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594 results for “Carboniferous”
Figure 18 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 18. Wing venation of Euchomenella heteroptera (De Haan, 1842) (NHM IWC OB 28; ♂; abbreviations: CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis; M, media; RP, posterior radius); arrows without label indicate the alternative origin of a branch of anterior cubitus (CuA), presumably homologous in both forewings (apparent fusion of posterior subcosta (ScP) with anterior radius (RA) is a result of artefacts of preparation). A, left forewing (ventral view). B, right forewing (dorsal view).
Figure 17 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 17. Wing venation of specimen IWC OB 239, belonging to Hoplocorypha sp. (♂; abbreviations: CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis; RA, anterior radius). A, left forewing, ventral view. B, detail of the origin of the anterior branch of posterior radius (RP*), as located on A; arrow without label indicates the origin of (the posterior branch of) RP*.
Figure 16 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 16. Wing venation of Hoplocorypha nigerica Beier, 1930 (♂; abbreviations: ScP, posterior subcosta; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis; RA, anterior radius). A, C, specimen NHM IWC OB 29, right forewing (dorsal view). B, D, specimen NHM IWC OB 31, right forewing (dorsal view). C, detail of the origin of the anterior branch of posterior radius (RP*), as located on A. D, detail of the origin of RP*, as located on B. E–H, specimen NHM IWC OB 30. E, left forewing (ventral view). F, right forewing (dorsal view). G, detail of the origin of RP*, as located on E. H, detail of the origin of RP*, as located on F.
Figure 15 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 15. Wing venation of Schizocephala bicornis (Linnaeus, 1758) (MNCN IWC 24, ♂; abbreviations: ScP, posterior subcosta; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis; RA, anterior radius). A, left forewing (ventral view). B, right forewing (dorsal view). C, detail of the connection of the anterior branch of posterior radius (RP*) with posterior radius + media (RP + M), as located on A. D, detail of the connection of RP* with RP + M, as located on B.
Figure 12 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 12. Intra-individual variations in the origin of the anterior branch of posterior radius (RP*); on B, D, arrows indicate the origin of RP* (abbreviations: ScP, posterior subcosta; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis; M, media; RA, anterior radius). A–D, forewings of Creobroter sp. (IWC OB 141, ♀). A, left forewing (ventral view). B, detail of left forewing apex. C, right forewing, atypical morphology (dorsal view). D, detail of right forewing apex. E–F, forewings of Deroplatys lobata (Guérin-Méneville, 1838) (IWC OB 237, ♂). E, left forewing (ventral view). F, right forewing, atypical morphology (dorsal view).
Figure 13 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 13. Wing venation of Statilia maculata (Thunberg, 1784) (♂; abbreviations: ScP, posterior subcosta; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis; RA, anterior radius). A, specimen NHM IWC OB 37, left forewing (ventral view), typical morphology. B, specimen NHM IWC OB 36, right forewing (dorsal view), atypical morphology. C, specimen NHM IWC OB 35, left forewing (dorsal view), atypical morphology. D, detail of the connection of the anterior branch of posterior radius (RP*) with posterior radius + media (RP + M), as located on C.
Figure 10 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 10. Wing venation of an undetermined Mantinae, atypical morphology (MNCN IWC OB 28; abbreviations: ScP, posterior subcosta; CuP, posterior cubitus; AA, anterior analis). A, left forewing (dorsal view); arrow without label indicates the origin of a branch of anterior cubitus (CuA) from posterior radius + media (RP + M). B, right forewing (ventral view); arrow without label indicates the origin of the same branch of CuA as in A. C, detail of the area between the anterior branch of RP + M and anterior radius (RA) as located on A; arrows indicate inflexion points of the anterior branch of the supernumerary branch of RP + M (see text). D, detail of the area between the anterior branch of RP + M and RA as located on B; arrows indicate the points of fusion and divergence of the supernumerary branch of RP + M with RA.
