockerell & Haines, 1921, holotype NHMUK I.9213. (16) Limnophila (Limnophila) deleta Cockerell, 1921, holotype NHMUK I.9053. (17) Pilaria hooleyi Krzemin´ski, n. sp., holotype, NHMUK In.25254. (18) Pilaria volodii Krzemin´ski, n. sp., holotype NHMUK I.9167. (19) Pseudolimnophila (Pseudolimnophila) disjunctula (Cockerell & Haines, 1921), holotype NHMUK. In.24355. (20) Dactylolabis (Dactylolabis) spiloptera (Cockerell, 1921) n. comb., holotype NHMUK I.9015. (21) Cheilotrichia (Cheilotrichia) duplicata Krzemin´ski, n. sp., holotype NHMUK II 2763. (22) Cheilotrichia (Empeda) ferruginea (Cockerell, 1921), holotype NHMUK I.8963. (23) Cheilotrichia (Empeda) hyalina (Cockerell, 1921), holotype NHMUK I.24342. (24) Cheilotrichia (Empeda) szwedoi Krzemin´ski, n. sp., holotype NHMUK In.17082. (25) Gonomyia (Gonomyia) indecisa Cockerell & Haines, 1921, holotype NHMUK. I.9087.

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Plate 2 Limoniidae. (a) Gurnardia corami Krzemin´ski, n. sp., holotype NHMUK In.64104. (b) Limnophila (Limnophila) cyclospila Cockerell, 1921, holotype NHMUK I.9213. (c) Limnophila (Limnophila) deleta Cockerell, 1921, holotype NHMUK I.9053. (d) Pilaria hooleyi Krzemin´ski, n. sp., holotype NHMUK In.25254. (e) Pilaria volodii Krzemin´ski, n. sp., holotype NHMUK I.9167. (f ) Pseudolimnophila (Pseudolimnophila) disjunctula (Cockerell & Haines, 1921) n. comb., holotype NHMUK In.24355. (g) Dactylolabis (Dactylolabis) spiloptera (Cockerell, 1921) n. comb., holotype NHMUK I.9015. (h) Cheilotrichia (Cheilotrichia) duplicata Krzemin´ski, n. sp., holotype NHMUK II 2763. (i) Cheilotrichia (Empeda) ferruginea (Cockerell, 1921), holotype part NHMUK I.8963. (j) Cheilotrichia (Empeda) hyalina (Cockerell, 1921), holotype NHMUK In.24342.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 12 WIESŁAW KRZEMIN´ SKI ET AL. Holotype. NHMUK I.9213 (female), Hooley Collection), Genus Pilaria Sintensis, 1889 Insect Bed; late Eocene; NW Isle of Wight, UK. Additional material. NHMUK I.9059, I.9868, I.9943, Brodie Type species. Limnobia pilicornis Zetterstedt, 1851, p. 3885 Collection; In.17491 (female), Smith Collection; In.24775, (designated by Sharp 1890). In.25209, In.25269, In.25270, Hooley Collection. Remarks. Forty-six recent species are known from Palaearctic Diagnosis. Wing with conspicuous colour pattern; Sc ending (15 sp.), Nearctic (14 sp.), Afrotropic (8), Oriental (7 sp.), a little before fork of Rs into R2 þ 3 þ 4andR5;R2þ 3 þ 4 Australian (1 sp.) and Neotropic (1 sp.) Regions. Five fossil very short; R4 16 times longer than R2 þ 3 þ 4; M1 long, 1.5 species are known from Eocene and Miocene of Europe (three times longer than d cell; cross-vein m-cu in half of d cell. from the Baltic amber). Redescription. Wing length 7.0–7.8 mm, with very distinct colour pattern (Fig. 15). Body is preserved partially only in two specimens (holotype I.9213 and In.17491). : only Pilaria hooleyi Krzemin´ski, n. sp. cylindrical scapus and broad, oval pedicel is preserved in one (Fig. 17, Pl. 2d) specimen, In.17491. Venation. Sc ending before fork of Rs into R2 þ 3 þ 4and Holotype. NHMUK In.25254, Hooley Collection, Insect R5; cross-vein sc-r at its length before end of Sc; R1 rather Bed; late Eocene; NW Isle of Wight, UK. short; cross-vein r-r (R2) at its length before end of R1; Additional material. NHMUK I.9032/In.64099 (part and R2 þ 3 þ 4 very short; R4 16 times longer than R2 þ 3 þ 4; counterpart), Brodie/Hooley Collections. Rs about 10 times longer than R2 þ 3 þ 4; d cell short and Derivation of name. A new species is dedicated to R.W. broad; petiole of m1 cell a little shorter than d cell; M1 about Hooley, the famous collector of fossil insects from the Isle of twice longer than petiole of m1 cell; cross-vein m-cu in half of Wight. d cell; A2 long and somewhat wavy. Diagnosis. Sc ending opposite fork of Rs into R2 þ 3 þ 4 Remarks. The original description of (Cockerell 1921) of and R5; d cell long and narrow; petiole of m1 cell very Limnophila cyclospila has many mistakes, the most important long, about twice longer than M1 and 1.5 times longer than d being the absence of vein Sc. Cross-vein m-cu is wrongly posi- cell. tioned in distal part of d cell position. Description. Wing length 2.9–5.2 mm, without colour pattern. The colour pattern may indicate genus Venation. Sc rather short, ending opposite fork of Rs; cross- Alexander, but without a complete specimen preserved in vein sc-r twice its length before end of Sc; R1 rather long; good condition it is not possible to make this taxonomical cross-vein r-r (R2) at its length before end of R1; Rs five times decision. longer than R2 þ 3 þ 4; R3 about 1.5 times longer than Rs; d cell long and narrow; petiole of m1 cell about twice longer Limnophila (Limnophila) deleta Cockerell, 1921 than M1 and 1.5 times longer than d cell; cross-vein in third (Fig. 16, Pl. 2c) portion of d cell; A2 little curved. Remarks. Basing only on wing venation it is very difficult to 1921 Limnophila deleta Cockerell, pp. 459, 462, fig. 9 decide about generic position of this species, but in my opinion 1994 Limnophila deleta Evenhuis, 1994, p. 75 the general pattern of wing venation is more similar to the genus Pilaria than to Limnophila or Pseudolimnophila Alexander. Holotype. NHMUK I.9053 (female), Brodie Collection, Insect Bed; late Eocene; NW Isle of Wight, UK. Pilaria volodii Krzemin´ski, n. sp. Additional material. NHMUK, I.9019, I.9060, I.9067, (Fig. 18, Pl. 2e) I.9684, Brodie Collection; In.17115, In.17171, In.24414, Smith Collection; In.17484/In.64127 (part and counterpart), Smith/ Hooley Collections; In.25217, In.25474, In.64127, Hooley Holotype. NHMUK I.9167/I.9201 (part and counterpart), Collection; PI. II. 2764, Palaeontological Institute, Moscow Brodie Collection, Insect Bed; late Eocene; NW Isle of Wight, team, north end Thorness Bay, Isle of Wight. UK. Diagnosis. Sc rather long, ending opposite fork of Rs into Derivation of name. A new species is dedicated to Vladimir R2 þ 3 þ 4 and R5; Rs twice longer than R2 þ 3 þ 4; d cell (Volodia) Blagoderov (NHM, London), a paleoentomologist short; cross-vein m-cu little behind fork of Mb into M1 þ 2 and specialist on Diptera. and M3 þ 4 in 1/4 of d cell; A2 long and somewhat wavy. Diagnosis. Sc very short, little shorter than half wing length, Redescription. Wing length 5.4–8 mm, without colour pattern. ending opposite 2/3 of Rs; R3 and M1 very short; petiole of Few specimens are preserved with small portion of the body. m1 cell more than twice longer than d cell and about five times Only holotype is preserved with body, but antennae and palps longer than M1. are missing. Description. Wing length 4.7–5.0 mm, without colour pattern; Venation. Sc rather long, ending opposite fork of Rs on anal part of the wing destroyed. R2 þ 3 þ 4 and R5; cross-vein sc-r at its length before end of Venation. Sc very short, little shorter than half wing length; Sc; R1 rather long; cross-vein r-r (R2) at its length before end cross-vein sc-r at three times its length before end of Sc; R1 of R1; Rs about twice longer than R2 þ 3 þ 4; R3 about 1/4 long; cross-vein r-r (R2) at end of R1; R2 þ 3 þ 4 about 1/6 longer than Rs; d cell small; petiole of m1 cell little longer shorter than Rs and only little longer than R4; R3 very short, than d cell; M1 about 1.4 times longer than petiole of m1 about 1/3 of R4; d cell long and narrow; M1 very short, cell; cross-vein m-cu in quarter of d cell; A2 long and little petiole of m1 cell more than twice longer than d cell and about wavy. five times longer than M1; cross-vein m-cu in half length of d Remarks. Limnophila deleta is one of most common species cell. of Limoniidae in the Isle of Wight. The specimens allotted Remarks. Venation pattern of the wing venation with very herein are very variable and they may possibly represent short Sc, R3 and M1 is rather rare among Limoniidae. This more than one species, but based only on wing venation it is new species is different from all Pilaria species from Baltic not possible separate them further. amber.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 13 Genus Pseudolimnophila Alexander, 1919 Dactylolabis (Dactylolabis) spiloptera (Cockerell, 1921) n. comb. Type species. Limnophila luteipennis Osten Sacken, 1860, p. (Fig. 20, Pl. 2g) 236 (designated by Alexander 1920). 1921 Epiphragma spilopterum Cockerell, pp. 458–59, fig. 8 1994 Epiphragma spilopterum Evenhuis, p. 70 Subgenus Pseudolimnophila Alexander, 1919 Holotype. NHMUK I.9015, Brodie Collection, Insect Bed, Type species. As for genus. late Eocene; NW Isle of Wight, UK. Remarks. One hundred recent species of the subgenus Pseudo- Diagnosis. Wing with colour pattern; Sc very long, ending limnophila are known from Oriental (38 sp.), Nearctic (28 sp.), opposite mid of R2 þ 3 þ 4; Rs very long, longer than R3. Neotropic (four sp.), Afrotropic (19 sp.), Palaearctic (seven Redescription. Wing length 11.5 mm, with colour pattern. sp.), Afrotropic (five sp.), Palaearctic (three sp.) Regions. Nine Head, thorax, part of the and most parts of the fossil species are known from Baltic amber (Eocene), one from wing are preserved. Sicilian amber (Miocene) and one from Canada (). Venation. Sc very long, ending opposite mid of R2 þ 3 þ 4; cross-vein sc-r at its length before end of Sc; R1 long; cross- Pseudolimnophila (Pseudolimnophila) disjunctula (Cockerell & vein r-r about twice its length before end of R1; Rs very long, Haines, 1921) n. comb. little longer than R2 þ 3 þ 4 and R3 together; R2 þ 3 þ 42.5 (Fig. 19, Pl. 2f ) times longer than R3; d cell very broad; cross-vein m-cu in about 1/3 of d cell; A2 rather long and straight. 1921 Adelphomyia disjunctula Cockerell and Haines, pp. 83– Remarks. Cockerell (1921) placed this species in the genus 84, fig. H1398 Epiphragma Osten Sacken, but a careful study has shown that 1994 Adelphomyia disjunctula Evenhuis, 1994, p. 61 the cross-vein in the costal cell, the most important character of the genus Epiphragma, is missing here. General venation pattern indicates that this species most probably belongs to Holotype. NHMUK In.24355, Hooley Collection, Insect the genus Dactylolabis. Bed; late Eocene; NW Isle of Wight, UK. Additional material. NHMUK I.9050, Brodie Collection; Subfamily Chioneinae Rondani, 1841 In.17383, Smith Collection; In.64119, Hooley Collection. Diagnosis. Sc long, ending opposite fork of Rs on Genus Cheilotrichia Rossi, 1848 R2 þ 3 þ 4 and R5; R1 long, ending opposite mid R3; M1 very long, twice longer than petiole of m1 cell and 2.5 times Type species. imbuta Meigen, 1818, p. 114 (by longer than petiole of m1 cell. monotypy). Redescription. Wing length 8.0–9.0 mm, without colour pattern. Specimens I.9050 and In.64119 are preserved with Subgenus Cheilotrichia Rossi, 1848 portions of the body. Type species. As for genus. Venation. Sc long, ending opposite mid of R2 þ 3 þ 4; Remarks. Thirty recent species of the subgenus Cheilotrichia cross-vein sc-r little longer than end of Sc; R1 long, ending are known from Palaearctic (18 sp.), Oriental (3 sp.), Afro- opposite mid of R3; cross-vein r-r (R2) about twice its length tropic (3 sp.), Australian (2 sp.) and Nearctic (1 sp.) Regions. before end of R1; R3 little wavy, about 1.5 times longer than Till now no fossil species from the nominative subgenus was Rs and five times longer than R2 þ 3 þ 4; M1 very long, twice known. longer than petiole of m1 cell and 1.5 times longer than d cell; cross-vein m-cu close to mid of d cell; A2 little wavy. Cheilotrichia (Cheilotrichia) duplicata Krzemin´ski, n. sp. Remarks. Cockerell & Haines (1921) placed this species in (Fig. 21, Pl. 2h) the genus Adelphomyia Bergroth, but absence of long Sc macrotrichia on wing membrane and presence of four medial Holotype. NHMUK II 2763, collected by the Palaeontological veins indicate that this species cannot belong to this genus Institute, Moscow team; Insect Bed; late Eocene; north end but rather to the genus Pseudolimnophila. Thorness Bay, Isle of Wight, UK. Diagnosis. Sc ending after 2/3 of Rs; Rs little shorter than Subfamily Dactylolabinae Alexander, 1920 R3; R4 twice longer than R2 þ 3 þ 4andR3þ 4 together. Genus Dactylolabis Osten Sacken, 1860 Description. Wing length 4.5 mm. Middle part of wing broken and partially destroyed. Type species. Limnophila montana Osten Sacken, 1860, Venation. Sc long, ending behind 2/3 of Rs; cross-vein sc-r p. 240 (by monotypy). twice its length before end of Sc; R1 long, ending behind fork of R3 þ 4 on R3 and R4; cross-vein r-r (R2) about five times Subgenus Dactylolabis Osten Sacken, 1860 before end of R1; R3 little longer than Rs and about twice longer than R2 þ 3 þ 4andR3þ 4together;R2þ 3 þ 4a Type species. As for genus. little longer than R3 þ 4; d cell short and narrow; M3 three Remarks. Fifty-seven recent species of the subgenus Dacty- times longer than d cell; cross-vein m-cu little before fork of lolabis are known only from Palaearctic (39 sp.) and Nearctic Mb on M1 þ 2andM3þ 4; anal vein somewhat wavy. (18 sp.) Regions. Thirteen fossil species are described from the Remarks. Cheilotrichia (Cheilotrichia) duplicata n. sp. is genus Dactylolabis but probably only four from the Oligocene the first fossil representative of the subgenus Cheilotrichia. and Miocene of Europe belong to the nominative subgenus. Recently the subgenus has been represented by 18 species From Baltic amber no representative of this subgenus is distributed in Holarctic, Oriental, Australian and Ethiopian known. Regions, but most species are described from Palaearctic

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 14 WIESŁAW KRZEMIN´ SKI ET AL. Region (nine sp.). Species of this subgenus prefer wet environ- Redescription. Wing length 4.0–5.0 mm. In both specimens ments near streams and small ponds. anal part of the wings and last portion of Cu, A1 and A2 are not preserved. Subgenus Empeda Osten Sacken, 1869 Venation. Sc rather long, ending after mid of Rs; cross-vein sc-r three times his length before end of Sc; R1 long, ending behind fork of R3 þ 4 into R3 and R4; cross-vein r-r (R2) Type species. Empeda stigmatica Osten Sacken, 1869, p. 184 about five times before end of R1; Rs as long as R2 þ 3 þ 4 (designated by Coquillett 1910). and R3 þ 4 together, and three times longer than R3; Remarks. One hundred and twelve recent species are R2 þ 3 þ 4 as long as R3; d cell long and narrow, M1 þ 2 described from Oriental (34 sp.), Neotropic (31 sp.), Palaearctic only little longer than d cell; cross-vein m-cu in proximal 1/4 (22 sp.), Nearctic (14 sp.), Australian (nine species) and Afro- length of d cell. tropic (two species) Regions. Remarks. Cockerell (1921) described specimen In.24344 Twelve fossil species are described, mostly (eight sp.) from (Hooley number H. 1534) as Gonomyia grisea because he had Baltic amber (Eocene), two from the Isle of Wight (late overlooked the presence of cross-vein r-r (R2). This vein is the Eocene), one from Sakhalin amber (Palaeocene) and one key character discerning genera Gonomyia and Cheilotrichia. from amber (Upper Cretaceous). Cheilotrichia (Empeda) szwedoi Krzemin´ski, n. sp. Cheilotrichia (Empeda) ferruginea (Cockerell, 1921) (Fig. 24, Pl. 3a) (Fig. 22, Pl. 2i) Holotype. NHMUK In.17082, Smith Collection; Insect 1921 Empeda ferruginea Cockerell, p. 457, fig. 6 Bed; late Eocene; NW Isle of Wight, UK. 1994 Cheilotrichia ferruginea Evenhuis, p. 65 Derivation of name. A new species is dedicated to Jacek Szwedo (Poland), specialist of fossil Homoptera. Holotype. NHMUK I.8963/I.9084 (part and counterpart), Diagnosis. Sc little shorter than half wing length; R1 short, Brodie Collection; Insect Bed; late Eocene; NW Isle of Wight, ending before fork of R3 þ 4 into R3 and R4; Rs long, 1.5 UK. times longer than R2 þ 3 þ 4andR3þ 4 together and four Additional material. I.9901/I.9139 (part and counterpart), times longer than R3; M1 þ 2 about 1.5 times longer than d Brodie Collection. cell. Diagnosis. Sc short, ending near after fork of Rs; Rs about Description. Specimen with most part of the body preserved, 1.5 times longer than R3; R4 1.5 times longer than R2 þ 3 þ 4 only last part of abdomen is lost. Wing length 6.1 mm, with and R3 þ 4 together; d cell rather short. venation clearly visible. Redescription. Wing length 4.4–4.7 mm, clear. Anal part of Antenna: scapus and pedicel invisible; 12 flagellomeres the wing destroyed and terminal portion of Cu, A1 and A2 preserved, basal three biggest and barrel like, next ones more not preserved. slender; with short three to four bristles. Venation. Sc rather short, ending a little behind fork of Rb Venation. Sc short, less than half wing length; cross-vein sc-r into R1 and Rs; cross-vein sc-r at its length before end of Sc; 1.5 times its length before end of Sc; R1 very short, ending- R1 long, ending behind fork of R3 þ 4 into R3 and R4; cross- opposite mid of R3 þ 4, far before R3 þ 4forkintoR3and vein r-r (R2) about three times before end of R1; Rs as long as R4; Rs long about 1.5 times longer than R2 þ 3 þ 4and R2 þ 3 þ 4andR3þ 4 together, and about 1.5 times longer R3 þ 4 together, and four times longer than R3; R2 þ 3 þ 4 than R3; R4 about 1.5 times longer than Rs; d cell rather as long as R3; d cell rather long; M1 þ 2 about 1.5 longer short and narrow; M1 þ 2 about twice longer than d cell; than d cell; cross-vein m-cu in proximal 1/3 of d cell length; cross-vein m-cu close to mid of d cell. anal field broad; A2 little wavy, terminal section strongly Remarks. Wing venation drawn by Cockerell (1921) is curved. incomplete and with many mistakes. Recent revision of the Remarks. This new species is represented only by one specimen, holotype and two additional specimens found in the collection but this very characteristic venation (especially length of Sc of NHMUK allowed a more complete reconstruction of the and R1) separates it from the remaining species of the sub- wing venation. genus Empeda from the Isle of Wight.

