A New Fossil Saldidae (Hemiptera: Heteroptera: Leptopodomorpha) from the Early Cretaceous in China
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Insetos Do Brasil
COSTA LIMA INSETOS DO BRASIL 2.º TOMO HEMÍPTEROS ESCOLA NACIONAL DE AGRONOMIA SÉRIE DIDÁTICA N.º 3 - 1940 INSETOS DO BRASIL 2.º TOMO HEMÍPTEROS A. DA COSTA LIMA Professor Catedrático de Entomologia Agrícola da Escola Nacional de Agronomia Ex-Chefe de Laboratório do Instituto Oswaldo Cruz INSETOS DO BRASIL 2.º TOMO CAPÍTULO XXII HEMÍPTEROS ESCOLA NACIONAL DE AGRONOMIA SÉRIE DIDÁTICA N.º 3 - 1940 CONTEUDO CAPÍTULO XXII PÁGINA Ordem HEMÍPTERA ................................................................................................................................................ 3 Superfamília SCUTELLEROIDEA ............................................................................................................ 42 Superfamília COREOIDEA ............................................................................................................................... 79 Super família LYGAEOIDEA ................................................................................................................................. 97 Superfamília THAUMASTOTHERIOIDEA ............................................................................................... 124 Superfamília ARADOIDEA ................................................................................................................................... 125 Superfamília TINGITOIDEA .................................................................................................................................... 132 Superfamília REDUVIOIDEA ........................................................................................................................... -
IGCP 632, the Jurassic–Cretaceous Transition In
IGCP 79 IGCP 632, The Jurassic–Cretaceous transition in North Eastern China (western Liaoning and Inner Mongolia): An IGCP meeting and field excursion on the conti- nental Jurassic Jingeng Sha1, Yanhong Pan1, Enpu Gong2, and Vivi Vajda3* 1 LPS, Nanjing Institute of Geology & Paleontology, Nanjing 210008, China 2 Northeastern University, Shenyang 110004, China 3 Swedish Museum of Natural History, Frescativägen 40, 114 18 Stockholm, Sweden, *Corresponding author, E-mail: [email protected] Exposures of strata spanning the Jurassic–Cretaceous boundary been discovered. However, the correlation of the various lithostrati- occur within several basins in western Liaoning and adjacent Inner graphic units in this area is complicated due to patchy exposures and Mongolia. These continental successions host world-renowned plant the scarcity of radiometric constraints, which pose a challenge to researchers and animal fossils including feathered dinosaurs and the oldest flow- working on these deposits. ering plant, Archaeofructus. The first feathered dinosaurs from north- To understand the stratigraphy and context of the Jurassic–Creta- eastern China where found about 20 years ago and created a major ceous biota in Liaoning province, the second IGCP-632 symposium impact in science and the media. Since then, many new specimens have was organized in Liaoning, including a two-day presentation (Sep- Figure 1. (A) Sketch map over the field excursion area in north-eastern China. (B) enlargement of the field region showing the localities of the field stops. Episodes Vol. 40, no. 1 80 intracontinental orogenic system, the Yanshan Movement, and creating a new basin-range system in east Asia. Vivi Vajda presented new results (Peterffy et al., 2015; Vajda et al., 2016) where she compre- hensively analyzed the end-Triassic mass extinc- tion and aftermath and its causal mechanisms, particularly stressing the affects of Jurassic vol- canism in disrupting the major ecosystems but also its importance for fossilization. -
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). -
Zootaxa,Revision of the Genus Suljuktocossus Becker-Migdisova
Zootaxa 1576: 57–62 (2007) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2007 · Magnolia Press ISSN 1175-5334 (online edition) Revision of the genus Suljuktocossus Becker-Migdisova, 1949 (Hemiptera, Palae- ontinidae), with description of a new species from Daohugou, Inner Mongolia, China YING WANG & DONG REN1 College of Life Science, Capital Normal University, Beijing 100037, China 1Corresponding author. E-mail: [email protected] Abstract In this paper a complete specimen of fossil Palaeontinidae, Suljuktocossus yinae sp. nov. from Daohugou (Jiulongshan Formation) in Inner Mongolia, China is described. This new species is established based on both complete forewings and hindwings. According to this specimen, the diagnosis of the genus Suljuktocossus is revised. Moreover, based on the dis- tribution of the genus Suljuktocossus, we consider the age of the Daohugou biota as Middle Jurassic. Key words fossil, morphology, Cicadomorpha, Middle Jurassic Introduction The genus Suljuktocossus erected by Becker-Migdisova is represented only by an incomplete forewing from the Early Jurassic of Shurab, Tadzhikistan (Becker-Migdisova, 1949). Recently another species belonging to this genus from the Daohugou biota, Inner Mongolia was reported (Wang et al., 2007). From the same beds, the specimen we discovered is in remarkably good condition; both forewings and hind wings can be seen clearly. Previously, the rich entomofauna from the Jiulongshan Formation in Daohugou Village, Ningcheng County, Inner Mongolia was dated as Middle Jurassic (Ren et al., 1995; Ren & Krzemiski, 2002; Ren et al., 2002; Shen et al., 2003; Chen et al., 2004; Liu et al., 2004; Gao & Ren, 2006; Huang et al., 2006; Ji et al., 2006; Yao et al., 2006; Tan & Ren, 2006; Liu et al., 2007), Late Jurassic (Zhang, 2002) or Early Cretaceous (Wang et al., 2005). -
