General Chharacters and Classification of Chondrichthyes

Total Page:16

File Type:pdf, Size:1020Kb

General Chharacters and Classification of Chondrichthyes GENERAL CHHARACTERS AND CLASSIFICATION OF CHONDRICHTHYES Subject – Zoology, Class - B.Sc. Part – II(Hons. and Subsi.) Paper – III(Hons.) & II(Subsi.) By:- KUNDAN PATEL Guest Faculty Department of Zoology, B.N. College, Patna INTRODUCTION Chondrichthyes includes cartilaginous fishes having cartilaginous endoskeleton. It includes some of the prominently known fishes like sharks, rays and chimaeras. Although these are cartilaginous, they have a wide range of adaptations on the earth. Let us see some of the prominent features and classification oh these fishes. GENERAL CHARACTERS OF CHONDRICHTHYES ● Comprise living sharks, rays and chimeras ● Marine, cold-blooded animals with streamlined body ● Have cartilaginous endoskeleton. The entire spinal column may be almost completely cartilaginous(Hexanchus and Heptranchias) ● Mouth is located ventrally ● Notochord is persistent throughout life ● Gill slits are separate and without operculum ● The skin is tough, containing placoid scales ● Teeth are modified placoid scales which are backwardy directed GENERAL CHARACTERS OF CHONDRICHTHYES ● Have powerful jaws ● Well-developed median and paired fins ● Caudal fin is large, and strongly heterocercal in the sharks and shark-like rays ● Predaceous animals ● They don’t have air bladder so they have to swim constantly to avoid sinking ● Have two-chambered heart; a rhythmically contractile conus arteriosus with several transverse rows of valves is always well- developed GENERAL CHARACTERS OF CHONDRICHTHYES ● Some have electric organs and some possess poison sting ● Sexes are separate. In males pelvic fins bear claspers ● Internal fertilization and many are viviparous ● Aperture of cloaca serves as a common outlet for the rectum and the renal and reproductive ducts ● The flattened form of the rays is an adaptation to bottom-dweling existence. E.g. – Manta – width of 22 feet, diamond-shaped body GENERAL CHARACTERS OF CHONDRICHTHYES ● In some cases, the head is produced forwards into a long rostrum. This is of great length and bordered with triangular teeth in the sawsharks(Pristiopherus) and saw fishes(Pristis) ● In the rays, dorsal fin is usually small, and the anal fin absent, pectoral fins are extremely large and much bigger than the pelvic fins, and the pectoral fins fringe the greater part of the length of the flattened body, and are prolonged forwards on either side and even in front of the head ● Along each side of the neck in the sharks, and on the ventral surface in the rays, there is a row of slit-like apertures – the branchial slits or clefts. These are usually 5 in number on each side but in Pliotrema, hexanchus, and chlamydoselachus, these are 6 in number and 7 in heptranchis GENERAL CHARACTERS OF CHONDRICHTHYES ● Truly cartilaginous fishes do not seem to have appeared before mid-Devonian ● It is likely that the elasmobranchs arose from a bony ancestor, and perhaps by neoteny ● Largest living shark – oviparous whale shark(Rhinodon) – nearly 70 feet, Basking shark(Cetorhinus) – app. 40 feet, great white shark or white pointer(Carcharodon carcharias) – man-eating – 36 feet; tiger shark(Galeocerdo) – 16 feet; grey nurse(Carcharias) – 9 feet; blue pointer or Mako(Isuropsis) – 13 feet GENERAL CHARACTERS OF CHONDRICHTHYES Placoid scales:- ● They are called dermal denticles ● Structurally homologous with vertebrate teeth, having a central pulp cavity supplied with blood vessels, surrounded by a conical layer of dentine, all of which sits on top of a rectangular basal plate that rests on dermis ● Cannot grow in size rather its number increases as the size of the fish increases ● It is a source of rawhide leather, called shagreen, used in making hand-grips for swords GENERAL CHARACTERS OF CHONDRICHTHYES GENERAL CHARACTERS OF CHONDRICHTHYES Sting:- ● A dangerous integumentary structure ● One or several deciduous spines, capable of independent movement, are attached some distance up the tail ● Grooves in the spine carry toxic secretions from continuous glands ● Sting-rays produce agonizing(causing great pain) wounds and hideous scarring ● A large ray may slash right down to the bone and often results into septicaemia. In 1938, a