Figure 9 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 9. Wing venation of Amorphoscelis pulchra Bolivar, 1908; in C, D, G, H, thickness of arrows indicates strength of indicated tracheae (abbreviations: ScP, posterior subcosta; CuP, posterior cubitus; AA, anterior analis). A–D, specimen NHM IWC OB 23. A, left forewing (ventral view). B, right forewing (dorsal view). C, detail of the connection of the anterior branch of posterior radius + media (RP + M) with anterior radius (RA), as located on A. D, detail of the connection of the anterior branch of RP + M with RA, as located on B. E–H, specimen NHM IWC OB 24. E–F, arrows without label indicate the origin of a branch of anterior cubitus (CuA). E, left forewing (ventral view). F, right forewing (dorsal view). G, detail of the connection of the anterior branch of RP + M with RA, as located on E. H, detail of the connection of the anterior branch of RP + M with RA, as located on F.
Figure 19 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 19. Possible transition from an anteriorly pectinate branch of the posterior branch of anterior cubitus (CuA2) to a posteriorly pectinate anterior cubitus (CuA). A, branching pattern of CuA as in Metallyticus spp. B, one of the branching patterns of CuA exhibited by Ameles decolor (Charpentier, 1825). C, most frequent branching pattern of CuA as in A. decolor (Charpentier, 1825). D, branching pattern of CuA as in Amorphoscelidae. E, branching pattern of CuA as in Chaeteessa spp.
Figure 11 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 11. Wing venation of an undetermined Oxypilinae sp. (MNCN IWC OB 31, ♂; abbreviations: ScP, posterior subcosta; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis). A, right forewing (dorsal view). B, left forewing (ventral view). C, detail of the connection of the anterior branch of posterior radius + media (RP + M) with anterior radius (RA), as located on A. D, detail of the connection of the anterior branch of RP + M with RA, as located on B.
Figure 8 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 8. Wing venation of Amorphoscelis sp. (IWC OB 190, ♂; abbreviations: ScP, posterior subcosta; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis). A, left forewing (ventral view). B, detail of the area between anterior radius (RA) and posterior radius + media (RP + M), as located on A; left arrow indicates the anterior branch of the anterior branch of RP + M; right arrow indicates the anterior branch of the anterior branch of RP + M emerging from RA; ° indicates the posterior branch of the anterior branch of RP + M. C, left forewing (dorsal view). D, detail of the area between RA and RP + M, as located on C; ° indicates the posterior branch of the anterior branch of RP + M. E, detail of the fusion of the anterior branch of RP + M with RA, as located on D; arrow indicates the RP + M trachea. F, detail of the divergence of the posterior branch of the anterior branch of RP + M from RA, as located on D; arrow indicates the trachea of the posterior branch of RP + M. G, detail of the divergence of the anterior branch of the anterior branch of RP + M from RA, as located on D; arrow indicates the trachea of the anterior branch of RP + M.
Figure 7 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 7. Wing venation of Amorphoscelis sp. (IWC OB 243, ♂; abbreviations: ScP, posterior subcosta; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis). A, left forewing (ventral view); left arrow indicates the fork of the anterior branch of posterior radius + media (RP + M), right arrow indicates the branching of RP + M and the fusion of the resulting branches. B, right forewing (dorsal view); arrow indicates the first fork of the anterior branch of RP + M.
Figure 6 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 6. Wing venation of praying mantids exhibiting no vein*. A, Metallyticus splendidus Westwood, 1835 (IWC OB 192, ♀; left forewing, ventral view; abbreviations: ScP, posterior subcosta; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis). B, detail of the area between anterior radius (RA) and posterior radius + media (RP + M), as located on A; arrows without labels indicate short sclerotized structures located between RA and an irregularly sclerotized structure, itself located between RA and RP + M. C, Chaeteessa sp. (MTD, Dresden; right forewing, dorsal view). D, detail of the area between RA and RP + M, as located on C. E, Mantoida maya Saussure & Zehntner, 1894 (specimen IWC OB 102, ♂; left forewing, dorsal view, reversed). F, detail of the area between RA and RP + M, as located on E; arrow indicates an isolated cross-vein.
Figure 5 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 5. Wing venation of Miomantis paykullii Stål, 1871 (♂; abbreviations: ScP, posterior subcosta; RA, anterior radius; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis; RP, posterior radius; M, media). A, B, specimen NHM IWC OB 38. A, left forewing (ventral view), typical morphology. B, right forewing (dorsal view), atypical morphology. C, D, specimen NHM IWC OB 39. C, left forewing (ventral view), typical morphology. D, right forewing (dorsal view), atypical morphology. E, specimen NHM IWC OB 40, right forewing (dorsal view), atypical morphology.
