THE CLASSIFICATION and EVOLUTION of the HETEROSTRACI Since 1858, When Huxley Demonstrated That in the Histological Struc
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Polskaakademianauk Instytutpaleobiologii
POLSKA AKADEMIA NAUK INSTYTUT PALEOBIOLOGII im. Romana Kozłowskiego SILURIAN AND DEVONIAN HETEROSTRACI FROM POLAND AND HYDRODYNAMIC PERFORMANCE OF PSAMMOSTEIDS Sylurskie i dewońskie Heterostraci z Polski oraz efektywność hydrodynamiczna psammosteidów Marek Dec Dissertation for degree of doctor of Earth and related environmental sciences, presented at the Institute of Paleobiology of Polish Academy of Sciences Rozprawa doktorska wykonana w Instytucie Paleobiologii Polskiej Akademii Nauk pod kierunkiem prof. dr hab. Magdaleny Borsuk-Białynickiej w celu uzyskania stopnia doktora w dyscyplinie Nauki o Ziemi oraz środowisku Warszawa 2020 CONTENTS ACKNOWLEDGMENTS…………………………………………………………….….... 3 STRESZCZENIE………………………………………………………………….....….. 4 SUMMARY……………………………………………………………………….…….. 8 CHAPTER I…………………………………………………………………………….. 13 TRAQUAIRASPIDIDAE AND CYATHASPIDIDAE (HETEROSTRACI) FROM LOWER DEVONIAN OF POLAND CHAPTER II……………………………………………………………………….…… 24 A NEW TOLYPELEPIDID (AGNATHA, HETEROSTRACI) FROM THE LATE SILURIAN OF POLAND CHAPTER III…………………………………………………………………………... 41 REVISION OF THE EARLY DEVONIAN PSAMMOSTEIDS FROM THE “PLACODERM SANDSTONE” - IMPLICATIONS FOR THEIR BODY SHAPE RECONSTRUCTION CHAPTER IV……………………………………………………………………….….. 82 NEW MIDDLE DEVONIAN (GIVETIAN) PSAMMOSTEID FROM HOLY CROSS MOUNTAINS (POLAND) CHAPTER V……………………………………………………………………………109 HYDRODYNAMIC PERFORMANCE OF PSAMMOSTEIDS: NEW INSIGHTS FROM COMPUTATIONAL FLUID DYNAMICS SIMULATIONS 2 ACKNOWLEDGMENTS First and foremost I would like to say thank you to my supervisor Magdalena -
Class Myxini Order Myxiniformes Family Myxinidae (Hagfishes)
Class Myxini Order Myxiniformes Family Myxinidae (hagfishes) • Lacks jaws • Mouth not disk-like • barbels present • Unpaired fins as continuous fin-fold • Branchial skeleton not well developed • Eyes degenerate • 70-200 slime glands • Isoosmotic, simple kidneys, stenohayline, marine • Four rudimentary hearts • No true stomach • Unpaired gonads Class Petromyzontida Order Petromyzontiformes Family Petromyzontidae Class Myxini Order Myxiniformes Family Myxinidae (hagfishes) (Northern Lampreys) • Knot-tying behavior • 8 genera, 34 species • Scavengers • Dorsal fins continuous in • Rely heavily on cutaneous respiration adults • Global, deep sea distribution • Oral disc • Commercial interest – eelskin • 7 pairs of gill openings • Single nostril • Pineal body opening • No bone • No scales • No paired fins • No jaws 1 Class Petromyzontida Order Petromyzontiformes Family Petromyzontidae Class Petromyzontida Order Petromyzontiformes Family Petromyzontidae (Northern Lampreys) (Northern Lampreys) • Anadramous and freshwater • Ammocoete • Parasitic forms: – Non-parasitic forms often • Non-parasitic: freshwater – Parasitic forms often anadramous • Life history Class Conodonta, Conodonts Class Pteraspidiomorphi • Extinct, late Triassic • Extinct • First “teeth” • One of the earliest known vertebrates • No jaws • Dermal skeleton • Cranium and teeth • No jaws • Small, thought to be of paedomorphic origin • Little known, an extinct monophyletic lineage. 2 Class Anapsid Class Cephalaspidomorphi, osteostraci • Extinct, Silurian period • Extinct, early Silurian -
Categorical Versus Geometric Morphometric Approaches To