Genus Gonomyia Meigen, 1818 Cheilotrichia (Empeda) hyalina (Cockerell, 1921) (Fig. 23, Pl. 2j) Type species. Limnobia tenella Meigen, 1818, p. 146 (by monotypy). 1921 Empeda hyalina Cockerell, p. 457, fig. 5 1921 ‘Gonomyia’ grisea Cockerell, p. 461, fig. 14, syn. nov. Subgenus Gonomyia Meigen, 1818 1994 Cheilotrichia hyalina Evenhuis, p. 65 Type species. As for genus. 1994 Gonomyia? grisea Evenhuis, p. 89 Remarks. Two hundred and sixteen recent species world- wide distributed from cold to tropical zone. Five fossil species Holotype. NHMUK I.24342, Hooley Collection; Insect of the genus Gonomyia are known, but probably only two Bed; late Eocene; NW Isle of Wight, UK. belong to the nominative subgenus: one from Italy (Miocene) Additional material. NHMUK In.24344, Hooley Collection, and one from Germany (Oligocene). Only one fossil species described as the holotype of the species Gonomyia grisea from the subgenus Electrogonomyia Alexander is described Cockerell, 1921. from Baltic amber. Diagnosis. Sc ending behind mid of Rs; Rs three times From the Isle of Wight Cockerell & Haines (1921) described longer than R3; R2 þ 3 þ 4andR3þ 4togetheraslongas Gonomyia indecisa; in the same year Cockerell (1921) described Rs; and 1.5 times longer than R4; d cell long and narrow. G. ferrea, G. grisea and G. lutescens. Revision of the holotypes

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Plate 3 Limoniidae. (a) Cheilotrichia (Empeda) szwedoi Krzemin´ski, n. sp., holotype NHMUK In.17082. (b) Gonomyia (Gonomyia) indecisa Cockerell & Haines, 1921, holotype NHMUK In.9087. (c) Gymnastes (Paragymnastes) fasciatipennis Cockerell, 1921, holotype NHMUK I.10242. (d) Symplecta (Psiloconopa) gurnetensis Krzemin´ski, n. sp., holotype NHMUK In.25266. (e) Styringomyia concinna (Cockerell, 1917a) n. comb., holotype NHMUK I.8666. (f ) Thaumastoptera undulata (Cockerell & Haines, 1921) n. comb., holotype NHMUK I.9146. (g) Orimarga (Orimarga) lenae Krzemin´ski, n. sp., holotype NHMUK In.25487. (h) Dicranomyia (Dicranomyia) aliena (Cockerell, 1921) n. comb., holotype NHMUK I.9018. (i) Dicranomyia (Dicranomyia) brodiei (Cockerell, 1917a) n. comb., holotype NHMUK I.8603. (j) Dicranomyia (Dicranomyia) excavata Cockerell & Haines, 1921, holotype NHMUK I.9946.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 16 WIESŁAW KRZEMIN´ SKI ET AL. demonstrated that they all belong to one very common though 1921 Gymnastes fasciatipennis Cockerell, pp. 456–457, fig. 4 somewhat variable species. Since G. indecisa was described 1931 Gymnastes fasciatipennis Edwards in Marshall & Staley, as the first, G. ferrea and G. lutescens are junior synonyms of p. 38 G. indecisa. G. grisea does not belong to the genus Gonomyia 1994 Gymnastes fasciatipennis Evenhuis, p. 75 but to Cheilotrichia and is a junior synonym of C. (Empeda) hyalina. Holotype. NHMUK I.10242, Brodie Collection; Insect Bed; late Eocene; NW Isle of Wight, UK. Gonomyia (Gonomyia) indecisa Cockerell & Haines, 1921 Additional material. NHMUK I, 9282, I.9297 (female), (Fig. 25, Pl. 3b) I.9959, Brodie Collection; I.17169 (male), In.17494, Smith Collection; In.25386, In.25408, I, 64105, In.64114, In.64115, I.64121, Hooley Collection; II 2848, Emma Ross Collection, 1921 Gonomyia indecisa Cockerell and Haines, p. 111, north end Thorness Bay; MIWG 3685 (female). fig. I9087 Diagnosis. Wings with three broad dark bands; Sc shorter 1921 ‘Gonomyia’ ferrea Cockerell, p. 460, fig. 12, syn. nov. than half wing, ending opposite mid Rs; cross-vein r-r (R2) 1921 ‘Gonomyia’ lutescens Cockerell, p. 461, fig. 13, syn. lost; R2 þ 3 very short. nov. Redescription. Wing 3.2–4.8 mm long, with three broad 1994 Gonomyia? ferrea Evenhuis, p. 89 dark grey bands, clearly separated. Some specimens with 1994 Gonomyia? lutescens Evenhuis, p. 89 body partially preserved. Head, thorax and abdomen dark brown or intensive black. Antennae and palps not preserved. Holotype. NHMUK I.9087, Brodie Collection; Insect Bed; Venation. Sc very short, shorter than half wing, ending late Eocene; NW Isle of Wight, UK. opposite mid Rs; cross-vein sc-r poorly visible, probably twice Additional material. In.24343 (described as G. ferrea –old its length before end of Sc; R1 short; cross-vein r-r (R2) twice number H.835, Hooley Collection); I.9217/I.9409 (part described its length before end of R1; Rs twice longer than R2 þ R3; R4 as G. lutescens), I.9044(1), I.9283, Brodie Collection; In.24632, 1.5 times longer than Rs and three times longer than R2 þ 3; In.24812, In.25420, In.25429, In.64120, In.64129, Hooley Collec- cross-vein r-m little before or in fork of Rs on R2 þ 3 þ 4and tion; I.9728/In.17216 (part and counterpart), Brodie/Smith R5; d cell very narrow and rather long; M1 þ 2littlemore Collections; In.17248, Smith Collection. than twice longer than d cell; cross-vein m-cu little before Diagnosis. Sc short, ending opposite 2/3 of Rs; Rs about fork of Mb into M1 þ 2andM3þ 4; A1 slightly wavy; A2 four times longer than R2 þ 3 þ 4 and twice longer than R3; rather straight. dcellopen. Remarks. Gymnastes fasipennis is one of the most common Description. Wing in very bad condition, only distal part fossil Limoniidae from the Isle of Wight. Recently the sub- (about 3 mm) is preserved, total length probably 5.5–6.0 mm. genus Paragymnastes is known only from the Oriental (16 sp.), Venation. Sc short, ending opposite 2/3 of Rs; cross-vein Australian (11 sp.) and Palaearctic (two sp.) Regions. All sc-r at its length before end of Sc; R1 rather short; R2 absent; species prefer warm climate. Presence of the representative of Rs about four times longer than R2 þ 3 þ 4 and twice longer this genus indicates tropical or subtropical climate in the late than R3; d cell open by atrophy of cross-vein m3-m4; position Eocene. of cross-vein m-cu variable: near before, in or little behind fork of Mb into M1 þ 2andM3þ 4; A2 somewhat wavy. Genus Symplecta Meigen, 1830 Remarks. Gonomyia indecisa is common in the materials from the Isle of Wight. Position of cross-vein m-cu and pro- Type species. Limnobia punctipennis Meigen, 1818, p. 147 portions between veins are so much variable that is not possible (designated by Westwood 1840). to find the border between species described by Cockerell (1921) and Cockerell & Haines (1921). In this situation wing venation Subgenus Psiloconopa Zetterstedt, 1838 cannot be used to establish a different species. Type species. Psiloconopa meigeni Zetterstedt, 1838, p. 847 Genus Gymnastes Brunetti, 1911 (by monotypy). Remarks. Sixty-one recent species are known from Nearctic Type species. Gymnastes violaceus Brunetti, 1911, p. 282 (29 sp.), Palaearctic (17 sp.), Oriental (11 sp.), Australian (two (by monotypy). sp.), Afrotropic (one sp.) and Neotropic (one sp.) Regions. Remarks. The genus Gymnastes is represented in Recent Only two fossil species are known from the Oligocene and fauna by three subgenera and 43 species in Oriental (25 sp.), Miocene of Europe. Australian (11 sp.), Afrotropic (three sp.), Palaearctic (three sp.) one species is known from Neotropic Region. Only one Symplecta (Psiloconopa) gurnetensis Krzemin´ski, n. sp. fossil species is known. (Fig. 27, Pl. 3d)

Subgenus Paragymnastes Alexander, 1922 Holotype. NHMUK In.25266, Hooley Collection); Insect Bed; late Eocene; NW Isle of Wight, UK. Type species. Limnobia fascipennis Thomson, 1869, p. 447 Derivation of name. The name species origin from the old (original designation). name of Gurnard Bay (Gurnet Bay). Remarks. Thirty-one recent species are known from Oriental, Diagnosis. Sc rather long, ending behind cross-vein r-r (R2); Australian and Eastpalaearctic Regions cross-vein sc-r opposite proximal 1/4 Rs; cross-vein very close to fork of Mb into M1 þ 2andM3þ 4. Gymnastes (Paragymnastes) fasciatipennis Cockerell, 1921 Description. Wing length 4.1 mm without colour pattern. (Fig. 26, Pl. 3c) Wing folded.

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Figures 26–36 Limoniidae, wing venation. (26) Gymnastes (Paragymnastes) fasciatipennis Cockerell, 1921, holotype, NHMUK I.10242. (27) Symplecta (Psiloconopa) gurnetensis Krzemin´ski, n. sp., holotype NHMUK In.25266. (28) Ilisia (Lunaria) incognita (Cockerell, 1921), holotype NHMUK I.9186. (29) Styringomyia concinna (Cockerell, 1917a), holotype NHMUK I.8666. (30) Thaumastoptera undulata (Cockerell & Haines, 1921), holotype NHMUK I.9146. (31) Orimarga (Orimarga) lenae Krzemin´ski, n. sp., holotype NHMUK In.25487. (32) Dicranomyia (Dicranomyia) aliena (Cockerell, 1921), holotype NHMUK I.9018. (33) Dicranomyia (Dicranomyia) brodiei (Cockerell, 1917a), holotype NHMUK I.8603. (34) Dicranomyia (Dicranomyia) excavata Cockerell & Haines, 1921, holotype NHMUK I.9946. (35) Dicranomyia (Dicranomyia) fasciata Krzemin´ski, n. sp., holotype NHMUK I.9058. (36) Limonia spilota (Cockerell, 1921), holotype NHMUK In.17114.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 18 WIESŁAW KRZEMIN´ SKI ET AL. Venation. Sc rather long, ending behind cross-vein r-r (R2); Remarks. One hundred and sixty-five recent species are cross-vein sc-r opposite proximal 1/4 Rs, about 17 times its known mostly from tropical and subtropical regions of the length before end of Sc; R1 long; cross-vein r-r (R2) 13 times world. Only four fossil species are known from the Eocene, its length before end of R1; Rs 3.5 times longer than Oligocene and of Europe. One species is described R2 þ 3 þ 4; R4 about 1.5 times longer than Rs and about six from Baltic amber. times longer than R2 þ 3 þ 4; d cell short; M3 2.3 times longer than d cell; cross-vein m-cu somewhat before fork of Mb into Styringomyia concinna (Cockerell, 1917a) M1 þ 2andM3þ 4; A2 long and strongly wavy in terminal (Fig. 29, Pl. 3e) section. Remarks. Representatives of the genus Symplecta generally 1917a Mesomyites concinnus Cockerell, pp. 377–78, 384, pl. are very rare in fossil material. Until now, they were described 31, fig. 7 only from the Oligocene of France (Theobald 1937), Miocene 1917b Styringomyia concinna Cockerell, p. 141 of Italy (Gentilini 1984; Krzemin´ski & Gentilini 1992) and 1921 Styringomyia extensa Cockerell and Haines, p. 112, fig. Miocene of Spain (Krzemin´ski and Arillo 2008). H261, syn. nov. 1994 Styringomyia concinna Evenhuis, p. 84 Genus Ilisia Rondani, 1856 1994 Styringomyia extensa Evenhuis, p. 84

Type species. Erioptera maculata Meigen, 1804, p. 51 Holotype. NHMUK I.8666, Brodie Collection; Insect Bed; (original designation). late Eocene; NW Isle of Wight, UK. Additional material. NHMUK In.24354, Hooley Collection Subgenus Lunaria Savchenko, 1973 (H 261), described as Styringomyia extensa; I.8998 (1), Brodie Collection; II 2,785 (2) collected by the Zoological Institute, Type species. Ilisia (Lunaria) idiophallus Savchenko, 1973, St Petersburg team, Burnt Wood, Isle of Wight. p. 38 (original designation). Diagnosis. Sc very short, about 1/3 wing length, ending just Remarks. Only two recent species are known from the behind fork of Rb into R1 and Rs; R1 ending opposite proximal Palaearctic Region. 1/3 of Rs; Rs twice times longer than R2 þ 3 þ 4. Redescription. Wing length 3.5–4.8 mm. Ilisia (Lunaria) incognita (Cockerell, 1921) n. comb. Venation. Sc very short, about 1/3 wing length, ending just (Fig. 28, Pl. 7b) behind fork of Rb into R1 and Rs; cross-vein sc-r absent; only three long radial veins present; R1 very short, ending opposite 1921 Limnophila incognita Cockerell, p. 462, Fig. 16 1/3 of Rs; cross- vein r-r (R2) and vein R3 probably lost by 1994 Limnophila incognita Evenhuis, p. 75 atrophy; Rs twice longer than R2 þ 3 þ 4; R5 1.75 times longer than Rs; d cell long and narrow, about twice longer Holotype. NHMUK I.9186, Brodie Collection; Insect Bed; than M3; cross-vein m-cu in 1/5 of d cell; A2 long and little late Eocene; NW Isle of Wight, UK. wavy. Additional material. NHMUK In.64111, Hooley Collection. Remarks. Cockerell (1917a) described Mesomyites concinnus Diagnosis. Sc short, ending before fork of Rs into and mistakenly included this species in the family Empididae R2 þ 3 þ 4 and R5; cross-vein opposite proximal 1/3 of Rs; (Diptera Brachycera) and together with Haines (Cockerell & M3 1.5 times longer than d cell; cross-vein m-cu behind fork Haines 1921) described new species Styringomyia extensa. of Mb into M1 þ 2andM3þ 4. Study of the holotypes of these species shoved that it is the Redescription. Most parts of body preserved, without palps, same species from the genus Styringomyia and S. extensa is legs and genitalia. Wing length 6.3 mm. the junior synonym. Antenna. scapus rather long; pedicel short and rounded; only three flagellomeres are preserved: first two short, broad Subfamily Limoniinae Speiser, 1909 and next narrow and elongate, little widened basally; all with bristles shorter than flagellomeres. Genus Thaumastoptera Mik, 1866 Venation. Sc short, ending before fork of Rs into R2 þ 3 þ 4 and R5; cross-vein opposite proximal 1/3 of Rs, about nine Type species. Thaumastoptera calceata Mik, 1866, p. 303 times its length before end of Sc; R1 rather long; cross-vein (original designation). r-r (R2) eight times its length before end of R1; Rs long, only about 1/3 shorter than R5; R2 þ 3 þ 4andR2þ 3veryshort, Subgenus: Thaumastoptera Mik, 1866 R2 þ 3 þ 4 only twice longer than R2 þ 3; d cell narrow; M3 1.5 times longer than d cell; cross-vein little behind fork of Mb Type species. As for genus. into M1 þ 2andM3þ 4; A2 slightly wavy. Remarks. Eight recent species are known from Palaearctic Remarks. Ilisia (Lunaria) incognita is the first fossil repre- (three sp.), Oriental (two sp.), Afrotropic (two sp.) and Nearctic sentative of the genus Ilisia. Recently, Ilisia is a small genus (one sp.) Regions. Only two fossil species are known from the whose species live mostly in Palaearctic and Oriental Regions, Baltic amber (Eocene). (some are also in Afrotropical and Australian Regions). Classification of the species from the Isle of Wight in the sub- Thaumastoptera undulata (Cockerell & Haines, 1921) genus Lunaria is based only on wing venation. n. comb. (Fig. 30, Pl. 3f ) Genus Styringomyia Loew, 1845 1921 Dicranomyia undulata Cockerell and Haines, p. 110, fig. I9146 Type species. Styringomyia venusta Loew, 1845, p. 6 (by 1931 Dicranomyia undulata Alexander, pp. 8, 41 monotypy) (fossil). 1994 Dicranomyia undulata Evenhuis, p. 68

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 19 Holotype. NHMUK I.9146, Brodie Collection; Insect Bed; Type species. As for genus. late Eocene, NW Isle of Wight, UK. Remarks. Eight hundred and fifty-seven recent species Diagnosis. Sc short, ending opposite fork of Rb into R1 and worldwide distributed from cold to tropical zones. About 30 Rs: Rb forked behind mid wing; cross-vein m-cu at its length fossil species are known from the Upper Cretaceous to Miocene. before fork of Mb into M1 þ 2andM2þ 3. Unfortunately, representatives of the nominal subgenus Redescription. Wing length 6.0 mm. cannot be identified without knowledge of morphology of Venation. Sc very short, only a little longer than half wing male genitalia, and only wings are presented. Four species are length, ending opposite fork of Rb into R1 and Rs; cross-vein known from Baltic amber. sc-r twice its length before end of Sc; Rb forked behind mid wing; R1 rather short; cross-vein r-r(R2) twice its length Dicranomyia (Dicranomyia) aliena (Cockerell, 1921) n. comb. before end of R1; Rs very short , only twice longer than (Fig. 32, Pl. 3h) R2 þ 3 þ 4; R3 þ 4 three times longer than R2 þ 3 þ 4and twice longer than Rs; R5 three times longer than Rs; d cell 1921 Limnophila aliena Cockerell, pp. 461–62, fig. 15 open by atrophy of cross-vein between M3 and M4; M3 1.5 1931 Limnophila aliena Alexander, p. 8 times longer than M1 þ 2; cross-vein m-cu at its length 1994 Limnophila aliena Evenhuis, p. 75 before fork of Mb into M1 þ 2andM3þ 4; A2 strongly wavy terminally. Remarks. Cockerell & Haines (1921) erroneously included Holotype. NHMUK I.9018/I.9420 (part and counterpart), T. undulata in the genus Dicranomyia. Brodie Collection; Insect Bed; late Eocene; NW Isle of Wight, Recently genus Thaumastoptera is not represented in UK. Australian and Neotropical Regions; most species live in the Additional material. NHMUK, I.9758, Brodie Collection. Holarctic Region. Until now only two species from Baltic Diagnosis. Sc rather long, ending opposite mid Rs; d cell amber have been described (Krzemin´ski, 1985). long and broad; cross-vein m-cu in proximal 1/3 of d cell. Description. Wing length 5.4–7.0 mm, basal part and small parts of medial and cubital field destroyed. Genus Orimarga Osten Sacken, 1869 Venation. Sc rather long, ending opposite mid of Rs; cross- vein sc-r at its length before end of Sc; R1 rather long, ending Type species. Limnobia alpina Zetterstedt, 1851, p. 3894 opposite fork; of R2 þ 3 þ 4intoR3andR3þ 4; Rs as long (designated by Coquillett 1910). as R2 þ 3 þ 4 and 1.5 times longer than R3 þ 4; R5 three times longer than R5; d cell long and broad; M3 1.3 longer Subgenus Orimarga Osten Sacken, 1869 than d cell; cross-vein m-cu in proximal 1/3 of d cell; A1 straight; A2 rather short and straight. Remarks. Cockerell (1921) erroneously included this species Type species. As for genus. in the genus Limnophila. Remarks. One hundred and thirty-seven recent species are known from Neotropic (42 sp.), Oriental (41 sp.), Palaearctic (21 sp.), Australian (15 sp.), Afrotropic (14 sp.) and Nearctic Dicranomyia (Dicranomyia) brodiei (Cockerell, 1917a) n. comb. (four sp.) Regions. (Fig. 33, Pl. 3i)

Orimarga (Orimarga) lenae Krzemin´ski, n. sp. 1917a Riphidia brodiei Cockerell, pp. 373, 384, pl. 31, fig. 7 (Fig. 31, Pl. 3g) 1917b Rhipidia brodiei Cockerell, p. 141 1994 Rhipidia brodiei Evenhuis, p. 84 Holotype. In.25487 Hooley Collection; Insect Bed; late Holotype. NHMUK I.8603, Brodie Collection; Insect Bed; Eocene; NW Isle of Wight, UK. late Eocene; NW Isle of Wight, UK. Derivation of name. The new species is dedicated to Lena Additional material. In.17486 (part and counterpart), Smith Lukashevich (Russia, Moscow), specialist of fossil Diptera. Collection; In.25460, In.25477/In.26051 (part and counter- Diagnosis. Sc ending opposite fork of Rs into R2 þ 3 þ 4 part), Hooley Collection. and R5; cross-vein m-cu little before fork of Mb into M1 þ 2 Diagnosis. Sc short, ending opposite fork of Rb on R1 and and M3 þ 4. Rs; d cell short and broad; cross-vein m-cu in or little before Description. Sc rather short, ending opposite fork of Rs into fork of Mb on M1 þ 2andM3þ 4. R2 þ 3 þ 4 and R5; cross-vein sc-r three time its length before Redescription. Wing 6.1–7.0 mm, with big, dark stigma. end of Sc; R1 short, ending opposite cross-vein of m-r; cross- Venation. Sc short ending opposite fork of Rb into R1 and vein r-r (R2) at its length before end of R1; R3 þ 4 three times Rs; cross-vein sc-r twice its length before end of Sc; R1 rather longer than R2 þ 3 þ 4 and little more than twice Rs; d cell long; R3 þ 4 2.3 times longer than Rs and 2.5 times longer open by atrophy of cross-vein m-m between M1 þ 2andM3; than R2 þ 3 þ 4; R5 2.5 times longer than Rs; d cell short cross-vein m-cu somewhat before fork of Mb into M1 þ 2and and broad; M3 as long as d cell; cross-vein m-cu in fork of M3 þ 4; A2 short and rather straight. Mb into M1 þ 2andM3þ 4, but in some specimens this cross Remarks. Orimarga(Orimarga) lenae is the first fossil repre- vein is positioned little before this fork; A1 straight or little sentative of the genus Orimarga. wavy; A2 little wavy. Remarks. Cockerell (1917a, b) erroneously included this Genus Dicranomyia Stephens, 1829 species in the genus Rhipidia. More detailed study of the holo- type and additional materials has shown that species described Type species. Limnobia modesta Meigen, 1818, p. 134 as Rhipidia brodei belongs to the genus Dicranomyia. (designated by Coquillett 1910). Dicranomyia (Dicranomyia) excavata Cockerell & Haines, 1921 Subgenus Dicranomyia Stephens, 1829 (Fig. 34, Pl. 3j)

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 20 WIESŁAW KRZEMIN´ SKI ET AL. 1921 Dicranomyia excavata Cockerell & Haines, pp. 110–11, genitalia show distinct differences between this species and all fig. I9946 other fossil species of the genus Dicranomyia. 1921 Dicranomyia excavata Cockerell, p. 458, fig. 7 (junior homonym of Dicranomyia excavata Cockerell & Haines Genus Limonia Meigen, 1803 1921) 1922 Dicranomyia excavata Cockerell, p. 17 Type species. Limonia tripunctata Fabricius, 1781, p. 405 1922 Dicranomyia exhumata Cockerell, p. 17 (new replacement (autom.). name for Dicranomyia excavata Cockerell 1921), syn. Remarks. Two hundred and twenty eight species are known nov. from Palaearctic (72 sp.), Oriental (88 sp.), Australian (39 sp.), 1994 Dicranomyia excavata Evenhuis, p. 67 Afrotropic (16 sp.) and Nearctic (13 sp.) Region. Evenhuis 1994 Dicranomyia exhumata Evenhuis, p. 67 (1994) included 17 fossil species in his catalogue, but many of them need to be revised, some may belong to Dicranomyia. Holotype. NHMUK I.9946 (male), Brodie Collection; Insect Bed; late Eocene; NW Isle of Wight, UK. Additional material. NHMUK I.8884 (described as the Limonia spilota (Cockerell, 1921) holotype of Dicranomyia exhumata Cockerell, 1922), I.9766, (Fig. 36, Pl. 4b) I.8862, Brodie Collection; In.64096/In.64108 (part and counter- part), Hooley Collection. 1921 Limnobia spilota Cockerell, pp. 459–60, fig. 10 Diagnosis. Sc ending little behind fork of Rb on R1 and Rs; 1994 Limonia spilota Evenhuis, p. 77 d cell short and broad; cross-vein m-cu behind fork of Mb into M1 þ 2andM3þ 4. Holotype. NHMUK In.17114/In.20538 (part and counter- Redescription. Wing length 6.0–6.5 mm, with big dark part), Smith Collection; Insect Bed; late Eocene; NW Isle of stigma. Holotype with wing partially destroyed in middle part Wight, UK. but most parts of the thorax and abdomen preserved. Additional material. In.25498, Hooley Collection. Venation. Sc ending little behind fork of Rb into R1 and Rs; Diagnosis. Sc ending opposite 1/3 of Rs; d cell short and cross-vein sc-r at its length before end of Sc; R1 long; R3 þ 4 broad; M3 1.5 times longer than d cell; cross-vein in fork of 1.3 times longer than Rs and 2.3 times longer than Mb into M1 þ 2andM3þ 4. R2 þ 3 þ 4; R5 2.3 times longer than Rs; d cell short and Redescription. Wing length 8.0 mm, without colour pattern. broad; M3 little shorter than d cell; A1 straight; A2 rather Two wings, parts of head, thorax and abdomen are preserved; short and little wavy. antennae, palps and hypopygium are missing. Remarks. Cockerell & Haines (1921) described Dicranomyia Venation. Sc short, ending opposite 1/3 of Rs; cross-vein excavata and in this same year Cockerell (June 1921) described sc-r twice its length before end of Sc; R1 long; cross-vein r-r another species under the same name. When he realised his mis- (R2) at its length before end of R1; R3 þ 4 about twice longer take, he changed the name of the latter species to Dicranomyia than R2 þ 3 þ 4; R5 about 1.3 times longer than Rs; d cell exhumata (Cockerell 1922). Present detailed study has shown short and broad; M3 1.5 times longer than d cell; cross-vein that differences between both species are small and can be m-cu in fork of Mb into M1 þ 2andM3þ 4; A2 straight. ascribed to intraspecific variability. Thus D. exhumata becomes Remarks. Recently genus Limonia is represented in most a junior synonym. regions of the Earth, except the Neotropical Region. In the fossil state the oldest species was described from Baltic amber Dicranomyia (Dicranomyia) fasciata Krzemin´ski, n. sp. (late Eocene). Some species of Dicranomyia are sometimes (Fig. 35, Pl. 4a) included in Limonia.

