Halwaxiids and the Early Evolution of the Lophotrochozoans. Science
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Durham Research Online
Durham Research Online Deposited in DRO: 23 May 2017 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Betts, Marissa J. and Paterson, John R. and Jago, James B. and Jacquet, Sarah M. and Skovsted, Christian B. and Topper, Timothy P. and Brock, Glenn A. (2017) 'Global correlation of the early Cambrian of South Australia : shelly fauna of the Dailyatia odyssei Zone.', Gondwana research., 46 . pp. 240-279. Further information on publisher's website: https://doi.org/10.1016/j.gr.2017.02.007 Publisher's copyright statement: c 2017 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Accepted Manuscript Global correlation of the early Cambrian of South Australia: Shelly fauna of the Dailyatia odyssei Zone Marissa J. -
Decoding the Fossil Record of Early Lophophorates
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1284 Decoding the fossil record of early lophophorates Systematics and phylogeny of problematic Cambrian Lophotrochozoa AODHÁN D. BUTLER ACTA UNIVERSITATIS UPSALIENSIS ISSN 1651-6214 ISBN 978-91-554-9327-1 UPPSALA urn:nbn:se:uu:diva-261907 2015 Dissertation presented at Uppsala University to be publicly examined in Hambergsalen, Geocentrum, Villavägen 16, Uppsala, Friday, 23 October 2015 at 13:15 for the degree of Doctor of Philosophy. The examination will be conducted in English. Faculty examiner: Professor Maggie Cusack (School of Geographical and Earth Sciences, University of Glasgow). Abstract Butler, A. D. 2015. Decoding the fossil record of early lophophorates. Systematics and phylogeny of problematic Cambrian Lophotrochozoa. (De tidigaste fossila lofoforaterna. Problematiska kambriska lofotrochozoers systematik och fylogeni). Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1284. 65 pp. Uppsala: Acta Universitatis Upsaliensis. ISBN 978-91-554-9327-1. The evolutionary origins of animal phyla are intimately linked with the Cambrian explosion, a period of radical ecological and evolutionary innovation that begins approximately 540 Mya and continues for some 20 million years, during which most major animal groups appear. Lophotrochozoa, a major group of protostome animals that includes molluscs, annelids and brachiopods, represent a significant component of the oldest known fossil records of biomineralised animals, as disclosed by the enigmatic ‘small shelly fossil’ faunas of the early Cambrian. Determining the affinities of these scleritome taxa is highly informative for examining Cambrian evolutionary patterns, since many are supposed stem- group Lophotrochozoa. The main focus of this thesis pertained to the stem-group of the Brachiopoda, a highly diverse and important clade of suspension feeding animals in the Palaeozoic era, which are still extant but with only with a fraction of past diversity. -
Paterimitra Pyramidalis Laurie, 1986, the First Tommotiid Discovered From
1 Paterimitra pyramidalis Laurie, 1986, the first tommotiid discovered from 2 the early Cambrian of North China 3 4 Bing Pana, b, Glenn A. Brockc, Christian B. Skovstedd, Marissa J. Bettse, Timothy P. Topperf, 5 Guo-Xiang Lia, * 6 7 a State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and 8 Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China 9 b University of Science and Technology of China, Hefei 230026, China 10 c Department of Biological Sciences, Macquarie University, NSW 2109, Australia 11 d Department of Palaeobiology, Swedish Museum of Natural History, Stockholm, Sweden. 12 e Palaeoscience Research Centre, School of Environmental and Rural Science, University of 13 New England, Armidale, NSW, Australia. 14 f Palaeoecosystems Group, Department of Earth Sciences, Durham University, Durham, UK. 15 * Corresponding author. 16 E-mail: [email protected] (B. Pan), [email protected] (G.A. Brock), 17 [email protected] (C.B. Skovsted), [email protected] (M.J. Betts), 18 [email protected] (T.P. Topper), [email protected] (G.X. Li) 19 20 ABSTRACT 21 The eccentrothecimorph tommotiid Paterimitra pyramidalis Laurie, 1986, was 22 previously only known from lower Cambrian rocks of the Northern Territory and South 23 Australia. Herein, we document the first occurrence of P. pyramidalis from the Xinji 24 Formation in the Shuiyu section at Ruicheng County, Shanxi Province, located at the 25 southwestern margin of the North China Platform. This represents the first report of a 1 26 tommotiid taxon from lower Cambrian strata of the North China Platform. -
