A Comparative Study of Piscine Defense the Scales of Arapaima
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Cambridge University Press 978-1-107-17944-8 — Evolution And
Cambridge University Press 978-1-107-17944-8 — Evolution and Development of Fishes Edited by Zerina Johanson , Charlie Underwood , Martha Richter Index More Information Index abaxial muscle,33 Alizarin red, 110 arandaspids, 5, 61–62 abdominal muscles, 212 Alizarin red S whole mount staining, 127 Arandaspis, 5, 61, 69, 147 ability to repair fractures, 129 Allenypterus, 253 arcocentra, 192 Acanthodes, 14, 79, 83, 89–90, 104, 105–107, allometric growth, 129 Arctic char, 130 123, 152, 152, 156, 213, 221, 226 alveolar bone, 134 arcualia, 4, 49, 115, 146, 191, 206 Acanthodians, 3, 7, 13–15, 18, 23, 29, 63–65, Alx, 36, 47 areolar calcification, 114 68–69, 75, 79, 82, 84, 87–89, 91, 99, 102, Amdeh Formation, 61 areolar cartilage, 192 104–106, 114, 123, 148–149, 152–153, ameloblasts, 134 areolar mineralisation, 113 156, 160, 189, 192, 195, 198–199, 207, Amia, 154, 185, 190, 193, 258 Areyongalepis,7,64–65 213, 217–218, 220 ammocoete, 30, 40, 51, 56–57, 176, 206, 208, Argentina, 60–61, 67 Acanthodiformes, 14, 68 218 armoured agnathans, 150 Acanthodii, 152 amphiaspids, 5, 27 Arthrodira, 12, 24, 26, 28, 74, 82–84, 86, 194, Acanthomorpha, 20 amphibians, 1, 20, 150, 172, 180–182, 245, 248, 209, 222 Acanthostega, 22, 155–156, 255–258, 260 255–256 arthrodires, 7, 11–13, 22, 28, 71–72, 74–75, Acanthothoraci, 24, 74, 83 amphioxus, 49, 54–55, 124, 145, 155, 157, 159, 80–84, 152, 192, 207, 209, 212–213, 215, Acanthothoracida, 11 206, 224, 243–244, 249–250 219–220 acanthothoracids, 7, 12, 74, 81–82, 211, 215, Amphioxus, 120 Ascl,36 219 Amphystylic, 148 Asiaceratodus,21 -
Lecture 6 – Integument ‐ Scale • a Scale Is a Small Rigid Plate That Grows out of an Animal’ S Skin to Provide Protection
Lecture 6 – Integument ‐ Scale • A scale is a small rigid plate that grows out of an animal’s skin to provide protection. • Scales are quite common and have evolved multiple times with varying structure and function. • Scales are generally classified as part of an organism's integumentary system. • There are various types of scales according to shape and to class of animal. • Although the meat and organs of some species of fish are edible by humans, the scales are usually not eaten. Scale structure • Fish scales Fish scales are dermally derived, specifically in the mesoderm. This fact distinguishes them from reptile scales paleontologically. Genetically, the same genes involved in tooth and hair development in mammals are also involved in scale development. Earliest scales – heavily armoured thought to be like Chondrichthyans • Fossil fishes • ion reservoir • osmotic control • protection • Weighting Scale function • Primary function is protection (armor plating) • Hydrodynamics Scales are composed of four basic compounds: ((gmoving from inside to outside in that order) • Lamellar bone • Vascular or spongy bone • Dentine (dermis) and is always associated with enamel. • Acellular enamel (epidermis) • The scales of fish lie in pockets in the dermis and are embeded in connective tissue. • Scales do not stick out of a fish but are covered by the Epithelial layer. • The scales overlap and so form a protective flexible armor capable of withstanding blows and bumping. • In some catfishes and seahorses, scales are replaced by bony plates. • In some other species there are no scales at all. Evolution of scales Placoid scale – (Chondricthyes – cartilagenous fishes) develop in dermis but protrude through epidermis. -
Fishes Scales & Tails Scale Types 1