Holotype. NHMUK I.9058, Brodie Collection; Insect Bed; Genus Helius Lepeletier & Seville, 1828 late Eocene; NW Isle of Wright, UK. Diagnosis. Sc long, ending opposite 3/4 of Rs; R3 þ 4 very Type species. Limnobia longirostris Meigen, 1818, p. 146 long and strongly curved. (autom.). Description. Wing length 8.0 mm, with big, dark stigma. Wing in medial, cubital and annal part destroyed; most parts of the body are preserved. Subgenus Helius Lepeletier & Seville, 1828 Head. antenna with big tubular scapus and small flat pedicel; flagellomeres short and rounded, with short bristles, not longer Type species. As for genus. than flagellomere. Remarks. One hundred and eighty recent species are known Thorax partially preserved, with only one strongly destroyed from Oriental (70 sp.), Neotropic (51 sp.), Afrotropic (23 sp.), wing. Palaearctic (20 sp.), Australian (14 sp.) and Nearctic (two sp.) Venation. Sc long, ending opposite 3/4 of Rs; cross-vein sc-r Regions. Seven fossil species are described from Upper Creta- at its length before end of Sc; R3 þ 4 very long and strongly ceous through Oligocene. curved, 2.3 times longer than Rs and about twice longer than R2 þ 3 þ 4; R5 very long, strongly curved, and more than Helius (Helius) edmundi Krzemin´ski, n. sp. twice longer than Rs. Remaining veins in most parts are de- (Fig. 37, Pl. 4c) stroyed. Abdomen. Male genitalia with outer dististyle large, balloon Holotype. NHMUK I.9810, Brodie Collection; Insect Bed; like; inner dististyle invisible; penis short and broad basally. late Eocene; NW Isle of Wight, UK. Remarks. Despite poor state of wing preservation, the Derivation of name. A new species is dedicate to Edmund venation retained (especially shape of radial veins) and male Jarzembowski (UK) specialist of fossil insects.

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Plate 4 Limoniidae, Scatopsidae and Anisopodidae. (a) Dicranomyia (Dicranomyia) fasciata Krzemin´ski, n. sp., holotype NHMUK I.9058. (b) Limonia spilota (Cockerell, 1921), holotype NHMUK In.17114. (c) Helius (Helius) edmundi Krzemin´ski, n. sp., holotype NHMUK I.9810. (d) Helius (Helius) popovi Krzemin´ski, n. sp., holotype NHMUK I.9392. (e) Dicranoptycha staryi Krzemin´ski, n. sp., holotype NHMUK In.24787. (f) Helius (Helius) vectensis (Cockerell, 1915) n. comb., holotype USNM 61439. (g) Trentepohlia (Mongoma) pallescens (Cockerell, 1921), NHMUK I.8898. (h) Trentepohlia (Mongoma) cruciferella (Cockerell, 1917a), holotype NHMUK I.8635. (i) Regmoclemina haennii Krzemin´ski, n. sp., holotype NHMUK In.9512. (j) Sylvicola hooleyi (Cockerell, 1921), holotype NHMUK In.24346. (k) Sylvicola problematica Krzemin´ski, n. sp., holotype NHMUK In.25675.

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Figures 37–42 Limoniidae, wing venation. (37) Helius (Helius) edmundi Krzemin´ski, n. sp., holotype NHMUK I.9810. (38) Helius (Helius) popovi Krzemin´ski, n. sp., holotype NHMUK I.9392. (39) Helius (Helius) vectensis (Cockerell, 1915), holotype USNM 61439. (40) Dicranoptycha staryi Krzemin´ski, n. sp., holotype NHMUK In.24787. (41) Trentepohlia (Mongoma) cruciferella (Cockerell, 1917a), holotype NHMUK I.8635. (42) Trentepohlia (Mongoma) pallescens (Cockerell, 1921), holotype NHMUK I.8898.

Diagnosis. Sc ending opposite fork of Rs into R2 þ 3 þ 4 M3 1.3 times longer than d cell; A1 and A2 little wavy in and R5; R5 twice longer than Rs, in mid part strongly wavy distal part. and d cell widened in proximal broaden in 1/3. Remarks. H. popovi differs from two other Helius species Description. Wing length 5.0 mm, with small black stigma. from the Isle of Wight by the regular rectangular shape of d Most parts of thorax, abdomen and two wings are preserved; cell. head is destroyed. Venation. Sc rather long, ending opposite fork of Sc into Helius (Helius) vectensis (Cockerell, 1915) n. comb. R2 þ 3 þ 4 and R5; cross-vein four times its length before (Fig. 39, Pl. 4f ) end of Sc; R1 long; R2 þ 3 þ 41.25timesofRs;R5twice longer than Rs, strongly wavy in mid part; d cell roughly 1915 Atarba vectensis Cockerell, pp. 492–93, 499, pl. 61, rhomboid, with rounded upper margin and widened in 1/3 fig. 10 length; M1 þ 2 strongly wavy; M3 1.25 times longer than d 1994 Atarba vectensis Evenhuis, p. 64 cell; A1 little wavy in distal part; A2 only slightly curved to anal margin of the wing. Holotype. USNM 61439 (Lacoe Collection 7513); Insect Remarks. Strong and wavy veins R5 and M1 þ 2 separate Bed; late Eocene; NW Isle of Wight, UK. this single species from all other representatives of Helius. Additional material. NHMUK I.10169 (female), Brodie Collection; In.25252/In.25512 (female, part and counterpart), Helius (Helius) popovi Krzemin´ski, n. sp. In.25464/In.25383 (part and counterpart), In.64097, Hooley (Fig. 38, Pl. 4d) Collection. Diagnosis. Sc ending opposite 2/3 of Rs; R5 2,5 times longer Holotype. NHMUK I.9392, Brodie Collection; Insect Bed; than Rs; d cell broaden in 1/3 of its length. late Eocene; NW Isle of Wight, UK. Redescription. Wing length 4.8–7.8 mm, with small, dark Derivation of name. The new species is dedicated to the late stigma. Some specimens preserved with body. Yuri Popov (Russia), specialist of fossil Heteroptera. Head with long rostrum, about twice longer than head; of Diagnosis. Sc ending opposite fork of Rs into R2 þ 3 þ 4 the antenna only scapus, pedicel and three flagellomeres are and R5; R5 twice longer than Rs; d cell rectangular. preserved. Scapus long and tubular; pedicle half as long as Description. Wing length 6.0 mm, with dark stigma. Only scapus and more broad; flagellomeres short and oval. small parts of thorax and abdomen are preserved. Venation. Sc ending opposite 2/3 of Rs; cross-vein sc-r twice Venation. Sc rather long, ending opposite fork of Rs into its length before end of Sc; R1 long; R2 þ 3 þ 4 1.5 times R2 þ 3 þ 4andR5;R1long;R2þ 3 þ 4 1.3 times longer longer than Rs; R5 2,5 times longer than Rs; d cell rhom- than Rs; R5 twice longer than Rs; d cell rectangular, broad; boid, widened in 1/3 length; M3 1.3 times longer than d cell;

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 23 cross-vein m-cu just behind fork of Mb into M1 þ 2and Head rather small, preserved without antennas and palps. M3 þ 4; terminal section of A1 wavy; A2 rather straight. Thorax in good condition, but without legs and only one Abdomen. Some specimens preserved with . wing is visible. Remarks. Helius vectensis is the most common species of Venation. Sc rather short, ending opposite 1/3 of the genus. Cockerell (1915) used old genus name Atarba,a R2 þ 3 þ 4 þ 5onR2þ 3 þ 4andR5;R1rathershort;r-r synonym of Helius. Recently the genus is rich in species and (R2) long, twice longer than last section of R1 and escaping distributed in all regions on the Earth. in fork of R2 þ 3 þ 4 þ 5; Rs 1.25 times longer than R2 þ 3 þ 4 þ 5, a little more than twice R3 þ 4 and a little Genus Dicranoptycha Osten Sacken, 1860 shorter than R5; d cell long and narrow, and about 1.3 longer than M3; cross-vein m-cu in fork of Mb into M1 þ 2and Type species. Dicranoptycha germana Osten Sacken, 1860, M3 þ 4 and strongly curved basally; Cu strongly curved in p. 217 (designated by Coquillett 1910). last section, connected with tip A1; A2 very short and wavy. Remarks. Eighty-nine recent species are known from Afro- Abdomen of specimen In.17264/I.9200 with well preserved trocic (31 sp.), Palaearctic (22 sp.), Nearctic (22 sp.), Oriental ovipositor. (six sp.) and Neotropic (three sp.) Regions. Five fossil species Trentepohlia (Mongoma) pallescens (Cockerell, 1921) are known from Upper Cretaceous through Miocene. (Fig. 42, Pl. 4g) Dicranoptycha staryi Krzemin´ski, n. sp. 1921 Mongoma pallescens Cockerell, p. 460, fig. 11 (Fig. 40, Pl. 4e) 1994 Trentepohlia (Mongoma) pallescens Evenhuis, p. 87 Holotype. NHMUK I.8898, Brodie Collection; Insect Bed; Holotype. NHMUK In.24787, Hooley Collection; Insect late Eocene; NW Isle of Wight, UK. Bed; late Eocene; NW Isle of Wight, UK. Additional material. In.17117/I.9051 (part and counterpart) Derivation of name. A new species is dedicated to Jaroslav Smith/Brodie Collections; In.17123, Smith Collection; Stary (Czech Republic), specialist of recent Limoniidae In.25431, In.25439, In.64113, Hooley Collection. (Diptera). Diagnosis. Cross-vein r-r (R2) about three times longer than Diagnosis. R5 2.3 length of Rs; cross-vein m-cu in fork of last section of R1 escaping in R2 þ 3 þ 4 þ 5, before fork of Mb into M1 þ 2andM3þ 4. this vein; d cell short and narrow, about half of M3. Description. Wing length 7.0 mm. Redescription. Sc rather short, ending opposite 1/4 of Venation. Sc ending opposite 1/4 of R2 þ 3 þ 4; cross-vein R2 þ 3 þ 4 þ 5; cross-vein sc-r at its length before end of sc-r at its length before end of Sc; R1 long; cross-vein r-r (R2) Sc; R1 rather short; cross-vein r-r (R2) about three times long, twice longer than last section of Sc; R3 þ 41.25times longer than last section of R1 and escaping directly in longer than R2 þ 3 þ 4 and only a little shorter than Rs; R5 R2 þ 3 þ 4 þ 5; Rs as long as R2 þ 3 þ 4 þ 5andR3þ 4 þ 5 2.5 times longer than Rs; d cell big and broad with rounded together, three times longer than R3 þ 4 and about half as upper margin; M3 as long as d cell; cross-vein m-cu in fork of long as R5; d cell short and narrow, about half as long as Mb into M1 þ 2andM3þ 4; A1 a little curved. M3; cross-vein in fork of Mb into M1 þ 2andM3þ 4, strong curved basally; Cu strongly curved in distal section, connected Genus Trentepohlia Bigot, 1854 with tip of A1; A2 very short and wavy. Remarks. These two species of the subgenus Mongoma Type species. Limnobia limnobioides Bigot, 1854, p. 456 are common at the site and indicate tropical or subtropical (original designation). climate. All recent representatives live in warm climate zones.

Subgenus Mongoma Westwood, 1881 Superfamily Psychodoidea Newman, 1834 by Dany Azar Type species. Mongoma fragillima Westwood, 1881, p. 364 (by monotypy). Family Psychodidae Newman, 1834 Remarks. One hundred and forty-one recent species are known from tropical and subtropical regions. Two fossil species Psychodidae are a cosmopolitan family habitually associated are known. with moist or sylvan habits. Most are nocturnal and can be found resting in shaded places in the daylight hours. Trentepohlia (Mongoma) cruciferella (Cockerell, 1917a) Fossil Psychodidae fossilised in the amber are sufficiently (Fig. 41, Pl. 4h) well preserved in pristine detail for accurate comparisons with the extant representatives of the family. Unfortunately, the study of insects’ fossil impressions in marl or limestone is 1917a Mongoma cruciferella Cockerell, p. 460, fig. 11 mainly based on the wing venation. 1994 Trentepohlia (Mongoma) cruciferella Evenhuis, p. 87 Cockerell (1915, 1921) described very succinctly two psy- chodid flies (Psychoda primaeva Cockerell, 1915, and Psychoda Holotype. NHMUK I.8635, Brodie Collection; Insect Bed; leucospila Cockerell, 1921). late Eocene; NW Isle of Wight, UK. The recent revision of the Isle of Wight fossil insect material Additional material. In.17116, In.17130, In.17259, Smith kept in the NHMUK and the Maidstone Museum and Art Collection; In.17264/I.9200 (female, part and counterpart) Gallery (Maidstone) revealed a new species of fossil psychodid Smith/Brodie Collections; In.25505, In.64123, Hooley Collection. flies and led to improvement of our knowledge of P. primaeva Diagnosis. Cross-vein r-r (R2) twice longer than last section Cockerell, 1915, and P. leucospila Cockerell, 1921. of R1 and escaping in to fork of R2 þ 3 þ 4intoR3þ 4and Herein I redescribe P. leucospila Cockerell, 1921, and P. R5; d cell long and narrow, about 1.3 times longer than M3. primaeva Cockerell, 1915, as Wightipsychoda leucospila Redescription. Wing length 5.0–6.0 mm. Female In.17264/ (Cockerell 1921) n. comb.; Pericoma primaeva (Cockerell I.9200 preserved with body.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 24 WIESŁAW KRZEMIN´ SKI ET AL. 1915) n. comb. One more species is recorded but unnamed. A Genus Pericoma Haliday, 1856 key for fossil psychodid flies from the Isle of Wight is given. Below I follow the wing venational nomenclature of McAlpine Type species. Pericoma trifasciata (Meigen 1804) ¼ (1981) Trichoptera trifasciata Meigen, 1804, by subsequent designa- tion of Coquillett (1910). Subfamily Psychodinae Newman, 1834 Pericoma primaeva (Cockerell, 1915) n. comb. Genus Wightipsychoda Azar, n. gen (Figs 46–49, Pl. 5d–g)

Derivation of name. After the Isle of Wight and Psychoda. 1915 Psychoda primaeva Cockerell, pp. 493, 494, plate 62, Type species. Psychoda leucospila Cockerell, 1921. fig. 5 Diagnosis. Presence of incomplete eye bridge. Wings shape 1994 Psychoda leucospila Evenhuis, p. 194 and venation very similar to those of the genus Psychoda with pointed wings; radial fork beyond medial, but with the differ- Holotype. USNM 61441 (Fig. 46, Pl. 5g), Lacoe Collection; ence of R4 ending at tip instead of R5. Males with white oval Insect Bed; late Eocene; NW Isle of Wight, UK. prominent tuft of scales shortly beyond costal node and be- Additional material. NHMUK I.8987 (Fig. 48), I.9011/ tween C and Sc. CuA2 well developed, strongly curved I.9272 (part and counterpart), I.9011, I.9149 (Pl. 5e), I.9165 basally and reaching costal margin. (female?, Fig. 49), I.9177 (male, Pl. 5d), I.9290 (male, Pl. 5f ), I.9319, I.9388, I.9600, I.9746, I.10403, Brodie Collection; Wightipsychoda leucospila (Cockerell, 1921) n. comb. In.25341, In.25342, In.25344, In.25345 (male, Fig. 47), (Figs 43–45, Pl. 5a–c) In.25346, In.26057, Hooley Collection; In.64535, Jarzembowski Collection (Thorness Bay); In.25456, Hooley collection; 1921 Psychoda leucospila Cockerell, p. 466, fig. 25 I.10069, Brodie collection; In.25343, Hooley collection; 1994 Psychoda leucospila Evenhuis, p. 194 I.9254, Brodie collection; II.2719, Azar Collection (Thorness Bay, May 2005); MNEMG 2018.6.0517; 2018.6.1522; Holotype. NHMUK I.9463, Brodie Collection, male (Fig. 43, 2018.6.0545/2018.6.0549 (part and counterpart); 2018.6.0159; Pl. 5a); Insect Bed; late Eocene; NW Isle of Wight, UK. 2018.6.0411; 2018.6.0684 and 2018.6.0761. Additional material. NHMUK I.10010, male (Fig. 44, Pl. 5b), Diagnosis. Presence of incomplete eye bridge. Antenna with I.9384, male (Fig. 45, Pl. 5c), I.9265 (female), I.9974, Brodie barrel-shaped flagellomeres. Wings obtusely pointed; radial Collection; In.17204 (probably male), Smith Collection; fork level very slightly distal to radial one. R5 ending in wing In.25340, Hooley Collection. margin beyond the apex. Diagnosis. As for the genus. Description. Eyes presenting a well-developed but incom- Description. Eyes with a developed eye bridge. Eyes separated plete eye bridge. Eyes separated with a distance of 0.025 mm by a distance of 0.017 mm. Wing 2.2 mm long, 1.02 mm wide. (after specimens I.8987 and I.9319). Antenna with barrel- Chalky-white large oval prominent tuft of scales shortly beyond shaped flagellomeres. The first one nearly twice longer than costal node and between C and Sc. Subcostal vein Sc distally the other flagellomeres (after specimen I.9319). Wings ob- reaching the costal margin. R1 reaching the costal margin tusely pointed 2.3–3 mm long (the holotype is 2.8 mm long), 1.4 mm from wing base. Branching of R2 þ 3 0.65 mm distal 0.9–1.2 mm wide (the holotype is 1.08 mm wide). Subcostal of wing base. R2 and R3 separated 1.1 mm distally. R2 and vein Sc distally reaching the costal margin. R1 reaching the R3 reaching costal margin. R4 reaching wing apex. Fork of costal margin 1.5–1.62 mm from wing base. Branching of M into M1 þ 2 and M3 0.8 mm distal of wing base. M3 reach- R2 þ 3 0.5–0.56 mm distal of wing base. R2 and R3 separated ing wing margin at 1.45 mm from wing base. CuA1 reaching 0.95 to 1 mm distally. R2 and R3 reaching costal margin. wing margin 1.1 mm distal of wing base. CuA2 rather developed, Fork of M into M1 þ 2 and M3 0.94 mm distal of wing strongly curved basally. Thorax (after specimen I.10010) 0.65 mm base. M3 reaching wing margin at 1.65–1.68 mm from long, 0.5 mm high. Abdomen 1 mm long, and 0.45 mm wide. wing base. CuA1 reaching wing margin 1.42–1.45 mm distal Remarks. Wightipsychoda leucospila (Cockerell 1921), shares of the wing base. CuA2 reaching wing margin at 0.83–1 mm with the Psychoda species the general known features of the from wing base. Anal vein well developed reaching wing genus such as (1) the presence of eye bridge; (2) pointed wing; margin at 0.375–0.43 mm apically. Thorax 0.6–0.85 mm long, (3) radial fork beyond medial; and (4) males with prominent 0.55–0.75 mm wide. Abdomen 0.9–1.4 mm long, and 0.5 mm tuft of scales shortly beyond costal node and between C and wide. Sc. It differs from Psychoda with R4 ending at wing apex Remarks. Cockerell (1915, pp. 493–94) described Pericoma instead of R5. The latest character allows the attribution of primaeva (Cockerell 1915) n. comb. and attributed it to the this species to a new genus Wightipsychoda. Cockerell (1921, genus Psychoda Latreille, 1796 because the ‘rather pointed p. 466) stated that no species could be found among living wingtip and general appearance indicate the reference to forms of psychodid flies with the presence of ‘chalky-white Psychoda’. But for all the species attributed to Psychoda,R5 costal patch’. A minute examination of this ovoid patch indi- ends at wingtip, and the antennal flagelomeres are not barrel- cates that it is formed of prominent tuft of scales. This charac- shaped but rather nodiform, thus Pericoma primaeva cannot ter is known in males of several taxa belonging to Psychoda belong to the genus Psychoda. According to the keys to genera genus as could be seen in Duckhouse (1966, p. 194), like Psy- given by Quate & Vockeroth (1981), Pericoma primaeva choda pennicillata Satchell, 1950; Psychoda mundula Duckhouse, (Cockerell 1915) n. comb. falls into the genera Pericoma 1966; Psychoda cristata Duckhouse, 1966; Psychoda gracilipenis Haliday, 1856 for the following reasons: (1) eyes with eye Duckhouse, 1966; Psychoda disaccus Duckhouse, 1966; Psy- bridge; (2) flagellomeres barrel-shaped; (3) R5 ending beyond choda salicorna Quate, 1954, etc. In females this patch is present wing apex; (4) radial fork on the same level as medial fork or but smaller and without scales. Excluding the general features slightly distal to it. of the family, Wightipsychoda leucospila does not share The relatively abundance of the belonging to Peri- special similarities with any of the known Tertiary fossils coma primaeva allows a better understanding of this species; flies. it indicates that there is a large range of morphological poly- morphism (not due to sexual dimorphism) in wing sizes and

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Figures 43–50 Psychodidae. (43)–(45) Wightipsychoda leucospila (Cockerell, 1921) n. comb.: (43) holotype, NHMUK I.9463, male; (44) NHMUK I.10010; (45) NHMUK I.9384. (46)–(49) Pericoma primaeva (Cockerell, 1915) n. comb.: (46) holotype, USNM 61441; (47) NHMUK In.25345, male; (48) NHMUK I.8987; (49) NHMUK I.9165, female? (50) Psychodinae? NHMUK In.26069(2). Scale bars ¼ 1 mm.

measurements. At a first examination I decided to split this sented by the unique specimen NHMUK In.26069(2), Hooley species into two different ones on the basis of the difference in Collection (Fig. 50, Pl. 5h). This species is very small (wing not wing length based on a 30 % of difference in size: a group with more than 1.35 mm long) and quite different from all the large wings and another one with small wings. But the minute known fossil psychodid flies from the Isle of Wight. The radial study of all the specimens shows clearly a gradualism in size fork apically well beyond the medial. Unfortunately the badly from small (wings of 2.3 mm) to large individuals (wings of preserved state of the specimen does not allow any further 3 mm) with a clear dominance of specimens of middle size consideration beyond the subfamily level. (six specimens with wings of 2.6 mm). Unfortunately, except Key to the fossil Eocene moth fly species from the Isle of the wing venation measurements, no preserved features could Wight be utilised to verify if the observed difference is only due to polymorphism. Except the common features of the genus, (1) Wings smaller in length than 1.5 mm...... the herein Pericoma primaeva doesn’t share particular similarities with any unnamed species of the known Tertiary fossils moth flies, but is much larger. Wings greater than 1.5 mm...... 2 (2) Wing with R4 ending in wing apex, and radial fork distal Subfamily ?Psychodinae Newman, 1834 to medial fork...... Wightipsychoda leucospila R4 and R5 beyond wing apex, and level radial fork The examination of all the Isle of Wight psychodid material slightly distal to medial one...... Pericoma primaeva allows the finding of one more fossil moth fly species repre-

