Some Aspects of Evolutionary Theory George M
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The Phylum Vertebrata: a Case for Zoological Recognition Naoki Irie1,2* , Noriyuki Satoh3 and Shigeru Kuratani4
Irie et al. Zoological Letters (2018) 4:32 https://doi.org/10.1186/s40851-018-0114-y REVIEW Open Access The phylum Vertebrata: a case for zoological recognition Naoki Irie1,2* , Noriyuki Satoh3 and Shigeru Kuratani4 Abstract The group Vertebrata is currently placed as a subphylum in the phylum Chordata, together with two other subphyla, Cephalochordata (lancelets) and Urochordata (ascidians). The past three decades, have seen extraordinary advances in zoological taxonomy and the time is now ripe for reassessing whether the subphylum position is truly appropriate for vertebrates, particularly in light of recent advances in molecular phylogeny, comparative genomics, and evolutionary developmental biology. Four lines of current research are discussed here. First, molecular phylogeny has demonstrated that Deuterostomia comprises Ambulacraria (Echinodermata and Hemichordata) and Chordata (Cephalochordata, Urochordata, and Vertebrata), each clade being recognized as a mutually comparable phylum. Second, comparative genomic studies show that vertebrates alone have experienced two rounds of whole-genome duplication, which makes the composition of their gene family unique. Third, comparative gene-expression profiling of vertebrate embryos favors an hourglass pattern of development, the most conserved stage of which is recognized as a phylotypic period characterized by the establishment of a body plan definitively associated with a phylum. This mid-embryonic conservation is supported robustly in vertebrates, but only weakly in chordates. Fourth, certain complex patterns of body plan formation (especially of the head, pharynx, and somites) are recognized throughout the vertebrates, but not in any other animal groups. For these reasons, we suggest that it is more appropriate to recognize vertebrates as an independent phylum, not as a subphylum of the phylum Chordata. -
Newsletter No. 236 April 2016
NewsletterNewsletter No.No. 236236 AprilApril 20162016 Contents: Future Programme 2 Other Societies and Events 4 Editorial 6 Annual General Meeting Report 7 Committee Norwegian Mines: Nickel, Molybdenum, Chairman Niobium, Cobalt and Silver 8 Graham Worton The Palaeobiology of the Placoderms 11 Vice Chairman Mike's Musings No. 2 - Age of the Earth? 14 Peter Twigg Members' Forum Hon Treasurer Alan Clewlow Birds, Diaphragms and Dinosaurs 16 Hon Secretary More Photos from the Lapworth 16 Linda Tonkin Cairngorm Gems Exhibition, Braemar 16 Field Secretary Andrew Harrison Newsletter Editor Julie Schroder Webmaster John Schroder Other Members Christopher Broughton Bob Bucki Copy date for the next Newsletter is Wednesday 1 June Newsletter No. 236 The Black Country Geological Society April 2016 Linda Tonkin, Andy Harrison, Julie Schroder, Honorary Secretary, Field Secretary, Newsletter Editor, 4 Heath Farm Road, Codsall, 42 Billesley Lane, Moseley, ☎ Wolverhampton, WV8 1HT. 01384 379 320 Birmingham, B13 9QS. ☎ 01902 846074 Mob: 07973 330706 ☎ 0121 449 2407 [email protected] [email protected] [email protected] For enquiries about field and geoconservation meetings please contact the Field Secretary. To submit items for the Newsletter please contact the Newsletter Editor. For all other business and enquiries please contact the Honorary Secretary. For further information see our website: bcgs.info Future Programme Indoor meetings will be held in the Abbey Room at the Dudley Archives, Tipton Road, Dudley, DY1 4SQ, 7.30 for 8.00 o’clock start unless stated otherwise. Visitors are welcome to attend BCGS events but there will be a charge of £1.00 from January 2016. Please let Andy Harrison know in advance if you intend to go to any of the field or geoconservation meetings. -
The Origins of Chordate Larvae Donald I Williamson* Marine Biology, University of Liverpool, Liverpool L69 7ZB, United Kingdom
