A New Upper Cretaceous Species of Chresmoda from Lebanon

Total Page:16

File Type:pdf, Size:1020Kb

A New Upper Cretaceous Species of Chresmoda from Lebanon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ig. 1. Chresmoda libanica sp. n., holotype specimen NI 3a, Fig. 2. Chresmoda libanica sp. n., holotype specimen NI 3a, photograph of general habitus. drawing of general habitus, scale bar represents 5 mm. 0.2 mm wide, bearing about 20 long and sharp spines long. The prothoracic femora are straight and elongate, (Fig. 10), probably corresponding to maxillary palpi. 10.7 mm long, 0.45 mm wide, bearing a short anterior These structures are better preserved in specimens NI 1 process and a series of small apical spines. The protho- and NI 2 than in NI 3. A short two- or three-segmented racic tibiae have a curved base, very short, 2.5 mm long, labial palpus is visible in NI 3, with no visible setae, 0.4 mm wide, representing the 23% of femoral length. about 1.0 mm long; mandibles visible in NI 3, 0.7 mm There is a row of small spines at tibial apex. The whole long and 0.5 mm wide, bearing a row of small obtuse prothoracic tarsus is 10.0 mm long, first tarsomere 3.0 teeth and several short but sharp spines (Figs 3–4). The mm long, second tarsomere about 2.5 mm long, third eyes are visible in NI 3, large elliptic, about 1.2 mm long about 1.0 mm long. The more distal segmentation of and 0.8 mm wide, 0.8 mm apart. The antennae are not visible, probably not preserved. The thorax is rather rounded but with a strong posterior concavity in ventral view, 4.0 mm long, 5.4 mm wide (NI 3), 2.5 mm long, 4.0 mm wide (NI 1), 2.5 mm long, 4.8 mm wide (NI 2), with no visible wing sheaths. The legs are very long and narrow, covered with very small hairs arranged in rows (visible in NI 2). The pairs of coxae are widely separated, 2.5 mm apart (NI 3), all similar, those of the same side of thorax being very close to each other, rounded and large, 0.8 mm wide and long. The trochanters are small and short, all similar, 0.5 mm Fig. 3. Chresmoda libanica sp. n., holotype specimen NI 3a, photograph of head and thorax, arrow indicates right mandible Fig. 4. Chresmoda libanica sp. n., holotype specimen NI 3a, with an apical short spine. drawing of ventral view of the body. Scale bar represents 5 mm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ig. 5. Chresmoda libanica sp. n., holotype specimen NI 3a, photograph of ovipositor. this last point. Interestingly, Martínez-Delclòs (1991) demonstrated that adult males of C. aquatica and C. obscura were apterous, suggesting that also the adult females of C. libanica could have been apterous. The presence of unique, highly specialized tarsi in C. obscura, C. aquatica, C. libanica sp. n., and probably C. orientalis strongly supports the hypothesis that these insects were living on the water surface, using the water superficial tension to “skate” on surface like extant Ger- Fig. 6. Chresmoda libanica sp. n., holotype specimen NI 3a, ridae and Veliidae, as already proposed by Martínez- drawing of ovipositor, scale bar represents 1 mm. Delclós (1991). Baudoin (1980) tried to establish that Chresmoda obscura could not live on water surface, (Baudoin 1980: 2). The oblique apices of the tarsomeres using the water superficial tension, through a comparison probably acted as a blocking system in order to avoid the with the extant Gerridae. He supposed that the Chres- complete distortion of the legs (see Figs 7–8, 13). Simi- moda were too large to float like Gerridae. But nobody larly, some Gerridae such as Potamobates thomasi Hun- knew in 1980 that at least some Chresmoda spp. could gerford, have no specialized setae but their have highly specialized legs and tarsi. Numerous extant two-segmented tarsi are curved (Andersen, 1982: Fig. Gerridae bear highly specialized setae that help them to 438). float by increasing their surface in contact with water sur- Nevertheless, the Chresmodidae probably did not use face (Andersen, 1982). Chresmoda aquatica and Chres- their legs for skating in the same way as modern Gerridae