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The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
Amphibia: Anura: Megophryidae) from Mount Jinggang, China, Based on Molecular and Morphological Data
Zootaxa 3546: 53–67 (2012) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2012 · Magnolia Press Article ISSN 1175-5334 (online edition) urn:lsid:zoobank.org:pub:94669404-4465-48A9-AB35-8860F1E46C82 Description of a new species of the genus Xenophrys Günther, 1864 (Amphibia: Anura: Megophryidae) from Mount Jinggang, China, based on molecular and morphological data YING-YONG WANG1,4, TIAN-DU ZHANG1, JIAN ZHAO2, YIK-HEI SUNG3, JIAN-HUAN YANG1, HONG PANG1 & ZHONG ZHANG2 1State Key Laboratory of Biocontrol / The Museum of Biology, School of Life Sciences, Sun Yat-sen University, Guangzhou 510275, P. R . C h in a 2Jinggangshan National Nature Reserve, Ciping, 343600, Jinggangshan City, Jiangxi, P.R. China 3Kadoorie Conservation China, Kadoorie Farm and Botanic Garden, Lam Kam Road, Tai Po, Hong Kong 4Corresponding author. E-mail: [email protected] Abstract A new species, Xenophrys jinggangensis sp. nov., is described based on a series of specimens collected from Mount Jing- gang, Jiangxi Province, Eastern China. The new species can be easily distinguished from other known congeners by mor- phology, morphometrics and molecular data of the mitochondrial 16SrRNA gene. The new species is characterized by its small size with adult females measuring 38.4–41.6 mm in snout-vent length and males measuring 35.1–36.7 mm; head length approximately equal to head width; tympanum large and distinct, about 0.8 times of eye diameter; vomerine teeth on two weak ridges; tongue not notched behind; relative finger length II < I < IV < III; slight lateral fringes present on digits; toes bases with thick, fleshy web; dorsum with tubercles and swollen dorsolateral folds; large pustules scattered on flanks; and unique color patterns. -
The Impact of Anchored Phylogenomics and Taxon Sampling on Phylogenetic Inference in Narrow-Mouthed Frogs (Anura, Microhylidae)
Cladistics Cladistics (2015) 1–28 10.1111/cla.12118 The impact of anchored phylogenomics and taxon sampling on phylogenetic inference in narrow-mouthed frogs (Anura, Microhylidae) Pedro L.V. Pelosoa,b,*, Darrel R. Frosta, Stephen J. Richardsc, Miguel T. Rodriguesd, Stephen Donnellane, Masafumi Matsuif, Cristopher J. Raxworthya, S.D. Bijug, Emily Moriarty Lemmonh, Alan R. Lemmoni and Ward C. Wheelerj aDivision of Vertebrate Zoology (Herpetology), American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024, USA; bRichard Gilder Graduate School, American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024, USA; cHerpetology Department, South Australian Museum, North Terrace, Adelaide, SA 5000, Australia; dDepartamento de Zoologia, Instituto de Biociencias,^ Universidade de Sao~ Paulo, Rua do Matao,~ Trav. 14, n 321, Cidade Universitaria, Caixa Postal 11461, CEP 05422-970, Sao~ Paulo, Sao~ Paulo, Brazil; eCentre for Evolutionary Biology and Biodiversity, The University of Adelaide, Adelaide, SA 5005, Australia; fGraduate School of Human and Environmental Studies, Kyoto University, Sakyo-ku, Kyoto 606-8501, Japan; gSystematics Lab, Department of Environmental Studies, University of Delhi, Delhi 110 007, India; hDepartment of Biological Science, Florida State University, Tallahassee, FL 32306, USA; iDepartment of Scientific Computing, Florida State University, Dirac Science Library, Tallahassee, FL 32306-4120, USA; jDivision of Invertebrate Zoology, American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024, USA Accepted 4 February 2015 Abstract Despite considerable progress in unravelling the phylogenetic relationships of microhylid frogs, relationships among subfami- lies remain largely unstable and many genera are not demonstrably monophyletic. -
Frogs (Amphibia, Anura) from the Eocene and Oligocene of the Phosphorites Du Quercy (France)
