HARPER-DISSERTATION-2019.Pdf

Total Page:16

File Type:pdf, Size:1020Kb

HARPER-DISSERTATION-2019.Pdf CRANIODENTAL ADAPTATION AND HOMOPLASY IN EARLY MAMMALS by Anthony Maxwell Harper A dissertation submitted to Johns Hopkins University in conformity with the requirements for the degree of Doctor of Philosophy Baltimore, Maryland September, 2019 Abstract For the first two-thirds of their over 180-million-year history, mammals left a sparse fossil record. Often the only direct evidence of these early forms are small and unassociated craniodental fragments. Despite these limitations, the three chapters of this thesis support the effectiveness of this type of material for estimating the functional and autecological capacities in Mesozoic mammals, through high resolution imaging and morphometric analysis of the molariform dentition. Each of the three chapters is a self-contained study addressing separate topics relating to the evolution of dental and petrosal morphology. The common thread between all sections is that variation in craniodental structure among Mesozoic lineages is greater than would be expected based only on the disparity seen among extant small mammals. This is a result of both the more “modern” dynamics of dental evolution in more Mesozoic mammalian lineages than historically appreciated (Chapters 1 and 3), and the more “primitive” morphology of the inner ear, even in groups very closely related to extant crown therians (Chapter 2). In both cases, the craniodental morphologies described are outside the range of variation seen in extant species. Chapter 1 describes several new specimens from the herbivorous stem-therian mammal Reigitherium, from the Late Cretaceous of Patagonia. These newly available specimens demonstrate that the herbivorous molar morphology seen in Reigitherium is ii derived from the more plesiomorphic tuberculosectorial pattern seen in the South American endemic group Meridiolestida. Chapter 2 presents descriptions and analysis of the internal structure of three stem therian petrosal bones from the Late Jurassic of North America, and middle Cretaceous of Mongolia. Within the comparative context of labyrinthine endocast evolution, it can be determined that many of the advanced features of modern therian hearing likely developed only after their divergence from their common ancestor with the fossil groups described here. Finally, Chapter 3 presents a macroevolutionary analysis of lower molariform shape change across a large sample of early mammaliaforms, using high-level morphometric methods. The results of this analysis suggest that the stochastic processes controlling the shape evolution of lower molariforms in crown Mammalia are shared across a wide range of “triconodont”, “symmetrodont”, and “tribosphenic” Mesozoic taxa. Dissertation Adviser Gabriel S. Bever Dissertation Readers Guillermo W. Rougier Brian M. Davis Adam D. Sylvester iii When I lay asleep, then did a sheep eat at the ivy-wreath on my head—it ate, and said thereby: “Zarathustra is no longer a scholar.” It said this, and went away clumsily and proudly. A child told it to me. I like to lie here where the children play, beside the ruined wall, among thistles and red poppies. A scholar am I still to the children, and also to the thistles and red poppies. Innocent are they, even in their wickedness. But to the sheep I am no longer a scholar: so willeth my lot—blessings upon it! F. Nietzsche Thus Spoke Zarathustra: Chapter 38 – On Scholars iv Acknowledgments Even during the darkest times in my academic and professional career, I have had the incredible good fortune of being able to look up toward several brilliant constellations. In the paleontological sphere these stars include the amazing people at the Los Angeles County Museums, especially Xiaoming Wang, Luis Chiappe, and Shelly Cox, who gave me my start as a volunteer in VP. I am also thankful for the kindness and patience shown by my supervisors Mark Roeder, Bruce Lander (both at Paleoenvironmental Associates), and Aaron Kaye (Badlands National Park) during my first part-time jobs in this