THE PROBLEM of the RELATIONSHIP BETWEEN AGNATHAN and GNATHOSTOME VERTEBRATES the Problem of the Relationship Between Agnatha
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Review of the Lampreys (Petromyzontidae) in Bosnia and Herzegovina: a Current Status and Geographic Distribution
Review of the lampreys (Petromyzontidae) in Bosnia and Herzegovina: a current status and geographic distribution Authors: Tutman, Pero, Buj, Ivana, Ćaleta, Marko, Marčić, Zoran, Hamzić, Adem, et. al. Source: Folia Zoologica, 69(1) : 1-13 Published By: Institute of Vertebrate Biology, Czech Academy of Sciences URL: https://doi.org/10.25225/jvb.19046 BioOne Complete (complete.BioOne.org) is a full-text database of 200 subscribed and open-access titles in the biological, ecological, and environmental sciences published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Complete website, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/terms-of-use. Usage of BioOne Complete content is strictly limited to personal, educational, and non - commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Downloaded From: https://bioone.org/journals/Journal-of-Vertebrate-Biology on 13 Feb 2020 Terms of Use: https://bioone.org/terms-of-use Journal of Open Acces Vertebrate Biology J. Vertebr. Biol. 2020, 69(1): 19046 DOI: 10.25225/jvb.19046 Review of the lampreys (Petromyzontidae) in Bosnia and Herzegovina: -
Fish Identification
FISH IDENTIFICATION Anurag Babu EWRG ,CES, IISc, Bangalore SUPER CLASS INFRAPHYLUM AGNATHA CYCLOSTOMAT A PHYLUM CHORDATA SUPER CLASS INFRAPHYLUM Incertae serdis GNATHOSTOMA SUPER CLASS OSTEICHTHYES CLASS CLASS CLASS MYXINI PETROMYZONTIDA CONODANTA CLASS CLASS CLASS CONDRICHTHYES PLACODERMI ACANTHODII CLASS CLASS ACTINOPTERYGII SARCOPTERYGII CLASS CLASS CLASS PTERASPIDOMORPHI THELODONTI ANASPIDA CLASS CEPHALASPIDOMORPHI So , What are the Steps FISH SAMPLING What is the purpose of our Sampling ? Use suitable gears Gears based on purpose Active Gear/ Sampling Passive Gear/ Sampling Fyke Net Cast Net Scoop Net Gill Net Angling FISH IDENTIFICATION ANATOMICAL BODY SHAPE Torpediform Dorso Ventrally Flattened Ribbon like Eel like Spheroid Laterally Flattened Arrow like COLOR & PATTERN ? Etroplus maculatus Scatophagus argus Etroplus suratensis MERISTIC FACIAL & CRANIAL BONES TYPE OF MOUTH Funneled Silver bellies Mouth Classification EYE Caranx latus EYE Caranx latus LEFT OR RIGHT Scophthalmus maximus Hippoglossus hippoglossus FINS DORSAL FINS CAUDAL FINS PECTORAL FIN PELVIC FIN ANAL FIN Caranx ignobilis Spiny Dorsal DORSAL FIN Rayed Dorsal Adipose Dorsal Spiny & Rayed Anal ANAl FIN Rayed Anal PECTORAL FINS PELVIC FINS Abdominal Thoracic CAUDAL FINS CAUDAL FINS What makes Spine & Ray Different ? GILL RAKERS SCALES LATERAL LINE CONTINUITY POSITION CURVE SCUTES IDENTIFICATION KEYS DICHOTOMOUS POLYTOMOUS FIN ( Neogobius melanostomus (Pallas, 1811).) FORMULAD1 VI (V-VII); D2 I + 14-16 (13-16); A I + 11-13 (11-14); P 18-19 (17-20). The anterior dorsal fin has 6 spines, ranging from 5-7 The posterior dorsal fin has one spine and 14-16 soft rays, ranging from 13-16 The anal fin has one spine, 11-13 soft rays, ranging from 11-14 The pectoral fins have 18-19 soft rays, ranging from 17-20 MORPHOMETRIC LET’S try Identifying A FISH !! FIN ( Neogobius melanostomus (Pallas, 1811).) FORMULAD1 VI (V-VII); D2 I + 14-16 (13-16); A I + 11-13 (11-14); P 18-19 (17-20). -
Hedges2009chap39.Pdf
Vertebrates (Vertebrata) S. Blair Hedges Vertebrates are treated here as a separate phylum Department of Biology, 208 Mueller Laboratory, Pennsylvania State rather than a subphylum of Chordata. 7 e morpho- University, University Park, PA 16802-5301, USA ([email protected]) logical disparity among the chordates (urochordates, cepahalochordates, and vertebrates), and their deep time of separation based on molecular clocks (5) is as great Abstract as that among other groups of related animal phyla (e.g., The vertebrates (~58,000 sp.) comprise a phylum of mostly arthropods, tardigrades, and onycophorans). 7 e phyl- mobile, predatory animals. The evolution of jaws and ogeny of the lineages covered here is uncontroversial, for limbs were key traits that led to subsequent diversifi cation. the most part. Evidence from nuclear genes and morph- Atmospheric oxygen change appears to have played a major ology (1, 2, 6, 7) agree in the backbone phylogeny of ver- role, with an initial rise in the late Precambrian (~580–542 tebrates represented by these nested groups: Tetrapoda million years ago, Ma) permitting larger body size, followed (Lissamphibia, Amniota), Sarcopterygii (Actinistia, by two Paleozoic pulses affecting prey. The First Pulse Dipnoi, Tetrapoda), Osteichthyes (Actinopterygii, (~430–390 Ma) brought fi shes to brackish and freshwater Sarcopterygii), and Gnathostomata (Chondrichthyes, environments where they diversifi ed, with one lineage giv- Osteichthyes). ing rise to tetrapods. The Second Pulse (~340–250 Ma) led to Cyclostomata wa s or ig i na l ly considered a ba sa l, mono- a Permo-Carboniferous explosion of tetrapods, adapting to phyletic group based on morphology (8), but later mor- diverse terrestrial niches. -