Phylum Chordata SUBPHYLUM VERTEBRATA Metameric chordates Linear series of cartilaginous or boney support (vertebrae) surrounding or replacing the notochord Expanded anterior portion of nervous system THE FISHES SCALES & TAILS SCALE TYPES 1. COSMOID (most primitive) First found on ostracaderm agnathans, thick & boney - composed of: Ganoine (enamel outer layer) Cosmine (thick under layer) Spongy bone Lamellar bone Perhaps selected for protection against eurypterids, but decreased flexibility 2. GANOID (primitive, still found on some living fish like gar) 3. PLACOID (old scale type found on the chondrichthyes) Dentine, tooth-like 4. CYCLOID (more recent scale type, found in modern osteichthyes) 5. CTENOID (most modern scale type, found in modern osteichthyes) TAILS HETEROCERCAL (primitive, still found on chondrichthyes) ABBREVIATED HETEROCERCAL (found on some primitive living fish like gar) DIPHYCERCAL (primitive, found on sarcopterygii) HOMOCERCAL (most modern, found on most modern osteichthyes) Agnatha (class) [connect the taxa] Cyclostomata (order) Placodermi Acanthodii (class) (class) Chondrichthyes (class) Osteichthyes (class) Actinopterygii (subclass) Sarcopterygii (subclass) Dipnoi (order) Crossopterygii (order) Ripidistia (suborder) Coelacanthiformes (suborder) Chondrostei (infra class) Holostei (infra class) Teleostei (infra class) CLASS AGNATHA ("without jaws") Most primitive - first fossils in Ordovician Bottom feeders, dorsal/ventral flattened Cosmoid scales (Ostracoderms) Pair of eyes + pineal eye - present in a few living fish and reptiles - regulates circadian rhythms Nine - seven gill pouches No paired appendages, medial nosril ORDER CYCLOSTOMATA (60 spp) Last living representatives - lampreys & hagfish Notochord not replaced by vertebrae Cartilaginous cranium, scaleless body Sea lamprey predaceous - horny teeth in buccal cavity & on tongue - secretes anti-coaggulant Lateral Line System No stomach or spleen 5 - 7 year life span - adults move into freshwater streams, spawn, & die. -
1 Lab External Morphology and Taxonomy
External Morphology Gross Anatomy: Fins Dorsal & Taxonomy Caudal Lab 1 Anal Pectoral Pelvic 1. Median fins (dorsal, anal, adipose, caudal) 2. Paired fins (pectoral and pelvic) – abdominal vs. thoracic placement 3. Fish use different fins for locomotion (wrasses use pectorals, triggerfish use median fins, tunas use caudal fins) 4. Fins are constructed of either radial cartilage (sharks) or bony rays (most fishes) Caudal Fin Shape Body Shape body shape can predict ecology: • fusiform tend to be fast swimming and inhabit the upper portions of the water column • compressed tend to be good maneuvers • elongate tend to be good accelerators Caudal fin shape can predict fish ecology (ambush • anguilliform and globiform tend to be poor swimmers and benthic predator, continuous swimmer, burst swimmer, benthic dweller, etc.) • depressed tend to be benthic Mouth Morphology Eyes Mouth morphology can be used to infer what types of prey are eaten (piscivores, planktivores, invertebrate eaters, herbivores, etc.) and where in the water column the prey are consumed Inferior Subterminal 1. placement and size may indicate something about the ecology of the fish 2. some fish (e.g., mudskippers) are adapted to see both in and outside of water 3. stalked eyes in deepwater fish are one adaptation to gather light Terminal Superior 1 Countershading Lateral Line • countershading is a feature common to most fish, especially those that inhabit the surface and midwater • fish are dark on the dorsal region and light on the ventral region • functions as camouflage in open water 1. lateral line extends along the midsection of the fish 2. can be continuous or broken 3. -
Threat-Protection Mechanics of an Armored Fish
JOURNALOFTHEMECHANICALBEHAVIOROFBIOMEDICALMATERIALS ( ) ± available at www.sciencedirect.com journal homepage: www.elsevier.com/locate/jmbbm Research paper Threat-protection mechanics of an armored fish Juha Songa, Christine Ortiza,∗, Mary C. Boyceb,∗ a Department of Materials Science and Engineering, Massachusetts Institute of Technology, 77 Massachusetts Avenue, RM 134022, Cambridge, MA 02139, USA b Department of Mechanical Engineering, Massachusetts Institute of Technology, 77 Massachusetts Avenue, Cambridge, MA 02139, USA ARTICLEINFO ABSTRACT Article history: It has been hypothesized that predatory threats are a critical factor in the protective functional design of biological exoskeletons or “natural armor”, having arisen through evolutionary processes. Here, the mechanical interaction between the ganoid armor of the predatory fish Polypterus senegalus and one of its current most aggressive threats, a Keywords: toothed biting attack by a member of its own species (conspecific), is simulated and studied. Exoskeleton Finite