An Overview of the Upper Carboniferous Fossil Deposit at Linton, Ohio1
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Die Microsauria Des Mitteleuropäischen Rotliegend
Die Microsauria des mitteleuropäischen Rotliegend Dissertation zur Erlangung des Grades „Doktor der Naturwissenschaften" im Promotionsfach Geologie/Paläontologie am Fachbereich Chemie, Pharmazie und Geowissenschaften der Johannes Gutenberg-Universität in Mainz Sabine Glienke geb. in Worms Mainz, 2011 http://d-nb.info/1058187503 Inhalt Inhalt 1. Einleitung 6 1.1. Allgemeine Merkmale und Bearbeitungsgeschichte 6 1.2. Fundorte und Erhaltung 9 2. Methoden, Abkürzungen und Material 16 2.1. Methoden 16 2.1.1. Bearbeitung der Skelette 16 2.1.2. Gewinnung und Bearbeitung der Einzelknochen 16 2.1.3. Kladogramme 17 2.2. Abkürzungen 17 2.2.1. Sammlungen 17 2.2.2. In den Zeichnungen verwendete Abkürzungen 17 2.3. Übersicht über die untersuchten Skelette 19 3. Beschreibungen 21 3.1. Die Familie Brachystelechidae CARROLL& GASKILL, 1978 21 3.1.1. Systematische Stellung 21 3.1.2. Diagnose 21 3.2. Die Gattung Batropetes CARROLL & GASKILL, 1971 21 3.2.1. Systematische Stellung 21 3.2.2. Diagnose 22 3.2.3. Die vier Spezies der Gattung Batropetes 22 3.3. Batropetes niederkirchensis n. sp 26 3.3.1. Diagnose 26 3.3.2. Beschreibung 28 3.3.2.1. Schädel 28 3.3.2.1.1. Schädeldach 28 3.3.2.1.2. Gaumen 38 3.3.2.1.3. Hirnkapsel 43 3.3.2.1.4. Unterkiefer 46 3.3.2.2. Postcraniales Skelett 48 Inhalt 3.4. Batropetes palatinus n. sp 62 3.4.1. Diagnose 62 3.4.2. Beschreibung 63 3.4.2.1. Schädel 74 3.4.2.1.1. Schädeldach 74 3.4.2.1.2. -
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 -
Identifying Heterogeneity in Rates of Morphological Evolution: Discrete Character Change in the Evolution of Lungfish (Sarcopterygii; Dipnoi)
ORIGINAL ARTICLE doi:10.1111/j.1558-5646.2011.01460.x IDENTIFYING HETEROGENEITY IN RATES OF MORPHOLOGICAL EVOLUTION: DISCRETE CHARACTER CHANGE IN THE EVOLUTION OF LUNGFISH (SARCOPTERYGII; DIPNOI) Graeme T. Lloyd,1,2 Steve C. Wang,3 and Stephen L. Brusatte4,5 1Department of Palaeontology, Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom 2E-mail: [email protected] 3Department of Mathematics and Statistics, Swarthmore College, Swarthmore, Pennsylvania 19081 4Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024 5Department of Earth and Environmental Sciences, Columbia University, New York, New York 10025 Received February 9, 2010 Accepted August 15, 2011 Data Archived: Dryad: doi:10.5061/dryad.pg46f Quantifying rates of morphological evolution is important in many macroevolutionary studies, and critical when assessing possible adaptive radiations and episodes of punctuated equilibrium in the fossil record. However, studies of morphological rates of change have lagged behind those on taxonomic diversification, and most authors have focused on continuous characters and quantifying patterns of morphological rates over time. Here, we provide a phylogenetic approach, using discrete characters and three statistical tests to determine points on a cladogram (branches or entire clades) that are characterized by significantly high or low rates of change. These methods include a randomization approach that identifies branches with significantly high rates and likelihood ratio tests that pinpoint either branches or clades that have significantly higher or lower rates than the pooled rate of the remainder of the tree. As a test case for these methods, we analyze a discrete character dataset of lungfish, which have long been regarded as “living fossils” due to an apparent slowdown in rates since the Devonian. -
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha)