field. Since joining the JHU anatomy program it has been an amazing experience contributing to three field seasons in the Big Horn Basin of Wyoming with Amy Chew, Shawn Zack, and Tonya Penkrot. And I will also fondly remember driving across central Patagonia looking for huesitos with Leandro Canessa, Andy Lires, Willy Turrazini, and Luca Appella-Guiscafre. Gracias por aguantarme. I have also been embarrassingly fortunate to have accumulated such an immense number of other friends, teachers and inspirations in paleontology, without whom this dissertation would have been impossible. Topping this list are Don Prothero, Michael Novacek, Rich Cifelli, ZheXi Luo, Annalisa Berta, Brian Davis, John Wible, Gabriel Bever, Eric Ekdale, David Weishampel, Cara Burres-Jones, Beth Strassler, Kena Fox-Dobbs, Paul Koch, Greg Wilson, Aneila Hogan, Yue Zhang, and Jessica Martin. To these folks I apologize for not knowing not to express how much your hard work and kindness has meant to me in this project, short of quoting G. G. Simpson the most prominent paleomammalologist, who in recommending his field to introverts like me wrote: “one of v the great values of paleontology is that it enables us to live in our own complex minds not just a few score years but more than three billion years.”1 Thank you for making those years so memorable. Above all, I am grateful for the direction provided by the brightest stars in my graduate career - David Archibald, Ken Rose, and Guillermo Rougier. It’s been a long strange trip. Thank you. I also want to thank all my friends and teachers in the Earth sciences, starting especially with David Douglass, Bruce Carter, Ling O’Connor, and Gerry Lewis, at Pasadena City College’s Geology Department, and the PCC Dana Club. As an undergraduate at UC Santa Cruz it was also a lot of fun taking part in several geology classes, and the 2007 Summer field season in the Inyo/White Mountains, thanks to the impressive organizational capabilities of Hide Schwatrz, Casey Moore, and Chris Pluhar (currently at Fresno State). I am also grateful to Gary Girty (SDSU), Ben Passey, and Naomi Levin (both currently at University of Michigan) for letting me into their exceptional graduate courses, and for allowing me to work on various non sequitur projects. Outside of the classroom, I am also extremely lucky to have received advice and encouragement from Thomas Bown, Judy King (CSU Dominguez Hills), Andy Evans (Geologist at AECOM), and Kimberly “Rain” Miner (Geoscientist at the Army Geospatial Research Lab). Thank you all for providing me with a compass in this strange world. Once this dissertation is finished I hope to see you in the field soon. vi The last decade and a half has also brought me into sympatric association with an amazing variety of biologists. The classes taught by Russell DiFiori (Pasadena City College), Tod Reeder, Marshall Hedin, Ken Burns, Michael Simpson, and Robert Zeller (SDSU) have been amazing experiences, for which I am extremely grateful. As a wildlife biologist at the San Diego Natural History Museum, working with my role models Scott Tremor, Phil Unit, Drew Stokes, Lori Hardgrove, Brad Holingsworth, and Melissa Stepek, has been one of the greatest times of my life. And my former supervisors Punkaj Kapahi (currently at Buck Institute), Viceca Sapin (Caltech), and Sandra Garver (SDSU anatomy), have also been inspirations to me throughout my academic career. Additionally, I have benefited immeasurably from the kindness of Patrick Luckett (JHU), Geoffrey Manley (University of Oldenburg), Steve Gliessman (UC Santa Cruz), Richard Etheridge, Mike Van Patten, Bob Mangan (the last three at SDSU), Phil Rundel (UCLA), Cindy Corbitt (University of Louisville), Samantha Young (Grossmont College), Yvea Moore (Crissy Field), and Isaac Simpson (Halibut for Humanity). Thank you all for making life so interesting. I will also be forever grateful for the expertise and patience that my teachers in the rarified spheres of math and other technical fields have shown me; starting especially with Anna Osipova, my high school math teacher