NATURE 935 the Origin of Land Vertebrates.1 by Prof
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BONY FISHES 602 Bony Fishes
click for previous page BONY FISHES 602 Bony Fishes GENERAL REMARKS by K.E. Carpenter, Old Dominion University, Virginia, USA ony fishes constitute the bulk, by far, of both the diversity and total landings of marine organisms encoun- Btered in fisheries of the Western Central Atlantic.They are found in all macrofaunal marine and estuarine habitats and exhibit a lavish array of adaptations to these environments. This extreme diversity of form and taxa presents an exceptional challenge for identification. There are 30 orders and 269 families of bony fishes presented in this guide, representing all families known from the area. Each order and family presents a unique suite of taxonomic problems and relevant characters. The purpose of this preliminary section on technical terms and guide to orders and families is to serve as an introduction and initial identification guide to this taxonomic diversity. It should also serve as a general reference for those features most commonly used in identification of bony fishes throughout the remaining volumes. However, I cannot begin to introduce the many facets of fish biology relevant to understanding the diversity of fishes in a few pages. For this, the reader is directed to one of the several general texts on fish biology such as the ones by Bond (1996), Moyle and Cech (1996), and Helfman et al.(1997) listed below. A general introduction to the fisheries of bony fishes in this region is given in the introduction to these volumes. Taxonomic details relevant to a specific family are explained under each of the appropriate family sections. The classification of bony fishes continues to transform as our knowledge of their evolutionary relationships improves. -
Amblyopsidae, Amblyopsis)
A peer-reviewed open-access journal ZooKeys 412:The 41–57 Hoosier(2014) cavefish, a new and endangered species( Amblyopsidae, Amblyopsis)... 41 doi: 10.3897/zookeys.412.7245 RESEARCH ARTICLE www.zookeys.org Launched to accelerate biodiversity research The Hoosier cavefish, a new and endangered species (Amblyopsidae, Amblyopsis) from the caves of southern Indiana Prosanta Chakrabarty1,†, Jacques A. Prejean1,‡, Matthew L. Niemiller1,2,§ 1 Museum of Natural Science, Ichthyology Section, 119 Foster Hall, Department of Biological Sciences, Loui- siana State University, Baton Rouge, Louisiana 70803, USA 2 University of Kentucky, Department of Biology, 200 Thomas Hunt Morgan Building, Lexington, KY 40506, USA † http://zoobank.org/0983DBAB-2F7E-477E-9138-63CED74455D3 ‡ http://zoobank.org/C71C7313-142D-4A34-AA9F-16F6757F15D1 § http://zoobank.org/8A0C3B1F-7D0A-4801-8299-D03B6C22AD34 Corresponding author: Prosanta Chakrabarty ([email protected]) Academic editor: C. Baldwin | Received 12 February 2014 | Accepted 13 May 2014 | Published 29 May 2014 http://zoobank.org/C618D622-395E-4FB7-B2DE-16C65053762F Citation: Chakrabarty P, Prejean JA, Niemiller ML (2014) The Hoosier cavefish, a new and endangered species (Amblyopsidae, Amblyopsis) from the caves of southern Indiana. ZooKeys 412: 41–57. doi: 10.3897/zookeys.412.7245 Abstract We describe a new species of amblyopsid cavefish (Percopsiformes: Amblyopsidae) in the genus Amblyopsis from subterranean habitats of southern Indiana, USA. The Hoosier Cavefish, Amblyopsis hoosieri sp. n., is distinguished from A. spelaea, its only congener, based on genetic, geographic, and morphological evi- dence. Several morphological features distinguish the new species, including a much plumper, Bibendum- like wrinkled body with rounded fins, and the absence of a premature stop codon in the gene rhodopsin. -
Batoid Locomotion: Effects of Speed on Pectoral Fin Deformation in the Little Skate, Leucoraja Erinacea Valentina Di Santo1,*, Erin L