[Palaeontology, 2020, pp. 1–16] CATEGORICAL VERSUS GEOMETRIC MORPHOMETRIC APPROACHES TO CHARACTERIZING THE EVOLUTION OF MORPHOLOGICAL DISPARITY IN OSTEOSTRACI (VERTEBRATA, STEM GNATHOSTOMATA) by HUMBERTO G. FERRON 1,2* , JENNY M. GREENWOOD1, BRADLEY DELINE3,CARLOSMARTINEZ-PEREZ 1,2,HECTOR BOTELLA2, ROBERT S. SANSOM4,MARCELLORUTA5 and PHILIP C. J. DONOGHUE1,* 1School of Earth Sciences, University of Bristol, Life Sciences Building, Tyndall Avenue, Bristol, BS8 1TQ, UK; [email protected], [email protected], [email protected] 2Institut Cavanilles de Biodiversitat i Biologia Evolutiva, Universitat de Valencia, C/ Catedratic Jose Beltran Martınez 2, 46980, Paterna, Valencia, Spain; [email protected], [email protected] 3Department of Geosciences, University of West Georgia, Carrollton, GA 30118, USA; [email protected] 4School of Earth & Environmental Sciences, University of Manchester, Manchester, M13 9PT, UK; [email protected] 5School of Life Sciences, University of Lincoln, Riseholme Hall, Lincoln, LN2 2LG, UK; [email protected] *Corresponding authors Typescript received 2 October 2019; accepted in revised form 27 February 2020 Abstract: Morphological variation (disparity) is almost aspects of morphology. Phylomorphospaces reveal conver- invariably characterized by two non-mutually exclusive gence towards a generalized ‘horseshoe’-shaped cranial mor- approaches: (1) quantitatively, through geometric morpho- phology and two strong trends involving major groups of metrics; -
K Urik, Pycnosteus Tuberculatus (Rohon), Ganosteus Stellatus Rohon and Psammosteus Bergi (Obr.) Are Now Presented in a Somewhat Modified Form
EESTI NSV TEADUSTE AKADEEMIA TOIMETISED. XVII KOIDE I(EEMIA • GEOLOOGIA. 1968, Nr. 3 H3BECTH51 AKAJlEMHH HAYK 3CTOHCKOH CCP. TOM XVII XI1MH5! * T'EOJ10ri15L 1968. N'o 0 D . OBRUCHEV, E. MARK-KURIK ON THE EVOLUTION OF THE PSAMMOSTEIDS (HETEROSTRACI) After our joint paper ( 1965) has been published, new materials of psammosteids have been collected in the Baltic area, and a number of new restorations have been made, and some of the older ones modified. The purpose of the present paper is to give a concise account of the evolution and ontogenetic development of this interesting group of fossil Agnatha, together with some data on their morphology. This study is based solely on the material from the Main Devonian Field (Baltic states, Leningrad, Pskov and adjacent regions), which is the chief area of deve iopment of the psammosteids in the Soviet Union, as well as in the world in general. In the Givetian and Frasnian of the Main Devonian Field the psam mosteids are represented by seven genera, comprising numerous species. Their fossil remains consist as a rule of isolated plates and scales. Only in very few cases same of the plates have been preserved in natural tonnection. Most frequently the branchial plates are met with, so that many species have been founded only on these plates. Lateral and ridge scales are rather common. Dorsal and ventral plates are twice as ·rare as the branchials. Other plates: rostrals, pineals, orbitals, postorbitals, cor nuals and the anterior plates of the ventral carapace, have been discovered only in a few occasions. Although the material of many forms is rather insufficient, attempts have been made to make restorations of a number of psammosteids (Fig. -
Classes of Fish #1 Agnatha : Jawless Fish 1) Oldest of All Fish 500 Mya 2) No Jaw 3) Eel-Like Body 4) Light Skeleton Made out of Cartilage
Classes of Fish #1 Agnatha : Jawless Fish 1) Oldest of all fish 500 mya 2) No Jaw 3) Eel-like Body 4) Light skeleton made out of cartilage. 5) Gill slits on the side of the body. 6) Unpaired fins 7) Examples: Lamprey and Hagfish Objectives: 1. List the three classes of fish. Draw a simple picture for each class and provide a one sentence description. 2. Describe the purposes associated with the lateral line http://www.flickr.com/photos/boarderjon/294353224/ system and the swim bladder. #2 Chondrichthyes : Cartilagenous fish 1) Stream-lined Body 2) Jaws Formed from a bony gill arch 3) Skeleton made of cartilage strengthened be calcium carbonate. A thin layer of bone covers the cartilage. 