who convinced me to “stick with it.” Likewise, this project would not have been possible without the superhuman commitment towards teaching shown by my graduate statistics professors Doug Deutschman and Matt Edwards at SDSU; and Gary Rosner, Robert Scharpf, Fernando Pineda, Frank Curriero, and Adam Sylvester at JHU. What little illustration skill I have is entirely due to the amazing talents of vii Tim Phelps, Ian Suk, Juan Garcia, and Gary Lees in the Johns Hopkins Art as Applied to Medicine Department; and the fact that this dissertation exists at all is due to Arlene Daniel (JHU Functional Anatomy and Evolution). To the many people I have missed here, please know that I am very sorry that I will never be able to list everyone who has indispensably helped me along my academic and professional trajectory. To everyone who has ever gotten behind me and helped push, thank you. Finally, because the best part of being a mammal is having a mom, I thank first and foremost my mom Lynn, and her mom Mary Ann (“Mimi”). Thank you for letting me pick apart those owl pellets, and everything else. 1In: Laporte, L. 2000. George Gaylord Simpson: Paleontologist and Evolutionist. Columbia University Press viii Publications and Coauthors The material in Chapter 1 is published as: Harper, T., A. Parras, and G. W. Rougier. Reigitherium (Meridiolestida, Mesungulatoidea) an enigmatic Late Cretaceous mammal from Patagonia, Argentina: morphology, affinities, and dental evolution. Journal of Mammalian Evolution (2018). https://doi.org/10.1007/s10914-018-9437-x This work was accomplished with the expert help and advice of the following coauthors: Ana Parras, INCITAP (CONICET-UNLPam), Facultad de Ciencias Exactas y Naturales, Universidad Nacional de La Pampa, Uruguay 151, 6300 Santa Rosa, La Pampa, Argentina Guillermo W. Rougier, Department of Anatomical Sciences and Neurobiology, University of Louisville, 511 S. Floyd St., Louisville, KY 40202, USA In particular, the sections “Study Area and Sample Provenance” and “Geological Background” in Chapter 1 were written by Ana Parras, one of the original discoverers of the Anfiteatro locality.
Recommended publications
  • Reptile-Like Physiology in Early Jurassic Stem-Mammals
    bioRxiv preprint doi: https://doi.org/10.1101/785360; this version posted October 10, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Title: Reptile-like physiology in Early Jurassic stem-mammals Authors: Elis Newham1*, Pamela G. Gill2,3*, Philippa Brewer3, Michael J. Benton2, Vincent Fernandez4,5, Neil J. Gostling6, David Haberthür7, Jukka Jernvall8, Tuomas Kankanpää9, Aki 5 Kallonen10, Charles Navarro2, Alexandra Pacureanu5, Berit Zeller-Plumhoff11, Kelly Richards12, Kate Robson-Brown13, Philipp Schneider14, Heikki Suhonen10, Paul Tafforeau5, Katherine Williams14, & Ian J. Corfe8*. Affiliations: 10 1School of Physiology, Pharmacology & Neuroscience, University of Bristol, Bristol, UK. 2School of Earth Sciences, University of Bristol, Bristol, UK. 3Earth Science Department, The Natural History Museum, London, UK. 4Core Research Laboratories, The Natural History Museum, London, UK. 5European Synchrotron Radiation Facility, Grenoble, France. 15 6School of Biological Sciences, University of Southampton, Southampton, UK. 7Institute of Anatomy, University of Bern, Bern, Switzerland. 8Institute of Biotechnology, University of Helsinki, Helsinki, Finland. 9Department of Agricultural Sciences, University of Helsinki, Helsinki, Finland. 10Department of Physics, University of Helsinki, Helsinki, Finland. 20 11Helmholtz-Zentrum Geesthacht, Zentrum für Material-und Küstenforschung GmbH Germany. 12Oxford University Museum of Natural History, Oxford, OX1 3PW, UK. 1 bioRxiv preprint doi: https://doi.org/10.1101/785360; this version posted October 10, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 13Department of Anthropology and Archaeology, University of Bristol, Bristol, UK. 14Faculty of Engineering and Physical Sciences, University of Southampton, Southampton, UK.
    [Show full text]
  • 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.