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) by Richard Kissel A thesis submitted in conformity with the requirements for the degree of doctor of philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto © Copyright by Richard Kissel 2010 Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) Richard Kissel Doctor of Philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto 2010 Abstract Based on dental, cranial, and postcranial anatomy, members of the Permo-Carboniferous clade Diadectidae are generally regarded as the earliest tetrapods capable of processing high-fiber plant material; presented here is a review of diadectid morphology, phylogeny, taxonomy, and paleozoogeography. Phylogenetic analyses support the monophyly of Diadectidae within Diadectomorpha, the sister-group to Amniota, with Limnoscelis as the sister-taxon to Tseajaia + Diadectidae. Analysis of diadectid interrelationships of all known taxa for which adequate specimens and information are known—the first of its kind conducted—positions Ambedus pusillus as the sister-taxon to all other forms, with Diadectes sanmiguelensis, Orobates pabsti, Desmatodon hesperis, Diadectes absitus, and (Diadectes sideropelicus + Diadectes tenuitectes + Diasparactus zenos) representing progressively more derived taxa in a series of nested clades. In light of these results, it is recommended herein that the species Diadectes sanmiguelensis be referred to the new genus -
Early Tetrapod Relationships Revisited
Biol. Rev. (2003), 78, pp. 251–345. f Cambridge Philosophical Society 251 DOI: 10.1017/S1464793102006103 Printed in the United Kingdom Early tetrapod relationships revisited MARCELLO RUTA1*, MICHAEL I. COATES1 and DONALD L. J. QUICKE2 1 The Department of Organismal Biology and Anatomy, The University of Chicago, 1027 East 57th Street, Chicago, IL 60637-1508, USA ([email protected]; [email protected]) 2 Department of Biology, Imperial College at Silwood Park, Ascot, Berkshire SL57PY, UK and Department of Entomology, The Natural History Museum, Cromwell Road, London SW75BD, UK ([email protected]) (Received 29 November 2001; revised 28 August 2002; accepted 2 September 2002) ABSTRACT In an attempt to investigate differences between the most widely discussed hypotheses of early tetrapod relation- ships, we assembled a new data matrix including 90 taxa coded for 319 cranial and postcranial characters. We have incorporated, where possible, original observations of numerous taxa spread throughout the major tetrapod clades. A stem-based (total-group) definition of Tetrapoda is preferred over apomorphy- and node-based (crown-group) definitions. This definition is operational, since it is based on a formal character analysis. A PAUP* search using a recently implemented version of the parsimony ratchet method yields 64 shortest trees. Differ- ences between these trees concern: (1) the internal relationships of aı¨stopods, the three selected species of which form a trichotomy; (2) the internal relationships of embolomeres, with Archeria -
Systematics and Phylogeny of Philautus Gistel, 1848 (Anura, Rhacophoridae) in the Western Ghats of India, with Descriptions of 12 New Species
Zoological Journal of the Linnean Society, 2009, 155, 374–444. With 66 figures Systematics and phylogeny of Philautus Gistel, 1848 (Anura, Rhacophoridae) in the Western Ghats of India, with descriptions of 12 new species S. D. BIJU1* and FRANKY BOSSUYT2 1Systematics Laboratory, Centre for Environmental Management of Degraded Ecosystems (CEMDE), School of Environmental Studies, University of Delhi, Delhi 110 007, India 2Biology Department, Unit of Ecology & Systematics, Free University of Brussels (VUB), Pleinlaan 2, B-1050 Brussels, Belgium Received 14 July 2005; accepted for publication 12 March 2008 A taxonomic account of the genus Philautus from the Western Ghats of India is presented. All known species of this genus, their type specimens, current taxonomic status, and geographical distribution are revised, based on museum and field studies. In addition, 12 new species are described and compared with other members of the genus, especially with the name-bearing types of Indian Philautus. Diagnoses, detailed