4)Teeth: modified scales 5) Some possess a lateral line system 6) Examples: Sharks, Rays, and Skates 1 #3 Osteichthyes : Bony Fish 1) Skeleton made of bone . 2) Lateral Line System : Specialized sensory system that runs along the length of the fish. It accurately indicates the position and rate of movement of the 2 Groups of Bony Fish fish. In addition, it can also detect motion of other 1) Ray-finned fish : Fins supported by living things in the water. It is similar in function to bony rays. hearing. Example: Perch 3) Gill Cover : A hard plate called an operculum covers 2) Lobe-finned fish : Fin is a fleshy lobe and protects the gills. Muscles attached to the supported by bone. operculum allow it to move in order to push water Example: Lungfish through the gills. Fish that do not have operculum must swim in order to breath. -
A New Middle Devonian (Givetian) Psammosteid (Vertebrata: Heterostraci) from Poland
Annales Societatis Geologorum Poloniae (2020), vol. 90: 75 – 93 doi: https://doi.org/10.14241/asgp.2020.04 A NEW MIDDLE DEVONIAN (GIVETIAN) PSAMMOSTEID (VERTEBRATA: HETEROSTRACI) FROM POLAND Marek DEC Institute of Palaeobiology, Polish Academy of Sciences, Twarda 51/55, 00-818 Warszawa, Poland; e-mail: [email protected] Dec, M., 2020. A new Middle Devonian (Givetian) psammosteid (Vertebrata: Heterostraci) from Poland. Annales Societatis Geologorum Poloniae, 90: 75 – 93. Abstract: A new genus and species of psammosteid heterostracan, Psarkosteus mediocris gen. et sp. nov., is de- scribed from the Middle Devonian (Givetian) of the Skały Formation, the Holy Cross Mountains, Poland. The dor- sal plate of Psarkosteus is constricted in its anterior part and the postorbital plate is long and narrow. Both features, along with the morphology and variety of tubercles, distinguish it from other representatives of the group. Most distinctive are big, teardrop-shaped tubercles, each with a flat or slightly concave surface and with its tip directed posteriorly, and a crenulated base, located along the branchial plates. The lateral line system in Psarkosteus is similar to that of Drepanaspis gemuendenensis and confirms earlier reconstructions. Key words: Pteraspidomorphi, Heterostraci, Psammosteidae, Middle Devonian, Holy Cross Mountains. Manuscript received 19 February, 2020 accepted 1 June 2020 INTRODUCTION The fossil record of the Heterostraci is poor in Poland, 2017; Glinskiy, 2018). The main problem is concerned although fossils are known from Upper Silurian, Lower with their relationships within the Pteraspidiformes. The and Middle Devonian deposits. From a core sample of the Psammosteidae were supposed to be (1) a sister group to the Upper Silurian (Přidoli) succession in Mielnik a represen- pteraspids s.l., that is Protopteraspididae + Pteraspididae s.l. -
Geological Survey of Ohio
GEOLOGICAL SURVEY OF OHIO. VOL. I.—PART II. PALÆONTOLOGY. SECTION II. DESCRIPTIONS OF FOSSIL FISHES. BY J. S. NEWBERRY. Digital version copyrighted ©2012 by Don Chesnut. THE CLASSIFICATION AND GEOLOGICAL DISTRIBUTION OF OUR FOSSIL FISHES. So little is generally known in regard to American fossil fishes, that I have thought the notes which I now give upon some of them would be more interesting and intelligible if those into whose hands they will fall could have a more comprehensive view of this branch of palæontology than they afford. I shall therefore preface the descriptions which follow with a few words on the geological distribution of our Palæozoic fishes, and on the relations which they sustain to fossil forms found in other countries, and to living fishes. This seems the more necessary, as no summary of what is known of our fossil fishes has ever been given, and the literature of the subject is so