In Burmese Amber

Total Page:16

File Type:pdf, Size:1020Kb

In Burmese Amber PROC. ENTOMOL. SOC. WASH. 109(3), 2007, pp. 649–655 LONGIOCULUS BURMENSIS, N. GEN., N. SP. (ORTHOPTERA: ELCANIDAE) IN BURMESE AMBER GEORGE POINAR,JR., ANDREJ V. GOROCHOV, AND RON BUCKLEY (GP) Department of Zoology, Oregon State University, Corvallis, OR 97331, U.S.A. (e-mail: [email protected]); (AG) Zoological Institute, Russian Academy of Sciences, S. Petersburg 199034, Russia (e-mail: [email protected]); (RB) 9635 Sumpter Road, Florence, KY 41042-8355, U.S.A. (e-mail: [email protected]) Abstract.—An adult orthopteran in Early Cretaceous Burmese amber is described as a new genus and species, Longioculus burmensis Poinar, Gorochov, and Buckley.On the basis of its tegminal venation, three-segmented tarsi, and large spines on the hind tibia, it is placed in the extinct family Elcanidae. This fossil differs from previously described members of the family by its relatively small and slender body, protruding eyes, enlarged scapes and antennal cavities, short pronotum, and unique venational and leg armament characters. Key Words: Orthoptera, Elcanidae, Longioculus, Longioculus burmensis, Burmese amber, Early Cretaceous Adult orthopterans in amber are rare, unpublished research 2002). Palyno- since these insects are usually strong morphs from the amber beds where the enough to free themselves from the resin. fossil originated have been assigned to the A well-preserved Burmese amber orthop- Upper Albian of the Lower Cretaceous teroid previously depicted in Poinar et al. (,100 mya) (Cruickshank and Ko 2003); (2005) is the topic of this paper. The however, since the amber is secondarily specimen has three-segmented tarsi, deposited, the age could be older. a short pronotum, enlarged hind femora, The piece of amber containing the and venational characters that align it specimen is rectangular in shape, mea- with members of the family Elcanidae suring 13 mm in length, 10 mm in width (Sharov 1968; Carpenter 1992; Gorochov and 6 mm in depth. The fossil is well 1995; Gorochov and Rasnitsyn 2002). preserved and complete except for the tips of the antennae and wings, one side MATERIALS AND METHODS of the apex of the abdomen (including Amber from Burma occurs in lignitic one cercus and the genital apparatus), seams in sandstone-limestone deposits in the left metatibia and metatarsus and the the Hukawng Valley, southwest of Main- apical portion of the right metatibia. gkhwan in the state of Kachin (26u209N, Other fossils in the same amber piece are 96u369E). Nuclear magnetic resonance three small adult beetles, one mite, one (NMR) spectra of amber samples taken adult nematoceran and several branched from the same locality as the fossils plant hairs. Observations and photo- indicated an araucarian (possibly Agathis) graphs were made with a Nikon SMZ- source of the amber (Lambert and Wu, 10 stereoscopic microscope and Nikon Proceedings of the Entomological Society of Washington went-109-03-13.3d 10/4/07 11:01:34 649 Cust # 06- 650 PROCEEDINGS OF THE ENTOMOLOGICAL SOCIETY OF WASHINGTON Proceedings of the Entomological Society of Washington went-109-03-13.3d 10/4/07 11:01:35 650 Cust # 06- VOLUME 109, NUMBER 3 651 Optiphot optical microscope (with mag- Cretaceous Cratoelcana Martins- Neto nifications up to 6503). (Martins-Neto 1991), by the apices of the branches of tegminal ‘‘C’’ positioned Family Elcanidae Handlirsch, 1906 within a short distance of each other and Longioculis Poinar, Gorochov, and the most proximal crossvein in the area Buckley, new genus between R+ RS (possibly the basal part of RS) situated near the bases of the third and Description.—Body relatively small fourth branches of RA. From Cratoelcana, and slender; scapes and antennal cavities with species over 20 mm in length, the new greatly enlarged, occupying entire area genus differs in being much smaller (under between compound eyes; compound eyes 8mminlength). large, protruding from head; ocelli lack- Type species.