Discovery of the oldest known Pterygota in the Lower Carboniferous of the Upper Silesian Basin in the Czech Republic (Insecta: Archaeorthoptera)

The earliest pterygote (winged insect), dated from the Lower Carboniferous (Namurian A/E1, circa 324 millions years ago) is described from the Upper Silesian Basin in the Czech Republic. On the basis of its wing venation, it is attributed to the Archaeorthoptera Béthoux and Nel, 2002, crown group of the “Orthoptera”. Besides Apterygota (Collembola and Archaeognatha) known from the Lower Devonian, extremely rare pterygote insects are known from Lower Carboniferous deposits when they first appeared. The present discovery supports the hypothesis of the presence of the ancestor lineage of the orthopteroid in the Lower Carboniferous ecosystems.     

中国古生代化石昆虫研究回顾

自林启彬先生1978年命名了我国第一个古生代昆虫至今, 中国学者共发表20余篇分类学论著, 描述鉴定我国古生代昆虫共61种, 归属于9目（总目）。这些标本分布于西北、 西南、 华东等9省区, 其中石炭纪47种, 二叠纪14种。本文统计了我国已发现的古生代化石昆虫属种名录以及它们的分布和地质年代, 总结了国内古生代化石昆虫当前的研究状况和发展趋势, 并分析了研究中存在的问题。其中关于化石昆虫普遍存在的脉序差异问题需给予足够的重视, 高级阶元的建立应更加慎重。研究表明我国古生代昆虫已经高度分异, 古翅类、 新翅类均已出现, 且代表着有翅昆虫辐射演化的重要阶段。     

Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology

Homologies of the forewing venation pattern of the order Mantodea (Insecta: Dictyoptera) consistent with the accepted insect wing venation groundplan are proposed. A comparative morphological analysis was carried out based on a broad taxonomic sample of extant taxa. Besides macromorphological aspects, focus is given to the pattern of the tracheal system as a basis for establishing primary homologies. All extant praying mantids exhibit a composite stem composed of the posterior radius (RP) and the media (M) and most praying mantids exhibit a fusion of the anterior branch of RP + M with the anterior radius (RA). The wing venation of the species ?Mesoptilus dolloi, previously assigned to the polyphyletic fossil assemblage ‘Protorthoptera’, is re‐interpreted in the light of the new homology statement. Our interpretation suggests that it is a putative stem‐Mantodea, as are some other ‘protorthopterous’ taxa. This hypothesis implies that the total‐group Mantodea arose as soon as the Late Carboniferous, i.e. about 175 million years earlier than previously estimated. This analysis contributes to the view that most of the Late Carboniferous ‘Protorthoptera’ are stem‐representatives of the major polyneopteran clades (e.g. cockroaches, grasshoppers and crickets, rock‐crawlers), suggesting a survivorship of several main Pterygota lineages at the end‐Permian extinction event higher than previously expected. © 2009 The Linnean Society of London, Zoological Journal of the Linnean Society, 2009, 156 , 79–113.     

A possible evolutionary pathway to insect flight starting from lepismatid organization

Starting from the hypothesis that flight in Pterygota evolved from lepismatid organization of their ancestors, the functional anatomy of the thorax was studied in Lepisma saccharina Linnaeus, 1758, and a Ctenolepisma sp. in regard to both the adaptations to the adaptive zone of Lepismatidae and to pre‐adaptations for the evolution of Pterygota. Well‐preserved parts of three subcoxal leg segments were found in the pleural zone participating in leg movement. The lepismatid strategy of escaping predators by running fast and hiding in narrow flat retreats led to a dorso‐ventrally flattened body which enabled gliding effects when dropped, followed by flight on the ground. The presumed exploitation of soft tissue at the tips of low growing Devonian vascular plants opened a canalized pathway to the evolution of the flying ability. Locomotion to another plant was facilitated by dropping. It is possible that threat by spider‐like predators favoured falling and gliding as escape reactions by selection. Falling experiments with `lepismatid' models revealed a narrow `window' for gliding, with optimum dimensions of 8 mm body length and 8 mg weight. An equation was derived which describes the glide distance as function of weight, area of the horizontal outline, the specific glide efficiency of the body, and a non‐linear function of the falling height. Improved gliding was made possible by enlarging thoracic paratergites into broad wing‐like extensions of light‐weight organization. The disadvantage of the lateral lobes for locomotion on the ground could be minimized by tilting them vertically when running and horizontally when gliding. This movability could be attained by the intercalation of a membranous strip between tergite and paratergite and the utilization of the pre‐existing muscular system and the articulation between the two most basal subcoxal sclerites as a pivot. The dorsal part of the most basal subcoxa was thus integrated into the wing. Initiation of active flight was possible by flapping movements during gliding. Morphological, ontogenetic and ecological aspects of the origin of Pterygota are discussed.     

Abdominal serial homologues of wings in Paleozoic insects

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COMMENT ON MARDEN (2013): “REANALYSIS AND EXPERIMENTAL EVIDENCE INDICATE THAT THE EARLIEST TRACE FOSSIL OF A WINGED INSECT WAS A SURFACE SKIMMING NEOPTERAN”

Marden's (2013) reanalysis of Knecht et al. (2011) suggesting that specimen SEMC‐F97 is the result of the skimming behavior of a neopteran insect and, more importantly, fossil evidence of “… surface skimming as a precursor to the evolution of flight in insects” (Marden 2013) is found to be deficient on three fronts: (1) the principal specimen was never viewed firsthand which led to significant morphological misinterpretations; (2) poorly designed and executed neoichnological experiments led to incredulous results; and (3) the assumption that this specimen is fossil evidence supporting the surface skimming hypothesis of the origin of insect flight despite the fact that since its induction into the literature that hypothesis has been refuted based on significant paleontological, phylogenetic, genetic, and developmental evidence.