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Description of Two New Ecuadorian Zilchistrophia Weyrauch 1960
A peer-reviewed open-access journal ZooKeys 453: 1–17 (2014)Description of two new Ecuadorian Zilchistrophia Weyrauch 1960... 1 doi: 10.3897/zookeys.453.8605 RESEARCH ARTICLE http://zookeys.pensoft.net Launched to accelerate biodiversity research Description of two new Ecuadorian Zilchistrophia Weyrauch, 1960, with the clarification of the systematic position of the genus based on anatomical data (Gastropoda, Stylommatophora, Scolodontidae) Barna Páll-Gergely1, Takahiro Asami1 1 Department of Biology, Shinshu University, Matsumoto 390-8621, Japan Corresponding author: Barna Páll-Gergely ([email protected]) Academic editor: M. Haase | Received 17 September 2014 | Accepted 14 October 2014 | Published 10 November 2014 http://zoobank.org/741A5972-D4B3-46E9-A5CA-8F38A2E90B5B Citation: Páll-Gergely B, Asami T (2014) Description of two new Ecuadorian Zilchistrophia Weyrauch, 1960, with the clarification of the systematic position of the genus based on anatomical data (Gastropoda, Stylommatophora, Scolodontidae). ZooKeys 453: 1–17. doi: 10.3897/zookeys.453.8605 Abstract Two new species of the genus Zilchistrophia Weyrauch, 1960 are described from Eastern Ecuadorian rain forest: Zilchistrophia hilaryae sp. n. and Z. shiwiarorum sp. n. These two new species extend the distribu- tion of the genus considerably northwards, because congeners have been reported from Peru only. For the first time we present anatomical data (radula, buccal mass, morphology of the foot and the genital struc- ture) of Zilchistrophia species. According to these, the genus belongs to the family Scolodontidae, sub- family Scolodontinae (=“Systrophiini”). The previously assumed systematic relationship of Zilchistrophia with the Asian Corillidae and Plectopylidae based on the similarly looking palatal plicae is not supported. Keywords Systrophiidae, Plectopylidae, Plectopylis, Corillidae, anatomy, taxonomy Copyright Barna Páll-Gergely, Takahiro Asami. -
MYRIAPODS 767 Volume 2 (M-Z), Pp
In: R. Singer, (ed.), 1999. Encyclopedia of Paleontology, MYRIAPODS 767 volume 2 (M-Z), pp. 767-775. Fitzroy Dearborn, London. MYRIAPODS JVlyriapods are many-legged, terrestrial arthropods whose bodies groups, the Trilobita, Chelicerata, Crustacea, and the Uniramia, the are divided into two major parts, a head and a trunk. The head last consisting of the Myriapoda, Hexapoda, and Onychophora (vel- bears a single pair of antennae, highly differentiated mandibles (or vet worms). However, subsequent structural and molecular evidence jaws), and at least one pair of maxillary mouthparts; the trunk indicates that there are several characters uniting major arthropod region consists of similar "metameres," each of which is a func- taxa. Moreover, paleobiologic, embryologie, and other evidence tional segment that bears one or two pairs of appendages. Gas demonstrates that myriapods and hexapods are fiindamentally exchange is accomplished by tracheae•a branching network of polyramous, having two major articulating appendages per embry- specialized tubules•although small forms respire through the ological body segment, like other arthropods. body wall. Malpighian organs are used for excretion, and eyes con- A fourth proposal (Figure ID) suggests that myriapods are sist of clusters of simple, unintegrated, light-sensitive elements an ancient, basal arthropod lineage, and that the Hexapoda that are termed ommatidia. These major features collectively char- emerged as an independent, relatively recent clade from a rather acterize the five major myriapod clades: Diplopoda (millipeds), terminal crustacean lineage, perhaps the Malacostraca, which con- Chilopoda (centipeds), Pauropoda (pauropods), Symphyla (sym- tains lobsters and crabs (Ballard et al. 1992). Because few crusta- phylans), and Arthropleurida (arthropleurids). Other features cean taxa were examined in this analysis, and due to the Cambrian indicate differences among these clades. -