lopmen ve ta e l B Williamson, Cell Dev Biol 2012, 1:1 D io & l l o l g DOI: 10.4172/2168-9296.1000101 e y C Cell & Developmental Biology ISSN: 2168-9296 Research Article Open Access The Origins of Chordate Larvae Donald I Williamson* Marine Biology, University of Liverpool, Liverpool L69 7ZB, United Kingdom Abstract The larval transfer hypothesis states that larvae originated as adults in other taxa and their genomes were transferred by hybridization. It contests the view that larvae and corresponding adults evolved from common ancestors. The present paper reviews the life histories of chordates, and it interprets them in terms of the larval transfer hypothesis. It is the first paper to apply the hypothesis to craniates. I claim that the larvae of tunicates were acquired from adult larvaceans, the larvae of lampreys from adult cephalochordates, the larvae of lungfishes from adult craniate tadpoles, and the larvae of ray-finned fishes from other ray-finned fishes in different families. The occurrence of larvae in some fishes and their absence in others is correlated with reproductive behavior. Adult amphibians evolved from adult fishes, but larval amphibians did not evolve from either adult or larval fishes. I submit that [1] early amphibians had no larvae and that several families of urodeles and one subfamily of anurans have retained direct development, [2] the tadpole larvae of anurans and urodeles were acquired separately from different Mesozoic adult tadpoles, and [3] the post-tadpole larvae of salamanders were acquired from adults of other urodeles. Reptiles, birds and mammals probably evolved from amphibians that never acquired larvae. -
Catalogue Palaeontology Vertebrates (Updated July 2020)
Hermann L. Strack Livres Anciens - Antiquarian Bookdealer - Antiquariaat Histoire Naturelle - Sciences - Médecine - Voyages Sciences - Natural History - Medicine - Travel Wetenschappen - Natuurlijke Historie - Medisch - Reizen Porzh Hervé - 22780 Loguivy Plougras - Bretagne - France Tel.: +33-(0)679439230 - email: [email protected] site: www.strackbooks.nl Dear friends and customers, I am pleased to present my new catalogue. Most of my book stock contains many rare and seldom offered items. I hope you will find something of interest in this catalogue, otherwise I am in the position to search any book you find difficult to obtain. Please send me your want list. I am always interested in buying books, journals or even whole libraries on all fields of science (zoology, botany, geology, medicine, archaeology, physics etc.). Please offer me your duplicates. Terms of sale and delivery: We accept orders by mail, telephone or e-mail. All items are offered subject to prior sale. Please do not forget to mention the unique item number when ordering books. Prices are in Euro. Postage, handling and bank costs are charged extra. Books are sent by surface mail (unless we are instructed otherwise) upon receipt of payment. Confirmed orders are reserved for 30 days. If payment is not received within that period, we are in liberty to sell those items to other customers. Return policy: Books may be returned within 14 days, provided we are notified in advance and that the books are well packed and still in good condition. Catalogue Palaeontology Vertebrates (Updated July 2020) Archaeology AE11189 ROSSI, M.S. DE, 1867. € 80,00 Rapporto sugli studi e sulle scoperte paleoetnologiche nel bacino della campagna romana del Cav. -
'Placoderm' (Arthrodira)
Jobbins et al. Swiss J Palaeontol (2021) 140:2 https://doi.org/10.1186/s13358-020-00212-w Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access A large Middle Devonian eubrachythoracid ‘placoderm’ (Arthrodira) jaw from northern Gondwana Melina Jobbins1* , Martin Rücklin2, Thodoris Argyriou3 and Christian Klug1 Abstract For the understanding of the evolution of jawed vertebrates and jaws and teeth, ‘placoderms’ are crucial as they exhibit an impressive morphological disparity associated with the early stages of this process. The Devonian of Morocco is famous for its rich occurrences of arthrodire ‘placoderms’. While Late Devonian strata are rich in arthrodire remains, they are less common in older strata. Here, we describe a large tooth-bearing jaw element of Leptodontich- thys ziregensis gen. et sp. nov., an eubrachythoracid arthrodire from the Middle Devonian of Morocco. This species is based on a large posterior superognathal with a strong dentition. The jawbone displays features considered syna- pomorphies of Late Devonian eubrachythoracid arthrodires, with one posterior and one lateral row of conical teeth oriented postero-lingually. μCT-images reveal internal structures including pulp cavities and dentinous tissues. The posterior orientation of the teeth and the traces of a putative occlusal contact on the lingual side of the bone imply that these teeth were hardly used for feeding. Similar to Compagopiscis and Plourdosteus, functional teeth were pos- sibly present during an earlier developmental stage and have been worn entirely. The morphological features of the jaw element suggest a close relationship with plourdosteids. Its size implies that the animal was rather large. Keywords: Arthrodira, Dentition, Food web, Givetian, Maïder basin, Palaeoecology Introduction important to reconstruct character evolution in early ‘Placoderms’ are considered as a paraphyletic grade vertebrates. -
