Fig. 1. Neadelhus Rotae N. Sp. Dorsal Aspect Ot Holotype. PSYCHE
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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. -
THE ORIGIN and EVOLUTION of HYMENOPTEROUS INSECTS [P
THE ORIGIN AND EVOLUTION OF HYMENOPTEROUS INSECTS [p. 24] Chapter 3 EVOLUTION OF THE INFRACLASS SCARABAEONES A. P. Rasnitzyn* Dragonflies [order Odonata] and mayflies [order Ephemeroptera], which have retained a primitive thorax structure (absence of a cryptosternum) but are specialized in other respects, occupy the most isolated position in the infraclass. They are similar to each other in a number of characters, but the nature of the latter does not allow drawing a conclusion about any close relationship of the two orders. Indeed, the primitiveness of the structure of the thorax common to both of them, like any symplesiomorphy, is not evidence of a common origin. The adaptations of the larvae of mayflies and dragonflies to an aquatic way of life are different, and they show, rather, an independent transition to development in water. The loss of the ability to fold the wings as well is connected with different processes in them: in mayflies, with the ephemerality of the imago, the function of which is essentially limited to nuptial flight and oviposition; and in dragonflies, with the metamorphosis of the adult insect to an active aerial predator. It is highly probable that mayflies and dragonflies are independent evolutionary branches. The belonging of dragonflies and mayflies to a common trunk of Scarabaeones, that is, the isolation of them from Protoptera as part of a single trunk with the remaining members of the infraclass (except Protoptera), is confirmed by the metamorphosis of the style of the ninth segment in mayfly males into part of the copulatory organ [endophallus], and in dragonfly females into a sheath of the ovipositor. -
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Novitates Paleoentomologicae No. 21, pp. 1–7 14 December 2018 First North American species of the European genus Archaemegaptilus from the Upper Carboniferous Potsville Formation of northern Alabama (Palaeodictyoptera: Archaemegaptilidae) Roy J. Beckemeyer1,2 & Michael S. Engel2,3,4 Abstract. A new palaeodictyopteran (Palaeodictyopterida: Palaeodictyoptera) taxon is de- scribed based on a nearly complete hind wing found in the Potsville Formation (Upper Car- boniferous) of Bibb County, Alabama. Archaemegaptilus blakelyi Beckemeyer & Engel, new species, is the sixth insect genus and species described from the Potsville of Alabama and the second palaeodictyopteran from those deposits. It is the third valid species assigned to the family Archaemegaptilidae. Previously known species are A. kieferi Meunier, from the Com- mentry of France and A. schloesseri Brauckmann et al., from the Hagen-Vorhalle of Germany. INTRODUCTION The Carboniferous insect fauna of Alabama is small, comprised of fve species (Beckemeyer & Engel, 2011). Another specimen has recently been discovered and de- posited in the collection of The University of Alabama Museum of Natural History. Like the earlier taxa, it is a well preserved wing of a large palaeopterous insect that we place here in the family Archaemegaptilidae. Carpenter (1992) characterized Ar- 1 957 Perry Avenue, Wichita, Kansas 67203-3141, USA ([email protected]). 2 Division of Entomology, Natural History Museum, 1501 Crestline Drive – Suite 140, University of Kansas, Lawrence, Kansas 66045-4415, USA ([email protected]). 3 Department of Ecology & Evolutionary Biology, University of Kansas, Lawrence, Kansas 66045, USA. 4 Division of Invertebrate Zoology, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024-5192, USA. -
Phylum Arthropoda*