    [Show full text]
  • A Dated Phylogeny of Marsupials Using a Molecular Supermatrix and Multiple Fossil Constraints
    Journal of Mammalogy, 89(1):175–189, 2008 A DATED PHYLOGENY OF MARSUPIALS USING A MOLECULAR SUPERMATRIX AND MULTIPLE FOSSIL CONSTRAINTS ROBIN M. D. BECK* School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, New South Wales 2052, Australia Downloaded from https://academic.oup.com/jmammal/article/89/1/175/1020874 by guest on 25 September 2021 Phylogenetic relationships within marsupials were investigated based on a 20.1-kilobase molecular supermatrix comprising 7 nuclear and 15 mitochondrial genes analyzed using both maximum likelihood and Bayesian approaches and 3 different partitioning strategies. The study revealed that base composition bias in the 3rd codon positions of mitochondrial genes misled even the partitioned maximum-likelihood analyses, whereas Bayesian analyses were less affected. After correcting for base composition bias, monophyly of the currently recognized marsupial orders, of Australidelphia, and of a clade comprising Dasyuromorphia, Notoryctes,and Peramelemorphia, were supported strongly by both Bayesian posterior probabilities and maximum-likelihood bootstrap values. Monophyly of the Australasian marsupials, of Notoryctes þ Dasyuromorphia, and of Caenolestes þ Australidelphia were less well supported. Within Diprotodontia, Burramyidae þ Phalangeridae received relatively strong support. Divergence dates calculated using a Bayesian relaxed molecular clock and multiple age constraints suggested at least 3 independent dispersals of marsupials from North to South America during the Late Cretaceous or early Paleocene. Within the Australasian clade, the macropodine radiation, the divergence of phascogaline and dasyurine dasyurids, and the divergence of perameline and peroryctine peramelemorphians all coincided with periods of significant environmental change during the Miocene. An analysis of ‘‘unrepresented basal branch lengths’’ suggests that the fossil record is particularly poor for didelphids and most groups within the Australasian radiation.
    [Show full text]
  • Studies on Continental Late Triassic Tetrapod Biochronology. I. the Type Locality of Saturnalia Tupiniquim and the Faunal Succession in South Brazil
    Journal of South American Earth Sciences 19 (2005) 205–218 www.elsevier.com/locate/jsames Studies on continental Late Triassic tetrapod biochronology. I. The type locality of Saturnalia tupiniquim and the faunal succession in south Brazil Max Cardoso Langer* Departamento de Biologia, FFCLRP, Universidade de Sa˜o Paulo (USP), Av. Bandeirantes 3900, 14040-901 Ribeira˜o Preto, SP, Brazil Received 1 November 2003; accepted 1 January 2005 Abstract Late Triassic deposits of the Parana´ Basin, Rio Grande do Sul, Brazil, encompass a single third-order, tetrapod-bearing sedimentary sequence that includes parts of the Alemoa Member (Santa Maria Formation) and the Caturrita Formation. A rich, diverse succession of terrestrial tetrapod communities is recorded in these sediments, which can be divided into at least three faunal associations. The stem- sauropodomorph Saturnalia tupiniquim was collected in the locality known as ‘Waldsanga’ near the city of Santa Maria. In that area, the deposits of the Alemoa Member yield the ‘Alemoa local fauna,’ which typifies the first association; includes the rhynchosaur Hyperodapedon, aetosaurs, and basal dinosaurs; and is coeval with the lower fauna of the Ischigualasto Formation, Bermejo Basin, NW Argentina. The second association is recorded in deposits of both the Alemoa Member and the Caturrita Formation, characterized by the rhynchosaur ‘Scaphonyx’ sulcognathus and the cynodont Exaeretodon, and correlated with the upper fauna of the Ischigualasto Formation. Various isolated outcrops of the Caturrita Formation yield tetrapod fossils that correspond to post-Ischigualastian faunas but might not belong to a single faunal association. The record of the dicynodont Jachaleria suggests correlations with the lower part of the Los Colorados Formation, NW Argentina, whereas remains of derived tritheledontid cynodonts indicate younger ages.
