Prof. Yong-Chong Hong: a Chinese Pioneering Palaeoentomologist
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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. -
Neuroptera (Lacewings, Doodlebugs, Antlions)
Return to insect order home Page 1 of 2 Visit us on the Web: www.gardeninghelp.org Insect Order ID: Neuroptera (Lacewings, Doodlebugs, Antlions) Life Cycle–Complete metamorphosis. Adults lay eggs. Larvae eat, grow and molt. This stage is repeated a varying number of times, depending on species, until hormonal changes cause the larvae to pupate. Inside the pupal case, they change in form and color and develop wings. The adults look completely different from the larvae. Adults–Lacewings have clear membranous wings with numerous cells, hence the name Neuroptera "nerve wing." The forewing and hindwing are about the same size. The eyes are large in relationship to the head, like glittering beads. (Click images to enlarge or orange text for more information.) Colors vary Numerous cells in wings Bright beadlike eyes from brown to green Eggs–The eggs of many species are laid at the end of a hairlike stalk. (Click images to enlarge or orange text for more information.) Lacewing eggs laid on a stalk Lacewing egg Return to insect order home Page 2 of 2 Larvae–All are campodeiform, spiny and soft-bodied with large hollow mandibles used to skewer victims and suck them dry. Some species place the dried remains of their victims on the spines on their backs, giving them the appearance of walking trash heaps. (Click images to enlarge or orange text for more information.) Campodeiform Large, hollow mandibles Hidden beneath the spiny, soft-bodied Campodeiform remains of its victim Pupae–All have a pupal stage, usually a silken cocoon, during which the adult, winged form develops. -
The Engineering of the Giant Dragonflies of the Permian: Revised Body Mass, Power, Air Supply, Thermoregulation and the Role of Air Density Alan E
© 2018. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2018) 221, jeb185405. doi:10.1242/jeb.185405 COMMENTARY The engineering of the giant dragonflies of the Permian: revised body mass, power, air supply, thermoregulation and the role of air density Alan E. R. Cannell ABSTRACT abdomen as well as spiny and surprisingly robust legs. Illustrations An engineering examination of allometric and analogical data on the of M. monyi and a female Meganeurula selysii (Shear and flight of giant Permian insects (Protodonata, Meganeura or griffinflies) Kukalova-Peck, 1990) also indicate creatures with strong mouth indicates that previous estimates of the body mass of these insects parts, well-developed pincers and strong long thick legs. In both are too low and that the largest of these insects (wingspan of 70 cm or drawings, the abdomen is similar in diameter to the thorax, unlike more) would have had a mass of 100–150 g, several times greater the structure of most modern dragonflies, which have much more – – than previously thought. Here, the power needed to generate lift and slender abdomens. This large size and consequently high mass fly at the speeds typical of modern large dragonflies is examined has attracted attention for over a hundred years as there are no extant together with the metabolic rate and subsequent heat generated by insects of this size and their physiology in terms of power generation the thoracic muscles. This evaluation agrees with previous work and thermoregulation is not understood. This Commentary suggesting that the larger specimens would rapidly overheat in the examines the questions of mass, power generation to fly and high ambient temperatures assumed in the Permian. -
New Siberian Islands Archipelago)