Hemiptera: first Record for an Australian Lophopid (Hemiptera, Lophopidae)
Australian Journal of Entomology (2007) 46, 129–132 Historical use of substrate-borne acoustic production within the Hemiptera: first record for an Australian Lophopid (Hemiptera, Lophopidae) Adeline Soulier-Perkins,1* Jérôme Sueur2 and Hannelore Hoch3 1Muséum National d’Histoire Naturelle, Département Systématique et Évolution, USM 601 MNHN & UMR 5202 CNRS, Case Postale 50, 45, Rue Buffon, F-75005 Paris, France. 2NAMC-CNRS UMR 8620, Bât. 446, Université Paris XI, F-91405 Orsay Cedex, France. 3Museum für Naturkunde, Institut für Systematische Zoologie, Humboldt-Universität zu Berlin Invalidenstr. 43, D- 10115 Berlin, Germany. Abstract Here the first record of communication through substrate-borne vibrations for the Lophopidae family is reported. The signals from Magia subocellata that the authors recorded were short calls with a decreasing frequency modulation. Acoustic vibrations have been observed for other families within the Hemiptera and a scenario concerning the historical use of vibrational communication within the Hemiptera is tested using a phylogenetic inference. The most parsimonious hypothesis suggests that substrate-borne communication is ancestral for the hemipteran order and highlights the groups for which future acoustic research should be undertaken. Key words Cicadomorpha, Coleorrhyncha, evolutionary scenario, Heteroptera, Sternorrhyncha, substrate vibration. INTRODUCTION Lophopidae migrating into America via the Bering land bridge. Some other ancestors of the extant groups moved onto Many animals have been recently recognised for their ability newly emerging land in the Pacific, expanding their distribu- to communicate through substrate-borne vibrations (Hill tion as far east as the Samoan Islands, and as far south as 2001). While elephants produce vibrations transmitted by the Australia (Soulier-Perkins 2000). -
Available Generic Names for Trilobites
AVAILABLE GENERIC NAMES FOR TRILOBITES P.A. JELL AND J.M. ADRAIN Jell, P.A. & Adrain, J.M. 30 8 2002: Available generic names for trilobites. Memoirs of the Queensland Museum 48(2): 331-553. Brisbane. ISSN0079-8835. Aconsolidated list of available generic names introduced since the beginning of the binomial nomenclature system for trilobites is presented for the first time. Each entry is accompanied by the author and date of availability, by the name of the type species, by a lithostratigraphic or biostratigraphic and geographic reference for the type species, by a family assignment and by an age indication of the type species at the Period level (e.g. MCAM, LDEV). A second listing of these names is taxonomically arranged in families with the families listed alphabetically, higher level classification being outside the scope of this work. We also provide a list of names that have apparently been applied to trilobites but which remain nomina nuda within the ICZN definition. Peter A. Jell, Queensland Museum, PO Box 3300, South Brisbane, Queensland 4101, Australia; Jonathan M. Adrain, Department of Geoscience, 121 Trowbridge Hall, Univ- ersity of Iowa, Iowa City, Iowa 52242, USA; 1 August 2002. p Trilobites, generic names, checklist. Trilobite fossils attracted the attention of could find. This list was copied on an early spirit humans in different parts of the world from the stencil machine to some 20 or more trilobite very beginning, probably even prehistoric times. workers around the world, principally those who In the 1700s various European natural historians would author the 1959 Treatise edition. Weller began systematic study of living and fossil also drew on this compilation for his Presidential organisms including trilobites. -
The Semiaquatic Hemiptera of Minnesota (Hemiptera: Heteroptera) Donald V
