Middle Ear Structures in the Permian Glanosuchus Sp. (Therocephalia, Therapsida), Based on Thin Sections
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Ear in Mammal-Like Reptiles and Early Mammals
Acta Palaeontologica Polonica Vol. 28, No. 1-2 pp, 147-158 Warszawa, 1983 Second Symposium on Mesozoic T erre stial Ecosystems, Jadwisin 1981 KENNETH A. KERMACK and FRANCES MUSSETT THE EAR IN MAMMAL-LIKE REPTILES AND EARLY MAMMALS KERMACK, K . A. a nd MUSS ETT, F.: The ear in mammal-like r eptiles an d early mammals. Acta Palaeont. P olonica , 28, 1-2, 147-158, 1983. Th e early m embers of the Theropsida lacked a tympanic membrane. In the later theropslds, the Therapsid a, a tym p an ic membrane develop ed from thc skin on the lateral side of th e lower jaw. The tympanum is not homologous In the Therapsida and ' t he Sauropslda. The ther apsid ea r w as a poor receiver of airborne sound, both In hi gh frequency r esp onse and In the r ange of frequencies encompassed. With the radiation of the Sauropsida in the Triassic the large therapsids became extinct, the small therap si ds evolv ed In to the mammal s and became nocturnal. High frequency hearin g w as essen tial for the nocturn al mode of life; quadrate and arttcutar became diss ociated from the jaw hinge to become the m ammali an au di tory ossi cles . I n the Theria the cochlea became coil ed. The spiral cochlea could n ot have existed until there w as a middle ear w ith the n ec essary h ig h f re q uency r esp onse. This m ay n ot have been until the Cretace ous. -
The Intramandibular Joint in Girella: a Mechanism for Increased Force Production?
JOURNAL OF MORPHOLOGY 271:271–279 (2010) The Intramandibular Joint in Girella: A Mechanism for Increased Force Production? Lara A. Ferry-Graham1,3* and Nicolai Konow2 1California State University, Moss Landing Marine Labs, Moss Landing, California 95039 2Brown University, Ecology and Evolutionary Biology, Providence, Box G-B204, Rhode Island 02912 3CEAZA, Centro de Estudios Avanzados de Zonas Aridas (Center for Advanced Studies in Arid Zones), Universidad Cato´lica del Norte. Box 599, Benavente 980, La Serena, Chile ABSTRACT Intramandibular joints (IMJ) are novel Bellwood, 2002). This is likely due to the forces articulations between bony elements of the lower jaw required for obtaining food items many of which are that have evolved independently in multiple fish line- either tough or firmly attached to the substrate ages and are typically associated with biting herbivory. (Alfaro et al., 2001). In several reef fish lineages, This novel joint is hypothesized to function by augment- aspects of the feeding apparatus have been radically ing oral jaw expansion during mouth opening, which would increase contact between the tooth-bearing area altered for force production, either via hypertro- of the jaws and algal substratum during feeding, result- phied or via structurally altered musculature (Friel ing in more effective food removal from the substrate. and Wainwright, 1997), modified muscle attach- Currently, it is not understood if increased flexibility in ments (Vial and Ojeda, 1990; Konow and Bellwood, a double-jointed mandible also results in increased force 2005), or increased suturing and/or reinforcement generation during herbivorous biting and/or scraping. of bony elements and dentition (Tedman, 1980; Therefore, we selected the herbivore Girella laevifrons Streelman et al., 2002; Bellwood et al., 2003). -
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. -
Joints Chapter 8
Chapter 8 Joints Alessandro Castriota-Scanderbeg, M.D. Joints develop secondarily in the mesenchyme com- Joint Contracture, Joint Stiffness prised between the developing ends of two adjacent bones (mesenchymal interpose) at about 5 1/2 weeks. ᭤ [Limitation (loss) of (active and passive) The mesenchyme is converted to form fibrous tissue, joint motion] hyaline cartilage, or fibrocartilage, depending on whether the developing joint is a fibrous joint, a syn- The issue discussed in the current section encom- chondrosis, or a symphysis, respectively.At the site of passes a heterogeneous group of conditions, both in- a synovial joint, while the primitive mesenchyme of herited and acquired, isolated and associated with the interzone undergoes liquefaction and cavitation, syndromic and nonsyndromic malformation spec- giving rise to the articular cavity, its peripheral con- tra, localized to one joint and generalized. An intro- densation results in formation of the joint capsule duction to the contractural abnormalities developing (Resnick et al.1995).This process is completed by ap- after birth is first provided, followed by a discussion proximately 7 weeks of fetal age, and by 8 weeks of the congenital forms, which represent the main fo- movements of the limbs about the joint are appear- cus of the section. ing. Motion is essential for the normal development Flexion contracture and joint stiffness may occur of joints and contiguous structures. As discussed in as late manifestations of conditions causing joint more detail in the following pages, congenital limita- and/or surrounding tissue infiltration (sarcoidosis, tion or loss of joint function may be caused by factors amyloidosis), hemorrhage (trauma, hemophilia), or that either are intrinsic to the joint, or are extrinsic inflammation (rheumatoid arthritis, systemic lupus but inhibit fetal movements. -