Upper Basin Pallid Sturgeon Recovery Workgroup Annual Report
UPPER BASIN PALLID STURGEON RECOVERY WORKGROUP 2004 ANNUAL REPORT Upper Basin Pallid Sturgeon Workgroup c/o Montana Fish, Wildlife and Parks 1420 East Sixth Helena MT 59620 August 2005 TABLE OF CONTENTS INTRODUCTION WORKGROUP MEETING NOTES 2004 Annual Meeting Notes – December 1-2, 2004 .............................................................5 March 9, 2005 Meeting Notes ...............................................................................................21 WORKGROUP LETTERS AND DOCUMENTS Intake BOR Letter..................................................................................................................29 Garrison Review Team Report Submission Letter to USFWS..............................................31 Review of pallid sturgeon culture at Garrison Dam NFH by the Upper Basin Pallid Sturgeon Review Team, March, 2005 ..............................................................36 RESEARCH AND MONITORING 2004 Pallid Sturgeon Recovery Efforts in the Upper Missouri River, Montana (RPMA #1), Bill Gardner, Montana Fish, Wildlife and Parks, Lewistown, MT...................49 Habitat Use, Diet, and Growth of Hatchery-reared Juvenile Pallid Sturgeon And Indigenous shovelnose sturgeon in the Missouri River avove Fort Peck Reservoir, Montana, Paul C. Gerrity, Christopher S. Guy, and William M. Gardner, Montana Cooperative Fishery Research Unit, Montana State University.............................65 Lower Missouri and Yellowstone Rivers Pallid Sturgeon Study, 2004 Report, Mtthew M. Klungle and Matthew W. Baxter, Montana -
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. -
Updated Checklist of Marine Fishes (Chordata: Craniata) from Portugal and the Proposed Extension of the Portuguese Continental Shelf
European Journal of Taxonomy 73: 1-73 ISSN 2118-9773 http://dx.doi.org/10.5852/ejt.2014.73 www.europeanjournaloftaxonomy.eu 2014 · Carneiro M. et al. This work is licensed under a Creative Commons Attribution 3.0 License. Monograph urn:lsid:zoobank.org:pub:9A5F217D-8E7B-448A-9CAB-2CCC9CC6F857 Updated checklist of marine fishes (Chordata: Craniata) from Portugal and the proposed extension of the Portuguese continental shelf Miguel CARNEIRO1,5, Rogélia MARTINS2,6, Monica LANDI*,3,7 & Filipe O. COSTA4,8 1,2 DIV-RP (Modelling and Management Fishery Resources Division), Instituto Português do Mar e da Atmosfera, Av. Brasilia 1449-006 Lisboa, Portugal. E-mail: [email protected], [email protected] 3,4 CBMA (Centre of Molecular and Environmental Biology), Department of Biology, University of Minho, Campus de Gualtar, 4710-057 Braga, Portugal. E-mail: [email protected], [email protected] * corresponding author: [email protected] 5 urn:lsid:zoobank.org:author:90A98A50-327E-4648-9DCE-75709C7A2472 6 urn:lsid:zoobank.org:author:1EB6DE00-9E91-407C-B7C4-34F31F29FD88 7 urn:lsid:zoobank.org:author:6D3AC760-77F2-4CFA-B5C7-665CB07F4CEB 8 urn:lsid:zoobank.org:author:48E53CF3-71C8-403C-BECD-10B20B3C15B4 Abstract. The study of the Portuguese marine ichthyofauna has a long historical tradition, rooted back in the 18th Century. Here we present an annotated checklist of the marine fishes from Portuguese waters, including the area encompassed by the proposed extension of the Portuguese continental shelf and the Economic Exclusive Zone (EEZ). The list is based on historical literature records and taxon occurrence data obtained from natural history collections, together with new revisions and occurrences. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
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. -
The Nearshore Cradle of Early Vertebrate Diversification Sallan, Lauren; Friedman, Matt; Sansom, Robert; Bird, Charlotte; Sansom, Ivan
University of Birmingham The nearshore cradle of early vertebrate diversification Sallan, Lauren; Friedman, Matt; Sansom, Robert; Bird, Charlotte; Sansom, Ivan DOI: 10.1126/science.aar3689 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Sallan, L, Friedman, M, Sansom, R, Bird, C & Sansom, I 2018, 'The nearshore cradle of early vertebrate diversification', Science, vol. 362, no. 6413, pp. 460-464. https://doi.org/10.1126/science.aar3689 Link to publication on Research at Birmingham portal Publisher Rights Statement: This is the author’s version of the work. It is posted here by permission of the AAAS for personal use, not for redistribution. The definitive version was published in Science on 26th October 2018. DOI: 10.1126/science.aar3689 General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document. -
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 ------ - --- - - - - - --- --- - -- --- - -- - - --- -
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. -
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.