FOSSIL IMPRINT • vol. 72 • 2016 • no. 1-2 • pp. 53–66 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) FROGS (AMPHIBIA, ANURA) FROM THE EOCENE AND OLIGOCENE OF THE PHOSPHORITES DU QUERCY (FRANCE). AN OVERVIEW JEAN-CLAUDE RAGE Sorbonne Universités, CR2P CNRS-MNHN-UPMC Paris 6, Département Histoire de la Terre, Muséum National d’Histoire Naturelle, CP 38, 57 rue Cuvier, 75005 Paris, France; e-mail: [email protected]. Rage, J.-C. (2016): Frogs (Amphibia, Anura) from the Eocene and Oligocene of the Phosphorites du Quercy (France). An overview. – Fossil Imprint, 72(1-2): 53–66, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on-line). Abstract: Anuran assemblages from the Eocene and Oligocene of the Phosphorites du Quercy (southwestern France) are documented by a modest number of isolated bones, incomplete skulls, and some ‘mummies’. However, at the family level, the diversity is not significantly lower than in coeval frog assemblages from other regions. By contrast, a larger number of amniote specimens and taxa are known from the Phosphorites. The sparse anuran record within the Phosphorites most likely results from the karstic environment in which the fossiliferous sites formed. Such an environment is not favorable for animals dependent on water and moisture. Upper middle and upper Eocene localities in the Phosphorites produced Alytidae, Pelobatidae, Pelodytidae and ranoids. The presence of bufonids or microhylids, and rhacophorids cannot be definitely rejected, and potentially distinctive, but unidentifiable taxa also may be present. The occurrence of Pelodytidae in the Eocene of Europe is confirmed by diagnostic bones from the Phosphorites. In Oligocene localities in the Phosphorites, anurans are even less diverse, with only Alytidae, Pelobatidae and ranoids having been recovered. -
Strange Tadpoles from the Lower Miocene of Turkey: Is Paedogenesis Possible in Anurans?
Strange tadpoles from the lower Miocene of Turkey: Is paedogenesis possible in anurans? ALAIN DUBOIS, STÉPHANE GROSJEAN, and JEAN−CLAUDE PAICHELER Dubois, A., Grosjean, S., and Paicheler, J.−C. 2010. Strange tadpoles from the lower Miocene of Turkey: Is paedogenesis possible in anurans? Acta Palaeontologica Polonica 55 (1): 43–55. Fossil material from the lower Miocene collected in the basin lake of Beşkonak (Turkey) included 19 slabs showing 19 amphibian anuran tadpoles of rather large size, at Gosner stages 36–38. These well preserved specimens show many mor− phological and skeletal characters. They are here tentatively referred to the genus Pelobates. Two of these tadpoles show an unusual group of black roundish spots in the abdominal region, and a third similar group of spots is present in another slab but we were unable to state if it was associated with a tadpole or not. Several hypotheses can be proposed to account for these structures: artefacts; intestinal content (seeds; inert, bacterial or fungal aggregations; eggs); internal or external parasites; diseases; eggs produced by the tadpole. The latter hypothesis is discussed in detail and is shown to be unlikely for several reasons. However, in the improbable case where these spots would correspond to eggs, this would be the first reported case of natural paedogenesis in anurans, a phenomenon which has been so far considered impossible mostly for anatomical reasons (e.g., absence of space in the abdominal cavity). Key words: Amphibia, Anura, egg, fossil, paedogenesis, tadpole, Miocene, Turkey. Alain Dubois [[email protected]] and Stéphane Grosjean [[email protected]], Département de Sytématique & Evolu− tion, Muséum National d’Histoire Naturelle, UMR 7205 Origine, Structure et Evolution de la Biodiversité, Reptiles et Amphibiens, Case 30, 25 rue Cuvier, 75005 Paris, France; Jean−Claude Paicheler [[email protected]], Laboratoire de Paléoparasitologie, UFR de Pharmacie, 51 rue Cognacq Jay, 51096 Reims Cedex, France. -
Curriculum Vitae
