18S Ribosomal RNA and Tetrapod Phylogeny
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Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna. -
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 -
Phylogeny of Basal Tetrapoda
Stuart S. Sumida Biology 342 Phylogeny of Basal Tetrapoda The group of bony fishes that gave rise to land-dwelling vertebrates and their descendants (Tetrapoda, or colloquially, “tetrapods”) was the lobe-finned fishes, or Sarcopterygii. Sarcoptrygii includes coelacanths (which retain one living form, Latimeria), lungfish, and crossopterygians. The transition from sarcopterygian fishes to stem tetrapods proceeded through a series of groups – not all of which are included here. There was no sharp and distinct transition, rather it was a continuum from very tetrapod-like fishes to very fish-like tetrapods. SARCOPTERYGII – THE LOBE-FINNED FISHES Includes •Actinista (including Coelacanths) •Dipnoi (lungfishes) •Crossopterygii Crossopterygians include “tetrapods” – 4- legged land-dwelling vertebrates. The Actinista date back to the Devonian. They have very well developed lobed-fins. There remains one livnig representative of the group, the coelacanth, Latimeria chalumnae. A lungfish The Crossopterygii include numerous representatives, the best known of which include Eusthenopteron (pictured here) and Panderichthyes. Panderichthyids were the most tetrapod-like of the sarcopterygian fishes. Panderichthyes – note the lack of dorsal fine, but retention of tail fin. Coelacanths Lungfish Rhizodontids Eusthenopteron Panderichthyes Tiktaalik Ventastega Acanthostega Ichthyostega Tulerpeton Whatcheeria Pederpes More advanced amphibians Tiktaalik roseae – a lobe-finned fish intermediate between typical sarcopterygians and basal tetrapods. Mid to Late Devonian; 375 million years old. The back end of Tiktaalik’s skull is intermediate between fishes and tetrapods. Tiktaalik is a fish with wrist bones, yet still retaining fin rays. The posture of Tiktaalik’s fin/limb is intermediate between that of fishes an tetrapods. Coelacanths Lungfish Rhizodontids Eusthenopteron Panderichthyes Tiktaalik Ventastega Acanthostega Ichthyostega Tulerpeton Whatcheeria Pederpes More advanced amphibians Reconstructions of the basal tetrapod Ventastega. -
Evolution of the Muscular System in Tetrapod Limbs Tatsuya Hirasawa1* and Shigeru Kuratani1,2
Hirasawa and Kuratani Zoological Letters (2018) 4:27 https://doi.org/10.1186/s40851-018-0110-2 REVIEW Open Access Evolution of the muscular system in tetrapod limbs Tatsuya Hirasawa1* and Shigeru Kuratani1,2 Abstract While skeletal evolution has been extensively studied, the evolution of limb muscles and brachial plexus has received less attention. In this review, we focus on the tempo and mode of evolution of forelimb muscles in the vertebrate history, and on the developmental mechanisms that have affected the evolution of their morphology. Tetrapod limb muscles develop from diffuse migrating cells derived from dermomyotomes, and the limb-innervating nerves lose their segmental patterns to form the brachial plexus distally. Despite such seemingly disorganized developmental processes, limb muscle homology has been highly conserved in tetrapod evolution, with the apparent exception of the mammalian diaphragm. The limb mesenchyme of lateral plate mesoderm likely plays a pivotal role in the subdivision of the myogenic cell population into individual muscles through the formation of interstitial muscle connective tissues. Interactions with tendons and motoneuron axons are involved in the early and late phases of limb muscle morphogenesis, respectively. The mechanism underlying the recurrent generation of limb muscle homology likely resides in these developmental processes, which should be studied from an evolutionary perspective in the future. Keywords: Development, Evolution, Homology, Fossils, Regeneration, Tetrapods Background other morphological characters that may change during The fossil record reveals that the evolutionary rate of growth. Skeletal muscles thus exhibit clear advantages vertebrate morphology has been variable, and morpho- for the integration of paleontology and evolutionary logical deviations and alterations have taken place unevenly developmental biology. -
Tetrapod Phylogeny