Permian Millipedes from the Fort Sill fissures of Southwestern Oklahoma, with Comments on Allied Taxa and Millipedes Preserved in Karstic Environments
Journal of Paleontology, 95(3), 2021, p. 586–600 Copyright © The Author(s), 2020. Published by Cambridge University Press on behalf of The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution-NonCommercial-ShareAlike licence (http:// creativecommons.org/licenses/by-nc-sa/4.0/), which permits non-commercial re-use, distribution, and reproduction in any medium, provided the same Creative Commons licence is included and the original work is properly cited. The written permission of Cambridge University Press must be obtained for commercial re-use. 0022-3360/21/1937-2337 doi: 10.1017/jpa.2020.100 Permian millipedes from the Fort Sill fissures of southwestern Oklahoma, with comments on allied taxa and millipedes preserved in karstic environments Joseph T. Hannibal1 and William J. May2 1Cleveland Museum of Natural History, 1 Wade Oval Drive, Cleveland, Ohio 44106, USA <[email protected]> 2Sam Noble Oklahoma Museum of Natural History, University of Oklahoma, Norman, Oklahoma 73072, USA <[email protected]> Abstract.—Permian millipedes are rare, especially so considering the relative abundance of millipedes in Carboniferous rocks. We report an early Permian millipede fauna containing three new genera and species of millipedes (Oklahoma- soma richardsspurense new genus new species, Karstiulus fortsillensis new genus new species, and Dolesea subtila new genus new species) found in fossil-producing pockets of the Fort Sill fissures exposed in the Dolese Quarry near Richards Spur, southwest Oklahoma, USA. These are the first new genera of invertebrates to be described from this site, one of the most prolific fossil-vertebrate sites in the world. -
Conchological Differentiation and Genital Anatomy of Nepalese Glessulinae (Gastropoda, Stylommatophora, Subulinidae), with Descriptions of Six New Species
A peer-reviewed open-access journal ZooKeys 675: 129–156Conchological (2017) differentiation and genital anatomy of Nepalese Glessulinae... 129 doi: 10.3897/zookeys.675.13252 RESEARCH ARTICLE http://zookeys.pensoft.net Launched to accelerate biodiversity research Conchological differentiation and genital anatomy of Nepalese Glessulinae (Gastropoda, Stylommatophora, Subulinidae), with descriptions of six new species Prem B. Budha1,3, Fred Naggs2, Thierry Backeljau1,4 1 University of Antwerp, Evolutionary Ecology Group, Universiteitsplein 1, B-2610, Antwerp, Belgium 2 Na- tural History Museum, Cromwell Road, London, SW7 5BD, UK 3 Central Department of Zoology, Tribhuvan University, Kirtipur, Kathmandu, Nepal 4 Royal Belgian Institute of Natural Sciences, Vautierstraat 29, B-1000, Brussels, Belgium Corresponding author: Prem B. Budha ([email protected]) Academic editor: F. Köhler | Received 17 April 2017 | Accepted 2 May 2017 | Published 23 May 2017 http://zoobank.org/E5C8F163-D615-47B9-8418-CEE8D71A7DAB Citation: Budha PB, Naggs F, Backeljau T (2017) Conchological differentiation and genital anatomy of Nepalese Glessulinae (Gastropoda, Stylommatophora, Subulinidae), with descriptions of six new species. ZooKeys 675: 129– 156. https://doi.org/10.3897/zookeys.675.13252 Abstract Eleven species of Glessulinae belonging to the genera Glessula Martens, 1860 (three species) and Rishetia Godwin-Austen, 1920 (eight species) are reported from Nepal, six of which are new to science and are described here, viz., G. tamakoshi Budha & Backeljau, sp. n., R. kathmandica Budha & Backeljau, sp. n., R. nagarjunensis Budha & Naggs, sp. n., R. rishikeshi Budha & Naggs, sp. n., R. subulata Budha & Naggs and R. tribhuvana Budha, sp. n. and two are new records for Nepal viz. G. cf. hebetata and R. -