The Teleost Intramandibular Joint: a Mechanism That Allows Fish to Obtain Prey Unavailable to Suction Feeders Alice C
Integrative and Comparative Biology Advance Access published May 21, 2015 Integrative and Comparative Biology Integrative and Comparative Biology, pp. 1–12 doi:10.1093/icb/icv042 Society for Integrative and Comparative Biology SYMPOSIUM The Teleost Intramandibular Joint: A mechanism That Allows Fish to Obtain Prey Unavailable to Suction Feeders Alice C. Gibb,1,* Katie Staab,† Clinton Moran* and Lara A. Ferry‡ *Department of Biology, Northern Arizona University, Flagstaff, AZ 86011-5640; †Biology Department, McDaniel College, Westminster, MD 21157; ‡School of Mathematical and Natural Sciences, Arizona State University, Glendale, AZ 85069-7100 From the symposium ‘‘New Insights into Suction Feeding Biomechanics and Evolution’’ presented at the annual meeting of the Society for Integrative and Comparative Biology, January 3–7, 2015 at West Palm Beach, Florida. 1Email: [email protected] Downloaded from Synopsis Although the majority of teleost fishes possess a fused lower jaw (or mandible), some lineages have acquired a secondary joint in the lower jaw, termed the intramandibular joint (IMJ). The IMJ is a new module that formed within http://icb.oxfordjournals.org/ the already exceptionally complex teleost head, and disarticulation of two bony elements of the mandible potentially creates a ‘‘double-jointed’’ jaw. The apparent independent acquisition of this new functional module in divergent lineages raises a suite of questions. (1) How many teleostean lineages contain IMJ-bearing species? (2) Does the IMJ serve the same purpose in all teleosts? (3) Is the IMJ associated with altered feeding kinematics? (4) Do IMJ-bearing fishes experience trade-offs in other aspects of feeding performance? (5) Is the IMJ used to procure prey that are otherwise unavailable? The IMJ is probably under-reported, but has been documented in at least 10 lineages within the Teleostei. -
AMERICAN MUSEUM Novitates PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET, NEW YORK, N.Y
AMERICAN MUSEUM Novitates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2827, pp. 1-57, figs. 1-45 August 13, 1985 An Essay on Euteleostean Classification DONN E. ROSEN' ABSTRACT The anatomy of the occipital region and rostral letic and raises questions about the monophyly of cartilage in euteleostean fishes is reviewed in some the fishes formerly grouped in the Osmeroidei. detail. These data, in combination with other an- Evidence is presented on how the occipital region atomical features taken from the literature, have might be used in acanthomorph systematics, and led to a reassessment of interrelationships within includes reasons for rejecting the concept of the the Euteleostei. This review supports the notions Paracanthopterygii, as this group was formerly that the Salmoniformes, Aulopiformes, Mycto- constituted. phiformes, and Beryciformes are nonmonophy- INTRODUCTION The earliest general classification of fishes dan (1923), A. Smith-Woodward (1932), in which it is possible to pick out many of Norman (1934), Berg (1940) and its various the main components of the Euteleostei is translations, reprinted editions and slightly that ofJohannes Muller (1844), in which the modified versions, and lastly Greenwood et teleosts as a whole were presented as a ver- al. (1966), McAllister (1968), and J. Nelson tebrate subclass, and their components as or- (1984)] went through an evolution from the ders. These orders of Muller's bore names early nonsubordinated, ordinal classifica- that may seem strange and unfamiliar to to- tions of Muller (1844), Agassiz (1858), Gill day's student, but the etymological charac- (1872), Boulenger (1904), and Regan (1909, teristics of many of them were preserved for 1929), to the complex subordinated, hierar- some time, a few even to the present. -
Amniote Phylogeny and the Importance of Fossils