Newzealand girl aged 18 was killed by stab-wounds from a fish that was almost certainly a sting-ray. In addition to inflicting three thigh wounds, the spine penetrated the thorax and both ventricles of the head GENERAL CHARACTERS OF CHONDRICHTHYES GENERAL CHARACTERS OF CHONDRICHTHYES CLASSIFICATION OF CHONDRICHTHYES The class chondrichthyes has been classified into two subclasses(Romer, 1959):- Subclass – 1. Selacchii:- ● It includes modern sharks ● The giils are placed in separate clefts and a spiracle is present behind each eye Order – 1. Cladoselachii:- ● Shark-like, fusiform ● Became extinct in Devonian to Permian periods and is the ancestor of all modern sharks ● Tail heterocercal with a large lower lobe, and a horizontal keel-like fin on each side of the caudal peduncle ● Pectoral, pelvic and two dorsal fins were very prominent ● The large sub-terminal mouth, long sharp teeth, relatively enormous forwardly directed eyes, body covered with small denticles, amphistylic jaw suspension, a well-developed postorbital process, paired nostrils and absence of claspers ● E.g. – cladoselache, cladodus, symmorium, diademonus, etc. CLASSIFICATION OF CHONDRICHTHYES CLASSIFICATION OF CHONDRICHTHYES Order – 2. Pleuacanthodii:- ● Slender, fresh water, shark-like fishes having dorsal fin extending along the body and tail ● It became extinct in Triassic period ● The pectoral fins are paddle-like, having long axis with pre- and post-axial rays ● The tail is diphycercal with equally developed blades of fin above and below the notochord ● A long spine on the head and claspers are present in male ● E.g. – Pleurocanthus CLASSIFICATION OF CHONDRICHTHYES Order – 3. Protoselachii:- ● The pectoral fin is notched at the posterior margin ● Claspers present in male ● Two types of teeth – one sharply pointed, located anteriorly and the other flat type placed behind for crushing molluscan shells ● They flourished in Palaeozoic seas and became extinct in Permian to Triassic period ● E.g. – Hybodus, Heterodontus, etc. Order – 4. Euselachii:- ● Shark and rays constituting this order are abundant in equatorial and temperate seas ● Teeth numerous, developed in continual succession ● Pectoral fins have three basal pieces, the pro-, meso- and metapterygium, from which a number of pre-axial radials spread out ● E.g. – chlamydoselachus, Heptranchius, Hexanchus, squalus, Pristis, Torpedo, Manta, etc. CLASSIFICATION OF CHONDRICHTHYES CLASSIFICATION OF CHONDRICHTHYES CLASSIFICATION OF CHONDRICHTHYES Subclass – 2. Bradyodonti:- ● Vertebrae are reduced to nodules ● Teeth are firmly attached to the jaws and modified into crushing plates ● Notochord remains unconstricted Order – 1. Eubradyonti:- ● Primitive bradyonts ● The teeth are few and fuse to form flattened crushing teeth ● The nature of vertebrae, mode of jaw suspension and cleavage pattern are primitive ● They became extinct at the end of Palaeozoic era ● E.g. – cochliodus, psammodus, helodus, etc. CLASSIFICATION OF CHONDRICHTHYES Order – 2. Holocephali:- ● Deep sea forms with claspers in male and large egg cases in females ● The skin is naked except for a few denticles restricted to the head claspers ● Jaw suspension holostylic, the upper jaw being immovably united with cranium ● Neither skull mor jaw are attached to hyoid arch ● The extra claspers are on the head and in front of the ordinary pair on the abdomen ● Cloaca and spiracle absent ● An operculum covers the gills ● The teeth are in the form of plates ● The first dorsal fin is far forward with strong spine ● The tail is slender and whip-like ● E.g. – chimaera, harriotta, callorhynchus, etc. CLASSIFICATION OF CHONDRICHTHYES CONCLUSION Cartilaginous fishes have a certain unique features compared to other fishes or other vertebrates. They have been classified into various subclasses and orders depending upon the variations in features and a large number of extinct species have also been included in the classification. They cannot be considered inferior in the race of evolution rather some of the forms like sharks seem to be very advanced in its size and strength. BIBLIOGRAPHY & REFERENCES 1. Chordate Zoology - E.L. Jordan and Dr. P.S. Verma 2. Vertebrates - R.L.Kotpal 3. A textbook of Zoology(Vol.II) – Parker and Haswell 4. Biology of Animals(Vol.II) - Sinha, Adhikari and Ganguli THANK YOU.
