Skeletal Development in Xenopus Laevis (Anura: Pipidae)
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Skeletal System
1 Name___________________________________ Date____________________________________ Laboratory Report Skeletal system: Axial skeleton and bony landmarks: Review each bone and landmark/s during lab. Skull- Cranial Bones: Frontal Bone supraorbital foramen frontal sinuses supraorbital margins glabella Parietal Bones sagittal suture coronal suture squamous suture lambdoid suture Temporal Bones zygomatic process mandibular fossa external auditory meatus mastoid process styloid process internal acoustic meatus carotid canal jugular foramen Occipital Bone: foramen magnum external occipital protuberance nuchal lines (superior and inferior) occipital condyle hypoglossal canal condylar canal Sphenoid: sella turcica tuberculum sellae dorsum sellae hypophyseal fossa greater wing lesser wing optic foramen superior orbital fissure pterygoid processes Foramen associated with the sphenoid: foramen ovale foramen lacerum* foramen rotundum foramen spinosum *found between sphenoid, temporal and occipital bones Ethmoid Bone: crista galli cribiform plate perpendicular plate cribiform/olfactory foramina superior nasal conchae/turbinates middle nasal conchae/turbinates 2 Skull- Facial Bones: Nasal Bones Palatine Bones Inferior Nasal chonchae/turbinates Vomer Maxillae: Intermaxillary suture Infraorbital foramen alveolar processes incisive foramen Zygomatic Bones temporal arch zygomaticofacial foramen Lacrimal Bones lacrimal fossa Mandible body rami angle condyloid process coronoid process mandibular foramen mental foramen alveolar process mandiubular condyles mandiubular notch Orbits (eye sockets) Formed by seven skull bones: 3 cranial; 4 facial: Frontal Sphenoid Ethmoid Zygomatic Maxillae Lacrimal Palatine Associated structures include: optic foramen superior orbital fissure inferior orbital fissure Bones associated with the skull Hyoid Bone: greater cornu lesser cornu body Auditory Ossicles: Malleus Incus Stapes 3 1. Label the following illustration of the skull (anterior view): 4 2. Label the following illustration of the skull (midsagittal view): 5 3. -
HOVASAURUS BOULEI, an AQUATIC EOSUCHIAN from the UPPER PERMIAN of MADAGASCAR by P.J
99 Palaeont. afr., 24 (1981) HOVASAURUS BOULEI, AN AQUATIC EOSUCHIAN FROM THE UPPER PERMIAN OF MADAGASCAR by P.J. Currie Provincial Museum ofAlberta, Edmonton, Alberta, T5N OM6, Canada ABSTRACT HovasauTUs is the most specialized of four known genera of tangasaurid eosuchians, and is the most common vertebrate recovered from the Lower Sakamena Formation (Upper Per mian, Dzulfia n Standard Stage) of Madagascar. The tail is more than double the snout-vent length, and would have been used as a powerful swimming appendage. Ribs are pachyostotic in large animals. The pectoral girdle is low, but massively developed ventrally. The front limb would have been used for swimming and for direction control when swimming. Copious amounts of pebbles were swallowed for ballast. The hind limbs would have been efficient for terrestrial locomotion at maturity. The presence of long growth series for Ho vasaurus and the more terrestrial tan~saurid ThadeosauTUs presents a unique opportunity to study differences in growth strategies in two closely related Permian genera. At birth, the limbs were relatively much shorter in Ho vasaurus, but because of differences in growth rates, the limbs of Thadeosau rus are relatively shorter at maturity. It is suggested that immature specimens of Ho vasauTUs spent most of their time in the water, whereas adults spent more time on land for mating, lay ing eggs and/or range dispersal. Specilizations in the vertebrae and carpus indicate close re lationship between Youngina and the tangasaurids, but eliminate tangasaurids from consider ation as ancestors of other aquatic eosuchians, archosaurs or sauropterygians. CONTENTS Page ABREVIATIONS . ..... ... ......... .......... ... ......... ..... ... ..... .. .... 101 INTRODUCTION . -
Laryngology and Otology