descriptions, illustrations, data on distribution, and natural history are provided for all species, and their relationships are estimated using molecular phylogenetic analyses of mitochondrial data sets. No reliable observations have been made for two species, Philautus chalazodes (Günther, 1876) and Philautus flaviventris (Boulenger, 1882), since the original descriptions in the 19th century. © 2009 The Linnean Society of London, Zoological Journal of the Linnean Society, 2009, 155, 374–444. ADDITIONAL KEYWORDS: biodiversity – biogeography – molecular phylogenetics – taxonomy. INTRODUCTION The Western Ghats, or Sahyadri Hills, is a chain of mountains that runs parallel with the west coast of The genus Philautus Gistel, 1848 assembles a group India over 1600 km from 8°15′N to 21°00′N. -
The Carboniferous Evolution of Nova Scotia
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The Carboniferous evolution of Nova Scotia J. H. CALDER Nova Scotia Department of Natural Resources, PO Box 698, Halifax, Nova Scotia, Canada B3J 2T9 Abstract: Nova Scotia during the Carboniferous lay at the heart of palaeoequatorial Euramerica in a broadly intermontane palaeoequatorial setting, the Maritimes-West-European province; to the west rose the orographic barrier imposed by the Appalachian Mountains, and to the south and east the Mauritanide-Hercynide belt. The geological affinity of Nova Scotia to Europe, reflected in elements of the Carboniferous flora and fauna, was mirrored in the evolution of geological thought even before the epochal visits of Sir Charles Lyell. The Maritimes Basin of eastern Canada, born of the Acadian-Caledonian orogeny that witnessed the suture of Iapetus in the Devonian, and shaped thereafter by the inexorable closing of Gondwana and Laurasia, comprises a near complete stratal sequence as great as 12 km thick which spans the Middle Devonian to the Lower Permian. Across the southern Maritimes Basin, in northern Nova Scotia, deep depocentres developed en echelon adjacent to a transform platelet boundary between terranes of Avalon and Gondwanan affinity. The subsequent history of the basins can be summarized as distension and rifting attended by bimodal volcanism waning through the Dinantian, with marked transpression in the Namurian and subsequent persistence of transcurrent movement linking Variscan deformation with Mauritainide-Appalachian convergence and Alleghenian thrusting. This Mid- Carboniferous event is pivotal in the Carboniferous evolution of Nova Scotia. Rapid subsidence adjacent to transcurrent faults in the early Westphalian was succeeded by thermal sag in the later Westphalian and ultimately by basin inversion and unroofing after the early Permian as equatorial Pangaea finally assembled and subsequently rifted again in the Triassic. -
Megapleuronzange3321schu.Pdf
UNIVERSE ftJJMOlS H URBA^-CHAMPAIGN LXLOGY b i/FIELDIANA J/ Geology Published by Field Museum of Natural History Volume 33, No. 21 January 28,1977 This volume is dedicated to Dr. Rainer Zangerl Megapleuron zangerli A New Dipnoan from the Pennsylvanian, Illinois HANS-PETER SCHULTZE APL. PROFESSOR GEOL.-PALXONT. INSTITUT, UNIVERSITXT GOTTINGEN ABSTRACT Megapleuron rochei Gaudry 1881 from the lower Permian of France is redescribed. Small juvenile specimens from the Middle Pennsylvanian of Illinois are placed in the same genus as the new species M. zangerli. The genus differs from all other contem- poraneous dipnoans in the arrangement of the bones in the skull roof. INTRODUCTION Denison ( 1969, pp. 208-209) described but did not name two juve- nile dipnoans with the tooth-plates in an early stage of develop- ment. A few additional specimens of the species have since been collected. The best preserved specimen, chosen as the type of a new species, was given first to Dr. D. Baird, Princeton, who offered it to me for description during my stay at Field Museum, Chicago. After realizing that the pattern of the bones of the skull roof differs from that in Sagenodus, I found an identical pattern in the poorly pre- served type and only specimen of Megapleuron rochei Gaudry 1881. The type specimen of M. rochei will be described first for proper comparison with the specimens from the Middle Pennsylvanian of Illinois. During my stay at Field Museum, I prepared polysulfide rubber casts of all specimens. These casts and the specimens have been investigated in Field Museum and in the GeoL-PalSont. -