Recommended publications
  • Symmoriiform Sharks from the Pennsylvanian of Nebraska
    Acta Geologica Polonica, Vol. 68 (2018), No. 3, pp. 391–401 DOI: 10.1515/agp-2018-0009 Symmoriiform sharks from the Pennsylvanian of Nebraska MICHAŁ GINTER University of Warsaw, Faculty of Geology, Żwirki i Wigury 93, PL-02-089 Warsaw, Poland. E-mail: [email protected] ABSTRACT: Ginter, M. 2018. Symmoriiform sharks from the Pennsylvanian of Nebraska. Acta Geologica Polonica, 68 (3), 391–401. Warszawa. The Indian Cave Sandstone (Upper Pennsylvanian, Gzhelian) from the area of Peru, Nebraska, USA, has yielded numerous isolated chondrichthyan remains and among them teeth and dermal denticles of the Symmoriiformes Zangerl, 1981. Two tooth-based taxa were identified: a falcatid Denaea saltsmani Ginter and Hansen, 2010, and a new species of Stethacanthus Newberry, 1889, S. concavus sp. nov. In addition, there occur a few long, monocuspid tooth-like denticles, similar to those observed in Cobelodus Zangerl, 1973, probably represent- ing the head cover or the spine-brush complex. A review of the available information on the fossil record of Symmoriiformes has revealed that the group existed from the Late Devonian (Famennian) till the end of the Middle Permian (Capitanian). Key words: Symmoriiformes; Microfossils; Carboniferous; Indian Cave Sandstone; USA Midcontinent. INTRODUCTION size and shape is concerned [compare the thick me- dian cusp, almost a centimetre long, in Stethacanthus The Symmoriiformes (Symmoriida sensu Zan- neilsoni (Traquair, 1898), and the minute, 0.5 mm gerl 1981) are a group of Palaeozoic cladodont sharks wide, multicuspid, comb-like tooth of Denaea wangi sharing several common characters: relatively short Wang, Jin and Wang, 2004; Ginter et al. 2010, figs skulls, large eyes, terminal mouth, epicercal but ex- 58A–C and 61, respectively].
    [Show full text]
  • 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.
    [Show full text]
  • Chondrichthyan Fauna of the Frasnian–Famennian Boundary Beds in Poland
    Chondrichthyan fauna of the Frasnian–Famennian boundary beds in Poland MICHAŁ GINTER Michał Ginter. 2002. Chondrichthyan fauna of the Frasnian–Famennian boundary beds in Poland. Acta Palaeontologica Polonica 47 (2): 329–338. New chondrichthyan microremains from several Frasnian–Famennian sections in the Holy Cross Mountains and Dębnik area (Southern Poland) are investigated and compared to previous data. The reaction of different groups of chondrichthyans to environmental changes during the Kellwasser Event is analysed. Following the extinction of phoebodont sharks of Phoebodus bifurcatus group before the end of the Frasnian, only two chondrichthyan species, viz. Protacrodus vetustus Jaekel, 1921 and Stethacanthus resistens sp. nov. (possibly closely related to “Cladodus” wildungensis Jaekel, 1921), occur in the upper part of Frasnian Palmatolepis linguiformis conodont Zone and persist into the Famennian. Global cooling is considered a possible cause of the extinction of Frasnian subtropical phoe− bodonts on Laurussian margins. Key words: Chondrichthyes, Kellwasser Event, Devonian, Poland. Michał Ginter [[email protected]], Instytut Geologii Podstawowej, Uniwersytet Warszawski, Żwirki i Wigury 93, PL−02−089 Warszawa, Poland. Introduction Characteristics of the localities Chondrichthyan faunas of the late Palmatolepis linguiformis Three sections spanning the Frasnian–Famennian boundary and the Palmatolepis triangularis conodont zones on south− were sampled bed by bed (for location of most samples, see ern Laurussian margins substantially differ from those of the Racka 2000): the middle wall of the Kowala–Wola Quarry in rest of the Frasnian and Famennian. The main difference is the south−western Holy Cross Mts, south of Kielce; an artficial the absence of Phoebodus, a typical Mid− to Late Devonian trench on the eastern bank of Łagowica River, between the vil− pelagic, shelf dwelling shark (Ginter and Ivanov 1992).