moda libanica sp. n. have no specialized setae on their and Veliidae do. These insects have short to very short legs but their exceptionally high number of tarsomeres fore legs, useless in skating, and they mainly use their (about 40 in C. libanica sp. n., about twelve in C. obscura median and partly hind legs for this purpose. The fore, and C. aquatica) probably helped to increase, thanks to mid and hind legs of the Chresmodidae have nearly the the curvature of the tarsi, the length of that part of the leg same lengths and structures, and so probably similar func- in contact with the water surface, and consequently to tions in skating. increase the vertical component of the superficial tension C. aquatica, Saurophthiroides mongolicus, and the Chresmodidae from Araripe (Lower Cretaceous of Brazil) probably lived in lacustrine palaeoenvironments. The Solnhofen lithographic limestone was a marine deposit, but it has yielded numerous fossils of terrestrial origin. The Nammoura “fish beds” are also of marine origin Fig. 8. Chresmoda libanica sp. n., holotype specimen NI 3a, Fig. 7. Chresmoda libanica sp. n., holotype specimen NI 3a, drawing of left median tibia and tarsi, scale bar represents 3 photograph of left median tarsus, arrows indicate tarsomeres. mm. 148 Fig. 10. Chresmoda libanica sp. n., paratype specimen NI 2b, photograph of maxillary palpi, arrow indicates some of the long and sharp spines of a palpus. less, two of the three known specimens of C. libanica sp. n. are well-preserved nymphal exuviae, which are very delicate remains that do not support long transport. This Fig. 9. Chresmoda libanica sp. n., paratype specimen NI 2b, suggests that these nymphs were living in the sea or very photograph of general habitus. close to it. C. libanica sp. n. was probably carnivorous since it (Schram et al., 1999), but with “a considerable influx of shows well-developed maxillary palpis, as in C. aquatica, terrestrial organic debris” (Krassilov and Bacchia, 2000: bearing numerous strong and sharp spines and it has 798). Thus both C. obscura and C. libanica sp. n. could strong mandibles. It would probably eat small insects have been marine or freshwater insects. trapped by the water surface tension, or planktonic or The long ovipositor with indentations
Recommended publications
  • Ancient Roaches Further Exemplify 'No Land Return' in Aquatic Insects
    Gondwana Research 68 (2019) 22–33 Contents lists available at ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr Ancient roaches further exemplify ‘no land return’ in aquatic insects Peter Vršanský a,b,c,d,1, Hemen Sendi e,⁎,1, Danil Aristov d,f,1, Günter Bechly g,PatrickMüllerh, Sieghard Ellenberger i, Dany Azar j,k, Kyoichiro Ueda l, Peter Barna c,ThierryGarciam a Institute of Zoology, Slovak Academy of Sciences, Dúbravská cesta 9, 845 06 Bratislava, Slovakia b Slovak Academy of Sciences, Institute of Physics, Research Center for Quantum Information, Dúbravská cesta 9, Bratislava 84511, Slovakia c Earth Science Institute, Slovak Academy of Sciences, Dúbravská cesta 9, P.O. BOX 106, 840 05 Bratislava, Slovakia d Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya 123, 117868 Moscow, Russia e Faculty of Natural Sciences, Comenius University, Ilkovičova 6, Bratislava 84215, Slovakia f Cherepovets State University, Cherepovets 162600, Russia g Staatliches Museum für Naturkunde Stuttgart, Rosenstein 1, D-70191 Stuttgart, Germany h Friedhofstraße 9, 66894 Käshofen, Germany i Bodelschwinghstraße 13, 34119 Kassel, Germany j State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, PR China k Lebanese University, Faculty of Science II, Fanar, Natural Sciences Department, PO Box 26110217, Fanar - Matn, Lebanon l Kitakyushu Museum, Japan m River Bigal Conservation Project, Avenida Rafael Andrade y clotario Vargas, 220450 Loreto, Orellana, Ecuador article info abstract Article history: Among insects, 236 families in 18 of 44 orders independently invaded water. We report living amphibiotic cock- Received 13 July 2018 roaches from tropical streams of UNESCO BR Sumaco, Ecuador.
