Andrias Davidianus (Amphibia:Urodela)
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Noise Annoys Not Mouriamorphs Filled a Niche THESE Days, Our Ears Are Too Sensitive for That Made Their Preserva Their Own Good
NEWS AND VIEWS DAEDALUS--------~ An orthodox interpret ation might be that sey Noise annoys not mouriamorphs filled a niche THESE days, our ears are too sensitive for that made their preserva their own good. Primitive tribes, with only tion unlikely until the begin natural sounds to listen to, retain their ning of the acute hearing into late age. Modern Permian, at which point civilization, however, batters our ears into taphonomic circumstances early deafness. They have a natural changed and they were protection mechanism, but it badly needs suddenly abundantly pre upgrading. served, both in Euramerica It uses two tiny muscles, the tensor and in those plates newly tympani and the stapedius, which reduce accreting to Euramerica in the ear's sensitivity by stiffening the the Lower Permian. How joints of its transmission bones. They are ever, with tetrapods also tensed automatically by loud noise. They FIG. 2 Discosauriscus, a small, probably larval seymouri diversifying in East Gond worked well in prehistoric times, when amorph from the Lower Permian of the Czech Republic. Cal wana in the Early Carbonif most noises built up slowly. But they ibrated scale bar, 5 cm. (Science Museum of Minnesota; erous, it is equally possible photograph by A. M.) cannot react fast enough to modern that seymouriamorphs first bangs and crashes, and sustained uproar apparently centred on equatorial appeared there and, instead of spreading fatigues them. Daedalus wants to warn Euramerica, was largely a process of westwards, spread or hopped north across them of noise in advance. ecological niche-hopping within a s ingle the chain of North China, Tarim and A sound wave launched upwards into continent. -
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 -
3D Maps of Mineral Composition and Hydroxyapatite Orientation in Fossil Bone Samples Obtained by X-Ray Diffraction Computed Tomo
www.nature.com/scientificreports OPEN 3D Maps of Mineral Composition and Hydroxyapatite Orientation in Fossil Bone Samples Obtained Received: 25 January 2018 Accepted: 20 June 2018 by X-ray Difraction Computed Published: xx xx xxxx Tomography Fredrik K. Mürer1, Sophie Sanchez2,3,4, Michelle Álvarez-Murga3, Marco Di Michiel3, Franz Pfeifer5,6, Martin Bech 7 & Dag W. Breiby1,8 Whether hydroxyapatite (HA) orientation in fossilised bone samples can be non-destructively retrieved and used to determine the arrangement of the bone matrix and the location of muscle attachments (entheses), is a question of high relevance to palaeontology, as it facilitates a detailed understanding of the (micro-)anatomy of extinct species with no damage to the precious fossil specimens. Here, we report studies of two fossil bone samples, specifcally the tibia of a 300-million-year-old tetrapod, Discosauriscus austriacus, and the humerus of a 370-million-year-old lobe-fnned fsh, Eusthenopteron foordi, using XRD-CT – a combination of X-ray difraction (XRD) and computed tomography (CT). Reconstructed 3D images showing the spatial mineral distributions and the local orientation of HA were obtained. For Discosauriscus austriacus, details of the muscle attachments could be discerned. For Eusthenopteron foordi, the gross details of the preferred orientation of HA were deduced using three tomographic datasets obtained with orthogonally oriented rotation axes. For both samples, the HA in the bone matrix exhibited preferred orientation, with the unit cell c-axis of the HA crystallites tending to be parallel with the bone surface. In summary, we have demonstrated that XRD-CT combined with an intuitive reconstruction procedure is becoming a powerful tool for studying palaeontological samples. -
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. -
Riversleigh World Heritage Area Brochure
ecological and biological processes. processes. biological and ecological processes. biological and ecological examples representing significant ongoing ongoing significant representing examples ongoing significant representing examples in Queensland. in Queensland. in stages of earth’s history, and Outstanding Outstanding and history, earth’s of stages Outstanding and history, earth’s of stages , including Riversleigh, are are Riversleigh, including , 5 — List Heritage World are Riversleigh, including , 5 — List Heritage World Outstanding examples representing major major representing examples Outstanding major representing examples Outstanding There are 19 Australian properties on the the on properties Australian 19 are There the on properties Australian 19 are There