Zootaxa 3703 (1): 017–026 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Correspondence ZOOTAXA Copyright © 2013 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3703.1.6 http://zoobank.org/urn:lsid:zoobank.org:pub:FBDB78E3-21AB-46E6-BD4F-A4ADBB940DCC Phylum Arthropoda* ZHI-QIANG ZHANG New Zealand Arthropod Collection, Landcare Research, Private Bag 92170, Auckland, New Zealand; [email protected] * In: Zhang, Z.-Q. (Ed.) Animal Biodiversity: An Outline of Higher-level Classification and Survey of Taxonomic Richness (Addenda 2013). Zootaxa, 3703, 1–82. Abstract The Arthropoda is here estimated to have 1,302,809 described species, including 45,769 fossil species (the diversity of fossil taxa is here underestimated for many taxa of the Arthropoda). The Insecta (1,070,781 species) is the most successful group, and it alone accounts for over 80% of all arthropods. The most successful insect order, Coleoptera (392,415 species), represents over one-third of all species in 39 insect orders. Another major group in Arthropoda is the class Arachnida (114,275 species), which is dominated by the Acari (55,214 mite and tick species) and Araneae (44,863 spider species). Other diverse arthropod groups include Crustacea (73,141 species), Trilobitomorpha (20,906 species) and Myriapoda (12,010 species). Key words: Classification, diversity, Arthropoda Introduction The Arthropoda, with over 1.5 million described species, is the largest animal phylum, and it alone accounts for about 80% of the total number of species in the animal kingdom (Zhang 2011a). In the last volume on animal higher-level classification and survey of taxonomic richness, 28 chapters by numerous teams of specialists were published on various taxa of the Arthropoda, but there were many gaps to be filled (Zhang 2011b). -
Evolution of the Insects David Grimaldi and Michael S
Cambridge University Press 0521821495 - Evolution of the Insects David Grimaldi and Michael S. Engel Frontmatter More information EVOLUTION OF THE INSECTS Insects are the most diverse group of organisms to appear in the 3-billion-year history of life on Earth, and the most ecologically dominant animals on land. This book chronicles, for the first time, the complete evolutionary history of insects: their living diversity, relationships, and 400 million years of fossils. Whereas other volumes have focused on either living species or fossils, this is the first comprehensive synthesis of all aspects of insect evolution. Current estimates of phylogeny are used to interpret the 400-million-year fossil record of insects, their extinctions, and radiations. Introductory sections include the living species, diversity of insects, methods of reconstructing evolutionary relationships, basic insect structure, and the diverse modes of insect fossilization and major fossil deposits. Major sections cover the relationships and evolution of each order of hexapod. The book also chronicles major episodes in the evolutionary history of insects: their modest beginnings in the Devonian, the origin of wings hundreds of millions of years before pterosaurs and birds, the impact that mass extinctions and the explosive radiation of angiosperms had on insects, and how insects evolved the most complex societies in nature. Evolution of the Insects is beautifully illustrated with more than 900 photo- and electron micrographs, drawings, diagrams, and field photographs, many in full color and virtually all original. The book will appeal to anyone engaged with insect diversity: professional ento- mologists and students, insect and fossil collectors, and naturalists. David Grimaldi has traveled in 40 countries on 6 continents collecting and studying recent species of insects and conducting fossil excavations. -
Rasnitsynala Sigambrorum Gen. Et Sp. N., a Small Odonatopterid
