New and poorly known grylloblattids (Insecta: Grylloblattida) from the Lopingian of the Lebombo Basin, South Africa.
A new genus and species of the grylloblattid family Chaulioditidae,
Iphikozulu kwayayaensis Aristov & Mostovski, gen. et sp. n., is
described from the Lopingian locality of KwaYaya in KwaZulu-Natal, South
Africa. This is the first record of the Chaulioditidae in Gondwanan
deposits. The genera Triadosialis Handlirsch, 1906, Protomia Aristov,
2004 and Miralioma Aristov, 2004 are transferred to the family
Chaulioditidae, and the genus Kargalella Martynov, 1937 is transferred
to the Liomopteridae. Neoliomopterum picturatum Riek, 1976 from the
Lopingian locality at Emakwezini Railway Station in KwaZulu-Natal is
redescribed and transferred from Grylloblattida incertae sedis to the
family Liomopteridae. The subfamily Kargalellinae Aristov, 2004 is
synonymised under Liomopteridae Sellards, 1909.
KEY WORDS: Insecta, Grylloblattida, Chaulioditidae, Liomopteridae, Permian, Lopingian, Gondwana, new taxa, new synonymy.
(Identification and classification)
|Publication:||Name: African Invertebrates Publisher: The Council of Natal Museum Audience: Academic Format: Magazine/Journal Subject: Zoology and wildlife conservation Copyright: COPYRIGHT 2009 The Council of Natal Museum ISSN: 1681-5556|
|Issue:||Date: Dec, 2009 Source Volume: 50 Source Issue: 2|
|Topic:||Event Code: 310 Science & research|
|Geographic:||Geographic Scope: South Africa Geographic Code: 6SOUT South Africa|
Grylloblattids have been found at a number of Lopingian (Upper Permian) localities in the north-eastern and eastern parts of the main Karoo Basin and in the Lebombo Basin (van Dijk 1997; Van Dijk & Geertsema 1999; Geertsema et al. 2002). A single representative of Megakhosaridae, Miolopterina tenuipennis Riek, 1976, is known from the Bulwer locality (Beaufort Group, Normandien Formation; previously known as the Estcourt Formation). The Emakwezini Railway Station locality near Empangeni (Beaufort Group, Emakwezini Formation; Normandien Formation equivalent) has yielded Neoliomopterum picturatum Riek, 1976. Two liomopterids, Mioloptera stuckenbergi Riek, 1973 and Mioloptoides andrei Riek, 1976, have been recorded from the Lidgetton locality (Beaufort Group, Normandien Formation) (van Dijk 1997). A nymph of uncertain affinity Thaumatophora pronotalis Riek, 1976, has been described from Haakdoornfontein (Ecca Group, Hammanskraal Formation; Vryheid Formation equivalent) (Riek 1976a). An incomplete grylloblattid forewing has been found recently at a locality near Colenso (Prevec et al. 2009). The Mooi River locality (Beaufort Group, Normandien Formation) has yielded the richest insect fauna, including representatives of four species in four genera, Mioloptoides andrei Riek, 1976, Mioloptera stuckenbergi Riek, 1973 (Liomopteridae), Miolopterina tenuipennis Riek, 1976 (Megakhosaridae) and Liomoptoides similis Riek, 1973 (Grylloblattida incertae sedis) (van Dijk 1997). The Mooi River locality is also remarkable for the high proportion of grylloblattids that have been collected. Grylloblattida represent 35% of the insect fauna, whereas in Russian and Middle Asian localities they comprise 5-7% of all insect remains.
Thus, the grylloblattid fauna of the South African Lopingian is represented by two families: the dominant Liomopteridae (63% of all grylloblattids) and the considerably rarer Megakhosaridae (22%). The family Chaulioditidae, being widely distributed in the Tatarian (= Lopingian, or Upper Permian) of Russia, has so far been unknown in Gondwanan deposits.
[FIGURE 1 OMITTED]
A new representative of the Chaulioditidae, Iphikozulu kwayayaensis gen. et sp. n., is herewith described from the locality of KwaYaya in KwaZulu-Natal. In addition, Neoliomopterum picturatum from the contemporaneous Emakwezini Railway Station locality is transferred from Grylloblattida incertae sedis to the family Liomopteridae.
To summarise, the composition of the South African grylloblattid fauna is typically Lopingian, with dominating Liomopteridae, and rare Megakhosaridae and Chaulioditidae. The only difference is a high ratio (35 %) of grylloblattids to other insect taxa.