scattered through scientific journals and the proceedings of learned societies, as to be practically inaccessible to most of those who will be readers of this report. I. THE ZOOLOGICAL RELATIONS OF OUR FOSSIL FISHES. To the common observer, the class of Fishes seems to be well defined and quite distin ct from all the other groups o f vertebrate animals; but the comparative anatomist finds in certain unusual and aberrant forms peculiarities of structure which link the Fishes to the Invertebrates below and Amphibians above, in such a way as to render it difficult, if not impossible, to draw the lines sharply between these great groups. -
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 ------ - --- - - - - - --- --- - -- --- - -- - - --- -
Fish and Amphibians
Fish and Amphibians Geology 331 Paleontology Phylum Chordata: Subphyla Urochordata, Cephalochordata, and: Subphylum Vertebrata Class Agnatha: jawless fish, includes the hagfish, conodonts, lampreys, and ostracoderms (armored jawless fish) Gnathostomates: jawed fish Class Chondrichthyes: cartilaginous fish Class Placoderms: armored fish Class Osteichthyes: bony fish Subclass Actinopterygians: ray-finned fish Subclass Sarcopterygians: lobe-finned fish Order Dipnoans: lung fish Order Crossopterygians: coelocanths and rhipidistians Class Amphibia Urochordates: Sea Squirts. Adults have a pharynx with gill slits. Larval forms are free-swimming and have a notochord. Chordates are thought to have evolved from the larval form by precocious sexual maturation. Chordate evolution Cephalochordate: Branchiostoma, the lancelet Pikaia, a cephalochordate from the Burgess Shale Yunnanozoon, a cephalochordate from the Lower Cambrian of China Haikouichthys, agnathan, Lower Cambrian of China - Chengjiang fauna, scale is 5 mm A living jawless fish, the lamprey, Class Agnatha Jawless fish do have teeth! A fossil jawless fish, Class Agnatha, Ostracoderm, Hemicyclaspis, Silurian Agnathan, Ostracoderm, Athenaegis, Silurian of Canada Agnathan, Ostracoderm, Pteraspis, Devonian of the U.K. Agnathan, Ostracoderm, Liliaspis, Devonian of Russia Jaws evolved by modification of the gill arch bones. The placoderms were the armored fish of the Paleozoic Placoderm, Dunkleosteus, Devonian of Ohio Asterolepis, Placoderms, Devonian of Latvia Placoderm, Devonian of Australia Chondrichthyes: A freshwater shark of the Carboniferous Fossil tooth of a Great White shark Chondrichthyes, Great White Shark Chondrichthyes, Carcharhinus Sphyrna - hammerhead shark Himantura - a ray Manta Ray Fish Anatomy: Ray-finned fish Osteichthyes: ray-finned fish: clownfish Osteichthyes: ray-finned fish, deep water species Lophius, an Eocene fish showing the ray fins. This is an anglerfish. -
Fossil Jawless Fish from China Foreshadows Early Jawed Vertebrate Anatomy
LETTER doi:10.1038/nature10276 Fossil jawless fish from China foreshadows early jawed vertebrate anatomy Zhikun Gai1,2, Philip C. J. Donoghue1, Min Zhu2, Philippe Janvier3 & Marco Stampanoni4,5 Most living vertebrates are jawed vertebrates (gnathostomes), and The new genus is erected for ‘Sinogaleaspis’ zhejiangensis23,24 Pan, 1986, the living jawless vertebrates (cyclostomes), hagfishes and lampreys, from the Maoshan Formation (late Llandovery epoch to early Wenlock provide scarce information about the profound reorganization of epoch, Silurian period, ,430 million years ago) of Zhejiang, China. the vertebrate skull during the evolutionary origin of jaws1–9. The Diagnosis. Small galeaspid (Supplementary Figs 6 and 7) distinct from extinct bony jawless vertebrates, or ‘ostracoderms’, are regarded as Sinogaleaspis in its terminally positioned nostril, posterior supraorbital precursors of jawed vertebrates and provide insight into this form- sensory canals not converging posteriorly, median