    [Show full text]
  • UFRJ a Paleoentomofauna Brasileira
    Anuário do Instituto de Geociências - UFRJ www.anuario.igeo.ufrj.br A Paleoentomofauna Brasileira: Cenário Atual The Brazilian Fossil Insects: Current Scenario Dionizio Angelo de Moura-Júnior; Sandro Marcelo Scheler & Antonio Carlos Sequeira Fernandes Universidade Federal do Rio de Janeiro, Programa de Pós-Graduação em Geociências: Patrimônio Geopaleontológico, Museu Nacional, Quinta da Boa Vista s/nº, São Cristóvão, 20940-040. Rio de Janeiro, RJ, Brasil. E-mails: [email protected]; [email protected]; [email protected] Recebido em: 24/01/2018 Aprovado em: 08/03/2018 DOI: http://dx.doi.org/10.11137/2018_1_142_166 Resumo O presente trabalho fornece um panorama geral sobre o conhecimento da paleoentomologia brasileira até o presente, abordando insetos do Paleozoico, Mesozoico e Cenozoico, incluindo a atualização das espécies publicadas até o momento após a última grande revisão bibliográica, mencionando ainda as unidades geológicas em que ocorrem e os trabalhos relacionados. Palavras-chave: Paleoentomologia; insetos fósseis; Brasil Abstract This paper provides an overview of the Brazilian palaeoentomology, about insects Paleozoic, Mesozoic and Cenozoic, including the review of the published species at the present. It was analiyzed the geological units of occurrence and the related literature. Keywords: Palaeoentomology; fossil insects; Brazil Anuário do Instituto de Geociências - UFRJ 142 ISSN 0101-9759 e-ISSN 1982-3908 - Vol. 41 - 1 / 2018 p. 142-166 A Paleoentomofauna Brasileira: Cenário Atual Dionizio Angelo de Moura-Júnior; Sandro Marcelo Schefler & Antonio Carlos Sequeira Fernandes 1 Introdução Devoniano Superior (Engel & Grimaldi, 2004). Os insetos são um dos primeiros organismos Algumas ordens como Blattodea, Hemiptera, Odonata, Ephemeroptera e Psocopera surgiram a colonizar os ambientes terrestres e aquáticos no Carbonífero com ocorrências até o recente, continentais (Engel & Grimaldi, 2004).
    [Show full text]
  • André Nel Sixtieth Anniversary Festschrift
    Palaeoentomology 002 (6): 534–555 ISSN 2624-2826 (print edition) https://www.mapress.com/j/pe/ PALAEOENTOMOLOGY PE Copyright © 2019 Magnolia Press Editorial ISSN 2624-2834 (online edition) https://doi.org/10.11646/palaeoentomology.2.6.1 http://zoobank.org/urn:lsid:zoobank.org:pub:25D35BD3-0C86-4BD6-B350-C98CA499A9B4 André Nel sixtieth anniversary Festschrift DANY AZAR1, 2, ROMAIN GARROUSTE3 & ANTONIO ARILLO4 1Lebanese University, Faculty of Sciences II, Department of Natural Sciences, P.O. Box: 26110217, Fanar, Matn, Lebanon. Email: [email protected] 2State Key Laboratory of Palaeobiology and Stratigraphy, Center for Excellence in Life and Paleoenvironment, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China. 3Institut de Systématique, Évolution, Biodiversité, ISYEB-UMR 7205-CNRS, MNHN, UPMC, EPHE, Muséum national d’Histoire naturelle, Sorbonne Universités, 57 rue Cuvier, CP 50, Entomologie, F-75005, Paris, France. 4Departamento de Biodiversidad, Ecología y Evolución, Facultad de Biología, Universidad Complutense, Madrid, Spain. FIGURE 1. Portrait of André Nel. During the last “International Congress on Fossil Insects, mainly by our esteemed Russian colleagues, and where Arthropods and Amber” held this year in the Dominican several of our members in the IPS contributed in edited volumes honoring some of our great scientists. Republic, we unanimously agreed—in the International This issue is a Festschrift to celebrate the 60th Palaeoentomological Society (IPS)—to honor our great birthday of Professor André Nel (from the ‘Muséum colleagues who have given us and the science (and still) national d’Histoire naturelle’, Paris) and constitutes significant knowledge on the evolution of fossil insects a tribute to him for his great ongoing, prolific and his and terrestrial arthropods over the years.