CURRICULUM VITAE AMY C. HENRICI Collection Manager Section of Vertebrate Paleontology Carnegie Museum of Natural History 4400 Forbes Avenue Pittsburgh, Pennsylvania 15213-4080, USA Phone:(412)622-1915 Email: [email protected] BACKGROUND Birthdate: 24 September 1957. Birthplace: Pittsburgh. Citizenship: USA. EDUCATION B.A. 1979, Hiram College, Ohio (Biology) M.S. 1989, University of Pittsburgh, Pennsylvania (Geology) CAREER Carnegie Museum of Natural History (CMNH) Laboratory Technician, Section of Vertebrate Paleontology, 1979 Research Assistant, Section of Vertebrate Paleontology, 1980 Curatorial Assistant, Section of Vertebrate Paleontology, 1980-1984 Scientific Preparator, Section of Paleobotany, 1985-1986 Scientific Preparator, Section of Vertebrate Paleontology, 1985-2002 Acting Collection Manager/Scientific Preparator, 2003-2004 Collection Manager, 2005-present PALEONTOLOGICAL FIELD EXPERIENCE Late Pennsylvanian through Early Permian of Colorado, New Mexico and Utah (fish, amphibians and reptiles) Early Permian of Germany, Bromacker quarry (amphibians and reptiles) Triassic of New Mexico, Coelophysis quarry (Coelophysis and other reptiles) Upper Jurassic of Colorado (mammals and herps) Tertiary of Montana, Nevada, and Wyoming (mammals and herps) Pleistocene of West Virginia (mammals and herps) Lake sediment cores and lake sediment surface samples, Wyoming (pollen and seeds) PROFESSIONAL APPOINTMENTS Associate Editor, Society of Vertebrate Paleontology, 1998-2000. Research Associate in the Science Division, New Mexico Museum of Natural History and Science, 2007-present. PROFESSIONAL ASSOCIATIONS Society of Vertebrate Paleontology Paleontological Society LECTURES and TUTORIALS (Invited and public) 1994. Middle Eocene frogs from central Wyoming: ontogeny and taphonomy. California State University, San Bernardino 1994. Mechanical preparation of vertebrate fossils. California State University, San Bernardino 1994. Mechanical preparation of vertebrate fossils. University of Chicago 2001. -
The Conservation Status of Biological Resources in the Philippines
: -.^,rhr:"-i-3'^^=£#?^-j^.r-^a^ Sj2 r:iw0,">::^^'^ \^^' Cfl|*ti-»;;^ THE CONSERVATION STATUS OF BIOLOGICAL RESOURCES IN THE PHILIPPINES A RRF'OHT V^Y THK lUCN CONSKRVATION MONITORING CENT:-!E PfcparGd by Roger Cox for the lnLf5rnaLion?.l InsLituLo Cor Knvironment and Development (IIED) February 1988 / fgrMsa^jnt-^'-agyga-- •r-r- ;.«-'> t ^-' isr* 1*.- i^^s. , r^^, ^».|;; ^b-^ ^.*%-^ *i,r^-v . iinnc [ '»/' C'A'. aSM!': Vi - '«.;s^ ; a-* f%h '3;riti7;.:- n'^'ji K ;ii;!'r ' <s:ii.uiy.. viii. K A xo.^ jf^'r;.' 3 10 ciJuJi i\ Ji\{ :::) Jnj:kf- .i. n ( im'.i) •V'lt r'v - -V.-^f~^?fl LP-ife- f^^ s.:.... --11 -^M.jj^^^ riB CC./Sfc^RvAriON .<*TC.rj^. OF EI3U:i' "I.VJ, JbO'TSOURCES ^^a THE PHILIPPlVl'fC ;j^...^..-r'^^ I ilRPOHT BY THK ILCJJ CGJJSIiKVA'ilCN M0N:.V:..):;1NG CKNT ^ Pc'jpas-fjr' ')y Roto* C(/X for the TiKD). {'obruary 1988 Digitized by the Internet Archive in 2010 with funding from UNEP-WCIVIC, Cambridge http://www.archive.org/details/conservationstat88coxr . 7' CONTENTS List of Figures, Appendices and Tables iii Summary iy Acknowledgements vii 1 INTRODUCTION 1.1 Background 1 1.2 Objectives 3 2 METHODS 4 3. FLORA, VEGETATION AND FOREST COVER 3.1 Description of the natural vegetation 4 3.1.1 The forests 4 3.1.2 Other vegetation types 7 3 2 Conservation status of the Philippine flora 8 3.2.1 Introduction 8 3.2.2 Causes of habitat destruction 9 3.2.3 Threatened plant species 11 3. 2. A Centres of plant diversity and endemism 12 4 COASTAL AND MARINE ECOSYSTEMS 4.1 Background 17 4.2 Mangroves 18 4.3 Coral reefs 19 4.4 Seagrass beds 22 5. -
3Systematics and Diversity of Extant Amphibians
Systematics and Diversity of 3 Extant Amphibians he three extant lissamphibian lineages (hereafter amples of classic systematics papers. We present widely referred to by the more common term amphibians) used common names of groups in addition to scientifi c Tare descendants of a common ancestor that lived names, noting also that herpetologists colloquially refer during (or soon after) the Late Carboniferous. Since the to most clades by their scientifi c name (e.g., ranids, am- three lineages diverged, each has evolved unique fea- bystomatids, typhlonectids). tures that defi ne the group; however, salamanders, frogs, A total of 7,303 species of amphibians are recognized and caecelians also share many traits that are evidence and new species—primarily tropical frogs and salaman- of their common ancestry. Two of the most defi nitive of ders—continue to be described. Frogs are far more di- these traits are: verse than