Detrital zircon ages and provenance of the Upper Paleozoic successions of Kotel’ny Island (New Siberian Islands archipelago) Victoria B. Ershova1,*, Andrei V. Prokopiev2, Andrei K. Khudoley1, Nikolay N. Sobolev3, and Eugeny O. Petrov3 1INSTITUTE OF EARTH SCIENCE, ST. PETERSBURG STATE UNIVERSITY, UNIVERSITETSKAYA NAB. 7/9, ST. PETERSBURG 199034, RUSSIA 2DIAMOND AND PRECIOUS METAL GEOLOGY INSTITUTE, SIBERIAN BRANCH, RUSSIAN ACADEMY OF SCIENCES, LENIN PROSPECT 39, YAKUTSK 677980, RUSSIA 3RUSSIAN GEOLOGICAL RESEARCH INSTITUTE (VSEGEI), SREDNIY PROSPECT 74, ST. PETERSBURG 199106, RUSSIA ABSTRACT Plate-tectonic models for the Paleozoic evolution of the Arctic are numerous and diverse. Our detrital zircon provenance study of Upper Paleozoic sandstones from Kotel’ny Island (New Siberian Island archipelago) provides new data on the provenance of clastic sediments and crustal affinity of the New Siberian Islands. Upper Devonian–Lower Carboniferous deposits yield detrital zircon populations that are consistent with the age of magmatic and metamorphic rocks within the Grenvillian-Sveconorwegian, Timanian, and Caledonian orogenic belts, but not with the Siberian craton. The Kolmogorov-Smirnov test reveals a strong similarity between detrital zircon populations within Devonian–Permian clastics of the New Siberian Islands, Wrangel Island (and possibly Chukotka), and the Severnaya Zemlya Archipelago. These results suggest that the New Siberian Islands, along with Wrangel Island and the Severnaya Zemlya Archipelago, were located along the northern margin of Laurentia-Baltica in the Late Devonian–Mississippian and possibly made up a single tectonic block. Detrital zircon populations from the Permian clastics record a dramatic shift to a Uralian provenance. The data and results presented here provide vital information to aid Paleozoic tectonic reconstructions of the Arctic region prior to opening of the Mesozoic oceanic basins. -
New Insects from the Earliest Permian of Carrizo Arroyo (New Mexico, USA) Bridging the Gap Between the Carboniferous and Permian Entomofaunas
Insect Systematics & Evolution 48 (2017) 493–511 brill.com/ise New insects from the earliest Permian of Carrizo Arroyo (New Mexico, USA) bridging the gap between the Carboniferous and Permian entomofaunas Jakub Prokopa,* and Jarmila Kukalová-Peckb aDepartment of Zoology, Faculty of Science, Charles University, Viničná 7, CZ-128 43 Praha 2, Czech Republic bEntomology, Canadian Museum of Nature, Ottawa, ON, Canada K1P 6P4 *Corresponding author, e-mail: [email protected] Version of Record, published online 7 April 2017; published in print 1 November 2017 Abstract New insects are described from the early Asselian of the Bursum Formation in Carrizo Arroyo, NM, USA. Carrizoneura carpenteri gen. et sp. nov. (Syntonopteridae) demonstrates traits in hindwing venation to Lithoneura and Syntonoptera, both known from the Moscovian of Illinois. Carrizoneura represents the latest unambiguous record of Syntonopteridae. Martynovia insignis represents the earliest evidence of Mar- tynoviidae. Carrizodiaphanoptera permiana gen. et sp. nov. extends range of Diaphanopteridae previously restricted to Gzhelian. The re-examination of the type speciesDiaphanoptera munieri reveals basally coa- lesced vein MA with stem of R and RP resulting in family diagnosis emendation. Arroyohymen splendens gen. et sp. nov. (Protohymenidae) displays features in venation similar to taxa known from early and late Permian from the USA and Russia. A new palaeodictyopteran wing attributable to Carrizopteryx cf. arroyo (Calvertiellidae) provides data on fore wing venation previously unknown. Thus, all these new discoveries show close relationship between late Pennsylvanian and early Permian entomofaunas. Keywords Ephemeropterida; Diaphanopterodea; Megasecoptera; Palaeodictyoptera; gen. et sp. nov; early Asselian; wing venation Introduction The fossil record of insects from continental deposits near the Carboniferous-Permian boundary is important for correlating insect evolution with changes in climate and in plant ecosystems. -