element analysis models of the quadlayered mineralized scale and representative Polypterus senegalus teeth are constructed and virtual penetrating biting events simulated. Parametric studies Natural armor reveal the effects of tooth geometry, microstructure and mechanical properties on its ability Armored fish to effectively penetrate into the scale or to be defeated by the scale, in particular the Mechanical properties deformation of the tooth versus that of the scale during a biting attack. Simultaneously, the role of the microstructure of the scale in defeating threats as well as providing avenues of energy dissipation to withstand biting attacks is identified. Microstructural length scale and material property length scale matching between the threat and armor is observed. Based on these results, a summary of advantageous and disadvantageous design strategies for the offensive threat and defensive protection is formulated. -
Ceratodus Tunuensis, Sp. Nov., a New Lungfish (Sarcopterygii, Dipnoi) from the Upper Triassic of Central East Greenland
Journal of Vertebrate Paleontology ISSN: 0272-4634 (Print) 1937-2809 (Online) Journal homepage: http://www.tandfonline.com/loi/ujvp20 Ceratodus tunuensis, sp. nov., a new lungfish (Sarcopterygii, Dipnoi) from the Upper Triassic of central East Greenland Federico L. Agnolin, Octávio Mateus, Jesper Milàn, Marco Marzola, Oliver Wings, Jan Schulz Adolfssen & Lars B. Clemmensen To cite this article: Federico L. Agnolin, Octávio Mateus, Jesper Milàn, Marco Marzola, Oliver Wings, Jan Schulz Adolfssen & Lars B. Clemmensen (2018) Ceratodus tunuensis, sp. nov., a new lungfish (Sarcopterygii, Dipnoi) from the Upper Triassic of central East Greenland, Journal of Vertebrate Paleontology, 38:2, e1439834, DOI: 10.1080/02724634.2018.1439834 To link to this article: https://doi.org/10.1080/02724634.2018.1439834 Published online: 12 Apr 2018. Submit your article to this journal Article views: 58 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=ujvp20 Journal of Vertebrate Paleontology e1439834 (6 pages) Ó by the Society of Vertebrate Paleontology DOI: 10.1080/02724634.2018.1439834 ARTICLE CERATODUS TUNUENSIS, SP. NOV., A NEW LUNGFISH (SARCOPTERYGII, DIPNOI) FROM THE UPPER TRIASSIC OF CENTRAL EAST GREENLAND FEDERICO L. AGNOLIN,1,2 OCTAVIO MATEUS, *,3,4 JESPER MILAN, 5,6 MARCO MARZOLA, 3,4,7,8 OLIVER WINGS,9 JAN SCHULZ ADOLFSSEN,10 and LARS B. CLEMMENSEN 7 1Laboratorio de Anatomıa Comparada y Evolucion de los Vertebrados, Museo Argentino de -
A Preliminary Study on the Ornamentation Patterns of Ganoid Scales in Some Mesozoic Actinopterygian Fishes
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/291973377 A preliminary study on the ornamentation patterns of ganoid scales in some Mesozoic actinopterygian fishes Article in Bollettino della Societa Paleontologica Italiana · December 2015 DOI: 10.4435/BSPI.2015.14 CITATIONS READS 0 206 2 authors: Claudio Garbelli Andrea Tintori Nanging Institute of Geology and paleontolo… University of Milan 14 PUBLICATIONS 36 CITATIONS 118 PUBLICATIONS 1,487 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Middle Triassic fishes across the Tethys View project All content following this page was uploaded by Andrea Tintori on 06 February 2016. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. TO L O N O G E I L C A A P I ' T A A T L E I I A Bollettino della Società Paleontologica Italiana, 54 (3), 2015, 219-228. Modena C N O A S S. P. I. A preliminary study on the ornamentation patterns of ganoid scales in some Mesozoic actinopterygian fishes Claudio GARBELLI & Andrea TINTORI C. Garbelli, Dipartimento di Scienze della Terra “Ardito Desio”, Università degli Studi di Milano, via Mangiagalli, 2, 20122 Milano, Italy; claudio. [email protected] A. Tintori, Dipartimento di Scienze della Terra “Ardito Desio”, Università degli Studi di Milano, via Mangiagalli, 2, 20122 Milano, Italy; andrea.tintori@ unimi.it KEY WORDS - Ganoid scales, basal actinopterygians, ornamentation, squamation pattern. -
Sarcopterygii, Tetrapodomorpha