    [Show full text]
  • 11. BIBLIOGRAFÍA 1. Arqueros Gallego, L. and L.M. Sanchez De La Fuente, Reconstrucción De Las Redes Tróficas Del Yacimiento De Las Hoyas
    11. BIBLIOGRAFÍA 1. Arqueros Gallego, L. and L.M. Sanchez de la Fuente, Reconstrucción de las redes tróficas del yacimiento de Las Hoyas. 1996. 2. Barale, G. and L.I. Viera, Description d'une nouvelle paléoflore dans le Crétacé inférieur du Nord de l'Espagne. Description of a new flora in the Lower Cretaceous in the North of Spain. Munibe: Ciencias naturales. Natur zientziak, 1991. 43: p. 21-35. 3. Barbadillo, L.J. and S.E. Evans, Lizards (Reptilia: Squamata) from the Early Cretaceous of Las Hoyas, Spain, in Extended Abstracts. 2nd International Symposium on Lithographic Limestones. 1995: Lleida-Cuenca, Spain. p. 27-28. 4. Blagoderov, V. and X. Martínez-Delclós, Two new fungus gnats (Insecta, Diptera, Mycetophilidae) from the Lower Cretaceous of Spain. Geobios, 2001. 34(1): p. 63-67. 5. Briggs, D.E.G., et al., The mineralization of dinosaur soft tissue in the Lower Cretaceous of Las Hoyas, Spain. Journal of the Geological Society, 1997. 154(4): p. 587-588. PDF 6. Buatois, L., et al., Short-term colonization trace-fossil assemblages in a carbonate lacustrineKonservat-Lagerstätte (Las Hoyas fossil site, Lower Cretaceous, Cuenca, Central Spain). Facies, 2000. 43(1): p. 145-156. 7. Buffetaut, E., Tetrapods from the Late Jurassic and Early Cretaceous lithographic limestones of Europe: A comparative review. Geobios, 1994. 27(Supplement 1): p. 259-265. 8. Buscalioni, A.D., Rutas por Museos y Colecciones de Paleontología de España 2: Castilla y León, Aragón. 2005, Madrid: Museo Geominero, IGME. 151. 9. Buscalioni, A.D., Rutas por Museos y Colecciones de Paleontología de España 1: Castilla la Mancha y Madrid.
    [Show full text]
  • Zootaxa, a Water-Skiing Chresmodid from the Middle Jurassic In
    Zootaxa 1762: 53–62 (2008) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2008 · Magnolia Press ISSN 1175-5334 (online edition) A water-skiing chresmodid from the Middle Jurassic in Daohugou, Inner Mongolia, China (Polyneoptera: Orthopterida) XIN-WEN ZHANG 1, DONG REN 2,3, HONG PANG 1,3 & CHUNG-KUN SHIH 2 1State Key Laboratory of Biocontrol and Institute of Entomology, Sun Yat-Sen University, Guangzhou 510275, China 2College of Life Sciences, Capital Normal University, Beijing 100037, China 3Corresponding author. E-mail: [email protected] or [email protected] Abstract A new genus with a new species (Jurachresmoda gaskelli gen. et sp. nov.) of Chresmodidae (Insecta: Polyneoptera: Orthopterida) is described and illustrated. They were collected from the Middle Jurassic in Daohugou, Jiulongshan For- mation, Inner Mongolia (Nei Mongol Autonomous Region), China. J. gaskelli have fringing hairs on tarsi and a part of tibiae of mid legs. These hairs and leg structures were probably associated with its water-skiing locomotion on freshwa- ter. A high number of tarsomeres, e. g. ultra-articulated tarsi as reported in other species of Chresmodidae, are also found for this new species. But, these true tarsi are mixed with some wrinkles resulted from dehydration and compression dur- ing fossilization process. Nymphs of the new species are also described. This is the first time that long and segmented cerci of the nymph are described in Chresmodidae. Key words: fossil insect, Chresmodidae, water-skiing, Middle Jurassic, Jiulongshan Formation, China Introduction Chresmodidae, a rare extinct family, is quite enigmatic. It is supposed to be an aquatic insect, probably carniv- orous (Baudoin, 1980; Nel et al., 2004; Nel et al., 2005).