experiencemountisa.com.au experiencemountisa.com.au two of the ten World Heritage criteria: criteria: Heritage World ten the of two criteria: Heritage World ten the of two Amazon Rainforest. Rainforest. Amazon Rainforest. Amazon of years ago. For more information visit visit information more For ago. years of visit information more For ago. years of the World Heritage List in 1994. Both areas meet meet areas Both 1994. in List Heritage World the meet areas Both 1994. in List Heritage World the Canyon, the Egyptian Pyramids and the the and Pyramids Egyptian the Canyon, the and Pyramids Egyptian the Canyon, within the Riversleigh landscape as it was millions millions was it as landscape Riversleigh the within millions was it as landscape Riversleigh the within Riversleigh and Naracoorte were inscribed on on inscribed were Naracoorte and Riversleigh on inscribed were Naracoorte and Riversleigh Other World Heritage Sites include the Grand Grand the include Sites Heritage World Other Grand the include Sites Heritage World Other fascinating reconstructions of prehistoric animals animals prehistoric of reconstructions fascinating animals prehistoric of reconstructions fascinating significance’ to all humanity. -
The Devonian Tetrapod Acanthostega Gunnari Jarvik: Postcranial Anatomy, Basal Tetrapod Interrelationships and Patterns of Skeletal Evolution M
Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, 363-421, 1996 The Devonian tetrapod Acanthostega gunnari Jarvik: postcranial anatomy, basal tetrapod interrelationships and patterns of skeletal evolution M. I. Coates ABSTRACT: The postcranial skeleton of Acanthostega gunnari from the Famennian of East Greenland displays a unique, transitional, mixture of features conventionally associated with fish- and tetrapod-like morphologies. The rhachitomous vertebral column has a primitive, barely differentiated atlas-axis complex, encloses an unconstricted notochordal canal, and the weakly ossified neural arches have poorly developed zygapophyses. More derived axial skeletal features include caudal vertebral proliferation and, transiently, neural radials supporting unbranched and unsegmented lepidotrichia. Sacral and post-sacral ribs reiterate uncinate cervical and anterior thoracic rib morphologies: a simple distal flange supplies a broad surface for iliac attachment. The octodactylous forelimb and hindlimb each articulate with an unsutured, foraminate endoskeletal girdle. A broad-bladed femoral shaft with extreme anterior torsion and associated flattened epipodials indicates a paddle-like hindlimb function. Phylogenetic analysis places Acanthostega as the sister- group of Ichthyostega plus all more advanced tetrapods. Tulerpeton appears to be a basal stem- amniote plesion, tying the amphibian-amniote split to the uppermost Devonian. Caerorhachis may represent a more derived stem-amniote plesion. Postcranial evolutionary trends spanning the taxa traditionally associated with the fish-tetrapod transition are discussed in detail. Comparison between axial skeletons of primitive tetrapods suggests that plesiomorphic fish-like morphologies were re-patterned in a cranio-caudal direction with the emergence of tetrapod vertebral regionalisation. The evolution of digited limbs lags behind the initial enlargement of endoskeletal girdles, whereas digit evolution precedes the elaboration of complex carpal and tarsal articulations. -
Universidade Federal Do Ceará Centro De Ciências
UNIVERSIDADE FEDERAL DO CEARÁ CENTRO DE CIÊNCIAS DEPARTAMENTO DE BIOLOGIA CURSO DE CIÊNCIAS BIOLÓGICAS NÁDIA MARIA FREITAS EDUARDO ANÁLISE FUNCIONAL DO ESQUELETO APENDICULAR DE UM MARSUPIAL AUSTRALIANO DO MIOCENO FORTALEZA 2017 NÁDIA MARIA FREITAS EDUARDO ANÁLISE FUNCIONAL DO ESQUELETO APENDICULAR DE UM MARSUPIAL AUSTRALIANO DO MIOCENO Monografia apresentada ao Curso de Ciências Biológicas do Departamento de Biologia da Universidade Federal do Ceará, como requisito parcial para obtenção do Título de Bacharel em Ciências Biológicas. Orientador: Prof. Dr. Vicente Vieira Faria. Co-orientador: Dr. Michael Archer. FORTALEZA 2017 Aos meus pais, Eduardo e Kátia. Ao Grupo de Discussão sobre Mamíferos e Aves (GDMA) AGRADECIMENTOS À minha mãe, Kátia Freitas, por ter sido meu porto seguro, meu suporte e minha conselheira durante toda a graduação, desde a época do vestibular, passando pelo intercâmbio, até minha formatura. Ao meu pai, que mesmo falecido, sempre foi minha inspiração. À minha irmã, por sempre me apoiar e me provocar questionamentos. A os meus professores, colegas de graduação, colegas de trabalho e funcionários da UFC. Enfim, a todos aqueles que cruzaram meu caminho durante esses anos de graduação e, de alguma forma, colaboraram para minha formação profissional, pessoal e critica. À Pró Reitoria de Assuntos Estudantis, por ter me provido com uma vaga no programa de Residência Universitária, permitindo com que eu concluísse meus estudos em Fortaleza. Ao Grupo de Discussão sobre Mamíferos e Aves, que foi meu refúgio e principal fonte de conhecimento e discussão durante a graduação. A todos os laboratórios dos quais eu fiz parte. Em especial, durante minha Iniciação Científica no Laboratório de Histologia Animal, onde dei meus primeiros passos na pesquisa científica. -