MATERIAL AND METHODS
The holotype of Iphikozulu kwayayaensis gen. et sp. n. was found in fine-grained, olive-grey mudstone in a railway cutting approx. 25 km west of Empangeni along the R34 and approx. 200 m west of the KwaYaya railway siding (28[degrees]41.915'S:31[degrees]40.730'E) (Fig. 1). The holotype is housed at the Natal Museum (NMSA).
Geological setting and palaeoenvironment
The fossiliferous deposits at KwaYaya lie within the upper part of the Emakwezini Formation, Adelaide Subgroup, Beaufort Group, Karoo Supergroup. The Emakwezini Formation was deposited in the Lebombo Basin, and crops out in a narrow strip just inland of, and parallel to, the north-eastern KwaZulu-Natal coastline. The formation is considered to be lithostratigraphically equivalent to the Normandien Formation (incorporating the previously recognised Estcourt Formation) in the north-eastern and eastern parts of the main Karoo Basin (e.g., Johnson et al. 2006). A review of the Emakwezini Formation is provided elsewhere (Bordy & Prevec 2008).
Bordy and Prevec (2008) interpreted the autochthonous nature of the deposits at KwaYaya, together with various associated sedimentary features, as indicative of deposition in a floodplain setting in the immediate vicinity of a broad, shallow, gently meandering channel in the overbank area of a large fluvial system. According to general climatic reconstructions (Chumakov & Zharkov 2003), this locality was situated within the southern temperate semiarid belt of middle latitudes. Locally, the Emakwezini Formation appears to have been deposited under cool, humid, perennially moist conditions. The latter assumption is supported by records of grylloblattids, which are known to be associated with cold and moist environments from their early days until the present (e.g., Shcherbakov 2008) contrary to the statement that they are indicative of warmer and drier conditions (Geertsema et al. 2002).
The KwaYaya locality has yielded a glossopterid-dominated palaeoflora, containing multiple elements typical of Late Permian floras from the main Karoo Basin of South Africa (e.g., Lacey et al. 1975; Anderson & Anderson 1985). These include at least five morphotypes of Glossopteris leaves and the glossopterid ovuliferous organs Lidgettonia africana, Rigbya arberioides and Plumsteadia gibbosa, and the glossopterid polleniferous organ Eretmonia natalensis. Also present are the sphenopsids Trizygia speciosa, Phyllotheca australis and Benlightfootia sp. (Bordy & Prevec 2008).
Order Grylloblattida Walker, 1914
Suborder Grylloblattina Walker, 1914
Family Chaulioditidae Handlirsch, 1906
Type genus: Chauliodites Heer, 1864 with 11 species from the Severodvinian--Olenekian of Russia, Induan of Mongolia, Olenekian of Germany, Anisian of France and Middle Triassic of China (Aristov, 2003, 2004b, 2008).
Diagnosis: Costal space broader than subcostal one; M not fused with CuA, branching beyond RS base; CuA divided into [CuA.sub.1] and [CuA.sub.2].
Description: Small and middle-sized insects. Anterior margin of forewing convex. Costal space broader than subcostal one. SC ends beyond midlength or in distal third of wing. RS starts in basal third of wing, with 2-4 branches. Base of M free, [M.sub.5] absent, M bifurcates into MA and MP beyond RS base. MA with 2-4 branches, sometimes forming regular comb; MP with 1 or 2 branches. CuA bifurcates into simple [CuA.sub.1] and [CuA.sub.2], and may change its state from concave to convex almost immediately after branching. Intercubital space narrow, traversed by simple crossveins. Anal area short and broad. [A.sub.1] simple, [A.sub.2] branched. Crossveins simple, straight, forming two rows of cells in the middle of radial field. In hindwing, base of M free, M with 4 branches, CuA with 2 branches, anal area large.
Genera included: Type genus, Triadosialis Handlirsch, 1906 with one species from the Olenekian of Germany; Nivopteria Lin, 1978 with one species from the Middle Triassic of China; Paratomia Aristov, 2004 with one species from the Induan of Russia; Protomia Aristov, 2004 with one species from the Kazanian of Russia; Miralioma Aristov, 2004 with two species from the Kazanian and Urzhumian of Russia; and monotypic Iphikozulu gen. n. from the Lopingian of KwaZulu-Natal, South Africa.
