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1 June 2011 The First Gondwanan Epimastax from the Lopingian of KwaZulu-Natal, South Africa (Insecta: Palaeomanteida = Miomoptera: Permosialidae)
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Abstract

Epimastax hesterae sp. n. is described from the Lopingian deposits of the Tarkastad Subgroup of the Beaufort Group. All described congeners are known from the Lower and Middle Permian (Sakmarian, Kungurian and Kazanian) of Central and East Europe.

INTRODUCTION

The Permian genus Epimastax Martynov, 1928 has a rather complicated taxonomic history. It was described from the Biarmian (= Middle Permian) (Lower Kazanian) deposits of eastern European Russia as a type of the family of its own within the order Protoblattodea next to the family Oryctoblattinidae (= Blattinopseidae) (Martynov 1928). This treatment was adopted by Sharov (1962). The second species E. celer Kukalová, 1965 was described from the Cisuralian (= Lower Permian) (Sakmarian) of Central Europe in the same family, at that time attributed to the order Protorthoptera (Kukalová 1965). This attribution was followed by Carpenter (1992). The third species from the Middle Permian of north European Russia was described under the name Sindomioptera soyanensis Rasnitsyn, 1977 in the family Permosialidae (order Miomoptera = Palaeomanteida). Sindomioptera was shortly afterwards synonymized under Epimastax (Rasnitsyn 1980). Later Rasnitsyn (in Rasnitsyn et al. 2004) transferred the genus from the Permosialidae to Palaeomanteidae but then he returned it back to Permosialidae (Rasnitsyn & Aristov, in press). The present description of a new finding in the Lopingian of South Africa considerably extends both the stratigraphical and geographical range of the genus.

MATERIAL AND METHODS

The fossil under description was collected by the junior author in a quarry in the town of Bulwer in KwaZulu-Natal, South Africa. It is kept in the KwaZulu-Natal Museum, Pietermaritzburg, South Africa (NMSA). The deposits are identified as the Normandien Formation, Tarkastad Subgroup, Beaufort Group, which is considered the uppermost in the South African Permian (Dijk 1997; Gastaldo et al. 2005). The stratigraphy and palaeoenvironment of this locality are discussed by Gastaldo et al. (2005). The photograph was taken by DEvD using a Nikon D70 camera body mounted on Nikon PB4 bellows with a Nikon E2 ring to permit wide-open focussing of a Nikkormat 50 mm lens. The line drawing is prepared by APR based on the photograph and using CorelDraw 12 software.

TAXONOMY

Order Palaeomanteida (= Miomoptera)
Family Permosialidae Martynov, 1928
Genus Epimastax Martynov, 1928
Epimastax hesterae sp. n.
Figs 1, 2

  • Etymology: The species name is in memory of Mrs Hester Heese-Van Dijk, who collected fossils, including insects, in Bulwer and at other sites in the South African Permian.

  • Description:

    Forewing length 6.8 mm as preserved, width 3.5 mm. Forewing convex, with fore margin apparently convex, R, RS, M1 and, to much lesser extent, anal veins inflated. SC short (only reaching level of M and CuA forks), almost straight, with three oblique, spaced, almost straight, visible preapical branchlets (probably only one or none missing). R slightly sigmoid, with oblique fore branchlets (of which six visible), basal one very long (at least half as long as SC), slightly sinuate, followed by slightly bent, gradually shortening ones. RS apparently connected to R with long, oblique, sinuate r—rs crossvein, and with three branches preserved, first forking well beyond SC apex. M and CuA forking well before RS, with forks long, parallel-sided. Clavus long (reaching or slightly surpassing level of SC apex), wide, with four simple, parallel anal veins visible. Crossveins (other than r—rs) spaced as preserved, subvertical, rarely causing distinct bends of main veins. Colour pattern absent or not preserved.

  • Comparison: Strikingly different from all congeners in having R with a very long basal fore branch and with long, sinuate r—rs crossvein.

  • Holotype: NMSA 2737, almost complete but somewhat damaged forewing, with fore and hind margins partially, and apical margin entirely, missing, a sub-basal portion of membrane lost, and the fore margin of clavus overlapping posterior margin of remigium. SOUTH AFRICA: KwaZulu-Natal: Bulwer Quarry (29.79953°S:29.78657°E); Lopingian, Lower Beaufort Group, Normandien Formation (Balfour Formation equivalent).

