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The Cambrian Explosion: a Big Bang in the Evolution of Animals
The Cambrian Explosion A Big Bang in the Evolution of Animals Very suddenly, and at about the same horizon the world over, life showed up in the rocks with a bang. For most of Earth’s early history, there simply was no fossil record. Only recently have we come to discover otherwise: Life is virtually as old as the planet itself, and even the most ancient sedimentary rocks have yielded fossilized remains of primitive forms of life. NILES ELDREDGE, LIFE PULSE, EPISODES FROM THE STORY OF THE FOSSIL RECORD The Cambrian Explosion: A Big Bang in the Evolution of Animals Our home planet coalesced into a sphere about four-and-a-half-billion years ago, acquired water and carbon about four billion years ago, and less than a billion years later, according to microscopic fossils, organic cells began to show up in that inert matter. Single-celled life had begun. Single cells dominated life on the planet for billions of years before multicellular animals appeared. Fossils from 635,000 million years ago reveal fats that today are only produced by sponges. These biomarkers may be the earliest evidence of multi-cellular animals. Soon after we can see the shadowy impressions of more complex fans and jellies and things with no names that show that animal life was in an experimental phase (called the Ediacran period). Then suddenly, in the relatively short span of about twenty million years (given the usual pace of geologic time), life exploded in a radiation of abundance and diversity that contained the body plans of almost all the animals we know today. -
J32 the Importance of the Burgess Shale < Soft Bodied Fauna >
580 Chapter j PALEOCONTINENTS The Present is the Key to the Past: HUGH RANCE j32 The importance of the Burgess shale < soft bodied fauna > Only about 33 animal body plans are presently [sic] being used on this planet (Margulis and Schwartz, 1988). —Scott F. Gilbert, Developmental Biology, 1991.1 Almost all animal phyla known today were already present by 505 million years ago— the age of the Burgess shale, Middle Cambrian marine sediments, discovered at the Kicking Horse rim, British Columbia, in 1909 by Charles Doolittle Walcott, that provide a unique window on life without hard parts that had continued to exist shortly after the time of the Cambrian explosion (see Topic j34).2 Legend has it that Walcott, then secretary of the Smithsonian Institution, vacationing near Field, British Columbia, was thrown from a horse carrying him, when it tripped on, and split open a stray fallen slab of shale. Walcott, with his face literally rubbed in it, saw strange, but not hallucinational, forms crisply etched in black against the blue-black bedding surface of the shale: a bonanza of fossils of sea creatures without mineralized shells or backbones. Many are preserved whole; including those with articulated organic (biodegradable) exoskeletons. Details of even their soft body parts can be seen (best using PTM)3 as silvery films (formed of phyllosilicates on a coating of kerogenized carbon) that commonly outline even the most delicate structures on the fossilized animal.4 The Burgess shale is part of the Stephen Formation of greenish shales and thin-bedded limestones, which is a marine-offlap deposit between the thick, massive, carbonates of the overlying Eldon formation, and the underlying Cathedral formation.6 As referenced in the Geological Atlas of the Western Canada Sedimentary Basin - Chapter 8, the Stephen Formation has been “informally divided into a normal, ‘thin Stephen’ on the platform areas and a ‘thick Stephen’ west of the Cathedral Escarpment. -
Hallucigenia
www.palaeontologyonline.com |Page 1 Title: Fossil Focus - Hallucigenia and the evolution of animal body plans Author(s): Martin Smith *1 Volume: 7 Article: 5 Page(s): 1-9 Published Date: 01/05/2017 PermaLink: http://www.palaeontologyonline.com/articles/2017/fossil_focus_hallucigenia/ IMPORTANT Your use of the P alaeontology [online] ar chive ind icates y our accep tance of P alaeontology [online]'s T erms and Conditions of Use, a vailable a t http://www.palaeontologyonline.com/site-information/terms-and-conditions/. COPYRIGHT Palaeontology [online] (w ww.palaeontologyonline.com) publishes all w ork, unless other wise s tated, under the Creative Commons A ttribution 3.0 Unport ed (CC BY 3.0) license. This license le ts other s dis tribute, r emix, tw eak, and build upon the published w ork, e ven commercially, as long as the y cr edit P alaeontology[online] f or the original cr eation. This is the mo st accommodating of licenses of fered b y Cr eative Commons and is r ecommended f or ma ximum dissemina tion of published ma terial. Further de tails ar e a vailable a t h ttp://www.palaeontologyonline.com/site-information/copyright/. CITATION OF ARTICLE Please cit e the f ollowing published w ork as: Smith, Martin. 