The Journal of Laryngology and Otology {Founded in 1887 by MORRELL MACKENZIE OK^NORRIS WOI.FF.NDFN) November 1978 Infratemporal fossa approach to tumours of the temporal bone and base of the skull* By U. FISCH (Zurich) IN spite of the translabyrinthine and middle cranial fossa approaches, tumours situated in the infralabyrinthine and apical regions of the pyramid and surrounding portions of the base of the skull remain a surgical chal- lenge for neurosurgeons and otolaryngologists as well. The transpalatal- transpharyngeal route proposed by Mullan et al. (1966) and the trans- cochlear approach of House and Hitselberger (1976) do not provide adequate exposure for large glomus jugulare tumours, clivus chordomas, cholesteatomas and carcinomas invading the pyramid tip and skull base. The proper management of these lesions requires a larger approach per- mitting exposure of the internal carotid artery from the carotid foramen to the cavernous sinus (Fig. 1). The infratemporal fossa exposure presented in this paper is a possible solution to this problem. The basic features of the proposed lateral approach to the skull base are: (a) the permanent anterior displacement of the facial nerve, (b) the subluxation or permanent resection of the mandibular condyle, (c) the temporary displacement of the zygomatic arch, and (d) the subtotal petrosectomy with obliteration of the middle ear cleft. Three different types of infratemporal fossa approach have developed from the experience gained in 51 patients. They will be described and illustrated with typical cases. Surgical technique The realization of the infratemporal fossa approach to the pyramid tip and base of the skull has been hampered by difficulties in handling the following structures (Fig. -
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 -
Craniofacial Morphology of Simosuchus Clarki (Crocodyliformes: Notosuchia) from the Late Cretaceous of Madagascar
Society of Vertebrate Paleontology Memoir 10 Journal of Vertebrate Paleontology Volume 30, Supplement to Number 6: 13–98, November 2010 © 2010 by the Society of Vertebrate Paleontology CRANIOFACIAL MORPHOLOGY OF SIMOSUCHUS CLARKI (CROCODYLIFORMES: NOTOSUCHIA) FROM THE LATE CRETACEOUS OF MADAGASCAR NATHAN J. KLEY,*,1 JOSEPH J. W. SERTICH,1 ALAN H. TURNER,1 DAVID W. KRAUSE,1 PATRICK M. O’CONNOR,2 and JUSTIN A. GEORGI3 1Department of Anatomical Sciences, Stony Brook University, Stony Brook, New York, 11794-8081, U.S.A., [email protected]; [email protected]; [email protected]; [email protected]; 2Department of Biomedical Sciences, Ohio University College of Osteopathic Medicine, Athens, Ohio 45701, U.S.A., [email protected]; 3Department of Anatomy, Arizona College of Osteopathic Medicine, Midwestern University, Glendale, Arizona 85308, U.S.A., [email protected] ABSTRACT—Simosuchus clarki is a small, pug-nosed notosuchian crocodyliform from the Late Cretaceous of Madagascar. Originally described on the basis of a single specimen including a remarkably complete and well-preserved skull and lower jaw, S. clarki is now known from five additional specimens that preserve portions of the craniofacial skeleton. Collectively, these six specimens represent all elements of the head skeleton except the stapedes, thus making the craniofacial skeleton of S. clarki one of the best and most completely preserved among all known basal mesoeucrocodylians. In this report, we provide a detailed description of the entire head skeleton of S. clarki, including a portion of the hyobranchial apparatus. The two most complete and well-preserved specimens differ substantially in several size and shape variables (e.g., projections, angulations, and areas of ornamentation), suggestive of sexual dimorphism. -
Records from the Aalenian–Bajocian of Patagonia (Argentina): an Overview