    [Show full text]
  • Heteroptera: Gerromorpha) in Central Europe
    Shortened web version University of South Bohemia in České Budějovice Faculty of Science Ecology of Veliidae and Mesoveliidae (Heteroptera: Gerromorpha) in Central Europe RNDr. Tomáš Ditrich Ph.D. Thesis Supervisor: Prof. RNDr. Miroslav Papáček, CSc. University of South Bohemia, Faculty of Education České Budějovice 2010 Shortened web version Ditrich, T., 2010: Ecology of Veliidae and Mesoveliidae (Heteroptera: Gerromorpha) in Central Europe. Ph.D. Thesis, in English. – 85 p., Faculty of Science, University of South Bohemia, České Budějovice, Czech Republic. Annotation Ecology of Veliidae and Mesoveliidae (Hemiptera: Heteroptera: Gerromorpha) was studied in selected European species. The research of these non-gerrid semiaquatic bugs was especially focused on voltinism, overwintering with physiological consequences and wing polymorphism with dispersal pattern. Hypotheses based on data from field surveys were tested by laboratory, mesocosm and field experiments. New data on life history traits and their ecophysiological consequences are discussed in seven original research papers (four papers published in peer-reviewed journals, one paper accepted to publication, one submitted paper and one communication in a conference proceedings), creating core of this thesis. Keywords Insects, semiaquatic bugs, life history, overwintering, voltinism, dispersion, wing polymorphism. Financial support This thesis was mainly supported by grant of The Ministry of Education, Youth and Sports of the Czech Republic No. MSM 6007665801, partially by grant of the Grant Agency of the University of South Bohemia No. GAJU 6/2007/P-PřF, by The Research Council of Norway: The YGGDRASIL mobility program No. 195759/V11 and by Czech Science Foundation grant No. 206/07/0269. Shortened web version Declaration I hereby declare that I worked out this Ph.D.
    [Show full text]
  • Geological History and Phylogeny of Chelicerata
    Arthropod Structure & Development 39 (2010) 124–142 Contents lists available at ScienceDirect Arthropod Structure & Development journal homepage: www.elsevier.com/locate/asd Review Article Geological history and phylogeny of Chelicerata Jason A. Dunlop* Museum fu¨r Naturkunde, Leibniz Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, Invalidenstraße 43, D-10115 Berlin, Germany article info abstract Article history: Chelicerata probably appeared during the Cambrian period. Their precise origins remain unclear, but may Received 1 December 2009 lie among the so-called great appendage arthropods. By the late Cambrian there is evidence for both Accepted 13 January 2010 Pycnogonida and Euchelicerata. Relationships between the principal euchelicerate lineages are unre- solved, but Xiphosura, Eurypterida and Chasmataspidida (the last two extinct), are all known as body Keywords: fossils from the Ordovician. The fourth group, Arachnida, was found monophyletic in most recent studies. Arachnida Arachnids are known unequivocally from the Silurian (a putative Ordovician mite remains controversial), Fossil record and the balance of evidence favours a common, terrestrial ancestor. Recent work recognises four prin- Phylogeny Evolutionary tree cipal arachnid clades: Stethostomata, Haplocnemata, Acaromorpha and Pantetrapulmonata, of which the pantetrapulmonates (spiders and their relatives) are probably the most robust grouping. Stethostomata includes Scorpiones (Silurian–Recent) and Opiliones (Devonian–Recent), while
    [Show full text]
  • Neuropterida of the Lower Cretaceous of Southern England, with a Study on Fossil and Extant Raphidioptera
    NEUROPTERIDA OF THE LOWER CRETACEOUS OF SOUTHERN ENGLAND, WITH A STUDY ON FOSSIL AND EXTANT RAPHIDIOPTERA A thesis submitted to The University of Manchester for the degree of PhD in the Faculty of Engineering and Physical Sciences 2010 JAMES EDWARD JEPSON SCHOOL OF EARTH, ATMOSPHERIC AND ENVIRONMENTAL SCIENCES TABLE OF CONTENTS FIGURES.......................................................................................................................8 TABLES......................................................................................................................13 