© J989 Elsevier Science Publishers B. V. (Biomédical Division) The Hierarchy of Life B. Fernholm, K. Bremer and H. Jörnvall, editors 337 CHAPTER 25 Tetrapod phylogeny JACQUES GAUTHIER', DAVID CANNATELLA^, KEVIN DE QUEIROZ^, ARNOLD G. KLUGE* and TIMOTHY ROWE^ ' Deparlmenl qf Herpelology, California Academy of Sciences, San Francisco, CA 94118, U.S.A., ^Museum of Natural Sciences and Department of Biology, Louisiana State University, Baton Rouge, LA 70803, U.S.A., ^Department of ^oology and Museum of Vertebrate ^oology. University of California, Berkeley, CA 94720, U.S.A., 'Museum of ^oology and Department of Biology, University of Michigan, Ann Arbor, MI 48109, U.S.A. and ^Department of Geological Sciences, University of Texas, Austin, TX 78713, U.S.A. Introduction Early sarcopterygians were aquatic, but from the latter part of the Carboniferous on- ward that group has been dominated by terrestrial forms commonly known as the tet- rapods. Fig. 1 illustrates relationships among extant Tetrápoda [1-4J. As the clado- grams in Figs. 2•20 demonstrate, however, extant groups represent only a small part of the taxonomic and morphologic diversity of Tetrápoda. We hope to convey some appreciation for the broad outlines of tetrapod evolution during its 300+ million year history from late Mississippian to Recent times. In doing so, we summarize trees de- rived from the distribution of over 972 characters among 83 terminal taxa of Tetrápo- da. More than 90% of the terminal taxa we discuss are extinct, but all of the subter- minal taxa are represented in the extant biota. This enables us to emphasize the origins of living tetrapod groups while giving due consideration to the diversity and antiquity of the clades of which they are a part. -
Objectives Tetrapod Characteristics
1/22/2018 Becky Hardman University of Tennessee College of Veterinary Medicine [email protected] 416 360 300 250 200 146 65 Objectives Define Tetrapod/Amphibian Origin of Tetrapods Split of Amphibians Modern Amphibians Extant Families Simplification Tetrapod Characteristics Four Limbs Tetra= Four; Pod=Foot Some lost or vestigial “One bonetwo boneslittle blobsfingers/toes”- Neil Shubin Some lost or vestigial Includes all non-fish vertebrates 1 1/22/2018 Amphibian Characteristics “Tetrapod vertebrates that pass through a larval state and undergo metamorphosis into terrestrial adults.” • Anamniotes • Eggs need moist environment • Larval; metamorphosis • Permeable Skin • Cutaneous respiration • Two Gland Types • Mucous • Poison • Pedicellate Teeth • Amphibian papillae/Opercular bone • Can Hear Vibrations • Fat Bodies • Green Rods- fxn unknown • Singular Sacrum • Lost in caecilians Amphibian Characteristics As a Fossil… Articular surface of axis convex Exoccipital Bone articulates with dermal roofing Hand (Manus) 4 digits Foot (Pes) 5 digits Some Secondarily Lost Important to determine for fossil realtionships 2 1/22/2018 Phylogenetic Trees Phylogenetic Trees 3 1/22/2018 Darwin’s Tree Geologic Time Scale 416 360 300 250 200 146 65 Devonian: Age of Fishes Lobed-Finned Fishes Lungfishes; Coelacanths Tetrapodomorpha Panderichthyids Ichthyostega, Acanthostega Tetrapods 4 1/22/2018 416 360 300 250 200 146 65 Devonian: Fish to Tetrapod Panderichthyids 380 mya Predators in shallow water Eyes on top of head Lung and Gills -
Systems Biology Approach to the Origin of the Tetrapod Limb Koh
Systems biology approach to the origin of the tetrapod limb Koh Onimaru1*, Luciano Marcon2* 1. Laboratory for Phyloinformatics, RIKEN Center for Biosystems Dynamics Research (BDR), 2-1 Hirosawa, Wako city, Saitama prefecture, 351-0198, Japan. E-mail: [email protected] 2. Andalusian Centre for Developmental Biology (CABD), Universidad Pablo de Olavide, Carretera de Utrera km1, 41013, Sevilla, Spain. E-mail: [email protected] *Corresponding author July 2019 Abstract It is still not understood how similar genomic sequences have generated diverse and spectacular forms during evolution. The difficulty to bridge phenotypes and genotypes stems from the complexity of multicellular systems, where thousands of genes and cells interact with each other providing developmental non-linearity. To understand how diverse morphologies have evolved, it is essential to find ways to handle such complex systems. Here, we review the fin-to-limb transition as a case study for the evolution of multicellular systems. We first describe the historical perspective of comparative studies between fins and limbs. Second, we introduce our approach that combines mechanistic theory, computational modeling, and in vivo experiments to provide a mechanical explanation for the morphological difference between fish fins and tetrapod limbs. This approach helps resolve a long-standing debate about anatomical homology between the skeletal elements of fins and limbs. We will conclude by proposing that due to the counter- intuitive dynamics of gene interactions, integrative approaches that combine computer modeling, theory and experiments are essential to understand the evolution of multicellular organisms. Introduction Multi-cellular organisms have evolved a remarkable diversity of their forms. In the last decades, thanks to the advance of DNA sequencing technologies, the genome sequence data of various species have become available. -