Tristichopterids (Sarcopterygii, Tetrapodomorpha) from the Upper Devonian tetrapod-bearing locality of Strud (Belgium, upper Famennian), with phylogenetic and paleobiogeographic considerations Sébastien Olive, Yann Leroy, Edward Daeschler, Jason Downs, S. Ladevèze, Gaël Clément To cite this version: Sébastien Olive, Yann Leroy, Edward Daeschler, Jason Downs, S. Ladevèze, et al.. Tristi- chopterids (Sarcopterygii, Tetrapodomorpha) from the Upper Devonian tetrapod-bearing locality of Strud (Belgium, upper Famennian), with phylogenetic and paleobiogeographic considerations. Journal of Vertebrate Paleontology, Society of Vertebrate Paleontology, 2020, 40 (1), pp.e1768105. 10.1080/02724634.2020.1768105. hal-03099746 HAL Id: hal-03099746 https://hal.archives-ouvertes.fr/hal-03099746 Submitted on 6 Jan 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Journal of Vertebrate Paleontology: For Review Only Tristichopterids (Sarcopterygii, Tetrapodomorpha) from the Late Devonian tetrapod-bearing locality of Strud (Belgium, late Famennian), with phylogenetic -
FISH BIOLOGY (2 UNITS) This Course Is Taught by Three (3) Lecturers
LECTURE NOTE ON FIS 301 FIS 301: FISH BIOLOGY (2 UNITS) This Course is taught by three (3) lecturers – Dr. I.T Omoniyi, Dr. F.I. Adeosun and Dr. A.A. Akinyemi. The Course Synopsis is further outlined on lecture basis as follows: Lectures 1 – 3: Gross external anatomy of typical bony and cartilaginous fishes. Lectures 4 – 5: Gross internal anatomy of typical bony and cartilaginous fishes. Lectures 6 – 7: Anatomy of systems and basic functions Lectures 8 – 9: Reproductive biology treated under fecundity Lectures 10 – 12: Embryology/life history of fish. GROSS EXTERNAL ANATOMY By way of introduction, basic diagnostic features of fish need to be identified. 1. Fishes are cold blooded/poikilothermic animals i.e their body temperature varying passively in accordance with the ambient temperature (surrounding water temperature). Although, fishes as a group can tolerate wide range of temperature from just below O0C to 450C, individual species generally have a preferred or optimum as well as a more restricted temperature range. For example, salmonids inhabit water with temperature range from 0-200C. Any change within the optimum range can significant influence the biology as related to the anatomy. 2. The adoption of aquatic habit has other implications for the structure and physiology of fish. For instance, it makes the streamlining and shaping of the body an important pre-requisite 1 for success in aquatic life. The shapes range from ovoid to torpedo-like or fusiform shape. This is due to the higher density of water than air. 3. Respiration assumes a greater important through the gills when compared to terrestrial th animals because water contains 1/20 of 02 available in air. -
The Origin and Diversification of Osteichthyans and Sarcopterygians: Rare Chinese Fossil Findings Advance Research on Key Issues of Evolution
Vol.24 No.2 2010 Paleoichthyology The Origin and Diversification of Osteichthyans and Sarcopterygians: Rare Chinese Fossil Findings Advance Research on Key Issues of Evolution YU Xiaobo1, 2 ZHU Min1* and ZHAO Wenjin1 1 Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology (IVPP), CAS, Beijing 100044, China 2 Department of Biological Sciences, Kean University, Union, New Jersey 07083, USA iving organisms represent into a hierarchical (or “set-within- chimaeras) with 970 living species, only 1% of all the biota that set”) pattern of groupings on the and the long-extinct placoderms and Lhas ever existed on earth. family tree, with members of each acanthodians. Within osteichthyans, All organisms, living or extinct, new group united by a common the actinopterygian lineage (with are related to each other by sharing ancestor and characterized by novel 26,981 living species) includes common ancestors at different levels, biological features. For instance, sturgeons, gars, teleosts and their like twigs and branches connected within vertebrates, gnathostomes (or relatives, while the sarcopterygian to each other at different nodes on jawed vertebrates) arose as a new lineage (with 26,742 living species) the great tree of life. One major task group when they acquired jaws as includes lungfishes, coelacanths for paleontologists and evolutionary novel features, which set them apart (Latimeria), their extinct relatives as biologists is to find out how the from jawless agnathans (lampreys, well as all land-dwelling tetrapods diverse groups of organisms arose hagfishes and their relatives). Within (amphibians, reptiles, birds, and and how they are related to each gnathostomes, four major groups mammals) (Fig.1). -