THE CLASSIFICATION and EVOLUTION of the HETEROSTRACI Since 1858, When Huxley Demonstrated That in the Histological Struc
ACTA PALAEONT OLOGICA POLONICA Vol. VII 1 9 6 2 N os. 1-2 L. BEVERLY TARLO THE CLASSIFICATION AND EVOLUTION OF THE HETEROSTRACI Abstract. - An outline classification is given of the Hetero straci, with diagnoses . of th e following orders and suborders: Astraspidiformes, Eriptychiiformes, Cya thaspidiformes (Cyathaspidida, Poraspidida, Ctenaspidida), Psammosteiformes (Tes seraspidida, Psarnmosteida) , Traquairaspidiformes, Pteraspidiformes (Pte ras pidida, Doryaspidida), Cardipeltiformes and Amphiaspidiformes (Amphiaspidida, Hiber naspidida, Eglonaspidida). It is show n that the various orders fall into four m ain evolutionary lineages ~ cyathaspid, psammosteid, pteraspid and amphiaspid, and these are traced from primitive te ssellated forms. A tentative phylogeny is pro posed and alternatives are discussed. INTRODUCTION Since 1858, when Huxley demonstrated that in the histological struc ture of their dermal bone Cephalaspis and Pteraspis were quite different from one another, it has been recognized that there were two distinct groups of ostracoderms for which Lankester (1868-70) proposed the names Osteostraci and Heterostraci respectively. Although these groups are generally considered to be related to on e another, Lankester belie ved that "the Heterostraci are at present associated with the Osteostraci because they are found in the same beds, because they have, like Cepha laspis, a large head shield, and because there is nothing else with which to associate them". In 1889, Cop e united these two groups in the Ostracodermi which, together with the modern cyclostomes, he placed in the Class Agnatha, and although this proposal was at first opposed by Traquair (1899) and Woodward (1891b), subsequent work has shown that it was correct as both the Osteostraci and the Heterostraci were agnathous. -
Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
Tayside, Central and Fife Tayside, Central and Fife
Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland. -
Questioning Hagfish Affinities of the Enigmatic Devonian
Downloaded from http://rsos.royalsocietypublishing.org/ on November 15, 2017 Questioning hagfish affinities of the enigmatic rsos.royalsocietypublishing.org Devonian vertebrate Research Palaeospondylus Cite this article: Johanson Z, Smith M, Zerina Johanson1, Moya Smith1,2, Sophie Sanchez3,4, Sanchez S, Senden T, Trinajstic K, Pfaff C. 2017 5 6 7 Questioning hagfish affinities of the enigmatic Tim Senden , Kate Trinajstic and Cathrin Pfaff Devonian vertebrate Palaeospondylus. R. Soc. 1Department of Earth Sciences, Natural History Museum, London, UK open sci. 4:170214. 2Tissue Engineering and Biophotonics, Dental Institute, King’s College London, http://dx.doi.org/10.1098/rsos.170214 London, UK 3Department of Organismal Biology, Uppsala University, Uppsala, Sweden 4European Synchrotron Radiation Facility, Grenoble, France 5Department of Applied Mathematics, Research School of Physics and Engineering, Received: 8 March 2017 Australian National University, Canberra, Australian Capital Territory 2601, Australia Accepted: 20 June 2017 6Environment and Agriculture, Curtin University, Kent Street, Bentley, Perth, Australia 7Department of Palaeontology, University of Vienna, Vienna, Austria ZJ, 0000-0002-8444-6776;CP,0000-0001-5539-2097 Subject Category: Earth science Palaeospondylus gunni Traquair, 1890 is an enigmatic Devonian vertebrate whose taxonomic affinities have been debated Subject Areas: since it was first described. Most recently, Palaeospondylus has been identified as a stem-group hagfish (Myxinoidea). evolution/palaeontology However, -
Devonian Daniel Childress Parkland College
Parkland College A with Honors Projects Honors Program 2019 Did You Know: Devonian Daniel Childress Parkland College Recommended Citation Childress, Daniel, "Did You Know: Devonian" (2019). A with Honors Projects. 