The Origin of Tetrapods Topic 4: the Origin of Tetrapods
8/19/2013 Topic 4: The Origin of Tetrapods Topic 4: The Origin of Tetrapods Next two lectures will deal with: What is the geological time scale and why is it important? Origin of Tetrapods, transition from Where do herps fit in the vertebrate water to land. phylogeny? What are the evolutionary origins of Origin of Amniotes, transition to dry tetrapods? habitats. What changes were involved in the transition from water to land? The geological time scale The geological time scale Organizes the history of the earth Eon Era MYA Precambrian accounts for Cenozoic 0-65 ~88% of Earth Based on geological and biological/fossil criteria history Phanerozoic Mesozoic 65-245 We will Allows us to consider “________________” concentrate on Phanerozoic Paleozoic 245-570 Time scale over which geological and ___________________ phenomena occur st Proterozoic 570-2500 1 multicellular organisms Organized into hierarchical ________, ________, Precambrian Archaen 2500-3800 1st unicellular organisms ______________, and ______________ Age of oldest rocks Hadean 3800-4600 The Paleozoic Era The Mesozoic Era Period MYA Events Period MYA Events - Mass extinction at end of 1st _________________ Permian 245-286 Cretaceous Cretaceous 65-144 - 1st modern Squamata 1st reptiles, amphibians Carboniferous 286-320 specialize st st Devonian 360-408 1 amphibians - 1 Urodela, Anura - 1st Rynchocephalia st Jurassic 144-208 Silurian 408-438 1 jawed fishes - High reptile diversity - 1st birds 1st jawless fishes & st Ordovician 438-505 land plants -1 Angiosperms, dinosaurs, mammals 1st vertebrates Cambrian 505-570 Triassic 208-245 - 1st Testudines, ___________ 1 8/19/2013 The Cenozoic Era What are stem and crown groups? Period Epoch MYA Comments _________________ – smallest Modern humans Holocene Recent monophyletic group to contain the last common ancestor of all extant members Quanternary Evolution of humans Pleistocene 0.01-1.5 of a taxon 1st hominines Pliocene 1.5-5 _________________ – contains crown Miocene 5-24 group plus closely related extinct taxa. -
Chapter 16 MORPHOLOGICAL CONSTRAINTS on TETRAPOD
Chapter 16 MORPHOLOGICAL CONSTRAINTS ON TETRAPOD FEEDING MECHANISMS: WHY WERE THERE NO SUSPENSION-FEEDING MARINE REPTILES? RACHEL COLLIN and CHRISTINE M. JANIS INTRODUCTION Although tetrapods are primarily designed for a terrestrial existence, tetrapod history is rife with secondarily aquatic forms. Semiaquatic taxa are usually freshwater, and more fully aquatic taxa are usually marine. With the reinvasion of the aquatic environment, modification of the tetrapod body plan originally designed for feeding and locomotion on land would be necessary to accommodate these functions in the very different medium of water. Both the diversity of living marine tetrapods and the additional diversity afforded by the fossil record demonstrate numerous examples of parallelisms and convergences in the various lineages (Massare, 1987, 1988; Carroll, 1985). Yet aquatic suspension feeding, common among fish, is conspicuously absent in marine nonmammalian tetrapods: baleen whales appear to be the only group that has adopted this form of feeding in past or present marine environments. The notion of morphological or phylogenetic constraint is often invoked when evolutionary patterns differ between groups of organisms (McKitrick, 1993; Carroll, 1985). In this chapter we review the morphological requirements for suspension feeding, and address the issue of whether differences in design between mammals and other tetrapods have resulted in morphological constraints that can explain the apparent absence of suspension-feeding marine reptiles. During the Paleozoic, when oceanic productivity is thought to have been comparatively low (Bambach, 1993 and personal communication), marine tetrapods were rare. Those tetrapods that did venture into the water, such as the Permian Ancient Marine Reptiles 451 Copyright © 1997 by Academic Press All rights of reproduction in any form reserved. -
Massive Increase in Visual Range Preceded the Origin of Terrestrial
