The Origins of the Cochlea and Impedance Matching Hearing in Synapsids
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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
On the Stratigraphic Range of the Dicynodont Taxon Emydops (Therapsida: Anomodontia) in the Karoo Basin, South Africa
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Wits Institutional Repository on DSPACE On the stratigraphic range of the dicynodont taxon Emydops (Therapsida: Anomodontia) in the Karoo Basin, South Africa Kenneth D. Angielczyk1*, Jörg Fröbisch2 & Roger M.H. Smith3 1Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, BS8 1RJ, United Kingdom 2Department of Biology, University of Toronto at Mississauga, 3359 Mississauga Rd., Mississauga, ON, L5L 1C6, Canada 3Divison of Earth Sciences, South African Museum, P.O. Box 61, Cape Town, 8000 South Africa Received 19 May 2005. Accepted 8 June 2006 The dicynodont specimen SAM-PK-708 has been referred to the genera Pristerodon and Emydops by various authors, and was used to argue that the first appearance of Emydops was in the Tapinocephalus Assemblage Zone in the Karoo Basin of South Africa. However, the specimen never has been described in detail, and most discussions of its taxonomic affinities were based on limited data. Here we redescribe the specimen and compare it to several small dicynodont taxa from the Tapinocephalus and Pristerognathus assemblage zones. Although the specimen is poorly preserved, it possesses a unique combination of features that allows it to be assigned confidently to Emydops. The locality data associated with SAM-PK-708 are vague, but they allow the provenance of the specimen to be narrowed down to a relatively limited area southwest of the town of Beaufort West. Strata from the upper Tapinocephalus Assemblage Zone and the Pristerognathus Assemblage Zone crop out in this area, but we cannot state with certainty from which of these biostratigraphic divisions the specimen was collected. -
Ischigualasto Formation. the Second Is a Sile- Diversity Or Abundance, but This Result Was Based on Only 19 of Saurid, Ignotosaurus Fragilis (Fig
This article was downloaded by: [University of Chicago Library] On: 10 October 2013, At: 10:52 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Journal of Vertebrate Paleontology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ujvp20 Vertebrate succession in the Ischigualasto Formation Ricardo N. Martínez a , Cecilia Apaldetti a b , Oscar A. Alcober a , Carina E. Colombi a b , Paul C. Sereno c , Eliana Fernandez a b , Paula Santi Malnis a b , Gustavo A. Correa a b & Diego Abelin a a Instituto y Museo de Ciencias Naturales, Universidad Nacional de San Juan , España 400 (norte), San Juan , Argentina , CP5400 b Consejo Nacional de Investigaciones Científicas y Técnicas , Buenos Aires , Argentina c Department of Organismal Biology and Anatomy, and Committee on Evolutionary Biology , University of Chicago , 1027 East 57th Street, Chicago , Illinois , 60637 , U.S.A. Published online: 08 Oct 2013. To cite this article: Ricardo N. Martínez , Cecilia Apaldetti , Oscar A. Alcober , Carina E. Colombi , Paul C. Sereno , Eliana Fernandez , Paula Santi Malnis , Gustavo A. Correa & Diego Abelin (2012) Vertebrate succession in the Ischigualasto Formation, Journal of Vertebrate Paleontology, 32:sup1, 10-30, DOI: 10.1080/02724634.2013.818546 To link to this article: http://dx.doi.org/10.1080/02724634.2013.818546 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. -
First Palaeohistological Inference of Resting