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Plate 5 Psychodidae and Dixidae. (a–c) Wightipsychoda leucospila (Cockerell, 1921) n. comb.: (a) holotype NHMUK I.9463, male; (b) NHMUK I.10010; (c) NHMUK I.9384. (d–g) Pericoma primaeva (Cockerell, 1915) n. comb.: (d) NHMUK I.9177, male; (e) NHMUK I.9149; (f ) NHMUK I.9290, male; (g) holotype, USNM 61441. (h) Unnamed new ?Psychodinae, NHMUK In.26069 (2). Scale bars ¼ 1 mm. (i–k) Dixella priscula (Cockerell, 1921) n. comb.: (i) NHMUK In 24345, holotype; (j) NHMUK In 17402, male; (k) NHMUK In 26055.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 27 Superfamily Latreille, 1817 transparent, without spots. Sc not reaching midwing, ending just before Rs origin. R fork about 1.5–2 times the length Family Dixidae Schiner, 1868 3+4 of its stem. Crossvein r-m just below Rs furcation, M forking by Elena Lukashevich just below r-m or slightly distal. M1+2 aligned with M stem. M1+2 fork somewhat shorter than its stem. Abdomen glabrous. Members of the extant cosmopolitan family Dixidae are Gonocoxite with elongate apical lobe, at least half as long delicate nematocerous flies, commonly called meniscus . as gonostylus. Approximate lengths (mm): partly preserved Larval Dixidae usually inhabit running water with shady water antenna 1.4; 3 distal palpomere 0.5; thorax 1.1; abdomen 2.3; edges and the non-feeding adults are found resting on vegetation wing 3.3–4.0. nearby. Worldwide, seven extant genera and about 175 species Remarks. Unfortunately, the extant genera are indistin- are recognised (Peters 1989). guishable by wing characters, so the isolated wing described The fossil representatives of the family have been recorded by Cockerell could in fact belong to any of them. However, from the Jurassic and Lower Cretaceous of Asia and Europe the well preserved male (In.17402) may be a member of (Lukashevich 1996; Lukashevich et al. 2001) and Cenozoic of Dixella based on indistinctly separated first antennal segments Europe and America (Evenhuis 1994). Mesozoic dixids (the basal flagellomere is probably elongated and cylindrical) (known from isolated wings only) have been assigned to and elongated apical lobe of gonocoxite. We suppose that the extinct genera, but Cenozoic ones (known from compression male is conspecific with D. priscula in spite of differences in fossils and amber inclusions) are placed in extant genera and size and several details of venation. Smaller size of this male belong to Dixa Meigen, 1818 or Dixella Dyar & Shannon, compared with the holotype (wing length 3.3 mm versus 1924 (like the majority of recent species). 4.0 mm) can be explained by sexual dimorphism (dixid females Seven species of Cenozoic Dixidae have been described, and are usually larger). Position of the base of M fork in poorly one specimen from Dominican amber (Oligocene/Miocene) preserved holotype, mentioned as m-cu proximal to r-m by was mentioned (Poinar 1992). Four species are known from Cockerell and considered to be a diagnostic feature by him, is Baltic amber (Eocene/Oligocene). Three of them are represen- very obscure and seems to be just below r-m. In the male and tatives of Dixella: D. succinea (Meunier 1906), D. distans two additional wings M is forked slightly distally of r-m, but (Hennig 1966) and D. filiforceps (Hennig 1966). The members similar variation of venation is known in the recent species of of Dixa are known from inclusions – D. minuta Meunier, 1906 Dixidae (sometimes the left wing is different from right one, (Baltic amber) and from impressions – D. tertiaria (Meunier e.g., in D. autumnalis Meigen, 1838 – Disney, 1975, pl. 2 M, N). 1915) ( ¼ D. hyalipennis Theobald 1937) (Aix en Provence, The wing colour pattern of the Cockerell holotype remains France; Oligocene), D. priscula Cockerell, 1921 (Bembridge unclear due to poor preservation, but in the male In.17402 and Marls Insect Bed of the Isle of Wight, England, late Eocene) wing In.26055 spots on the wing are clearly absent. and D. cimbrica Ansorge, 1992 (Fur-Formation (Moler) of Among described fossils of Dixidae only Dixa minuta is Jylland, Denmark; Upper Paleocene/Lower Eocene). See undoubtedly not a member of Dixella (Hennig 1966); Dixa below for discussion about generic position of these species. tertiaria (¼D. hyalipennis) probably also belongs to Dixa The holotype of D. priscula was described by T. D. A. sensu stricto because of first flagellomere slightly fusiform and Cockerell from the R. W. Hooley Collection In.24345 (old clearly separated (Theobald 1937, pl. XXIII, fig. 15a), so we number H 708). Later, three other specimens of Dixidae were cannot compare these species with D. priscula.However, discovered there: In.25478 (H 535), In.25470 (H 567) and Dixa cimbrica is known from an isolated wing so, in fact, In.26055 (H 1518). However, meniscus midges are also known can belong to any of extant genera, including Dixella. Dixa in other collections from Gurnard Bay, P. B. Brodie collection cimbrica and Dixella priscula are similar in size (wing length (I.8896) and E. J. A’Court Smith collection (In.17402); so one about 4 mm), with wing membrane without spots; the only can conclude that Dixidae in Bembridge Marls are rare, but difference of the latter compared with the former, the position regularly found. of r-m beyond Rs furcation, cannot be a diagnostic character Genus Dixella Dyar & Shannon, 1924 of the species taking into account the variability of venation in the recent species (Disney 1975). Type species. Dixella lirio Dyar & Shannon, 1924, by Among amber species described or redescribed by Hennig, monotypy. D. priscula resembles Dixella filiforceps and Dixella distans in the structure of genitalia (Hennig 1966, Abb. 12, 13; more Dixella priscula (Cockerell, 1921) n. comb. detailed comparison with inclusions is impossible due to (Figs 51–54, Pl. 5i–k) different type of preservation of the male from Bembridge). 1921 Dixa priscula Cockerell, p. 466, fig. 26 However, at least in D. distans the scutum and abdomen are 1923 Dixa priscula Cockerell; Edwards, p. 142 covered with short macrotrichia (pers. obs.), instead of 1929 Dixa priscula Cockerell; Martini, p. 16 glabrous in D. priscula (in Bembridge fossils pubescence is 1932 Dixa priscula Cockerell; Edwards, p. 6 usually preserved). So at the present stage of knowledge it is 1992 Dixa priscula Cockerell; Ansorge, p. 516 impossible to decide if Dixella priscula is not conspecific with 1994 Dixa priscula Cockerell; Evenhuis, p. 222 D. filiforceps and D. cimbrica.

Holotype. NHMUK In.24345 (Fig. 54, Pl. 5i), Hooley Family Dixidae? Schiner, 1868 Collection; poorly preserved wing; Insect Bed; late Eocene; Specimens NHMUK In.25478 (well preserved impression of NW Isle of Wight, UK. isolated wing 2.6 mm long – Fig. 51) and I.8896 (partly pre- Material. NHMUK In.17402 (well preserved male without served body and wing) are not conspecific with D. priscula legs, Fig. 52, Pl. 5j), In.25470 (partly preserved wing), In.26055 due to much smaller size and can be identified only as Dixidae (well preserved wing without anal lobe, Fig. 53, Pl. 5k), Hooley inc. sedis. Collection. Description. First antennal segments indistinctly separated Family Culicidae Meigen, 1818 (probably the basal flagellomere elongate, cylindrical and no segments of flagellum fusiform). Scutum glabrous. Wing by Ryszard Szadziewski

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1915 Culex protolepis Cockerell, p. 488, pl. 62, fig. 1 (Gurnet Bay, wing, sex not indicated) 1915 Culex petrifactellus Cockerell, 489, pl. 61, fig. 12 (Gurnet Bay, wing; sex not indicated) 1923 protolepis (Cockerell); Edwards, p. 142, figs 1, 2; pl. 7: figs 2–4 (Gurnet Bay, combination, syn. C. petri- factellus, male, female) 1944b Aedes protolepis (Cockerell); Statz: 114 (comments) 1994 Aedes protolepis (Cockerell); Evenhuis, p. 232 (in catalogue) 1998 Aedes protolepis (Cockerell); Szadziewski, p. 234 (comments)

Holotype. USNM. 61429, Lacoe Collection; Insect Bed; late Eocene; NW Isle of Wight, UK. Description (from Edwards 1923). Wing length 3.2–4.0 mm. Wing scales slender; subcostal vein short, ending at level of base of vein R2 þ 3; vein R2 þ 3 relatively long, only 1.4 times shorter then R2 (10:7). Male palpi are longer than proboscis with fourth and fifth segments of almost equal length. Male genitalia barely preserved; gonostyli rather long, slender, curved, with single apical tooth. Discussion. Cockerell (1915) briefly described Culex protolepis and Culex petrifactellus from single incomplete wings housed in the Smithsonian Institution, Washington. Sex was not indicated. Edwards (1923) suggested that C. protolepis is a female Figures 51–54 Dixidae. (51) Dixidae incertae sedis NHMUK In.25478, wing. (52)–(54) Dixella priscula (Cockerell, 1921) n. comb.: while C. petrifactellus a male of the same species. In the collec- (52) NHMUK In.17402, male; (53) NHMUK In.26055, wing; (54) tion of the NHM he determined a further 24 males and 14 NHMUK In.24345, holotype, wing. Scale bar ¼ 1 mm. females and completed a description of the species which was assigned to the genus Aedes. Edwards (l.c.) suggested that another 40 incomplete specimens probably belong to the The Culicidae is a well known family of nematocerous flies. same species. In the extant world fauna over 3200 species are known. They Reinert (2000) proposed to divide the composite genus are frequent parasites of and as females feed Aedes Meigen into two genera Aedes and Ochlerotatus and on their blood. larvae and pupae inhabit exclusively this proposition is widely accepted. The great majority of the shallow stagnant waters. extant Holarctic species belongs to the genus Ochlerotatus. Despite of the fact that the phylogenetic history of mosqui- The oldest fossil species in the genus is Ochlerotatus serafini toes goes back to the Mesozoic era, they are rarely preserved (Szadziewski 1998) from Eocene Baltic amber (Szadziewski & as fossils. The oldest true mosquitoes are reported from the Giłka 2011). Upper Cretaceous in Canadian amber (Poinar et al. 2000) In Ochlerotatus the gonostyli are long, narrow, somewhat and (Borkent & Grimaldi 2004). curved, with a single gonostylar tooth while in Aedes the Fossil mosquitoes from the Tertiary are reviewed by Edwards gonostyli have the distal portion expanded, bifurcated and (1923), Statz (1944a), Evenhuis (1994) and Szadziewski (1998). usually with more than one apical claw. Drawings of male Some named fossils are barely preserved and the visible genitalia of Aedes protolepis determined by Edwards (1923, characters show nothing more than that they are mosquitoes. fig. 1c–e) show that gonostyli are rather long, slender, curved, Mosquitoes are very rare in Eocene Baltic amber (Szadziewski with single apical tooth as in the genus Ochlerotatus. This 1998; Podenas 1999), while they are more common in younger indicates that the species should be placed in this genus. Miocene Dominican amber (Szadziewski & Grogan 1994; Poinar 2005), Miocene deposits of Rott (Statz 1944a) or the Genus Coquillettidia Dyar, 1905 Oligocene Insect Bed of the Isle of Wight described here. Dipterans of the family Culicidae are common fossils Type species. Culex perturbans Walker, 1856. among insects from the Bembridge Marls (Cockerell 1915; Edwards 1923). Over 140 specimens of adult mosquitoes and Coquillettidia cockerelli (Edwards, 1923) n. comb. one have been found in the collection of the NHM (Figs 57, 58) (Edwards 1923; A. Ross, pers. comm.). This paper presents results of an examination of the collection of mosquitoes housed at the NHM, London. 1923 Taeniorhynchus (?) cockerelli Edwards, p. 151, fig. 4b (Gurnet Bay, female, fig. wing) Subfamily Latreille, 1817 1944b Mansonia cockerelli Edwards; Statz, p. 114 (combina- tion) Genus Ochlerotatus Lynch Arriba´lzaga, 1891 1994 Ochlerotatus cockerelli Edwards; Evenhuis, p. 234 (combination, in catalogue) Type species. Ochlerotatus confirmatus Lynch Arriba´lzaga, 1998 Mansonia cockerelli Edwards; Szadziewski, pp. 234, 1891 (¼Aedes scapularis Rondani, 1848). 243 (comments, in key)

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Edwards (1923) provisionally placed this fossil in 1998 Culex vectensis Edwards; Szadziewski, 1998, p. 244 (in the Ochlerotatus Lynch Arriba´lzaga, 1891 (¼Taeniorhynchus key) Lynch Arriba´lzaga 1891) treating as a subgenus of Aedes and now is as a distinct genus. This fossil mosquito with broad Holotype. NHMUK I.9324, (female) Brodie Collection; wing scales was included in genus Mansonia Blanchard, 1901 Insect Bed; late Eocene; NW Isle of Wight, UK. by Statz (1944b) and Szadziewski (1998). Recently the sub- Description. Female. Body length about 2.9 mm. Proboscis genus Coquillettidia was removed from the genus Mansonia and antennae incomplete (Fig. 55). Second segment of palpus and elevated to a distinct genus (Dahl 1997). Mansonia is 1.6 times longer than the first [probably 1 þ 2]. Distal part of absent in the extant fauna of Europe while Coquillettidia is wing preserved 1.66 mm long. Subcostal vein long, reaching represented by one species, C. richiardii (Ficalbi 1889). Larvae almost level of base of vein R2. Vein R2 2.8 times longer and pupae of species from both genera pierce water and than vein R2 þ 3. Wing scales slender (Fig. 56). Tip of abdomen take air from tissues. They are able to inhabit lakes and missing. Male unknown. ponds with fish, hiding against predators among plants in the Discussion. Mosquitoes are common fossils in the Bembridge littoral zone. Two other species described by Statz (1944b) in Marls. However, they are barely preserved and their determina- the genus Mansonia from the early Miocene deposits of Rott tions should be treated with a certain caution. These materials in Germany. Their generic position was determined by an are not comparable with extant forms or with fossils from expert in that family, Prof. E. Martini of Hamburg. In the . Among over 140 preserved mosquitoes, four species present paper these species are also included in the genus are determined in three extant genera Coquillettidia, Ochlerotatus Coquillettidia as new combinations: C. martinii (Statz 1944b), and Culex of worldwide distribution. These genera are common n. comb. and C. varivestita (Statz 1944b), n. comb. The oldest inhabitants of shallow reservoirs of stagnant water in present-day report of the genus is from Eocene Baltic amber (Szadziewski Europe. Larvae and pupae of Coquillettidia live among water & Giłka 2011). plants, pierce them by siphon or thoracic trumpet and take air from plant tissues. In this way they are able to inhabit the littoral Genus Culex Linnaeus, 1758 of lakes and ponds with fish. Key to Mosquitoes from Bembridge Marls Type species. Culex pipiens Linnaeus, 1758. (1) Wing veins with broad scales...... Coquillettidia cockerelli Culex protorhinus Cockerell, 1915 (Edwards 1923) Wing veins with slender scales...... 2 (2) Subcostal vein long, reaching level of vein R2 base...... 1915 Culex protorhinus Cockerell, p. 488, pl. 62, fig. 2 (Gurnet Culex vectensis Edwards 1923 (female) Bay, male, no wings, head, thorax and abdomen in Subcostal vein short, ending at level of vein R2 þ 3 lateral view, apex absent) base...... 3 1923 Culex protorhinus Cockerell; Edwards, p. 148, fig. 3 (3) Female cerci slender, apex of abdomen pointed. Wing (male, female) length 3.2–4.0 mm...... Ochlerotatus protolepis 1944b Culex protorhinus Cockerell; Statz, p. 114 (comments) (Cockerell 1915) 1994 Culex protorhinus Cockerell; Evenhuis, p. 233 (in Female cerci not visible. Wing length 4.3–5.2 mm...... catalogue) Culex protorhinus Cockerell 1915 1998 Culex protorhinus Cockerell; Szadziewski, p. 243 (in key) Superfamily Newman, 1834 Family Chironomidae Newman, 1834 Holotype. USNM 61430, Lacoe Collection; Insect Bed; late Eocene; NW Isle of Wight, UK. by Ryszard Szadziewski Additional material. NHMUK I.8998(2), (male), Brodie Dipterans of the family Chironomidae are rare and barely Collection. preserved fossils among insects from Bembridge Marls and Description. Female and male. Body length about 6 mm. were not examined previously. Wing length 4.3–5.2 mm; scales slender; subcostal vein short, Chironomidae (Diptera) form a large family of nemato- reaching level of base of R2 þ 3; vein R2 þ 3about1.7times cerous flies common in all types of freshwater habitats. Some shorter than R2 in male, and 1.8 times in female. Length of species of the subfamily are semiaquatic and male proboscis 3.7 mm, palpi 3.3 mm. Palpi probably shorter live in moist close to permanent water bodies and a than proboscis (Edwards 1923). few are truly terrestrial. The family includes over 5000 extant Discussion. Cockerell (1915) described the species from the species (Giłka, pers. comm.) and over 170 fossil species collection of the Smithsonian Institution, Washington, from a (Evenhuis 1994). Chironomids are common in the fossil record, barely preserved male devoid of wings and genitalia. Sub- and sometimes well preserved. sequently, Edwards (1923) determined 14 further specimens in This paper presents results of an examination of a small the collection of the NHM, London, and redescribed both collection of 35 adult chironomids housed at the NHMUK. sexes. The species is similar to O. protolepis in having the Better preserved specimens are determined to the subfamilies same wing venation (see key). (four specimens), Orthocladiinae (one) and

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Figures 55–58 Culicidae. (55), (56) Culex vectensis Edwards, 1923, holotype female, NHMUK I.9324: (55) habitus; (56) wing. (57), (58) Coquillettidia cockerelli (Edwards, 1923), holotype female, part and counterpart: (57) NHMUK I.10106; (58) NHMUK I.17190.

Chironominae (14). The other 16 barely preserved specimens length 3.4 mm; I.10060, one female, lateral view, no wings, remain undetermined. body 2.2 mm long; I.10217, one female, lateral position, thorax and abdomen 4.0 mm, all Brodie Collection; In.17470, Family Chironomidae Newman, 1834 one female, barely visible, dorsal position, Smith Collection; (Figs 59–64) In.25394, one male, lateral position, wings not preserved; In.25759, one male, barely preserved, body length 5.0 mm, Hooley Collection; all from the Insect Bed; late Eocene; NW Indeterminate material. NHMUK I.8475, one female, Isle of Wight, UK. lateral position; I.8530, one female, lateral position, no wings, length of preserved body 1.4 mm; I.8542, one female, lateral position, no wings; I.8991, one male, lateral position, no Subfamily Tanypodinae Frey, 1927 wings; I.9660, barely preserved remnants of three specimens; I.9782, one male, lateral position, no wings; I.9793, one Material. NHMUK I.9308, one female, wing 1.9 mm long; female, dorsal view, no wings; I.9880, one male, partly pre- I.9589, one female, lateral position, flagellum short, with served; I.9964, one male, lateral position, no wings, body numerous flagellomeres, body length 2.7 mm; I.9750, one

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Figures 59–64 Chironomidae. (59) Tanypodinae indet., female, NHMUK I.9921. (60) Orthocladiinae indet., male, NHMUK I.17390. (61) indet., male, NHMUK I.9665. (62) indet., male and female, NHMUK I.8912. (63) Chironomini indet., male, NHMUK I.9611. (64) Chironomini indet., male, NHMUK In.17388.

male, dorsal position, wings partly preserved, body 4.3 mm Material. NHMUK I.8912, one male, body 3.6 mm long, long; I.9921 (Fig. 59), one female, lateral position, flagellum one female, body 2.7 mm long, without wings (Fig. 62); composed of numerous flagellomeres, wings absent, all Brodie I.9611, one male, lateral position, wings not preserved, body Collection. length 4.0 mm (Fig. 63); I.9623, one female, lateral position, wings absent, body 4.2 mm long, Brodie Collection; In.17109, Subfamily Orthocladiinae Kiefer, 1911b one male, body 7.1 mm long, wings and genitalia not pre- served; In.17388, three males, two females, one male very large, abdomen plus thorax 9.4 mm long (Fig. 64), Smith Material. I.17390(1), one male, body length without flagellum Collection; In.26040, part and counterpart, one female, lateral 1.9 mm (Fig. 60), together with indet. (Ceratopogo- position, no wings, body 2.8 mm long, Hooley Collection. nidae), Smith Collection. Comments. Chironomids are rare fossils preserved in the Insect Bed of the Bembridge Marls. They are poorly preserved Subfamily Chironominae Newman, 1834 and have little taxonomic value. Among better preserved com- pression fossils from the early Miocene deposits of Rott in Material. NHMUK I.9665, one male with preserved genitalia, Germany the chironomids were represented by adults and body 4.5 mm long, in lateral position (Fig. 61); I.10071, two pupae assigned to the same subfamilies (Statz 1944b). females, lateral position, wing in one specimen visible, Brodie Collection. Family Ceratopogonidae Newman, 1834 Chironomini Newman, 1834 by Ryszard Szadziewski

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Figures 65–68 Ceratopogonidae. (65) Stilobezzia sp. indet., NHMUK I.9809. (66), (67) Palpomyia edwardsi Cockerell, 1921, NHMUK I.9757. (68) sp. indet., NHMUK I.9453.

Biting midges (Diptera: Ceratopogonidae) form a small n. comb. and genera Amberaspinus Evenhuis, 1994 and family of nematocerous flies which is relatively well known in Aspinus Hong, 1981 are recognised as new junior synonyms the recent fauna and has well studied fossil record from the of . However, two other species described by Lower Cretaceous to the Miocene. The family includes 5,471 Hong (1981) from females in the genus Aspinus (A. amblopteres extant species and 253 fossil species (Borkent & Wirth 1997; Hong, 1981 and A. stenopteres Hong, 1981) actually are Borkent, personal comm.). Fossil species from the Lower and members of the Chironomidae. I propose to leave these species Upper Cretaceous as well as from many Tertiary deposits in the original combination within the Chironomidae as species were described within 19 fossil and 25 extant genera. The best incertae sedis. known is the fossil fauna of biting midges in Eocene Baltic Dipterans of the family Ceratopogonidae are rare fossils amber (Szadziewski 1988). among insects from the Bembridge Marls. Until now only Hong (1981) described within the family Chironomidae a one biting Palpomyia edwardsi has been described new fossil genus Aspinus Hong, 1981, p. 52, with type-species from the collection of the NHM by Cockerell (1921). Aspinus orientalus Hong, 1981, p. 53 from Eocene Fushun Nine fossils of Ceratopogonidae from the NHMUK, were amber. Evenhuis (1994) discovered that the Aspinus was pre- examined. Nine of them were determined to genera, one barely occupied and replaced it with the name Amberaspinus Even- preserved specimen (NHMUK In.25394) remains undeter- huis, 1994, p. 260. The single known male of Amberaspinus mined. orientalus (Hong), based on the description and illustration by Hong (1981), is clearly a member of the genus Forcipomyia Tribe Newman, 1834 Meigen, 1818 of the family Ceratopogonidae. The overall habitus, presence of 13 flagellomeres (10–13 elongated), elon- Genus Stilobezzia Kieffer, 1911a gated proboscis with relatively short palpi and the shape of gonocoxites and gonostyli indicate this generic placement. Type species. Stilobezzia festiva Kieffer, 1911a. The wing venation and the shape of tergite IX in genitalia are probably incorrect in the drawings. The type species Stilobezzia sp. indet. of Aspinus is here therefore named Forcipomyia orientalus, (Figs 65, 69)

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 33 Discussion. Hong (1981) described and illustrated a female of Palpomyia unca from Eocene amber of Fushun. Subsequently Hong et al. (2000) proposed a new genus Eopalpomyitis for this species. Actually the female of the type species has all femora armed with ventral spines, enlarged fore femora, two first radial cells well developed, sessile median veins, tarsal claws moderately long, equal to subequal, with basal inner tooth and other characters typical of the genus Palpomyia (Szadziewski 1988; Grogan, pers. comm.). Other characters used by Hong et al. (2000) for diagnosing a new genus like 14-segmented flagellum, first flagellomere with sensillum coeloconicum, costal vein prolonged to M1, sensory pit on third palpal segment are most probably a result of misinterpretations of structures not clearly visible in amber. In the biting midges antenna in both sexes never includes more than 13 flagello- meres, and within the tribe the costal vein is never prolonged beyond R2 þ 3, sensilla coeloconica are absent on first flagellomere as well as the sensory pit is not developed Figures 69–70 Ceratopogonidae. (69) Stilobezzia sp. indet., on the third palpal segment. I suggest placing the generic NHMUK I.9809. (70) Palpomyia edwardsi Cockerell, 1921, NHMUK name Eopalpomyitis proposed by Hong et al. (2000) among I.9757. synonyms of the large, worldwide distributed extant genus Palpomyia.