Massive increase in visual range preceded the origin PNAS PLUS of terrestrial vertebrates Malcolm A. MacIvera,b,c,1, Lars Schmitzd,e,1, Ugurcan Muganc, Todd D. Murpheyb, and Curtis D. Mobleyf aThe Neuroscience and Robotics Laboratory, Northwestern University, Evanston, IL 60208; bDepartment of Mechanical Engineering, Northwestern University, Evanston, IL 60208; cDepartment of Biomedical Engineering, Northwestern University, Evanston, IL 60208; dW. M. Keck Science Department, Claremont McKenna, Pitzer, and Scripps Colleges, Claremont, CA 91711; eDinosaur Institute, Natural History Museum of Los Angeles County, Los Angeles, CA 90007; and fSection for Optical Oceanography, Sequoia Scientific, Inc., Bellevue, WA 98005 Edited by Neil H. Shubin, The University of Chicago, Chicago, IL, and approved January 24, 2017 (received for review September 17, 2016) The evolution of terrestrial vertebrates, starting around 385 mil- Large Eyes Appeared Before Terrestriality lion years ago, is an iconic moment in evolution that brings to Fig. 1 shows the sequence of steps of our study across its par- mind images of fish transforming into four-legged animals. Here, ent disciplines. We start with the assembly of a time-calibrated we show that this radical change in body shape was preceded by phylogeny of 59 tetrapodomorph taxa that bracket the water– an equally dramatic change in sensory abilities akin to transition- land transition and have measurable skull and eye socket lengths ing from seeing over short distances in a dense fog to seeing over (Materials and Methods). We generated a set of 1,000 evolu- long distances on a clear day. Measurements of eye sockets and tionary trees to account for uncertainties in phylogeny. -
Evolution, Homology, and Development of Tetrapod Limb Muscles
diversity Review Evolution, Homology, and Development of Tetrapod Limb Muscles Julia L. Molnar 1,* and Rui Diogo 2 1 Department of Anatomy, New York Institute of Technology, College of Osteopathic Medicine, Northern Boulevard, Old Westbury, NY 11568, USA 2 Department of Anatomy, Howard University College of Medicine, 520 W St NW, Washington, DC 20059, USA; [email protected] * Correspondence: [email protected] Abstract: Since the early 1900s, researchers have attempted to unravel the origin and evolution of tetrapod limb muscles using a combination of comparative anatomy, phylogeny, and development. The methods for reconstructing soft tissues in extinct animals have been refined over time as our abil- ity to determine muscle homology and phylogenetic relationships between tetrapods has improved. Since many muscles do not leave osteological correlates, muscle reconstruction in extinct animals is largely based on anatomy and development in extant animals. While muscle anatomy in extant tetrapods is quite conservative, the homologies of certain muscles between taxonomic groups are still uncertain. Comparative developmental studies can help to resolve these controversies, as well as revealing general patterns of muscle morphogenesis across tetrapod groups. We review the methods, results, and controversies in the muscle reconstructions of early members of the amniote, mammalian, and lissamphibian lineages, including recent attempts to reconstruct limb muscles in members of the tetrapod stem group. We also review the contribution of recent comparative developmental studies toward understanding the evolution of tetrapod limb muscles, including morphogenic gradients, Citation: Molnar, J.L.; Diogo, R. the origin of paired fins, and the evolution of morphological complexity. Finally, we discuss the role Evolution, Homology, and of broad, comparative myological studies as part of an integrative research program on vertebrate Development of Tetrapod Limb evolutionary biology. -
Chapter 27 the "Tetrapod"
CHAPTER 27 THE "TETRAPOD" by P.DA.NEL '^Prdsident d 'Honneur" of SOGREAH and L. GRES10U Head of the Maritime Research and Design Department at SOGREAH The Tetrapod was invented twelve years ago and the first breakwater with a Tetrapod protection was built eleven years ago. It is felt that a review of the results since obtained with these ar- tificial blocks may be of some interest, preferably in the form of an ob- jective practical examination of the behaviour of Tetrapod-protected structures during the past few years, and of the way in which they have stood up to bad wheather during the period. First, however, a brief des- cription will be given of the development of the Tetrapod and the Tetrapod technique. Most breakwaters are of the rubble-mound type, because of the very good hydraulic properties of this type of design ; the seaward slope, roughness and "porosity" of their facings are generally such as to ensure the gradual destruction of wave energy, reduce wave overtopping and re- flection and minimize toe erosion risks. Unfortunately, however, rubble mound breakwater designs vary conside- rably, and some of them do not successfully combine all these essential features. Following an examination of a large number of designs of this type, therefore, it was decided to try, by systematic research, to deter- mine ways and means of improving the properties of rubble mound breakwa- ters, especially in respect of the following : a) Hydraulic properties : (i) Stability of armour components. (ii) Strength of the structure as a whole, (in) Reduced overtopping by waves.