Physical and Environmental Drivers of Paleozoic Tetrapod Dispersal Across Pangaea
ARTICLE https://doi.org/10.1038/s41467-018-07623-x OPEN Physical and environmental drivers of Paleozoic tetrapod dispersal across Pangaea Neil Brocklehurst1,2, Emma M. Dunne3, Daniel D. Cashmore3 &Jӧrg Frӧbisch2,4 The Carboniferous and Permian were crucial intervals in the establishment of terrestrial ecosystems, which occurred alongside substantial environmental and climate changes throughout the globe, as well as the final assembly of the supercontinent of Pangaea. The fl 1234567890():,; in uence of these changes on tetrapod biogeography is highly contentious, with some authors suggesting a cosmopolitan fauna resulting from a lack of barriers, and some iden- tifying provincialism. Here we carry out a detailed historical biogeographic analysis of late Paleozoic tetrapods to study the patterns of dispersal and vicariance. A likelihood-based approach to infer ancestral areas is combined with stochastic mapping to assess rates of vicariance and dispersal. Both the late Carboniferous and the end-Guadalupian are char- acterised by a decrease in dispersal and a vicariance peak in amniotes and amphibians. The first of these shifts is attributed to orogenic activity, the second to increasing climate heterogeneity. 1 Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK. 2 Museum für Naturkunde, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Invalidenstraße 43, 10115 Berlin, Germany. 3 School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK. 4 Institut -
A Redescription of the Lungfish Eoctenodus Hills 1929, with Reassessment of Other Australian Records of the Genus Dipterns Sedgwick & Murchison 1828
Ree. West. Aust. Mus. 1987, 13 (2): 297-314 A redescription of the lungfish Eoctenodus Hills 1929, with reassessment of other Australian records of the genus Dipterns Sedgwick & Murchison 1828. J.A. Long* Abstract Eoctenodus microsoma Hills 1929 (= Dipterus microsoma Hills, 1931) from the Frasnian Blue Range Formation, near Taggerty, Victoria, is found to be a valid genus, differing from Dipterus, and other dipnoans, by the shape of the parasphenoid and toothplates. The upper jaw toothp1ates and entopterygoids, parasphenoid, c1eithrum, anoc1eithrum and scales of Eoctenodus are described. Eoctenodus may represent the earliest member of the Ctenodontidae. Dipterus cf. D. digitatus. from the Late Devonian Gneudna Formation, Western Australia (Seddon, 1969), is assigned to Chirodipterus australis Miles 1977; and Dipterus sp. from the Late Devonian of Gingham Gap, New South Wales (Hills, 1936) is thought to be con generic with a dipnoan of similar age from the Hunter Siltstone, New South Wales. This form differs from Dipterus in the shape of the parasphenoid. The genus Dipterus appears to be restricted to the Middle-Upper Devonian of Europe, North America and the USSR (Laurasia). Introduction Although Hills (1929) recognised a new dipnoan, Eoctenodus microsoma, in the Late Devonian fish remains from the Blue Range Formation, near Taggerty, he later (Hills 1931) altered the generic status of this species after a study trip to Britain in which D,M.S. Watson pointed out similarities between the Australian form and the British genus Dipterus Sedgwick and Murchison 1828. Studies of the head of Dipterus by Westoll (1949) and White (1965) showed the structure of the palate and, in particular, the shape of the parasphenoid which differs from that in the Taggerty dipnoan. -
