BASKING SHARK Class
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Luís M.D. Barcelos1, 2*, José M.N. Azevedo1, 3, Jürgen Pollerspöck4, and João P
ACTA ICHTHYOLOGICA ET PISCATORIA (2018) 48 (2): 189–194 DOI: 10.3750/AIEP/02436 REVIEW OF THE RECORDS OF THE SMALLTOOTH SAND TIGER SHARK, ODONTASPIS FEROX (ELASMOBRANCHII: LAMNIFORMES: ODONTASPIDIDAE), IN THE AZORES Luís M.D. Barcelos1, 2*, José M.N. Azevedo1, 3, Jürgen Pollerspöck4, and João P. Barreiros1, 2 1Centre for Ecology, Evolution, and Environmental Changes, Azorean Biodiversity Group, Angra do Heroísmo, Portugal 2Faculty of Agricultural and Environmental Sciences, University of the Azores, Angra do Heroísmo, Portugal 3Faculty of Sciences and Technology, University of the Azores, Ponta Delgada, Portugal 4Bavarian State Collection of Zoology, Munich, Germany Barcelos L.M.D., Azevedo J.M.N., Pollerspöck J., Barreiros J.P. 2018. Review of the records of the smalltooth sand tiger shark, Odontaspis ferox (Elasmobranchii: Lamniformes: Odontaspididae), in the Azores. Acta Ichthyol. Piscat. 48 (2): 189–194. Abstract. In recent years Azorean fishermen reported the presence of the smalltooth sand tiger shark,Odontaspis ferox (Risso, 1810), a very rare demersal shark species, associated with insular shelves and slopes, with occasional incursions into shallow waters and of poorly known biology and ecology. There are fourteen new records of this species, between 1996 and 2014, captured by spearfishing, harpoons, hand lines, or entangled in fishing gear in the Azores. These records were analysed and complemented with fishermen interviews, providing new locations and new biological data for this species. Also, specimens photographs were studied and post-mortem analysis were carefully carried out in one individual. This species is rare and captured only as bycatch in shallow waters. More detailed information on this species is critically needed in order to assess its conservation status and implement management guidelines. -
Can Threshold Foraging Responses of Basking Sharks Be Used to Estimate Their Metabolic Rate?
MARINE ECOLOGY PROGRESS SERIES Vol. 200: 289-296,2000 Published July 14 Mar Ecol Prog Ser ~ NOTE Can threshold foraging responses of basking sharks be used to estimate their metabolic rate? David W. Sims* Department of Zoology, University of Aberdeen. Tillydrone Avenue. Aberdeen AB24 2TZ. United Kingdom ABSTRACT: Empirical and theoretical determinations of There are 3 species of filter-feeding shark, the whale minimum threshold prey densities for filter-feeding basking shark ~hi~~~d~~typus of warm-temperate and tropical sharks Cetorhinus maximus were used to test the idea that threshold foraging behaviour could provide a means for esti- seas worldwide, the basking shark Cetorhinus max- mating oxygen consumption (a proxy for metabolic rate). The im~~that inhabits warm-temperate to boreal waters threshold feeding levelrepres&nts the prey density at which circumglobally, and the megamouth shark Mega- there will be no net energy gain (energy intake equals expen- chasms pelagjos occurs in the Pacific and At- diture). Basking sharks were observed to cease feeding at lantic, primarily in deep water (Compagno 1984, Yano their theoretical threshold; thus, the assumption underpin- ning the concept presented here was that over the narrow et They are the largest marine verte- range of zooplankton prey densities that induce 'switching' brates attaining body lengths of up to 14, 10 and 6 m re- between feeding and non-feeding in basking sharks, the spectively. Comparatively little is known about the bi- energetic value of the minimum threshold prey density is ology of planktivorous sharks despite the fact that they equivalent to the shark's instantaneous level of energy expen- diture. -
An Introduction to the Classification of Elasmobranchs