—Longioculis burmensis, ing; pronotum short, hind tibia with n. sp. dorsal row of denticles and row of much larger spines in middle part (and possibly Longioculis burmensis Poinar, Gorochov, in distal part); ventral surface of hind and Buckley, new species basitarsus with row of rather long spines; tegmina with both branches of false (Figs. 1–12) costa (‘‘C’’) meeting within short dis- Description.—Characters as listed un- tance of each other on anterior wing der generic description. Alate male; body margin; tegminal area between ‘‘C’’ and brown with transparent wing; length Sc narrow; tegminal crossveins in visible body, 7.14 mm; length pronotum, 2.4 area between R+ RA reduced (most mm; length hind femur, 6.4 mm. proximal crossvein in the area, possibly Head: Narrow; without rostral tuber- basal part of RS, situated between bases cles between antennal cavities; ocelli not of third and fourth branches of RA). observed; antennal cavities in contact with Etymology.—‘‘Longioculis’’ is from each other, with edges prominent; anten- the Latin ‘‘oculus’’ for eye and ‘‘longus’’ nal scapes enlarged; antennal flagellum for long, in reference to the protruding longer than body (both antennae cut off at eyes. The gender is masculine. edge of amber piece); filiform; antenno- Diagnosis.—On the basis of the nar- meres short, equal or subequal in size; row, large spines on the hind tibiae, the each antennomere bears one to several new genus may belong to the Late spines; genae narrow; clypeus and mouth- Jurassic-Early Cretaceous subfamily Elca- parts more or less normal for Ensifera ninae (5 Baisselcaninae). Longioculis is (only lower edge of labrum exposed). similarinsizetotheEarlyCretaceous Thorax: Pronotum saddle-shaped, with genus Minelcana Gorochov, Jarzembow- anterior margin convex; pronotal dorsum sky, and Coram (Gorochov et al. 2006) with seven circular light blotches with and the smallest species of the Early dark borders located in depressions sym- Cretaceous genus Panorpidium Westwood metrically positioned on each side; hind (Westwood 1854), but can be distinguished part of pronotum convex, not prolonged from both these genera as well as from over abdomen; legs covered with short other genera of Elcanidae, except the Early hairs; fore- and midfemora with pair of r Figs. 1–4. Longioculis burmensis in Burmese amber. 1, Lateral view of entire specimen. Bar 5 1.6 mm. 2, Metatarsus showing long spine (arrow) and two denticles (arrowheads). Bar 5 88 mm. 3, Dorsal view of anterior portion showing protruding eyes (arrows) and round colored areas on pronotum. Bar 5 542 mm. 4, Portion of antenna showing scattered setae. Bar 5 63 mm. Proceedings of the Entomological Society of Washington went-109-03-13.3d 10/4/07 11:01:55 651 Cust # 06- 652 PROCEEDINGS OF THE ENTOMOLOGICAL SOCIETY OF WASHINGTON Proceedings of the Entomological Society of Washington went-109-03-13.3d 10/4/07 11:01:56 652 Cust # 06- VOLUME 109, NUMBER 3 653 Figs. 10–12. Longioculis burmensis in Burmese amber. 10, Venation of tegmina. Dotted portions represent reconstructed areas. Bar 5 1 mm. 11, Frontal view showing protruding eyes, prominent antennal cavities and enlarged antennal scapes. Bar 5 1 mm. 12, Hind leg showing denticles and spines on dorsal surface of metatibia and spines on ventral surface of basitarsus. Dotted portions represent reconstructed areas. Bar 5 1 mm. rounded apical lobules, lacking denticles; dorsal surface bearing single row of small fore tibia with single apical outer spine; denticles from 25–31 mminheightand mid- and hind tibiae with pair of apical 25–31 mm in width at base; distance spines; basal portion of hind tibia on between denticles 201–246 mm; denticles r Figs. 5–9. Longioculis burmensis in Burmese amber. 