Developing Perspectives on Molluscan Shells, Part 1: Introduction and Molecular Biology
CHAPTER 1 DEVELOPING PERSPECTIVES ON MOLLUSCAN SHELLS, PART 1: INTRODUCTION AND MOLECULAR BIOLOGY KEVIN M. KOCOT1, CARMEL MCDOUGALL, and BERNARD M. DEGNAN 1Present Address: Department of Biological Sciences and Alabama Museum of Natural History, The University of Alabama, Tuscaloosa, AL 35487, USA; E-mail: [email protected] School of Biological Sciences, The University of Queensland, St. Lucia, Queensland 4072, Australia CONTENTS Abstract ........................................................................................................2 1.1 Introduction .........................................................................................2 1.2 Insights From Genomics, Transcriptomics, and Proteomics ............13 1.3 Novelty in Molluscan Biomineralization ..........................................21 1.4 Conclusions and Open Questions .....................................................24 Keywords ...................................................................................................27 References ..................................................................................................27 2 Physiology of Molluscs Volume 1: A Collection of Selected Reviews ABSTRACT Molluscs (snails, slugs, clams, squid, chitons, etc.) are renowned for their highly complex and robust shells. Shell formation involves the controlled deposition of calcium carbonate within a framework of macromolecules that are secreted by the outer epithelium of a specialized organ called the mantle. Molluscan shells display remarkable morphological -
Segmented Worms (Phylum Annelida): a Celebration of Twenty Years of Progress Through Zootaxa and Call for Action on the Taxonomic Work That Remains
Zootaxa 4979 (1): 190–211 ISSN 1175-5326 (print edition) https://www.mapress.com/j/zt/ Review ZOOTAXA Copyright © 2021 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4979.1.18 http://zoobank.org/urn:lsid:zoobank.org:pub:8CEAB39F-92C2-485C-86F3-C86A25763450 Segmented worms (Phylum Annelida): a celebration of twenty years of progress through Zootaxa and call for action on the taxonomic work that remains WAGNER F. MAGALHÃES1, PAT HUTCHINGS2,3, ALEJANDRO OCEGUERA-FIGUEROA4, PATRICK MARTIN5, RÜDIGER M. SCHMELZ6, MARK J. WETZEL7, HELENA WIKLUND8, NANCY J. MACIOLEK9, GISELE Y. KAWAUCHI10 & JASON D. WILLIAMS11 1Institute of Biology, Federal University of Bahia, Salvador, 40170-115, Bahia, Brazil. �[email protected]; https://orcid.org/0000-0002-9285-4008 2Australian Museum Research Institute, Australian Museum, Sydney, NSW. Australia. �[email protected]; https://orcid.org/0000-0001-7521-3930 3Biological Sciences, Macquarie University, North Ryde, NSW 2019, Australia. 4Departamento de Zoología, Instituto de Biología, Universidad Nacional Autónoma de México, Tercer circuito s/n, Ciudad Universitaria, 04510, Mexico City, Mexico. �[email protected]; https://orcid.org/0000-0002-5514-9748 5Royal Belgian Institute of Natural Sciences, Taxonomy and Phylogeny, 29 rue Vautier, B-1000 Brussels, Belgium. �[email protected]; https://orcid.org/0000-0002-6033-8412 6IfAB Institute for Applied Soil Biology, Hamburg, Germany. �[email protected] 7Illinois Natural History Survey, Prairie Research Institute at the University of Illinois at Urbana-Champaign, Forbes Natural History Building, MC-652, 1816 S. Oak Street, Champaign, Illinois 61820 USA. �[email protected]; https://orcid.org/0000-0002-4247-0954 8Department of Marine Sciences, University of Gothenburg, Gothenburg, Sweden. -
Small Shelly Fossils from the Argillaceous Facies of the Lower Cambrian Forteau Formation of Western Newfoundland