An introduction to the classification of elasmobranchs 17 Rekha J. Nair and P.U Zacharia Central Marine Fisheries Research Institute, Kochi-682 018 Introduction eyed, stomachless, deep-sea creatures that possess an upper jaw which is fused to its cranium (unlike in sharks). The term Elasmobranchs or chondrichthyans refers to the The great majority of the commercially important species of group of marine organisms with a skeleton made of cartilage. chondrichthyans are elasmobranchs. The latter are named They include sharks, skates, rays and chimaeras. These for their plated gills which communicate to the exterior by organisms are characterised by and differ from their sister 5–7 openings. In total, there are about 869+ extant species group of bony fishes in the characteristics like cartilaginous of elasmobranchs, with about 400+ of those being sharks skeleton, absence of swim bladders and presence of five and the rest skates and rays. Taxonomy is also perhaps to seven pairs of naked gill slits that are not covered by an infamously known for its constant, yet essential, revisions operculum. The chondrichthyans which are placed in Class of the relationships and identity of different organisms. Elasmobranchii are grouped into two main subdivisions Classification of elasmobranchs certainly does not evade this Holocephalii (Chimaeras or ratfishes and elephant fishes) process, and species are sometimes lumped in with other with three families and approximately 37 species inhabiting species, or renamed, or assigned to different families and deep cool waters; and the Elasmobranchii, which is a large, other taxonomic groupings. It is certain, however, that such diverse group (sharks, skates and rays) with representatives revisions will clarify our view of the taxonomy and phylogeny in all types of environments, from fresh waters to the bottom (evolutionary relationships) of elasmobranchs, leading to a of marine trenches and from polar regions to warm tropical better understanding of how these creatures evolved. -
Electrosensory Pore Distribution and Feeding in the Basking Shark Cetorhinus Maximus (Lamniformes: Cetorhinidae)
Vol. 12: 33–36, 2011 AQUATIC BIOLOGY Published online March 3 doi: 10.3354/ab00328 Aquat Biol NOTE Electrosensory pore distribution and feeding in the basking shark Cetorhinus maximus (Lamniformes: Cetorhinidae) Ryan M. Kempster*, Shaun P. Collin The UWA Oceans Institute and the School of Animal Biology, The University of Western Australia, 35 Stirling Highway, Crawley, Western Australia 6009, Australia ABSTRACT: The basking shark Cetorhinus maximus is the second largest fish in the world, attaining lengths of up to 10 m. Very little is known of its sensory biology, particularly in relation to its feeding behaviour. We describe the abundance and distribution of ampullary pores over the head and pro- pose that both the spacing and orientation of electrosensory pores enables C. maximus to use passive electroreception to track the diel vertical migrations of zooplankton that enable the shark to meet the energetic costs of ram filter feeding. KEY WORDS: Ampullae of Lorenzini · Electroreception · Filter feeding · Basking shark Resale or republication not permitted without written consent of the publisher INTRODUCTION shark Rhincodon typus and the megamouth shark Megachasma pelagios, which can attain lengths of up Electroreception is an ancient sensory modality that to 14 and 6 m, respectively (Compagno 1984). These 3 has evolved independently across the animal kingdom filter-feeding sharks are among the largest living in multiple groups (Scheich et al. 1986, Collin & White- marine vertebrates (Compagno 1984) and yet they are head 2004). Repeated independent evolution of elec- all able to meet their energetic costs through the con- troreception emphasises the importance of this sense sumption of tiny zooplankton. -
A Rhinopristiform Sawfish (Genus Pristis) from the Middle Eocene (Lutetian) of Southern Peru and Its Regional Implications
Carnets Geol. 20 (5) E-ISSN 1634-0744 DOI 10.4267/2042/70759 A rhinopristiform sawfish (genus Pristis) from the middle Eocene (Lutetian) of southern Peru and its regional implications Alberto COLLARETA 1, 2 Luz TEJADA-MEDINA 3, 4 César CHACALTANA-BUDIEL 3, 5 Walter LANDINI 1, 6 Alí ALTAMIRANO-SIERRA 7, 8 Mario URBINA-SCHMITT 7, 9 Giovanni BIANUCCI 1, 10 Abstract: Modern sawfishes (Rhinopristiformes: Pristidae) are circumglobally distributed in warm wa- ters and are common in proximal marine and even freshwater habitats. The fossil record of modern pristid genera (i.e., Pristis and Anoxypristis) dates back to the early Eocene and is mostly represented by isolated rostral spines and oral teeth, with phosphatised rostra representing exceptional occurren- ces. Here, we report on a partial pristid rostrum, exhibiting several articulated rostral spines, from middle Eocene strata of the Paracas Formation (Yumaque Member) exposed in the southern Peruvian East Pisco Basin. This finely preserved specimen shows anatomical structures that are unlikely to leave a fossil record, e.g., the paracentral