Kinematics and Hydrodynamics Analysis of Swimming Anurans Reveals Striking Inter- Specific Differences in the Mechanism for Producing Thrust
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Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna. -
Rampant Tooth Loss Across 200 Million Years of Frog Evolution
bioRxiv preprint doi: https://doi.org/10.1101/2021.02.04.429809; this version posted February 6, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. 1 Rampant tooth loss across 200 million years of frog evolution 2 3 4 Daniel J. Paluh1,2, Karina Riddell1, Catherine M. Early1,3, Maggie M. Hantak1, Gregory F.M. 5 Jongsma1,2, Rachel M. Keeffe1,2, Fernanda Magalhães Silva1,4, Stuart V. Nielsen1, María Camila 6 Vallejo-Pareja1,2, Edward L. Stanley1, David C. Blackburn1 7 8 1Department of Natural History, Florida Museum of Natural History, University of Florida, 9 Gainesville, Florida USA 32611 10 2Department of Biology, University of Florida, Gainesville, Florida USA 32611 11 3Biology Department, Science Museum of Minnesota, Saint Paul, Minnesota USA 55102 12 4Programa de Pós Graduação em Zoologia, Universidade Federal do Pará/Museu Paraense 13 Emilio Goeldi, Belém, Pará Brazil 14 15 *Corresponding author: Daniel J. Paluh, [email protected], +1 814-602-3764 16 17 Key words: Anura; teeth; edentulism; toothlessness; trait lability; comparative methods 1 bioRxiv preprint doi: https://doi.org/10.1101/2021.02.04.429809; this version posted February 6, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. -
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. -
(Temnospondyli), and the Evolution of Modern
THE LOWER PERMIAN DISSOROPHOID DOLESERPETON (TEMNOSPONDYLI), AND THE EVOLUTION OF MODERN AMPHIBIANS Trond Sigurdsen Department of Biology McGill University, Montreal November 2009 A thesis submitted to McGill University in partial fulfillment of the requirements of the degree of Doctor of Philosophy © Trond Sigurdsen 2009 1 ACKNOWLEDGMENTS I am deeply grateful to my supervisors Robert L. Carroll and David M. Green for their support, and for revising and correcting the drafts of the individual chapters. Without their guidance, encouragement, and enthusiasm this project would not have been possible. Hans Larsson has also provided invaluable help, comments, and suggestions. Special thanks go to John R. Bolt, who provided specimens and contributed to Chapters 1 and 3. I thank Farish Jenkins, Jason Anderson, and Eric Lombard for making additional specimens available. Robert Holmes, Jean-Claude Rage, and Zbyněk Roček have all provided helpful comments and observations. Finally, I would like to thank present and past members of the Paleolab at the Redpath Museum, Montreal, for helping out in various ways. Specifically, Thomas Alexander Dececchi, Nadia Fröbisch, Luke Harrison, Audrey Heppleston and Erin Maxwell have contributed helpful comments and technical insight. Funding was provided by NSERC, the Max Stern Recruitment Fellowship (McGill), the Delise Allison and Alma Mater student travel grants (McGill), and the Society of Vertebrate Paleontology Student Travel Grant. 2 CONTRIBUTIONS OF AUTHORS Chapters 1 and 3 were written in collaboration with Dr. John R. Bolt from the Field Museum of Chicago. The present author decided the general direction of these chapters, studied specimens, conducted the analyses, and wrote the final drafts. -
ESCAPA, I.H., J. STERLI, D. POL, & L. NICOLI. 2008. Jurassic
Revista de la Asociación Geológica Argentina 63 (4): 613 - 624 (2008) 613 JURASSIC TETRAPODS AND FLORA OF CAÑADÓN ASFALTO FORMATION IN CERRO CÓNDOR AREA, CHUBUT PROVINCE Ignacio H. ESCAPA1, Juliana STERLI2, Diego POL1 and Laura NICOLI3 1 CONICET. Museo Paleontológico Egidio Feruglio. Trelew, Chubut. Email: [email protected], [email protected] 2 CONICET. Museo de Historia Natural de San Rafael, San Rafael, Mendoza. Email: [email protected] 3 CONICET. Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires. Buenos Aires. Email: [email protected] ABSTRACT The plant and tetrapod fossil record of the Cañadón Asfalto Formation (Middle to Late Jurassic) found in Cerro Cóndor area (Chubut Province) is summarized here. The flora is dominated by conifers (Araucariaceae, Cupressaceae sensu lato) but also includes ferns and equisetaleans. The tetrapod fauna is composed of dinosaur taxa described in the 70's as well as other remains recently described and other vertebrate groups such as amphibians, turtles, and mammals. The amphibian remains have been interpreted as representatives of a new species of Notobatrachus, considered one of the most basal members of the anuran lineage. Similarly, turtle remains have been recently recognized as a new species of basal turtle, bringing valuable infor- mation about the early evolution of this group. The dinosaur remains are largely dominated by saurischian taxa, represented by basal forms of Eusauropoda and Tetanurae. In addition, three different mammalian species have been identified and con- sidered as early representatives of an endemic Gondwanan mammalian fauna. The fossil record of this formation represents the most completely known biota from the continental Middle to Late Jurassic of the Southern Hemisphere and one of the most complete of the entire world. -
Downloaded from Brill.Com10/11/2021 02:28:07AM Via Free Access 202 Ascarrunz Et Al
Contributions to Zoology, 85 (2) 201-234 (2016) Triadobatrachus massinoti, the earliest known lissamphibian (Vertebrata: Tetrapoda) re-examined by µCT scan, and the evolution of trunk length in batrachians Eduardo Ascarrunz1, 2, Jean-Claude Rage2, Pierre Legreneur3, Michel Laurin2 1 Department of Geosciences, University of Fribourg, Chemin du Musée 6, 1700 Fribourg, Switzerland 2 Sorbonne Universités CR2P, CNRS-MNHN-UPMC, Département Histoire de la Terre, Muséum National d’Histoire Naturelle, CP 38, 57 rue Cuvier, 75005 Paris, France 3 Inter-University Laboratory of Human Movement Biology, University of Lyon, 27-29 Bd du 11 Novembre 1918, 69622 Villeurbanne Cédex, France 4 E-mail: [email protected] Key words: Anura, caudopelvic apparatus, CT scan, Salientia, Triassic, trunk evolution Abstract Systematic palaeontology ........................................................... 206 Geological context and age ................................................. 206 Triadobatrachus massinoti is a batrachian known from a single Description .............................................................................. 207 fossil from the Early Triassic of Madagascar that presents a com- General appearance of the reassembled nodule ............ 207 bination of apomorphic salientian and plesiomorphic batrachian Skull ........................................................................................... 208 characters. Herein we offer a revised description of the specimen Axial skeleton ......................................................................... -
The Earliest Equatorial Record of Frogs from the Late Triassic of Arizona
Palaeontology The earliest equatorial record of frogs royalsocietypublishing.org/journal/rsbl from the Late Triassic of Arizona Michelle R. Stocker1, Sterling J. Nesbitt1, Ben T. Kligman1,2, Daniel J. Paluh3, Adam D. Marsh2, David C. Blackburn3 and William G. Parker2 Research 1Department of Geosciences, Virginia Tech, Blacksburg, VA 24061, USA 2 Cite this article: Stocker MR, Nesbitt SJ, Petrified Forest National Park, 1 Park Road, Petrified Forest, AZ 86028, USA 3Florida Museum of Natural History, University of Florida, Gainesville, FL 32611, USA Kligman BT, Paluh DJ, Marsh AD, Blackburn DC, Parker WG. 2019 The earliest equatorial record MRS, 0000-0002-6473-8691; SJN, 0000-0002-7017-1652; BTK, 0000-0003-4400-8963; DJP, 0000-0003-3506-2669; ADM, 0000-0002-3223-8940; DCB, 0000-0002-1810-9886; of frogs from the Late Triassic of Arizona. Biol. WGP, 0000-0002-6005-7098 Lett. 15: 20180922. http://dx.doi.org/10.1098/rsbl.2018.0922 Crown-group frogs (Anura) originated over 200 Ma according to molecular phylogenetic analyses, though only a few fossils from high latitudes chronicle the first approximately 60 Myr of frog evolution and distribution. We report fos- sils that represent both the first Late Triassic and the earliest equatorial record of Received: 29 December 2018 Salientia, the group that includes stem and crown-frogs. These small fossils con- Accepted: 1 February 2019 sist of complete and partial ilia with anteriorly directed, elongate and distally hollow iliac blades. These features of these ilia, including the lack of a prominent dorsal protuberance and a shaft that is much longer than the acetabular region, suggest a closer affinity to crown-group Anura than to Early Triassic stem anur- ans Triadobatrachus from Madagascar and Czatkobatrachus from Poland, both Subject Areas: high-latitude records. -