    [Show full text]
  • Um Novo E Peculiar Cinodonte Traversodontídeo Para O Triássico Médio Do Rio Grande Do Sul E Suas Implicações Para a Paleoecologia De
    UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL INSTITUTO DE GEOCIÊNCIAS PROGRAMA DE PÓS-GRADUAÇÃO EM GEOCIÊNCIAS Um Novo e Peculiar Cinodonte Traversodontídeo para o Triássico Médio do Rio Grande do Sul e suas Implicações para a Paleoecologia de Cynodontia Míriam Reichel Orientador: Prof. Dr. Cesar Leandro Schultz Co-Orientadora: Profª. Drª. Marina Bento Soares Comissão Examinadora: Prof. Dr. José Fernando Bonaparte Prof. Dr. Mario Cozzuol Profª. Drª. Cristina Vega Dias Dissertação de Mestrado apresentada como requisito para obtenção do título de Mestre em Ciências Livros Grátis http://www.livrosgratis.com.br Milhares de livros grátis para download. Reichel, Miriam Um novo e peculiar Cinodonte Traversodontídeo para triássico médio do Rio Grande do Sul e suas implicações para a Paleoecologia de Cynodontia. / Miriam Reichel. - Porto Alegre : UFRGS, 2006. [145 f.] il. Dissertação (Mestrado). - Universidade Federal do Rio Grande do Sul. Instituto de Geociências. Programa de Pós-Graduação em Geociências. Porto Alegre, RS - BR, 2006. 1. Paleoecologia. 2. Cynodontia. 3. Traversodontidae. 4. Triássico Médio. 5. Formação Santa Maria. 6. Rio Grande do Sul. I. Título. _____________________________ Catalogação na Publicação Biblioteca Geociências - UFRGS Renata Cristina Grun CRB 10/1113 AGRADECIMENTOS • Ao professor Dr. José Fernando Bonaparte, pelos ensinamentos a respeito dos cinodontes, por estimular este trabalho, contribuindo com importantes comentários, e pela grande dedicação à paleontologia e àqueles que por ela se interessam. • Ao professor Dr. Cesar Leandro Schultz, por orientar este trabalho, por sempre tornar o ambiente de trabalho agradável, pelos conselhos e pela amizade. • À professora Dra. Marina Bento Soares, por me trazer para o mundo dos cinodontes, pela paciência e didática de fundamental importância para este trabalho, pelo carinho e pela amizade.
    [Show full text]
  • Using Dental Enamel Wrinkling to Define Sauropod Tooth Morphotypes from the Cañadón Asfalto Formation, Patagonia, Argentina
    RESEARCH ARTICLE Using Dental Enamel Wrinkling to Define Sauropod Tooth Morphotypes from the Cañadón Asfalto Formation, Patagonia, Argentina Femke M. Holwerda1,2,3*, Diego Pol4,5, Oliver W. M. Rauhut1,3 1 Staatliche Naturwissenschaftliche Sammlungen Bayerns (SNSB), Bayerische Staatssammlung für Paläontologie und Geologie, München, Germany, 2 GeoBioTec, Departamento de Ciências da Terra, Faculdade de Ciências e Tecnologia (FCT), Universidade Nova de Lisboa, Caparica, Portugal, 3 Department of Earth and Environmental Sciences and GeoBioCenter, Ludwig Maximilians Universität, München, Germany, 4 Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Buenos Aires, Argentina, 5 Museo Paleontológico Egidio Feruglio, Trelew, Argentina * [email protected] Abstract OPEN ACCESS The early Middle Jurassic is regarded as the period when sauropods diversified and be- Citation: Holwerda FM, Pol D, Rauhut OWM (2015) came major components of the terrestrial ecosystems. Not many sites yield sauropod mate- Using Dental Enamel Wrinkling to Define Sauropod Tooth Morphotypes from the Cañadón Asfalto rial of this time; however, both cranial and postcranial material of eusauropods have been Formation, Patagonia, Argentina. PLoS ONE 10(2): found in the Cañadón Asfalto Formation (latest Early Jurassic–early Middle Jurassic) in e0118100. doi:10.1371/journal.pone.0118100 Central Patagonia (Argentina), which may help to shed light on the early evolution of Academic Editor: Peter Dodson, University of eusauropods. These eusauropod remains include teeth associated with cranial and man- Pennsylvania, UNITED STATES dibular material as well as isolated teeth found at different localities. In this study, an assem- Received: September 1, 2014 blage of sauropod teeth from the Cañadón Asfalto Formation found in four different Accepted: January 7, 2015 localities in the area of Cerro Condor (Chubut, Argentina) is used as a mean of assessing sauropod species diversity at these sites.