5, Frontal view. Bar 5 375 mm. 6, Mouthparts. Bar 5 700 mm. 7, Metatarsus (arrow points to small spines on first tarsal segment of metatarsus) and mesotarsus (arrowhead). Note rows of large spines opposite small spines on ventral surface of basimetatarsus. Bar 5 800 mm. 8, Denticles on proximal portion of metatibia. Bar 5 575 mm. 9. Portion of abdomen showing remaining cercus. Bar 5 800 mm. Proceedings of the Entomological Society of Washington went-109-03-13.3d 10/4/07 11:02:20 653 Cust # 06- 654 PROCEEDINGS OF THE ENTOMOLOGICAL SOCIETY OF WASHINGTON replaced on middle part (and possibly on suggests that the entire distal portion distal part) of dorsal surface of hind tibia contained a row of large spines, which is by large spines (only one complete spine, typical for elcanids. The depressed col- 265 mm long and 63 mmwide,andone ored areas on the dorsum of the prono- partial second spine visible); distance tum probably served as camouflage. between first and second large tibial spines, 315 mm; all tarsi with first segment longer DISCUSSION than 2nd and 3rd combined; apex of all Fossils of the superfamily Elcanoidea basitarsi with 2 pairs of apical spines; first appeared in the Early Permian and midtarsus very short, less than J as long extended into the mid-Cretaceous. Mem- as basitarsus; third tarsal segments with bers of the grasshopper-appearing family well- developed, simple, slightly curved Elcanidae first appeared in the Early claws; arolium absent; fore- and midbasi- Jurassic and representatives of the sub- tarsi with 2 rows of short spines on dorsal family Elcaninae, which ranged from and ventral surfaces; hind basitarsus with Siberia to England and Brazil, were rather two rows of spines, dorsal row composed common in Lower Cretaceous localities of 27 short spines and ventral row with 7 (Martins-Neto 1991; Gorochov 1995; large spines; midtarsus without spines; Gorochov and Rasnitsyn 2002). The tegmina membranous (wings folded); ve- small size of Longioculis may indicate nation as shown in Fig. 10; tegmina how it became entrapped in amber. coloration light (transparent) with dark veins and clear area between first and second branches of RA. ACKNOWLEDGMENTS Abdomen: Short, robust; cercus slen- We thank Jim Davis for supplying the der, pointed, approximately 1/3 length of amber, J.
Recommended publications
  • 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]
  • The Strawberry Bank Lagerstätte Reveals Insights Into Early Jurassic Lifematt Williams, Michael J
    XXX10.1144/jgs2014-144M. Williams et al.Early Jurassic Strawberry Bank Lagerstätte 2015 Downloaded from http://jgs.lyellcollection.org/ by guest on September 27, 2021 2014-144review-articleReview focus10.1144/jgs2014-144The Strawberry Bank Lagerstätte reveals insights into Early Jurassic lifeMatt Williams, Michael J. Benton &, Andrew Ross Review focus Journal of the Geological Society Published Online First doi:10.1144/jgs2014-144 The Strawberry Bank Lagerstätte reveals insights into Early Jurassic life Matt Williams1, Michael J. Benton2* & Andrew Ross3 1 Bath Royal Literary and Scientific Institution, 16–18 Queen Square, Bath BA1 2HN, UK 2 School of Earth Sciences, University of Bristol, Bristol BS8 2BU, UK 3 National Museum of Scotland, Chambers Street, Edinburgh EH1 1JF, UK * Correspondence: [email protected] Abstract: The Strawberry Bank Lagerstätte provides a rich insight into Early Jurassic marine vertebrate life, revealing exquisite anatomical detail of marine reptiles and large pachycormid fishes thanks to exceptional preservation, and especially the uncrushed, 3D nature of the fossils. The site documents a fauna of Early Jurassic nektonic marine animals (five species of fishes, one species of marine crocodilian, two species of ichthyosaurs, cephalopods and crustaceans), but also over 20 spe- cies of insects. Unlike other fossil sites of similar age, the 3D preservation at Strawberry Bank provides unique evidence on palatal and braincase structures in the fishes and reptiles. The age of the site is important, documenting a marine ecosystem during recovery from the end-Triassic mass extinction, but also exactly coincident with the height of the Toarcian Oceanic Anoxic Event, a further time of turmoil in evolution.