    [Show full text]
  • 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.
    [Show full text]
  • From the Sülstorf Beds (Chattian, Late Oligocene) of the Southeastern North Sea Basin, Northern Germany
    ARTICLE Two new scyliorhinid shark species (Elasmobranchii, Carcharhiniformes, Scyliorhinidae), from the Sülstorf Beds (Chattian, Late Oligocene) of the southeastern North Sea Basin, northern Germany THOMAS REINECKE Auf dem Aspei 33, D-44801 Bochum, Germany E-mail: [email protected] Abstract: Based on isolated teeth two new scyliorhinid shark species, Scyliorhinus biformis nov. sp. and Scyliorhinus suelstorfensis nov. sp., are described from the Sülstorf Beds, early to middle Chattian, of Mecklenburg, north-eastern Germany. They form part of a speciose assemblage of nectobenthic sharks and batoids which populated the warm-temperate to subtropical upper shelf sea of the south-eastern North Sea Basin. Keywords: Scyliorhinus, Scyliorhinidae, Elasmobranchii, Chattian, North Sea Basin. Submitted 14 February 2014, Accepted 14 April 2014 © Copyright Thomas Reinecke April 2014 INTRODUCTION of the south-eastern North Sea Basin (Von Bülow & Müller, 2004; Standke et al., 2005). The succession comprises the early Chattian basal Plate Beds (0-20 m), the early to middle Chat- Elasmobranch assemblages of the Chattian in the boreal pro- tian Sülstorf Beds (ca. 80 m), and the late Chattian Rogahn vince are comparably less well studied than those of the Rupe- Beds (ca. 30 m thick; Von Bülow, 2000). Whereas the Plate lian and Neogene. This is mainly due to the limited access to Beds consist of fossil-poor, silty clays and silts, continuing the Chattian deposits which have very localized occurrences and basin-type sedimentation of the underlying Rupel Clay, the were only temporarily exposed in the northern peripheral zo- Sülstorf Beds (= “Sülstorfer Schichten”, Lotsch, 1981) are a nes of the Mesozoic low mountain ranges of Lower Saxony sequence of calcareous silts containing glauconite and white (Doberg, Astrup), and Hesse (Ahnetal, Glimmerode, Nieder- mica, that are coarsening upwards into well sorted fine sands.
    [Show full text]
  • Class Wars: Chondrichthyes and Osteichthyes Dominance in Chesapeake Bay, 2002-2012
    Class Wars: Chondrichthyes and Osteichthyes dominance in Chesapeake Bay, 2002-2012. 01 July 2013 Introduction The objective of this analysis was to demonstrate a possible changing relationship between two Classes of fishes, Osteichthyes (the bony fishes) and Chondrichthyes (the cartilaginous fishes) in Chesapeake Bay based on 11 years of monitoring. If any changes between the two Classes appeared to be significant, either statistically or anecdotally, the data were explored further in an attempt to explain the variation. The Class Osteichthyes is characterized by having a skeleton made of bone and is comprised of the majority of fish species worldwide, while the Chondrichthyes skeleton is made of cartilage and is represented by the sharks, skates, and rays (the elasmobranch fishes) and chimaeras1. Many shark species are generally categorized as apex predators, while skates and rays and some smaller sharks can be placed into the mesopredator functional group (Myers et al., 2007). By definition, mesopredators prey upon a significant array of lower trophic groups, but also serve as the prey base for apex predators. Global demand for shark and consequential shark fishing mortality, estimated at 97 million sharks in 2010 (Worm et al., 2013), is hypothesized to have contributed to the decline of these apex predators in recent years (Baum et al., 2003 and Fowler et al., 2005), which in turn is suggested to have had a cascading effect on lower trophic levels—an increase in mesopredators and subsequent decrease in the prey base (Myers et al., 2007). According to 10 years of trawl survey monitoring of Chesapeake Bay, fish species composition of catches has shown a marked change over the years (Buchheister et al., 2013).