The Semiaquatic Hemiptera of Minnesota (Hemiptera: Heteroptera) Donald V. Bennett Edwin F. Cook Technical Bulletin 332-1981 Agricultural Experiment Station University of Minnesota St. Paul, Minnesota 55108 CONTENTS PAGE Introduction ...................................3 Key to Adults of Nearctic Families of Semiaquatic Hemiptera ................... 6 Family Saldidae-Shore Bugs ............... 7 Family Mesoveliidae-Water Treaders .......18 Family Hebridae-Velvet Water Bugs .......20 Family Hydrometridae-Marsh Treaders, Water Measurers ...22 Family Veliidae-Small Water striders, Rime bugs ................24 Family Gerridae-Water striders, Pond skaters, Wherry men .....29 Family Ochteridae-Velvety Shore Bugs ....35 Family Gelastocoridae-Toad Bugs ..........36 Literature Cited ..............................37 Figures ......................................44 Maps .........................................55 Index to Scientific Names ....................59 Acknowledgement Sincere appreciation is expressed to the following individuals: R. T. Schuh, for being extremely helpful in reviewing the section on Saldidae, lending specimens, and allowing use of his illustrations of Saldidae; C. L. Smith for reading the section on Veliidae, checking identifications, and advising on problems in the taxon omy ofthe Veliidae; D. M. Calabrese, for reviewing the section on the Gerridae and making helpful sugges tions; J. T. Polhemus, for advising on taxonomic prob lems and checking identifications for several families; C. W. Schaefer, for providing advice and editorial com ment; Y. A. Popov, for sending a copy ofhis book on the Nepomorpha; and M. C. Parsons, for supplying its English translation. The University of Minnesota, including the Agricultural Experi ment Station, is committed to the policy that all persons shall have equal access to its programs, facilities, and employment without regard to race, creed, color, sex, national origin, or handicap. The information given in this publication is for educational purposes only. -
Reconstructions of Late Ordovician Crinoids and Bryozoans from the Decorah Shale, Upper Mississippi Valley Sibo Wang Senior Inte
Reconstructions of Late Ordovician crinoids and bryozoans from the Decorah Shale, Upper Mississippi Valley Sibo Wang Senior Integrative Exercise March 10, 2010 Submitted in partial fulfillment of the requirements for a Bachelor of Arts degree from Carleton College, Northfield, Minnesota TABLE OF CONTENTS ABSTRACT INTRODUCTION ........................................................................................................ 01 GEOLOGIC SETTING ................................................................................................ 03 Late Ordovician world ................................................................................. 03 Southern Minnesota and the Decorah Shale ............................................... 03 Benthic community ....................................................................................... 05 Marine conditions ........................................................................................ 05 CRINOIDS ................................................................................................................. 06 General background and fossil record ........................................................ 06 Anatomy ....................................................................................................... 07 Decorah Shale crinoids ................................................................................10 BRYOZOANS ............................................................................................................. 10 General background and -
Crustaceans Topics in Biodiversity
Topics in Biodiversity The Encyclopedia of Life is an unprecedented effort to gather scientific knowledge about all life on earth- multimedia, information, facts, and more. Learn more at eol.org. Crustaceans Authors: Simone Nunes Brandão, Zoologisches Museum Hamburg Jen Hammock, National Museum of Natural History, Smithsonian Institution Frank Ferrari, National Museum of Natural History, Smithsonian Institution Photo credit: Blue Crab (Callinectes sapidus) by Jeremy Thorpe, Flickr: EOL Images. CC BY-NC-SA Defining the crustacean The Latin root, crustaceus, "having a crust or shell," really doesn’t entirely narrow it down to crustaceans. They belong to the phylum Arthropoda, as do insects, arachnids, and many other groups; all arthropods have hard exoskeletons or shells, segmented bodies, and jointed limbs. Crustaceans are usually distinguishable from the other arthropods in several important ways, chiefly: Biramous appendages. Most crustaceans have appendages or limbs that are split into two, usually segmented, branches. Both branches originate on the same proximal segment. Larvae. Early in development, most crustaceans go through a series of larval stages, the first being the nauplius larva, in which only a few limbs are present, near the front on the body; crustaceans add their more posterior limbs as they grow and develop further. The nauplius larva is unique to Crustacea. Eyes. The early larval stages of crustaceans have a single, simple, median eye composed of three similar, closely opposed parts. This larval eye, or “naupliar eye,” often disappears later in development, but on some crustaceans (e.g., the branchiopod Triops) it is retained even after the adult compound eyes have developed. In all copepod crustaceans, this larval eye is retained throughout their development as the 1 only eye, although the three similar parts may separate and each become associated with their own cuticular lens. -
Late Neogene Insect and Other Invertebrate Fossils from Alaska and Arctic/Subarctic Canada