salamanders and caecelians combined; more than 6,400 (~88%) of extant amphibian species are frogs, 1. Nearly all amphibians have complex life histories. almost 25% of which have been described in the past Most species undergo metamorphosis from an 15 years. Salamanders comprise more than 660 species, aquatic larva to a terrestrial adult, and even spe- and there are 200 species of caecilians. Amphibian diver- cies that lay terrestrial eggs require moist nest sity is not evenly distributed within families. For example, sites to prevent desiccation. Thus, regardless of more than 65% of extant salamanders are in the family the habitat of the adult, all species of amphibians Plethodontidae, and more than 50% of all frogs are in just are fundamentally tied to water. -
Oviposition Sites of the Hoang Lien Horned Frog, Megophrys Hoanglienensis (Tapley Et Al., 2018)
Herpetology Notes, volume 14: 937-939 (2021) (published online on 29 June 2021) Oviposition sites of the Hoang Lien Horned Frog, Megophrys hoanglienensis (Tapley et al., 2018) Benjamin Tapley1,*, Luan Thanh Nguyen2, Chung Thanh Nguyen3, Giang Truong Hoang3, and Timothy Cutajar4 The genus Megophrys Kuhl & Van Hasselt, 1822 Vietnam and likely qualifies for an assessment as comprises 111 species in seven subgenera (Mahony et Endangered (Tapley et al., 2018). The species is al., 2017; Frost, 2021). Other than advertisement calls associated with streams in broadleaf forests at elevations and larval descriptions there are very few published from 1898–2242 m (Tapley et al., 2018). Males are observations of breeding behaviour and oviposition known to call from streamside vegetation and rocks in sites of Megophrys. Male frogs of the subgenus June, and larvae at stage 26 (Gosner, 1960) have been Brachytarsophrys are reported to call from within deep collected in a 5 m wide stream with rocky substrate in crevices between boulders in streams (Smith, 1921; September (Tapley et al., 2020). Tapley, 2011) and guard egg clutches that are laid in On 11 June 2018 we encountered several clusters water (Stuart, 2005). Megophrys (Brachytarsophrys) of eggs on Mount Fansipan, at a site bordering Sa Pa platyparietus is known to oviposit eggs on the underside District, Lao Cai Province, and Tam Duong District, Lai of boulders (Li et al., 2020). Megophrys (Xenophrys) cf. Chau Province (22.3422°N, 103.7764°E; elevation 2000 major have been reported to lay clutches with hundreds m). One cluster of eggs was adhered to the underside of of white eggs, each with a diameter of approximately a muddy bolder overhanging a seepage with a gravel 1.9 mm (Vassilieva at al., 2016). -
BOA5.1-2 Frog Biology, Taxonomy and Biodiversity
The Biology of Amphibians Agnes Scott College Mark Mandica Executive Director The Amphibian Foundation [email protected] 678 379 TOAD (8623) Phyllomedusidae: Agalychnis annae 5.1-2: Frog Biology, Taxonomy & Biodiversity Part 2, Neobatrachia Hylidae: Dendropsophus ebraccatus CLassification of Order: Anura † Triadobatrachus Ascaphidae Leiopelmatidae Bombinatoridae Alytidae (Discoglossidae) Pipidae Rhynophrynidae Scaphiopopidae Pelodytidae Megophryidae Pelobatidae Heleophrynidae Nasikabatrachidae Sooglossidae Calyptocephalellidae Myobatrachidae Alsodidae Batrachylidae Bufonidae Ceratophryidae Cycloramphidae Hemiphractidae Hylodidae Leptodactylidae Odontophrynidae Rhinodermatidae Telmatobiidae Allophrynidae Centrolenidae Hylidae Dendrobatidae Brachycephalidae Ceuthomantidae Craugastoridae Eleutherodactylidae Strabomantidae Arthroleptidae Hyperoliidae Breviceptidae Hemisotidae Microhylidae Ceratobatrachidae Conrauidae Micrixalidae Nyctibatrachidae Petropedetidae Phrynobatrachidae Ptychadenidae Ranidae Ranixalidae Dicroglossidae Pyxicephalidae Rhacophoridae Mantellidae A B † 3 † † † Actinopterygian Coelacanth, Tetrapodomorpha †Amniota *Gerobatrachus (Ray-fin Fishes) Lungfish (stem-tetrapods) (Reptiles, Mammals)Lepospondyls † (’frogomander’) Eocaecilia GymnophionaKaraurus Caudata Triadobatrachus 2 Anura Sub Orders Super Families (including Apoda Urodela Prosalirus †) 1 Archaeobatrachia A Hyloidea 2 Mesobatrachia B Ranoidea 1 Anura Salientia 3 Neobatrachia Batrachia Lissamphibia *Gerobatrachus may be the sister taxon Salientia Temnospondyls -