© 2017. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2017) 220, 705-712 doi:10.1242/jeb.148767 RESEARCH ARTICLE Batoid locomotion: effects of speed on pectoral fin deformation in the little skate, Leucoraja erinacea Valentina Di Santo1,*, Erin L. Blevins1,2 and George V. Lauder1 ABSTRACT more efficient at higher speeds and for long-distance translocations Most batoids have a unique swimming mode in which thrust is (Di Santo and Kenaley, 2016). Although many batoid species are generated by either oscillating or undulating expanded pectoral fins accurately described by these two extreme modes, several species that form a disc. Only one previous study of the freshwater stingray has fall into a continuum between 0.5 and 1.0 wave, and are defined as quantified three-dimensional motions of the wing, and no comparable ‘semi-oscillators’ (Schaefer and Summers, 2005). data are available for marine batoid species that may differ The mechanics of propulsion in cartilaginous fishes have been considerably in their mode of locomotion. Here, we investigate three- investigated over the years through studies of morphology, dimensional kinematics of the pectoral wing of the little skate, kinematics, hydrodynamics, muscle activity and energetics Leucoraja erinacea, swimming steadily at two speeds [1 and (Daniel, 1988; Di Santo and Kenaley, 2016; Donley and 2 body lengths (BL) s−1]. We measured the motion of nine points in Shadwick, 2003; Fontanella et al., 2013; Lauder, 2015; Lauder three dimensions during wing oscillation and determined that there are and Di Santo, 2015; Porter et al., 2011; Rosenberger and Westneat, significant differences in movement amplitude among wing locations, 1999; Rosenblum et al., 2011). -
Université Du Québec
UNIVERSITÉ DU QUÉBEC PRÉCISIONS SUR L'ANATOMIE DE L'OSTÉOLÉPIFORME EUSTHENOPTERON FOORDI DU DÉVONIEN SUPÉRIEUR DE MIGUASHA, QUÉBEC MÉMOIRE PRÉSENTÉ À L'UNIVERSITÉ DU QUÉBEC À RIMOUSKI Comme exigence partielle du programme de Maîtrise en Gestion de la Faune et de ses Habitats PAR JOËL LEBLANC Août 2005 UNIVERSITÉ DU QUÉBEC À RIMOUSKI Service de la bibliothèque Avertissement La diffusion de ce mémoire ou de cette thèse se fait dans le respect des droits de son auteur, qui a signé le formulaire « Autorisation de reproduire et de diffuser un rapport, un mémoire ou une thèse ». En signant ce formulaire, l’auteur concède à l’Université du Québec à Rimouski une licence non exclusive d’utilisation et de publication de la totalité ou d’une partie importante de son travail de recherche pour des fins pédagogiques et non commerciales. Plus précisément, l’auteur autorise l’Université du Québec à Rimouski à reproduire, diffuser, prêter, distribuer ou vendre des copies de son travail de recherche à des fins non commerciales sur quelque support que ce soit, y compris l’Internet. Cette licence et cette autorisation n’entraînent pas une renonciation de la part de l’auteur à ses droits moraux ni à ses droits de propriété intellectuelle. Sauf entente contraire, l’auteur conserve la liberté de diffuser et de commercialiser ou non ce travail dont il possède un exemplaire. 11 TABLE DES MATIÈRES TABLE DES MATIÈRES .... ..... ............................. .. ...... .. .... .. .... ........... ... ............................. .ii LISTE DES TABLEAUX .. ............ -
Tetrapods, Amphibians, and Life on Land
Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Strolling through life Tetrapods, amphibians, and life on land Tetrapods - the clade of four- limbed terrestrial vertebrates Living tetrapod groups: * amphibians * mammals (including humans) * lizards and snakes * crocodilians * birds Eurypos , early Permian temnospondyl (painting by Douglas Henderson, 1990) Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Lobe-finned fish (Sarcopterygia) Living coelacanth Fossil sarcopterygians Late Cretaceous (ca. 65 mya) Carboniferous (ca. 300 mya) Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Comparison of pectoral fins Actinopterygian Sarcopterygian (ray finned) (lobe finned) Scapulocoracoid Humerus Ulna Radius Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Coelacanth pectoral fins Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Ancestral characteristics of living tetrapods • Pelvic and pectoral girdles • Forelimb with humerus, radius, and ulna bones • Hindlimb with femur, tibia, and