Molluscs from the Miocene Pebas Formation of Peruvian and Colombian Amazonia
Molluscs from the Miocene Pebas Formation of Peruvian and Colombian Amazonia F.P. Wesselingh, with contributions by L.C. Anderson & D. Kadolsky Wesselingh, F.P. Molluscs from the Miocene Pebas Formation of Peruvian and Colombian Amazonia. Scripta Geologica, 133: 19-290, 363 fi gs., 1 table, Leiden, November 2006. Frank P. Wesselingh, Nationaal Natuurhistorisch Museum, Postbus 9517, 2300 RA Leiden, The Nether- lands and Biology Department, University of Turku, Turku SF20014, Finland (wesselingh@naturalis. nnm.nl); Lauri C. Anderson, Department of Geology and Geophysics, Louisiana State University, Baton Rouge, LA 70803, U.S.A. ([email protected]); D. Kadolsky, 66, Heathhurst Road, Sanderstead, South Croydon, Surrey CR2 OBA, England ([email protected]). Key words – Mollusca, systematics, Pebas Formation, Miocene, western Amazonia. The mollusc fauna of the Miocene Pebas Formation of Peruvian and Colombian Amazonia contains at least 158 mollusc species, 73 of which are introduced as new; 13 are described in open nomenclature. Four genera are introduced (the cochliopid genera Feliconcha and Glabertryonia, and the corbulid genera Pachy- rotunda and Concentricavalva) and a nomen novum is introduced for one genus (Longosoma). A neotype is designated for Liosoma glabra Conrad, 1874a. The Pebas fauna is taxonomically dominated by two fami- lies, viz. the Cochliopidae (86 species; 54%) and Corbulidae (23 species; 15%). The fauna can be character- ised as aquatic (155 species; 98%), endemic (114 species; 72%) and extinct (only four species are extant). Many of the families represented by a few species in the Pebas fauna include important ecological groups, such as indicators of marine infl uence (e.g., Nassariidae, one species), terrestrial settings (e.g., Acavidae, one species) and stagnant to marginally agitated freshwaters (e.g., Planorbidae, four species). -
The Joggins Fossil Cliffs UNESCO World Heritage Site: a Review of Recent Research
The Joggins Fossil Cliffs UNESCO World Heritage site: a review of recent research Melissa Grey¹,²* and Zoe V. Finkel² 1. Joggins Fossil Institute, 100 Main St. Joggins, Nova Scotia B0L 1A0, Canada 2. Environmental Science Program, Mount Allison University, Sackville, New Brunswick E4L 1G7, Canada *Corresponding author: <[email protected]> Date received: 28 July 2010 ¶ Date accepted 25 May 2011 ABSTRACT The Joggins Fossil Cliffs UNESCO World Heritage Site is a Carboniferous coastal section along the shores of the Cumberland Basin, an extension of Chignecto Bay, itself an arm of the Bay of Fundy, with excellent preservation of biota preserved in their environmental context. The Cliffs provide insight into the Late Carboniferous (Pennsylvanian) world, the most important interval in Earth’s past for the formation of coal. The site has had a long history of scientific research and, while there have been well over 100 publications in over 150 years of research at the Cliffs, discoveries continue and critical questions remain. Recent research (post-1950) falls under one of three categories: general geol- ogy; paleobiology; and paleoenvironmental reconstruction, and provides a context for future work at the site. While recent research has made large strides in our understanding of the Late Carboniferous, many questions remain to be studied and resolved, and interest in addressing these issues is clearly not waning. Within the World Heritage Site, we suggest that the uppermost formations (Springhill Mines and Ragged Reef), paleosols, floral and trace fossil tax- onomy, and microevolutionary patterns are among the most promising areas for future study. RÉSUMÉ Le site du patrimoine mondial de l’UNESCO des falaises fossilifères de Joggins est situé sur une partie du littoral qui date du Carbonifère, sur les rives du bassin de Cumberland, qui est une prolongation de la baie de Chignecto, elle-même un bras de la baie de Fundy. -
