From the Middle Jurassic of Daohugou, Inner Mongolia, China
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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). -
Universidade Federal Do Ceará Centro De Ciências Departamento De Geologia Programa De Pós-Graduação Em Geologia Luís Carlo
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 (Interno) Universidade Federal do Ceará (UFC) _________________________________________ Prof. Dr. Marcos Antônio Leite do Nascimento (Externo) Universidade Federal do Rio Grande do Norte (UFRN) _________________________________________ Prof. Dr Kleberson de Oliveira Porpino (Externo) Universidade do Estado do Rio Grande do Norte (UERN) ________________________________________ Dra Pâmela Moura (Externo) Universidade Federal do Ceará (UFC) 5 A Deus. -
Phylogeny and Historical Biogeography of Silky Lacewings (Neuroptera: Psychopsidae)
Systematic Entomology (2018), 43, 43–55 DOI: 10.1111/syen.12247 Phylogeny and historical biogeography of silky lacewings (Neuroptera: Psychopsidae) DEON K. BAKKES* , MERVYN W. MANSELLand CATHERINE L. SOLE Department of Zoology and Entomology, University of Pretoria, Hatfield, South Africa Abstract. Psychopsidae (silky winged lacewings) are a small family of Neuroptera characterized by broad hirsute wings that impart a physical resemblance to moths. The fossil record includes many psychopsid-like taxa from the Late Triassic to Early Oligocene from all major continents. Extant species have a disjunct, tripartite distribution comprising Afrotropical, Southeast Asian and Australian regions that is significant to historical biogeography. Two subfamilies are currently recognized: Zygophlebiinae in the Afrotropics, and Psychopsinae in Australia and Southeast Asia. This study explores phylogeny and historical biogeography of Psychopsidae, using data from biogeography, comparative morphology and molecular sequences (16S, 18S, CAD, COI). Our results show that: (i) the morphological phylogeny is incongruent with molecular data; (ii) Afrotropical Silveira Navás represent a separate lineage that warrants placement in its own subfamily; (iii) the family originated in Pangea; and (iv) the present genus level distribution resulted from two vicariance events associated with Gondwanan fragmentation. Introduction species are known to live under the bark of myrtaceous trees, preying on Microlepidoptera (Tillyard, 1919b; Tjeder, 1960). Psychopsidae Handlirsch -
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. -
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. -
Burmese Amber Taxa
Burmese (Myanmar) amber taxa, on-line checklist v.2017.1 Andrew J. Ross 28/02/2017 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 2016. 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. The list comprises 31 classes (or similar rank), 85 orders (or similar rank), 375 families, 530 genera and 643 species. This includes 6 classes, 54 orders, 342 families, 482 genera and 591 species of arthropods. Some previously recorded families have since been synonymised or relegated to subfamily level- these are included in -
Keynote Presentations Abstracts
6th International Congress on Fossil Insects, Arthropods and Amber Byblos, April 2013 ----------------------------------------------------------------------------------------------------------------------------------- Keynote presentations abstracts - 1 - 6th International Congress on Fossil Insects, Arthropods and Amber Byblos, April 2013 ----------------------------------------------------------------------------------------------------------------------------------- Sic transit gloria mundi: When bad things happen to good bugs Michael S. Engel University of Kansas Natural History Museum & American Museum of Natural History Origination and extinction, the ‘Alpha and Omega’ of Evolution, are the principal factors shaping biological diversity through time and yet the latter is often ignored in phylogenetic studies of insects. Extinct lineages play a dramatic role in revising our concepts of genealogical relationships and the evolution of major biological phenomena. These forgotten extinct clades or grades often rewrite our understanding of biogeographic patterns, timing of episodes of diversification, correlated biological/geological events, and other macroevolutionary trends. Examples are provided throughout the long history of insects of the importance of studying insect fossils, particularly those preserved with such high fidelity in amber, for resolving long- standing questions in entomology. In each example, the need for further integration of paleontological evidence into modern phylogenetic research on insects is emphasized. - 2 -
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. -
The Fossil Record of Plant-Insect Dynamics
EA41CH12-Labandeira ARI 19 April 2013 15:52 The Fossil Record of Plant-Insect Dynamics Conrad C. Labandeira1,2,3,4 and Ellen D. Currano5 1Department of Paleobiology, National Museum of Natural History, Washington, District of Columbia 20013; email: [email protected] 2Department of Geology, Rhodes University, Grahamstown 6140, South Africa 3College of Life Sciences, Capital Normal University, Beijing 100048, China 4Department of Entomology and BEES Program, University of Maryland, College Park, Maryland 20742 5Department of Geology and Environmental Earth Science, Miami University, Oxford, Ohio 45056; email: [email protected] Annu. Rev. Earth Planet. Sci. 2013. 41:287–311 Keywords First published online as a Review in Advance on damage type, end-Cretaceous event, functional feeding group, herbivory, March 7, 2013 Paleocene-Eocene Thermal Maximum, pollination The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: Progress toward understanding the dynamics of ancient plant-insect associa- 10.1146/annurev-earth-050212-124139 tions has addressed major patterns in the ecology and evolution of herbivory Copyright c 2013 by Annual Reviews. and pollination. This advancement involves development of more analyti- All rights reserved Annu. Rev. Earth Planet. Sci. 2013.41:287-311. Downloaded from www.annualreviews.org cal ways of describing plant-insect associational patterns in time and space and an assessment of the role that the environment and internal biologi- cal processes have in their control. Current issues include the deep origins of terrestrial herbivory, the spread of herbivory across late Paleozoic land- by Smithsonian Institution Libraries - National Museum of Natural History Library on 06/05/13. -