Feeding in Amphibians: Evolutionary Transformations and Phenotypic Diversity As Drivers of Feeding System Diversity
Chapter 12 Feeding in Amphibians: Evolutionary Transformations and Phenotypic Diversity as Drivers of Feeding System Diversity Anthony Herrel, James C. O’Reilly, Anne-Claire Fabre, Carla Bardua, Aurélien Lowie, Renaud Boistel and Stanislav N. Gorb Abstract Amphibians are different from most other tetrapods because they have a biphasic life cycle, with larval forms showing a dramatically different cranial anatomy and feeding strategy compared to adults. Amphibians with their exceptional diversity in habitats, lifestyles and reproductive modes are also excellent models for studying the evolutionary divergence in feeding systems. In the present chapter, we review the literature on amphibian feeding anatomy and function published since 2000. We also present some novel unpublished data on caecilian feeding biome- chanics. This review shows that over the past two decades important new insights in our understanding of amphibian feeding anatomy and function have been made possible, thanks to a better understanding of the phylogenetic relationships between taxa, analyses of development and the use of biomechanical modelling. In terms of functional analyses, important advances involve the temperature-dependent nature of tongue projection mechanisms and the plasticity exhibited by animals when switch- A. Herrel (B) Département Adaptations du Vivant, Muséum national d’Histoire naturelle, UMR 7179 C.N.R.S/M.N.H.N, 55 rue Buffon, 75005, Paris Cedex 05, France e-mail: [email protected] J. C. O’Reilly Department of Biomedical Sciences, Ohio University, Cleveland Campus, Cleveland, Ohio 334C, USA A.-C. Fabre · C. Bardua Life Sciences Department, The Natural History Museum, Cromwell Road, London SW7 5BD, UK A. Lowie Department of Biology Evolutionary, Morphology of Vertebrates, Ghent University, K.L. -
New Morphological Synapomorphies for the New World Direct-Developing Frogs (Amphibia: Anura: Terrarana)
Herpetologica, 69(3), 2013, 342–357 Ó 2013 by The Herpetologists’ League, Inc. NEW MORPHOLOGICAL SYNAPOMORPHIES FOR THE NEW WORLD DIRECT-DEVELOPING FROGS (AMPHIBIA: ANURA: TERRARANA) 1 2 3 1,4,5 CARLOS TABOADA ,TARAN GRANT ,JOHN D. LYNCH , AND JULIA´ N FAIVOVICH 1Division´ Herpetologıa,´ Museo Argentino de Ciencias ‘‘Naturales ‘‘Bernardino Rivadavia’’– CONICET, Angel Gallardo 470, C1405DJR, Buenos Aires, Argentina 2Departamento de Zoologia, Instituto de Biociencias,ˆ Universidade de Sa˜o Paulo, Sa˜o Paulo, SP 05508-090, Brazil 3Instituto de Ciencias Naturales, Universidad Nacional de Colombia, Apartado 7495, Bogota´ D. C., Colombia 4Departamento de Biodiversidad y Biologıa´ Experimental, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires ABSTRACT: The New World direct-developing frogs (Terrarana) comprise more than 970 species distributed from the southern United States to northern Argentina. Although the composition of this clade has been remarkably stable for many decades, evidence for its monophyly is derived mostly from DNA sequences with putative phenotypic synapomorphies limited to the occurrence of direct development, an embryonic egg tooth (known in few species), and T-shaped terminal phalanges. Based on a survey of the urogenital and vascular systems and the submandibular musculature of hyloid frogs, we report 16 characters that provide putative synapomorphies at a variety of hierarchic levels. Most significantly, they include seven putative synapomorphies for Terrarana that can be observed through simple dissections, including (1) fusion of the Wolffian ducts, resulting in a single, common cloacal opening; (2) Wolffian duct fusion located anteriorly with a single, common duct along the posterior, . 1/3 of the distance between caudal edge of kidneys and cloacal wall; (3) presence of the posterior dorsolumbar vein; (4) absence of the medial dorsolumbar vein; (5) origin of the posterior caval vein in the anterior 1/3 of the kidneys; (6) posterior origin of dorsolumbar arteries; and (7) presence of the pelvic lymphatic septum.