grooves that extend along the ventral surface of the rostrum. Ba- sed on the morphology of the rostral spines, this fossil sawfish is here identified as belonging to Pristis. To our knowledge, this discovery represents the geologically oldest known occurrence of Pristidae from the Pacific Coast of South America. Although the fossil record of pristids from the East Pisco Basin spans from the middle Eocene to the late Miocene, sawfishes are no longer present in the modern cool, upwelling-influenced coastal waters of southern Peru. Given the ecological preferences of the extant members of Pristis, the occurrence of this genus in the Paracas deposits suggests that middle Eocene nearshore waters in southern Peru were warmer than today. -
On Giant Filter Feeders 170 Million Years
PERSPECTIVES PALEONTOLOGY Massive fi lter-feeding vertebrates have roamed the world’s oceans for the past On Giant Filter Feeders 170 million years. Lionel Cavin he largest living marine verte- years ago), the diversity of mysticete whales these fi shes engulfed water by swimming brates—baleen whales and several was linked to the diversity of diatoms and to with an open mouth and sieved food while T lineages of sharks and rays—feed climatic variations (4 ). water escaped through the gill arches. directly on very small organisms (such as In the Jurassic (200 to 145 million years Giant reptiles roamed the Jurassic and plankton and small fi shes). Planktivorous ago) and the Cretaceous (145 to 65 million Cretaceous oceans, and some huge ray- sharks and rays collect food by fi ltering sea- years ago), ray-fi nned fi shes called pachy- fi nned fi shes—the ichthyodectiforms (bull- water through gill rakers (fi ngerlike pro- cormiforms lived in the oceans. These extinct dog fi sh and relatives)—emerged at the end jections on gill arches), whereas mysticete fishes are regarded as primitive teleosts, of the Cretaceous. But all these beasts were whales sieve small animals from seawater the group to which most living bony fi shes apex predators that fed on large preys, and through whalebone or baleen (comblike belong (5 ). A giant representative from the none had a fi lter-feeding diet. The newly keratin structures in their upper jaws) (1 , Middle Jurassic, Leedsichthys, was up to 9 discovered clade of massive fi lter-feeding 2). On page 990 of this issue, Friedman et m long and has been interpreted as a fi lter fi shes thus fi lls a large ecological niche. -
Order LAMNIFORMES ODONTASPIDIDAE Sand Tiger Sharks Iagnostic Characters: Large Sharks
click for previous page Lamniformes: Odontaspididae 419 Order LAMNIFORMES ODONTASPIDIDAE Sand tiger sharks iagnostic characters: Large sharks. Head with 5 medium-sized gill slits, all in front of pectoral-fin bases, Dtheir upper ends not extending onto dorsal surface of head; eyes small or moderately large, with- out nictitating eyelids; no nasal barbels or nasoral grooves; snout conical or moderately depressed, not blade-like;mouth very long and angular, extending well behind eyes when jaws are not protruded;lower labial furrows present at mouth corners; anterior teeth enlarged, with long, narrow, sharp-edged but unserrated cusps and small basal cusplets (absent in young of at least 1 species), the upper anteriors separated from the laterals by a gap and tiny intermediate teeth; gill arches without rakers; spiracles present but very small. Two moderately large high dorsal fins, the first dorsal fin originating well in advance of the pelvic fins, the second dorsal fin as large as or somewhat smaller than the first dorsal fin;anal fin as large as second dorsal fin or slightly smaller; caudal fin short, asymmetrical, with a strong subterminal notch and a short but well marked ventral lobe. Caudal peduncle not depressed, without keels; a deep upper precaudal pit present but no lower pit. Intestinal valve of ring type, with turns closely packed like a stack of washers. Colour: grey or grey-brown to blackish above, blackish to light grey or white, with round or oval dark spots and blotches vari- ably present on 2 species. high dorsal fins upper precaudal eyes without pit present nictitating eyelids intestinal valve of ring type Habitat, biology, and fisheries: Wide-ranging, tropical to cool-temperate sharks, found inshore and down to moderate depths on the edge of the continental shelves and around some oceanic islands, and in the open ocean. -
A Review of Planktivorous Fishes: Their Evolution, Feeding Behaviours, Selectivities, and Impacts