A Triassic-Jurassic Window Into the Evolution of Lepidoptera
A Triassic-Jurassic window into the evolution of Lepidoptera Authors: Timo van Eldijk, Torsten Wappler, Paul Klee Strother, Carolien van der Weijst, Hossein Rajaei, Henk Visscher, Bas van de Schootbrugge Persistent link: http://hdl.handle.net/2345/bc-ir:107692 This work is posted on eScholarship@BC, Boston College University Libraries. Published in Science Advances, vol. 4, no. 1, January 2018 Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC) SCIENCE ADVANCES | RESEARCH ARTICLE EVOLUTIONARY BIOLOGY Copyright © 2018 The Authors, some A Triassic-Jurassic window into the evolution rights reserved; exclusive licensee of Lepidoptera American Association for the Advancement 1 2 3 1 of Science. No claim to Timo J. B. van Eldijk, Torsten Wappler, Paul K. Strother, Carolien M. H. van der Weijst, original U.S. Government 4 1 1 Hossein Rajaei, Henk Visscher, Bas van de Schootbrugge * Works. Distributed under a Creative On the basis of an assemblage of fossilized wing scales recovered from latest Triassic and earliest Jurassic sediments Commons Attribution from northern Germany, we provide the earliest evidence for Lepidoptera (moths and butterflies). The diverse scales NonCommercial confirm a (Late) Triassic radiation of lepidopteran lineages, including the divergence of the Glossata, the clade that License 4.0 (CC BY-NC). comprises the vast multitude of extant moths and butterflies that have a sucking proboscis. The microfossils extend the minimum calibrated age of glossatan moths by ca. 70 million years, refuting ancestral association of the group with flowering plants. Development of the proboscis may be regarded as an adaptive innovation to sucking free liquids for maintaining the insect’s water balance under arid conditions. -
Fossil Perspectives on the Evolution of Insect Diversity
FOSSIL PERSPECTIVES ON THE EVOLUTION OF INSECT DIVERSITY Thesis submitted by David B Nicholson For examination for the degree of PhD University of York Department of Biology November 2012 1 Abstract A key contribution of palaeontology has been the elucidation of macroevolutionary patterns and processes through deep time, with fossils providing the only direct temporal evidence of how life has responded to a variety of forces. Thus, palaeontology may provide important information on the extinction crisis facing the biosphere today, and its likely consequences. Hexapods (insects and close relatives) comprise over 50% of described species. Explaining why this group dominates terrestrial biodiversity is a major challenge. In this thesis, I present a new dataset of hexapod fossil family ranges compiled from published literature up to the end of 2009. Between four and five hundred families have been added to the hexapod fossil record since previous compilations were published in the early 1990s. Despite this, the broad pattern of described richness through time depicted remains similar, with described richness increasing steadily through geological history and a shift in dominant taxa after the Palaeozoic. However, after detrending, described richness is not well correlated with the earlier datasets, indicating significant changes in shorter term patterns. Corrections for rock record and sampling effort change some of the patterns seen. The time series produced identify several features of the fossil record of insects as likely artefacts, such as high Carboniferous richness, a Cretaceous plateau, and a late Eocene jump in richness. Other features seem more robust, such as a Permian rise and peak, high turnover at the end of the Permian, and a late-Jurassic rise. -
New Cretaceous Antlion-Like Lacewings Promote a Phylogenetic Reappraisal of the Extinct Myrmeleontoid Family Babinskaiidae
www.nature.com/scientificreports OPEN New Cretaceous antlion‑like lacewings promote a phylogenetic reappraisal of the extinct myrmeleontoid family Babinskaiidae Xiumei Lu1*, Bo Wang2 & Xingyue Liu3* Babinskaiidae is an extinct family of the lacewing superfamily Myrmeleontoidea, currently only recorded from the Cretaceous. The phylogenetic position of this family is elusive, with inconsistent inferences in previous studies. Here we report on three new genera and species of Babinskaiidae from the mid‑Cretaceous Kachin amber of Myanmar, namely Calobabinskaia xiai gen. et sp. nov., Stenobabinskaia punctata gen. et sp. nov., and Xiaobabinskaia lepidotricha gen. et sp. nov. These new babinskaiids are featured by having specialized characters, such as the rich number of presectoral crossveins and the presence of scaly setae on forewing costal vein, which have not yet been found in this family. The exquisite preservation of the Kachin amber babinskaiids facilitate a reappraisal of the phylogenetic placement of this family based on adult morphological characters. Our result from the phylogenetic inference combining the data from fossil and extant myrmeleontoids recovered a monophyletic clade composed of Babinskaiidae and another extinct family Cratosmylidae, and further assigned this clade to be sister group to a clade including Nemopteridae, Palaeoleontidae, and Myrmeleontidae. Babinskaiidae appears to be a transitional lineage between Nymphidae and advanced myrmeleontoids, with ancient morphological diversifcation. Babinskaiidae is an extinct lacewing family belonging to the superfamily Myrmeleontoidea, presently known with 13 species in nine genera 1. Te adults of Babinskaiidae are diagnosed by a combination of characters, including the fliform antennae, the presence of trichosors, the origin of RP + MA far distal to wing base, the presence of presectoral crossveins in both fore- and hind wings, and the reduction of hind wing A2 and A3 veins.