A peer-reviewed open-access journal ZooKeys 130: 57–66 (2011)Rasnitsynala sigambrorum gen. et sp. n., a small odonatopterid... 57 doi: 10.3897/zookeys.130.1458 RESEARCH ARTICLE www.zookeys.org Launched to accelerate biodiversity research Rasnitsynala sigambrorum gen. et sp. n., a small odonatopterid (“Eomeganisoptera”, “Erasipteridae”) from the early Late Carboniferous of Hagen-Vorhalle (Germany) Wolfgang Zessin1,†, Carsten Brauckmann2,‡, Elke Gröning2,§ 1 Lange Straße 9, 19230 Jasnitz, Germany 2 Clausthal University of Technology, Institute of Geology and Paleontology, Leibnizstraße 10, 38678 Clausthal-Zellerfeld, Germany † urn:lsid:zoobank.org:author:EE854837-A2FB-457C-82F1-60406627EC58 ‡ urn:lsid:zoobank.org:author:A9B536B4-6DEF-48C4-980A-9EB8A9467F8B § urn:lsid:zoobank.org:author:6D085012-9A15-4937-B408-FEFDF39B4907 Corresponding author: Wolfgang Zessin ([email protected]) Academic editor: D. Shcherbakov | Received 2 May 2011 | Accepted 26 August 2011 | Published 24 September 2011 urn:lsid:zoobank.org:pub:708DBB4C-244E-4606-992B-D10129016158 Citation: Zessin W, Brauckmann C, Gröning E (2011) Rasnitsynala sigambrorum gen. et sp. n., a small odonatopterid (“Eomeganisoptera”, “Erasipteridae”) from the early Late Carboniferous of Hagen-Vorhalle (Germany). In: Shcherbakov DE, Engel MS, Sharkey MJ (Eds) Advances in the Systematics of Fossil and Modern Insects: Honouring Alexandr Rasnitsyn. ZooKeys 130: 57–66. doi: 10.3897/zookeys.130.1458 Abstract Besides Erasipteroides valentini (Brauckmann in Brauckmann, Koch & Kemper, 1985), Zessinella siope Brauckmann, 1988, and Namurotypus sippeli Brauckmann & Zessin, 1989, Rasnitsynala sigambrorum gen. et sp. n. is the fourth species of the Odonatoptera from the early Late Carboniferous (Early Penn- sylvanian: Namurian B, Marsdenian) deposits of the important Hagen-Vorhalle Konservat-Lagerstätte in Germany. -
Neuropterida of the Lower Cretaceous of Southern England, with a Study on Fossil and Extant Raphidioptera
NEUROPTERIDA OF THE LOWER CRETACEOUS OF SOUTHERN ENGLAND, WITH A STUDY ON FOSSIL AND EXTANT RAPHIDIOPTERA A thesis submitted to The University of Manchester for the degree of PhD in the Faculty of Engineering and Physical Sciences 2010 JAMES EDWARD JEPSON SCHOOL OF EARTH, ATMOSPHERIC AND ENVIRONMENTAL SCIENCES TABLE OF CONTENTS FIGURES.......................................................................................................................8 TABLES......................................................................................................................13 ABSTRACT.................................................................................................................14 LAY ABSTRACT.........................................................................................................15 DECLARATION...........................................................................................................16 COPYRIGHT STATEMENT...........................................................................................17 ABOUT THE AUTHOR.................................................................................................18 ACKNOWLEDGEMENTS..............................................................................................19 FRONTISPIECE............................................................................................................20 1. INTRODUCTION......................................................................................................21 1.1. The Project.......................................................................................................21 -
Changes to the Fossil Record of Insects Through Fifteen Years of Discovery
This is a repository copy of Changes to the Fossil Record of Insects through Fifteen Years of Discovery. White Rose Research Online URL for this paper: https://eprints.whiterose.ac.uk/88391/ Version: Published Version Article: Nicholson, David Blair, Mayhew, Peter John orcid.org/0000-0002-7346-6560 and Ross, Andrew J (2015) Changes to the Fossil Record of Insects through Fifteen Years of Discovery. PLosOne. e0128554. https://doi.org/10.1371/journal.pone.0128554 Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ RESEARCH ARTICLE Changes to the Fossil Record of Insects through Fifteen Years of Discovery David B. Nicholson1,2¤*, Peter J. Mayhew1, Andrew J. Ross2 1 Department of Biology, University of York, York, United Kingdom, 2 Department of Natural Sciences, National Museum of Scotland, Edinburgh, United Kingdom ¤ Current address: Department of Earth Sciences, The Natural History Museum, London, United Kingdom * [email protected] Abstract The first and last occurrences of hexapod families in the fossil record are compiled from publications up to end-2009. -