Plate Tectonic Regulation of Global Marine Animal Diversity
Plate tectonic regulation of global marine animal diversity Andrew Zaffosa,1, Seth Finneganb, and Shanan E. Petersa aDepartment of Geoscience, University of Wisconsin–Madison, Madison, WI 53706; and bDepartment of Integrative Biology, University of California, Berkeley, CA 94720 Edited by Neil H. Shubin, The University of Chicago, Chicago, IL, and approved April 13, 2017 (received for review February 13, 2017) Valentine and Moores [Valentine JW, Moores EM (1970) Nature which may be complicated by spatial and temporal inequities in 228:657–659] hypothesized that plate tectonics regulates global the quantity or quality of samples (11–18). Nevertheless, many biodiversity by changing the geographic arrangement of conti- major features in the fossil record of biodiversity are consis- nental crust, but the data required to fully test the hypothesis tently reproducible, although not all have universally accepted were not available. Here, we use a global database of marine explanations. In particular, the reasons for a long Paleozoic animal fossil occurrences and a paleogeographic reconstruction plateau in marine richness and a steady rise in biodiversity dur- model to test the hypothesis that temporal patterns of continen- ing the Late Mesozoic–Cenozoic remain contentious (11, 12, tal fragmentation have impacted global Phanerozoic biodiversity. 14, 19–22). We find a positive correlation between global marine inverte- Here, we explicitly test the plate tectonic regulation hypothesis brate genus richness and an independently derived quantitative articulated by Valentine and Moores (1) by measuring the extent index describing the fragmentation of continental crust during to which the fragmentation of continental crust covaries with supercontinental coalescence–breakup cycles. The observed posi- global genus-level richness among skeletonized marine inverte- tive correlation between global biodiversity and continental frag- brates. -
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. -
Is Ellipura Monophyletic? a Combined Analysis of Basal Hexapod
ARTICLE IN PRESS Organisms, Diversity & Evolution 4 (2004) 319–340 www.elsevier.de/ode Is Ellipura monophyletic? A combined analysis of basal hexapod relationships with emphasis on the origin of insects Gonzalo Giribeta,Ã, Gregory D.Edgecombe b, James M.Carpenter c, Cyrille A.D’Haese d, Ward C.Wheeler c aDepartment of Organismic and Evolutionary Biology, Museum of Comparative Zoology, Harvard University, 16 Divinity Avenue, Cambridge, MA 02138, USA bAustralian Museum, 6 College Street, Sydney, New South Wales 2010, Australia cDivision of Invertebrate Zoology, American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024, USA dFRE 2695 CNRS, De´partement Syste´matique et Evolution, Muse´um National d’Histoire Naturelle, 45 rue Buffon, F-75005 Paris, France Received 27 February 2004; accepted 18 May 2004 Abstract Hexapoda includes 33 commonly recognized orders, most of them insects.Ongoing controversy concerns the grouping of Protura and Collembola as a taxon Ellipura, the monophyly of Diplura, a single or multiple origins of entognathy, and the monophyly or paraphyly of the silverfish (Lepidotrichidae and Zygentoma s.s.) with respect to other dicondylous insects.Here we analyze relationships among basal hexapod orders via a cladistic analysis of sequence data for five molecular markers and 189 morphological characters in a simultaneous analysis framework using myriapod and crustacean