PATTERNS of ECOLOGICAL DIVERSIFICATION in THELODONTS by HUMBERTO G
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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). -
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. -
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. -
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. -
Silurian Thelodonts from the Niur Formation, Central Iran
Silurian thelodonts from the Niur Formation, central Iran VACHIK HAIRAPETIAN, HENNING BLOM, and C. GILES MILLER Hairapetian, V., Blom, H., and Miller, C.G. 2008. Silurian thelodonts from the Niur Formation, central Iran. Acta Palaeontologica Polonica 53 (1): 85–95. Thelodont scales are described from the Silurian Niur Formation in the Derenjal Mountains, east central Iran. The mate− rial studied herein comes from four stratigraphic levels, composed of rocks formed in a shallow water, carbonate ramp en− vironment. The fauna includes a new phlebolepidiform, Niurolepis susanae gen. et sp. nov. of late Wenlock/?early Lud− low age and a late Ludlow loganelliiform, Loganellia sp. cf. L. grossi, which constitute the first record of these thelodont groups from Gondwana. The phlebolepidiform Niurolepis susanae gen. et sp. nov. is diagnosed by having trident trunk scales with a raised medial crown area separated by two narrow spiny wings from the lateral crown areas; a katoporodid− type histological structure distinguished by a network of branched wide dentine canals. Other scales with a notch on a smooth rhomboidal crown and postero−laterally down−stepped lateral rims have many characters in common with Loganellia grossi. Associated with the thelodonts are indeterminable acanthodian scales and a possible dentigerous jaw bone fragment. This finding also provides evidence of a hitherto unknown southward dispersal of Loganellia to the shelves of peri−Gondwana. Key words: Thelodonti, Phlebolepidiformes, Loganelliiformes, palaeobiogeography, Silurian, Niur Formation, Iran. Vachik Hairapetian [[email protected]], Department of Geology, Islamic Azad University, Khorasgan branch, PO Box 81595−158, Esfahan, Iran; Henning Blom [[email protected]], Subdepartment of Evolutionary Organismal Biology, Department of Physiol− ogy and Developmental Biology, Uppsala University, Norbyvägen 18A, SE−752 36 Uppsala, Sweden; C. -
A New Groenlandaspidid Arthrodire (Vertebrata: Placodermi) from the Famennian of Belgium
GEOLOGICA BELGICA (2005) 8/1-2: 51-67 A NEW GROENLANDASPIDID ARTHRODIRE (VERTEBRATA: PLACODERMI) FROM THE FAMENNIAN OF BELGIUM Philippe JANVIER1-2 and Gaël CLÉMENT1 1. UMR 5143 du CNRS, Département «Histoire de la Terre», Muséum National d ’Histoire Naturelle, 8 rue Buffon, 75005 Paris, France. [email protected] 2. Toe Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom (9 figures, 1 table and 2 plates) ABSTRACT. A new species of the arthrodire genus Groenlandaspis is described from the upper part of the Evieux Formation (Upper Famennian), based on several specimens collected from quarries at Modave and Villers-le-Temple, Liège Province, Belgium. It is the first occurrence of this widespread genus in continental Europe. This new species is characterized by an almost smooth dermal armour, except for some scattered tubercles on its skull roof, median dorsal and spinal plates. Its median dorsal plate is triangular in shape and almost perfectly equilateral in lateral aspect and bears large, spiniform denticles on its posterior edge. All these Groenlandaspis remains occur in micaceous, dolomitic claystones or siltstones probably deposited in a subtidal environment. Outcrops of the same area have yielded other vertebrate remains, such as the placoderms Phyllolepis and Bothriolepis, acanthodians, various piscine sarcopterygians (Holoptychius , dipnoans, a rhizodontid, Megalichthys, Eusthenodon and a large tristichopterid), and a tetrapod that is probably close to Ichthyostega. The biogeographical history of the genus Groenlandaspis -
Copyrighted Material
06_250317 part1-3.qxd 12/13/05 7:32 PM Page 15 Phylum Chordata Chordates are placed in the superphylum Deuterostomia. The possible rela- tionships of the chordates and deuterostomes to other metazoans are dis- cussed in Halanych (2004). He restricts the taxon of deuterostomes to the chordates and their proposed immediate sister group, a taxon comprising the hemichordates, echinoderms, and the wormlike Xenoturbella. The phylum Chordata has been used by most recent workers to encompass members of the subphyla Urochordata (tunicates or sea-squirts), Cephalochordata (lancelets), and Craniata (fishes, amphibians, reptiles, birds, and mammals). The Cephalochordata and Craniata form a mono- phyletic group (e.g., Cameron et al., 2000; Halanych, 2004). Much disagree- ment exists concerning the interrelationships and classification of the Chordata, and the inclusion of the urochordates as sister to the cephalochor- dates and craniates is not as broadly held as the sister-group relationship of cephalochordates and craniates (Halanych, 2004). Many excitingCOPYRIGHTED fossil finds in recent years MATERIAL reveal what the first fishes may have looked like, and these finds push the fossil record of fishes back into the early Cambrian, far further back than previously known. There is still much difference of opinion on the phylogenetic position of these new Cambrian species, and many new discoveries and changes in early fish systematics may be expected over the next decade. As noted by Halanych (2004), D.-G. (D.) Shu and collaborators have discovered fossil ascidians (e.g., Cheungkongella), cephalochordate-like yunnanozoans (Haikouella and Yunnanozoon), and jaw- less craniates (Myllokunmingia, and its junior synonym Haikouichthys) over the 15 06_250317 part1-3.qxd 12/13/05 7:32 PM Page 16 16 Fishes of the World last few years that push the origins of these three major taxa at least into the Lower Cambrian (approximately 530–540 million years ago). -
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. -
Ludlow, Silurian) Positive Carbon Isotope Excursion in the Type Ludlow Area, Shropshire, England?