Invertebrate Zoology, 2019, 16(2): 126–153 © INVERTEBRATE ZOOLOGY, 2019 Late Neogene insect and other invertebrate fossils from Alaska and Arctic/Subarctic Canada J.V. Matthews, Jr.1, A. Telka2, S.A. Kuzmina3* 1 Terrain Sciences Branch, Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada K1A 0E8. Present address: 1 Red Maple Lane, Hubley, N.S., Canada B3Z 1A5. 2 PALEOTEC Services – Quaternary and late Tertiary plant macrofossil and insect fossil analyses, 1-574 Somerset St. West, Ottawa, Ontario K1R 5K2, Canada. 3 Laboratory of Arthropods, Borissiak Paleontological Institute, RAS, Profsoyuznaya 123, Moscow, 117868, Russia. E-mails: [email protected]; [email protected]; [email protected] * corresponding author ABSTRACT: This report concerns macro-remains of arthropods from Neogene sites in Alaska and northern Canada. New data from known or recently investigated localities are presented and comparisons made with faunas from equivalent latitudes in Asia and Greenland. Many of the Canadian sites belong to the Beaufort Formation, a prime source of late Tertiary plant and insect fossils. But new sites are continually being discovered and studied and among the most informative of these are several from the high terrace gravel on Ellesmere Island. One Ellesmere Island locality, known informally as the “Beaver Peat” contains spectacularly well preserved plant and arthropod fossils, and is the only Pliocene site in Arctic North America to yield a variety of vertebrate fossils. Like some of the other “keystone” localities discussed here, it promises to be important for dating and correlation as well as for documenting high Arctic climatic and environmental conditions during the Pliocene. -
Hemiptera, Prosorrhyncha) with Special Reference to the Pregenital Abdominal Structure1
© Biologiezentrum Linz/Austria; download unter www.biologiezentrum.at Justification for the Aradimorpha as an infraorder of the suborder Heteroptera (Hemiptera, Prosorrhyncha) with Special Reference to the Pregenital Abdominal Structure1 M.H. SWEET Abstract: Aradomorpha SWEET 1996 is replaced with Aradimorpha because of homonymy with Arado- morpha CHAMPION 1899, a genus of Reduviidae. The Aradimorpha differ from the Pentatomomorpha s.s. and the Leptopodomorpha in having a plesiomorphic connexivum of dorsal epipleurites and ventral hy- popleurites rather than having the connexivum turned over so that the hypopleurites are dorsalized and the epipleurites folded into the abdomen. In most Aradimorpha, in both males and females, sterna 3 to 7 are free with intersegmental conjunctiva; terga 1-2 and 3 to 6 are united, but all epipleurites are free. In the Pentatomomorpha at least abdominal sterna 2 to 4 in females and sterna 2 to 5 in males are uni- ted or fused without conjunctiva. In some aradids the hypopleurites are united or fused with the sterna, but hypopleurite 2 is usually free. Sternum 2 is sometimes united to fused with sternum 1 and the meta- sternum. The abdominal spiracles in the Aradimorpha are ventral on the hypopleurites, although some- times very lateral in position on the hypopleurites, with the exception of the Chinamyersiini in which spiracles 4, 5 and 6 are dorsal on the epipleurites in Chinamyersia, and 5 and 6 dorsal in Gnostocoris, whi- le in the Tretocorini (Tretocoris and Kumaressa) spiracle 2 seems dorsal but is actually very lateral on the hypopleurite. In the Termitaphididae, epipleurites and hypopleurites are distinct, forming mobile lateral abdominal lobes. -
Adult Nepidae of Florida
Graduate Student Project – Insect Classification – ENY 6166 University of Florida - Kendra Pesko - December 8, 2004 Adult Nepidae of Florida The family Nepidae, common name “waterscorpions”, is an aquatic insect family in the order Hemiptera (suborder Heteroptera). Of 13 species and three genera known throughout the United States and Canada, only five species in one genus (Ranatra) occur in Florida. Ranatra species are found in aquatic vegetation and debris, and can be collected by sweeping an aquatic net through vegetation along the edges of lakes. They will cling to emergent vegetation such as cattails to hide during the day, and return to the water surface at night. Ranatra species also make night time flights in order to colonize new areas, and will often end up on car windshields, which they may mistake for open water. Nepidae are unique among water bugs in possessing a stridulatory mechanism which consists of serrations on their fore-coxal cavity that contact coarse ridges which appear to be sclerotized setae. Both nymphs and adults of Ranatra possess these structures. Checklist of Species of Florida Ranatra Fabricius (Hemiptera: Heteroptera: Nepidae) R. australis Hungerford R. buenoi Hungerford R.drakei Hungerford R. kirkaldyi Torre-Bueno R. nigra Herrich-Schaeffer Key to Species of Adult Florida Nepidae (adapted from Sites and Polhemus 1994) 1. Prothorax with mid-ventral hollow groove (fig. 6)…Ranatra buenoi Hungerford 1’. Prothorax without mid-ventral hollow groove, but may be ventrally flattened or have a paired ventro-lateral longitudinal depressed lines .........................................................2 2. Penultimate antennal segment with lateral projection absent or if present, < ½ length of terminal antennal segment (Figs.