[CIM] International Society for Myriapodology
Centre International de Myriapodologie [CIM] International Society for Myriapodology Newsletter n°4 (December 2019) Edited by Stylianos Simaiakis 1 New CIM Council and Board 2019-2021 The new CIM Council 2019-2021 comprises 13 members: Peter Decker (Germany) [President] Nesrine Akkari (Tunisia) [Vice-President] Stylianos Simaiakis (Greece) [General-Secretary] Jean-Jacques Geoffroy (France) [Associate-Secretary] Hans Reip (Germany) [Treasurer] Dragan Antic (Serbia) Lucio Bonato (Italy) Amazonas Chagas-Junior (Brazil) László Dányi (Hungary) Carsten Müller (Germany) Piyatida Pimvichai (Thailand) Petra Sierwald (USA) Varpu Vahtera (Finland) Cover Image: A micro-CT scan of a 100-million-year old millipede preserved in amber (offered by T. Wesener) 2 The 19TH International Congress of Myriapodology, Quindío, COLOMBIA, August 2021 FIRST MESSAGE TO THE MYRIAPODOLOGICAL COMMUNITY Warm greetings to all myriapodologists and onychophorologists of the World! We are pleased to announce that the next Congress of the International Society of Myriapodology will be held in Colombia, August 2021. First, we would like to thank the assistants to the 18th ICM in Budapest, Hungary, for their trust in our proposal for the headquarters of the 19th ICM. We have formed a Committee, that is eagerly working in organizing an event that lives up to your expectations. At the moment, we can communicate to the international myriapodological community that the event is going to take place in a country hotel located in the Colombian department of Quindío (within the coffee-producing region of Colombia), nestled in the Central Andes Mountain Range, with a pleasant mild climate throughout the year. We have selected this region for its breathtaking landscapes, its multiple tourist attractions, and because it was the location of previous international academic events, with excellent results. -
The Joggins Cliffs of Nova Scotia: B2 the Joggins Cliffs of Nova Scotia: Lyell & Co's "Coal Age Galapagos" J.H
GAC-MAC-CSPG-CSSS Pre-conference Field Trips A1 Contamination in the South Mountain Batholith and Port Mouton Pluton, southern Nova Scotia HALIFAX Building Bridges—across science, through time, around2005 the world D. Barrie Clarke and Saskia Erdmann A2 Salt tectonics and sedimentation in western Cape Breton Island, Nova Scotia Ian Davison and Chris Jauer A3 Glaciation and landscapes of the Halifax region, Nova Scotia Ralph Stea and John Gosse A4 Structural geology and vein arrays of lode gold deposits, Meguma terrane, Nova Scotia Rick Horne A5 Facies heterogeneity in lacustrine basins: the transtensional Moncton Basin (Mississippian) and extensional Fundy Basin (Triassic-Jurassic), New Brunswick and Nova Scotia David Keighley and David E. Brown A6 Geological setting of intrusion-related gold mineralization in southwestern New Brunswick Kathleen Thorne, Malcolm McLeod, Les Fyffe, and David Lentz A7 The Triassic-Jurassic faunal and floral transition in the Fundy Basin, Nova Scotia Paul Olsen, Jessica Whiteside, and Tim Fedak Post-conference Field Trips B1 Accretion of peri-Gondwanan terranes, northern mainland Nova Scotia Field Trip B2 and southern New Brunswick Sandra Barr, Susan Johnson, Brendan Murphy, Georgia Pe-Piper, David Piper, and Chris White The Joggins Cliffs of Nova Scotia: B2 The Joggins Cliffs of Nova Scotia: Lyell & Co's "Coal Age Galapagos" J.H. Calder, M.R. Gibling, and M.C. Rygel Lyell & Co's "Coal Age Galapagos” B3 Geology and volcanology of the Jurassic North Mountain Basalt, southern Nova Scotia Dan Kontak, Jarda Dostal, -