Geol. Mag.: page 1 of 11. c Cambridge University Press 2013 1 doi:10.1017/S0016756813000058 Ophthalmosaurian (Ichthyosauria) records from the Aalenian–Bajocian of Patagonia (Argentina): an overview ∗ MARTA S. FERNÁNDEZ † & MARIANELLA TALEVI‡ ∗ División Palaeontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina. CONICET ‡Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, 8332 General Roca, Río Negro, Argentina. CONICET (Received 12 September 2012; accepted 11 January 2013) Abstract – The oldest ophthalmosaurian records worldwide have been recovered from the Aalenian– Bajocian boundary of the Neuquén Basin in Central-West Argentina (Mendoza and Neuquén provinces). Although scarce, they document a poorly known period in the evolutionary history of parvipelvian ichthyosaurs. In this contribution we present updated information on these fossils, including a phylogenetic analysis, and a redescription of ‘Stenopterygius grandis’ Cabrera, 1939. Patagonian ichthyosaur occurrences indicate that during the Bajocian the Neuquén Basin palaeogulf, on the southern margins of the Palaeopacific Ocean, was inhabited by at least three morphologically discrete taxa: the slender Stenopterygius cayi, robust ophthalmosaurian Mollesaurus periallus and another indeterminate ichthyosaurian. Rib bone tissue structure indicates that rib cages of Bajocian ichthyosaurs included forms with dense rib microstructure (Mollesaurus) and forms with an ‘osteoporotic-like’ pattern (Stenopterygius cayi). Keywords: Mollesaurus,‘Stenopterygius grandis’, Middle Jurassic, Neuquén Basin, Argentina. 1. Introduction all Callovian and post-Callovian ichthyosaurs, two different Early Jurassic taxa have been proposed as Ichthyosaurs were one of the main predators in the ophthalmosaurian sister taxa: Stenopterygius (Maisch oceans all over the world during most of the Mesozoic & Matzke, 2000; Sander, 2000; Druckenmiller & (Massare, 1987). -
A Review of Neusibatrachus Wilferti, an Early Cretaceous Frog from the Montsec Range, Northeastern Spain
A review of Neusibatrachus wilferti, an Early Cretaceous frog from the Montsec Range, northeastern Spain ANA M. BÁEZ and BORJA SANCHIZ Báez, A.M. and Sanchiz, B. 2007. A review of Neusibatrachus wilferti, an Early Cretaceous frog from the Montsec Range, northeastern Spain. Acta Palaeontologica Polonica 52 (3): 477–487. Neusibatrachus wilferti is an anuran from the late Berriasian–early Valanginian fossiliferous lacustrine limestones that are exposed in the eastern part of the Montsec Range, province of Lleida, Spain. It was originally described by Seiffert in 1972 and its phylogenetic position has since been discussed. Neusibatrachus has been considered an undeterminable fos− sil, an abnormal individual, or a primitive palaeobatrachid. Here we redescribe the only available specimen, and clarify features, such as absence of palatines, nine presacrals, and procoelous vertebral centra, that have been the subject of previ− ous debates. We consider the specimen to be a postmetamorphic individual and make developmental interpretations of some of its characters. In particular, we provide evidence of a living anuran (Rana iberica) that resembles Neusibatrachus in the development of intervertebral articulations. Neusibatrachus is considered a valid genus, which differs from other anurans, except for the pipoids, in the joint presence of an azygous frontoparietal and a parasphenoid lacking the subotic alae, although it differs from the pipoids in having nine presacral vertebrae. Morphological evidence indicates that Neusi− batrachus is related to Xenoanura, the pipoid branch in the living Amphibia Tree of Life based on molecular data. More− over, it might be a member of the pipoid clade proper, which presently includes the Pipidae, Rhinophrynidae, and several fossil taxa, including the Palaeobatrachidae, although the evidence is not conclusive. -
Lab Week 7 Part 1 Radius and Ulna