    [Show full text]
  • Constraints on the Timescale of Animal Evolutionary History
    Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J.
    [Show full text]
  • The Oldest Platypus and Its Bearing on Divergence Timing of the Platypus and Echidna Clades
    The oldest platypus and its bearing on divergence timing of the platypus and echidna clades Timothy Rowe*†, Thomas H. Rich‡§, Patricia Vickers-Rich§, Mark Springer¶, and Michael O. Woodburneʈ *Jackson School of Geosciences, University of Texas, C1100, Austin, TX 78712; ‡Museum Victoria, PO Box 666, Melbourne, Victoria 3001, Australia; §School of Geosciences, PO Box 28E, Monash University, Victoria 3800, Australia; ¶Department of Biology, University of California, Riverside, CA 92521; and ʈDepartment of Geology, Museum of Northern Arizona, Flagstaff, AZ 86001 Edited by David B. Wake, University of California, Berkeley, CA, and approved October 31, 2007 (received for review July 7, 2007) Monotremes have left a poor fossil record, and paleontology has broadly affect our understanding of early mammalian history, been virtually mute during two decades of discussion about with special implications for molecular clock estimates of basal molecular clock estimates of the timing of divergence between the divergence times. platypus and echidna clades. We describe evidence from high- Monotremata today comprises five species that form two resolution x-ray computed tomography indicating that Teinolo- distinct clades (16). The echidna clade includes one short-beaked phos, an Early Cretaceous fossil from Australia’s Flat Rocks locality species (Tachyglossus aculeatus; Australia and surrounding is- (121–112.5 Ma), lies within the crown clade Monotremata, as a lands) and three long-beaked species (Zaglossus bruijni, Z. basal platypus. Strict molecular clock estimates of the divergence bartoni, and Z. attenboroughi, all from New Guinea). The between platypus and echidnas range from 17 to 80 Ma, but platypus clade includes only Ornithorhynchus anatinus (Austra- Teinolophos suggests that the two monotreme clades were al- lia, Tasmania).
    [Show full text]
  • Fossil Focus: Dinosaurs Down Under Author(S): Stephen F
    www.palaeontologyonline.com |Page 1 Title: Fossil Focus: Dinosaurs Down Under Author(s): Stephen F. Propat *1 Volume: 5 Article: 1 Page(s): 1-11 Published Date: 01/01/2015 PermaLink: http://www.palaeontologyonline.com/articles/2015/fossil-focus-dinosaurs/ IMPORTANT Your use of the Palaeontology [online] archive indicates your acceptance of Palaeontology [online]'s Terms and Conditions of Use, available at http://www.palaeontologyonline.com/site-information/terms-and-conditions/. COPYRIGHT Palaeontology [online] (www.palaeontologyonline.com) publishes all work, unless otherwise stated, under the Creative Commons Attribution 3.0 Unported (CC BY 3.0) license. This license lets others distribute, remix, tweak, and build upon the published work, even commercially, as long as they credit Palaeontology[online] for the original creation. This is the most accommodating of licenses offered by Creative Commons and is recommended for maximum dissemination of published material. Further details are available at http://www.palaeontologyonline.com/site-information/copyright/. CITATION OF ARTICLE Please cite the following published work as: Propat, Stephen F.. 2015. Fossil Focus: Dinosaurs Down Under, Palaeontology Online, Volume 5, Article 1, 1- 11. Published by: Palaeontology [online] www.palaeontologyonline.com |Page 2 Fossil Focus: Dinosaurs Down Under by Stephen F. Poropat*1,2 Introduction: Ask the average person in the street to name an Australian dinosaur, and you will be lucky if you get a correct answer. If they say crocodile, they are in the right postcode but have the wrong address. If they say emu, then they are correct, strictly speaking, but they are either lucky or being smart. If they say kangaroo, back away slowly and avoid eye contact.