outgroups.Using a sensitivity analysis approach and testing for stability, the most congruent parameters resolve Tricholepidion as sister group to the remaining Dicondylia, whereas most suboptimal parameter sets group Tricholepidion with Zygentoma.Stable hypotheses include the monophyly of Diplura, and a sister group relationship between Diplura and Protura, contradicting the Ellipura hypothesis.Hexapod monophyly is contradicted by an alliance between Collembola, Crustacea and Ectognatha (i.e., exclusive of Diplura and Protura) in molecular and combined analyses. -
Prey Recognition in Larvae of the Antlion Euroleon Nostras (Neuroptera, Myrrneleontidae)
Acta Zool. Fennica 209: 157-161 ISBN 95 1-9481-54-0 ISSN 0001-7299 Helsinki 6 May 1998 O Finnish Zoological and Botanical Publishing Board 1998 Prey recognition in larvae of the antlion Euroleon nostras (Neuroptera, Myrrneleontidae) Bojana Mencinger Mencinger, B., Department of Biology, University ofMaribor, Koro&a 160, SLO-2000 Maribor, Slovenia Received 14 July 1997 The behavioural responses of the antlion larva Euroleon nostras to substrate vibrational stimuli from three species of prey (Tenebrio molitor, Trachelipus sp., Pyrrhocoris apterus) were studied. The larva reacted to the prey with several behavioural patterns. The larva recognized its prey at a distance of 3 to 15 cm from the rim of the pit without seeing it, and was able to determine the target angle. The greatest distance of sand tossing was 6 cm. Responsiveness to the substrate vibration caused by the bug Pyrrhocoris apterus was very low. 1. Introduction efficient motion for antlion is to toss sand over its back (Lucas 1989). When the angle between the The larvae of the European antlion Euroleon head in resting position and the head during sand nostras are predators as well as the adults. In loose tossing is 4S0, the section of the sand tossing is substrate, such as dry sand, they construct coni- 30" (Koch 1981, Koch & Bongers 1981). cal pits. At the bottom of the pit they wait for the Sensitivity to vibration in sand has been stud- prey, which slides into the trap. Only the head ied in a few arthropods, e.g. in the nocturnal scor- and sometimes the pronotum of the larva are vis- pion Paruroctonus mesaensis and the fiddler crab ible; the other parts of the body are covered with Uca pugilator. -
Appendix A. Supplementary Material
Appendix A. Supplementary material Comprehensive taxon sampling and vetted fossils help clarify the time tree of shorebirds (Aves, Charadriiformes) David Cernˇ y´ 1,* & Rossy Natale2 1Department of the Geophysical Sciences, University of Chicago, Chicago 60637, USA 2Department of Organismal Biology & Anatomy, University of Chicago, Chicago 60637, USA *Corresponding Author. Email: [email protected] Contents 1 Fossil Calibrations 2 1.1 Calibrations used . .2 1.2 Rejected calibrations . 22 2 Outgroup sequences 30 2.1 Neornithine outgroups . 33 2.2 Non-neornithine outgroups . 39 3 Supplementary Methods 72 4 Supplementary Figures and Tables 74 5 Image Credits 91 References 99 1 1 Fossil Calibrations 1.1 Calibrations used Calibration 1 Node calibrated. MRCA of Uria aalge and Uria lomvia. Fossil taxon. Uria lomvia (Linnaeus, 1758). Specimen. CASG 71892 (referred specimen; Olson, 2013), California Academy of Sciences, San Francisco, CA, USA. Lower bound. 2.58 Ma. Phylogenetic justification. As in Smith (2015). Age justification. The status of CASG 71892 as the oldest known record of either of the two spp. of Uria was recently confirmed by the review of Watanabe et al. (2016). The younger of the two marine transgressions at the Tolstoi Point corresponds to the Bigbendian transgression (Olson, 2013), which contains the Gauss-Matuyama magnetostratigraphic boundary (Kaufman and Brigham-Grette, 1993). Attempts to date this reversal have been recently reviewed by Ohno et al. (2012); Singer (2014), and Head (2019). In particular, Deino et al. (2006) were able to tightly bracket the age of the reversal using high-precision 40Ar/39Ar dating of two tuffs in normally and reversely magnetized lacustrine sediments from Kenya, obtaining a value of 2.589 ± 0.003 Ma. -