    [Show full text]
  • 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.
    [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]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • Amber! Conrad C
    AMBER! CONRAD C. LABANDEIRA! Department of Paleobiology, National Museum of Natural History, Smithsonian Institution Washington, D.C. 20013 USA ˂[email protected]! ˃ and! Department of Entomology, University of Maryland, College Park, MD 20742 USA ABSTRACT.—The amber fossil record provides a distinctive, 320-million-year-old taphonomic mode documenting gymnosperm, and later, angiosperm, resin-producing taxa. Resins and their subfossil (copal) and fossilized (amber) equivalents are categorized into five classes of terpenoid, phenols, and other compounds, attributed to extant family-level taxa. Copious resin accumulations commencing during the early Cretaceous are explained by two hypotheses: 1) abundant resin production as a byproduct of plant secondary metabolism, and 2) induced and constitutive host defenses for warding off insect pest and pathogen attack through profuse resin production. Forestry research and fossil wood-boring damage support a causal relationship between resin production and pest attack. Five stages characterize taphonomic conversion of resin to amber: 1) Resin flows initially caused by biotic or abiotic plant-host trauma, then resin flowage results from sap pressure, resin viscosity, solar radiation, and fluctuating temperature; 2) entrapment of live and dead organisms, resulting in 3) entombment of organisms; then 4) movement of resin clumps to 5) a deposition site. This fivefold diagenetic process of amberization results in resin→copal→amber transformation from internal biological and chemical processes and external geological forces. Four phases characterize the amber record: a late Paleozoic Phase 1 begins resin production by cordaites and medullosans. A pre-mid-Cretaceous Mesozoic Phase 2 provides increased but still sparse accumulations of gymnosperm amber. Phase 3 begins in the mid-early Cretaceous with prolific amber accumulation likely caused by biotic effects of an associated fauna of sawflies, beetles, and pathogens.
    [Show full text]
  • David A. Grimaldi
    1 David A. Grimaldi January, 2019 Division of Invertebrate Zoology American Museum of Natural History Central Park West at 79th Street New York, New York 10024-5192 Telephone: 212-769-5615, -5277 (fax) Email: [email protected] RESEARCH INTERESTS Diversity, fossil record, and evolution of insects; fossilization in amber; systematics of Drosophilidae and other Diptera; evolution of sociality in insects; insect pollination and its evolutionary history; the evolution of biological communities, particularly tropical forests; extinction and environmental deterioration; history of science; biological illustration and imaging. EDUCATION B.Sc., 1979, University of Connecticut. Major concentrations in Biology and Fine Arts. M.Sc., 1983, State University of New York, Binghamton. Evolutionary Biology. Ph.D., 1986, Cornell University. Entomology. POSITIONS 1986–1991: Assistant Curator, American Museum of Natural History. 1988–present: Adjunct Professor, City University of New York. (Graduate Program in Ecology and Evolutionary Biology) 1991–1996: Associate Curator (tenured), American Museum of Natural History. 1994–1999: Chairman, Department of Entomology, American Museum of Natural History. 1994–present: Adjunct Professor, Cornell University (Department of Entomology). 1995–present: Adjunct Professor, Columbia University. (Department of Ecology, Evolution, and Environmental Biology). 1996–present: Curator, American Museum of Natural History. 2008–present: Professor, Gilder Graduate School, Program in Comparative Biology, American Museum of Natural History. TEACHING AND MENTORING*: last 10 years GRADUATE STUDENT COMMITTEES/MENTORING (Major Advisor): Caroline S. Chaboo, Ph.D., 2005, Cornell University: Systematics of cassidine Chrysomelidae (tortoise beetles). Presently: Assistant Professor, University of Kansas. Sara Lubkin, Ph.D., 2007, Cornell University: Systematics and paleontology of Paleozoic and Mesozoic Archostemata (Coleoptera). Craig Gibbs, Ph.D., 2007, CUNY: Patterns of drosophilid fly species diversity and abundance in Neotropical forest canopies.