First palaeohistological inference of resting metabolic rate in an extinct synapsid, Moghreberia nmachouensis (Therapsida: Anomodontia) Chloe Olivier, Alexandra Houssaye, Nour-Eddine Jalil, Jorge Cubo To cite this version: Chloe Olivier, Alexandra Houssaye, Nour-Eddine Jalil, Jorge Cubo. First palaeohistological inference of resting metabolic rate in an extinct synapsid, Moghreberia nmachouensis (Therapsida: Anomodon- tia). Biological Journal of the Linnean Society, Linnean Society of London, 2017, 121 (2), pp.409-419. 10.1093/biolinnean/blw044. hal-01625105 HAL Id: hal-01625105 https://hal.sorbonne-universite.fr/hal-01625105 Submitted on 27 Oct 2017 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. First palaeohistological inference of resting metabolic rate in extinct synapsid, Moghreberia nmachouensis (Therapsida: Anomodontia) CHLOE OLIVIER1,2, ALEXANDRA HOUSSAYE3, NOUR-EDDINE JALIL2 and JORGE CUBO1* 1 Sorbonne Universités, UPMC Univ Paris 06, CNRS, UMR 7193, Institut des Sciences de la Terre Paris (iSTeP), 4 place Jussieu, BC 19, 75005, Paris, France 2 Sorbonne Universités -CR2P -MNHN, CNRS, UPMC-Paris6. Muséum national d’Histoire naturelle. 57 rue Cuvier, CP38. F-75005, Paris, France 3Département Écologie et Gestion de la Biodiversité, UMR 7179, CNRS/Muséum national d’Histoire naturelle, 57 rue Cuvier, CP 55, Paris, 75005, France *Corresponding author. -
Micheli Stefanello
UNIVERSIDADE FEDERAL DE SANTA MARIA CENTRO DE CIÊNCIAS NATURAIS E EXATAS PROGRAMA DE PÓS-GRADUAÇÃO EM BIODIVERSIDADE ANIMAL Micheli Stefanello DESCRIÇÃO E FILOGENIA DE UM NOVO ESPÉCIME DE CINODONTE PROBAINOGNÁTIO DO TRIÁSSICO SUL-BRASILEIRO Santa Maria, RS 2018 Micheli Stefanello DESCRIÇÃO E FILOGENIA DE UM NOVO ESPÉCIME DE CINODONTE PROBAINOGNÁTIO DO TRIÁSSICO SUL-BRASILEIRO Dissertação apresentada ao Curso de Mestrado do Programa de Pós-Graduação em Biodiversidade Animal, Área de Concentração em Sistemática e Biologia Evolutiva, da Universidade Federal de Santa Maria (UFSM, RS), como requisito parcial para obtenção do grau de Mestre em Ciências Biológicas – Área Biodiversidade Animal. Orientador: Prof. Dr. Sérgio Dias da Silva Santa Maria, RS 2018 Micheli Stefanello DESCRIÇÃO E FILOGENIA DE UM NOVO ESPÉCIME DE CINODONTE PROBAINOGNÁTIO DO TRIÁSSICO SUL-BRASILEIRO Dissertação apresentada ao Curso de Mestrado do Programa de Pós-Graduação em Biodiversidade Animal, Área de Concentração em Sistemática e Biologia Evolutiva, da Universidade Federal de Santa Maria (UFSM, RS), como requisito parcial para obtenção do grau de Mestre em Ciências Biológicas – Área Biodiversidade Animal. Aprovada em 28 de fevereiro de 2018: Santa Maria, RS 2018 AGRADECIMENTOS Ao meu orientador, Dr. Sérgio Dias da Silva, pela orientação, por todo o tempo despendido ao longo desse mestrado e por possibilitar meu aprimoramento na área a qual tenho apreço. Aos colegas do Centro de Apoio à Pesquisa Paleontológica da Quarta Colônia da Universidade Federal de Santa Maria (CAPPA/UFSM) e do Laboratório de Paleobiodiversidade Triássica, dessa mesma instituição, pela convivência e por terem ajudado-me de diferentes formas ao longo do mestrado. Em especial, ao colega Rodrigo Temp Müller, pela coleta do espécime (objeto de estudo dessa dissertação), por toda a ajuda com o TNT e com as figuras, e por auxiliar-me de inúmeras formas. -
The Sauropodomorph Biostratigraphy of the Elliot Formation of Southern Africa: Tracking the Evolution of Sauropodomorpha Across the Triassic–Jurassic Boundary
Editors' choice The sauropodomorph biostratigraphy of the Elliot Formation of southern Africa: Tracking the evolution of Sauropodomorpha across the Triassic–Jurassic boundary BLAIR W. MCPHEE, EMESE M. BORDY, LARA SCISCIO, and JONAH N. CHOINIERE McPhee, B.W., Bordy, E.M., Sciscio, L., and Choiniere, J.N. 2017. The sauropodomorph biostratigraphy of the Elliot Formation of southern Africa: Tracking the evolution of Sauropodomorpha across the Triassic–Jurassic boundary. Acta Palaeontologica Polonica 62 (3): 441–465. The latest Triassic is notable for coinciding with the dramatic decline of many previously dominant groups, followed by the rapid radiation of Dinosauria in the Early Jurassic. Among the most common terrestrial vertebrates from this time, sauropodomorph dinosaurs provide an important insight into the changing dynamics of the biota across the Triassic–Jurassic boundary. The Elliot Formation of South