Hydrobiologia 146: 97-167 (1987) 97 0 Dr W. Junk Publishers, Dordrecht - Printed in the Netherlands A review of planktivorous fishes: Their evolution, feeding behaviours, selectivities, and impacts I Xavier Lazzaro ORSTOM (Institut Français de Recherche Scientifique pour le Développement eri Coopération), 213, rue Lu Fayette, 75480 Paris Cedex IO, France Present address: Laboratorio de Limrzologia, Centro de Recursos Hidricob e Ecologia Aplicada, Departamento de Hidraulica e Sarzeamento, Universidade de São Paulo, AV,DI: Carlos Botelho, 1465, São Carlos, Sï? 13560, Brazil t’ Mail address: CI? 337, São Carlos, SI? 13560, Brazil Keywords: planktivorous fish, feeding behaviours, feeding selectivities, electivity indices, fish-plankton interactions, predator-prey models Mots clés: poissons planctophages, comportements alimentaires, sélectivités alimentaires, indices d’électivité, interactions poissons-pltpcton, modèles prédateurs-proies I Résumé La vision classique des limnologistes fut de considérer les interactions cntre les composants des écosystè- mes lacustres comme un flux d’influence unidirectionnel des sels nutritifs vers le phytoplancton, le zoo- plancton, et finalement les poissons, par l’intermédiaire de processus de contrôle successivement physiqucs, chimiques, puis biologiques (StraSkraba, 1967). L‘effet exercé par les poissons plaiictophages sur les commu- nautés zoo- et phytoplanctoniques ne fut reconnu qu’à partir des travaux de HrbáEek et al. (1961), HrbAEek (1962), Brooks & Dodson (1965), et StraSkraba (1965). Ces auteurs montrèrent (1) que dans les étangs et lacs en présence de poissons planctophages prédateurs visuels. les conimuiiautés‘zooplanctoniques étaient com- posées d’espèces de plus petites tailles que celles présentes dans les milieux dépourvus de planctophages et, (2) que les communautés zooplanctoniques résultantes, composées d’espèces de petites tailles, influençaient les communautés phytoplanctoniques. -
Can Sharks Be Saved? a Global Plan of Action for Shark Conservation in the Regime of the Convention on Migratory Species
Seattle Journal of Environmental Law Volume 5 Issue 1 Article 15 5-31-2015 Can Sharks be Saved? A Global Plan of Action for Shark Conservation in the Regime of the Convention on Migratory Species James Kraska Leo Chan Gaskins Follow this and additional works at: https://digitalcommons.law.seattleu.edu/sjel Part of the Education Commons, Environmental Law Commons, Intellectual Property Law Commons, Internet Law Commons, Land Use Law Commons, Natural Resources Law Commons, Science and Technology Law Commons, and the Water Law Commons Recommended Citation Kraska, James and Gaskins, Leo Chan (2015) "Can Sharks be Saved? A Global Plan of Action for Shark Conservation in the Regime of the Convention on Migratory Species," Seattle Journal of Environmental Law: Vol. 5 : Iss. 1 , Article 15. Available at: https://digitalcommons.law.seattleu.edu/sjel/vol5/iss1/15 This Article is brought to you for free and open access by the Student Publications and Programs at Seattle University School of Law Digital Commons. It has been accepted for inclusion in Seattle Journal of Environmental Law by an authorized editor of Seattle University School of Law Digital Commons. Can Sharks be Saved? A Global Plan of Action for Shark Conservation in the Regime of the Convention on Migratory Species James Kraska† and Leo Chan Gaskins‡ Shark populations throughout the world are at grave risk; some spe- cies have declined by 95 percent. The most recent IUCN (Interna- tional Union for the Conservation of Nature) assessment by the Shark Specialist Group (SSG) found that one-fourth of shark and ray spe- cies face the prospect of extinction. -
Filter-Feeding Ecology of Aquatic Insects
Annual Reviews www.annualreviews.org/aronline AnmRev. F.ntomol. 1980. 