    [Show full text]
  • 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.
    [Show full text]
  • Lower Triassic Postcanine Teeth with Allotherian-Like Crowns
    Research Letters South African Journal of Science 103, May/June 2007 245 Lower Triassic postcanine teeth with allotherian-like crowns F. Abdala*‡, H. Mocke*§ and P.J. Hancox* The Allotheria are fossil mammals with upper and lower post- canines usually showing two longitudinal rows of cusps separated by a central valley. The group comprises the poorly known haramiyids, mostly represented by isolated teeth, and the notably diverse and long-lived multituberculates; its monophyly is uncer- tain. The oldest records of this particular group are the Late Triassic (Norian–Rhaetian) haramiyids. We present here postcanines with haramiyid-like crowns that were recovered from the Lower Triassic of South Africa. A distinguishing feature of the new teeth is that they are single-rooted. This is the oldest record of mammal-like teeth with crowns having parallel rows of cusps, representing a temporal extension of some 43 million years from similar crown patterns of haramiyids and tritylodontids. This finding reinforces evidence of the remarkable faunal turnover of therapsids in the Early/Middle Triassic, at which time an explosive origin followed by a rapid early diversification of herbivorous/omnivorous forms with occluding expanded postcanines took place. Introduction The Beaufort Group of the South African Karoo shows an abundance and diversity of non-mammalian synapsids, which have allowed for biostratigraphic subdivisions ranging from Middle Permian to Middle Triassic.1 The youngest of these Fig. 1.Allotherian-like teeth.A, Occlusal and lateral views of BP/1/6515 (Pattern 1); B, occlusal and lateral views of BP/1/6516 (Pattern 2). biozones, the Cynognathus Assemblage Zone (AZ), comprises the full extent of the Burgersdorp Formation of the Tarkastad Sub- found to be most parsimonious from an unconstrained search, group (J.
    [Show full text]
  • Osteohistology of Late Triassic Prozostrodontian Cynodonts from Brazil
    Osteohistology of Late Triassic prozostrodontian cynodonts from Brazil Jennifer Botha-Brink1,2, Marina Bento Soares3 and Agustín G. Martinelli3 1 Department of Karoo Palaeontology, National Museum, Bloemfontein, South Africa 2 Department of Zoology and Entomology, University of the Free State, Bloemfontein, South Africa 3 Departamento de Paleontologia e Estratigrafia, Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Porto Alegre, Brazil ABSTRACT The Prozostrodontia includes a group of Late Triassic-Early Cretaceous eucynodonts plus the clade Mammaliaformes, in which Mammalia is nested. Analysing their growth patterns is thus important for understanding the evolution of mammalian life histories. Obtaining material for osteohistological analysis is difficult due to the rare and delicate nature of most of the prozostrodontian taxa, much of which comprises mostly of crania or sometimes even only teeth. Here we present a rare opportunity to observe the osteohistology of several postcranial elements of the basal prozostrodontid Prozostrodon brasiliensis, the tritheledontid Irajatherium hernandezi, and the brasilodontids Brasilodon quadrangularis and Brasilitherium riograndensis from the Late Triassic of Brazil (Santa Maria Supersequence). Prozostrodon and Irajatherium reveal similar growth patterns of rapid early growth with annual interruptions later in ontogeny. These interruptions are associated with wide zones of slow growing bone tissue. Brasilodon and Brasilitherium exhibit a mixture of woven-fibered bone tissue and slower growing parallel-fibered and lamellar bone. The slower growing bone tissues are present even during early ontogeny. The relatively slower growth in Brasilodon and Brasilitherium may be related to their small body size compared to Prozostrodon and Irajatherium. These brasilodontids also exhibit osteohistological similarities with the Late Triassic/Early Jurassic mammaliaform Morganucodon and the Late Cretaceous multituberculate mammals Kryptobaatar and Nemegtbaatar.
    [Show full text]