    [Show full text]
  • Paleogene Origin of Planktivory in the Batoidea
    Paleogene Origin Of Planktivory In The Batoidea CHARLIE J. UNDERWOOD, 1+ MATTHEW A. KOLMANN, 2 and DAVID J. WARD 3 1Department of Earth and Planetary Sciences, Birkbeck, University of London, UK, [email protected]; 2 Department of Ecology and Evolutionary Biology, University of Toronto, Canada, [email protected]; 3Department of Earth Sciences, Natural History Museum, London, UK, [email protected] +Corresponding author RH: UNDERWOOD ET AL.—ORIGIN OF PLANKTIVOROUS BATOIDS 1 ABSTRACT—The planktivorous mobulid rays are a sister group to, and descended from, rhinopterid and myliobatid rays which possess a dentition showing adaptations consistent with a specialized durophageous diet. Within the Paleocene and Eocene there are several taxa which display dentitions apparently transitional between these extreme trophic modality, in particular the genus Burnhamia. The holotype of Burnhamia daviesi was studied through X-ray computed tomography (CT) scanning. Digital renderings of this incomplete but articulated jaw and dentition revealed previously unrecognized characters regarding the jaw cartilages and teeth. In addition, the genus Sulcidens gen. nov. is erected for articulated dentitions from the Paleocene previously assigned to Myliobatis. Phylogenetic analyses confirm Burnhamia as a sister taxon to the mobulids, and the Mobulidae as a sister group to Rhinoptera. Shared dental characters between Burnhamia and Sulcidens likely represent independent origins of planktivory within the rhinopterid – myliobatid clade. The transition from highly-specialized durophagous feeding morphologies to the morphology of planktivores is perplexing, but was facilitated by a pelagic swimming mode in these rays and we propose through subsequent transition from either meiofauna-feeding or pelagic fish-feeding to pelagic planktivory.
    [Show full text]
  • The Absence of Sharks from Abyssal Regions of the World's Oceans
    Proc. R. Soc. B (2006) 273, 1435–1441 doi:10.1098/rspb.2005.3461 Published online 21 February 2006 The absence of sharks from abyssal regions of the world’s oceans Imants G. Priede1,*, Rainer Froese2, David M. Bailey3, Odd Aksel Bergstad4, Martin A. Collins5, Jan Erik Dyb6, Camila Henriques1, Emma G. Jones7 and Nicola King1 1University of Aberdeen, Oceanlab, Newburgh, Aberdeen AB41 6AA, UK 2Leibniz-Institut fu¨r Meereswissenschaften, IfM-GEOMAR, Du¨sternbrooker Weg 20, 24105 Kiel, Germany 3Marine Biology Research Division, Scripps Institution of Oceanography, UCSD 9500 Gilman Drive, La Jolla, CA 92093-0202, USA 4Institute of Marine Research, Flødevigen Marine Research Station, 4817 His, Norway 5British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK 6Møre Research, Section of Fisheries, PO Box 5075, 6021 Aalesund, Norway 7FRS Marine Laboratory, 375 Victoria Road, Aberdeen AB11 9DB, UK The oceanic abyss (depths greater than 3000 m), one of the largest environments on the planet, is characterized by absence of solar light, high pressures and remoteness from surface food supply necessitating special molecular, physiological, behavioural and ecological adaptations of organisms that live there. Sampling by trawl, baited hooks and cameras we show that the Chondrichthyes (sharks, rays and chimaeras) are absent from, or very rare in this region. Analysis of a global data set shows a trend of rapid disappearance of chondrichthyan species with depth when compared with bony fishes. Sharks, apparently well adapted to life at high pressures are conspicuous on slopes down to 2000 m including scavenging at food falls such as dead whales.