Remarks: The new genus described below is characterised by the combination of a broad costal space, M branching beyond the RS base and branched [CuA.sub.1]. A similar venation pattern is characteristic of the genera Triadosialis Handlirsch, 1906, Protomia Aristov, 2004 and Miralioma Aristov, 2004. The genus Triadosialis was described by Handlirsch (1906) for Chauliodites zinkeni Heer, 1864 from the Lower Triassic (Middle Bundsandstein) locality of Godevitz in Germany (Heer 1864). Handlirsch assigned this genus to the family Chaulioditidae in the order Megaloptera. The family Chaulioditidae, with the only species Ch. picteti Heer, 1864, was transferred to the order Grylloblattida and considered a senior synonym of the family Tomiidae Martynov, 1936 (Aristov 2004b). The genera Protomia and Miralioma were described in the family Liomopteridae (Aristov 2004c). Both of them differ from other liomopterids in the M that branches late, and from chaulioditids in the branched [CuA.sub.1]. The position of the M in relation to the RS base is a more reliable character than the number of [CuA.sub.1] branches. Thus, the genera Triadosialis, Protomia, Miralioma and Iphikozulu gen. n. are herewith transferred to the family Chaulioditidae, the type genus of which is characterised by the M that branches beyond the RS base. The description of the new genus and the transfer of the genera Triadosialis, Protomia and Miralioma to Chaulioditidae have necessitated changes to the familial diagnosis. Previously, one of the diagnostic features was simple [CuA.sub.1]. Currently, a broad costal space and M branching beyond the RS base remain diagnostic for chaulioditids.
[FIGURE 2 OMITTED]
The genus Kargalella Martynov, 1937 from the Urzhumian of Russia was placed in a separate subfamily of Chaulioditidae on the basis of a broad costal space and simple [CuA.sub.1]. The M in Kargalella bifurcates proximal to the RS base (Aristov 2004b). The combination of these characters precludes us from keeping this genus in Chaulioditidae, and it is transferred to the family Liomopteridae, with the subfamily Kargalellinae Aristov, 2004 being considered as a new junior subjective synonym of Liomopteridae Sellards, 1909. Kargalella differs from other liomopterids in the combination of fused RS+MA and simple [CuA.sub.1].
An incomplete grylloblattid forewing, which has been recently found at a locality near Colenso (Prevec et al. 2009: 486, pl. XIV, figs 1, 2), also probably belongs to Chaulioditidae on the grounds of its wing venation. Regrettably, its further identification is difficult without a closer examination of the specimen.
Genus Iphikozulu Aristov & Mostovski, gen. n.
Etymology: From Zulu iPhiko (wing) and Zulu (Zulu Kingdom). Gender masculine. Type and only species: I. kwayayaensis Aristov & Mostovski, sp. n.
Diagnosis: Middle-sized insects. Costal space near RS base 3 times as broad as subcostal one. SC with simple anterior branches, ends before distal third of wing. RS starts in basal quarter of wing. [CuA.sub.1] starts branching before midlength, with four branches.
Comparison: The new genus is closest to Protomia from the Kazanian deposits of Russia, from which it differs in simple branches of SC, as well as in [CuA.sub.2] and CuP ending on the posterior margin of the wing. In Protomia, [CuA.sub.2] anastomoses with [CuA.sub.1], and CuP terminates on [CuA.sub.2] (Aristov 2004c).
Iphikozulu kwayayaensis Aristov & Mostovski, sp. n.
Figs 2A, 2B
Etymology: From the type locality, KwaYaya.
Description: Forewing impression approx. 18 mm long, approx. 9 mm wide. Anterior margin of wing convex. RS starts branching in distal third of wing, with 2 or more branches. MA and MP with 2 branches each, start branching proximal to RS fork. CuP bent basally, straight afterwards. Crossveins simple.
Holotype: NMSA 2736 (field no. KY785a, b), the part and counterpart of a single insect wing impression. SOUTH AFRICA: KwaZulu-Natal: KwaYaya locality (see detail information under Material and Methods); Permian, Lopingian, Beaufort Group, Emakwezini Formation.
Family Liomopteridae Sellards, 1909
Genus Neoliomopterum Riek, 1976
Type and only species: N. picturatum Riek, 1976, by monotypy.
Diagnosis: Small insects. Anterior margin of forewing weakly convex, costal space slightly broader than subcostal one. SC with simple anterior branches, enters C near wing tip. RS base near wing midlength, at level of separation of M into MA and MP. Branches of CuA simple.
Neoliomopterum picturatum Riek, 1976
Figs 2C, 2D
Neoliomopterumpicturatum: Riek 1976b: 763, pl. 1, fig. 7; Carpenter 1992: 111; Storozhenko 1998: 188.