fibula bones • five digits on the feet • sprawling posture • undulating locomotion • skull with no fenestra Department of Geological Sciences | Indiana University Dinosaurs and their relatives (c) 2015, P. David Polly Geology G114 Tetrapoda: vertebrates more closely related to living Phylogeny of Bony Fish amphibians and amniotes than to their nearest living relatives Fossil taxa coelocanths and Fish-like amphibian-like lung fish Tetrapods Tetrapods Actinopterygia Coelocanths Dipnoans (lungfish) Osteolepis Eusthenopteron Pandericthyes Acanthostega Icthyostega tetrapods Derived Tetrapoda Sarcopterygia Osteichthyes After Coates and Ruta, 2007. -
Identifying Heterogeneity in Rates of Morphological Evolution: Discrete Character Change in the Evolution of Lungfish (Sarcopterygii; Dipnoi)
ORIGINAL ARTICLE doi:10.1111/j.1558-5646.2011.01460.x IDENTIFYING HETEROGENEITY IN RATES OF MORPHOLOGICAL EVOLUTION: DISCRETE CHARACTER CHANGE IN THE EVOLUTION OF LUNGFISH (SARCOPTERYGII; DIPNOI) Graeme T. Lloyd,1,2 Steve C. Wang,3 and Stephen L. Brusatte4,5 1Department of Palaeontology, Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom 2E-mail: [email protected] 3Department of Mathematics and Statistics, Swarthmore College, Swarthmore, Pennsylvania 19081 4Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024 5Department of Earth and Environmental Sciences, Columbia University, New York, New York 10025 Received February 9, 2010 Accepted August 15, 2011 Data Archived: Dryad: doi:10.5061/dryad.pg46f Quantifying rates of morphological evolution is important in many macroevolutionary studies, and critical when assessing possible adaptive radiations and episodes of punctuated equilibrium in the fossil record. However, studies of morphological rates of change have lagged behind those on taxonomic diversification, and most authors have focused on continuous characters and quantifying patterns of morphological rates over time. Here, we provide a phylogenetic approach, using discrete characters and three statistical tests to determine points on a cladogram (branches or entire clades) that are characterized by significantly high or low rates of change. These methods include a randomization approach that identifies branches with significantly high rates and likelihood ratio tests that pinpoint either branches or clades that have significantly higher or lower rates than the pooled rate of the remainder of the tree. As a test case for these methods, we analyze a discrete character dataset of lungfish, which have long been regarded as “living fossils” due to an apparent slowdown in rates since the Devonian. -
A New Osteolepidid Fish From
Rea. West. Aust. MU8. 1985, 12(3): 361-377 ANew Osteolepidid Fish from the Upper Devonian Gogo Formation, Western Australia J.A. Long* Abstract A new osteolepidid crossopterygian, Gogonasus andrewsi gen. et sp. nov., is des cribed from a single fronto-ethmoidal shield and associated ethmosphenoid, from the Late Devonian (Frasnian) Gogo Formation, Western Australia. Gogonasus is is distinguished from other osteolepids by the shape and proportions of the fronto ethmoidal shield, absence of palatal fenestrae, well developed basipterygoid pro cesses and moderately broad parasphenoid. The family Osteolepididae is found to be paraphyletic, with Gogonasus being regarded as a plesiomorphic osteolepidid at a similar level of organisation to Thursius. Introduction Much has been published on the well-preserved Late Devonian fish fauna from the Gogo Formation, Western Australia, although to date all the papers describing fish have been on placoderms (Miles 1971; Miles and Dennis 1979; Dennis and Miles 1979-1983; Young 1984), palaeoniscoids (Gardiner 1973, 1984; Gardiner and Bartram 1977) or dipnoans (Miles 1977; Campbell and Barwick 1982a, 1982b, 1983, 1984a). This paper describes the only osteolepiform from the fauna (Gardiner and Miles 1975), a small snout with associated braincase, ANU 21885, housed in the Geology Department, Australian National University. The specimen, collected by the Australian National University on the 1967 Gogo Expedition, was prepared by Dr S.M. Andrews (Royal Scottish Museum) and later returned to the ANU. Onychodus is the only other crossopterygian in the fauna. In its proportions and palatal structure the new specimen provides some additional new points of the anatomy of osteolepiforms. Few Devonian crossopte rygians are known from Australia, and so the specimen is significant in having resemblances to typical Northern Hemisphere species. -