Africa and Lesotho preserves the richest assemblage of sauropodomorphs known from this age, and is a key index assemblage for biostratigraphic correlations with other simi- larly-aged global terrestrial deposits. Past assessments of Elliot Formation biostratigraphy were hampered by an overly simplistic biozonation scheme which divided it into a lower “Euskelosaurus” Range Zone and an upper Massospondylus Range Zone. Here we revise the zonation of the Elliot Formation by: (i) synthesizing the last three decades’ worth of fossil discoveries, taxonomic revision, and lithostratigraphic investigation; and (ii) systematically reappraising the strati- graphic provenance of important fossil locations. We then use our revised stratigraphic information in conjunction with phylogenetic character data to assess morphological disparity between Late Triassic and Early Jurassic sauropodomorph taxa. Our results demonstrate that the Early Jurassic upper Elliot Formation is considerably more taxonomically and morphologically diverse than previously thought. -
Width Measured at the Level of Anterior Squamosal/Parietal Suture
Fig. 5. (A) Scaling of brain vault size (width measured at the level of anterior squamosal/parietal suture) relative to skull size (measured at the distance between the left versus right temporomandibular joints). This shows that allometry of small size of Hadrocodium, by itself, is not sufficient to account for its very large braincase. Had-rocodium's brain vault is larger (wider) than expected for the crown-group mammals with similar skull width from the allometrical regression. By contrast, all contemporaneous mammaliaforms (triangles: Sinoconodon, Morganucodon, and Haldanodon) with the postdentary trough and meckelian groove have smaller (narrower) brain vaults than those living mammal taxa (and Hadrocodium) of comparable skull size. The brain vault is narrower in nonmammaliaform cynodonts (squares: Chaliminia, Massetoganthus, Probelesodon, Probainognathus, and Yunnanodon) than in mammaliaform stem taxa and much narrower than expected for crown group mammals of similar size. The allometric equation (natural logarithmic scale) for the brain vault width (Y) to the skull width at the level of TMJ (X) for species in the mammalian crown groups (circles: 37 living and 8 fossil species): Y =0.98X -0.31 (R2 – 0.715). Data from cynodonts, mammaliaforms, and Hadrocodium are added second arily for comparison with the regression of extant and fossil species of mammalian crown group. (B) Estimated body-size distributions of mammaliaform insectivores in the Early Jurassic Lufeng fauna [following method of Gingerich (50)]. The estimated 2-g body mass of Hadrocodium is in strong contrast to its contemporary mammaliaforms of the Late Triassic and Early Jurassic, such as Sinconodon (from ~13 to ~517 g, based on skull length from 22 to 62 mm) and Morganucodon (from 27 to 89 g, based on skull length from 27 to 38 mm). -
The Anatomy and Phylogenetic Relationships of Antetonitrus Ingenipes (Sauropodiformes, Dinosauria): Implications for the Origins of Sauropoda
THE ANATOMY AND PHYLOGENETIC RELATIONSHIPS OF ANTETONITRUS INGENIPES (SAUROPODIFORMES, DINOSAURIA): IMPLICATIONS FOR THE ORIGINS OF SAUROPODA Blair McPhee A dissertation submitted to the Faculty of Science, University of the Witwatersrand, in partial fulfilment of the requirements for the degree of Master of Science. Johannesburg, 2013 i ii ABSTRACT A thorough description and cladistic analysis of the Antetonitrus ingenipes type material sheds further light on the stepwise acquisition of sauropodan traits just prior to the Triassic/Jurassic boundary. Although the forelimb of Antetonitrus and other closely related sauropododomorph taxa retains the plesiomorphic morphology typical of a mobile grasping structure, the changes in the weight-bearing dynamics of both the musculature and the architecture of the hindlimb document the progressive shift towards a sauropodan form