    [Show full text]
  • Art 09 Rafael
    “DEATH BEHAVIOUR” – THANATOETHOLOGY, NEW TERM AND CONCEPT: A TAPHONOMIC ANALYSIS PROVIDING POSSIBLE PALEOETHOLOGIC INFERENCES. SPECIAL CASES FROM ARTHROPODS OF THE SANTANA FORMATION (LOWER CRETACEOUS, NORTHEAST BRAZIL) Rafael Gioia MARTINS-NETO 1 & Oscar Florencio GALLEGO 2 (1) Professor Visitante, Programa de Pós-graduação em Ciências Biológicas, Comportamento e Biologia Animal, Universidade Federal de Juiz de Fora (UFJF). Campus Universitário Martelos. CEP 36036-900. Juiz de Fora, MG. E-mail: [email protected]. (2) Paleontología, Facultad de Ciencias Exactas y Naturales y Agrimensura, Universidad Nacional del Nordeste, y Área Paleontología, Centro de Ecología Aplicada del Litoral (CONICET). Casilla de Correo 128, 3400. Corrientes, Argentina. E-mail: [email protected]. Introduction The Multivariate Premises Responsible for the Santana Formation Lagerstätten The Selected Preserved Arthropod Groups and its Taphonomic Peculiarities What is the Paleoecological Importance in Know if the Specimen Arrived Live or Death in the Depositional Site? The “Movies Effect”: The Death Step by Step Paleoethology: the Distinct Faces of the Animal Behaviour Tanatosis (Death Simulation – To Fake of Dead) The Death Behaviour: Thanatoethology, a New Concept Application to the Paleoichnology Bibliographic References ABSTRACT – A new concept, thanatoethology, is proposed and several peculiarities of the Santana Formation (Lower Cretaceous, Northeast Brazil) taphocenosis are analysed. Thanatoethology refers to the identification, interpretation and study of a specific behaviour performed by an organism moments before its definitive death, and also before the beginning of the fossilization process. This behaviour expresses agony, often due to asphyxia in land, air or water, and can be expressed in fossils as well as ichnofossils. The death behaviour in several cases can be associated with a mass mortality event and can be an extremely useful tool for paleoecological and paleoethological analysis.
    [Show full text]
  • Paleocene of Menat Formation, France, Reveals an Extraordinary Diversity of Orthopterans and the Last Known Survivor of a Mesozoic Elcanidae
    Paleocene of Menat Formation, France, reveals an extraordinary diversity of orthopterans and the last known survivor of a Mesozoic Elcanidae THOMAS SCHUBNEL, LAURE DESUTTER-GRANDCOLAS, ROMAIN GARROUSTE, SOPHIE HERVET, and ANDRÉ NEL Schubnel, T., Desutter-Grandcolas, L., Garrouste, R., Hervet, S., and Nel, A. 2020. Paleocene of Menat Formation, France, reveals an extraordinary diversity of orthopterans and the last known survivor of a Mesozoic Elcanidae. Acta Palaeontologica Polonica 65 (2): 371–385. 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. Key words: Insecta, Ensifera, Elcanoidea, Acridoidea, Eumastacoidea, Paleogene, France.