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. -
Gobiodon Winterbottomi, a New Goby (Actinopterygii: Perciformes: Gobiidae) from Iriomote-Jima Island, the Ryukyu Islands, Japan
Bull. Natl. Mus. Nat. Sci., Ser. A, Suppl. 6, pp. 59–65, March 30, 2012 Gobiodon winterbottomi, a New Goby (Actinopterygii: Perciformes: Gobiidae) from Iriomote-jima Island, the Ryukyu Islands, Japan Toshiyuki Suzuki1, Korechika Yano2 and Hiroshi Senou3 1 Kawanishi-midoridai Senior High School, 1–8 Kouyoudai, Kawanishi, Hyogo 666–0115, Japan E-mail: [email protected] 2 Dive Service Yano, 537 Uehara, Taketomi-cho, Okinawa 907–1541, Japan 3 Kanagawa Prefectural Museum of Natural History, 499 Iryuda, Odawara, Kanagawa 250–0031, Japan E-mail: [email protected] Abstract The gobiid ¿sh Gobiodon winterbottomi is described as a new species from three spec- imens (19.0–32.9 mm SL) collected from Echinopora lamellose, the plate-shaped coral of the fam- ily Faviidae, in 5 m depth on the reef slope off Iriomote-jima Island, the Ryukyu Islands, Japan. It is characterized by the following in combination: the jaw teeth subequal in shape and size; lack of post-symphysial canine teeth; lack of an interopercle-isthmus groove; a narrow gill opening; lack of elongated dorsal-¿n spines; large second dorsal, anal and pelvic ¿ns; 15 or 16 pectoral-¿n rays; and head, body and ¿ns gray, absence of stripes or other markings when fresh or alive. Key words: Gobiodon winterbottomi, new species, Gobiidae, Ryukyu Islands, Japan. Gobiodon Bleeker, 1856 is an Indo-Paci¿c Sawada and Arai, 1972 (validity questionable), gobiid ¿sh genus, comprising often colorful, Gobiodon axillaris De Viz, 1884, Gobiodon bro- tropical species living in obligate commensal chus (Harold and Winterbottom, 1999), Gobio- association with reef-building corals. -
Oxyeleotris Colasi (Teleostei: Eleotridae), a New Blind Cave Fish from Lengguru in West Papua, Indonesia
Oxyeleotris colasi (Teleostei: Eleotridae), a new blind cave fish from Lengguru in West Papua, Indonesia by Laurent POUYAUD* (1), KADARUSMAN (1, 2), Renny K. HADIATY (3), Jacques SLEMBROUCK (1), Napoleon LEMAUK (4), Ruby V. KUSUMAH (5) & Philippe KEITH (6) ABSTRACT. - Oxyeleotris colasi is the first hypogean fish recorded from West Papua. The habitat consists of a freshwater pool in the cave of Jabuenggara located in the heart of Seraran anticline in the limestone karst of Lengguru. The new spe- cies is most closely related to the blind cave fishO. caeca described by Allen (1996) from eastern New Guinea. The two troglomorphic species are hypothesised to be related to O. fimbriata, an epigean freshwater gudgeon that ranges widely in New Guinea and northern Australia (Allen, 1996). Oxyeleotris colasi differs from its congeners by the absence of eyes, its skin and fins being totally depigmented, the presence of a well developed sensory papillae system partly consisting of low raised fleshy ridges on each side of the head, a reduced number of cephalic sensory pores, a reduced number of scales on head and body, a long head with a short snout length, a narrow mouth width and a long upper jaw length, body shape with a shallow anterior body depth and narrow body width, a long and deep caudal peduncle, long predorsal and prepectoral lengths, and a long pectoral fin. RÉSUMÉ. - Oxyeleotris colasi, une nouvelle espèce de poisson cavernicole de Lengguru en Papouasie occidentale (Teleostei : Eleotridae). Oxyeleotris colasi est la première espèce de poisson hypogée décrite de Papouasie occidentale. Elle a été capturée dans un trou d’eau douce situé dans la grotte de Jabuenggara au cœur de l’anticlinal de Seraran dans le karst de Lengguru. -