Clndistirs (1988)4: 105-209 AMNIOTE PHYLOGENY AND THE IMPORTANCE OF FOSSILS Jacques Gauthierl,3,Arnold G. Klugel, and Timothy Rowe2 I Museum of ,500logy and Department of Biology, University of Michigan, Ann Arbor, MI 48109-1079; Department of Geological Sciences, University of Texas, Austin, TX 78713-7909, U.S.A. Ah.~/mcl Srvrral prominrnt cladists haw qurstioiied thc importancc of fossils in phylogrnctic inference, and it is becoming iiicreasingly popular to simply fit extinct forms, ifthcy are considered at all, 10 a cladogram ofReccnt taxa. Gardiner’s [ 1982) arid Lovtrup’s [ 1985) study ofamniote phylogeny rxcmplilirs this dilfrrrntial treatment, and we focuard on that group of organisms to test the proposition that hssils c;mnot overturn a theory of‘relatioiiships based only on the Recent biota. Our parsimony analysis of amniotc phylogrny, special knowledge contributed by fossils being scrupulously avoided, led to the followiiig best fitting classification, which is similar to the novel hypothesis Gardiner published: (lcpidmaurs (turtles (mammals (birds, crocodiles)))).However, adding fossils resulted in a markedly dilfcrcnt most parsimonious cladogram or thc extant taxa: (mammals (turtles (lepidosaurs [birds, crocodilrs)))).‘l‘hat classification is likr thr traditional hypothesis, and it provides a brttrr fit to the stratigraphic rrcord. ‘1.0 isolate thr extinct taxa rcsponsihle for the lattcr c,lassification, thr data wrrr succcssi~elypartitioned with each phylogenetic analysis, and wc coneluded that: (1) the ingroup, not the outgroup, fossils were important; (2) synapsid, not reptile, fossils wcrc pivotal; (3) certain syiiapsid fossils, not the rarliest or latrst, were responsible. ‘Ihr critical nature of thr syiiapsid lossils sremcd to lir in the particular comhinatioti of primitive arid derivrd c.haracter states they exhibited. -
Skeletal System
AccessScience from McGraw-Hill Education Page 1 of 22 www.accessscience.com Skeletal system Contributed by: Mike Bennett Publication year: 2014 The supporting tissues of animals which often serve to protect the body, or parts of it, and play an important role in the animal’s physiology. Skeletons can be divided into two main types based on the relative position of the skeletal tissues. When these tissues are located external to the soft parts, the animal is said to have an exoskeleton. If they occur deep within the body, they form an endoskeleton. All vertebrate animals possess an endoskeleton, but most also have components that are exoskeletal in origin. Invertebrate skeletons, however, show far more variation in position, morphology, and materials used to construct them. Exoskeletons Many of the invertebrate phyla contain species that have a hard exoskeleton, for example, corals (Cnidaria); limpets, snails, and Nautilus (Mollusca); and scorpions, crabs, insects, and millipedes (Arthropoda). However, these exoskeletons have different physical properties and morphologies. The form that each skeletal system takes presumably represents the optimal configuration for survival. See See also: ARTHROPODA ; MOLLUSCA ; ZOOPLANKTON . Calcium carbonate is the commonly found inorganic material in invertebrate hard exoskeletons. The stony corals have exoskeletons made entirely of calcium carbonate, which protect the polyps from the effects of the physical environment and the attention of most predators. Calcium carbonate also provides a substrate for attachment, allowing the coral colony to grow. However, it is unusual to find calcium carbonate as the sole component of the skeleton. It normally occurs in conjunction with organic material, in the form of tanned proteins, as in the hard shell material characteristic of many mollusks. -
Origin and Phylogenetic Interrelationships of Teleosts Honoring Gloria Arratia
Origin and Phylogenetic Interrelationships of Teleosts Honoring Gloria Arratia Joseph S. Nelson, Hans-Peter Schultze & Mark V. H. Wilson (editors) TELEOSTEOMORPHA TELEOSTEI TELEOCEPHALA s. str. Leptolepis Pholidophorus † Lepisosteus Amia †? †? † †Varasichthyidae †Ichthyodectiformes Elopidae More advanced teleosts crown- group apomorphy-based group stem-based group Verlag Dr. Friedrich Pfeil • München Contents Preface ................................................................................................................................................................ 7 Acknowledgments ........................................................................................................................................... 9 Gloria Arratia’s contribution to our understanding of lower teleostean phylogeny and classifi cation – Joseph S. Nelson ....................................................................................... 11 The case for pycnodont fi shes as the fossil sister-group of teleosts – J. Ralph Nursall ...................... 37 Phylogeny of teleosts based on mitochondrial genome sequences – Richard E. Broughton ............. 61 Occipito-vertebral fusion in actinopterygians: conjecture, myth and reality. Part 1: Non-teleosts – Ralf Britz and G. David Johnson ................................................................................................................... 77 Occipito-vertebral fusion in actinopterygians: conjecture, myth and reality. Part 2: Teleosts – G. David Johnson and Ralf Britz .................................................................................................................. -
MAMMALS the Success of the Mammals: Chewing and Homeostasis
