Covariation of the Endocranium and Splanchnocranium During Great Ape Ontogeny
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A New Osteolepidid Fish From
Rea. West. Aust. MU8. 1985, 12(3): 361-377 ANew Osteolepidid Fish from the Upper Devonian Gogo Formation, Western Australia J.A. Long* Abstract A new osteolepidid crossopterygian, Gogonasus andrewsi gen. et sp. nov., is des cribed from a single fronto-ethmoidal shield and associated ethmosphenoid, from the Late Devonian (Frasnian) Gogo Formation, Western Australia. Gogonasus is is distinguished from other osteolepids by the shape and proportions of the fronto ethmoidal shield, absence of palatal fenestrae, well developed basipterygoid pro cesses and moderately broad parasphenoid. The family Osteolepididae is found to be paraphyletic, with Gogonasus being regarded as a plesiomorphic osteolepidid at a similar level of organisation to Thursius. Introduction Much has been published on the well-preserved Late Devonian fish fauna from the Gogo Formation, Western Australia, although to date all the papers describing fish have been on placoderms (Miles 1971; Miles and Dennis 1979; Dennis and Miles 1979-1983; Young 1984), palaeoniscoids (Gardiner 1973, 1984; Gardiner and Bartram 1977) or dipnoans (Miles 1977; Campbell and Barwick 1982a, 1982b, 1983, 1984a). This paper describes the only osteolepiform from the fauna (Gardiner and Miles 1975), a small snout with associated braincase, ANU 21885, housed in the Geology Department, Australian National University. The specimen, collected by the Australian National University on the 1967 Gogo Expedition, was prepared by Dr S.M. Andrews (Royal Scottish Museum) and later returned to the ANU. Onychodus is the only other crossopterygian in the fauna. In its proportions and palatal structure the new specimen provides some additional new points of the anatomy of osteolepiforms. Few Devonian crossopte rygians are known from Australia, and so the specimen is significant in having resemblances to typical Northern Hemisphere species. -
Morfofunctional Structure of the Skull
N.L. Svintsytska V.H. Hryn Morfofunctional structure of the skull Study guide Poltava 2016 Ministry of Public Health of Ukraine Public Institution «Central Methodological Office for Higher Medical Education of MPH of Ukraine» Higher State Educational Establishment of Ukraine «Ukranian Medical Stomatological Academy» N.L. Svintsytska, V.H. Hryn Morfofunctional structure of the skull Study guide Poltava 2016 2 LBC 28.706 UDC 611.714/716 S 24 «Recommended by the Ministry of Health of Ukraine as textbook for English- speaking students of higher educational institutions of the MPH of Ukraine» (minutes of the meeting of the Commission for the organization of training and methodical literature for the persons enrolled in higher medical (pharmaceutical) educational establishments of postgraduate education MPH of Ukraine, from 02.06.2016 №2). Letter of the MPH of Ukraine of 11.07.2016 № 08.01-30/17321 Composed by: N.L. Svintsytska, Associate Professor at the Department of Human Anatomy of Higher State Educational Establishment of Ukraine «Ukrainian Medical Stomatological Academy», PhD in Medicine, Associate Professor V.H. Hryn, Associate Professor at the Department of Human Anatomy of Higher State Educational Establishment of Ukraine «Ukrainian Medical Stomatological Academy», PhD in Medicine, Associate Professor This textbook is intended for undergraduate, postgraduate students and continuing education of health care professionals in a variety of clinical disciplines (medicine, pediatrics, dentistry) as it includes the basic concepts of human anatomy of the skull in adults and newborns. Rewiewed by: O.M. Slobodian, Head of the Department of Anatomy, Topographic Anatomy and Operative Surgery of Higher State Educational Establishment of Ukraine «Bukovinian State Medical University», Doctor of Medical Sciences, Professor M.V. -
ASPECTS of the CRANIAL MORPHOLOGY of the THEROCEPHALIAN Moschorhlnus (REPTILIA: THERAPSIDA)