    [Show full text]
  • Biomechanics of Locomotion in Sharks, Rays, and Chimaeras
    5 Biomechanics of Locomotion in Sharks, Rays, and Chimaeras Anabela M.R. Maia, Cheryl A.D. Wilga, and George V. Lauder CONTENTS 5.1 Introduction 125 5.1.1 Approaches to Studying Locomotion in Chondrichthyans 125 5.1.2 Diversity of Locomotory Modes in Chondrichthyans 127 5.1.3 Body Form and Fin Shapes 127 5.2 Locomotion in Sharks 128 5.2.1 Function of the Body during Steady Locomotion and Vertical Maneuvering 128 5.2.2 Function of the Caudal Fin during Steady Locomotion and Vertical Maneuvering 130 5.2.3 Function of the Pectoral Fins during Locomotion 134 5.2.3.1 Anatomy of the Pectoral Fins 134 5.2.3.2 Role of the Pectoral Fins during Steady Swimming 136 5.2.3.3 Role of the Pectoral Fins during Vertical Maneuvering 138 5.2.3.4 Function of the Pectoral Fins during Benthic Station-Holding 139 5.2.3.5 Motor Activity in the Pectoral Fins 139 5.2.4 Routine Maneuvers and Escape Responses 140 5.2.5 Synthesis 141 5.3 Locomotion in Skates and Rays 142 5.4 Locomotion in Holocephalans 145 5.5 Material Properties of Chondrichthyan Locomotor Structures 146 5.6 Future Directions 147 Acknowledgments 148 References 148 5.1.1 Approaches to Studying 5.1 Introduction Locomotion in Chondrichthyans The body form of sharks is notable for the distinctive Historically, many attempts have been made to under- heterocercal tail with external morphological asymme- stand the function of the median and paired fins in try present in most taxa and the ventrolateral winglike sharks and rays, and these studies have included work pectoral fins extending laterally from the body (Figure with models (Affleck.
    [Show full text]
  • Postrelease Survival, Vertical and Horizontal Movements, and Thermal Habitats of Five Species of Pelagic Sharks in the Central
    341 Abstract—From 2001 to 2006, 71 Postrelease survival, vertical and horizontal pop-up satellite archival tags (PSATs) were deployed on five species of movements, and thermal habitats of five species pelagic shark (blue shark [Prionace glauca]; shortfin mako [Isurus oxy- of pelagic sharks in the central Pacific Ocean rinchus]; silky shark [Carcharhinus falciformis]; oceanic whitetip shark Michael K. Musyl (contact author)1 [C. longimanus]; and bigeye thresher 2 [Alopias superciliosus]) in the central Richard W. Brill Pacific Ocean to determine species- Daniel S. Curran3 specific movement patterns and sur- 4 vival rates after release from longline Nuno M. Fragoso fishing gear. Only a single postrelease Lianne M. McNaughton1 mortality could be unequivocally doc- Anders Nielsen5 umented: a male blue shark which 3* succumbed seven days after release. Bert S. Kikkawa Meta-analysis of published reports Christopher D. Moyes6 and the current study (n=78 reporting Email address for contact author: [email protected] PSATs) indicated that the summary effect of postrelease mortality for blue * Deceased 3 Pacific Islands Fisheries Science Center sharks was 15% (95% CI, 8.5–25.1%) NOAA Fisheries 1 University of Hawaii and suggested that catch-and-release 2570 Dole Street Joint Institute for Marine and Atmospheric in longline fisheries can be a viable Honolulu, Hawaii 96822 Research (JIMAR) management tool to protect paren- Kewalo Research Facility/NOAA 4 Large Pelagics Research Center tal biomass in shark populations. 1125B Ala Moana Boulevard
    [Show full text]
  • Great White Shark Carcharodon Carcharias