MAMMALS Benton, M. J. (2000) Mammals. Pp. 639-644, in The Oxford Companion to the Earth, P. L. Hancock and B. J. Skinner (eds), Oxford University Press, 1174 pp. Mammals are not a diverse group, and yet they have achieved a dominant position in many ecosystems. There are estimated to be 4000 species of mammals alive today, a low number compared to the insects or flowering plants, and indeed only two-thirds of the current diversity of reptiles. The success of the mammals is measured rather in their wide adaptability, and by the sheer abundance of some species, such as humans and rats. Class Mammalia is divided into three uneQual groups, the Subclasses Monotremata, Marsupialia (or Metatheria), and Placentalia (or Eutheria). The monotremes, the duck- billed platypus and the echidnas of Australasia, are characterized by the fact that they lay eggs, the retention of a primitive reptilian character. Marsupials, such as the opossums of the Americas and the kangaroos, koalas, and wombats of Australasia, generally give birth to tiny immature young which then complete their development in a pouch. The placental mammals, by far the largest group, and consisting of all other mammals from mice to elephants, aardvarks to zebras, and bats to whales, give birth to well-developed young which have been nourished by means of a placenta in the maternal womb. The success of the mammals: chewing and homeostasis It is impossible to point to a single feature of mammals that can explain their great success. Mammals are distinguished from their reptilian forebears by a number of anatomical and physiological characters, and some of these appear to have led to the great adaptability of the group. -
Mammalogy Lecture 2 - Origin of Mammals Introduction to the Geologic Time Scale
Mammalogy Lecture 2 - Origin of Mammals Introduction to the Geologic Time Scale. We’ll begin in the Carboniferous (Mississippian), ~ 363 MYA. I. There are three major living (extant) groups of mammals A. Monotremes – egg-laying mammals (echidna) B. Metatherians – marsupial mammals (kangaroo) C. Eutherians – Placental mammals (pangolin) These are related by the following evolutionary tree or phylogeny Monotremes Metatherians (Marsupials) Eutherians (Placentals) Node - Divergence Event Branch - Common Ancestor Marsupials and placentals share an ancestor not shared by monotremes. II. A. In order to understand the origin of mammals, we have to look farther back, ~360 MYA, and look at relationships among tetrapod vertebrates. Amphibians Mammals Squamates Turtles Crocodylians Dinosaur9I Birds Dinosaur9II Synapsids Stem9Amniotes Amnion Evolution9of9Limbs We can mark evolutionary changes along this phylogeny; the evolution of limbs, the evolution of the amnion, etc. It’s this lineage labeled Synapsida that we’ll examine in order to understand the origin of mammals. We need to understand the situation just prior to this in the “stem amniotes” (a.k.a. stem reptiles), the ancestors to mammals, birds, turtles, and other reptiles. Stem Amniotes. B. In the Carboniferous, ca. 350 MYBP, the stem amniotes evolved, and the synapsid lineage diverged from these 30 MY later 320 MYA, and it’s this lineage that will eventually lead the modern mammals. Synapsid - “together arch” describes a skull condition that is unique to this lineage. The word “synapsid” is also used to refer to the group of organisms that exhibit this condition. Stem amniotes were anapsid; they had no temporal fenestra. The temporal region (temple) is a solid shield of bone. -
The Oldest Specialized Tetrapod Herbivore: a New Eupelycosaur from the Permian of New Mexico, USA
Palaeontologia Electronica palaeo-electronica.org The oldest specialized tetrapod herbivore: A new eupelycosaur from the Permian of New Mexico, USA Spencer G. Lucas, Larry F. Rinehart, and Matthew D. Celeskey ABSTRACT Gordodon kraineri is a new genus and species of edaphosaurid eupelycosaur known from an associated skull, lower jaw and incomplete postcranium found in the early Permian Bursum Formation of Otero County, New Mexico, USA. It has a special- ized dental apparatus consisting of large, chisel-like incisors in the front of the jaws separated by a long diastema from relatively short rows of peg-like maxillary and den- tary cheek teeth. The dorsal vertebrae of Gordodon have long neural spines that bear numerous, randomly arranged, small, thorn-like tubercles. The tubercles on long neu- ral spines place Gordodon in the Edaphosauridae, and the dental apparatus and dis- tinctive tubercles on the neural spines distinguish it from the other edaphosaurid genera—Edaphosaurus, Glaucosaurus, Lupeosaurus and Ianthasaurus. Gordodon is the oldest known tetrapod herbivore with a dentary diastema, extending the temporal range of that anatomical feature back 95 million years from the Late Triassic. The den- tal apparatus of Gordodon indicates significantly different modes of ingestion and intra- oral transport of vegetable matter than took place in Edaphosaurus and thus represents a marked increase in disparity among edaphosaurids. There were two very early pathways to tetrapod herbivory in edaphosaurid evolution, one toward general- ized browsing on high-fiber plant items (Edaphosaurus) and the other (Gordodon) toward more specialized browsing, at least some of it likely on higher nutrient, low fiber plant items.