Small shelly fossils from the argillaceous facies of the Lower Cambrian Forteau Formation of western Newfoundland CHRISTIAN B. SKOVSTED and JOHN S. PEEL Skovsted, C.B. and Peel, J.S. 2007. Small shelly fossils from the argillaceous facies of the Lower Cambrian Forteau For− mation of western Newfoundland. Acta Palaeontologica Polonica 52 (4): 729–748. A diverse fauna of helcionelloid molluscs, hyoliths, and other small shelly fossils is described from limestone layers within the Forteau Formation of the Bonne Bay region in western Newfoundland. The fauna is dominated by internal moulds of various molluscs and tubular problematica, but also includes hyolith opercula, echinoderm ossicles, and other calcareous small shelly fossils preserved by phosphatisation. Originally organophosphatic shells are comparatively rare, but are represented by brachiopods, hyolithelminths, and tommotiids. The fauna is similar to other late Early Cambrian faunas from slope and outer shelf settings along the eastern margin of Laurentia and may be of middle Dyeran age. The similarity of these faunas indicates that at least by the late Early Cambrian, a distinctive and laterally continuous outer shelf fauna had evolved. The Forteau Formation also shares elements with faunas from other Early Cambrian provinces, strengthening ties between Laurentia and Australia, China, and Europe during the late Early Cambrian. Two new taxa of problematic fossil organisms are described, the conical Clavitella curvata gen. et sp. nov. and the wedge−shaped Sphenopteron boomerang gen. et sp. nov. Key words: Helcionellidae, Hyolitha, Brachiopoda, small shelly fossils, Cambrian, Laurentia, Newfoundland. Christian B. Skovsted [[email protected]], Centre for Ecostratigraphy and Palaeobiology, Macquarie University, NSW 2109, Marsfield, Sydney, Australia. -
Insect Morphology
PRINCIPLES OF INSECT MORPHOLOGY BY R. E. SNODGRASS United States Department of Agriculture Bureau of Entomolo(JY and Plant Quarantine FIRST EDITION SECOND IMPRESSION McGRA W-HILL BOOK COMPANY, INC. NEW YORK AND LONDON 1935 McGRAW-HILL PUBLICATIONS- IN THE ZOOLOGICAL SCaNCES A. FRANKLIN SHULL, CONSULTING EDITOR PRINCIPLES OF INSECT MORPHOLOGY COPYRIGHT, 1935, BY THE l\1CGRAW-HILIi BOOK COMPANY, INC. PRINTED IN THE UNITED STATES OF AMERICA All rights reserved. This book, or parts thereof, may not be reproduced in any form without permission oj the publishers. \ NLVS/IVRI 111111111 II 1111 1111111111111 01610 TaE MAPLE PRESS COMPANY, YORK, PA. PREFACE The principal value of fa cis is that they give us something to think about. A scientific textbook, therefore, should contain a fair amount of reliable information, though it may be a matter of choice with the author whether he leaves it to the reader to formulate his own ideas as to the meaning of the facts, or whether he attempts to guide the reader's thoughts along what seem to him to be the proper channels. The writer of the present text, being convinced that generalizations are more important than mere knowledge of facts, and being also somewhat partial to his own way of thinking about insects, has not been able to refrain entirely from presenting the facts of insect anatomy in a way to suggest relations between them that possibly exist only in his own mind. Each of the several chapters of this book, in other words, is an attempt to give a coherent morphological view of the fundamental nature and the apparent evolution of a particular group of organs or associated struc tures. -
'Scaly-Foot' Gastropod
Earth and Planetary Science Letters 242 (2006) 39–50 www.elsevier.com/locate/epsl Sclerite formation in the hydrothermal-vent bscaly-footQ gastropod—possible control of iron sulfide biomineralization by the animal Yohey Suzuki a,*, Robert E. Kopp b, Toshihiro Kogure c, Akinobu Suga d, Ken Takai a, Shinji Tsuchida e, Noriaki Ozaki f, Kazuyoshi Endo g, Jun Hashimoto h, Yasuhiro Kato i, Chitoshi Mizota j, Takafumi Hirata d, Hitoshi Chiba k, Kenneth H. Nealson a,l, Koki Horikoshi a, Joseph L. Kirschvink b a Extremobiosphere Research Center, Japan Agency for Marine-Earth Science & Technology, Yokosuka 237-0061, Japan b Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA c Department of Earth and Planetary Science, the University of Tokyo, Hongo, Tokyo 113-0033, Japan d Laboratory for Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551, Japan e Marine Ecosystems Research Department, Japan Agency for Marine-Earth Science & Technology, Yokosuka 237-0061, Japan f Ocean Research