    Great White Shark Carcharodon carcharias Great White Sharks (Great Whites) are large predators at the top of the marine food chain. They are in the same class as all sharks and rays (Chondrichthyes) – this group is different from other fish as their skeleton is made from cartilage instead of bone. They have an average length of four to five metres, but can grow up to seven metres. Using their powerful tails to propel them, these sharks can move Bioregion resources through the water at up to 24 km per hour. Their mouths are lined with up to 300 serrated triangular teeth arranged in several rows. Diet Great Whites are able to use electroreception (the ability to detect weak electrical currents) to find and attack prey without seeing it. This can be useful in murky water or when their prey is hidden under sediment. This gives them the ability to navigate by sensing the Earth’s magnetic field. They have a strong sense of smell which is also useful in detecting prey. Contrary to some people’s beliefs, they often only attack humans to ‘sample bite’ and do not usually choose to eat human flesh, preferring marine mammals such as seals and sea lions. They are also known to feed on dolphins, octopus, squid, other sharks, rays and lobster, fish, crabs and seabirds. Breeding Great Whites have a low reproduction rate that makes it difficult for species numbers to recover. Males mature at eight to ten years and females mature at 12-18 years. Females give birth to two to ten pups once every two to three years.
    [Show full text]
  • Zob Paleozojskega Morskega Psa Rodu Glikmanius (Chondrichthyes, Ctenacanthidae) Iz Karavank (Slovenija)
    GEOLOGIJA 58/1, 57-62, Ljubljana 2015 doi:10.5474/geologija.2015.004 Zob paleozojskega morskega psa rodu Glikmanius (Chondrichthyes, Ctenacanthidae) iz Karavank (Slovenija) Upper Paleozoic shark tooth of genus Glikmanius (Chondrichthyes, Ctenacanthidae) from Karavanke Mts. (NW Slovenia) Matija KRIŽNAR Prirodoslovni muzej Slovenije, Pre{ernova 20, SI–1001 Ljubljana; mkriznar�pms-lj.si Prejeto / Received 16. 3. 2015; Sprejeto / Accepted 10. 4. 2015 Klju~ne besede: paleozojski morski pes, Glikmanius, spodnji perm, Karavanke, Slovenija Key words: Paleozoic shark, cladodont shark, Glikmanius, Lower Permian, Karavanke Mts., Slovenia Izvle~ek Zgornjepaleozojske (karbonske in permske) plasti v Karavankah so znane po pestri favni nevreten~arjev in posameznih najdbah karbonskih rastlin. Zelo redki so ostanki vreten~arjev. Nova in presenetljiva je najdba ve~jega zoba ktenakantidnega morskega psa vrste Glikmanius cf. occidentalis (Leidy) iz spodnjepermskih plasti med Dovjim in Plav{kim Rovtom, severno od Hru{ice. Gre za prvo najdbo te vrste v južni Evropi. Abstract Upper Paleozoic beds of Karavanke Mountains are rich in invertebrate and plant fossils, while the remains of vertebrates are extremely rare. A new cladodont shark tooth was found in Lower Permian beds near Hru{ica, at the locality named Na Visokih. We have identified the tooth as belonging to speciesGlikmanius cf. occidentalis (Leidy). This is the first find of this species in the southern Europe. Uvod (Ramovš, 1978). V zgornjekarbonskih plasteh so na{li predvsem trilobite (HAHN et al., 1977) Na ozemlju med Jesenicami in Dovjim poznamo in razli~ne ramenonožce (Ramovš, 1969; NOVAK vrsto zanimivih najdi{~ fosilov, ki stratigrafsko & SKABERNE, 2009). Spodnjepermske plasti ustrezajo zgornjemu karbonu (Auerni{ka in vsebujejo poleg bogate favne ramenonožcev Schulterkofelska formacija) in spodnjemu permu (SCHELLWIEN, 1900) in trilobitov (HAHN et al., 1990) Sl.
    [Show full text]