ABSTRACT.................................................................................................................14 LAY ABSTRACT.........................................................................................................15 DECLARATION...........................................................................................................16 COPYRIGHT STATEMENT...........................................................................................17 ABOUT THE AUTHOR.................................................................................................18 ACKNOWLEDGEMENTS..............................................................................................19 FRONTISPIECE............................................................................................................20 1. INTRODUCTION......................................................................................................21 1.1. The Project.......................................................................................................21
    [Show full text]
  • Changes to the Fossil Record of Insects Through Fifteen Years of Discovery
    This is a repository copy of Changes to the Fossil Record of Insects through Fifteen Years of Discovery. White Rose Research Online URL for this paper: https://eprints.whiterose.ac.uk/88391/ Version: Published Version Article: Nicholson, David Blair, Mayhew, Peter John orcid.org/0000-0002-7346-6560 and Ross, Andrew J (2015) Changes to the Fossil Record of Insects through Fifteen Years of Discovery. PLosOne. e0128554. https://doi.org/10.1371/journal.pone.0128554 Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ RESEARCH ARTICLE Changes to the Fossil Record of Insects through Fifteen Years of Discovery David B. Nicholson1,2¤*, Peter J. Mayhew1, Andrew J. Ross2 1 Department of Biology, University of York, York, United Kingdom, 2 Department of Natural Sciences, National Museum of Scotland, Edinburgh, United Kingdom ¤ Current address: Department of Earth Sciences, The Natural History Museum, London, United Kingdom * [email protected] Abstract The first and last occurrences of hexapod families in the fossil record are compiled from publications up to end-2009.
    [Show full text]
  • 1 Universidade Federal Do Ceará Centro De Ciências
    1 UNIVERSIDADE FEDERAL DO CEARÁ CENTRO DE CIÊNCIAS DEPARTAMENTO DE GEOLOGIA PROGRAMA DE PÓS-GRADUAÇÃO EM GEOLOGIA LUÍS CARLOS BASTOS FREITAS DESCRIÇÃO DE NOVOS TAXONS DE INSETOS FÓSSEIS DOS MEMBROS CRATO E ROMUALDO DA FORMAÇÃO SANTANA E COMENTÁRIOS SOBRE A GEODIVERSIDADE DO GEOPARK ARARIPE, BACIA SEDIMENTAR DO ARARIPE, NORDESTE DO BRASIL FORTALEZA 2019 2 LUÍS CARLOS BASTOS FREITAS DESCRIÇÃO DE NOVOS TAXONS DE INSETOS FÓSSEIS DOS MEMBROS CRATO E ROMUALDO DA FORMAÇÃO SANTANA E COMENTÁRIOS SOBRE A GEODIVERSIDADE DO GEOPARK ARARIPE, BACIA SEDIMENTAR DO ARARIPE, NORDESTE DO BRASIL Tese apresentada ao Programa de Pós- Graduação em Geologia da Universidade Federal do Ceará, como requisito parcial à obtenção do título de doutor em Geologia. Área de concentração: Geologia Sedimentar e Paleontologia. Orientador: Prof. Dr. Geraldo Jorge Barbosa de Moura. Coorientador: Prof. Dr. César Ulisses Vieira Veríssimo. FORTALEZA 2019 3 4 LUÍS CARLOS BASTOS FREITAS DESCRIÇÃO DE NOVOS TAXONS DE INSETOS FÓSSEIS DOS MEMBROS CRATO E ROMUALDO DA FORMAÇÃO SANTANA E COMENTÁRIOS SOBRE A GEODIVERSIDADE DO GEOPARK ARARIPE, BACIA SEDIMENTAR DO ARARIPE, NORDESTE DO BRASIL Tese apresentada ao Programa de Pós- Graduação em Geologia da Universidade Federal do Ceará, como requisito parcial à obtenção do título de doutor em Geologia. Área de concentração: Geologia Sedimentar e Paleontologia. Aprovada em: 18/01/2019. BANCA EXAMINADORA ________________________________________ Prof. Dr. Geraldo Jorge Barbosa de Moura (Orientador) Universidade Federal Rural de Pernambuco (UFRPE) _________________________________________ Prof. Dr. Marcio Mendes Universidade Federal do Ceará (UFC) _________________________________________ Prof. Dr. Marcos Antônio Leite do Nascimento Universidade Federal do Rio Grande do Norte (UFRN) _________________________________________ Prof. Dr Kleberson de Oliveira Porpino Universidade do Estado do Rio Grande do Norte (UERN) ________________________________________ Dra Pâmela Moura Universidade Federal do Ceará (UFC) 5 A Deus.