Institute, University of Tokyo, Nakano, Tokyo 164-8639, Japan g Institute of Geoscience, University of Tsukuba, Tsukuba 305-8572, Japan h Faculty of Fisheries, Nagasaki University, Nagasaki, 852-8521, Japan i Department of Geosystem Engineering, Unversity of Tokyo, Tokyo 113-8656, Japan j Faculty of Agriculture, Iwate University, Morioka, Iwate 020-8550, Japan k Department of Earth Sciences, Okayama University, Okayama, Okayama 700-8530, Japan l Department of Earth Sciences, University of Southern California, 3651 Trousdale Pkwy., Los Angeles, CA 90089-0740, USA Received 24 March 2005; received in revised form 23 August 2005; accepted 22 November 2005 Available online 10 January 2006 Editor: E. -
SKELETAL MICROSTRUCTURE INDICATES CHANCELLORIIDS and HALKIERIIDS ARE CLOSELY RELATED by SUSANNAH M
[Palaeontology, Vol. 51, Part 4, 2008, pp. 865–879] SKELETAL MICROSTRUCTURE INDICATES CHANCELLORIIDS AND HALKIERIIDS ARE CLOSELY RELATED by SUSANNAH M. PORTER Department of Earth Science, University of California at Santa Barbara, Santa Barbara, CA 93106, USA; e-mail: [email protected] Typescript received 7 November 2005; accepted in revised form 7 September 2007 Abstract: Chancelloriids are problematic, sac-like animals and siphogonuchitid sclerites are homologous. The difference whose sclerites are common in Cambrian fossil assemblages. in chancelloriid and halkieriid body plans can be resolved in They look like sponges, but were united with the slug-like two ways. Chancelloriids either represent a derived condition halkieriids in the group Coeloscleritophora Bengtson and exhibiting complete loss of bilaterian characters or they repre- Missarzhevsky, 1981 based on a unique mode of sclerite con- sent the ancestral condition from which the bilaterally sym- struction. Because their body plans are so different, this pro- metric halkieriids, and the Bilateria as a whole, derived. The posal has never been well accepted, but detailed study of their latter interpretation, proposed by Bengtson (2005), implies sclerite microstructure presented here provides additional that coeloscleritophoran sclerites (‘coelosclerites’) are a plesi- support for this grouping. Both taxa possess walls composed omorphy of the Bilateria, lost or transformed in descendent of a thin, probably organic, sheet overlying a single layer of lineages. Given that mineralized coelosclerites appear in the aragonite fibres orientated parallel to the long axis of the fossil record no earlier than c. 542 Ma, this in turn implies sclerite. In all halkieriids and in the chancelloriid genus Archi- either that the Ediacaran record of bilaterians has been misin- asterella Sdzuy, 1969, bundles of these fibres form inclined terpreted or that coelosclerite preservability increased at the projections on the upper surface of the sclerite giving it a beginning of the Cambrian Period. -
Parts of Insects the Integument Cuticle Exoskeleton
The Integument Week #2 Consequences of having your skeleton on the outside External Morphology 1. Muscles attach on the inside of Insects 2. The exoskeleton is also a suit of armor 3. Sensing the outside world is a challenge 4. Growth is impaired 5. There is a limit on insect size Parts of insects • Integument (body wall) • Thorax – Skeleton – Segments – Cuticle – Legs – Formation – Wings – Physical properties – Modifications • Head • Abdomen – Major functions – Cerci – Eyes – Ovipositor – Mouthparts: types and – Modifications positions – Antennae – Modifications The Integument Outer covering; includes cuticle and epidermis Cuticle The external skeletal structure, composed of chitin and protein Exoskeleton The external, hardened, cuticular skeleton to which muscles are attached internally 1 The Integument Consequences of having your skeleton on the outside 1. Muscles attach on the inside 2. The exoskeleton is also a suit of armor 3. Sensing the outside world is a challenge 4. Growth is impaired 5. There is a limit on insect size 2 The Integument Consequences of having your skeleton on the outside 1. Muscles attach on the inside 2. The exoskeleton is also a suit of armor 3. Sensing the outside world is a challenge 4. Growth is impaired 5. There is a limit on insect size The Integument Consequences of having your skeleton on the outside 1. Muscles attach on the inside 2. The exoskeleton is also a suit of armor 3. Sensing the outside world is a challenge 4. Growth is impaired 5. There is a limit on insect size Chitin, polysaccaride similar to cellulose; gives the cuticle its strength Chitin, a major cuticle component, is insoluble in water, alcohol, ether, dilute acids, and dilute or concentrate alkali. -