A Multi-Proxy Geochemical Investigation of the Early Paleocene (Danian) Continental Palaeoclimate at the Fontllonga-3 Site (Sout
A multi-proxy geochemical investigation of the early Paleocene (Danian) continental palaeoclimate at the Fontllonga-3 site (South Central Pyrenees, Spain) ⁎ Laura Domingo a, , Nieves López-Martínez a, Rodrigo Soler-Gijón a,b, Stephen T. Grimes c a Dept. Paleontología, Facultad CC, Geológicas. Universidad Complutense, 28040 Madrid, Spain b Institut für Paläontologie, Museum für Naturkunde Humboldt Universität, D-10115 Berlin, Germany c School of Earth, Ocean and Environmental Sciences, University of Plymouth, Drake Circus, PL4 8AA Plymouth, Devon, United Kingdom Received 11 January 2007; received in revised form 6 August 2007; accepted 3 September 2007 Abstract Chronologically well constrained non-marine deposits across the Cretaceous–Tertiary boundary (KTb) are exceptionally rare. The Fontllonga section (Tremp Formation, South Central Pyrenees, Lleida, Spain) constitutes one of these rare global records. 18 13 Stable isotope (δ OCO3 and δ C) analyses have been performed on the carbonate fraction of 29 samples from diverse skeletal micro-remains (charophyte gyrogonites, gastropod shells, ostracod valves and isolated skeletal remains of lepisosteids and pycnodonts) from the earliest Danian site, Fontllonga-3. A mean Ba/Ca water palaeotemperature of 28.0±6.7 °C has been obtained from the ganoine of 25 lepisosteid scales. This mean palaeotemperature is comparable with the temperature tolerance range for extant relatives of fossil osteoglossiform fish found at Fontllonga-3, which require a temperature range of 24°–35 °C (mean annual temperature 27–30 °C) to survive. Using the temperature range provided by the Ba/Ca palaeothermometer (21.3–34.7 °C), it is 18 possible to determine δ Owater values from the isotopic content of charophyte gyrogonites, gastropod shells, ostracod valves and 18 18 fish remains (mean δ OCO3 =−5.00 ‰, σ=0.21). -
A High Latitude Devonian Lungfish, from the Famennian of South Africa
A high latitude Devonian lungfish, from the Famennian of South Africa Robert W. Gess1,2,3,* and Alice M. Clement4,* 1 Geology Department, Rhodes University, Makhanda/Grahamstown, South Africa 2 Albany Museum, Makhanda/Grahamstown, South Africa 3 Wits University, DST-NRF Centre of Excellence in Palaeosciences (CoE-Pal), Johannesburg, South Africa 4 College of Science and Engineering, Flinders University, Adelaide, SA, Australia * These authors contributed equally to this work. ABSTRACT New fossil lungfish remains comprising two parasphenoids, tooth plates and scales from the Famennian Witpoort Formation of South Africa are described. From the parasphenoid material, which bears similarity to Oervigia and Sagenodus but is nevertheless unique, a new genus, Isityumzi mlomomde gen. et sp. nov. is erected. Tooth plates and scales from the same locality may be conspecific but are not yet assigned until further material becomes available. The tooth plates closely resemble those of some taxa in the Carboniferous genus Ctenodus. The new taxon is significant as only the second Devonian lungfish described from the African continent, and for hailing from the high-latitude (polar) Waterloo Farm environment situated close to 70 south during the Famennian. Subjects Paleontology, Taxonomy Keywords Waterloo farm, Witpoort formation, Dipnoi, Famennian, South Africa, Western Gondwana, Sarcopterygii, Palaeozoic INTRODUCTION Lungfish (Dipnoi) are a clade of sarcopterygian (lobe-finned) fishes with their origins Submitted 30 July 2019 stretching back to the Early Devonian, over 410 million years ago (Campbell & Barwick, Accepted 21 October 2019 Published 4 December 2019 1983; Chang & Yu, 1984; Denison, 1968; Wang et al., 1993). They reached a peak of diversity and abundance throughout the Devonian with close to 100 species described Corresponding author Alice M.