Evolution of the Insects David Grimaldi and Michael S
Cambridge University Press 0521821495 - Evolution of the Insects David Grimaldi and Michael S. Engel Index More information INDEX 12S rDNA, 32, 228, 269 Aenetus, 557 91; general, 57; inclusions, 57; menageries 16S rDNA, 32, 60, 237, 249, 269 Aenigmatiinae, 536 in, 56; Mexican, 55; parasitism in, 57; 18S rDNA, 32, 60, 61, 158, 228, 274, 275, 285, Aenne, 489 preservation in, 58; resinite, 55; sub-fossil 304, 307, 335, 360, 366, 369, 395, 399, 402, Aeolothripidae, 284, 285, 286 resin, 57; symbioses in, 303; taphonomy, 468, 475 Aeshnoidea, 187 57 28S rDNA, 32, 158, 278, 402, 468, 475, 522, 526 African rock crawlers (see Ambermantis wozniaki, 259 Mantophasmatodea) Amblycera, 274, 278 A Afroclinocera, 630 Amblyoponini, 446, 490 aardvark, 638 Agaonidae, 573, 616: fossil, 423 Amblypygida, 99, 104, 105: in amber, 104 abdomen: function, 131; structure, 131–136 Agaoninae, 423 Amborella trichopoda, 613, 620 Abies, 410 Agassiz, Alexander, 26 Ameghinoia, 450, 632 Abrocomophagidae, 274 Agathiphaga, 560 Ameletopsidae, 628 Acacia, 283 Agathiphagidae, 561, 562, 567, 630 American Museum of Natural History, 26, 87, acalyptrate Diptera: ecological diversity, 540; Agathis, 76 91 taxonomy, 540 Agelaia, 439 Amesiginae, 630 Acanthocnemidae, 391 ages, using fossils, 37–39; using DNA, 38–40 ametaboly, 331 Acari, 99, 105–107: diversity, 101, fossils, 53, Ageniellini, 435 amino acids: racemization, 61 105–107; in-Cretaceous amber, 105, 106 Aglaspidida, 99 ammonites, 63, 642 Aceraceae, 413 Aglia, 582 Amorphoscelidae, 254, 257 Acerentomoidea, 113 Agrias, 600 Amphientomidae, -
Carboniferous Protodonatoid Dragonfly Nymphs and the Synapo- Morphies of Odonatoptera and Ephemeroptera (Insecta: Palaeoptera)
Palaeodiversity 2: 169–198; Stuttgart, 30.12.2009. 169 Carboniferous protodonatoid dragonfly nymphs and the synapo- morphies of Odonatoptera and Ephemeroptera (Insecta: Palaeoptera) JARMILA KUKALOVÁ-PECK Abstract Three extremely rare fossil protodonatoid dragonfly nymphs are described from the middle Pennsylvanian (Moscovian) of Mazon Creek, Illinois: Dragonympha srokai n. gen., n. sp. (Meganisoptera), a large, nearly com- plete young nymph with an extended labial mask and uplifted wing pads; Alanympha richardsoni n. gen., n. sp. (Meganisoptera), a nymphal forewing with two articular plates attached to it; and Carbonympha herdinai n. gen., n. sp. (Eomeganisoptera), a detached nymphal forewing. Plesiomorphic states in Dragonympha n. gen. indicate ho- mologies unresolved in modern Odonata. The segmented head bears 3rd tergum ventrally invaginated. The extended labial mask still shows limb segments. The prothorax bears a pair of winglets. The short wing pads are fully articu- lated, twisted, uplifted and streamlined with body. The mesothoracic anepisternum is placed between acrotergite and prescutum. The abdominal leglets form long, segmented, serial gill filaments. In the ontogenesis of modern dragonflies, the wing and articulation disc occurs just above subcoxal pleuron and far from tergum. Wing sclerites are arranged in eight rows protecting eight blood pathways running towards eight wing veins. The sistergroup of Odonatoptera has not yet been convincingly resolved with computer cladistic approaches. Reasons are examined and discussed. More accurate, evolution-based character evaluations are shown with examples. The role of a correct model of the pan-arthropod limb and the origin of insect wings is discussed. Groundplan characters in dragonflies and mayflies are compared in their Paleozoic and modern states, their obscurity is clarified and complex synapo- morphies are proposed. -