The Earliest Annelids: Lower Cambrian Polychaetes from the Sirius Passet Lagerstätte, Peary Land, North Greenland
The earliest annelids: Lower Cambrian polychaetes from the Sirius Passet Lagerstätte, Peary Land, North Greenland SIMON CONWAY MORRIS and JOHN S. PEEL Conway Morris, S. and Peel, J.S. 2008. The earliest annelids: Lower Cambrian polychaetes from the Sirius Passet Lagerstätte, Peary Land, North Greenland. Acta Palaeontologica Polonica 53 (1): 137–148. Apart from the Phyllopod Bed of the Burgess Shale (Middle Cambrian) polychaete annelids are practically unknown from any of the Cambrian Lagerstätten. This is surprising both because their diversity in the Burgess Shale is considerable, while to date the Chengjiang Lagerstätte which is equally impressive in terms of faunal diversity has no reliable records of any annelids. Here we describe, on the basis of about 40 specimens, Phragmochaeta canicularis gen. et sp. nov. from the Lower Cambrian Sirius Passet Lagerstätte of Peary Land, North Greenland. This makes it by far the oldest known polychaete, with a likely age of lower to middle Atdabanian, The body consists of approximately 20 segments, each bearing notochaetae and neurochaetae. The former appeared to have formed a felt−like covering on the dorsum, whilst the neurochaetae projected obliquely to the longitudinal axis. Apart from minor differences in chaetal size at either end there is no other tagmosis. Details of the head are obscure, and presence of palps, tentacles and eyes are conjectural. Jaws appear to have been absent. The gut was straight, and flanked by massive longitudinal musculature. P. canicularis was evidently benthic, propelling itself on the neurochaetae, with the dorsal neurochaetae conferring protection. Its stratigraphic position and generalized appearance are consistent with P. -
Coat of Many Colours—DNA Reveals Polymorphism of Mantle Patterns and Colouration in Caribbean Cyphoma Röding, 1798 (Gastropoda, Ovulidae)
Coat of many colours—DNA reveals polymorphism of mantle patterns and colouration in Caribbean Cyphoma Röding, 1798 (Gastropoda, Ovulidae) Bastian T. Reijnen1 and Sancia E.T. van der Meij1,2,3 1 Naturalis Biodiversity Center, Leiden, The Netherlands 2 Oxford University Museum of Natural History, University of Oxford, Oxford, United Kingdom 3 Linacre College, Oxford, United Kingdom ABSTRACT The iconic gastropod genus Cyphoma is commonly observed in the Caribbean, where it lives in association with various octocorallian hosts. Each species in the genus Cyphoma has a unique, characteristic mantle pattern and colouration, which separates the valid taxa. Because of its abundance and recognisability Cyphoma gibbosum has been used as a model organism in several studies concerning allelochemicals, reef degradation, and physical defence mechanisms. Molecular analyses based on four molecular markers (COI, 16S, H3 and 28S) for three Cyphoma species (C. gibbosum, C. mcgintyi, C. signatum) and an unidentified black morph, collected from three localities in the Caribbean, show that they represent morphological varieties of a single, genetically homogeneous species. This outcome is in agreement with previous anatomical studies. As a result C. mcgintyi and C. signatum are synonymised with C. gibbosum, which is a key result for future work using C. gibbosum as a model organism. The striking morphological differences in mantle pattern and colouration are hypothesised to be the result of one of three possible scenarios: rapid divergence, supergenes (including balanced polymorphism), or incipient speciation. Submitted 25 March 2016 Accepted 23 January 2017 Subjects Biodiversity, Marine Biology, Molecular Biology, Taxonomy Published 2 March 2017 Keywords Gastropoda, Marine invertebrates, Molecular phylogeny, Octocorallia, Taxonomy, Corresponding author Systematics Bastian T.