Phylogeny of Caecilian Amphibians (Gymnophiona) Based on Complete Mitochondrial Genomes and Nuclear RAG1
MOLECULAR PHYLOGENETICS AND EVOLUTION Molecular Phylogenetics and Evolution 33 (2004) 413–427 www.elsevier.com/locate/ympev Phylogeny of caecilian amphibians (Gymnophiona) based on complete mitochondrial genomes and nuclear RAG1 Diego San Mauroa, David J. Gowerb, Oommen V. Oommenc, Mark Wilkinsonb, Rafael Zardoyaa,* a Departamento de Biodiversidad y Biologı´a Evolutiva, Museo Nacional de Ciencias Naturales, CSIC, Jose´ Gutie´rrez Abascal, 2, 28006 Madrid, Spain b Department of Zoology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK c Department of Zoology, University of Kerala, Kariavattom 695 581, Thiruvananthapuram, Kerala, India Received 15 January 2004; revised 20 May 2004 Available online 28 July 2004 Abstract We determined the complete nucleotide sequence of the mitochondrial (mt) genome of five individual caecilians (Amphibia: Gym- nophiona) representing five of the six recognized families: Rhinatrema bivittatum (Rhinatrematidae), Ichthyophis glutinosus (Ichthy- ophiidae), Uraeotyphlus cf. oxyurus (Uraeotyphlidae), Scolecomorphus vittatus (Scolecomorphidae), and Gegeneophis ramaswamii (Caeciliidae). The organization and size of these newly determined mitogenomes are similar to those previously reported for the cae- cilian Typhlonectes natans (Typhlonectidae), and for other vertebrates. Nucleotide sequences of the nuclear RAG1 gene were also determined for these six species of caecilians, and the salamander Mertensiella luschani atifi. RAG1 (both at the amino acid and nucleotide level) shows slower rates of evolution than almost all mt protein-coding genes (at the amino acid level). The new mt and nuclear sequences were compared with data for other amphibians and subjected to separate and combined phylogenetic analyses (Maximum Parsimony, Minimum Evolution, Maximum Likelihood, and Bayesian Inference). All analyses strongly support the monophyly of the three amphibian Orders. -
Bones, Molecules, and Crown- Tetrapod Origins
TTEC11 05/06/2003 11:47 AM Page 224 Chapter 11 Bones, molecules, and crown- tetrapod origins Marcello Ruta and Michael I. Coates ABSTRACT The timing of major events in the evolutionary history of early tetrapods is discussed in the light of a new cladistic analysis. The phylogenetic implications of this are com- pared with those of the most widely discussed, recent hypotheses of basal tetrapod interrelationships. Regardless of the sequence of cladogenetic events and positions of various Early Carboniferous taxa, these fossil-based analyses imply that the tetrapod crown-group had originated by the mid- to late Viséan. However, such estimates of the lissamphibian–amniote divergence fall short of the date implied by molecular studies. Uneven rates of molecular substitutions might be held responsible for the mismatch between molecular and morphological approaches, but the patchy quality of the fossil record also plays an important role. Morphology-based estimates of evolutionary chronology are highly sensitive to new fossil discoveries, the interpreta- tion and dating of such material, and the impact on tree topologies. Furthermore, the earliest and most primitive taxa are almost always known from very few fossil localities, with the result that these are likely to exert a disproportionate influence. Fossils and molecules should be treated as complementary approaches, rather than as conflicting and irreconcilable methods. Introduction Modern tetrapods have a long evolutionary history dating back to the Late Devonian. Their origins are rooted into a diverse, paraphyletic assemblage of lobe-finned bony fishes known as the ‘osteolepiforms’ (Cloutier and Ahlberg 1996; Janvier 1996; Ahlberg and Johanson 1998; Jeffery 2001; Johanson and Ahlberg 2001; Zhu and Schultze 2001).