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Here we describe the first discoveries of insects from the Gzhelian of the Reyran Basin (northern part of Esterel, South of France). These are a new mylacrid, Opsiomylacris sp. an undetermined genus and species of Phyloblattidae, two other roachoids of uncertain affinities, and a Palaeodictyoptera, all based on forewings. Although these discoveries demonstrate that insects were present in the corresponding paleoforest, they remain less diverse and rarer than the plant remains. The genus Opsiomylacris is currently supposed to have lived under xeric environments, possibly corresponding to the more xeric paleobiotas of the margin of the humid valley bottoms. [ABSTRACT FROM AUTHOR]

A new genus and species of the archaeorthopteran order Caloneurodea are described and illustrated from the Salagou Formation (France) as Lodevogramma pumilia gen. et sp. nov. The particular wing venation of this species precludes its placement within one of the already described families of Caloneurodea. Consequently, the family Lodevogrammatidae fam. nov. is created to accommodate this specimen. A detailed comparison of the new species with other Caloneurodea is provided. This new species differs from all other Caloneurodea because it has: petiolate wings; the area between C and R/RA is very narrow; vein RA ends near the wing apex; vein RP has two branches; the fork of CuP basad the base of M; and two very short anal veins are present. This new species increases the diversity of Caloneurodea in the Salagou Formation and provides additional information on the diversity of the order around the late Capitanian extinction. We compared the diversity of Caloneurodea with that of Megasecoptera, another order with a similar history between the Carboniferous and the Permian, and hypothesized that the decrease in the size of both groups could be an indicator of their declines, possibly related to floral changes, following a pattern similar to that of Permian tetrapods. The decline of Caloneurodea could also be related to the diversification of the Orthoptera during the middle–late Permian. [ABSTRACT FROM AUTHOR]

A new dictyoneurid insect, Dictyoneura goujonorum n. sp. from the Latest Ghzelian – Asselian basin of Graissessac (Hérault, France) is described in details. It is represented by a well-preserved specimen with wings of 32–35 mm long and 13–14 mm wide and other peculiar diagnostic characters such an MP with four branches and a CuP with three branches. As all the other Dictyoneura species are known from the Namurian and/or the Wesphalian, Dictyoneura goujonorum n. sp. is the youngest representative of the genus. It is also the first record of the order Palaeodictyoptera from the Graissessac basin. The Carboniferous-Permian palaeodictyopterans are well-known to have lived in rather humid swamp forests. The global warming and drying of the climate during the Permian and/or the rise of potential predators may be responsible of their extinction. [ABSTRACT FROM AUTHOR]

The genus Klebsiella Meunier, 1908 from the latest Carboniferous of Commentry, is revised, confirming its attribution to the Blattinopsidae. The family name Klebsiellidae should have priority on its junior synonym Blattinopsidae, but the common usage over time could allow maintaining the later. The first Blattinopsidae from the Moscovian Konservat–lagerstätte of Avion is described as a new genus and species Avionblattinopsis oudardi gen. et n. sp. on the basis of a single forewing. It differs from the other genera of this family in the vein ScP distally fused to the vein RA. It increases our knowledge about this family, known between the Late Carboniferous and the Middle Permian. An emended family diagnosis is proposed. Protoblattiniella minutissima Meunier, 1912, based on a mature nymph would better fit with the Paoliidae than with the Blattinopsidae. [ABSTRACT FROM AUTHOR]

The orthopteran fauna of the Paleocene of Menat Formation (France) is revised. It comprises at least 12 species in the following clades: Grylloidea (an undescribed species, Menatgryllus longixiphus gen. et sp. nov.); Tettigoniidae (Prophasgonura lineatocollis); Elcanidae (Cenoelcanus menatensis gen. et sp. nov.); two Eumastacoidea (Paleochina duvergeri gen. et sp. nov. and Paleochina minuta sp. nov., tentatively placed in the extant family Chorotypidae). These two last taxa are compared to the other described fossil Eumastacoidea. As all these Eumastacoidea are represented by tegmina or hindwings, their previous attributions to the Eumastacidae sensu stricto are questionable. All previously described fossil Caelifera from Menat are considered of uncertain position. Those that were previously considered as Acridoidea are excluded from this clade. In consequence, the oldest described Acridoidea are Oligocene, at the time of diversification of the grasses on which these insects predominantly live, in accordance with the most recent molecular dating of the Acrididae. Cenoelcanus menatensis is the youngest and first Cenozoic representative of the Mesozoic Elcanidae, showing that this family survived the Cretaceous--Paleocene extinction and became extinct during the Paleogene. [ABSTRACT FROM AUTHOR]

Abstract: Apart frequent and relatively common ichnites, only a few body fossils (Ostracoda) have been mentioned in the Red Continental Permian formations of Provence till these last years. During 2006 and 2007 field researches, new arthropods have been discovered in the Pradineaux Formation of the Bas-Argens. They are Triopsidae (Crustacea, Notostraca) and an insect wing (Syntonopteridae) corresponding to a new genus and species Gallolithoneura butchlii gen. et sp. n. This latter is the first insect record in the Permian of Provence and the youngest one of this enigmatic Carboniferous paleopteran family. As in the other French Permian basins (Lodève, Saint-Affrique), these discoveries demonstrate that the Permian Provençal paleofauna was rich and diverse. For the Upper part of the Pradineaux Formation, Capitanian (Upper Guadalupian) in age, the Triopsidae mean the presence of periodical ponds settled in a playa environment evolving under a xerophytic climate. Gallolithoneura butchlii suggests also the presence of aquatic habitats. [Copyright &y& Elsevier]