Madygen, Triassic Lagerstätte Number One, Before and After Sharov
ALAVESIA, 2: 113-124 (2008) ISSN 1887-7419 Madygen, Triassic Lagerstätte number one, before and after Sharov Dmitry E. SHCHERBAKOV Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya 123, Moscow 117647, Russia. E-mail: [email protected] ABSTRACT The insect fauna of the world’s richest Triassic fossil locality, Madygen (Ladinian–Carnian of Kyrgyzstan) is reviewed; other groups of animals and plants recorded from the locality are also listed. The research history, fossil preservation and paleoenvironment of the Madygen Formation are briefly discussed. The site was discovered in 1933, and the better part of fossils was collected from the outcrop richest in insects, Dzhayloucho, during five expeditions headed by Alexander Sharov, who discovered there and described two peculiar gliding reptiles that made Madygen worldwide known. The entomofauna includes 20 orders (including the earliest Hymenoptera and early Diptera) and nearly 100 families. The insect assemblage is numerically dominated by Coleoptera, Blattodea, and Auchenorrhyncha. In Dzhayloucho, subdo- minants are Mecoptera, Orthoptera, and Protorthoptera. The largest insects belong to Titanoptera, the order established by Sharov and the most diverse in Madygen. Amphibiotic insects are rare and represented almost exclusively by adults. In some outcrops phyllopod Kazacharthra are common. The paleoenvironment may be reconstructed as an intermontane river valley in seasonally arid climate, with mineralized oxbow lakes and ephemeral ponds on the floodplain. KEY WORDS: Middle–Late Triassic. Insects. Composition of entomofauna. Paleoenvironment. INTRODUCTION 1966; cited after Dobruskina 1995). According to her ideas The world renown fossil site near the village of Mady- the Madygen Formation contains both Permian and Trias- gen, in foothills of the Turkestan Range (south of Fergana sic strata (cropping out in different areas), and the Permian Valley), Kyrgyzstan has yielded more than twenty thousand Madygen flora was rich in Mesozoic elements. -
Dermaptera Hindwing Structure and Folding: New Evidence for Familial, Ordinal and Superordinal Relationships Within Neoptera (Insecta)
Eur. J. Entorno!. 98: 445-509, 2001 ISSN 1210-5759 Dermaptera hindwing structure and folding: New evidence for familial, ordinal and superordinal relationships within Neoptera (Insecta) Fabian HAAS1 and Jarmila KUKALOVÂ-PECK2 1 Section ofBiosystematic Documentation, University ofUlm, Helmholtzstr. 20, D-89081 Ulm, Germany; e-mail: [email protected] 2Department ofEarth Sciences, Carleton University, Ottawa, ON K1S 5B6, Canada; e-mail: [email protected] Key words.Dermaptera, higher phylogenetics, Pterygota, insect wings, wing folding, wing articulation, protowing Abstract. The Dermaptera are a small order of insects, marked by reduced forewings, hindwings with a unique and complicated folding pattern, and by pincer-like cerci. Hindwing characters of 25 extant dermapteran species are documented. The highly derived hindwing venation and articulation is accurately homologized with the other pterygote orders for the first time. The hindwing base of Dermaptera contains phylogenetically informative characters. They are compared with their homologues in fossil dermapteran ancestors, and in Plecoptera, Orthoptera (Caelifera), Dictyoptera (Mantodea, Blattodea, Isoptera), Fulgoromorpha and Megaloptera. A fully homologized character matrix of the pterygote wing complex is offered for the first time. The wing venation of the Coleo- ptera is re-interpreted and slightly modified . The all-pterygote character analysis suggests the following relationships: Pterygota: Palaeoptera + Neoptera; Neoptera: [Pleconeoptera + Orthoneoptera] +