ASPECTS OF THE CRANIAL MORPHOLOGY OF THE THEROCEPHALIAN Moschorhlnus (REPTILIA: THERAPSIDA) Jacobus Francois Durand A thesis submitted to the Faculty of Science, University of the Witwaters.-and, Johannesburg, in fulfilment of the requirements for the degree of Doctor of Philosophy. Johannesburg 1989 ERRATA p ill, line 11 For "alhough" read "although". p 11 "The dorsal part of the pterygoid contacts the foot of the epiptexygoid doreally" should read "The dorsal part of the pterygoid contacts the ventral surface of the foot of the epipterygoid". VP 6 , 7 "within the jugal arch" should read "medial to the jugal arch". PP 6 , 25, 26, 52, "temporal fossa" should read "temporal fenestra". 129 p 82 "ventro-lateral flange of the parietal" should read "latero-ventral flange of the parietal". pp 9 , 62, 65, 65, "processus aecendene of the epipterygoid" should read 105, 150, 151, 172 "££0088808 Mcendena". pp 125, 124, 128, "Jollie (1962)" should read "Jollie (197?)". 150, 151 p p 103, 161 "Hopsoa" should read "Hopcsa". Add to References BOOMSTRA, L.D. 19)8. On a Soutn African mamal-like reptile Baurla oynops. Palaeobioloairq 6 t 164-183. OVER, R. 1876. Description of the Reptiliia. of South Africa in the collection of the British Museum". 1-2 London $ British Museum. ii ABSTRACT A sound understanding of the morphology of the Therocephal1 a Is essential to our understanding of the reptile-mammal transition. In this thesis the anatony of the posterior half o the Moschorhinus skull Is described in detail. This study revealed many aspects overlooked or misinterpreted by othtr authors. Two Moschorhinus skulls were studied externally. -
Late Cretaceous) of Morocco : Palaeobiological and Behavioral Implications Remi Allemand
Endocranial microtomographic study of marine reptiles (Plesiosauria and Mosasauroidea) from the Turonian (Late Cretaceous) of Morocco : palaeobiological and behavioral implications Remi Allemand To cite this version: Remi Allemand. Endocranial microtomographic study of marine reptiles (Plesiosauria and Mosasauroidea) from the Turonian (Late Cretaceous) of Morocco : palaeobiological and behavioral implications. Paleontology. Museum national d’histoire naturelle - MNHN PARIS, 2017. English. NNT : 2017MNHN0015. tel-02375321 HAL Id: tel-02375321 https://tel.archives-ouvertes.fr/tel-02375321 Submitted on 22 Nov 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. MUSEUM NATIONAL D’HISTOIRE NATURELLE Ecole Doctorale Sciences de la Nature et de l’Homme – ED 227 Année 2017 N° attribué par la bibliothèque |_|_|_|_|_|_|_|_|_|_|_|_| THESE Pour obtenir le grade de DOCTEUR DU MUSEUM NATIONAL D’HISTOIRE NATURELLE Spécialité : Paléontologie Présentée et soutenue publiquement par Rémi ALLEMAND Le 21 novembre 2017 Etude microtomographique de l’endocrâne de reptiles marins (Plesiosauria et Mosasauroidea) du Turonien (Crétacé supérieur) du Maroc : implications paléobiologiques et comportementales Sous la direction de : Mme BARDET Nathalie, Directrice de Recherche CNRS et les co-directions de : Mme VINCENT Peggy, Chargée de Recherche CNRS et Mme HOUSSAYE Alexandra, Chargée de Recherche CNRS Composition du jury : M. -
Redalyc.Ontogeny of the Cranial Bones of the Giant Amazon River
Acta Scientiarum. Biological Sciences ISSN: 1679-9283 [email protected] Universidade Estadual de Maringá Brasil Gonçalves Vieira, Lucélia; Quagliatto Santos, André Luiz; Campos Lima, Fabiano Ontogeny of the cranial bones of the giant amazon river turtle Podocnemis expansa Schweigger, 1812 (Testudines, Podocnemididae) Acta Scientiarum. Biological Sciences, vol. 32, núm. 2, 2010, pp. 181-188 Universidade Estadual de Maringá .png, Brasil Available in: http://www.redalyc.org/articulo.oa?id=187114387012 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative DOI: 10.4025/actascibiolsci.v32i2.5777 Ontogeny of the cranial bones of the giant amazon river turtle Podocnemis expansa Schweigger, 1812 (Testudines, Podocnemididae) Lucélia Gonçalves Vieira*, André Luiz Quagliatto Santos and Fabiano Campos Lima Laboratório de Pesquisas em Animais Silvestres, Universidade Federal de Uberlândia, Av. João Naves De Avila, 2121, 38408-100, Uberlandia, Minas Gerais, Brazil. *Author for correspondence. E-mail: [email protected] ABSTRACT. In order to determine the normal stages of formation in the sequence of ossification of the cranium of Podocnemis expansa in its various stages of development, embryos were collected starting on the 18th day of natural incubation and were subjected to bone diaphanization and staining. In the neurocranium, the basisphenoid and basioccipital bones present ossification centers in stage 19, the supraoccipital and opisthotic in stage 20, the exoccipital in stage 21, and lastly the prooptic in stage 24. Dermatocranium: the squamosal, pterygoid and maxilla are the first elements to begin the ossification process, which occurs in stage 16. -