Tetrapod Biostratigraphy and Biochronology Across the Triassic-Jurassic Boundary in Northeastern Arizona
Heckert, A.B., and Lucas, S.G., eds., 2005, Vertebrate Paleontology in Arizona. New Mexico Museum of Natural History and Science Bulletin No. 29. 84 TETRAPOD BIOSTRATIGRAPHY AND BIOCHRONOLOGY ACROSS THE TRIASSIC-JURASSIC BOUNDARY IN NORTHEASTERN ARIZONA SPENCER G. LUCAS1, LAWRENCE H. TANNER2 and ANDREW B. HECKERT3 1New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375; 2Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY, 13214; 3Department of Geology, Appalachian State University, ASU Box 32067, Boone, NC, 28608-2067 Abstract—Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups in northeastern Arizona and adjacent areas preserve tetrapod body fossils and footprints that are one of the world’s most extensive tetrapod fossil records across the Triassic-Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean-Wassonian boundary approximates the Triassic-Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic-Jurassic transition on the southern Colorado Plateau confirms that non-crocodilian crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. Keywords: Triassic, Jurassic, vertebrate, biostratigraphy, Arizona, Glen Canyon Gp, Moenave Fm INTRODUCTION 114o Gateway Lisbon Valley The Four Corners (common boundary of Utah, Colorado, UTAH 50 km COLORADO Arizona and New Mexico) sit in the southern portion of the Colo- rado Plateau (Fig. -
Calsoyasuchus Valliceps, a New Crocodyliform from the Early Jurassic Kayenta Formation of Arizona
Journal of Vertebrate Paleontology 22(3):593±611, September 2002 q 2002 by the Society of Vertebrate Paleontology CALSOYASUCHUS VALLICEPS, A NEW CROCODYLIFORM FROM THE EARLY JURASSIC KAYENTA FORMATION OF ARIZONA RONALD S. TYKOSKI1,2, TIMOTHY B. ROWE1,2,3, RICHARD A. KETCHAM1,3, and MATTHEW W. COLBERT1,2,3 1Jackson School of Geosciences, [email protected]; 2Texas Memorial Museum Vertebrate Paleontology Laboratory; 3High Resolution X-ray CT Facility, The University of Texas at Austin, Austin, Texas 78712 ABSTRACTÐWe describe a new fossil crocodyliform archosaur from the Early Jurassic Kayenta Formation of the Navajo Nation that is surprisingly derived for so ancient a specimen. High-resolution X-ray CT analysis reveals that its long snout houses an extensive system of pneumatic paranasal cavities. These are among the most distinctive features of modern crocodylians, yet the evolutionary history of this unique system has been obscured by the inaccessibility of internal structures in most fossil crania. Preliminary phylogenetic analysis indicates that the new species is the oldest known member of a monophyletic Goniopholididae, and within this lineage to be the sister taxon of Eutretauranosu- chus, from the Late Jurassic Morrison formation of Colorado. Goniopholididae became extinct at the end of the Cretaceous, but it is more closely related to living crocodylians than are several lineages known only from Cretaceous and younger fossils. The new taxon nearly doubles the known length of goniopholid history and implies a deep, as yet undiscovered, Mesozoic history for several crocodyliform lineages that were once thought to have relatively com- plete fossil records. INTRODUCTION 7) for this report. -
BOA1.2 Introduction of Amphibians.Key
The Biology of Amphibians @ Agnes Scott College Mark Mandica Executive Director The Amphibian Foundation [email protected] 678 379 TOAD (8623) Phyllomedusidae: Agalychnis moreletii 1.2: Introduction of Amphibians Centrolenidae: Hyalinobatrachium valeroi 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 *Gerobatrachus may be the sister taxon Temnospondyls † to Batrachia Tetrapods Osteichthyes Sarcopterygian (Bony Fishes) (Lobe-fin Fishes) Amphibian Reign Time Period Devonian Carboniferus Permian Triassic Jurassic Cretaceous Millions of Years Ago (420 MYA) (350 MYA) (300 MYA) (250 MYA) (200 MYA) (150-65 MYA) Present Day resembles Plate Tectonics Gondwana + Laurussia Pangea Pangea Pangea begins to break Pangea breaks present day The Biology of Amphibians amphibbio.amphibianfoundation.org Plate Tectonics 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 *Gerobatrachus may be the sister taxon Temnospondyls † to Batrachia Tetrapods Osteichthyes Sarcopterygian (Bony Fishes) (Lobe-fin Fishes) Amphibian -