    [Show full text]
  • Arthropod Paleobiology
    ARTHROPOD PALEOBIOLOGY SHORT COURSES IN PALEONTOLOGY NUMBER 3 1990 convened by Donald G, Mikulic Stephen J. Culver, Series Editor A Publication of The Paleontological Society Arthropod Terrestriality Conrad C. Labandeira Department of Plant Biology University of Illinois Urbana, Illinois 61801 and Bret S. Beall Department of Geology Field Museum of Natural History Chicago, Illinois 60605 INTRODUCTION Since the late Paleozoic, insects and arachnids have diversified in the terrestrial world so spectacularly that they have become unquestionably the most diverse group of organisms to ever inhabit the planet. In fact, this 300 million year interval may appropriately be referred to as the age of arthropods. What is the origin and history of terrestrial arthropods? How is arthropod diversity maintained on land? In this rhetorical context we will discuss (1) the degree to which terrestriality is found in arthropods, (2) the physiological barriers to terrestrialization that arthropod clades confronted, (3) the historical record of arthropod diversity on land based on paleobiological, comparative physiological and zoogeographical evidence, and (4) some tentative answers to the "why" of terrestrial arthropod success. We are providing a geochronologic scope to terrestriality that includes not only the early history of terrestrial arthropods, but also the subsequent expansion of arthropods into major terrestrial habitats. The term "terrestrial" has been used in various contexts to refer to land but may or may not include freshwater. Therefore, clarifications of the term must be made. From the Latin, "terrestrial" both denotes and connotes land, and it is in this more restrictive sense that we are using the term. Freshwater ecosystems are excluded here, although those land-based habitats that are frequently moist (e.g., humus, leaf litter, cloud forest canopies, carrion, dung) are included.
    [Show full text]
  • The First Elcanidae (Orthoptera, Elcanoidea) from the Daohugou Fossil Bed of Northeastern China
    A peer-reviewed open-access journal ZooKeys 897: 19–28Elcanidae (2019) (Orthoptera, Elcanoidea) from the Daohugou fossil bed of China 19 doi: 10.3897/zookeys.897.37608 SHORT COMMUNICATION http://zookeys.pensoft.net Launched to accelerate biodiversity research The first Elcanidae (Orthoptera, Elcanoidea) from the Daohugou fossil bed of northeastern China He Tian1, Jun-Jie Gu2, Xiang Chu Yin3,4, Dong Ren1 1 College of Life Sciences, Capital Normal University, 105 Xisanhuanbeilu, Haidian District, Beijing, 100048, China 2 Institute of Ecological Agriculture, College of Agronomy, Sichuan Agricultural University, Chengdu, Sichuan, 611130, China 3 Northwest Institute of Plateau Biology, Chinese Academy of Sciences, 23, Xinning Road, 810008, Xining, China 4 College of Life Sciences, Hebei University, Baoding, 071002, China Corresponding author: Jun-Jie Gu ([email protected]) Academic editor: F. Montealegre-Z | Received 22 June 2019 | Accepted 1 November 2019 | Published 9 December 2019 http://zoobank.org/3CA86E3F-9828-4E1F-A065-B14C3417A851 Citation: Tian H, Gu J-J, Yin XC, Ren D (2019) The first Elcanidae (Orthoptera, Elcanoidea) from the Daohugou fossil bed of northeastern China. ZooKeys 897: 19–28. https://doi.org/10.3897/zookeys.897.37608 Abstract A new species of Elcanidae (Orthoptera, Elcanoidea), Parelcana pulchmacula sp. nov., is described based on four new specimens from the Middle Jurassic Jiulongshan Formation of northeastern China. The new species differs from all other known Archelcaninae species by its combination of wing-venation characters. This new finding improves our knowledge of variation on wing venation in elcanid insects and constitutes the first record of Elcanidae from the Daohugou fossil bed (Yanliao Biota) of northeastern China.
    [Show full text]