2017. F ossil F ocus - Hallucigenia and the e volution of animal body plans. P alaeontology Online, Volume 5, Article 5, 1-9. Published by: Palaeontology [online] www.palaeontologyonline.com |Page 2 Fossil Focus: Hallucigenia and the evolution of animal body plans by Martin Smith *1 Introduction: Five hundred and fifty million years ago, few (if any) organisms on Earth were much more complex than seaweed. -
The Diapsid Origin of Turtles
THE DIAPSID ORIGIN OF TURTLES Mrs. Basawarajeshwari Indur Dept of Zoology, Sharnbasva University, Kalaburagi. A B S T R A C T The origin of turtles has been a persistent unresolved problem involving unsettled questions in embryology, morphology, and paleontology. New fossil taxa from the early Late Triassic of China (Odontochelys) and the Late Middle Triassic of Germany (Pappochelys) now add to the understanding of (i) the evolutionary origin of the turtle shell, (ii) the ancestral structural pattern of the turtle skull, and (iii) the phylogenetic position of Testudines. As has long been postulated on the basis of molecular data, turtles evolved from diapsid reptiles and are more closely related to extant diapsids than to parareptiles, which had been suggested as stem group by some paleontologists. The turtle cranium with its secondarily closed temporal region represents a derived rather than a primitive condition and the plastron partially evolved through the fusion of gastralia Key word –Carapace, Plastron, Reptiles, Turtle origins I.INTRODUCTION The origin and early evolution of turtles has been a longstanding problem in vertebrate morphology and phylogeny (Rieppel and Reisz, 1999). The unique composition of the turtle shell as well as the closed (anapsid) architecture of the skull had been controversially debated issues for more than a century. The lack of fossils documenting plausible stem taxa predating the Late Triassic had long formed a major obstacle in this context. Until recently, the geologically oldest and most primitive stem turtles reached back only to the later part of the Late Triassic, whereas it was long thought that the turtle clade likely diverged from other reptiles already during the Permian. -
Hallucigenia's Onychophoran-Like Claws
LETTER doi:10.1038/nature13576 Hallucigenia’s onychophoran-like claws and the case for Tactopoda Martin R. Smith1 & Javier Ortega-Herna´ndez1 The Palaeozoic form-taxon Lobopodia encompasses a diverse range of Onychophorans lack armature sclerites, but possess two types of ap- soft-bodied‘leggedworms’ known from exceptionalfossil deposits1–9. pendicular sclerite: paired terminal claws in the walking legs, and den- Although lobopodians occupy a deep phylogenetic position within ticulate jaws within the mouth cavity9,23.AsinH. sparsa, claws in E. Panarthropoda, a shortage of derived characters obscures their evo- kanangrensis exhibit a broad base that narrows to a smooth conical point lutionary relationships with extant phyla (Onychophora, Tardigrada (Fig. 1e–h). Each terminal clawsubtends anangle of130u and comprises and Euarthropoda)2,3,5,10–15. Here we describe a complex feature in two to three constituent elements (Fig. 1e–h). Each smaller element pre- the terminal claws of the mid-Cambrian lobopodian Hallucigenia cisely fills the basal fossa of its container, from which it can be extracted sparsa—their construction from a stack of constituent elements— with careful manipulation (Fig. 1e, g, h and Extended Data Fig. 3a–g). and demonstrate that equivalent elements make up the jaws and claws Each constituent element has a similar morphology and surface orna- of extant Onychophora. A cladistic analysis, informed by develop- ment (Extended Data Fig. 3a–d), even in an abnormal claw where mental data on panarthropod head segmentation, indicates that the element tips are flat instead of pointed (Extended Data Fig. 3h). The stacked sclerite components in these two taxa are homologous— proximal bases of the innermost constituent elements are associated with resolving hallucigeniid lobopodians as stem-group onychophorans. -