of graviportal locomotion. Nonetheless, the presence of hypertrophied muscle attachment sites in Antetonitrus suggests the retention of an intermediary form of facultative bipedality. The term Sauropodiformes is adopted here and given a novel definition intended to capture those transitional sauropodomorph taxa occupying a contiguous position on the pectinate line towards Sauropoda. The early record of sauropod diversification and evolution is re- examined in light of the paraphyletic consensus that has emerged regarding the ‘Prosauropoda’ in recent years. iii ACKNOWLEDGEMENTS First, I would like to express sincere gratitude to Adam Yates for providing me with the opportunity to do ‘real’ palaeontology, and also for gladly sharing his considerable knowledge on sauropodomorph osteology and phylogenetics. This project would not have been possible without the continued (and continual) support (both emotionally and financially) of my parents, Alf and Glenda McPhee – Thank you. -
Evolution of the Mammalian Fauces Region and the Origin of Suckling
Evolution of the mammalian fauces region and the origin of suckling The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Crompton, Alfred, Catherine Musinsky, Jose Bonaparte, Bhart- Anjan Bhullar, and Tomasz Owerkowicz. Evolution of the mammalian fauces region and the origin of suckling (2018). Citable link https://nrs.harvard.edu/URN-3:HUL.INSTREPOS:37364482 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA 1 Evolution of the mammalian fauces region and the origin of suckling Alfred Crompton1†, Catherine Musinsky1, Jose Bonaparte2, Bhart-Anjan Bhullar3, Tomasz Owerkowicz4 1: Harvard University, Organismic and Evolutionary Biology Department, Museum of Comparative Zoology, 26 Oxford St, Cambridge, MA 02138 USA 2: Museo Municipal de C. Naturales "C. Ameghino", 6600 MERCEDES – BS. AS. Argentina 3: Department of Geology & Geophysics, Yale University, PO Box 208109, New Haven, CT 06520- 8109 USA 4: Department of Biology, California State University in San Bernadino, 5500 University Pkwy, San Bernardino, CA 92407 USA †corresponding author: ORCID 0000-0001-6008-2587, [email protected], 617-495-3202 Acknowledgments Thanks to Dr. Edgar Allin for his comments on an early draft of this paper. Thanks to the Museum of Comparative Zoology, its Director, Professor James Hanken, and to the Center for Nanoscale Systems at Harvard University for providing the facilities and finances for this research. -
The Role of Fossils in Interpreting the Development of the Karoo Basin
Palaeon!. afr., 33,41-54 (1997) THE ROLE OF FOSSILS IN INTERPRETING THE DEVELOPMENT OF THE KAROO BASIN by P. J. Hancox· & B. S. Rubidge2 IGeology Department, University of the Witwatersrand, Private Bag 3, Wits 2050, South Africa 2Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, Wits 2050, South Africa ABSTRACT The Permo-Carboniferous to Jurassic aged rocks oft1:J.e main Karoo Basin ofSouth Africa are world renowned for the wealth of synapsid reptile and early dinosaur fossils, which have allowed a ten-fold biostratigraphic subdivision ofthe Karoo Supergroup to be erected. The role offossils in interpreting the development of the Karoo Basin is not, however, restricted to biostratigraphic studies. Recent integrated sedimentological and palaeontological studies have helped in more precisely defming a number of problematical formational contacts within the Karoo Supergroup, as well as enhancing palaeoenvironmental reconstructions, and basin development models. KEYWORDS: Karoo Basin, Biostratigraphy, Palaeoenvironment, Basin Development. INTRODUCTION Invertebrate remains are important as indicators of The main Karoo Basin of South Africa preserves a facies genesis, including water temperature and salinity, retro-arc foreland basin fill (Cole 1992) deposited in as age indicators, and for their biostratigraphic potential. front of the actively rising Cape Fold Belt (CFB) in Fossil fish are relatively rare in the Karoo Supergroup, southwestern Gondwana. It is the deepest and but where present are useful indicators of gross stratigraphically most complete of several depositories palaeoenvironments (e.g. Keyser 1966) and also have of Permo-Carboniferous to Jurassic age in southern biostratigraphic potential (Jubb 1973; Bender et al. Africa and reflects changing depositional environments 1991). -