  • Remark: A characteristically sinuate, long, oblique r—rs crossvein is otherwise known in some species of Permonka Riek, 1973 (Rasnitsyn 1977). This similarity might indicate a relationship between the two genera.

  • Figs 1, 2.

    Epimastax hesterae sp. n., holotype NMSA 2737: (1) left forewing, laterally inverted; (2) venation details. Venation symbols are standard.

    f01_207.jpg

    ACKNOWLEDGEMENTS

    For APR, this study is supported in part by the Programme ‘Biosphere Origin and Evolution of Geo-Biological Systems’ of the Presidium of the Russian Academy of Sciences, and the Russian Foundation for Basic Research grant no. 09-04-01241.

    REFERENCES

    1.

    F.M. Carpenter 1992. Superclass Hexapoda. In : R.C. Moore et al., eds, Treatise on Invertebrate Paleontology. Pt. 4: Arthropoda, Vols 3, 4. Boulder, Col. & Lawrence, Kan.: Geological Society of America & University of Kansas. Google Scholar

    2.

    D.E., van Dijk . 1997. Insect faunas of South Africa from the Upper Permian and the Permian/Triassic boundary. Palaeontologica Africana 34: 43–48. (erratum with same vol. & pp. published in 1998) Google Scholar

    3.

    R.A. Gastaldo , R. Adendorff , M. Bamford , C.C. Labandeira , J. Neveling & H. Sims 2005. Taphonomic trends of macrofloral assemblages across the Permian—Triassic boundary, Karoo Basin, South Africa. Palaios 20 (5): 479–497. Google Scholar

    4.

    J. Kukalová 1965. Permian Protelytroptera, Coleoptera, and Protorthoptera (Insecta) of Moravia. Sbornik Geologickych Ved, Paleontologie 6: 61–95, 8 pls. Google Scholar

    5.

    A.V. Martynov 1928. Permian fossil insects of North-East Europe. Trudy Geologicheskogo muzeya Academii nauk SSSR [Transactions of the Geological Museum, Academy of Sciences of USSR] 4: 38–118, 19 pls. Google Scholar

    6.

    A.P Rasnitsyn 1977. New Paleozoic and Mesozoic insects. Paleontologicheskiy zhurnal (1): 64–77. (in Russian, translated into English in Paleontological Journal (1977) 1978 11: 60–72.) Google Scholar

    7.

    A.P Rasnitsyn 1980. Origin and evolution of Hymenoptera. Transactions of the Paleontological Isnstitute, Academy of Sciences of USSR 174: 1–192. (in Russian). Google Scholar

    8.

    A.P. Rasnitsyn & D.S. Aristov In press. New fossil insects from the Middle and Upper Permian of European Russia. Paleontological Journal.  Google Scholar

    9.

    A.P. Rasnitsyn , D.S. Aristov , A.V. Gorokhov , J.M. Rowland , N.D. Sinitshenkova & I.D. Sukatsheva 2004. Important new insect fossils from Carrizo Arroyo and the Permo-Carboniferous faunal boundary. In : S.G. Lucas & K.E. Ziegler , eds, Carboniferous—Permian transition. New Mexico Museum of Natural History and Science Bulletin 25: 215–246. Google Scholar

    10.

    A.G. Sharov 1962. Otryad [Ordo] Protoblattodea. In : B.B. Rohdendorf , ed., Osnovy paleontologii. Chlenistonogie. Trakheynye i khelitserovye. Moscow: Academy of Sciences of the USSR, pp. 116–118. (in Russian; English translation: Sharov, A.G. 1991. Order Protoblattodea. In: Rohdendorf, B.B., ed., Fundamentals of paleontology. Arthropoda, Tracheata, Chelicerata. Vol. 9. Washington, DC: Smithsonian Institute Libraries and The National Science Foundation, pp. 146–150.) Google Scholar
    A. P. Rasnitsyn and D. E. van Dijk "The First Gondwanan Epimastax from the Lopingian of KwaZulu-Natal, South Africa (Insecta: Palaeomanteida = Miomoptera: Permosialidae)," African Invertebrates 52(1), 207-209, (1 June 2011). https://doi.org/10.5733/afin.052.0110
    Published: 1 June 2011
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