Redescription: Forewing length approx. 7 mm, width approx. 3.5 mm. R with one simple anterior branch. Stems of RS, MA and MP thickened basally and near wing midlength, abruptly thinning out in distal quarter, RS and MA simple, MP with 2 branches. Branches of CuA thickened. Crossveins simple and forming double row of cell in inter-radial field. Colour pattern in form of spots in intermedial and medial fields.
Holotype: NMSA 910 (Type no. 1972), impression of well-preserved brachypterous forewing without anal field. SOUTH AFRICA: KwaZulu-Natal: Emakwezini Railway Station nr Empangeni; Permian, Lopingian, Beaufort Group, Emakwezini Formation.
Remarks: N. picturatum had originally been described as a forewing fragment of a representative of the family Liomopteridae (Riek 1976b). It remained in this family until some time ago (Carpenter 1992), but later was transferred to Grylloblattida incertae sedis on the basis of its incomplete preservation (Storozhenko 1998). Re-examination of the holotype illustrated by a photograph in the original description has shown that the preservation of the wing is almost complete. This species is characterized by a shortened wing, which is twice as long as it is broad (wings of the majority of grylloblattids are three times as long as broad), and by the stems of RS, MA, MP and CuA thickened basally and at the wing midlength. Such characters are typical of shortened wings, which can be divided into brachypterous and micropterous forms. In brachypterous individuals, the wing is longer than half of a fully developed wing, and does not have considerably modified venation. In micropterous individuals, the wing is shorter than half of a normal wing, and both its shape and venation are heavily modified (Sinitshenkova 1987). Shortened wings are recorded in some grylloblattids. Micropterous wings are known in Protoblattiniella minutissima Meinier, 1912 from the Upper Carboniferous locality of Commentry in France and Sylvamicropteron harpax Aristov, 2004 from the Kungurian locality of Tshekarda in Russia. The genus Protoblattiniella belongs to the family Protoperlidae (Storozhenko 2002), and Sylvamicropteron has been described as Grylloblattida incertae sedis (Aristov 2004a). Despite the unusual proportions of the wing, N. picturatum still displays venation typical of grylloblattids, suggesting that we are dealing with a brachypterous wing. A rather wide costal space that is traversed by simple branches of SC, and a simple [CuA.sub.1] are features typical of two grylloblattid families, viz. Liomopteridae and Chaulioditidae. The latter family is characterized by M being divided into MA and MP beyond the RS stem (Aristov 2004b). This character is missing in Neoliomopterum, which favours its assignment to the Liomopteridae. N. picturatum differs from other liomopterids in having both a long SC, which reaches the wing apex, and oligomerized venation of RS, MA, MP and [CuA.sub.1]. These differences are possibly caused by changed proportions of the wing, but the comparison with other known liomopterids does not offer an opportunity to synonymise this genus.
The authors are grateful to Prof. A.P. Rasnitsyn (Paleontological Institute, Moscow) and Dr S. Storozhenko (Institute of Biology and Pedology, Vladivostok) for useful comments on an early draft of the manuscript, Ms Th. Nxele (NMSA) for her kind help with the etymology for the new genus and Dr E. Bordy (Rhodes University) for assistance in the field. D. Aristov's research was supported by the Russian Foundation for Basic Research (grant no. 09-04-01241-a), and funding for research and fieldwork was provided to R. Prevec by Rhodes University, the National Science Foundation (EAR-0230024), the National Research Foundation (African Origins Grant, UID: 65241) and the Palaeontological Scientific Trust (PAST). The holotype of the newly described species was collected under AMAFA Permit no. 06/01 issued to R. Prevec.
Anderson, J.M. & Anderson, H.M. 1985. Palaeoflora of southern Africa. Prodomus of southern African megafloras Devonian to Lower Cretaceous. Rotterdam: A.A. Balkema.
Aristov, D.S. 2003. Revision of the family Tomiidae (Insecta: Grylloblattida). Paleontological Journal 37 (1): 31-38.
--2004a. The fauna of grylloblattid insects (Grylloblattida) of the Lower Permian locality of Tshekarda. Paleontological Journal 38 (Suppl. 2): 80-145.
--2004b. Grylloblattids of the family Chaulioditidae (= Tomiidae syn. nov.) (Insecta: Grylloblattida) from the Upper Permian of Orenburg Region. Paleontological Journal 38 (Suppl. 2): 146-149.
--2004c. Grylloblattids of the family Liomopteridae (Insecta: Grylloblattida) of the upper half of the Upper Permian. Paleontological Journal 38 (Suppl. 2): 150-157.
--2008. New Tatarian representatives of the subfamily Chaulioditinae (Insecta: Grylloblattida: Chau lioditidae) from European Russia. Paleontological Journal 42 (1): 32-35.