Therocephalian (Therapsida) And
第55卷 第1期 古 脊 椎 动 物 学 报 pp. 24-40 2017年1月 VERTEBRATA PALASIATICA figs. -1 7 Therocephalian (Therapsida) and chroniosuchian (Reptiliomorpha) from the Permo-Triassic transitional Guodikeng Formation of the Dalongkou Section, Jimsar, Xinjiang, China LIU Jun1,2 Fernando ABDALA3 (1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044, China [email protected]) (2 University of Chinese Academy of Sciences Beijing 100039) (3 Evolutionary Studies Institute, University of the Witwatersrand Private Bag 3, WITS 2050, Johannesburg, South Africa) Abstract The Guodikeng Formation encompasses the terrestrial Permo-Triassic transition sequence in China. This formation crops out in the Dalongkou section, Jimsar, Xinjiang where remains of the dicynodonts Jimusaria and Lystrosaurus were found. We are describing here a therocephalian and a chroniosuchian from the Dalongkou section, which are the first records of these groups for the Guodikeng Formation. Diagnostic characters of the new therocephalian, Dalongkoua fuae gen. and sp. nov., include maxillary ventral margin strongly concave in lateral view; incisors spatulated and rounded; incisors and canines with faint serrations; coronoid process of the dentary with a marked external adductor fossa; triangular reflected lamina of the angular with two smooth concavities. Chroniosuchians are represented by several postcranial elements and the vertebral morphology is similar to Bystrowiana and Bystrowiella. These remains are interpreted as representing a Bystrowianidae indeterminate. The new findings increase the diversity of the Guodikeng Formation that is now represented by three or four dicynodonts, one therocephalian and one chroniosuchian. All these groups survived the massive P-T extinction but disappear from the fossil record in the Middle to Upper Triassic. -
The Sutural Pattern of Skull-Roof Bones in Lower Permian Discosauriscus Austriacus from Moravia
The sutural pattern of skull-roof bones in Lower Permian Discosauriscus austriacus from Moravia JOZEF KLEMBARA Klembara, J. 1994 06 15 The sutural pattern of skull-roofbones in Lower Permian DiKosauricN LETHAIA alcmiacuc &om Moravia. Lethaia, Vol. 27, pp. 85-95. Oslo. ISSN 0024-1 164. Sutures between ornamented bones of Discosaurixuc aumiacuc are mostly simple, but there are also more complicated, rarely serrated, sutures between some bones. In small individuals, the sutures are simple, but the same sutures also occur in the largest specimens. The character of the sutures and the incomplete ossification ofbones around the pineal foramen indicate the larva type of organization of DiKosauriKur The fenestra between premaxihies and nasals appears to be absent. In the majority of specimens, a squamosal-intertemporal sutural contact is present, altho~itissometimesredu~andinafewcasesintermptedbyapostorbitalandsupratemporal contact Therefore the character ‘intertmporal-squamosal suture present or absent’ cannot be used in this rigorous sense for testing the relationshipsof early tetrapods.The configuration of the suture between both parietals in osteolepiforms, Dixosaurixuc, and various early amphibians and reptiles indicates that the bones enclosing the pineal foramen in osteolepifonns are kontals. ODI~~RISCUS.Seymouriamorpha, Lower Permian mapod, skull woskLlcton, sutures. JoZqKlrmbara, Zoological Imthte, Faculty of Natural SCienceJ, Comeniuc University, Mlynskd dolina B-2,&42 15 Bratislava, Slovakia; 30th September, 1992; revised20th April, 1993. Two localities in the Boskovice Furrow in Moravia (Czech Material, methods and localities Republic) have produced a relatively large assemblage of more or less three-dimensional skeletal material of discosau- The localities and methods have been described by Klembara riscids (Klembara & MeszAroS 1992). Despite certain Mer- & MeszAroS (1992). -
Investigating the Biomechanics of a Lizard Skull Using Advanced Computer Modelling Techniques with Experimental Validation