dorsal sensory ative episode in vertebrate evolution8–14. Here, using synchrotron canals absent, only one median transverse sensory canal and six pairs radiation X-ray tomography15,16, we describe the cranial anatomy of of lateral transverse sensory canals17,23. galeaspids, a 435–370-million-year-old ‘ostracoderm’ group from Description of cranial anatomy. To elucidate the gross cranial ana- China and Vietnam17. The paired nasal sacs of galeaspids are located tomy of galeaspids, we used synchrotron radiation X-ray tomographic anterolaterally in the braincase, -
Designing the Dinosaur: Richard Owen's Response to Robert Edmond Grant Author(S): Adrian J
Designing the Dinosaur: Richard Owen's Response to Robert Edmond Grant Author(s): Adrian J. Desmond Source: Isis, Vol. 70, No. 2 (Jun., 1979), pp. 224-234 Published by: The University of Chicago Press on behalf of The History of Science Society Stable URL: http://www.jstor.org/stable/230789 . Accessed: 16/10/2013 13:00 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The University of Chicago Press and The History of Science Society are collaborating with JSTOR to digitize, preserve and extend access to Isis. http://www.jstor.org This content downloaded from 150.135.115.18 on Wed, 16 Oct 2013 13:00:27 PM All use subject to JSTOR Terms and Conditions Designing the Dinosaur: Richard Owen's Response to Robert Edmond Grant By Adrian J. Desmond* I N THEIR PAPER on "The Earliest Discoveries of Dinosaurs" Justin Delair and William Sarjeant permit Richard Owen to step in at the last moment and cap two decades of frenzied fossil collecting with the word "dinosaur."' This approach, I believe, denies Owen's real achievement while leaving a less than fair impression of the creative aspect of science. -
The Need for Sedimentary Geology in Paleontology
The Sedimentary Record The Habitat of Primitive Vertebrates: The Need for Sedimentary Geology in Paleontology Steven M. Holland Department of Geology, The University of Georgia, Athens, GA 30602-2501 Jessica Allen Department of Geology and Geophysics, The University of Utah, Salt Lake City, UT 84112-0111 ABSTRACT That these were fish fossils was immediately controversial, with paleontological giants E.D. Cope and E.W. Claypole voicing The habitat in which early fish originated and diversified has doubts. long been controversial, with arguments spanning everything The controversy over habitat soon followed. By 1935, a fresh- from marine to fresh-water. A recent sequence stratigraphic water or possibly estuarine environment for early fish was generally analysis of the Ordovician Harding Formation of central preferred, but essentially in disregard for the sedimentology of the Colorado demonstrates that the primitive fish first described by Harding (Romer and Grove, 1935). Devonian fish were abundant Charles Walcott did indeed live in a shallow marine in fresh-water strata and the lack of fish in demonstrably marine environment, as he argued.This study underscores the need for Ordovician strata supported a fresh-water origin. The abrasion of analyses of the depositional environment and sequence dermal plates in the Harding was considered proof that the fish architecture of fossiliferous deposits to guide paleobiological and were transported from a fresh-water habitat to their burial in a biostratigraphic inferences. littoral environment. The fresh-water interpretation quickly led to paleobiological inference, as armored heads were thought to be a defense against eurypterids living in fresh-water habitats. Paleobiological inference also drove the fresh-water interpretation, INTRODUCTION with biologists arguing that the physiology of kidneys necessitated a For many years, the habitat of primitive vertebrates has been fresh-water origin for fish.