Material. NHMUK I.9210, female, preserved one wing, part Palpomyia edwardsi Cockerell, 1921 of abdomen; I.9798, female, preserved one wing, abdomen in (Figs 66, 67, 70) dorsal view, scutum; I.9809, probably female, one wing 1921 Palpomyia edwardsi Cockerell, p. 469, fig. 31 (Gurnet and part of thorax preserved, Brodie Collection; In.17390(2), Bay, fig. wing, thorax) female?, wing incomplete, part of thorax preserved; In.17471, 1988 Palpomyia edwardsi Cockerell; Szadziewski, p. 240 female, one wing, thorax plus abdomen in lateral view pre- 1994 Palpomyia edwardsi Cockerell; Evenhuis, p. 251 served, Smith Collection; all from the Insect Bed; late Eocene; 1997 Palpomyia edwardsi Cockerell; Borket and Wirth, NW Isle of Wight, UK. p. 131 Description. Female. Wing length 2.40–2.51 mm, costal ratio CR 0.73–0.81. Venation typical of the genus Stilobezzia Holotype. NHMUK I.9757. One wing, thorax and partly Kieffe with median veins M1 and M2 petiolate and both first abdomen in lateral view preserved, Brodie Collection; Insect radial cells well developed (Figs 65, 69). Macrotrichia on wing Bed; late Eocene; NW Isle of Wight, UK. membrane not visible. Description. Female. Body length about 4.4 mm. Wing Male unknown. length 2.74 mm, CR 0.92. Second radial cell 2.47 times longer Discussion. Preserved wings of the fossils allow us to than first one. Median vein M2 forked proximal of cross-vein determine them as members of the extant genus Stilobezzia. r-m (Figs 66, 67, 70). Male unknown. However, they are poorly preserved females devoid of sub- Remarks. The generic position of this fossil determined generic and specific features which indicate the subgeneric solely by wing characters is not certain. Similar wing venation position or allow distinguishing them from other fossil species can be found also in some other genera of predatory biting known from Tertiary ambers and rocks. It seems that all midges within the tribes Sphaeromiini or Heteromyiini. How- specimens examined from the Bembridge Marls belong to one ever, legs which are necessary for final determination of the species. genus are not preserved. The relatively broad wing and stout Fossil Stilobezzia were reported from Paleocene amber of preserved part of abdomen suggest that it is a female. Sakhalin (Szadziewski 1990, one species indet.), Eocene Baltic Palpomyia is an extant genus of biting midges which amber (Szadziewski 1988, 1993, four sp.), Miocene Dominican evolved during Tertiary (Szadziewski 1996). It includes 11 fossil amber (Szadziewski & Grogan 1998a, two sp.), and Miocene species reported from Eocene Baltic amber (Szadziewski 1988, compression fossils from Rott (Statz 1944c; Szadziewski 1993, four sp.), Eocene Chinese amber (Hong 1981, one sp.), 1993, one sp.). Oligocene Bembridge Marls (one sp., see above), Miocene Stilobezzia is a worldwide distributed genus with 310 extant Dominican amber (Szadziewski & Grogan 1997, one sp.) and species (Borkent & Wirth 1997). Females are predators on Miocene nodules from California (Pierce 1966, four sp.). other small insects. Predatory larvae are good swimmers Palpomyia is a genus distributed worldwide that includes which live in small water bodies and semiaquatic habitats. 234 recent species (Borkent & Wirth 1997). Females are preda- tors on small insects. In most cases the prey consists of males Tribe Palpomyiini Enderlein, 1936 of Chironomidae, or small Ephemeroptera. Swimming larvae of Palpomyia are common inhabitants of different types of Genus Palpomyia Meigen, 1818 aquatic and semiaquatic habitats where they feed on other small animals. 1818 Palpomyia Meigen, p. 82. Type species fla- vipes Meigen, 1804 Subfamily Dasyheleinae Lenz, 1934 2000 Eopalpomyitis Hong, Guo & Ren, p. 226. Type species Genus Dasyhelea Kieffer, 1911c Palpomyia unca Hong, 1981, by original designation. Eopalpo- myitis: Hong, 2002, p. 165. Syn. nov. Type species. Dasyhelea halophila Kieffer, 1911c.

2002 Palpoimyitis Hong, p. 165. Nomen nudum Dasyhelea sp. indet. 2002 Palpomyitis Hong, p. 165. Nomen nudum (Fig. 68)

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 34 WIESŁAW KRZEMIN´ SKI ET AL. Material. NHMUK I.9453, female, wings absent, thorax Material: The single simuliid pupa was collected from late and abdomen in lateral view and flagellum preserved, doubt- Eocene deposits of the Isle of Wight, southern England. It is ful determination, Brodie Collection; In.25374/In.25405 (part deposited in the palaeontological collection of the NHMUK and counterpart), female, one wing, thorax and abdomen under collection no. In.36778. Both part and counterpart are partly preserved; Insect Bed; late Eocene; NW Isle of Wight, present. On the same pieces of limestone is a specimen of a UK. female Culex protorhinus Cockerell 1915 (Culicidae) is located Description. Female. Body length 1.1 mm, wing length which was mentioned by Edwards (1923) under its old collec- 0.8 mm, costal ratio CR about 0.4. Radial cells barely visible. tion no. H. 540 (former Hooley Collection, now included in Remarks. The shape of partly preserved flagellum, wing the collection of the NHMUK). venation and total habitus show that most probably it is a Methods: The fossil was examined with a Leica MZ 9.5 species of the genus Dasyhelea. The oldest records of Dasyhelea Stereomicroscope. Drawings were produced directly from the are from Eocene Baltic amber (Szadziewski 1988, 1993, four specimen with a camera lucida attachment on a Leica MZ 9.5 sp.). The genus was also reported from Miocene Dominican Stereomicroscope. Photographs were made with a Leica MZ amber (Szadziewski & Grogan 1998b, four sp.), Mexican 9.5 Stereomicroscope, and a Nikon Coolpix 4500 digital amber (Szadziewski & Grogan 1996, one species indet.) and camera. Miocene nodules from California (Palmer 1957; Pierce 1966, Terminology and systematics: Morphological terminology six sp.). follows Adler et al. (2004). Current systematic placement of The phyto- and/or saprophagous larvae of Dasyhelea are Simuliidae is in (Yeates & Wiegmann 2005). A aquatic and usually inhabit small and shallow bodies of water. recent molecular analysis by Beckenbach & Borkent (2003) The genus is distributed worldwide and includes 466 recent suggests that Simuliidae is the sister group of (Ceratogogoni- species (Borkent & Wirth 1997). Adults of both sexes feed on dae þ Chironomidae). For Simuliidae the phylogeny given in honeydew or visit flowers for . Adler et al. (2004) is followed. Discussion. Biting midges are rare fossils preserved in the Insect Bed of Bembridge Marls. They are poorly preserved Family Simuliidae Newman, 1834 and have a little taxonomic value. The examined Ceratopogo- Subfamily Newman, 1834 nidae represent large extant genera of worldwide distribution: Gen. et sp. indet. Palpomyia, Stilobezzia and Dasyhelea. Their larvae live in (Figs 71–74) aquatic and semiaquatic habitats. Larvae and female adults of Palpomyia and Stilobezzia are predaceous while those of Description. The fossil pupa is preserved in the special three- Dasyhelea phyto- and/or saprophagous. Females of the latter dimensional mode of preservation typically found in insects genus feed on nectar of flowers and honeydew like males of from the Isle of Wight. The counterparts of the fossil show biting midges. completely different aspects of the fossil. The former body left Among better preserved compression fossils from the early behind a cavity which reveals morphological features rich in Miocene deposits of Rott in Germany, the biting midges were detail. In this fossil probably also remains of the former cuticle represented by five genera: Kieffer, are preserved which have a dark colour. Kieffer, Latreille, Stilobezzia Kieffer and Length of the visible part of the body (without gills) is Meigen (Statz 1944c). As in Bembridge Marls they are about 2.5 mm, both from the ventral side (In.36778a, H. 540) exclusively extant genera of worldwide distribution which are and from the dorsal side (In.36778b, H. 229). Present are common in recent semiaquatic and aquatic habitats. head, thorax and two basal segments of the abdomen. The apical abdominal segments are not visible, probably they are Family Simuliidae Newman, 1834 still embedded in the sediment. The estimated length of the complete pupa probably would have been 5 mm. Maximum by Sonja Wedmann width of the preserved thorax is 1.75 mm. In.36778a shows the pupa from its ventrolateral view (Figs Fossil black flies are very rare and fossils of immature simu- 71, 73). The pupa is of the obtect type, its appendages are not liids are rarer still. Compared to the more than 2100 described free but soldered to the body. extant species (Adler & Crosskey 2011), there are only very The head lies anteroventral to the thorax. An imprint of the few fossil specimens recorded. Evenhuis (1994) gave an over- basal part of one antennal sheath is visible at the uppermost view of the fossil record of Simuliidae. Updated information part of the head. Both eyes, parts of the mouthparts and other on fossil simuliids (excluding subfossil specimens) is discussed structures are discernable in the head and in the ventral by Currie & Grimaldi (2000). Up to now, there are only 12 thoracic region. Imprints of the sheaths of the rather long fossil simuliid species described, which are listed in Adler & maxillary palps can be seen clearly. No special surface sculp- Crosskey (2011). But in the private collection of Christel and ture on head and thorax is discernible, and no cephalic or Hans Werner Hoffeins there are several yet undescribed inclu- thoracic trichomes can be identified. sions of adult black flies in Baltic and Bitterfeld amber (C. & As in In.36778b the prothoracic gills are partly visible. They H. W. Hoffeins 2007, pers. comm.). The oldest undisputed are arborescent, with many filaments preserved only frac- simuliid fossil records are from the Jurassic/Cretaceous of tionally. The imprints of the leg sheaths of the first and second Siberia (Currie & Grimaldi 2000). pair of legs are conspicuous. The imprints of the wing pads are Additionally, there are a few undetermined immature simu- preserved completely and show an uneven surface. In the tips liid fossils, e.g., from the Lower Cretaceous of Australia (Jell of the wing sheaths there seem to be some dark patches of & Duncan 1986; Currie & Grimaldi 2000). Because of the pigmented cuticle preserved. The rest of the body is missing. scarcity of records of immature simuliids, the fossil record of No trace of a cocoon is preserved. the pupa from the late Eocene Insect Bed of the Isle of Wight In.36778b shows the pupa in dorsal view with most of the is interesting even if its exact systematic placement cannot be abdomen not visible (Figs 72, 74). The thorax is enlarged determined. and most probably kind of hump-backed or arched, but no

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Figures 71–74 Simuliid pupa gen. et sp. indet. (71), (72) Photographs. (73), (74) Drawings. In the drawings, black colour indicates areas where dark pigment is present in the fossil, dotting illustrates three-dimensional preservation. (71), (73) NHMUK In.36778a, showing the ventral side of the fossil. (72), (74) NHMUK In.36778b, showing the dorsal side of the fossil. Scale bar ¼ 1 mm. Abbreviations: a1 ¼ abdominal segment 1; a2 ¼ abdominal segment 2; ¼ antennal sheath; e ¼ eye; g ¼ gill; l1 ¼ sheath of leg 1; l2 ¼ sheath of leg 2; mxp ¼ sheath of maxillary palp; psb ¼ postscutellar bridge; w ¼ wing sheath.

trichomes are discernible. The dark former integument pre- smooth. Anterior to the first abdominal segment the served in the thoracic region laterally shows a structure con- postscutellar bridge is visible. Only the first and second basal sisting of small fissures, but this could also be secondary due abdominal segments are preserved. Most of the abdomen is to diagenetic processes during fossilisation. not visible. At each anterolateral corner of the prothorax one gill is Owing to the very well preserved three-dimensional struc- present which consists of many long, slender branches. In the ture of this fossil imprint, it seems most probable that the fossil there is no basal stalk visible. The number of the main fossil was a pupa from which the adult fly had not emerged trunks of the gill cannot be seen, only two or three thickened yet. A moulted pupal skin could not generate such a good basal parts are preserved. The number of secondary filaments three-dimensional imprint. With the preserved structures it is is high, approaching 40 to 50 fine secondary filaments per gill. not possible to determine the sex of the pupa. The surface sculpture of the gill is not discernible in detail, but Discussion: Systematic placement. The fossil pupa can be with 60-fold magnification its surface seems to be quite placed systematically in Simuliidae: Simuliinae because

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 36 WIESŁAW KRZEMIN´ SKI ET AL. simuliid pupae are characterised by a pair of large prothoracic coloration) cannot be applied for many compression fossils spiracular gills which are multibranched. Branched pupal gills from nearly all lacustrine outcrops because of problems of are considered as an autapomorphy of the pupal groundplan preservation. Species described from one outcrop can hardly of Simuliidae (Adler et al. 2004, p. 131). It must be noted be recognised in other places. This has led to an unsupported that branched pupal gills also occur convergently in some multiplication of the fossil species. Thus it is necessary to other groups of nematocerous Diptera (e.g., Hinton 1965), revise the very old and poorly described taxa before any new but the overall morphology with the big and arched thorax attempt of description of new species, especially for the genera and the presence of the postscutellar bridge strongly suggest a Bibio and Plecia. Therefore we thought it unnecessary to add systematic placement of this pupa in Simuliidae. new species descriptions, except in very particular unambiguous A systematic placement of the fossil pupa in Parasimuliinae cases. Herein we revise and describe bibionid species from the can be ruled out because in this taxon the pupal gills consist late Eocene of the Isle of Wight, together with a few other of only three filaments (diagnostic feature, Adler et al. 2004, species of special interest from other outcrops. p. 235). Another feature which might exclude the belonging of the fossil pupa to Parasimuliinae is the possible presence Subfamily Bibioninae Fleming, 1821 of pigmentation in the pupal integument. The extent of the pigmentation is indicated by black markings in Figs 72, 74. Tribe Dilophini Pinto & Amorim, 2000 But it is also possible that these remains of pigmentation be- Genus Dilophus Meigen, 1803 longed to the adult fly developing in the pupa. The pupal gills are characteristic for simuliid pupae, but within Simuliidae the number of filaments per gill is very Type species. Tipula febrilis Linnaeus, 1758, by subsequent variable. Intraspecific variation in the filament number is designation of Latreille (1810, p. 442). especially common in species that have more than 16 filaments (Adler et al. 2004, p. 49). Multibranched gills as found in Dilophus andrewrossi Nel, Colomb & Waller, n. sp. the fossil specimen occur in many different genera among (Figs 75–78, Pl. 6a, Table 2) Simuliinae, both in and in . A more precise systematic placement seems not possible Holotype. NHMUK I.I.9073/9235 (part and counterpart, because insufficient morphological details are preserved in Figs 75, 77, Pl. 6a), Brodie Collection; Insect Bed; late this fossil pupa, and because most of its abdominal segments Eocene; NW Isle of Wight, UK. are not visible. Paratypes. In.26048 (Fig. 76), I.9148 (Fig. 78). Ecology. The immature stages of black flies are bound to Derivation of name. After Dr Andrew Ross. flowing freshwater (Adler et al. 2004, p. 71); that is, they Diagnosis. Two small apical spines and no strong spur on usually need lotic conditions. The most typical larval habitat fore tibia; wing hyaline, 3.85 mm long; r-m cross-vein two of blackflies is streams and rivers, but blackflies can develop times as long as basal part of Rs. in almost every kind of natural running water (Crosskey Description (see Table 2). The body of these small flies are 1990, p. 182ff.). The larvae mostly are attached to the sub- either missing or poorly preserved, with nearly no available strate. They are filter-feeding organisms, but they can also character. Nevertheless the fore tibia of the holotype has scrape organic material from the substrate (Crosskey 1990, two small apical spines and no strong apical spur. The wing p. 138). For pupation, simuliid larvae usually construct a is hyaline, 3.85 mm long in mean, 1.45 mm wide; pterostigma cocoon which is made from . In extant basal taxa such elliptic, clearly sclerified, 0.60 mm long, 0.13 mm wide; C

as , the prosimuliines, and basal simuliines the ends 0.15 mm distal of apex of R4 þ 5; Sc ends just basal of cocoon is quite shapeless and saclike (Adler et al. 2004, pterostigma; R1 reaches the costal margin in the pterostigma; p. 50). A possible reason for the lack of a cocoon in this fossil basal part of R4 þ 5 is short, 0.15 mm long in mean, distinctly might be that the pupa was ripped out of its cocoon and got shorter than r-m; r-m is 0.305 mm long in mean; distance carried away by strong water currents. There are also several between base of r-m and fork of M into M1 and M2 0.72 mm simuliid taxa whose pupae are fixed to the substrate by only a in mean; cross-vein bm-cu slightly basal of fork of M or few threads of cocoon material (Crosskey 1990, p. 296), and ending on it; bm-cu 0.30 mm long; A1 well defined, reaching this might be another explanation for the lack of a cocoon in posterior wing margin. the fossil specimen. Remarks. These fossils are attributable to the same species The length of pupal life varies with the water temperature of because of their very similar wing venation and proportions, the habitat. Under tropical conditions the adult fly can emerge and to Dilophus rather than to Bibio or Bibiodes because of within two days of pupation, in cold climates this period the presence of only two small apical spines on fore tibia rarely exceeds 14 days (Crosskey 1990, p. 320). (Hardy 1981). The very long r-m cross-vein two times as long The adult flies feed on the nectar of a wide variety of plants as basal part of Rs is a very secondary character that could be (Crosskey 1990, p. 388). Additionally, the females of many present in Dilophus, but that also occurs in the genus Bibio. species feed on the blood of warm-blooded This structure can be very variable in the same species of a (Crosskey 1990, p. 411). recent Bibio,viz.B. hortulanus. Among the fossil bibionids from the Isle of Wight, Bibio gurnetensis Cockerell, 1917a has Superfamily Bibionoidea Fleming, 1821 also a very long r-m, about three times as long as basal part of Rs, but this species is distinctly larger than D. andrewrossi, by Andre´ Nel, Franc¸ois-Marie Collomb and Alain Waller with a wing 4.8 mm long. Comparison of D. andrewrossi with the recent species is impossible to achieve because of the lack Family Bibionidae Fleming, 1821 of the genital structures in our material. The fossil record of The past diversity of Bibionidae is difficult to estimate. Dilophus is extremely scarce compared to that of Bibio, with Their systematic is far from being easy as these insects have eight species, Dilophus campbelli Harris, 1983 (, New an important intraspecific variability, in body size and wing Zealand, Eocene), D. krantzii Heyden, 1870 (Rott am venation (see above). Also, several characters that can be Siebengebirge, Germany, Oligocene), D. magnus Du¨rrenfeldt, used for recent species (male anal appendages, body and wing 1968 (Germany, Pliocene), D. priscus Loew, 1850 (Baltic amber, Eocene/Oligocene), D. matilei Waller et al., 2000

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Figures 75–95 Bibionidae. (75–78) Dilophus andrewrossi Nel, Colomb & Waller, sp. n.: (75) holotype counter- part NHMUK I.9235; (76) paratype NHMUK In.26048; (77) holotype part NHMUK I.9073; (78) paratype NHMUK I.9148. (79–81) ?Bibio gurnetensis Cockerell, 1917a: (79) holotype part NHMUK I.8641; (80) NHMUK I.9604 (type of Bibio oblitus Cockerell, 1921 syn. nov.); (81) holotype counterpart NHMUK I.8900. (82–84) ?Bibio oligocenus Cockerell, 1917a: (82) holotype NHMUK I.8650; (83) NHMUK In.32283; (84) NHMUK In.25243. (85) ?Bibio extremus Cockerell, 1921, holotype NHMUK I.8860. (86) ?Bibio sp., NHMUK I.9363. (87) Bibiodes confluens (Cockerell, 1915) n. comb., NHMUK In.43454 (scale bar ¼ 4 mm). (88) Plecia acourti Cockerell, 1921, holotype NHMUK In.17098/In.17500. (89–92) Plecia sp.: (89) NHMUK In.26049; (90) NHMUK In.17230/In.17474; (91) NHMUK In.25249; (92) NHMUK In.20558/In.20557. (93) Plecia undans Zeuner, 1941, holotype NHMUK In.37274. (94, 95) Penthetria sp.: (94) NHMUK In.24800; (95) NHMUK In.25246. (Scale bars ¼ 1 mm if not stated otherwise.)

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Plate 6 Bibionidae. (a) Dilophus andrewrossi Nel, Colomb & Waller, n. sp. holotype counterpart NHMUK I.9235. (b–d) ?Bibio gurnetensis Cockerell, 1917a: (b) holotype part NHMUK I.8641. (c) NHMUK I.9604 (type of Bibio oblitus Cockerell, 1921 syn nov.). (d) holotype counterpart NHMUK I.8900. (e) ?Bibio oligocenus Cockerell, 1917a, holotype NHMUK I.8650. (f ) Bibio obliteratus (Cockerell, 1915) n. comb., holotype USNM 61442. (g) ?Bibio extremus Cockerell, 1921, holotype NHMUK I.8860. (h) ?Bibio sp., NHMUK I.9363. (i) Bibiodes confluens (Cockerell, 1915) n. comb., NHMUK In.43454. (j) Plecia acourti Cockerell, 1921, holotype counterpart NHMUK In.17500. (k) ?Plecia sp., NHMUK In.26049.

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Table 2 Dilophus andrewrossi sp. n. Main wing dimensions of the type material. Abbreviations: L wing ¼ wing length; W wing ¼ wing width; L r-m ¼ length of r-m; L Rs base ¼ length of basal part of Rs; L bm-cu ¼ length of bm-cu.