Hallucigenia's Head and the Pharyngeal Armature Of
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Apollo 1 Hallucigenia’s head and the pharyngeal armature of early ecdysozoans 2 Martin R. Smith1 and Jean-Bernard Caron2,3 3 1Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK. 4 <[email protected]> 5 2Department of Natural History (Palaeobiology Section), Royal Ontario Museum, Toronto, 6 ON M5S 2C6, Canada. <[email protected]> 7 3Department of Ecology and Evolutionary Biology and Earth Sciences, University of 8 Toronto, Toronto, ON M5S 3B2, Canada. 9 Keywords: Hallucigenia, Ecdysozoa, Panarthropoda, Onychophora, Lobopodia, Burgess 10 Shale, Cambrian explosion. 11 The molecularly-defined clade Ecdysozoa1 comprises the panarthropods 12 (Euarthropoda, Onychophora, and Tardigrada) and the cycloneuralian worms 13 (Nematoda, Nematomorpha, Priapulida, Loricifera, and Kinorhyncha). These 14 disparate phyla are united by their means of moulting, but otherwise share few 15 morphological characters – none of which has a meaningful fossilization potential. As 16 such, the early evolutionary history of the group as a whole is largely uncharted. Here 17 we redescribe the 508 million year old stem-group onychophoran Hallucigenia sparsa2–6 18 from the mid-Cambrian Burgess Shale. We document an elongate head with a pair of 19 simple eyes, a terminal buccal chamber containing a radial array of sclerotized 20 elements, and a differentiated foregut that is lined with acicular teeth. The radial 21 elements and pharyngeal teeth resemble the sclerotized circumoral elements and 22 pharyngeal teeth expressed in tardigrades7–9, stem-group euarthropods10–12, and 23 cycloneuralian worms13. Phylogenetic results indicate that equivalent structures 24 characterized the ancestral panarthropod and, seemingly, the ancestral ecdysozoan – 25 demonstrating the deep homology of panarthropod and cycloneuralian mouthparts, and 26 providing an anatomical synapomorphy for the ecdysozoan supergroup. -
The Early History of the Metazoa—A Paleontologist's Viewpoint
ISSN 20790864, Biology Bulletin Reviews, 2015, Vol. 5, No. 5, pp. 415–461. © Pleiades Publishing, Ltd., 2015. Original Russian Text © A.Yu. Zhuravlev, 2014, published in Zhurnal Obshchei Biologii, 2014, Vol. 75, No. 6, pp. 411–465. The Early History of the Metazoa—a Paleontologist’s Viewpoint A. Yu. Zhuravlev Geological Institute, Russian Academy of Sciences, per. Pyzhevsky 7, Moscow, 7119017 Russia email: [email protected] Received January 21, 2014 Abstract—Successful molecular biology, which led to the revision of fundamental views on the relationships and evolutionary pathways of major groups (“phyla”) of multicellular animals, has been much more appre ciated by paleontologists than by zoologists. This is not surprising, because it is the fossil record that provides evidence for the hypotheses of molecular biology. The fossil record suggests that the different “phyla” now united in the Ecdysozoa, which comprises arthropods, onychophorans, tardigrades, priapulids, and nemato morphs, include a number of transitional forms that became extinct in the early Palaeozoic. The morphology of these organisms agrees entirely with that of the hypothetical ancestral forms reconstructed based on onto genetic studies. No intermediates, even tentative ones, between arthropods and annelids are found in the fos sil record. The study of the earliest Deuterostomia, the only branch of the Bilateria agreed on by all biological disciplines, gives insight into their early evolutionary history, suggesting the existence of motile bilaterally symmetrical forms at the dawn of chordates, hemichordates, and echinoderms. Interpretation of the early history of the Lophotrochozoa is even more difficult because, in contrast to other bilaterians, their oldest fos sils are preserved only as mineralized skeletons. -
A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes
ORIGINAL RESEARCH published: 02 November 2017 doi: 10.3389/feart.2017.00088 A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes Michel Laurin 1* and Graciela H. Piñeiro 2 1 CR2P (UMR 7207) Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (Centre National de la Recherche Scientifique/MNHN/UPMC, Sorbonne Universités), Paris, France, 2 Departamento de Paleontología, Facultad de Ciencias, University of the Republic, Montevideo, Uruguay We reassess the phylogenetic position of mesosaurs by using a data matrix that is updated and slightly expanded from a matrix that the first author published in 1995 with his former thesis advisor. The revised matrix, which incorporates anatomical information published in the last 20 years and observations on several mesosaur specimens (mostly from Uruguay) includes 17 terminal taxa and 129 characters (four more taxa and five more characters than the original matrix from 1995). The new matrix also differs by incorporating more ordered characters (all morphoclines were ordered). Parsimony Edited by: analyses in PAUP 4 using the branch and bound algorithm show that the new matrix Holly Woodward, Oklahoma State University, supports a position of mesosaurs at the very base of Sauropsida, as suggested by the United States first author in 1995. The exclusion of mesosaurs from a less inclusive clade of sauropsids Reviewed by: is supported by a Bremer (Decay) index of 4 and a bootstrap frequency of 66%, both of Michael S. Lee, which suggest that this result is moderately robust. The most parsimonious trees include South Australian Museum, Australia Juliana Sterli, some unexpected results, such as placing the anapsid reptile Paleothyris near the base of Consejo Nacional de Investigaciones diapsids, and all of parareptiles as the sister-group of younginiforms (the most crownward Científicas y Técnicas (CONICET), Argentina diapsids included in the analyses). -
Patterns of Morphological Evolution in the Skull of Turtles: Contributions from Digital Paleontology, Neuroanatomy and Biomechanics
Patterns of morphological evolution in the skull of turtles: contributions from digital paleontology, neuroanatomy and biomechanics Dissertation der Mathematisch-Naturwissenschaftlichen Fakultät der Eberhard Karls Universität Tübingen zur Erlangung des Grades eines Doktors der Naturwissenschaften (Dr. rer. nat.) vorgelegt von M.Sc. Gabriel S. Ferreira aus Santa Bárbara d’Oeste/ Brasilien Tübingen 2019 Gedruckt mit Genehmigung der Mathematisch-Naturwissenschaftlichen Fakultät der Eberhard Karls Universität Tübingen. Tag der mündlichen Qualifikation: 27.05.2019 Dekan: Prof. Dr. Wolfgang Rosenstiel 1. Berichterstatter: Prof. Dr. Madelaine Böhme 2. Berichterstatter: Prof. Dr. Max C. Langer In nature we never see anything isolated, but everything in connection with something else which is before it, beside it, under it and over it Johann Wolfgang von Goethe Doubt is not a pleasant condition, but certainty is absurd François Voltaire i Ferreira – Patterns of morphological evolution in the skull of turtles Acknowledgements I am very grateful to my supervisor Max Langer, who offered me a space in his lab for the past ten years and immensily contributed to shape my career path until now. Max not only helped me think through paleo-problems, but also about career options and personal matters, always being present and giving support when I needed. I also thank my PhD co- supervisor in Tübingen, Prof. Dr. Madelaine Böhme, who accepted and welcomed me at the Senckenberg Institute and Universität Tübingen for a whole year, offering me not only a space to work, but also interesting discussions on various subjects. I am very grateful to my “unofficial” co-supervisor, PD Dr. Ingmar Werneburg, who has supported me from the beginning of my PhD, helping already when I was writing my doctoral research project and now, during this agitated last year. -
Phylogeny of Hallucigenia
Phylogeny of Hallucigenia By Annette Hilton December 4th, 2014 Invertebrate Paleontology Cover artwork from: http://people.ds.cam.ac.uk/ms609/ 2 Abstract Hallucigenia is an extinct genus from the lower-middle Cambrian. A small worm-like organism with dorsal spines, Hallucigenia is rare in fossil history, and its identity and morphology have often been confounded. Since its original discovery in the Burgess Shale by Walcott, Hallucigenia has since become an iconic fossil. Its greater systematics and place in the phylogenetic tree is controversial and not completely understood. New evidence and the discovery of additional species of Hallucigenia have contributed much to the understanding of this genus and its broader relations in classification and evolutionary history. Introduction Hallucigenia is a genus that encompasses three known species that lived during the Cambrian period—Hallucigenia sparsa, Hallucigenia fortis, and Hallucigenia hongmeia (Ma et al., 2012). Hallucigenia’s taxonomy in figure 1. Kingdom Animalia Phylum Onychophora (Lobopodia) Class Xenusia Order Scleronychophora Genus Hallucigenia Figure 