    [Show full text]
  • Evolution of the Insects
    CY501-C14[607-645].qxd 2/16/05 1:16 AM Page 607 quark11 27B:CY501:Chapters:Chapter-14: 14InsectsInsects Become Become Modern: The MCretaceousodern: and The Tertiary Periods is ambiguous and controversial, as we will soon discuss. THE CRETACEOUS CretaceousWithout question, and though, the angiosperm radiations opened The Cretaceous Period, 145–65 MYA, is one of the most signif- vast niches that insects exploited supremely well. icant geological periods for insect evolution of the seven The earth was geologically more restless during the Creta- major periods in which insects are preserved. Hexapods ceous than most times in its history. There was dramatic cli- appeared inTe the Devonian;r wingedtiary insects, in the Carbonif- Periodsmate change and tectonic activity, the latter of which resulted erous; and the earliest members of most modern orders, in in widespread volcanism and the splitting and drifting of the Permian to Triassic. In the Cretaceous, however, there continents. The fragmentation of Gondwana into the present evolved a nascent modern biota, amidst unprecedented southern continents 120–100 MYA is often invoked to explain geological and evolutionary episodes. Because the Creta- contemporary distributions of various plants and animals ceous is so much younger than the Paleozoic and earlier (including insects) that have closely related species occupy- Mesozoic periods, the fossil record of this period has been ing Australia, New Zealand, southern South America, and erased less by faulting, erosion, and other earth processes. southern Africa. Ancestors of these austral relicts purportedly Thus, Cretaceous fossils have left a particularly vivid record drifted with the continents, though some Cretaceous and of radiations and extinctions.
    [Show full text]
  • Burmese Amber Taxa
    Burmese (Myanmar) amber taxa, on-line checklist v.2018.1 Andrew J. Ross 15/05/2018 Principal Curator of Palaeobiology Department of Natural Sciences National Museums Scotland Chambers St. Edinburgh EH1 1JF E-mail: [email protected] http://www.nms.ac.uk/collections-research/collections-departments/natural-sciences/palaeobiology/dr- andrew-ross/ This taxonomic list is based on Ross et al (2010) plus non-arthropod taxa and published papers up to the end of April 2018. It does not contain unpublished records or records from papers in press (including on- line proofs) or unsubstantiated on-line records. Often the final versions of papers were published on-line the year before they appeared in print, so the on-line published year is accepted and referred to accordingly. Note, the authorship of species does not necessarily correspond to the full authorship of papers where they were described. The latest high level classification is used where possible though in some cases conflicts were encountered, usually due to cladistic studies, so in these cases an older classification was adopted for convenience. The classification for Hexapoda follows Nicholson et al. (2015), plus subsequent papers. † denotes extinct orders and families. New additions or taxonomic changes to the previous list (v.2017.4) are marked in blue, corrections are marked in red. The list comprises 37 classes (or similar rank), 99 orders (or similar rank), 510 families, 713 genera and 916 species. This includes 8 classes, 64 orders, 467 families, 656 genera and 849 species of arthropods. 1 Some previously recorded families have since been synonymised or relegated to subfamily level- these are included in parentheses in the main list below.
    [Show full text]