Specimen/dimensions L wing W wing L r-m L Rs base L bm-cu I.9235 3.9 mm 1.5 mm 0.29 mm 0.15 mm 0.30 mm I.26048 3.8 mm 1.4 mm 0.30 mm 0.18 mm 0.30 mm I.9073 4.0 mm 1.51 mm 0.30 mm 0.13 mm 0.28 mm I.9148 3.7 mm ? 0.33 mm 0.15 mm ?

(Dominican Republic amber, Miocene), D. palaeofebrilis Sc ends just basal of pterostigma; R1 reaches the costal margin Skartveit, 2009, D. crassicornis Skartveit, 2009 and D. succineus in the pterostigma; basal part of R4+5 is short, 0.20–0.26 mm Skartveit 2009 (Evenhuis 1994; Waller et al. 2000; Skartveit long, three times shorter than r-m; r-m 0.60–0.64 mm long; 2009). Statz (1943, p. 56) added an undescribed record from distance between base of r-m and fork of M into M1 and M2 the Late Oligocene of Aix-en-Provence, France. This record is 0.9–1.0 mm; cross-vein bm-cu slightly basal of fork of M or very unlikely: in 26 years we have never collected any represen- ending on it; bm-cu 0.44–0.49 mm long; A1 well defined, tatives of this genus among the thousands of bibionids from reaching posterior wing margin. this outcrop. Remarks. Cockerell (1917a, pp. 375, 384, pl. 31, fig. 4; 1921, The original description and figures of D. krantzii are not p. 468, fig. 29) described B. gurnetensis and B. oblitus on the very convincing and this species should be redescribed. Never- basis of rather poorly preserved wings. There is no correct theless, its wing is distinctly longer than that of D. andrewrossi, character to separate to the two species. All these fossils are i.e., about 7.9 mm long, instead of 3.85 mm in D. andrewrossi attributable to the same species because of their very similar (Heyden 1870, p. 255, pl. 45, fig. 24). The wings of D. wing venation and proportions, especially in the large wing matilei are shorter: 2 mm long (Waller et al. 2000). The and the very long r-m, about three times as long as basal part wings of D. magnus are distinctly longer: 8.0 mm long (Du¨rren- of Rs. Nevertheless, its attribution to the genus Bibio rather feldt 1968, p. 50). D. palaeofebrilis, D. crassicornis and D. than Dilophus is impossible to establish as there is no wing succineus have wing length similar to that of D. andrewrossi, character that would be sufficient to separate the two genera. between 3.15 and 3.80 mm. The r-m cross-vein is distinctly more than two times as long as basal part of Rs in both D. ?Bibio oligocenus Cockerell, 1917a palaeofebrilis and D. crassicornis. D. andrewrossi has only two (Figs 82–84, Pl. 6e) small apical spines on fore tibia, instead of four or five in D. palaeofebrilis, D. crassicornis, and D. succineus. D. priscus 1917a Bibio oligocenus Cockerell, pp. 375, 384, pl. 62, fig. 3a–d has apparently never been revised and is very poorly known, 1994 Bibio oligocenus Evenhuis, p. 125 by the following information concerning the strong thoracic setae: ‘Von der Gattung Dilophus ist mir nur ein einziges Holotype. NHMUK I.8650 (Fig. 82); Insect Bed; late Weibchen vorgekommen, welches in der Stellung der dicken Eocene; NW Isle of Wight, UK. Dornen auf dem Thorax von allen bei uns einheimischen Arten Description. Wing hyaline, about 9.1 mm long, 3.7 mm abweicht. Ich nenne die Art Dilophus priscus.’ (Loew 1850, wide; pterostigma elliptic, clearly sclerified, 1.3 mm long, p. 38). Thus it is impossible to compare to our fossils. 1.42 mm wide; C ends just distal of apex of R4+5;ScandR1 reach the costal margin in the pterostigma; basal part of R4+5 Tribe Bibionini Frey, 1927 is long, 0.82 mm long, three times longer than r-m; r-m 0.27 mm long; distance between base of r-m and fork of M Subtribe Bibionina Frey, 1927 into M1 and M2 unknown; position of cross-vein bm-cu Genus Bibio Geoffroy, 1762 unknown; A1 well defined. Remarks. Cockerell (1917a, pp. 375, 384, pl. 31, fig. 5) described and figured this species on the basis of an incom- Type species. Tipula hortulana Linnaeus, 1758, by subsequent plete and rather poorly preserved wing. Its main character is designation of Latreille (1810, p. 442) (as ‘Hirtea hortulana its very large wing, with a long basal part of Rs. It is probably Fabr.’). (Validated by I.C.Z.N. (1957a, p. 86).) a Bibio but the possible attribution to Dilophus cannot be excluded. Two other specimens In.32283 (Fig. 83, Colenutt ?Bibio gurnetensis Cockerell, 1917a Collection) and In.25243 (Fig. 84, Hooley Collection) with (Figs 79–81, Pl. 6b–d) very large wings could belong to the same species, but their 1917a ?Bibio gurnetensis Cockerell, p. 375, 384, pl. 31, fig. 4 wings are slightly shorter and narrower than that of the type 1921 Bibio oblitus Cockerell, p. 468, fig. 29 syn. nov. of B. oligocenus and their r-m are very short or completely 1994 Bibio gurnetensis Evenhuis, p. 124 reduced. 1994 Bibio oblitus Evenhuis, p. 125 Bibio obliteratus (Cockerell, 1915) n. comb. Pl. 6f Holotype. NHMUK I.8641/I.8900 (part and counterpart 1915 Protoberis obliterata Cockerell, pp. 494, 499, pl. 63, Figs 79, 81, Pl. 6b, d), Brodie Collection; Insect Bed; late figs A,B Eocene; NW Isle of Wight, UK. 1992 Protoberis obliterata Carpenter, p. 422 Additional material. I.9604 (type of Bibio oblitus, Fig. 80, 1994 Protoberis obliterata Evenhuis, p. 309 Pl. 6c). Description. Wing hyaline, 4.8–4.9 mm long, 1.8–2.0 mm Remarks. Cockerell (1915, pp. 494, 499, pl. 63, fig. 1a, b) wide; pterostigma elliptic, clearly sclerified, 0.7–0.8 mm long, described and figured a very poor specimen (holotype USNM 0.2–0.3 mm wide; C ends 0.1–0.2 mm distal of apex of R4+5; 61442) he attributed to the Stratiomyidae under the name

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In addition to holotype specimen NHMUK (Fig. 85, Pl. 6g) In.43454 (Fig. 87, Pl. 6i), Hooley Collection. Description. (Based on specimen In.43454) An isolated 1921 Bibio extremus Cockerell, p. 486, fig. 30 wing, hyaline, about 4.32 mm long (about 5 mm in the holo- 1994 Bibio extremus Evenhuis, p. 124 type), 1.66 mm wide; pterostigma elliptic, clearly sclerified, 0.82 mm long, 0.25 mm wide; C ends just distal of apex of Holotype. NHMUK I.8860, Brodie Collection; Insect Bed; R4+5; Sc reaches the costal margin just basal of the pteros- late Eocene; NW Isle of Wight, UK.. tigma and R1 in the pterostigma; basal part of R4+5 is long, Description. Wing hyaline, about 5.5 mm long, 2.0 mm 0.27 mm long; Rs fused with M for 0.25 mm; cross-vein wide; pterostigma elliptic, clearly sclerified, 0.82 mm long, bm-cu deformed; A1 present. 0.27 mm wide; apex of C not preserved; Sc and R1 reach the Remarks. The attribution of In.43454 to Bibiodes confluens costal margin in the pterostigma; basal part of R4+5 is long, is based on its very close wing dimensions. Its fusion Rs-M 0.42 mm long, r-m completely reduced and Rs and M touch- slightly longer than in the type of this species supports its attri- ing in one point; distance between this point and fork of M bution to Bibiodes. into M1 and M2 1.0 mm; cross-vein bm-cu 0.42 mm long; A1 well defined. Subfamily Plecinae Duda, 1930 Remarks. The figure by Cockerell (1921, p. 468, fig. 30) is partly erroneous as he figured a short r-m cross-vein. It is Genus Plecia Wiedmann, 1828 smaller than B. oligocenus and longer than Bibiodes confluens (see below), but the complete reduction of r-m suggests possible Type species. Hirtea fulvicollis Fabricius, 1805, by subse- affinities with Bibiodes, which cannot be definitely demon- quent designation of Blanchard (1840, p. 576). strated. Another specimen (I.9363, see Fig. 86, Pl. 6h) has also its r-m completely reduced and Rs and M touching in one Plecia acourti Cockerell, 1921 point, but its wing is shorter than that of B. extremus (4.5 mm (Fig. 88, Pl. 6j) long instead of 5.5 mm in the latter). I.9363 could correspond to a different species but this difference in size is not sufficient 1921 Plecia acourti Cockerell, pp. 467–68, fig. 28 to clearly separate it from B. extremus. We prefer to consider it 1994 Plecia acourti Evenhuis, p. 129 as a Bibio? species. Holotype. NHMUK In.17098/In.17500 (part and counter- Subtribe Bibiodina Frey, 1927 part), Smith Collection; Insect Bed; late Eocene; NW Isle of Wight, UK. Genus Bibiodes Coquillett, 1904 Description. This species is based on a rather poorly pre- 1904 Bibiodes Coquillett, p. 171 served female specimen (abdomen, part of thorax and one 1915 Bibiodites Cockerell, p. 493; syn. nov. wing) (Cockerell 1921, pp. 467–68). Wing infuscate, 6.4 mm long, 2.5 mm wide; pterostigma not visible; basal part of Rs long, 1.0 mm long, r-m 0.26 mm long; R2+3 separates from Type species. Bibiodes halteralis Coquillett, 1904, by original R4+5 1.5 mm distal of r-m; R2+3 nearly straight, 0.78 mm designation. long, strongly diverging from R4+5; distance between r-m and The fossil record of this recent Nearctic genus comprises fork of M into M1 and M2 0.58 mm; cross-vein bm-cu 0.6 mm Bibiodes intermedia James, 1937, B. nanus Skartveit, 2009 and basal of r-m, 0.3 mm long; A1 well defined. Abdomen broad B. balticus Skartveit, 2009. Cockerell (1915, p. 493) separated (female), but deformed. his fossil genus Bibiodites from Bibiodes on the basis of its Remark. The generic attribution of this species is confirmed, shorter confluence between Rs and M. The ratio (length but it is nearly impossible to compare it to the other Cenozoic of confluent Rs-M/wing length) is 0.09 in the recent Bibiodes Plecia. aestivus Melander, 1912, 0.05 in the type specimen of Bibio- dites confluens, 0.06 in specimen In.43454, 0.0325 in the type ?Plecia spp. specimen of Bibiodes intermedia (Cockerell 1915; James 1937) and 0.03 in Bibiodes massiliensis sp. n. The differences are too Among the Plecia from the Isle of Wight, three other poten- weak to justify a generic separation. Thus we support the syn- tial ‘species’ can be defined: onymisation of the two genera and the transfer of Bibiodites confluens Cockerell, 1915 into the genus Bibiodes, as proposed e A smaller one (specimen In.26049, wing length 4.3 mm), by Skartveit (2009). The presence of the Nearctic genus Bibiodes with R2+3 strongly curved (Fig. 89, Pl. 6k) in the Eocene and Oligocene of Europe is of great interest for e A larger one (specimen In.17230/In.17474, wing length its age and past distribution. Its relatively recent discovery in 10.4 mm), with R2+3 elongate and sigmoidal (Fig. 90, China (Bibiodes sinensis Yang & Luo 1987) supports its ancient Pl. 9c) presence in the Palaearctic region (Yang & Luo 1987). e A species of nearly the same size as Plecia acourti (speci- mens In.25249 (Fig. 91, Pl. 9a), wing length 8.25 mm and Bibiodes confluens (Cockerell, 1915) n. comb. In.20558/In.20557 (Fig. 92), wing length 9.1 mm), with (Fig. 87, Pl. 6i) R2+3 very long and nearly parallel to R4+5, but less than in

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 41 the Penthetria from the same outcrop (see below). The wing widely used in the of the subfamily. Until further of this species is very similar to that of Plecia undans advance in classification of gnats it is possible to Zeuner, 1941 from the early Eocene of the Isle of Mull say that Mycetophila vectensis Cockerell, 1915 (Pl. 7g), (UK). ‘Rymosia’ edwardsi Cockerell, 1921 (Pl. 7d), ‘Rymosia’ ferruginea Cockerell, 1921 (Pl. 7e) and ‘Rymosia’ rufescens We prefer to maintain these fossils as ‘Plecia species un- Cockerell, 1921 (Pl. 7f) most probably belong to the tribe determined’, in order to avoid increasing confusion in the Mycetophilini; Rymosia grisea Cockerell, 1921 (Pl. 7h) is a Cenozoic bibionid taxonomy. representative of the subfamily Mycetophilinae. These species will not be redescribed in the present paper. Plecia undans Zeuner, 1941 Fifteen specimens of the subfamily Sciophilinae belong to (Fig. 93) 10 species of eight genera: Acnemia, Azana, Aglaomyia, Coelosia, Dziedzickia, Palaeoempalia, Mycomya and Leia,mostofthem, except Palaeoempalia, are found in recent fauna. All the genera, Holotype. NHMUK In.37274. except Aglaomya, are known from Baltic amber. Aglaomya can Additional material. Paratype NHMUK In.37266. be easily mistaken for , known from the Baltic amber Age and outcrop. Early , early Eocene, Ardtun and Oligocene and Miocene of Europe. A species of Mycomya Head, Isle of Mull, UK. Evenhuis (1994, p. 133) indicated is also known from Palaeocene amber of the Sakhalin Island that this outcrop was , but it is now con- (Blagoderov 2007). sidered as Early Eocene (Royer et al. 2001). The detailed comparison of the fauna can be made only Description. Zeuner (1941, pp. 94–95, figs 13, 14) proposed after revision of the Baltic amber material. However, an exact figures of the type material. We had the opportunity to apparent observation can be made. From 155 species of revise the paratype specimen. Wing about 11.0 mm long, Mycetophilidae described from Baltic amber, 126 belong to about 3.52 mm wide; pterostigma not visible; basal part of Rs the subfamily Sciophilinae, while more than a half of species long, 1.12 mm long, r-m 0.4 mm long; R2+3 separates from (12) and more than two-third of specimens of the Isle of Wight R4+5 1.2 mm distal of r-m; R2+3 very long, sigmoidal, and fungus gnats are from the subfamily Mycetophilinae. Larvae nearly parallel to R4+5, 2.3 mm long; distance between r-m of Mycetophilinae are almost obligatory mycetophagous, and fork of M into M1 and M2 0.56 mm; cross-vein bm-cu developing on fruiting bodies of mushrooms. Sciophilinae, on 1.2 mm basal of r-m, 0.2 mm long. the other hand demonstrate a number of various biologies, including sapromycetophagy, zoomycetophagy, xylomycetophagy Subfamily Penthetriinae Enderlein, 1936 and occasionally eumycetophagy. The great diversity and abundance of mycetophiline fungus gnats in the Isle of Wight Genus Penthetria Meigen, 1803 oryctocenosis allows us to reconstruct warm temperate and (Figs 94, 95, Pl. 9b) rather humid forest environment.

Type species. Penthetria funebris Meigen, 1804, by subse- Family Mycetophilidae Newman, 1834 quent monotypy in Meigen (1804, p. 104). Subfamily Sciophilinae Rondani, 1840 Penthetria sp. Remarks. We discovered in the NHM collection two Genus Acnemia Winnertz, 1863 specimens, In.24800 (Fig. 94) and In.25246 (Fig. 95, Pl. 9b) (both Hooley Collection), attributable to this genus that was 1863 Acnemia Winnertz, p. 798. Type species Leia nitidicollis previously unrecorded from the Isle of Wight. The genus Meigen, 1818, by subsequent designation by Johannsen is rather frequent in the Oligocene and Miocene of Europe. 1909, p. 63 Its oldest records date from the Late Eocene of Monteils 1865 Agaricobia Philippi, p. 626. Type species Agaricobia (undescribed species, France, see above), the North American fulvicollis Philippi, 1865, by monotypy Eocene, namely Penthetria whipsawensis Rice, 1959 and P. creedensis (James 1938) and two Baltic amber species Remarks. The genus includes about 40 species distributed (Fitzgerald 1999; Skartveit 2009). It is not necessary to create worldwide, mainly from temperate to warm temperate zones. new species for the material of the Isle of Wight because it would hardly be comparable with the already described species. Acnemia simplex Cockerell, 1921 (Pl. 8a) Superfamily Billberg, 1820 1921 Acnemia simplex Cockerell, pp. 463, 464, fig. 19 by Vladimir Blagoderov 1994 Acnemia simplex Evenhuis, p. 146

The fungus gnats of the late Eocene of the Isle of Wight are Holotype. NHMUK I.9597, Brodie Collection; Insect Bed; surprisingly diverse and rather abundant. Keroplatidae are late Eocene; NW Isle of Wight, UK. represented by seven species (17 specimens) and Mycetophilidae Diagnosis. The species differs from A. bolsiusi Meunier, by 22 species (55 specimens studied). Cockerell (1915, 1921) 1904 in having very short section M2 (M fork is 2.5 times the described eight species of Mycetophilidae and one species of section M3 in the latter species). It differs from A. cyclosoma Keroplatidae. Although all described taxa constitute good Cockerell, 1925 in smaller size and having RS base more species, their taxonomic position should be reconsidered. proximal (at 0.4 times the wing length in the latter species). Seventy-two per cent of the studied specimens of mycetophilids Description. Wing, 2.5 mm. Wing membrane with macrotri- belong to the subfamily Mycetophilinae. Among 40 specimens chia decumbent. Costa with two rows of setae, all veins except of Mycetophilinae from the collection of the NHM one could RS and section M3 with macrotrichia. Sc2 at the level of base distinguish up to 12 different species, but their generic assign- of r-m. Terminal part of Sc (distad of Sc2) three time the r-m. ment remains unclear. Characters of wing venation are not Costa continues beyond the tip of R5 at 1/5 of distance

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Plate 7 Tipulidae, Limoniidae, Mycetophilidae and Sciaridae. (a) Leptotarsus (Longurio) wegiereki Krzeminski, n. sp., NHMUK In.17493. (b) Ilisia (Lunaria) incognita (Cockerell, 1921) n. comb., NHMUK I.9186. (c) Paltostomopsis ciliata Cockerell, 1915, holotype, USNM 61433 (Tipulomorpha indet.). (d) ‘Rymosia’ edwardsi Cockerell, 1921 NHMUK I.9336. (e) ‘Rymosia’ ferruginea Cockerell, 1921, NHMUK I.9802. (f ) ‘Rymosia’ rufescens Cockerell, 1921, NHMUK I.8865. (g) Mycetophila vectensis Cockerell, 1915, USNM 61434. (h) Rymosia grisea Cockerell, 1921, NHMUK I.8956. (i) Sciara gurnetensis Cockerell, 1915, USNM 61435. (j) Sciara protoberidis Cockerell, 1915, USNM 61437. (k) Sciara lacoei Cockerell, 1915, USNM 61436.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 43 between tips of R5 and M1. Length of r-m about the length of of r-m, and length of RS base is 0.5 times the length of r-m. section M3 and 1.2 times the length of RS1. Distance from the Section M2 is 1.87 the section M3. Base of fork M3 þ 4and wing base to RS is 0.28 times the wing length. Length of Sc is CuA proximad of the base of section M2. 0.37 times the length of wing; length of R1 is 0.65 times the Remarks. The species is assigned to genus Aglaomyia as length of wing. M fork is 10 times the length of section M3, having a combination of following characters: R4 absent; Sc section M2 is three times the length of section M3. long, reaching the level of r-m base, ending in C; Sc2 in terminal 1/3 of Sc. The genus is close to Boletina Staeger. A number of Genus Azana Walker, 1856 species of Boletina is described from the Eocene–Miocene of Europe, North America and China, but they should be revised. 1856 Azana Walker, p. 26. Type species Azana scatopsoides Some of them do not belong to Mycetophilidae at all (B. Walker, 1956, p. 234, by monotypy ¼ Boletina anomala acropteris Hong, 1981 – probably Chironomidae, B. melaina Staeger, 1840, p. 238 Hong, 1981, B. pulvinata Hong, 1981, B. uda Hong, 1981 – Sciaridae). Remarks. Fifteen species in Holarctic and Oriental Regions, temperate to tropic. One fossil species in Eocene of Baltic Genus Coelosia Winnertz, 1863 amber. 1863 Coelosia Winnertz, p. 796. Type species Boletina flava Azana cockerelli Blagoderov, n. sp. Staeger, subsequent designation by Johannsen, 1909, (Fig. 96, Pl. 8b) p. 86

Holotype. NHMUK I.9264, partly preserved thorax, abdo- Twenty-four species mainly in Holarctic. Larvae in fungi men and a wing, Brodie Collection; Insect Bed; late Eocene; (Soli 1997). NW Isle of Wight, UK. Diagnosis. The species differs from A. rarissima Meunier, ?Coelosia virgata (Cockerell, 1921) n. comb. 1904 from the Baltic amber in having RS base more proximal (Fig. 98, Pl. 8e) (R base is 2.71 times the R1 in the latter species) and CuA longer (0.63 times the wing length in latter species). 1921 Phronia (?) virgata Cockerell, pp. 465–66, fig. 20 Description. Measurements: body 2.8 mm, wing 2.1 mm. 1994 Phronia virgata Evenhuis, p. 161 Costa slightly extends beyond the tip of R5. Sc not apparent. Length of R þ R1 is 0.44 times the wing length. R base Holotype NHMUK I.9789, Brodie Collection; Insect Bed; (measured between humeris and RS base) is 1.89 times the late Eocene; NW Isle of Wight, UK. R1. Length of r-m is 1.56 times the length of terminal section Additional material. NHMUK In.25315, In.25290, Hooley of Sc (distad of Sc2). Length of R5 is 0.83 times the wing Collection. length, length of CuA – 0.75 times the wing length. Basal Diagnosis. The species differs from other species of Coelosia half of M vein is obsolete. M curved posteriorly at the very in absence of macrotrichia on Sc. end. CuA is evenly curved. Description. Measurements: body 3 mm; wing 2.5–3 mm (holotype 2.7). Wing: wing membrane with microtrichia not Subfamily Gnoristinae Edwards, 1925 organised in rows. Costa extends beyond the tip of R5 to 1/2 Genus Aglaomyia Vockeroth, 1980 of the distance between the tips of R5 and M1. Costa, R base, R1, R5 and r-m setose. Sc bare, ending at C at the distad of 1980 Aglaomyia Vockeroth, p. 537, type species Aglaomyia the level of r-m base, its length 0.24–0.29 times the length of gatineau Vockeroth, by original designation the wing (holotype 0.29). Sc2 absent. Length of R1 is 0.71– 0.78 times the length of the wing (holotype 0.78). Length of Two species in Nearctic and Palaearctic. Larvae in decaying R5 (measured from the base of RS) is 0.59–0.63 times the wood of deciduous trees. length of the wing (holotype 0.63). Length of section M3 is 1.21–1.44? times the length of r-m (holotype 1.44) and 0.77– Aglaomyia vectis Blagoderov, n. sp. 0.87 times the section M2 (holotype 0.87). M-ratios (Soli (Fig. 97, Pl. 8c) 1997) are 0.26 and 0.31, Cu ratios are 1.9–2.5 (holotype 1.9) and 4.47–4.8 (holotype 4.47). Thorax. Mediotergite and Derivation of name. From Vecta insula, Latin name of the laterotergites without apparent hairs. Isle of Wight. Holotype. NHMUK In.24819, partial wing, Hooley Collec- Genus Dziedzickia Johannsen, 1909 tion; Insect Bed; late Eocene; NW Isle of Wight, UK. Other material. In.25321, In.25318, In.25194, Hooley 1885 Hertwigia Dziedzicki, p. 165. Preoccupied by Schmidt. Collection. Type species Hertwigia marginara Dziedzicki, 1885, by Diagnosis. It differs from A. ingrica and A. gatineau in monotypy having section M3 longer (in recent species length of M3 is 1909 Dziedzickia Johannsen, p. 44. Replacement name for about the length of r-m). Hertwigia Dziedzicki Description. Measurements: wing: 3.7–4 mm (holotype – 4 mm). Wing membrane with microtrichia only. Costa, R1 Approximately 60 species worldwide, distributed from cold and R5 with macrotrichia. Costa extends beyond the tip of temperate to equatorial zone. Biology unknown. Five fossil R5 to 1/4 of the distance between the tips of R5 and M1. Sc species are known from the Baltic amber and the Oligocene ending in C at the level of the base of section M3. Sc2 in of Rott. terminal 1/3 of Sc, slightly proximad of the level of M3 þ 4 and CuA fork base. Veins R1 and R5 almost straight, not Dziedzickia oligocenica Blagoderov, n. sp. curved posteriorly. Length of section M3 is 2.3 the length (Fig. 99, Pl. 8g)

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Figures 96–104 Mycetophilidae and Keroplatidae, wing venation. (96) Azana cockerelli Blagoderov, n. sp., holotype NHMUK I.9264. (97) Aglaomyia vectis Blagoderov, n. sp., holotype NHMUK In.24819. (98) ?Coelosia virgata (Cockerell, 1921), n. comb., holotype NHMUK I.9789. (99) Dziedzickia oligocenica Blagoderov, n. sp., holotype NHMUK In.25301. (100) Palaeoempalia saxea Blagoderov, n. sp., holotype NHMUK I.9360. (101) Mycomya oblita Cockerell, 1921, holotype NHMUK I.8973. (102) Mycomya hoolei Blagoderov, n. sp., holotype NHMUK In.25330. (103) Leia gurnardensis, n. sp., holotype NHMUK In.25295. (104) Macrocera obliqua (Cockerell, 1921), n. comb., holotype NHMUK I.9657.

