Scaphwpus Intermontanus Cope Great Basin Spadefoot
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BOA2.1 Caecilian Biology and Natural History.Key
The Biology of Amphibians @ Agnes Scott College Mark Mandica Executive Director The Amphibian Foundation [email protected] 678 379 TOAD (8623) 2.1: Introduction to Caecilians Microcaecilia dermatophaga Synapomorphies of Lissamphibia There are more than 20 synapomorphies (shared characters) uniting the group Lissamphibia Synapomorphies of Lissamphibia Integumen is Glandular Synapomorphies of Lissamphibia Glandular Skin, with 2 main types of glands. Mucous Glands Aid in cutaneous respiration, reproduction, thermoregulation and defense. Granular Glands Secrete toxic and/or noxious compounds and aid in defense Synapomorphies of Lissamphibia Pedicellate Teeth crown (dentine, with enamel covering) gum line suture (fibrous connective tissue, where tooth can break off) basal element (dentine) Synapomorphies of Lissamphibia Sacral Vertebrae Sacral Vertebrae Connects pelvic girdle to The spine. Amphibians have no more than one sacral vertebrae (caecilians have none) Synapomorphies of Lissamphibia Amphicoelus Vertebrae Synapomorphies of Lissamphibia Opercular apparatus Unique to amphibians and Operculum part of the sound conducting mechanism Synapomorphies of Lissamphibia Fat Bodies Surrounding Gonads Fat Bodies Insulate gonads Evolution of Amphibians † † † † Actinopterygian Coelacanth, Tetrapodomorpha †Amniota *Gerobatrachus (Ray-fin Fishes) Lungfish (stem-tetrapods) (Reptiles, Mammals)Lepospondyls † (’frogomander’) Eocaecilia GymnophionaKaraurus Caudata Triadobatrachus Anura (including Apoda Urodela Prosalirus †) Salientia Batrachia Lissamphibia -
SHIS 056.Pdf
A Bibliography of the Green Frog. Paivia clamitatjs Latreille 1801-B81 MARGARET M. STEWART & LINDA F. BIUSO Department of Biological Sciences State University of Mew York at Albany SMITHSONIAN HERPETOLOGICAL INFORMATION SERVICE NO. 56 1982 •"^'VX V ^/SRARIES ,.- SMITHSONIAN HERPETOLOGICAL INFORMATION SERVICE The SHIS series publishes and distributes translations, bibliographies, indices, and similar items judged useful to individuals interested in the biology of amphibians and reptiles, but unlikely to be published in the normal technical journals. Single copies are distributed free to interested individuals. Libraries, herpetological associations, and research laboratories are invited to exchange their publications with us. We wish to encourage individuals to share their bibliographies, translations, etc. with other herpetologists through the SHIS series. If you have such items please contact George Zug for instructions. Contributors receive 50 free copies. Please address all requests for copies and inquiries to George Zug, Division of Reptiles and Amphibians, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560, U.S.A. INTRODUCTION Rana clamitans , the green frog, is one of the most abundant and widespread ranids in North America. It occurs throughout eastern North America from central Florida to 50° N Latitude in Canada. The literature concerning the species, described in 1801, is vast. With the help of numerous persons, we have attempted to compile a complete bibliography, through 1981, of publications concerning the green frog. We have listed papers and notes containing substantive information about the species, including range records. Papers that only mentioned other references already included are omitted. Although all references have not been checked, we included them if the source were reliable. -
A.11 Western Spadefoot Toad (Spea Hammondii) A.11.1 Legal and Other Status the Western Spadefoot Toad Is a California Designated Species of Special Concern