Figure 4 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 4. Wing venation of an undetermined Mantinae (MNCN IWC OB 27, ♂; abbreviations: ScP, posterior subcosta; RA, anterior radius; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis; RP, posterior radius; M, media). A, left forewing (ventral view), typical morphology. B, right forewing (ventral view, reversed), atypical morphology. C, detail of the wing base, as located on B; arrow indicates a narrow trachea directed towards radius (R), interpreted as the median trachea.
Figure 3. Evidence for a in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 3. Evidence for a fusion of posterior radius (RP) with media (M) at the wing base in Mantodea (abbreviations: ScP, posterior subcosta; RA, anterior radius; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis). A, Creobroter sp., detail of forewing base (IWC OB 126, ♂; right forewing, ventral view, reversed); arrows without label indicate the course of the median trachea. B, detail of forewing base, as located on A; arrows indicate the course of the median trachea. C, Creobroter sp., detail of forewing base (IWC OB 144, ♀; left forewing, ventral view). D, detail of forewing base, as located on C. E, Hymenopus coronatus (Olivier, 1792), detail of forewing base (IWC OB 249, ♀; left forewing, ventral view). F, detail of forewing, base as located on E. G, Hymenopus coronatus (Olivier, 1792), detail of forewing base (IWC OB 238, ♂; right forewing, dorsal view). H, Deroplatys desiccata Westwood, 1839, detail of forewing base (IWC OB 155, ♂; right forewing, ventral view, reversed).
Figure 2 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 2. Forewing venation of Metallyticus violaceus (Burmeister, 1838), atypical morphology (NHM IWC OB 22, London; left forewing, ventral view; abbreviations: ScP, posterior subcosta; RA, anterior radius; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis; M, media). A, photograph. B–C, detail of the wing venation as located on A; arrows without labels indicate a supernumerary tracheae.
Figure 1 in Evidence for Carboniferous origin of the order Mantodea (Insecta: Dictyoptera) gained from forewing morphology
Figure 1. Forewing venation of Metallyticus violaceus (Burmeister, 1838), atypical morphology (MNHN, Paris, ♀; right forewing, dorsal view; abbreviations: ScP, posterior subcosta; RA, anterior radius; CuA, anterior cubitus; CuP, posterior cubitus; AA, anterior analis). A, photograph. B, detail of the wing venation as located on A. C–F, detail of the wing venation as located on B; arrows indicate various tracheae (see text for explanations).
Text-fig. 2. Geological setting of the studied sites. a: Stratigraphic position of the Mospyne Formation in the Carboniferous succession of the Donets Basin. b: Stratigraphic position of the studied locality of ammonoids (numbers in circles to the right of the lithological column). c–f: Some studied localities, c – stratigraphic level with ammonoids No. 8, d – stratigraphic level No. 4, e – stratigraphic level No. 3, f – part of the section of the Mospyne Formation in Sukha Ravine and the position of stratigraphic levels with ammonoids. Abbreviations: Tour. – Tournaisian, Serpukhov. – Serpukhovian, Kasimov. – Kasimovian. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine
Text-fig. 2. Geological setting of the studied sites. a: Stratigraphic position of the Mospyne Formation in the Carboniferous succession of the Donets Basin. b: Stratigraphic position of the studied locality of ammonoids (numbers in circles to the right of the lithological column). c–f: Some studied localities, c – stratigraphic level with ammonoids No. 8, d – stratigraphic level No. 4, e – stratigraphic level No. 3, f – part of the section of the Mospyne Formation in Sukha Ravine and the position of stratigraphic levels with ammonoids. Abbreviations: Tour. – Tournaisian, Serpukhov. – Serpukhovian, Kasimov. – Kasimovian.
Figs 6, 7 in An enigmatic Palaeozoic stem-group: Paoliida, designation of new taxa from the Upper Carboniferous of the Czech Republic (Insecta: Paoliidae, Katerinkidae fam. n.)
Figs 6, 7. Katerinka hilaris gen. et sp. n. (Katerinkidae fam. n.), photograph and line drawing of holotype specimen B11978, collection of the Municipal Museum of Ostrava.
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