Derivation of name. From Oligocene. and CuA very proximal; D. sepulta Meunier, 1917 – in Holotype. NHMUK In.25301, a wing, Hooley Collection; absence of R4 vein. D. nashi Blagoderov & Grimaldi, 2004 Insect Bed; late Eocene; NW Isle of Wight, UK. from the Upper Cretaceous New Jersey amber differs from Diagnosis. D. hadroneuroides Meunier, 1923 differs from the the new species in having small cell bigger, Sc longer and new species by larger size, P6mm; D. johannseni Meunier, base on M3 þ 4 and CuA fork more proximal. 1917 – in having section M3 shorter than r-m and base of Description. Measurements. Wing 3.1 mm (preserved part M3 þ 4 and CuA fork proximad of r-m base; D. lepida Statz, 2.9 mm). Wing membrane with microtrichia only. Costa 1944a in having RS base more proximal, small sell long and extends beyond the tip of R5 to 1/5 of the distance between rectangular, and base of M3 þ 4 and CuA fork proximally; the tips of R5 and M1. R base with 12–13 setae, R1 with D. sedula Meunier, 1923 – in having base on fork M3 þ 4 6 þ 23 setae, and R5 with 14 setae. Sc ending at R at the level

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Plate 8 Mycetophilidae and Keroplatidae. (a) Acnemia simplex Cockerell, 1921, holotype NHMUK I.9597. (b) Azana cockerelli Blagoderov, n. sp., holotype NHMUK I.9264. (c) Aglaomyia vectis Blagoderov, n. sp., holotype NHMUK In.24819. (d) Palaeoempalia saxea Blagoderov, n. sp., holotype NHMUK I.9360. (e) ?Coelosia virgata (Cockerell, 1921), n. comb., holotype NHMUK I.9789. (f ) Leia gurnardensis Blagoderov, n. sp., holotype counterpart NHMUK In.25314. (g) Dziedzickia oligocenica Blagoderov, n. sp., holotype NHMUK In.25301. (h) Mycomya hoolei Blagoderov, n. sp., holotype NHMUK In.25330. (i) Mycomya oblita Cockerell, 1921, holotype NHMUK I.8973. (j) Macrocera obliqua (Cockerell, 1921), n. comb., holotype NHMUK I.9657.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 46 WIESŁAW KRZEMIN´ SKI ET AL. of RS base. R5 straight. R4 present, small cell trapezoid. of the level of base of M2; M. unicolor Statz, 1944a – in Section RS1 is 1.2 times the section RS2. Length of r-m 1.7 having Sc ending at R and section M2 approximately the times the section RS1 and 0.34 times the section M3. Section same length as crossvein r-m. M. helmi (Cockerell, 1904) M2 is 1.9 the section M3. M fork is 3.28 times the section differs from the new species in having section M3 much M3. Base of fork M3 þ 4 and CuA at the level of base of r-m. shorter. Comparison with other fossil species is difficult due Remarks. It was noted (Hutson 1979; Vockeroth 1980; to insufficient descriptions and/or illustrations. Matile 1992; Chandler 1999) that the genus in the present Description. Measurements: wing 3.3 mm, abdomen 2.2 mm. definition is most probably polyphyletic, so detailed com- Wing: Sc ending at Costa, its length 0.43 times the wing parison can be made only after the revision of the genus. length. Sc2 slightly proximal of the middle of small cell. Section RS1 is 1.1 times the crossvein r-m and 0.38 times the Genus Palaeoempalia Meunier, 1897 section RS2. Section M2 is 3.8 times the section RS2 and 1.1 times the section M2. Length of fork M1 and M2 approxi- 1897 Palaeoempalia Meunier, p. 218 mately equal the section M3. Base of fork M3 þ 4 and CuA at the level of Sc2, M3 þ 4 and CuA stalk is 1.29 times the Type species. P. brongniarti Meunier, 1904, by subsequent section M2. designation of Johannsen, 1909. Eleven species were described from the Baltic amber, Mycomya hoolei Blagoderov, n. sp. although the genus needs to be revised. (Fig. 102, Pl. 8h)

Palaeoempalia saxea Blagoderov, n. sp. Derivation of name. In honour of R. W. Hooley, collector of (Fig. 100, Pl. 8d) the type specimen. Holotype. NHMUK In.25330, wing, Hooley Collection; Derivation of name. From Latin saxeus meaning made of Insect Bed; late Eocene; NW Isle of Wight, UK. stone. Diagnosis. The new species is the closest to M. helmi Holotype. NHMUK I.9360, partial body and wing, Brodie (Cockerell, 1904) from which it differs in having M3 þ 4and Collection; Insect Bed; late Eocene; NW Isle of Wight, UK. CuA fork base proximad of the level of base of M2. Diagnosis. The new species differs from P. brongniarti in Description. Measurements: wing 5.5 mm. Sc ending at having longer section M3, and position of Sc2 and base of Costa, its length 0.46 times the wing length. Sc2 at the fork M3 þ 4 and CuA more distally. Edwards (1940) noted proximal 1/4 of the middle of small cell. Section RS1 is equal that most of the species referred by Meunier to Palaeoempalia the crossvein r-m and 0.53 times the section RS2. Section M2 may belong to Palaeoboletina. The detailed comparison can is two times the section RS2 and 0.60 times the section M2. be possible only after revision of the Baltic amber species. Length of fork M1 and M2 is 2.17 times the section M3. Description. Measurements: body 4.2 mm, wing 3 mm. Base of fork M3 þ 4 and CuA proximad of the level of Sc2, Wing: R base, R1 and R5 setose. Sc ending at C, just before M3 þ 4 and CuA stalk is 0.72 times the section M2. the level of R4, its length 0.39 times the wing length. Sc2 present, at the level of RS. Section RS2 is 1.2 times the section Genus Leia Meigen, 1818 RS1. Length of crossvein r-m is 1.44 times the section RS1. Section M3 is 3.05 times the length of crossvein r-m. Section 1818 Leia Meigen, p. 258. Type species Leia fascipennis M2 is 2.23 times the section M2. M fork is 3.27 times the sec- Meigen, by subsequent designation by Curtis, 1837, tion M3; tips of veins M1 and M2 diverging. Base of M3 þ 4 p. 645 and CuA fork at the level of base of r-m. 1856 Lejosoma Rondani, p. 195, unjustified replacement name for Leia Meigen. Type species Leia bimaculata Genus Mycomya Rondani, 1856 Meigen, by original designation 1856 Lejomya Rondani, p. 195, incorrect original spelling of 1856 Mycomya Rondani, p. 194. Type species Lejosoma marginata Meigen, 1818, by monotypy 1863 Glaphyroptera Winnertz, p. 771. Preoccupied by Heer. 1865 Cnephaeophila Philippi, p. 618. Type species Cnephaeo- Type species Leia fascipennis Meigen, by subsequent phila fenestralis Philippi, 1865, by monotypy designation by Coquillett 1910, p. 547 1878 Neoglaphyroptera Osten Sacken, 1878, p. 10. Replace- The genus has world wide distribution and includes more ment name for Glaphyroptera Winnertz than 300 extant species. About 15 fossil species of Mycomya Leja auct. Misspelling. are described from Cainozoic localities of Europe, North America and Far East. The genus has worldwide distribution and includes about 130 species. Larvae were reported from mushroom fruiting Mycomya oblita Cockerell, 1921 bodies, on surface of fungi or decaying wood, in birds’ nests. (Fig. 101, Pl. 8i) 1921 Mycomya oblita Cockerell, p. 463, fig. 18 Leia gurnardensis Blagoderov, n. sp. 1994 Mycomya oblita Evenhuis, p. 157 (Fig. 103, Pl. 8f )

Holotype. NHMUK I.8973, partial insect, Brodie Collec- Derivation of name. From Gurnard Bay of the Isle of tion; Insect Bed; late Eocene; NW Isle of Wight, UK. Wight. Diagnosis. M. unicolor, M. fossilis, M. kuhni, M. umbonata, Holotype. In.25295/In.25314 (part and counterpart), wing M. fulvescens Statz, 1944a differ from the new species in hav- without apex and partial thorax, Hooley Collection; Insect ingScendingatRandM3þ 4 and CuA fork base proximad Bed; late Eocene; NW Isle of Wight, UK.

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 47 Diagnosis. The new species differs from L. abberans Statz, Specimens In.25299 and I.10061 also belong to two different 1944a, L. curvipetiolata Meunier, 1904, L. gracilima Fo¨ster in species of Macrocera distinguishable by details of venation. having section M3 shorter than crossvein r-m, from L. crassi- Specimens In.25298 and In.17260 by having the base of palpis Meunier, 1904 and L. longipetiolata Meunier, 1904 in M3 þ 4 curved and divergent from CuA could be attributed having fork of M3 þ 4 and CuA very long, from L. miocenica to the subfamily Macrocerinae, but their generic assignment Cockerell 1911 and L. vertula Meunier, 1919 in having vein is unclear. Specimen I.9714 could be considered as belonging M3 þ 4 interrupted at the base. Comparison with other fossil to the tribe Orfelini of subfamily Kereplatinae on the base of species is difficult due to vague descriptions and absence of having filiform antennae. Specimens I.10226 and In.25328 illustrations. could be identified as representatives of subfamily Keroplatinae. Description. Measurements: wing 3.5 mm (preserved), 4 mm The formal description of these species would be more feasible (complete reconstructed). Wing. Sc2 distad of the middle of after revision of Cainozoic fossil Keroplatidae. Sc. S Length of Sc is 0.22 times the wing. Length of R1 is 0.61 the wing. R, R1 and R5 setose. Crossvein r-m 1.76 times Family Sciaridae Billberg, 1820 the length of R1, and 1.52 times the section M3. Section M2 is 2.35 times the section M3. Medial veins reach wing margin, Sciara gurnetensis Cockerell, 1915 M1 and M2 fork 3.41 times the section M3, M1 and M2 Pl. 7i slightly curved back. M3 þ 4 interrupted at the base, originates 1915 Sciara gurnetensis Cockerell, pp. 490–91 at the level of apex of Sc, slightly sinusoid. 1994 Sciara gurnetensis Evenhuis, p. 174 Family Keroplatidae Rondani, 1856 Holotype. USNM 61435 Subfamily Macrocerinae Rondani, 1856 Genus Macrocera Meigen, 1803 Sciara lacoei Cockerell, 1915 Pl. 7k 1803 Macrocera Meigen, p. 261. Type species: Macrocera lutea Meigen, 1803, by subsequent designation by 1915 Sciara lacoei Cockerell, pp. 491, 499, pl. 62, figs 6A,B Curtis, 1837 1994 Sciara lacoei Evenhuis, p. 174 1800 Euphrosyne Meigen, p. 16. Suppressed by International Code of Zoological Nomenclature (Op. 638, 1963, Holotype. USNM 61436 p. 339). Type species Macrocera lutea Meigen, 1803, by subsequent designation by Coquillett, 1910 Sciara protoberidis Cockerell, 1915 1863 Geneja Lioy, p. 229. Replacement name for Macrocera Pl. 7j Meigen, non Latreille, 1810. Type species Macrocera lutea Meigen, 1803, automatic 1915 Sciara protoberidis Cockerell, pp. 491–92, 499, pl. 62, 1913 Promacrocera Speiser, p. 134. Type species Promacro- fig. 7 cera interrogationis Speiser, 1913, by original designa- 1994 Sciara protoberidis Evenhuis, p. 175 tion Holotype. USNM 61437. 1938 Promacrocera Armbruster, p. 118. Preoccupied by Speiser, 1913. Type species Promacrocera archaica Superfamily Scatopsoidea Newman, 1834 Armbruster, 1938, by monotypy by Wiesław Krzemin´ski Macrocera obliqua (Cockerell, 1921) n. comb. Family Scatopsidae Newman, 1834 (Fig. 104, Pl. 8j) Scatopsidae are extremely rare in fossil materials from the 1921 Platyura obliqua Cockerell, p. 463 late Eocene sediments of the Isle of Wight. Only two specimens 1994 Platyura obliqua Evenhuis, p. 142 were found in the old collections of Brodie and Hooley, housed 2006 ‘Platyura obliqua’ Evenhuis, p. 125 in the NHM in London. These specimens were not examined previously. Holotype. NHMUK I.9657, partial insect, Brodie Collec- Recent Scatopsidae are a small family with about 350 tion; Insect Bed; late Eocene; NW Isle of Wight, UK. species of worldwide distribution. All known larvae of extant Description. Measurements: wing 3.8 mm. Wing elongate, species are saprophagous, living on decaying plant and with strong anal angle, widest distally of its middle, at the matter. level of the base of R4. Costa and Sc setose. Sc ends at Costa Scatopsidae are probably direct descendants of the extinct at the level of r-m fusion base. Sc length 0.27 times the wing. family Protoscatopsidae, known from Early to Late Jurassic R1 ends just proximally of the base of R4, its length 0.60 times (Rohdendorf 1946; Kovalev in Kalugina & Kovalev 1985). the wing. Length of R5 4 times the length of R4. Length The older fossil representatives of the Scatopsidae were known ration of sections RS1, RS2 and RS3 (¼R5) is 1:1.8:2.3. from Cretaceous ambers from Siberia and Canada (McAlpine Fusion r-m short, section M3 is equal in length to m-cu and & Martin 1969; Zherikhin & Sukacheva 1973; Cook 1981). 2.5 times the section M2. Length of M fork 5.7 times the Until now the family Scatopsidae has included 16 fossil section M3. Section M1 reduced completely. Length of basal species (Evenhuis 1994; Nel & Prokop 2004) mostly from the cell is 0.36 times the wing. M3 þ 4stronglycurvedand Eocene Baltic amber. weakened at the base. In the collection of BNHM two specimens of Scatopsidae Remarks. The combination of such characters as wide wing, are housed. large basal cell, long R1 reaching beyond the middle of the wing, vein M3 þ 4 curved and weakened at the base suggests Genus Regmoclemina Enderlein, 1936 attribution of the species to genus Macrocera. Partly preserved wing In.25331 may be conspecific. An additional seven speci- Regmoclemina haennii Krzemin´ski, n. sp. mens from the NHM collection also belong to Keroplatidae. (Figs 105, 106, Pl. 4i)

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Figures 105–106 Scatopsidae. Regmoclemina haennii Krzemin´ski, n. sp., holotype NHMUK I.9512. (105) Antenna. (106) Wing venation.

Derivation of name. This species is named in honour of Figures 107–108 Anisopodidae – wing venation. (107) Sylvicola Jean-Paul Haenni, an outstanding specialist of Scatopsidae hooleyi (Cockerell, 1921), holotype NHMUK In.24346. (108) Sylvicola problematica Krzemin´ski, n. sp., holotype NHMUK In.25675. (Muse´e national d’histoire naturelle in Neuchaˆtel, Switzerland), with thanks for the critical reading of the manuscript. Holotype. NHMUK I.9512, Brodie Collection; Insect Bed; late Eocene; NW Isle of Wight, UK. Anisopodidae are direct descendants of an extinct family Other material. NHMUK In.25255, Hooley Collection. Protorhyphidae, known from numerous fossils of Jurassic and Diagnosis. Antennae 13 segmented; vein A2 very strong and Cretaceous of Europe (Krzemin´ski & Krzemin´ska 2003). characteristically double bent. Eight fossil species of Sylvicola have been described so far Description. Very small specimens preserved with wings and from the Eocene and Miocene of Europe and North America. body. Wing length 1.3–1.8 mm; body length 1.8–2.8 mm. Recent Anisopodidae are a small family of ca.100 species Head small, only partially visible; antenna (Fig. 105) twice of two subfamilies, distributed on all continents apart from longer than width of head, composed of 13 segments; last Antarctida. The most numerous is the genus Sylvicola. flagellomere twice longer than penultimate; palps invisible. Species live usually at borders of forest, among higher vege- Thorax and legs only partially visible. Wings badly preserved, tation, loose shrubs and garden. The larvae feed on decaying only one wing of holotype is in state allowing its partial recon- detritus. struction (Fig. 106). Vein Sc very short; R1 as long as R4 þ 5; R4 þ 5 long, ending in Costa beyond fork of Mb; cross-vein r-m invisible, having been fused with Mb and R4 þ 5 into one Genus Sylvicola Harris, 1780 horizontal vein; fork of M1 þ 2 very long. M1 poorly visible Sylvicola hooleyi (Cockerell, 1921) and its shape in Fig. 106 may be inaccurately reconstructed, (Fig. 107, Pl. 4j) but in any case it is 1.5 times longer than Mb; false vein (f vn) present between Mb-M2 and Cu; A1 has complicate shape, 1921 Rhyphus hooleyi Cockerell, p. 467, fig. 27 characteristically double bent; membrane of anal part with 1994 Sylvicola hooleyi Evenhuis, p. 206 few macrosetae. Abdomen very broad; genitalia preserved only partially. Holotype. NHMUK In.24346, Hooley collection (H. 456); Shape of abdomen and genitalia suggests that both specimens Insect Bed; late Eocene; NW Isle of Wight, UK. are females, but in neither the spermatheca is visible. Additional material. NHMUK I.9063/In.17136 (part and Remarks. Both specimens are poorly preserved but have counterpart) Brodie/Smith Collections; II 2811 (part and well visible 13-segmented antennae. It is a unique feature in counterpart), collected by the Polish team, north end Thorness Scatopsidae family; most recent and fossil species have no Bay; I.8851, Brodie collection. more than 12 segments. I included this species from the late Diagnosis. Wing regularly oval, with several distinct spots; Eocene of the Isle of Wight in the genus Regmoclemina, R4 þ 5 ca3.5 times longer than Rs. because all visible characters (wing venation and macrosetae Redescription. Holotype specimen is a single, almost com- on anal lobe) are in concordance with reminding species of plete wing 5.2 mm long, with distinct dark spots, which are this genus. also preserved in remaining specimens allotted to this species. Superfamily Anisopodoidea Knab, 1912 Venation: Sc ending distinctly before fork of M1 þ 2 into M1 by Wiesław Krzemin´ski and M2; R2 þ 3 2 times longer than Rs; R4 þ 5almostfour times longer than Rs; M1 two times longer than upper margin Family Anisopodidae Knab, 1912 of d cell; Cu conspicuously wavy. Anisopodidae are rare in the Isle of Wight fossil material. Remarks. All specimens show almost no variation in wing The only taxon represented is Rhyphus hooleyi (¼Sylvicola venation, which is also characteristic of recent representatives hooleyi) described by Cockerell in 1921 on the basis of a of Sylvicola. single, very well-preserved wing originally labelled No. H. 456 (now NHMUK In.24346), and the specimen preserved on Sylvicola problematica Krzemin´ski, n. sp. two counterparts: In.17136 and I.9063. (Fig. 108, Pl. 4k)

