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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. -
The Secrets of Fossils Lesson by Tucker Hirsch
The Secrets of Fossils Lesson by Tucker Hirsch Video Titles: Introduction: A New view of the Evolution of Animals Cambrian Explosion Jenny Clack, Paleontologist: The First Vertebrate Walks on Land Des Collins, Paleontologist: The Burgess Shale Activity Subject: Assessing evolutionary links NEXT GENERATION SCIENCE STANDARDS and evidence from comparative analysis of the fossil MS-LS4-1 Analyze and interpret data for patterns record and modern day organisms. in the fossil record that document the existence, diversity, extinction, and change of life forms Grade Level: 6 – 8 grades throughout the history of life on Earth under the Introduction assumptions that natural laws operate today as In this lesson students make connections between in the past. [Clarification Statement: Emphasis fossils and modern day organisms. Using the is on finding patterns of changes in the level of information about the Cambrian Explosion, they complexity of anatomical structures in organisms explore theories about how and why organisms diversified. Students hypothesize what evidence and the chronological order of fossil appearance might be helpful to connect fossil organisms to in the rock layers.] [Assessment Boundary: modern organisms to show evolutionary connections. Assessment does not include the names of Students use three videos from shapeoflife.org. individual species or geological eras in the fossil record.] Assessments Written MS-LS4-2 Apply scientific ideas to construct an Time 100-120 minutes (2 class periods) explanation for the anatomical similarities and Group Size Varies; single student, student pairs, differences among modern organisms and between entire class modern and fossil organisms to infer evolutionary relationships. [Clarification Statement: Emphasis Materials and Preparation is on explanations of the evolutionary relationships • Access to the Internet to watch 4 Shape of Life videos among organisms in terms of similarity or • Video Worksheet differences of the gross appearance of anatomical • “Ancient-Modern” Activity. -
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 Fossil Record of the Cambrian “Explosion”: Resolving the Tree of Life Critics As Posing Challenges to Evolution
Article The Fossil Record of the Cambrian “Explosion”: 1 Resolving the Tree of Life Keith B. Miller Keith B. Miller The Cambrian “explosion” has been the focus of extensive scientifi c study, discussion, and debate for decades. It has also received considerable attention by evolution critics as posing challenges to evolution. In the last number of years, fossil discoveries from around the world, and particularly in China, have enabled the reconstruction of many of the deep branches within the invertebrate animal tree of life. Fossils representing “sister groups” and “stem groups” for living phyla have been recognized within the latest Precambrian (Neoproterozoic) and Cambrian. Important transitional steps between living phyla and their common ancestors are preserved. These include the rise of mollusks from their common ancestor with the annelids, the evolution of arthropods from lobopods and priapulid worms, the likely evolution of brachiopods from tommotiids, and the rise of chordates and echinoderms from early deuterostomes. With continued new discoveries, the early evolutionary record of the animal phyla is becoming ever better resolved. The tree of life as a model for the diversifi cation of life over time remains robust, and strongly supported by the Neoproterozoic and Cambrian fossil record. he most fundamental claim of bio- (such as snails, crabs, or sea urchins) as it logical evolution is that all living does to the fi rst appearance and diversi- T organisms represent the outer tips fi cation of dinosaurs, birds, or mammals. of a diversifying, upward- branching tree This early diversifi cation of invertebrates of life. The “Tree of Life” is an extreme- apparently occurred around the time of ly powerful metaphor that captures the the Precambrian/Cambrian boundary over essence of evolution. -
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 Origin of Animal Body Plans: a View from Fossil Evidence and the Regulatory Genome Douglas H
© 2020. Published by The Company of Biologists Ltd | Development (2020) 147, dev182899. doi:10.1242/dev.182899 REVIEW The origin of animal body plans: a view from fossil evidence and the regulatory genome Douglas H. Erwin1,2,* ABSTRACT constraints on the interpretation of genomic and developmental The origins and the early evolution of multicellular animals required data. In this Review, I argue that genomic and developmental the exploitation of holozoan genomic regulatory elements and the studies suggest that the most plausible scenario for regulatory acquisition of new regulatory tools. Comparative studies of evolution is that highly conserved genes were initially associated metazoans and their relatives now allow reconstruction of the with cell-type specification and only later became co-opted (see evolution of the metazoan regulatory genome, but the deep Glossary, Box 1) for spatial patterning functions. conservation of many genes has led to varied hypotheses about Networks of regulatory interactions control gene expression and the morphology of early animals and the extent of developmental co- are essential for the formation and organization of cell types and option. In this Review, I assess the emerging view that the early patterning during animal development (Levine and Tjian, 2003) diversification of animals involved small organisms with diverse cell (Fig. 2). Gene regulatory networks (GRNs) (see Glossary, Box 1) types, but largely lacking complex developmental patterning, which determine cell fates by controlling spatial expression -
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. -
Ontogeny, Morphology and Taxonomy of the Softbodied Cambrian Mollusc
[Palaeontology, 2013, pp. 1–15] ONTOGENY, MORPHOLOGY AND TAXONOMY OF THE SOFT-BODIED CAMBRIAN ‘MOLLUSC’ WIWAXIA by MARTIN R. SMITH1,2,3 1Department of Ecology and Evolutionary Biology, University of Toronto, Toronto, Ontario, M5S 3G5, Canada 2Palaeobiology Section, Department of Natural History, Royal Ontario Museum, Toronto, Ontario, M5S 2C6, Canada 3Current address: Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK; e-mail: [email protected] Typescript received 26 September 2012; accepted in revised form 25 May 2013 Abstract: The soft-bodied Cambrian organism Wiwaxia sclerites. I recognize a digestive tract and creeping foot in poses a taxonomic conundrum. Its imbricated dorsal scleri- Wiwaxia, solidifying its relationship with the contemporary tome suggests a relationship with the polychaete annelid Odontogriphus. Similarities between the scleritomes of worms, whereas its mouthparts and naked ventral surface Wiwaxia, halkieriids, Polyplacophora and Aplacophora hint invite comparison with the molluscan radula and foot. 476 that the taxa are related. A molluscan affinity is robustly new and existing specimens from the 505-Myr-old Burgess established, and Wiwaxia provides a good fossil proxy for Shale cast fresh light on Wiwaxia’s sclerites and scleritome. the ancestral aculiferan – and perhaps molluscan – body My observations illuminate the diversity within the genus plan. and demonstrate that Wiwaxia did not undergo discrete moult stages; rather, its scleritome developed gradually, with Key words: halwaxiids, scleritomorphs, Aculifera, Mollusca, piecewise addition and replacement of individually secreted evolution, Cambrian explosion. T HE slug-like Cambrian organism Wiwaxia perennially Nevertheless, Butterfield (2006, 2008) identified char- resists classification, in part due to its unusual scleritome acters that could place these taxa deeper within of originally chitinous scales and spines. -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida -
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.