New Evidence on Brain-Endocranial Cavity Relationships in Ornithischian
New evidence on brain−endocranial cavity relationships in ornithischian dinosaurs DAVID C. EVANS Evans, D.C. 2005. New evidence on brain−endocranial cavity relationships in ornithischian dinosaurs. Acta Palaeonto− logica Polonica 50 (3): 617–622. Discussions of brain morphology and relative brain size in nonavian dinosaurs have been complicated by uncertainty in the extent to which the brain filled the endocranial cavity. Recently reported vascular imprints (valleculae) on the endocranial sur− faces of the braincase suggest that nonavian maniraptoriform theropods had brains that tightly fit the endocranium. Similar impressions of the intracranial vascular system are reported here in two ornithischian clades, Hadrosauridae and Pachy− cephalosauridae. These structures are more widespread in dinosaurs than previously thought, and suggest that the brain closely fit the endocranium in some regions of the forebrain through hindbrain in several distantly related dinosaur groups. Key words: Dinosauria, Hadrosauridae, Pachycephalosauridae, endocranial cavity, brain, Cretaceous. David C. Evans [[email protected]], University of Toronto, 3359 Mississauga Rd., Mississauga, ON, Canada, L5L 1C6. Introduction that complex endocranial vascular impressions also occur in hadrosaurid and pachycephalosaurid ornithischians, and that Traditionally nonavian dinosaurs have been regarded as “rep− the brain may have been closely associated with the endo− tilian” in that their brains were thought to have filled a rela− cranium in some regions of the forebrain and post−cerebrum in tively small portion of the endocranial cavity in contrast with these groups. the conditions in mammals and birds (Jerison 1969, 1973; Institutional abbreviations (all in Canada).—CMN, Cana− Hopson 1977, 1979; Rogers 1999; Larsson et al. 2000; Lars− dian Museum of Nature, Ottawa; ROM, Royal Ontario Mu− son 2001). -
Reptilia, Diapsida): New Insights from High-Resolution Ct Scanning of the Holotype
Palaeontologia Electronica http://palaeo-electronica.org THE BRAINCASE OF YOUNGINA CAPENSIS (REPTILIA, DIAPSIDA): NEW INSIGHTS FROM HIGH-RESOLUTION CT SCANNING OF THE HOLOTYPE Nicholas M. Gardner, Casey M. Holliday, and F. Robin O’Keefe Nicholas M. Gardner. Department of Biological Sciences, Marshall University, Huntington, West Virginia. [email protected] Casey M. Holliday. Department of Pathology & Anatomical Sciences, University of Missouri, Columbia, Missouri. [email protected] F. Robin O’Keefe. Department of Biological Sciences, Marshall University, Huntington, West Virginia. [email protected] ABSTRACT Detailed descriptions of braincase anatomy in early diapsid reptiles have been historically rare given the difficulty of accessing this deep portion of the skull, because of poor preservation of the fossils or the inability to remove the surrounding skull roof. Previous descriptions of the braincase of Youngina capensis, a derived stem-diapsid reptile from the Late Permian (250 MYA) of South Africa, have relied on only partially preserved fossils. High resolution X-ray computed tomography (HRXCT) scanning, a new advance in biomedical sciences, has allowed us to examine the reasonably com- plete braincase of the holotype specimen of Youngina capensis for the first time by dig- itally peering through the sandstone matrix that filled the skull postmortem. We present the first detailed 3D visualizations of the braincase and the vestibular system in a Permian diapsid reptile. This new anatomical description is of great comparative and phylogenetic relevance to the study of the structure, function and evolution of the reptil- ian head. KEY WORDS: Youngina capensis, diapsid reptiles, CT scanning, 3D models PE ERRATUM In the paper Gardner et al. -
The Endocranium of the Theropod Dinosaur Ceratosaurus Studied with Computed Tomography