INVESTIGATING THE BIOMECHANICS OF A LIZARD SKULL USING ADVANCED COMPUTER MODELLING TECHNIQUES WITH EXPERIMENTAL VALIDATION Being a Thesis submitted for the Degree of PhD In the University of Hull By Mehran Moazen, BSc (Hons) December 2008 Dedicated to my parents Table of contents Abstract Acknowledgements Contents…………………………………………………………………i Chapter 1: Introduction ......................................................................... 1 1.1 Overview............................................................................................................ 1 1.2 Model creation: geometry .................................................................................. 4 1.3 Biomechanical modelling .................................................................................. 5 1.3.1 Musculoskeletal modelling ......................................................................... 5 1.3.2 Finite element modelling ............................................................................ 7 1.4 Experimental validation study ........................................................................... 7 1.5 Methodology ...................................................................................................... 8 1.6 Goals of project.................................................................................................. 9 1.7 Chapter organization.......................................................................................... 9 Chapter 2: Lizard anatomy................................................................. -
A New Discosauriscid Seymouriamorph Tetrapod from the Lower Permian of Moravia, Czech Republic
A new discosauriscid seymouriamorph tetrapod from the Lower Permian of Moravia, Czech Republic JOZEF KLEMBARA Klembara, J. 2005. A new discosauriscid seymouriamorph tetrapod from the Lower Permian of Moravia, Czech Repub− lic. Acta Palaeontologica Polonica 50 (1): 25–48. A new genus and species, Makowskia laticephala gen. et sp. nov., of seymouriamorph tetrapod from the Lower Permian deposits of the Boskovice Furrow in Moravia (Czech Republic) is described in detail, and its cranial reconstruction is pre− sented. It is placed in the family Discosauriscidae (together with Discosauriscus and Ariekanerpeton) on the following character states: short preorbital region; rounded to oval orbits positioned mainly in anterior half of skull; otic notch dorsoventrally broad and anteroposteriorly deep; rounded to oval ventral scales. Makowskia is distinguished from other Discosauriscidae by the following characters: nasal bones equally long as broad; interorbital region broad; prefrontal− postfrontal contact lies in level of frontal mid−length (only from D. pulcherrimus); maxilla deepest at its mid−length; sub− orbital ramus of jugal short and dorsoventrally broad with long anterodorsal−posteroventral directed lacrimal−jugal su− ture; postorbital anteroposteriorly short and lacks elongated posterior process; ventral surface of basioccipital smooth; rows of small denticles placed on distinct ridges and intervening furrows radiate from place immediately laterally to artic− ular portion on ventral surface of palatal ramus of pterygoid (only from D. pulcherrimus); -
New Chroniosuchian Materials from Xinjiang, China
第58卷 第4期 古 脊 椎 动 物 学 报 pp. 283–292 figs. 1–4 2020年10月 VERTEBRATA PALASIATICA DOI: 10.19615/j.cnki.1000-3118.200415 New chroniosuchian materials from Xinjiang, China LIU Jun1,2,3 (1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044) (2 CAS Center for Excellence in Life and Paleoenvironment Beijing 100044 [email protected]) (3 College of Earth and Planetary Sciences, University of Chinese Academy of Sciences Beijing 100049) Abstract Chroniosuchians have the earliest representatives in Gansu, China, but the Chinese records were scarcer compared to Russia, especially the Triassic one. In Xinjiang, there was only one specimen reported from the upper part of the Guodikeng Formation. Here three new chroniosuchian specimens are reported from three new stratigraphic horizons: the Quanzijie Formation (middle Permian), the base of the Guodikeng Formation (upper Permian), and the Jiucaiyuan Formation (Lower Triassic). The osteoderm from the Jiucaiyuan Formation represents the first definite Triassic chroniosuchian from China. The new findings increase the chroniosuchian diversity and their time range in China. The bystrowianid chroniosuchian specimens from the Guodikeng and Jiucaiyuan formations demonstrated that this group survived in the end-Permian mass extinction in Xinjiang, China. Key words Xinjiang, China; Permian, Triassic; Quanzijie Formation, Guodikeng Formation, Jiucaiyuan Formation; Bystrowianidae, chroniosuchians Citation Liu J, 2020. New chroniosuchian materials from Xinjiang, China. Vertebrata PalAsiatica, 58(4): 283–292 1 Introduction The chroniosuchians were an enigmatic clade of non-amniotic tetrapods with uncertain phylogenetic position (Clack and Klembara, 2009; Schoch et al., 2010; Buchwitz et al., 2012; Witzmann and Schoch, 2018; Marjanović and Laurin, 2019).