Appendix A. Species Account Butte County Association of Governments Western Spadefoot Toad A.11 Western Spadefoot Toad (Spea hammondii) A.11.1 Legal and Other Status The western spadefoot toad is a California designated Species of Special Concern. This species currently does not have any federal listing status. Although this species is not federally listed, it is addressed in the Recovery Plan for Vernal Pool Ecosystems of California and Southern Oregon (USFWS 2005). A.11.2 Species Distribution and Status A.11.2.1 Range and Status The western spadefoot toad historically ranged from Redding in Shasta County, California, to northwestern Baja California, Mexico (Stebbins 1985). This species was known to occur throughout the Central Valley and the Coast Ranges and along the coastal lowlands from San Francisco Bay to Mexico (Jennings and Hayes 1994). The western spadefoot toad has been extirpated throughout most southern California lowlands (Stebbins 1985) and from many historical locations within the Central Valley (Jennings and Hayes 1994, Fisher and Shaffer 1996). It has severely declined in the Sacramento Valley, and their density has been reduced in eastern San Joaquin Valley (Fisher and Shaffer 1996). While the species has declined in the Coast Range, they appear healthier and more resilient than those in the valleys. The population status and trends of the western spadefoot toad outside of California (i.e., Baja California, Mexico) are not well known. This species occurs mostly below 900 meters (3,000 feet) in elevation (Stebbins 1985). The average elevation of sites where the species still occurs is significantly higher than the average elevation for historical sites, suggesting that declines have been more pronounced in lowlands (USFWS 2005). -
Palaeoecology and Depositional Environments of the Tendaguru Beds (Late Jurassic to Early Cretaceous, Tanzania)
Mitt. Mus. Nat.kd. Berl., Geowiss. Reihe 5 (2002) 19-44 10.11.2002 Palaeoecology and depositional environments of the Tendaguru Beds (Late Jurassic to Early Cretaceous, Tanzania) Martin Aberhan ', Robert Bussert2, Wolf-Dieter Heinrich', Eckhart Schrank2, Stephan Schultkal, Benjamin Sames3, Jiirgen =wet4 & Saidi Kapilima5 With 6 figures, 2 tables, and 2 plates Abstract The Late Jurassic to Early Cretaceous Tendaguru Beds (Tanzania, East Africa) have been well known for nearly a century for their diverse dinosaur assemblages. Here, we present sedimentological and palaeontological data collected by the German- Tanzanian Tendaguru Expedition 2000 in an attempt to reconstruct the palaeo-ecosystems of the Tendaguru Beds at their type locality. Our reconstructions are based on sedimentological data and on a palaeoecological analysis of macroinverte- brates, microvertebrates, plant fossils and microfossils (ostracods, foraminifera, charophytes, palynomorphs). In addition, we included data from previous expeditions, particularly those on the dinosaur assemblages. The environmental model of the Tendaguru Beds presented herein comprises three broad palaeoenvironmental units in a marginal marine setting: (1) Lagoon-like, shallow marine environments above fair weather wave base and with evidence of tides and storms. These formed behind barriers such as ooid bar and siliciclastic sand bar complexes and were generally subject to minor salinity fluctuations. (2) Extended tidal flats and low-relief coastal plains. These include low-energy, brackish coastal lakes and ponds as well as pools and small fluvial channels of coastal plains in which the large dinosaurs were buried. Since these environments apparently were, at best, poorly vegetated, the main feeding grounds of giant sauropods must have been elsewhere. -
Anura: Pelobatidae) MCZ by LIBRARY
Scientific Papers Natural History Museum The University of Kansas 18 July 2003 Number 30:1-13 Skeletal Development of Pelobates cultripes and a Comparison of the Osteogenesis of Pelobatid Frogs (Anura: Pelobatidae) MCZ By LIBRARY Z008 Anne M. Magl.a' JUL 2 3 Division of Hcrpetologi/, Natural History Museiiui and Biodiversity Researcli Center, and Department ojEonbgi^gMSpY Evolutionary Biology, The University of Kansas, Laivreuce, Kansas 66045, USA CONTENTS ABSTRACT 1 RESUMEN 2 INTRODUCTION 2 Acknowledgments 2 MATERIALS AND METHODS 2 RESULTS 3 Cranial Development 3 Hyobranchial Development 6 PosTCRANiAL Development 6 DISCUSSION 8 LITERATURE CITED 13 ABSTRACT The larval skeleton and osteogenesis of Pelobates cultripjes is described and compared to that of several pelobatoid and non-pelobatoid taxa. Several features of the larval skeleton are of inter- est, including: absence of a cartilaginous strip between the cornua trabeculae, type of articulation of cornua and suprarostrals, presence of adrostral tissues, and the condition of the otic process. By com- paring sequence of ossification events across taxa, several patterns of skeletal development for Pelobates cultripes emerge, including: conserved timing of prootic ossification, delayed onset of mentomeckelian ossification, and early formation of vomerine teeth. Several other developmental features, including the absence of a palatine (= neopalatine) bone and the formation of the frontoparietal, also are discussed. Key Words: Anura, Pelobatoidea, Pelobatidae, desarollo, osteologia, Pelobates, -
Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal)
Alexandre Renaud Daniel Guillaume Licenciatura em Biologia celular Mestrado em Sistemática, Evolução, e Paleobiodiversidade Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal) Dissertação para obtenção do Grau de Mestre em Paleontologia Orientador: Miguel Moreno-Azanza, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Co-orientador: Octávio Mateus, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Júri: Presidente: Prof. Doutor Paulo Alexandre Rodrigues Roque Legoinha (FCT-UNL) Arguente: Doutor Hughes-Alexandres Blain (IPHES) Vogal: Doutor Miguel Moreno-Azanza (FCT-UNL) Júri: Dezembro 2018 MICROVERTEBRATES OF THE LOURINHÃ FORMATION (LATE JURASSIC, PORTUGAL) © Alexandre Renaud Daniel Guillaume, FCT/UNL e UNL A Faculdade de Ciências e Tecnologia e a Universidade Nova de Lisboa tem o direito, perpétuo e sem limites geográficos, de arquivar e publicar esta dissertação através de exemplares impressos reproduzidos em papel ou de forma digital, ou por qualquer outro meio conhecido ou que venha a ser inventado, e de a divulgar através de repositórios científicos e de admitir a sua cópia e distribuição com objetivos educacionais ou de investigação, não comerciais, desde que seja dado crédito ao autor e editor. ACKNOWLEDGMENTS First of all, I would like to dedicate this thesis to my late grandfather “Papi Joël”, who wanted to tie me to a tree when I first start my journey to paleontology six years ago, in Paris. And yet, he never failed to support me at any cost, even if he did not always understand what I was doing and why I was doing it. He is always in my mind. Merci papi ! This master thesis has been one-year long project during which one there were highs and lows. -
The Tendaguru Formation (Late Jurassic to Early Cretaceous, Southern Tanzania): Definition, Palaeoenvironments, and Sequence Stratigraphy
Fossil Record 12 (2) 2009, 141–174 / DOI 10.1002/mmng.200900004 The Tendaguru Formation (Late Jurassic to Early Cretaceous, southern Tanzania): definition, palaeoenvironments, and sequence stratigraphy Robert Bussert1, Wolf-Dieter Heinrich2 and Martin Aberhan*,2 1 Institut fr Angewandte Geowissenschaften, Technische Universitt Berlin, Skr. BH 2, Ernst-Reuter-Platz 1, 10587 Berlin, Germany. E-mail: [email protected] 2 Museum fr Naturkunde – Leibniz Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, Invalidenstr. 43, 10115 Berlin, Germany. E-mail: [email protected]; [email protected] Abstract Received 8 December 2008 The well-known Late Jurassic to Early Cretaceous Tendaguru Beds of southern Tanza- Accepted 15 February 2009 nia have yielded fossil plant remains, invertebrates and vertebrates, notably dinosaurs, Published 3 August 2009 of exceptional scientific importance. Based on data of the German-Tanzanian Tenda- guru Expedition 2000 and previous studies, and in accordance with the international stratigraphic guide, we raise the Tendaguru Beds to formational rank and recognise six members (from bottom to top): Lower Dinosaur Member, Nerinella Member, Middle Dinosaur Member, Indotrigonia africana Member, Upper Dinosaur Member, and Ruti- trigonia bornhardti-schwarzi Member. We characterise and discuss each member in de- tail in terms of derivation of name, definition of a type section, distribution, thickness, lithofacies, boundaries, palaeontology, and age. The age of the whole formation appar- ently ranges at least from the middle Oxfordian to the Valanginian through Hauterivian or possibly Aptian. The Tendaguru Formation constitutes a cyclic sedimentary succes- sion, consisting of three marginal marine, sandstone-dominated depositional units and three predominantly coastal to tidal plain, fine-grained depositional units with dinosaur remains. -