The Pelvic and Hind Limb Anatomy of the Stem-Sauropodomorph Saturnalia Tupiniquim (Late Triassic, Brazil)
PaleoBios 23(2):1–30, July 15, 2003 © 2003 University of California Museum of Paleontology The pelvic and hind limb anatomy of the stem-sauropodomorph Saturnalia tupiniquim (Late Triassic, Brazil) MAX CARDOSO LANGER Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, BS8 1RJ Bristol, UK. Current address: Departamento de Biologia, Universidade de São Paulo (USP), Av. Bandeirantes, 3900 14040-901 Ribeirão Preto, SP, Brazil; [email protected] Three partial skeletons allow a nearly complete description of the sacrum, pelvic girdle, and hind limb of the stem- sauropodomorph Saturnalia tupiniquim, from the Late Triassic Santa Maria Formation, South Brazil. The new morphological data gathered from these specimens considerably improves our knowledge of the anatomy of basal dinosaurs, providing the basis for a reassessment of various morphological transformations that occurred in the early evolution of these reptiles. These include an increase in the number of sacral vertebrae, the development of a brevis fossa, the perforation of the acetabulum, the inturning of the femoral head, as well as various modifications in the insertion of the iliofemoral musculature and the tibio-tarsal articulation. In addition, the reconstruction of the pelvic musculature of Saturnalia, along with a study of its locomotion pattern, indicates that the hind limb of early dinosaurs did not perform only a fore-and-aft stiff rotation in the parasagittal plane, but that lateral and medial movements of the leg were also present and important. INTRODUCTION sisting of most of the presacral vertebral series, both sides Saturnalia tupiniquim was described in a preliminary of the pectoral girdle, right humerus, partial right ulna, right fashion by Langer et al. -
Dashankou Fauna: a Unique Window on the Early Evolution of Therapsids
Vol.24 No.2 2010 Paleoherpetology Dashankou Fauna: A Unique Window on the Early Evolution of Therapsids LIU Jun* Institute of Vertebrate Paleontology and Paleoanthropology, CAS, Beijing 100044, China n the 1980s, the Institute of Geology, Chinese Academy of IGeological Sciences (IGCAGS) sent an expedition to the area north of the Qilian Mountains to study the local terrestrial Permian and Triassic deposits. A new vertebrate fossil locality, later named Dashankou Fauna, was discovered by Prof. CHENG Zhengwu in Dashankou, Yumen, Gansu Province in 1981. Small-scale excavations in 1981, 1982 and 1985 demonstrated that this locality was a source of abundant and diverse vertebrate fossils. In the 1990s, supported by the National Natural Science Foundation of China, the Fig. 1 Prof. LI Jinling in the excavation of 1995. She first summarized the known IGCAGS, the Institute of Vertebrate members of the Dashankou Fauna and brought it to light as the most primitive and abundant Chinese tetrapod fauna. Paleontology and Paleoanthropology (IVPP) under CAS, and the Geological Museum of China formed a joint team IVPP were productive and have since investigations were first disseminated to work on this fauna. Three large- unveiled an interesting episode in the to the public in 1995. In 2001, Prof. scale excavations, undertaken in transition from reptiles to mammals in LI Jinling summarized the known 1991, 1992, and 1995 respectively, as evolutionary history. members of the fauna and discussed well as the subsequent ones held by The results from these their features. She pointed out that * To whom correspondence should be addressed at [email protected].