The endocranium of the theropod dinosaur Ceratosaurus studied with computed tomography R. KENT SANDERS and DAVID K. SMITH Sanders, R.K. and Smith, D.K. 2005. The endocranium of the theropod dinosaur Ceratosaurus studied with computed to− mography. Acta Palaeontologica Polonica 50 (3): 601–616. A well preserved specimen of the theropod Ceratosaurus from the Upper Jurassic Morrison Formation of western Colorado was recently described and given the name C. magnicornis. The systematics of the genus is outside the scope of the present study but, as a generally accepted basal tetanuran, the braincase was CT scanned to provide a description of the endocranium, inner ear, pneumatic, and venous sinus systems in a primitive member of this clade. Five major subregions of the theropod endocranium are distinguished for the purpose of simplifying cranial computed tomographic interpretation and to provide a systematic means of comparison to other endocrania. The skull morphology of Ceratosaurus influences the overall braincase morphology and the number and distribution of the major foramina. The low pontine angle and relatively unflexed braincase is considered a more primitive character. The orientation of the horizontal semicircular canal confirms a rather horizontal and unerect posture of the head and neck. As in birds, the narrower skull morphology of Ceratosaurus is as− sociated with fewer cranial nerve foramina. Additionally, the maxillary dominated dentigerous upper jaw of Ceratosaurus is felt to share with the alligator a large rostrally directed maxillary division of the trigeminal nerve and a small ophthalmic branch. The upper bill of birds, being dominated by the premaxillary and lacking teeth, is innervated predominantly by the ophthalmic division of the trigeminal nerve. -
Axial Skeleton 214 7.7 Development of the Axial Skeleton 214
SKELETAL SYSTEM OUTLINE 7.1 Skull 175 7.1a Views of the Skull and Landmark Features 176 7.1b Sutures 183 7.1c Bones of the Cranium 185 7 7.1d Bones of the Face 194 7.1e Nasal Complex 198 7.1f Paranasal Sinuses 199 7.1g Orbital Complex 200 Axial 7.1h Bones Associated with the Skull 201 7.2 Sex Differences in the Skull 201 7.3 Aging of the Skull 201 Skeleton 7.4 Vertebral Column 204 7.4a Divisions of the Vertebral Column 204 7.4b Spinal Curvatures 205 7.4c Vertebral Anatomy 206 7.5 Thoracic Cage 212 7.5a Sternum 213 7.5b Ribs 213 7.6 Aging of the Axial Skeleton 214 7.7 Development of the Axial Skeleton 214 MODULE 5: SKELETAL SYSTEM mck78097_ch07_173-219.indd 173 2/14/11 4:58 PM 174 Chapter Seven Axial Skeleton he bones of the skeleton form an internal framework to support The skeletal system is divided into two parts: the axial skele- T soft tissues, protect vital organs, bear the body’s weight, and ton and the appendicular skeleton. The axial skeleton is composed help us move. Without a bony skeleton, we would collapse into a of the bones along the central axis of the body, which we com- formless mass. Typically, there are 206 bones in an adult skeleton, monly divide into three regions—the skull, the vertebral column, although this number varies in some individuals. A larger number of and the thoracic cage (figure 7.1). The appendicular skeleton bones appear to be present at birth, but the total number decreases consists of the bones of the appendages (upper and lower limbs), with growth and maturity as some separate bones fuse. -
Skull – Ii Dermatocranium
BIOLOGY 524 ADVANCED VERTEBRTE MORPHOLOGY -OSTEOLOGY- SKULL – II DERMATOCRANIUM S. S. SUMIDA INTRODUCTION RECALL: SPLANCHNOCRANIUM – The splanchnocranium (sometimes called the viscerocranium) is the phylogenetically most ancient part of the skull. It arose even before vertebrates themselves to support the pharyngeal gill slits of protochordates. Within the vertebrates, it supports gill structures or their evolutionary derivatives. The cartilagenous or bony components are derived from neural crest, and form endochondrally. Components of the upper and lower jaw are derived from this. CHONDROCRANIUM – The chondrocranium is a cradle that supports the underside of the brain itself. Its components form endochondrally, and can be derived from either mesoderm or neural crest. The chondrocranium is derived from multiple individual structures that fuse to become this cradle. Not all components ossify, with some remaining as cartilage. DERMATOCRANIUM – The dermatocranium is slightly later in