252. https://spark.parkland.edu/ah/252 Open access to this Poster is brought to you by Parkland College's institutional repository, SPARK: Scholarship at Parkland. For more information, please contact [email protected]. GENUS PHYLUM CLASS ORDER SIZE ENVIROMENT DIET: DIET: DIET: OTHER D&D 5E “PERSONAL NOTES” # CARNIVORE HERBIVORE SIZE ACANTHOSTEGA Chordata Amphibia Ichthyostegalia 58‐62 cm Marine (Neritic) Y ‐ ‐ small 24in amphibian 1 ACICULOPODA Arthropoda Malacostraca Decopoda 6‐8 cm Marine (Neritic) Y ‐ ‐ tiny Giant Prawn 2 ADELOPHTHALMUS Arthropoda Arachnida Eurypterida 4‐32 cm Marine (Neritic) Y ‐ ‐ small “Swimmer” Scorpion 3 AKMONISTION Chordata Chondrichthyes Symmoriida 47‐50 cm Marine (Neritic) Y ‐ ‐ small ratfish 4 ALKENOPTERUS Arthropoda Arachnida Eurypterida 2‐4 cm Marine (Transitional) Y ‐ ‐ small Sea scorpion 5 ANGUSTIDONTUS Arthropoda Malacostraca Angustidontida 6‐9 cm Marine (Pelagic) Y ‐ ‐ small Primitive shrimp 6 ASTEROLEPIS Chordata Placodermi Antiarchi 32‐35 cm Marine (Transitional) Y ‐ Y small Placo bottom feeder 7 ATTERCOPUS Arthropoda Arachnida Uraraneida 1‐2 cm Marine (Transitional) Y ‐ ‐ tiny Proto‐Spider 8 AUSTROPTYCTODUS Chordata Placodermi Ptyctodontida 10‐12 cm Marine (Neritic) Y ‐ ‐ tiny Half‐Plate 9 BOTHRIOLEPIS Chordata Placodermi Antiarchia 28‐32 cm Marine (Neritic) ‐ ‐ Y tiny Jawed Placoderm 10 -
New Information on the Evolution of the Bradyodont Chondrichthyes the Lf
UBUVERSt' 3? KJUN01S i H UWNA-CHAMPAICN L30LOGY «H CD FIELDIANA Geology Published by Field Museum of Natural History Volume 33, No. 28 July 29, 1977 This volume is dedicated to Dr. Rainer Zangerl New Information on the Evolution of the Bradyodont Chondrichthyes The Lf Richard Lund 1H7C Department of Biology IYIhK 1 4 1^1 C Adelphi University University oj Illinois INTRODUCTION * UrbanaCham ^» Among the taxa of Chondrichthyans from the upper Mississip- pian Bear Gulch Limestone of Montana (Lund, 1974; Lund and Zangerl, 1974) are holomorphs of four petalodonts, two cochlio- donts, and a chimaeroid. These forms have all been included by vari- ous authors within the Holocephali, or Bradyodonti, usually ranked as a subclass within the Chondrichthyes (Arambourg and Bertin, 1958; Obruchev, 1967). Holomorphs of bradyodont fish are ex- tremely rare (Patterson, 1965) and considerable controversy sur- rounds the inter-relationships of the Bradyodonti and the phyletic position of the group (Patterson, 1968; Bendix-Almgreen, 1968; 1970). This paper attempts to relate some new information to the evolution of the Bradyodont chondrichthyes. CLASS CHONDRICHTHYES: The Chondrichthyes are char- acterized by a cartilaginous endoskeleton which may be superfi- cially calcified; an exoskeleton composed of cyclomorial, synchro- nomorial, or lepidomorial scales which may be lost, modified as cephalic spines, or fused into plates; gill chambers covered by an opercular fold or opening separately to the outside; the absence of an air bladder or lung; otoconia, not compact otoliths in the inner ear which remains open to the outside through endolymphatic ducts. Internal fertilization with copulation is present, males have claspers developed as extensions of the axis of pelvic fins. -
Synchrotron-Aided Reconstruction of the Conodont Feeding Apparatus and Implications for the Mouth of the first Vertebrates
Synchrotron-aided reconstruction of the conodont feeding apparatus and implications for the mouth of the first vertebrates Nicolas Goudemanda,1, Michael J. Orchardb, Séverine Urdya, Hugo Buchera, and Paul Tafforeauc aPalaeontological Institute and Museum, University of Zurich, CH-8006 Zürich, Switzerland; bGeological Survey of Canada, Vancouver, BC, Canada V6B 5J3; and cEuropean Synchrotron Radiation Facility, 38043 Grenoble Cedex, France Edited* by A. M. Celâl Sxengör, Istanbul Technical University, Istanbul, Turkey, and approved April 14, 2011 (received for review February 1, 2011) The origin of jaws remains largely an enigma that is best addressed siderations. Despite the absence of any preserved traces of oral by studying fossil and living jawless vertebrates. Conodonts were cartilages in the rare specimens of conodonts with partly pre- eel-shaped jawless animals, whose vertebrate affinity is still dis- served soft tissue (10), we show that partial reconstruction of the puted. The geometrical analysis of exceptional three-dimensionally conodont mouth is possible through biomechanical analysis. preserved clusters of oro-pharyngeal elements of the Early Triassic Novispathodus, imaged using propagation phase-contrast X-ray Results synchrotron microtomography, suggests the presence of a pul- We recently discovered several fused clusters (rare occurrences ley-shaped lingual cartilage similar to that of extant cyclostomes of exceptional preservation where several elements of the same within the feeding apparatus of euconodonts (“true” conodonts). animal were diagenetically cemented together) of the Early This would lend strong support to their interpretation as verte- Triassic conodont Novispathodus (11). One of these specimens brates and demonstrates that the presence of such cartilage is a (Fig. 2A), found in lowermost Spathian rocks of the Tsoteng plesiomorphic condition of crown vertebrates.