The First Permian Centipedes from Russia
The first Permian centipedes from Russia ALEXANDER V. KHRAMOV, WILLIAM A. SHEAR, RANDY MERCURIO, and DMITRY KOPYLOV Khramov, A.V., Shear, W.A., Mercurio, R., and Kopylov, D. 2018. The first Permian centipedes from Russia. Acta Palaeontologica Polonica 63 (3): 549–555. While fossils of myriapods are well-known from the Devonian and Carboniferous, until recently sediments from the Permian have been largely devoid of the remains of this important group of terrestrial arthropods. Only one locality reported to yield fossils of a single species of millipede has been cited for the Permian, and that through a reevalu- ation of strata previously thought to be Triassic. We report fossils of two species of scolopendromorph centipedes (Chilopoda), Permocrassacus novokshonovi gen. et sp. nov., from the lower Permian of Tshekarda (the Urals, Russia) and Permocryptops shelleyi gen. et sp. nov., from the upper Permian of Isady (North European Russia). These are the first centipedes to be reported and the second and third myriapods to be formally named from the Permian Period. They are compared to previously described scolopendromorphs from the Carboniferous and Cretaceous. The new species possess enlarged ultimate legs, which probably were used as means of anchoring themselves to the substrate, or to aid in defense and prey capture. Key words: Chilopoda, Scolopendromorpha, Permian, Russia, Tshekarda, Isady. Alexander V. Khramov [[email protected]] and Dmitry Kopylov [[email protected]], Borissiak Paleontological Institute of Russian Academy of Sciences, Profsoyuznaya str. 123, 117997 Moscow, Russia; Cherepovets State University, Lunacharskogo str 5, 162600 Cherepovets, Russia; William A. Shear [[email protected]], Hampden-Sydney College, Hampden-Sydney, VA 23943, USA; Randy Mercurio [[email protected]], Eastern Research Group, Inc., Engineer- ing and Science Division, 601 Keystone Park Drive, Suite 700, Morrisville, NC 27560, USA. -
08-Schneider Et Al. (Arthropleura).P65
Lucas et al., eds., 2010, Carb-Permian transition in Cañon del Cobre. New Mexico Museum of Natural History and Science Bulletin 49. 49 EURAMERICAN LATE PENNSYLVANIAN / EARLY PERMIAN ARTHROPLEURID/TETRAPOD ASSOCIATIONS – IMPLICATIONS FOR THE HABITAT AND PALEOBIOLOGY OF THE LARGEST TERRESTRIAL ARTHROPOD JÖRG W. SCHNEIDER1, SPENCER G. LUCAS2, RALF WERNEBURG3 AND RONNY RÖßLER4 1 TU Bergakademie Freiberg, Institut für Geologie, B.v.Cotta-Strasse 2, D-09596 Freiberg, Germany; 2 New Mexico Museum of Natural History and Science, 1801 Mountain Road N.W., Albuquerque, New Mexico 87104; 3 Naturhistorisches Museum Schloss Bertholdsburg, Burgstrasse 6, D-98553 Schleusingen, Germany; 4 Museum für Naturkunde, Moritzstrasse 20, D-09111 Chemnitz, Germany Abstract—The giant arthropod Arthropleura was a common member of the late Paleozoic continental biota of paleo-equatorial biomes for more than 35 million years, from the Early Carboniferous late Visean (FOD; Middle Mississippian, Asbian/Brigantian) up to the Early Permian lower Rotliegend (LOD = ?LAD; Asselian). In Upper Pennsylvanian red beds in Cañon del Cobre of northern New Mexico, trackways of Arthropleura are present in strata that also yield body fossils of the amphibian Eryops. We review the Arthropleura tracksite from Cañon del Cobre, New Mexico, as well as other tracksites of this animal and arthropleurid/eryopid associations in order to better interpret the paleoenvironmental preference and the paleobiology of Arthropleura. This review supports the conclusion that Arthropleura was well adapted to alluvial environments of ever wet humid to seasonally dry and semihumid climates. Preferred habitats of semi-adult and adult Arthropleura were open, vegetated, river landscapes. They co-occurred in these habitats with semi-aquatic eryopid amphibians and terrestrial pelycosaurs. -