Bordy, E.M. & Prevec, R. 2008. Sedimentology, palaeontology and palaeo-environments of the Middle (?) to Upper Permian Emakwezini Formation (Karoo Supergroup, South Africa). South African Journal of Geology 111 (4): 429-458.
Carpenter, F.M. 1992. Superclass Hexapoda. In: Moore, R.C. & Kaesler, R.L., eds, Treatise on invertebrate paleontology. Part R, Arthropoda 4, 3/4. Boulder, Colorado: The Geological Society of America and the University of Kansas, pp. 1-655.
Chumakov, N.M. & Zharkov, M.A. 2003. Climate during the Permian-Triassic biosphere reorganizations. Article 2. Climate of the Late Permian and Early Triassic: General inferences. Stratigraphy and Geological Correlation 11 (4): 361-375.
Geertsema, H., van Dijk, D.E. & van den Heever, J.A. 2002. Palaeozoic insects of southern Africa: A review. Palaeontologia africana 38: 19-25.
Handlirsch, A. 1906-1908. Die Fossilen Insekten und die Phylogenie der rezenten Formen. Leipzig: Engelmann.
Heer, O. 1864. Uber die fossilen Kakerlaken (Blattidae). Vierteljahresschrift der Naturforschenden Gesellschaft, Zurich 9: 273-302.
Johnson, M.R., van Vuuren, C.J., Visser, J.N.J., Cole, D.I., Wickens, H. de V., Christie, A.D.M., Roberts, D.L. & BRAND, G. 2006. Sedimentary rocks of the Karoo Supergroup. In: johnson, M.R., Anhaeusser, C.R. & Thomas, R.J., eds, The geology of South Africa. Johannesburg, Pretoria: Geological Society of South Africa & Council for Geoscience, pp. 461-501.
Lacey, W., van Dijk, D.E. & Gordon-Gray, K.D. 1975. Fossil plants from the Upper Permian in the Mooi River district of Natal, South Africa. Annals of the Natal Museum 22 (2): 349-420.
Prevec, R., Labandeira, C.C., Neveling, J., Gastaldo, R.A., Looy, C.V. & Bamford, M.K. 2009. Portrait of a Gondwanan ecosystem: A new late Permian fossil locality from KwaZulu-Natal, South Africa. Review of Palaeobotany andPalynology 156 (3-4): 454-493.
Riek, E.F. 1976a. Fossil insects from the Middle Ecca (Lower Permian) of southern Africa. Palaeontologia africana 19: 145-148.
--1976b. New Upper Permian insects from Natal. Annals of the Natal Museum 22 (3): 755-789.
Shcherbakov, D.E. 2008. On Permian and Triassic insect faunas in relation to biogeography and the Permian Triassic crisis. Paleontological Journal 42 (1): 15-31.
Sinitshenkova, N.D. 1987. The historical development of stoneflies. Transactions of the Paleontological Institute of the USSR Academy of Sciences [Trudy Paleontologicheskogo instituta Akademii nauk SSSR] 221: 1-142. (in Russian)
Storozhenko, S.Yu. 1998. Systematics, phylogeny and evolution of grylloblattid insects (Insecta: Grylloblattida). Vladivostok, Russia: Dal'nauka. (in Russian)
--2002. Order Grylloblattida Walker, 1914. In: Rasnitsyn, A.P. & Quicke, D.L.J., eds, History of Insects. Dordrecht: Kluwer Acad. Publ., pp. 278-281.
van Dijk, D.E. 1997. Insect fauna of South Africa from the Upper Permian and the Permian/Triassic boundary. Palaeontologia africana 34: 43-48.
van Dijk, D.E. & Geertsema, H. 1999. Permian Insects from the Beaufort Group of Natal, South Africa. Annals of the Natal Museum 40: 137-171.
D. S. Aristov (1), R. Prevec (2) and M. B. Mostovski (1,3)
(1) Paleontological Institute, Russian Academy of Sciences, 123 Profsoyuznaya Str., Moscow, 117868 Russia; firstname.lastname@example.org
(2) Department of Geology, Rhodes University, P.O. Box 94, Grahamstown, 6140 South Africa; email@example.com
(3) Natal Museum, P. Bag 9070, Pietermaritzburg, 3200 South Africa, and School of Biological & Conservation Sciences, University of KwaZulu-Natal, P. Bag X01, Scotsville, 3209 South Africa; firstname.lastname@example.org
|Gale Copyright:||Copyright 2009 Gale, Cengage Learning. All rights reserved.|