On the Origin of and Phylogenetic Relationships Among Living Amphibians
On the origin of and phylogenetic relationships among living amphibians Rafael Zardoya*† and Axel Meyer‡ *Museo Nacional de Ciencias Naturales, Jose´Gutierrez Abascal, 2, 28006 Madrid, Spain; and ‡Department of Biology, University of Konstanz, 78457 Konstanz, Germany Edited by David B. Wake, University of California, Berkeley, CA, and approved April 4, 2001 (received for review September 22, 2000) The phylogenetic relationships among the three orders of modern (9) integrated previous morphological and paleontological evi- amphibians (Caudata, Gymnophiona, and Anura) have been esti- dence, and concluded that the Lissamphibia were a natural mated based on both morphological and molecular evidence. Most group. The monophyly of Lissamphibia has since gained wide morphological and paleontological studies of living and fossil acceptance among researchers (refs. 1 and 10–16; Fig. 1 a–c). A amphibians support the hypothesis that salamanders and frogs are noteworthy exception is Carroll (17–21), who suggests that sister lineages (the Batrachia hypothesis) and that caecilians are Lissamphibia are nonmonophyletic because he believes that more distantly related. Previous interpretations of molecular data salamanders and caecilians have affinities with different lineages based on nuclear and mitochondrial rRNA sequences suggested of microsauria (an extinct group of Lepospondyl amphibians), that salamanders and caecilians are sister groups to the exclusion whereas frogs are related to another extinct group, the temno- of frogs. In an attempt to resolve this apparent conflict, the spondyl amphibians (Fig. 1d). complete mitochondrial genomes of a salamander (Mertensiella Although monophyly of the Lissamphibia is widely accepted, luschani) and a caecilian (Typhlonectes natans) were determined it is still controversial whether the extinct temnospondyls (Fig. -
Presence of Amphibian Species Prediction Using Features Obtained
International Journal of Academic and Applied Research (IJAAR) ISSN: 2643-9603 Vol. 4 Issue 11, November - 2020, Pages: 13-22 Presence of Amphibian Species Prediction Using Features Obtained from GIS and Satellite Images Nadia Shaker Habib, Omar Kamal Abu Maghasib, Ahmed Rashad Al-Ghazali, Bassem S. Abu-Nasser, Samy S. Abu-Naser Department of Information Technology, Faculty of Engineering and Information Technology, Al-Azhar University - Gaza, Palestine Abstract: The establishment of the transport infrastructure is usually preceded by an EIA procedure, which should determine amphibian breeding sites and migration routes. However, evaluation is very difficult due to the large number of habitats spread over a vast area and the limited time available for field work. An artificial Neural Network (ANN) is proposed for predicting the presence of amphibians species near the water reservoirs based on features obtained from GIS systems and satellite images. The dataset collected from UCI Machine Learning repository. The dataset is a multi-label classification problem. The goal of this study is to predict the presence of amphibians species near the water reservoirs based on features obtained from GIS systems and satellite images. After preprocessing the data, the proposed model was trained and evaluated. The accuracy of the proposed model for predicting the presence of amphibian’s species was 100%. Keywords: ANN, JNN, amphibian, multi-label classification, 1. Introduction Amphibians are ectothermic, tetrapod vertebrates of the class Amphibia. All living amphibians belong to the group Lissamphibia. They inhabit a wide variety of habitats, with most species living with in terrestrial, fossorial, arboreal or freshwater aquatic ecosystems. Thus amphibians typically start out as larvae living in water, but some species have developed behavioral adaptations to bypass this.