A Redescription of the Lungfish Eoctenodus Hills 1929, with Reassessment of Other Australian Records of the Genus Dipterns Sedgwick & Murchison 1828
Ree. West. Aust. Mus. 1987, 13 (2): 297-314 A redescription of the lungfish Eoctenodus Hills 1929, with reassessment of other Australian records of the genus Dipterns Sedgwick & Murchison 1828. J.A. Long* Abstract Eoctenodus microsoma Hills 1929 (= Dipterus microsoma Hills, 1931) from the Frasnian Blue Range Formation, near Taggerty, Victoria, is found to be a valid genus, differing from Dipterus, and other dipnoans, by the shape of the parasphenoid and toothplates. The upper jaw toothp1ates and entopterygoids, parasphenoid, c1eithrum, anoc1eithrum and scales of Eoctenodus are described. Eoctenodus may represent the earliest member of the Ctenodontidae. Dipterus cf. D. digitatus. from the Late Devonian Gneudna Formation, Western Australia (Seddon, 1969), is assigned to Chirodipterus australis Miles 1977; and Dipterus sp. from the Late Devonian of Gingham Gap, New South Wales (Hills, 1936) is thought to be con generic with a dipnoan of similar age from the Hunter Siltstone, New South Wales. This form differs from Dipterus in the shape of the parasphenoid. The genus Dipterus appears to be restricted to the Middle-Upper Devonian of Europe, North America and the USSR (Laurasia). Introduction Although Hills (1929) recognised a new dipnoan, Eoctenodus microsoma, in the Late Devonian fish remains from the Blue Range Formation, near Taggerty, he later (Hills 1931) altered the generic status of this species after a study trip to Britain in which D,M.S. Watson pointed out similarities between the Australian form and the British genus Dipterus Sedgwick and Murchison 1828. Studies of the head of Dipterus by Westoll (1949) and White (1965) showed the structure of the palate and, in particular, the shape of the parasphenoid which differs from that in the Taggerty dipnoan. -
The Devonian Tetrapod Acanthostega Gunnari Jarvik: Postcranial Anatomy, Basal Tetrapod Interrelationships and Patterns of Skeletal Evolution M
Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, 363-421, 1996 The Devonian tetrapod Acanthostega gunnari Jarvik: postcranial anatomy, basal tetrapod interrelationships and patterns of skeletal evolution M. I. Coates ABSTRACT: The postcranial skeleton of Acanthostega gunnari from the Famennian of East Greenland displays a unique, transitional, mixture of features conventionally associated with fish- and tetrapod-like morphologies. The rhachitomous vertebral column has a primitive, barely differentiated atlas-axis complex, encloses an unconstricted notochordal canal, and the weakly ossified neural arches have poorly developed zygapophyses. More derived axial skeletal features include caudal vertebral proliferation and, transiently, neural radials supporting unbranched and unsegmented lepidotrichia. Sacral and post-sacral ribs reiterate uncinate cervical and anterior thoracic rib morphologies: a simple distal flange supplies a broad surface for iliac attachment. The octodactylous forelimb and hindlimb each articulate with an unsutured, foraminate endoskeletal girdle. A broad-bladed femoral shaft with extreme anterior torsion and associated flattened epipodials indicates a paddle-like hindlimb function. Phylogenetic analysis places Acanthostega as the sister- group of Ichthyostega plus all more advanced tetrapods. Tulerpeton appears to be a basal stem- amniote plesion, tying the amphibian-amniote split to the uppermost Devonian. Caerorhachis may represent a more derived stem-amniote plesion. Postcranial evolutionary trends spanning the taxa traditionally associated with the fish-tetrapod transition are discussed in detail. Comparison between axial skeletons of primitive tetrapods suggests that plesiomorphic fish-like morphologies were re-patterned in a cranio-caudal direction with the emergence of tetrapod vertebral regionalisation. The evolution of digited limbs lags behind the initial enlargement of endoskeletal girdles, whereas digit evolution precedes the elaboration of complex carpal and tarsal articulations.