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 TRUE FLIES FROM THE LATE EOCENE INSECT LIMESTONE OF THE ISLE OF WIGHT 49 Holotype. NHMUK In.25675, Hooley Collection; Insect Additional material. NHMUK I.8775, I.8779 (Fig. 112), Bed; late Eocene; NW Isle of Wight, UK. I.8796, I.8802, I.8892 (Fig. 113), I.8975, I.9044, I.9172, Diagnosis. Wing with basal portion widened, with only I.10114 (Fig. 109, Pl. 9g), Brodie Collection; In.17221, one small infuscate area along m-cu; R4 þ 5 about 4.5 times? In.17253 (Fig. 110, Pl. 9f ), In.17356, In.17478, Smith Collec- longer than Rs. tion; In.25276, In.25277, In.25390, In.25414, In.25744, Description. Holotype is a single wing with anal portion Hooley Collection; In.25508/I.8786 (part and counterpart), missing, 5.2 mm long, distinctly widened basally. This shape Hooley/Brodie Collections; In.64530 (¼In.64647) (Pl. 9d), is unusual for the genus Sylvicola. Membrane clear, apart Jarzembowski Collection; USNM 61443, Lacoe Collection from slight infuscation along cross-vein m-cu, and dark 7510, 7586 (both on same piece of rock as holotype); stigma. Venation: terminal portion of Sc not preserved, but CAMSM X.50140.8 (TN57). obviously must have ended opposite or a little before fork of Diagnosis. As in Cockerell (1915) with the following addi- M1 þ 2; R2 þ 3 more than 2.5 times longer than Rs; M1 two tions: antennae with spine-like tip and short basal segment; times longer than upper margin of d cell; Cu conspicuously lacks scutellar spines; postscutellum projects further than the wavy. scutellum. Remarks. The shape of wing is unusual for the genus Redescription. Head oblique in lateral view and median Sylvicola and may indicate a new subgenus. Unfortunately, antennal segments inflated (Fig. 109); thorax entirely dark in other body parts are missing; therefore, the new species is colour; postscutellum large for genus; abdomen more elongate tentatively allotted to Sylvicola, on the basis of similar wing and slender than typical in extant Odontomyia spp.; where venation. wing preservation is exceptional, membrane has a fine wrinkled Conclusions. Usually Anisopodidae are rather rare in fossil texture (Pl. 9f); total length of individual specimens varies materials. Five specimens representing two species show that between 9–14 mm. Anisopodidae were abundant on Isle of Wight and they are Remarks. Cockerell’s original drawing of the holotype wing similar to Baltic amber species. is inaccurate in the shape of the discal cell. Rather than being nearly parallel sided (in Cockerell 1915) it tapers distally Suborder Brachycera Macquart, 1834 (Fig. 111). His discussion of the colour patterning is based on what was seen on the inside surface of the few specimens Superfamily Latreille, 1802 available to him, so do not apply to the species external by David B. Nicholson patterning as a whole. What is seen varies with fidelity of preservation and how the rock fractures (as can be seen with Family Stratiomyidae Latreille, 1802 parts and counterparts) so precise description is not possible with any certainty. Suffice to say it is typical for larger Two species of fossil soldierfly have been described previ- Odontomyia species, broadly mimicking hymenopteran patterns ously from this deposit – Stratiomys brodiei Cockerell 1915 (Pl. 9d) and generally similar to the extant Odontomyia and Protoberis obliterata Cockerell 1915. It was suggested by ornata. Collin in Marshall & Staley (1931) that S. brodiei should be Without knowledge of the antennae, no character is pre- placed in Odontomyia based on the presence of a short basal served in the specimens which can be used to distinguish antennal segment. This assertion is confirmed here. Sixteen between Stratiomys and Odontomyia. Molecular phylogenies larval specimens (Pl. 10f ) attributable to the aquatic Strat- have shown Stratiomys and Odontomyia to be sister genera iomyini are present in the NHM collection but can only be within the (Brammer & Dohlen 2007) and tentatively assigned to Odontomyia brodiei. P. obliterata is a differences in the wing venation, when present, are subtle. It bibionid (see above, Bibionidae) and is not considered here. has been commented that the size variation seen in the fossils A brief review of fossil Stratiomyidae is provided in Huang & (see redescription) suggest that more than one species may be Lin (2007). A new member of the subfamily is present (Collin in Marshall & Staley 1931; A. Ross 2006, pers. described and named. comm.). However, this need not be the case. Having viewed the NHM holdings of world and UK Odontomyia, the varia- Subfamily Stratiomyinae Latreille, 1802 tion seen in the fossils is not unusual for the genus. In extant Odontomyia the discal cell shape is fairly consistent within Tribe Stratiomyini Latreille, 1802 each species (pers. obs.). In O. brodiei the angle in the poste- Genus Odontomyia Meigen, 1803 rior face delimited by the branching of M3 is most often 170– 180, but some specimens have markedly more acute angles Type species. Musca hydroleon Linnaeus, 1758, by subse- (Figs 116–135); for example, I8779, Brodie Collection, which quent designation of Westwood (1840). has an angle of 129 (Fig. 117). Together with the lack of crossvein m-cu in specimen I.8892, Brodie collection (Figs Odontomyia brodiei (Cockerell, 1915) 124, 125), this provides some support for the existence of (Figs 109–113, 116–135, Pl. 9d–g) more than one species, although it remains possible these are simply aberrant specimens. A statistical analysis of the discal 1915 Stratiomys brodiei Cockerell, p. 493, pl. 62, fig. 8 cell shapes could provide further information, although past 1931 Odontomyia brodiei (Cockerell); Collin in Marshall & attempts to apply statistics to dipteran wing venation for the Staley, p. 39 purpose of taxonomic identification have proven inconclusive 1994 Odontomyia brodiei (Cockerell); Evenhuis, p. 308 (S. Wedmann, pers. comm. 2006). Collin in Marshall & Staley (1931) noted that the lack of Holotype. USNM 61443, Lacoe Collection 7507 (Fig. 111, scutellar spines is not common for the genus but pointed out Pl. 9e) comprising the abdomen, partial thorax and partial that some species do share the trait (O. mutica, O. ngriventris, left wing showing some venation; Insect Bed; late Eocene; O. fallax, O. inermis). Based on the details of the colour NW Isle of Wight, UK. patterning, wing venation and antenna, he concluded that

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Figures 109–115 Stratiomyidae. (109)–(113) Odontomyia brodiei (Cockerell, 1915): (109) NHMUK I.10114 antenna; (110) NHMUK In.17253 wing venation; (111) USNM 61443 holotype; (112) NHMUK I.8779 wing venation showing acute angled discal cell; (113) NHMUK I.8892 wing venation lacking m–cu. (114), (115) Palaeoberidops barkeri Nicholson, n. gen., n. sp.: (114) NHMUK I.9866(3) holotype part; (115) NHMUK I.9718(3) holotype counterpart.

O. brodiei must be the ‘Oligocene’ ancestor of modern Odonto- Derivation of name. Greek, palaeo, ancient, and beridops, myia. Fossil and molecular data indicates the divergence the genus to which it bears a close resemblance. between Odontomyia and Stratiomys occurred 25–35 Ma Type species. Palaeoberidops barkeri n. gen., n. sp. by (Brammer & Dohlen 2007). While the uppermost Eocene age monotypy. of the Bembridge Marls open the possibility that Diagnosis. As for the type and only known species. O. brodiei could be the most recent common ancestor to Stratiomys and Odontomyia, the lack of scutellar spines Palaeoberidops barkeri Nicholson, n. gen., n. sp. (which are nearly ubiquitous in both genera today) makes it Figs 114, 115, Pl. 9h, i unparsimonious to assume this to be the case, or that it is a direct ancestor of all modern Odontomyia. Sixteen stratiomyid larvae are held in the NHM collections, Derivation of name. In honour of Dr Michael Barker in his provisionally assigned to the subfamily Stratiomyinae. Larvae retirement from the School of Earth and Environmental in this subfamily are aquatic and some are known to be able Sciences, University of Portsmouth, UK. to withstand highly saline water (James 1981), so it is possible Holotype. NHMUK I.9718/I.9866(3) (part and counter- that these were living in the , though more likely to be part), Brodie Collection, incomplete single wing Insect Bed; that they were washed in by streams. late Eocene; NW Isle of Wight, UK. Diagnosis. Absence of M3 and m-cu, with CuA1 originating at the point where CuA meets the discal cell; R strongly Subfamily Beridinae Westwood, 1838 2+3 curved anteriorly; width of discal cell two thirds the length; Genus Palaeoberidops, n. gen. length of discal cell less than half that of cell r1; wing apex

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Figures 116–135 Stratiomyidae: Odontomyia brodiei. Representations of the shape of the discal cell in fossil specimens, where preserved. For ease of comparison all cells have been made roughly the same size and oriented with the proximal wall of the cell vertical and some images reversed so all appear as on a right wing. (116) NHMUK I.8775. (117) NHMUK I.8779. (118) NHMUK I.8796. (119) NHMUK I.8802. (120) NHMUK I.8892. (121) NHMUK I.8975. (122) NHMUK I.9044. (123) NHMUK I.9172. (124) NHMUK I.17221. (125) NHMUK In.17253. (126) NHMUK In.17356. (127) NHMUK In.17478. (128) NHMUK In.25276. (129) NHMUK In.25277. (130) NHMUK In.25390. (131) NHMUK In.25414. (132) NHMUK In.25508. (133) NHMUK In.25744. (134) CAMSM X.50140.8. (135) USNM 61443 (Lacoe 7507).

not visible but trajectories suggest R4 less than half the length curved at base of fork, otherwise straight; pterostigma black; of R5;R4+5 substantially thicker than all other veins; pteros- branches of medial vein (M1 and M2) fade distally; anterior tigma present in cell r1 and possibly extends into subcostal wing margin not completely visible. Preserved section of the cell (sc). wing 3.8 mm long. Description. Single partial wing with colouration preserved Remarks. Initial comparison to miocenica James, in veins. Preservation fades in from proximal end of basal cells 1937, from the Eocene Florissant Beds, USA, shows P. barkeri through nearly to the apex of the wing; costal vein from has a much more strongly curved R2+3, resulting in less crowded anterior end of R1 out towards apex; CuA2 and relatively radial cells. Comparison with extant species of Beris (e.g., B. short A1 join more anteriorly than is commonly seen in the fuscipes, B. chalybata, B. geniculata, B. morisii and B. vallata) Subfamily; CuA2 short and slightly recurved; R4 only slightly shows P. barkeri has a markedly less elongate discal cell, with

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Plate 9 Bibionidae and Stratiomyidae. (a) Plecia sp., NHMUK In.25249. (b) Penthetria sp., NHMUK In.25246. (c) Plecia sp., NHMUK In.17230. (d–g) Odontomyia brodiei (Cockerell, 1915): (d) NHMUK In.64530 (¼ In.64647), dorsal view showing abdominal colour patterning; (e) holotype USNM 61443 (Lacoe Collection 7507); (f) NHMUK In.17253, showing exceptional wing preservation; (g) NHMUK I.10114, lateral view showing full antenna. (h, i) Palaeoberidops barkeri Nicholson, n. gen., n. sp., holotype: (h) NHMUK I.9866(3), part; (i) I.9718(3), counterpart.

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Figures 136–137 and Phoridae. (136) Hybotidae, NHMUK I.8981. (137) Phoridae, NHMUK I.9488.

a shape more like that seen in the tribe Stratiomyini. With the Holotype.In.24349 exception of Beridops spp., all other genera in the Beridinae have the CuA1 originating on the discal cell and the discal Chrysopilus stigmaticus Cockerell, 1921 cell markedly elongate. Beridops differs from Palaeoberidops (Pl. 10e) barkeri in that the discal cell shows some elongation and is at 1921 Chrysopilus stigmaticus Cockerell, p. 471, fig. 36 (Leptidae) least two-thirds the length of cell r1. 1994 Chrysopilus stigmaticus Evenhuis, p. 292 The following taxa have been previously described or newly recognised from the Insect Limestone, but have not been Holotype. NHMUK In.24350. studied for this project. Family Tabanidae Latreille, 1802 Family Bombyliidae Latreille, 1802 Tabanus vectensis (Cockerell, 1921) (Pl. 10g) Systropus acourti Cockerell, 1921 (Pl. 10a) 1921 Chrysops vectensis Cockerell, p. 472, fig. 37 1994 Tabanus vectensis Evenhuis, p. 289 1921 Systropus acourti Cockerell, p. 469, fig. 32 1973 Systropus acourti Hull, p. 59 Holotype. NHMUK In.24351. 1994 Systropus acourti Evenhuis, p. 336 Family Empididae Latreille, 1804 Holotype. NHMUK In.17208/In.17293. Specimens NHMUK I.8981, I.9289, I.9371, I.9401, I.9465, Family Asilidae Latreille, 1802 I.9730, I.10275, I.10372, I.10378 (Pl. 10h), In.17199, In.25288, In.25264, In.43435. Asilus gurnetensis Cockerell, 1921 (Pl. 10b) Family Dolichopodidae Latreille, 1809 1921 Asilus gurnetensis Cockerell, p. 470, fig. 33 1962 Asilus gurnetensis Hull, p. 24 Specimens NHMUK I.8443, I.10260, I.8666, I.8850, I.8930, 1994 Asilus gurnetensis Evenhuis, p. 324 I.8974, I.9080, I.9094, I.9328, I.9391, I.9765, I.9826, In.17110, In.17488, In.20534, In.24635, In.25173, In.25224, In.25233 Holotype. NHMUK In.24348. (Pl. 10i), In.25262, In.25273, In.25348, In.25377, In.25397, In.25438, In.25506, In.25732. Proctacanthus fractus Cockerell, 1921 (Pl. 10c) Family Hybotidae Meigen, 1820 1921 Proctacanthus fractus Cockerell, p. 470, fig. 34 1962 Proctacanthus fractus Hull, p. 24 Specimen NHMUK I.8981 (Fig. 136) 1994 Proctacanthus fractus Evenhuis, p. 327 Family Syrphidae Latreille, 1802 Holotype. NHMUK In.24347. Specimens NHMUK In.17355, In.20551, In.24809 (Pl. 10j), Family Rhagionidae Latreille, 1802 In.25261, In.25264. Chrysopilus anglicus Cockerell, 1921 Family Phoridae Curtis, 1833 (Pl. 10d)

1921 Chrysopilus anglicus Cockerell, p. 471, fig. 35 (Leptidae) Specimens NHMUK I.9488, I.9512, In.20534b (Fig. 137). 1994 Chrysopilus anglicus Evenhuis, p. 292

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Plate 10 Bombyliidae, Asilidae, Rhagionidae, Stratiomyidae, Tabanidae, Empididae, Dolichopodidae, and Syrphidae. (a) Systropus acourti Cockerell, 1921 (Bombyliidae), holotype NHMUK In.17208. (b) Asilus gurnetensis Cockerell, 1921 (Asilidae), holotype NHMUK In.24348. (c) Proctacanthus fractus Cockerell, 1921, holotype NHMUK In.24347. (d) Chrysopilus anglicus Cockerell, 1921 (Rhagionidae), holotype NHMUK In.24349. (e) Chrysopilus stigmaticus Cockerell, 1921, holotype NHMUK In.24350. (f ) Odontomyia brodiei? (Cockerell, 1915) (Stratiomyidae) larva, NHMUK II.2978, A. Yule Coll. (g) Tabanus vectensis (Cockerell 1921), holotype NHMUK In.24351. (h) Empididae, NHMUK I.10378. (i) Dolichopodidae, NHMUK In.25233. (j) Syrphidae, NHMUK In.24809.

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Table 3 Diptera known from Bembridge Marls.

Tipulidae ?Bibio gurnetensis Cockerell, 1917a Brachypremna gurnetensis (Cockerell, 1921) ?Bibio oligocenus Cockerell, 1917a Ischnotoma (Ischnotoma) vasifera (Cockerell & Haines, 1921) Bibiodes confluens (Cockerell, 1915), n. comb. Leptotarsus (Longurio) fragmentatus Krzeminski, n. sp. Dilophus andrewrossi Nel, Colomb & Waller, n. sp. Leptotarsus (Longurio) wegiereki Krzeminski, n. sp. Penthetria indet. Leptotarsus (Macromastix) cladoptera (Cockerell & Haines, 1921) Plecia acourti Cockerell, 1921 Tipula (s. lato) acourti Cockerell, 1921 Keroplatidae Tipula (s. lato) gardneri Cockerell, 1917a Macrocerinae: Macrocera obliqua (Cockerell, 1921), n. comb. Tipula (s. lato) limiformis Cockerell, 1915 Keroplatinae: Orfelini Tipula (s. lato) anglicana Krzeminski, n. sp. Mycetophilidae Tipulomorpha indet. Acnemia simplex Cockerell, 1921 Paltostomopsis ciliata Cockerell, 1915 Aglaomyia vectis Blagoderov, n. sp. Cylindrotomidae Azana cockerelli Blagoderov, n. sp. Cyttaromyia rossi Krzeminski, n. sp. ?Coelosia virgata (Cockerell, 1921), n. comb. Limoniidae Dziedzickia oligocenica Blagoderov, n. sp. Cheilotrichia (Cheilotrichia) duplicata Krzemin´ski, n. sp. Leia gurnardensis Blagoderov, n. sp. Cheilotrichia (Empeda) ferruginea (Cockerell, 1921) Mycetophila vectensis Cockerell, 1915 Cheilotrichia (Empeda) hyalina (Cockerell, 1921) Mycomya hoolei Blagoderov, n. sp. Cheilotrichia (Empeda) szwedoi Krzemin´ski, n. sp. Mycomya oblita Cockerell, 1921 Dactylolabis (Dactylolabis) spiloptera (Cockerell, 1921), n. comb. Palaeoempalia saxea Blagoderov, n. sp. Dicranomyia (Dicranomyia) aliena (Cockerell, 1921), n. comb. ‘Rymosia’ edwardsi Cockerell, 1921 Dicranomyia (Dicranomyia) brodiei (Cockerell, 1917a) ‘Rymosia’ ferruginea Cockerell, 1921 Dicranomyia (Dicranomyia) excavata Cockerell & Haines, 1921 Rymosia grisea Cockerell, 1921 Dicranomyia (Dicranomyia) fasciata Krzemin´ski, n. sp. ‘Rymosia’ rufescens Cockerell, 1921 Dicranoptycha staryi Krzemin´ski, n. sp. Sciaridae Gonomyia (Gonomyia) indecisa Cockerell & Haines, 1921 Sciara protoberidis Cockerell, 1915 Gurnardia corami Krzemin´ski, n. gen., n. sp. Sciara gurnetensis Cockerell, 1915 Gymnastes (Paragymnastes) fasciatipennis Cockerell, 1921 Sciara lacoei Cockerell, 1915 Helius (Helius) edmundi Krzemin´ski, n. sp. Scatopsidae Helius (Helius) popovi Krzemin´ski, n. sp. Regmoclemina haennii Krzemin´ski, n. sp. Helius (Helius) vectensis (Cockerell, 1915), n. comb. Anisopodidae Ilisia (Lunaria) incognita (Cockerell, 1921), n. comb. Sylvicola hooleyi (Cockerell, 1921) Limnophila (Limnophila) cyclospila Cockerell, 1921 Sylvicola problematica Krzemin´ski, n. sp. Limnophila (Limnophila) deleta Cockerell, 1921 Rhagionidae Limonia spilota (Cockerell, 1921) Chrysopilus anglicus Cockerell, 1921 Orimarga (Orimarga) lenae Krzemin´ski, n. sp. Chrysopilus stigmaticus Cockerell, 1921 Pilaria hooleyi Krzemin´ski, n. sp. Tabanidae Pilaria volodii Krzemin´ski, n. sp. Chrysops vectensis Cockerell, 1921 Pseudolimnophila (Pseudolimnophila) disjunctula (Cockerell & Haines, Stratiomyidae 1921), n. comb. Odontomyia brodiei (Cockerell, 1915) Styringomyia concinna (Cockerell, 1917a) Palaeoberidops barkeri Nicholson, n. gen., n. sp. Symplecta (Psiloconopa) gurnetensis Krzemin´ski, n. sp. Bombyliidae Thaumastoptera undulata (Cockerell & Haines, 1921), n. comb. Systropus acourti Cockerell, 1921 Trentepohlia (Mongoma) cruciferella (Cockerell, 1917a) Asilidae Trentepohlia (Mongoma) pallescens (Cockerell, 1921) Asilus gurnetensis Cockerell, 1921 Psychodidae Proctacanthus fractus Cockerell, 1921 Pericoma primaeva (Cockerell, 1915), n. comb. Empididae (undescribed, NHM collection) Wightipsychoda leucospila (Cockerell, 1921), n. comb. Dolichopodidae (undescribed, NHM collection) Dixidae Hybotidae (undescribed, NHM collection) Dixella priscula (Cockerell, 1921), n. comb. Syrphidae (undescribed, NHM collection) Culicidae Phoridae (undescribed, NHM collection) Coquillettidia cockerelli (Edwards, 1923), n. comb. Otitidae Culex protorhinus Cockerell, 1915 Stenomyites fuscipennis Cockerell, 1915 Culex vectensis Edwards, 1923 Lauxaniidae indet. (Zlobin, 2007) Ochlerotatus protolepis (Cockerell, 1915), n. comb. Agromyzidae indet. (Zlobin, 2007) Chironomidae Anthomyzidae Chironominae: Chironomini indet. ‘Ephydra’ sepulta Cockerell, 1915 Orthocladiinae indet. ‘Ephydra’ oligocena Cockerell, 1915 Tanypodinae indet. Chloropidae Ceratopogonidae Hippelates brodiei Cockerell, 1915 Dasyhelea indet. Heleomyzidae indet. (Zlobin, 2007) Palpomyia edwardsi Cockerell, 1921 Ephydridae Stilobezzia indet. Protoscinis perparvus Cockerell, 1917a Simuliidae ‘Sphaerocera’ sepultula Cockerell, 1915 Simuliidae gen. et sp. indet. Bibionidae Bibio obliteratus (Cockerell, 1915), n. comb. ?Bibio extremus Cockerell, 1921

Downloaded from https://www.cambridge.org/core. Chalmers Tekniska Högskola, on 06 Oct 2019 at 16:48:14, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S1755691018000464 56 WIESŁAW KRZEMIN´ SKI ET AL. 3. Diptera fauna and habitat of the insect bed 4. Acknowledgements SW wants to thank Dr Andrew Ross (London) and Prof. Dr A list of Diptera known up to date from Insect Limestone is Rainer Willmann (Go¨ttingen) for their support of this re- provided in Table 3. In total, 102 species and 32 families are search, Theresa Howard (London) for access to extant simu- recorded from the locality. Among the Diptera from the Isle liid pupae and INTAS (Project-No. 03-51-4367) for financial of Wight the most abundant are those that depend directly on support. D.N. extends special thanks to Andrew Ross, Wieslaw the water habitat. Thus most abundant are the Limoniidae Krzemin´ski, Vladimir Blagoderov, David Martill, Erica (135 specimens), Chironomidae (170 specimens), Culicidae McAlister and Michael Barker. RS is much indebted to Dr A. (140 specimens), Psychodidae (39) and Stratiomyidae (41); rare Ross, for arranging the loan of materials and his kind hospital- are the Dixidae (6 specimens) and Simuliidae (one specimen). ity during his visit to England; to Dr A. Borkent of Salmon Surprisingly numerous are the Culicidae, which are scarcely Arm, Canada, Dr N. Evenhuis of Bernice P. Bishop Museum, represented in older sediments and in Baltic amber (Eocene) Honolulu, Hawaii and Dr W. L. Grogan of Salisbury State (Szadziewski & Szadziewska 1985; Szadziewski 1998; Podenas University for their advice and discussions on synonymy and 1999; Wichard et al. 2009). The Isle of Wight is the oldest nomenclatural problems. locality with so rich representation of culicid adults. Culicidae from the Isle of Wight belong to three extant genera of world- wide distribution (Coquillettidia, Ochlerotatus and Culex), whose extant species are common inhabitants of shallow reservoirs of stagnant water. Larvae and pupae of the genus 5. References Coquillettidia live among water plants and take air from plant Adler, P. H. and Currie, D. C. & Wood, D. M. 2004. The black flies tissues. (Simuliidae) of North America. Ithaca: Cornell University Press. Some of the Tipulidae (represented by 32 specimens in the Adler, P. H. & Crosskey, R. W. 2011. World blackflies (Diptera: Simuliidae): a comprehensive revision of the taxonomic and fauna) also prefer semiaquatic habitats or live directly in geographical inventory. http://entweb.clemson.edu/biomia/pdfs/ water, as several species of Tipula and Ischnotoma (Alexander blackflyinventory.pdf (accessed 21 December 2011). 1944, 1971). Alexander, C. P. 1919. The crane-flies of . Part I. 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MS received 28 March 2014. Accepted for publication 31 July 2017

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