Lamarck, 1822
Boletín Nahuelbuta Natural (abril 2020) 6: 5 Comunicación breve NUEVOS ANTECEDENTES EVOLUTIVOS Y BIOGEOGRÁFICOS DE MACROCYCLIS PERUVIANUS (LAMARCK, 1822), ESPECIE ENDÉMICA EN LOS BOSQUES DE CHILE) New evolutionary and biogeographic antecedents of Macrocyclis peruvianus (Lamarck, 1822), endemic species in the forests of Chile) Carmen G. Fuentealba1 & Edgardo Flores2 1Departamento de Ciencias Básicas, Facultad de Ciencias, Universidad del Biobío, Avenida Andrés Bello s/n, Casilla 447, Chillán, Chile. E-mail: [email protected] 2Fundación Nahuelbuta Natural. Jerónimo Trettel 105, Cañete, Chile. Introducción La localidad tipo de esta especie, inicialmente se La fauna de gasterópodos terrestres a describió en Perú, sin embargo, se transfirió a diferencia de los dulceacuícolas y marinos en Chile, pero bajo la denominación de ambigua. Chile es bastante poco conocida, una especie Actualmente es un género monotípico y es la única especie de la familia Acavidae en Chile emblemática de esta fauna de gasterópodos (Stuardo & Vega, 1985). Se distribuye terrestres es Mcrocyclis peruvianus conocido latitudinalmente entre los 35° y 45° S, su comúnmente como, “caracol negro” o “caracol distribución es restringida también a Zona de gigante” (Silva & Thome 2009) (Fig.1). Neuquén, sector río Negro, incluyendo Respecto a la sinonimia corresponde a las avistamiento en Nahuel Huapi (Letelier & Ramos siguientes especies: Helix peruviana Lamarck, 2002). 1822, Helix laxata A.E.J. Férussac, 1821, Helix (Helicella) laxata A.E.J. Férussac, 1821, Helicella El tamaño promedio es de 6 a 7 cm, superficie laxata (A.E.J. Férussac, 1821), Macrocyclis de la concha de un color marrón rojizo, laxata (A.E.J. Férussac, 1821). heliforme, umbilicada espira obtusa, perístomo agudo, conchilla no esculturada, la abertura oblicua (Fernández & Castellanos, 1973). -
A Geological Perspective on the Evolution of Amazonian Biota
TURUN YLIOPISTON JULKAISUJA ANNALES UNIVERSITATES TURKUENSIS SARJA - SER. AII OSA - TOM. 232 BIOLOGICA - GEOGRAPHICA - GEOLOGICA MOLLUSCAN RADIATIONS AND LANDSCAPE EVOLUTION IN MIOCENE AMAZONIA by Frank P. Wesselingh TURUN YLIOPISTO Turku 2008 From the section of Biodiversity and Environmental Science Department of Biology University of Turku FI-20014 Turku Finland Supervised by Prof Jukka Salo formerly Section of Biodiversity and Environmental Science Department of Biology University of Turku FI-20014 Turku Finland Reviewed by Dr Matthias Glaubrecht Humboldt-Universität zu Berlin Museum für Naturkunde 10099 Berlin Germany and Dr Mathias Harzhauser Department of Geology Naturhistorisches Museum Wien Burgring 7 A-1010 Vienna Austria Opponent Prof Dr John Lundberg Ichthyology Department Academy of Natural Sciences 1900 Benjamin Franklin Parkway, Philadelphia, PA 19103 U.S.A. ISBN 978-951-29-3765-3 (PDF) ISSN 0082-6979 Painosalama Oy – Turku, Finland, 2008 List of Original Articles 3 LIST OF ORIGINAL ARTICLES This thesis is based on the following articles, which are referred to by their Roman numerals in the text: I. Wesselingh, F.P. 2006. Molluscs from the Miocene Pebas Formation of Peruvian and Colombian Amazonia. Scripta Geologica 133: 19-290. http://www.repository.naturalis.nl/document/41346 II. Wesselingh, F.P., Hoorn, M.C., Guerrero, J., Räsänen, M.E., Romero Pittmann L. & Salo, J. 2006. The stratigraphy and regional structure of Miocene deposits in western Amazonia (Peru, Colombia and Brazil), with implications for Late Neogene landscape evolution. Scripta Geologica 133: 291-322. http://www.repository.naturalis.nl/document/41347 III. Wesselingh, F.P., Guerrero, J., Räsänen, M.E., Romero Pitmann, L. & Vonhof, H.B.