A Study of the Genus Scaphiopus: the Spade-Foot Toads
Great Basin Naturalist Volume 1 Number 1 Article 4 7-25-1939 A study of the genus Scaphiopus: the spade-foot toads Vasco M. Tanner Brigham Young University, Provo, UT Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Tanner, Vasco M. (1939) "A study of the genus Scaphiopus: the spade-foot toads," Great Basin Naturalist: Vol. 1 : No. 1 , Article 4. Available at: https://scholarsarchive.byu.edu/gbn/vol1/iss1/4 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. A STUI)^' ( )F THE CiI':NUS SCAIMIIOPUS^^) Thk Spade-foot Toads AWSCO M. TANNER Professor of Zoology and Entomolog\- Brigham Young University INTRODUCTION It is a little more than a Inindred years since Holbrook, 1836, erected the t;enus Scaplilopits descril)in,ij solifariiis, a species found along the Atlantic Coast, as the type of the genus. This species, how- ever, was described the year prevousl}-, 1835, by Harlan as Rana Jiolhrookii : thus holhrookii becomes the accepted name of the genotype. Many species and sub-species have been named since this time, the great majority of them, however, have been considered as synonyms. In this study I liave recognized the following species: holhrookii, hitrtcrii, couchii, homhifrons, haminondii, and interttiontamis. A vari- ety of holhrookii, described by Garman as alhiis, from Key West. Florida, may be a vaUd form ; but since I have had only a specimen or two for study. -
Biol 119 – Herpetology Lab 4: Phylogeny Exercise, Anuran Diversity Fall 2013
Biol 119 – Herpetology Lab 4: Phylogeny Exercise, Anuran Diversity Fall 2013 Philip J. Bergmann Lab objectives The objectives of today’s lab are to: 1. Continue to familiarize yourselves with local herps and their external anatomy. 2. Use this knowledge to collect morphological character data from specimens. 3. Reconstruct a phylogeny using your collected character data. 4. Be able to discuss phylogenetic concepts introduced in lecture in the context of the lab. 5. Familiarize yourselves with extant diversity of the Anura. Collecting data from specimens and using it to reconstruct a phylogeny will reinforce your knowledge of local herps and accustom you to using the terminology from last week’s lab. During today’s lab you will also begin studying amphibian diversity. The lab will introduce the Anura (frogs). Tips for learning the material Take some time today to review material that was covered last week. The same specimens are out to allow you to do this. Use the opportunity to quiz yourself or a partner by covering up species names and identifying specimens. Note which ones you find easy to ID and which ones give you trouble. Why do those give you troubles? Refine your criteria for differentiating them and take some more notes. However, do not spend too much time reviewing last week’s material – there are new things to cover as well. Today’s phylogeny exercise will help you to reinforce some of this material, at least for the frogs, which will be the focus of that exercise. Although the Anura has a conserved body plan – all are rather short and rigid bodied, with well-developed limbs, there is an incredible amount of diversity. -
Three Different Types of Tumors in Salientia
Three Different Types of Tumors in Salientia E. ELKAN (Group IX Laboratories, Shrod4ts Hospital, Watford, Herts. England) SUMMARY Three tumors of widely differing structure occurring in, Salientia (Amphibia) are described. They are: (a) a nephroblastoma, (b) an atypical facial papilloma or melano carcinoma, and (c) an epithelioma resembling ulcus rodens. The first two tumors oc curred in specimens of the South African claw-footed toad (Xenopus laevis D.), the third in a specimen of the common grass frog (Rana temporaria L.). A NEPHROBLASTOMAIN Xenopus laevis DAUDIN any of these animals falls ill, it hides in the most Neoplasms of various kinds are common in fish, inaccessible corner of the cage; many are, in any much rarer in reptiles, very rare in amphibians. case, nocturnal in their habits, and when their The first comprehensive review of the tumors de death is discovered, decomposition has usually ad scribed from cold-blooded animals was made by vanced to such a degree as to make further inves Luckéand Schlumberger (Balls [1] lists 68 