At what stratigraphical level is the mid Ludfordian (Ludlow, Silurian) positive carbon isotope excursion in the type Ludlow area, Shropshire, England? DAVID K. LOYDELL & JIØÍ FRÝDA The balance of evidence suggests that the mid Ludfordian positive carbon isotope excursion (CIE) commences in the Ludlow area, England in the uppermost Upper Whitcliffe Formation, with the excursion continuing into at least the Platyschisma Shale Member of the overlying Downton Castle Sandstone Formation. The Ludlow Bone Bed Member, at the base of the Downton Castle Sandstone Formation has previously been considered to be of Přídolí age. Conodont and 13 thelodont evidence, however, are consistent with the mid Ludfordian age proposed here. New δ Corg data are presented from Weir Quarry, W of Ludlow, showing a pronounced positive excursion commencing in the uppermost Upper Whitcliffe Formation, in strata with a palynologically very strong marine influence. Elsewhere in the world, the mid Ludfordian positive CIE is associated with major facies changes indicated shallowing; the lithofacies evidence from the Ludlow area is consistent with this. There appears not to be a major stratigraphical break at the base of the Ludlow Bone Bed Member. • Key words: Silurian, Ludlow, carbon isotopes, conodonts, chitinozoans, thelodonts, stratigraphy. LOYDELL, D.K. & FRÝDA, J. 2011. At what stratigraphical level is the mid Ludfordian (Ludlow, Silurian) positive car- bon isotope excursion in the type Ludlow area, Shropshire, England? Bulletin of Geosciences 86(2), 197–208 (5 figures, 2 tables). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript received January 17, 2011; accepted in re- vised form March 28, 2011; published online April 13, 2011; issued June 20, 2011. -
Annual Meeting 2002
Newsletter 51 74 Newsletter 51 75 The Palaeontological Association 46th Annual Meeting 15th–18th December 2002 University of Cambridge ABSTRACTS Newsletter 51 76 ANNUAL MEETING ANNUAL MEETING Newsletter 51 77 Holocene reef structure and growth at Mavra Litharia, southern coast of Gulf of Corinth, Oral presentations Greece: a simple reef with a complex message Steve Kershaw and Li Guo Oral presentations will take place in the Physiology Lecture Theatre and, for the parallel sessions at 11:00–1:00, in the Tilley Lecture Theatre. Each presentation will run for a New perspectives in palaeoscolecidans maximum of 15 minutes, including questions. Those presentations marked with an asterisk Oliver Lehnert and Petr Kraft (*) are being considered for the President’s Award (best oral presentation by a member of the MONDAY 11:00—Non-marine Palaeontology A (parallel) Palaeontological Association under the age of thirty). Guts and Gizzard Stones, Unusual Preservation in Scottish Middle Devonian Fishes Timetable for oral presentations R.G. Davidson and N.H. Trewin *The use of ichnofossils as a tool for high-resolution palaeoenvironmental analysis in a MONDAY 9:00 lower Old Red Sandstone sequence (late Silurian Ringerike Group, Oslo Region, Norway) Neil Davies Affinity of the earliest bilaterian embryos The harvestman fossil record Xiping Dong and Philip Donoghue Jason A. Dunlop Calamari catastrophe A New Trigonotarbid Arachnid from the Early Devonian Windyfield Chert, Rhynie, Philip Wilby, John Hudson, Roy Clements and Neville Hollingworth Aberdeenshire, Scotland Tantalizing fragments of the earliest land plants Steve R. Fayers and Nigel H. Trewin Charles H. Wellman *Molecular preservation of upper Miocene fossil leaves from the Ardeche, France: Use of Morphometrics to Identify Character States implications for kerogen formation Norman MacLeod S. -
Silurian and Earliest Devonian Birkeniid Anaspids from the Northern Hemisphere
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/233484471 Silurian and earliest Devonian birkeniid anaspids from the Northern Hemisphere Article in Transactions of the Royal Society of Edinburgh Earth Sciences · June 2002 DOI: 10.1017/S0263593300000250 CITATIONS READS 47 725 3 authors: Henning Blom Tiiu Märss Uppsala University Tallinn University of Technology 429 PUBLICATIONS 3,403 CITATIONS 100 PUBLICATIONS 1,270 CITATIONS SEE PROFILE SEE PROFILE C. Giles Miller Natural History Museum, London 81 PUBLICATIONS 575 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Conodonts from the Silurian and Ordovician of Oman, Saudi Arabia and Iran View project Silurian and Devonian vertebrate microremains View project All content following this page was uploaded by C. Giles Miller on 30 October 2014. The user has requested enhancement of the downloaded file. Transactions of the Royal Society of Edinburgh: Earth Sciences, 92, 263±323, 2002 (for 2001) Silurian and earliest Devonian birkeniid anaspids from the Northern Hemisphere H. Blom, T. MaÈ rss and C. G. Miller ABSTRACT: The sculpture of scales and plates of articulated anaspids from the order Birkeniida is described and used to clarify the position of scale taxa previously left in open nomenclature. The dermal skeleton of a well-preserved squamation of Birkenia elegans Traquair, 1898 from the Silurian of Scotland shows a characteristic ®nely tuberculated sculpture over the whole body. Rhyncholepis parvula Kiñr, 1911, Pterygolepis nitida (Kiñr, 1911) and Pharyngolepis oblonga Kiñr, 1911, from the Silurian of Norway show three other sculpture types.