11/7/2018 Lab Week 7 Part 1 Radius and Ulna Part 1 Activities 1. Observe bones and structures from list 2. Bones of the Forearm worksheet in packet 3. Bones of the Pectoral Girdle and Upper Limbs worksheet in packet Part 2 Femur, Tibia, & Fibula 1 11/7/2018 Part 2 Activities 1. Observe bones and structures from list 2. Bones of the Lower Limbs worksheet in packet 3. Bones of the Pelvic Girdle and Lower Limbs worksheet in packet Functions of the Skull • Support • Movement Part 3 • Protection Skull Notes may be found in your packet: SS 27-28 The Skull The Skull 22 bones, 2 groups 2. Facial bones (14 bones) 1. Cranial bones (8) • Framework of face • Enclose the brain in the cranial cavity • Cavities for special sense organs of sight, taste, and • Provide sites of attachment for head and neck muscles smell • • Provide support Openings for air and food passage • Sites of attachment for teeth and muscles of facial expression 2 11/7/2018 Sutures Bones of cranium (cranial vault) • Immovable joints Coronal suture – Become more complex with age Squamous • Fontanelles suture – Soft regions of connective tissue holding bones together at birth • Permits – Brain growth Lambdoid Facial suture bones – Entry into birth canal Occipitomastoid – Normally replaced by bone by about 1 year of age suture Cranial and facial divisions of the skull Foramina Sinuses • Allow passage of blood vessels and nerves • Cavities lined with mucous membranes & ciliated epithelium – • About 85 named openings (foramina, canals, Frontal sinus – Sphenoidal sinus fissures) – Maxillary -
A Possible 150 Million Years Old Cirripede Crustacean Nauplius and the Phenomenon of Giant Larvae
Contributions to Zoology, 86 (3) 213-227 (2017) A possible 150 million years old cirripede crustacean nauplius and the phenomenon of giant larvae Christina Nagler1, 4, Jens T. Høeg2, Carolin Haug1, 3, Joachim T. Haug1, 3 1 Department of Biology, Ludwig-Maximilians-Universität München, Großhaderner Straße 2, 82152 Planegg- Martinsried, Germany 2 Department of Biology, University of Copenhagen, Universitetsparken 15, 2100 Copenhagen, Denmark 3 GeoBio-Center, Ludwig-Maximilians-Universität München, Richard-Wagner-Straße 10, 80333 Munich, Germany 4 E-mail: [email protected] Key words: nauplius, metamorphosis, palaeo-evo-devo, Cirripedia, Solnhofen lithographic limestones Abstract The possible function of giant larvae ................................ 222 Interpretation of the present case ....................................... 223 The larval phase of metazoans can be interpreted as a discrete Acknowledgements ....................................................................... 223 post-embryonic period. Larvae have been usually considered to References ...................................................................................... 223 be small, yet some metazoans possess unusually large larvae, or giant larvae. Here, we report a possible case of such a giant larva from the Upper Jurassic Solnhofen Lithographic limestones (150 Introduction million years old, southern Germany), most likely representing an immature cirripede crustacean (barnacles and their relatives). The single specimen was documented with up-to-date -
Paleontological Discoveries in the Chorrillo Formation (Upper Campanian-Lower Maastrichtian, Upper Cretaceous), Santa Cruz Province, Patagonia, Argentina
Rev. Mus. Argentino Cienc. Nat., n.s. 21(2): 217-293, 2019 ISSN 1514-5158 (impresa) ISSN 1853-0400 (en línea) Paleontological discoveries in the Chorrillo Formation (upper Campanian-lower Maastrichtian, Upper Cretaceous), Santa Cruz Province, Patagonia, Argentina Fernando. E. NOVAS1,2, Federico. L. AGNOLIN1,2,3, Sebastián ROZADILLA1,2, Alexis M. ARANCIAGA-ROLANDO1,2, Federico BRISSON-EGLI1,2, Matias J. MOTTA1,2, Mauricio CERRONI1,2, Martín D. EZCURRA2,5, Agustín G. MARTINELLI2,5, Julia S. D´ANGELO1,2, Gerardo ALVAREZ-HERRERA1, Adriel R. GENTIL1,2, Sergio BOGAN3, Nicolás R. CHIMENTO1,2, Jordi A. GARCÍA-MARSÀ1,2, Gastón LO COCO1,2, Sergio E. MIQUEL2,4, Fátima F. BRITO4, Ezequiel I. VERA2,6, 7, Valeria S. PEREZ LOINAZE2,6 , Mariela S. FERNÁNDEZ8 & Leonardo SALGADO2,9 1 Laboratorio de Anatomía Comparada y Evolución de los Vertebrados. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina - fernovas@yahoo. com.ar. 2 Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina. 3 Fundación de Historia Natural “Felix de Azara”, Universidad Maimonides, Hidalgo 775, C1405BDB Buenos Aires, Argentina. 4 Laboratorio de Malacología terrestre. División Invertebrados Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina. 5 Sección Paleontología de Vertebrados. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina. 6 División Paleobotánica. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina. 7 Área de Paleontología. Departamento de Geología, Universidad de Buenos Aires, Pabellón 2, Ciudad Universitaria (C1428EGA) Buenos Aires, Argentina. 8 Instituto de Investigaciones en Biodiversidad y Medioambiente (CONICET-INIBIOMA), Quintral 1250, 8400 San Carlos de Bariloche, Río Negro, Argentina. -