1. Taxonomy of Hallucigenia species. Collectively, all Hallucigenia specimens are rare, with a portion of specimens incomplete. The understanding of Hallucigenia and its life mode has been confounded since the 3 original discovery of H. sparsa, but subsequent species discoveries has shed light on some of its mysteries (Conway Morris, 1998). Even more information concerning Hallucigenia is currently being unearthed—its classification into the phylum Onychophora and wider relations to other invertebrate groups like Arthropoda and the poorly understood Lobopodian group (Campbell et al., 2011). Hallucigenia, an iconic fossil of the Burgess Shale, demonstrates the well-known diversity of the Cambrian period, its morphology providing increasing numbers of clues to its connection into the greater systematic system. -
THE ORIGIN of the TURTLE BODY PLAN: EVIDENCE from FOSSILS and EMBRYOS by RAINER R
[Palaeontology, 2019, pp. 1–19] REVIEW ARTICLE THE ORIGIN OF THE TURTLE BODY PLAN: EVIDENCE FROM FOSSILS AND EMBRYOS by RAINER R. SCHOCH1 and HANS-DIETER SUES2 1Staatliches Museum fur€ Naturkunde, Rosenstein 1, D-70191, Stuttgart, Germany; [email protected] 2Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560, USA; [email protected] Typescript received 4 June 2019; accepted in revised form 23 September 2019 Abstract: The origin of the unique body plan of turtles plan within a phylogenetic framework and evaluate it in light has long been one of the most intriguing mysteries in evolu- of the ontogenetic development of the shell in extant turtles. tionary morphology. Discoveries of several new stem-turtles, The fossil record demonstrates that the evolution of the tur- together with insights from recent studies on the develop- tle shell took place over millions of years and involved a ment of the shell in extant turtles, have provided crucial new number of steps. information concerning this subject. It is now possible to develop a comprehensive scenario for the sequence of evolu- Key words: turtle, carapace, plastron, development, phy- tionary changes leading to the formation of the turtle body logeny. T URTLES are unique among known extant and extinct tet- name Testudines to the clade comprising the most recent rapods, including other forms with armour formed by common ancestor of Chelonia mydas and Chelus fimbria- bony plates (e.g. armadillos), in their possession of a tus (matamata) and all descendants of that ancestor. bony shell that incorporates much of the vertebral col- The origin of the turtle body plan has long been one of umn and encases the trunk (Zangerl 1969; Fig. -
Development of the Turtle Plastron, the Order-Defining Skeletal Structure
Development of the turtle plastron, the order-defining skeletal structure Ritva Ricea,1, Aki Kallonenb, Judith Cebra-Thomasc,d, and Scott F. Gilberta,c,1 aDevelopmental Biology, Institute of Biotechnology, University of Helsinki, Helsinki 00014, Finland; bDepartment of Physics, University of Helsinki, Helsinki 00014, Finland; cDepartment of Biology, Swarthmore College, Swarthmore, PA 19081; and dDepartment of Biology, Millersville University, Millersville, PA 17551 Edited by Clifford J. Tabin, Harvard Medical School, Boston, MA, and approved March 30, 2016 (received for review January 19, 2016) The dorsal and ventral aspects of the turtle shell, the carapace and the fontanel at the midline of the plastron. Moreover, processes extend plastron, are developmentally different entities. The carapace con- dorsally from the hyoplastron and hypoplastron to form a bridge that tains axial endochondral skeletal elements and exoskeletal dermal connects the plastron with the ribs and the carapace. In some turtles bones. The exoskeletal plastron is found in all extant and extinct (especially ancient lineages), a further set of paired plastron bones, species of crown turtles found to date and is synaptomorphic of the the mesoplastra, lie between the hyoplastra and hypoplastra (7). order Testudines. However, paleontological reconstructed transition Although the anatomy of plastron bones has been known for forms lack a fully developed carapace and show a progression of centuries, and the homology of these bones to the skeletal structures bony elements ancestral to the plastron. To understand the evolu- of other reptilian clades has been debated almost as long (3, 4, 6, 8), tionary development of the plastron, it is essential to know how it has we still know very little about how these intramembranous bones formed.