Diptera) Diversity in a Patch of Costa Rican Cloud Forest: Why Inventory Is a Vital Science
Zootaxa 4402 (1): 053–090 ISSN 1175-5326 (print edition) http://www.mapress.com/j/zt/ Article ZOOTAXA Copyright © 2018 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4402.1.3 http://zoobank.org/urn:lsid:zoobank.org:pub:C2FAF702-664B-4E21-B4AE-404F85210A12 Remarkable fly (Diptera) diversity in a patch of Costa Rican cloud forest: Why inventory is a vital science ART BORKENT1, BRIAN V. BROWN2, PETER H. ADLER3, DALTON DE SOUZA AMORIM4, KEVIN BARBER5, DANIEL BICKEL6, STEPHANIE BOUCHER7, SCOTT E. BROOKS8, JOHN BURGER9, Z.L. BURINGTON10, RENATO S. CAPELLARI11, DANIEL N.R. COSTA12, JEFFREY M. CUMMING8, GREG CURLER13, CARL W. DICK14, J.H. EPLER15, ERIC FISHER16, STEPHEN D. GAIMARI17, JON GELHAUS18, DAVID A. GRIMALDI19, JOHN HASH20, MARTIN HAUSER17, HEIKKI HIPPA21, SERGIO IBÁÑEZ- BERNAL22, MATHIAS JASCHHOF23, ELENA P. KAMENEVA24, PETER H. KERR17, VALERY KORNEYEV24, CHESLAVO A. KORYTKOWSKI†, GIAR-ANN KUNG2, GUNNAR MIKALSEN KVIFTE25, OWEN LONSDALE26, STEPHEN A. MARSHALL27, WAYNE N. MATHIS28, VERNER MICHELSEN29, STEFAN NAGLIS30, ALLEN L. NORRBOM31, STEVEN PAIERO27, THOMAS PAPE32, ALESSANDRE PEREIRA- COLAVITE33, MARC POLLET34, SABRINA ROCHEFORT7, ALESSANDRA RUNG17, JUSTIN B. RUNYON35, JADE SAVAGE36, VERA C. SILVA37, BRADLEY J. SINCLAIR38, JEFFREY H. SKEVINGTON8, JOHN O. STIREMAN III10, JOHN SWANN39, PEKKA VILKAMAA40, TERRY WHEELER††, TERRY WHITWORTH41, MARIA WONG2, D. MONTY WOOD8, NORMAN WOODLEY42, TIFFANY YAU27, THOMAS J. ZAVORTINK43 & MANUEL A. ZUMBADO44 †—deceased. Formerly with the Universidad de Panama ††—deceased. Formerly at McGill University, Canada 1. Research Associate, Royal British Columbia Museum and the American Museum of Natural History, 691-8th Ave. SE, Salmon Arm, BC, V1E 2C2, Canada. Email: [email protected] 2. -
Zootaxa, Empidoidea (Diptera)
ZOOTAXA 1180 The morphology, higher-level phylogeny and classification of the Empidoidea (Diptera) BRADLEY J. SINCLAIR & JEFFREY M. CUMMING Magnolia Press Auckland, New Zealand BRADLEY J. SINCLAIR & JEFFREY M. CUMMING The morphology, higher-level phylogeny and classification of the Empidoidea (Diptera) (Zootaxa 1180) 172 pp.; 30 cm. 21 Apr. 2006 ISBN 1-877407-79-8 (paperback) ISBN 1-877407-80-1 (Online edition) FIRST PUBLISHED IN 2006 BY Magnolia Press P.O. Box 41383 Auckland 1030 New Zealand e-mail: [email protected] http://www.mapress.com/zootaxa/ © 2006 Magnolia Press All rights reserved. No part of this publication may be reproduced, stored, transmitted or disseminated, in any form, or by any means, without prior written permission from the publisher, to whom all requests to reproduce copyright material should be directed in writing. This authorization does not extend to any other kind of copying, by any means, in any form, and for any purpose other than private research use. ISSN 1175-5326 (Print edition) ISSN 1175-5334 (Online edition) Zootaxa 1180: 1–172 (2006) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA 1180 Copyright © 2006 Magnolia Press ISSN 1175-5334 (online edition) The morphology, higher-level phylogeny and classification of the Empidoidea (Diptera) BRADLEY J. SINCLAIR1 & JEFFREY M. CUMMING2 1 Zoologisches Forschungsmuseum Alexander Koenig, Adenauerallee 160, 53113 Bonn, Germany. E-mail: [email protected] 2 Invertebrate Biodiversity, Agriculture and Agri-Food Canada, C.E.F., Ottawa, ON, Canada