development and makes up the outer casing of the skull. It protects the brain above, and protects the entire braincase from below as the plate. Embryology of the Dermatocranium All components of the vertebrate dermatocranium form intramembranously from neural crest cells. In fact, it is unfortunate, as this type of formation used to be known as “dermal bone formation” (because of the proximity of the ne to the skin. However, even though we no longer use the term dermal formation, we still use the term dermatocranium. Notably, whereas the entire dermatocranium is derived from neural crest forms intramembranously, it is not the only part of the skeleton derived from neural crest (also the splanchnocranium, which forms endochondrally), and it is not the only part of the skeleton that forms intramembranously (also significant parts of the pectoral girdle, which is derived from mesoderm). -
Jaw Suspension
JAW SUSPENSION Jaw suspension means attachment of the lower jaw with the upper jaw or the skull for efficient biting and chewing. There are different ways in which these attachments are attained depending upon the modifications in visceral arches in vertebrates. AMPHISTYLIC In primitive elasmobranchs there is no modification of visceral arches and they are made of cartilage. Pterygoqadrate makes the upper jaw and meckel’s cartilage makes lower jaw and they are highly flexible. Hyoid arch is also unchanged. Lower jaw is attached to both pterygoqadrate and hyoid arch and hence it is called amphistylic. AUTODIASTYLIC Upper jaw is attached with the skull and lower jaw is directly attached to the upper jaw. The second arch is a branchial arch and does not take part in jaw suspension. HYOSTYLIC In modern sharks, lower jaw is attached to pterygoquadrate which is in turn attached to hyomandibular cartilage of the 2nd arch. It is the hyoid arch which braces the jaw by ligament attachment and hence it is called hyostylic. HYOSTYLIC (=METHYSTYLIC) In bony fishes pterygoquadrate is broken into epipterygoid, metapterygoid and quadrate, which become part of the skull. Meckel’s cartilage is modified as articular bone of the lower jaw, through which the lower jaw articulates with quadrate and then with symplectic bone of the hyoid arch to the skull. This is a modified hyostylic jaw suspension that is more advanced. AUTOSTYLIC (=AUTOSYSTYLIC) Pterygoquadrate is modified to form epipterygoid and quadrate, the latter braces the lower jaw with the skull. Hyomandibular of the second arch transforms into columella bone of the middle ear cavity and hence not available for jaw suspension. -
On the Labyrinthodonts of the USSR. II. Permian Labyrinthodonts of the Former Government of Viatka by I
On the labyrinthodonts of the USSR. II. Permian labyrinthodonts of the former Government of Viatka by I. A. Efremov [= Efremoff ]* 1. A new description of the labyrinthodont Platyops stuckenbergi Trautschold from the Late Permian deposits of the Kityak River, a confluent of the the Viatka River. The skull of Platyops stuckenbergi, which was described by Trautschold (16)† in the seventies of the last century, is the only preserved type of all the labyrinthodonts that have been described in Russia up to the eighties. The description of Trautschold, who has not prepared his object, does not answer the demands of present-day paleontology, and as a result it was necessary to re-work his material. Thanks to the kindness of the late Prof. Noinsky, Director of the Geological Division of Kazan University, where Trautschold’s material is kept, I have succeed in obtaining the Platyops cranium for the purpose of preparation and examination. I had at my disposal together with the type—an incomplete skull that was pictured by Trautschold under No. 1 in plate I (see Fig. 20)—several fragments pictured in this place under Nos. 2, 3, 4, 5, 6, 7, 14, and 16. The locality of all the remains is known with sufficient certainty. The entire material was collected by Prof. Stuckenberg in an abandoned copper mine near the village of Akbatyrova on the Kityak River (the right confluent of the Viatka River), in the Malmysh district of the former Viatka Government. The layer containing the bones represents a lens of compact cuprous marl that is somewhat bituminous and undoubtedly belongs to a continental facies.