relevant tigation impossible. Much interesting material is titles) in 1948—1949.Cohrs et a!. in their textbook lost in this way. Circumstances are a little more Pathology ofLaboratory Animak reviewed the liter promising in laboratories where less attention is ature up to 196g. Finally Balls (1), reporting on paid to the imitation of natural surroundings and six new cases in Xenopus, reviewed the literature more to the health of the animals. However, even up to 196g. The present paper gives a short decrip those departments which keep large numbers of tion of three types of tumors not previously seen frogs under constant close supervision have re in Salientia. -
Recovery Strategy for the Great Basin Spadefoot (Spea Intermontana) in Canada
Species at Risk Act Recovery Strategy Series Adopted under Section 44 of SARA Recovery Strategy for the Great Basin Spadefoot (Spea intermontana) in Canada Great Basin Spadefoot 2017 1 Recommended citation: Environment and Climate Change Canada. 2017. Recovery Strategy for the Great Basin Spadefoot (Spea intermontana) in Canada. Species at Risk Act Recovery Strategy Series. Environment and Climate Change Canada, Ottawa. 2 parts, 31 pp. + 40 pp. For copies of the recovery strategy, or for additional information on species at risk, including the Committee on the Status of Endangered Wildlife in Canada (COSEWIC) Status Reports, residence descriptions, action plans, and other related recovery documents, please visit the Species at Risk (SAR) Public Registry1. Cover illustration: © Karl Larsen Également disponible en français sous le titre « Programme de rétablissement du crapaud du Grand Bassin (Spea intermontana) au Canada » © Her Majesty the Queen in Right of Canada, represented by the Minister of Environment and Climate Change, 2017. All rights reserved. ISBN 978-0-660-24364-1 Catalogue no. En3-4/279-2017E-PDF Content (excluding the illustrations) may be used without permission, with appropriate credit to the source. 1 http://sararegistry.gc.ca/default.asp?lang=En&n=24F7211B-1 RECOVERY STRATEGY FOR THE GREAT BASIN SPADEFOOT (Spea intermontana) IN CANADA 2017 Under the Accord for the Protection of Species at Risk (1996), the federal, provincial, and territorial governments agreed to work together on legislation, programs, and policies to protect wildlife species at risk throughout Canada. In the spirit of cooperation of the Accord, the Government of British Columbia has given permission to the Government of Canada to adopt the Recovery Plan for the Great Basin Spadefoot (Spea intermontana) in British Columbia (Part 2) under Section 44 of the Species at Risk Act (SARA). -
How Ecology and Evolution Shape Species Distributions and Ecological Interactions Across Time and Space
HOW ECOLOGY AND EVOLUTION SHAPE SPECIES DISTRIBUTIONS AND ECOLOGICAL INTERACTIONS ACROSS TIME AND SPACE by IULIAN GHERGHEL Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy Advisor: Ryan A. Martin Department of Biology CASE WESTERN RESERVE UNIVERSITY January, 2021 CASE WESTERN RESERVE UNIVERSITY SCHOOL OF GRADUATE STUDIES We hereby approve the dissertation of Iulian Gherghel Candidate for the degree of Doctor of Philosophy* Committee Chair Dr. Ryan A. Martin Committee Member Dr. Sarah E. Diamond Committee Member Dr. Jean H. Burns Committee Member Dr. Darin A. Croft Committee Member Dr. Viorel D. Popescu Date of Defense November 17, 2020 * We also certify that written approval has been obtained for any proprietary material contained therein TABLE OF CONTENTS List of tables ........................................................................................................................ v List of figures ..................................................................................................................... vi Acknowledgements .......................................................................................................... viii Abstract ............................................................................................................................. iix INTRODUCTION............................................................................................................. 1 CHAPTER 1. POSTGLACIAL RECOLONIZATION OF NORTH AMERICA BY SPADEFOOT TOADS: INTEGRATING