Anatomy and Relationships of the Triassic Temnospondyl Sclerothorax
Anatomy and relationships of the Triassic temnospondyl Sclerothorax RAINER R. SCHOCH, MICHAEL FASTNACHT, JÜRGEN FICHTER, and THOMAS KELLER Schoch, R.R., Fastnacht, M., Fichter, J., and Keller, T. 2007. Anatomy and relationships of the Triassic temnospondyl Sclerothorax. Acta Palaeontologica Polonica 52 (1): 117–136. Recently, new material of the peculiar tetrapod Sclerothorax hypselonotus from the Middle Buntsandstein (Olenekian) of north−central Germany has emerged that reveals the anatomy of the skull and anterior postcranial skeleton in detail. Despite differences in preservation, all previous plus the new finds of Sclerothorax are identified as belonging to the same taxon. Sclerothorax is characterized by various autapomorphies (subquadrangular skull being widest in snout region, ex− treme height of thoracal neural spines in mid−trunk region, rhomboidal interclavicle longer than skull). Despite its pecu− liar skull roof, the palate and mandible are consistent with those of capitosauroid stereospondyls in the presence of large muscular pockets on the basal plate, a flattened edentulous parasphenoid, a long basicranial suture, a large hamate process in the mandible, and a falciform crest in the occipital part of the cheek. In order to elucidate the phylogenetic position of Sclerothorax, we performed a cladistic analysis of 18 taxa and 70 characters from all parts of the skeleton. According to our results, Sclerothorax is nested well within the higher stereospondyls, forming the sister taxon of capitosauroids. Palaeobiologically, Sclerothorax is interesting for its several characters believed to correlate with a terrestrial life, although this is contrasted by the possession of well−established lateral line sulci. Key words: Sclerothorax, Temnospondyli, Stereospondyli, Buntsandstein, Triassic, Germany. -
From the Early Cretaceous Crato Formation
Journal of South American Earth Sciences 92 (2019) 222–233 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames A new genus of pipimorph frog (Anura) from the Early Cretaceous Crato T Formation (Aptian) and the evolution of South American tongueless frogs ∗ ∗∗ Ismar Souza Carvalhoa, , Federico Agnolinb,c, , Mauro A. Aranciaga Rolandob, Fernando E. Novasb, José Xavier-Netod, Francisco Idalécio Freitase, José Artur Ferreira Gomes Andradef a Universidade Federal do Rio de Janeiro, Departamento de Geologia, CCMN/IGEO 21.949-900 Cidade Universitária - Ilha do Fundão, Rio de Janeiro, Brazil b Museo Argentino de Ciencias Naturales ‘Bernardino Rivadavia’, Consejo Nacional de Investigaciones Científicas y Técnicas – CONICET, Buenos Aires, Argentina c Fundación de Historia Natural ‘Félix de Azara’, Universidad Maimónides, Buenos Aires, Argentina d Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq), Brasília (DF), Brazil e Geopark Araripe, Rua Carolino Sucupira s/n, Pimenta, 105 Centro, 63.100-490 Ceará, Brazil f Departamento Nacional da Produção Mineral, Ceará, Praça da Sé, 105 Centro, 63.100-440 Ceará, Brazil ARTICLE INFO ABSTRACT Keywords: Pipimorpha is a clade of tongueless anurans with a wide fossil record. Furthermore, the oldest South American Crato Formation fossils come from the Late Cretaceous (Cenomanian) of Patagonia, Argentina. The aim of the present con- Lower Cretaceous tribution is to describe a new genus and species of Pipimorpha from the Crato Formation (Aptian, Early Pipimorpha Cretaceous), Araripe Basin, Brazil. The new specimen consists of a nearly complete skeleton that shows several Brazil anatomical similarities with other fossils from South America.