25:103-32 Copyright© 1980 by AnnualReviews Inc. All rights reserved FILTER-FEEDING ECOLOGY ~6185 OF AQUATIC INSECTS J. BruceWallace Departmentof Entomology,University of Georgia, Athens, Georgia 30602 Richard W. Merritt Departmentof Entomology,Michigan State University, East Lansing, Michigan48824 INTRODUCTION Filter feeders are organisms that have evolved various sieving mechanisms for removing particulate matter from suspension (100). Several groups aquatic insects, with habitats ranging from high elevation streams to saltwa- ter estuaries, use this feeding methodand consumesignificant quantities of suspended material (seston), including living organisms and both organic and inorganic detritus. Filter-feeding insects constitute important pathways for energy flow and are very important in the productivity of aquatic environments. Yet, someof these animals epitomize the complexrelation- ship between manand insects since biting adults of certain groups are amongman’s oldest adversaries. The major objectives of this article are to review the meansby which filter-feeding insects obtain their food and to assess the role of these animals in aquatic ecosystems.Filter-feeding strate- gies by other invertebrates in both marine and freshwater habitats have been partially reviewed elsewhere (82, 100, 101). SOURCES OF FOOD Lotic ecosystems in forested regions receive large inputs of allochthonous organic matter (4, 36-38, 98, 137). Anderson& Sedell (4) recently reviewed the role of macroinvertebrates in detritus processing. There is ample evi- dence from lotic studies that the concentration of particulate organic seston 103 0066-4170/80/0101-0103501.00 Annual Reviews www.annualreviews.org/aronline 104 WALLACE& MERRITT is skewed toward the smallest size fractions (<50 /zm) (119, 148, 191). -
Biodiversity Series Background Document for Basking Shark
Background Document for Basking shark Cetorhinus maximus Biodiversity Series 2009 OSPAR Convention Convention OSPAR The Convention for the Protection of the La Convention pour la protection du milieu Marine Environment of the North-East Atlantic marin de l'Atlantique du Nord-Est, dite (the “OSPAR Convention”) was opened for Convention OSPAR, a été ouverte à la signature at the Ministerial Meeting of the signature à la réunion ministérielle des former Oslo and Paris Commissions in Paris anciennes Commissions d'Oslo et de Paris, on 22 September 1992. The Convention à Paris le 22 septembre 1992. La Convention entered into force on 25 March 1998. It has est entrée en vigueur le 25 mars 1998. been ratified by Belgium, Denmark, Finland, La Convention a été ratifiée par l'Allemagne, France, Germany, Iceland, Ireland, la Belgique, le Danemark, la Finlande, Luxembourg, Netherlands, Norway, Portugal, la France, l’Irlande, l’Islande, le Luxembourg, Sweden, Switzerland and the United Kingdom la Norvège, les Pays-Bas, le Portugal, and approved by the European Community le Royaume-Uni de Grande Bretagne and Spain. et d’Irlande du Nord, la Suède et la Suisse et approuvée par la Communauté européenne et l’Espagne. Acknowledgement This report has been prepared by the Association pour l'Etude et la Conservation des Sélaciens (APECS) and Ms Amelia Curd (France). Thanks are also due for contributions provided by Colin Speedie, Sarah Fowler, David Sims, Jean-Luc Solandt Photo acknowledgement: Cover page: Basking shark, wikipedia Contents Background Document -
Lamniformes, Odontaspididae) from the Eocene of Antarctica Provides New Information About the Paleobiogeography and Paleobiology of Paleogene Sand Tiger Sharks
Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 124(2): 283-298. July 2018 THE SOUTHERNMOST OCCURRENCE OF BRACHYCARCHARIAS (LAMNIFORMES, ODONTASPIDIDAE) FROM THE EOCENE OF ANTARCTICA PROVIDES NEW INFORMATION ABOUT THE PALEOBIOGEOGRAPHY AND PALEOBIOLOGY OF PALEOGENE SAND TIGER SHARKS GIUSEPPE MARRAMÀ1*, ANDREA ENGELBRECHT1, THOMAS MÖRS2, MARCELO A. REGUERO3 & JÜRGEN KRIWET1 1*Corresponding author. Department of Paleontology, University of Vienna, Althanstrasse 14, 1090 Vienna, Austria. E-mail: [email protected], [email protected], [email protected] 2 Department of Paleozoology, Swedish Museum of Natural History, P.O, Box 50007, SE-104 05 Stockholm, Sweden. E-mail: [email protected] 3 Division Paleontologia de Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 81900 FWA La Plata, Argentina, CONICET. E-mail: [email protected] ARKU To cite this article: Marramà G., Engelbrecht A., Mörs T., Reguero M.A. & Kriwet J. (2018) - The southernmost occurrence of Brachycarcharias (Lamniformes, Odontaspididae) from the Eocene of Antarctica provides new information about the paleobiogeography and paleobiology of Paleogene sand tiger sharks. Riv. It. Paleontol. Strat., 124(2): 283-298. Keywords: Chondrichthyes; Elasmobranchii; Ypresian; La Meseta Formation; biotic turnovers. Abstract. The first record of one of the most common and widespread Paleogene selachians, the sand tiger shark Brachycarcharias, in the Ypresian strata of the La Meseta Formation, Seymour Island, Antarctica, is pro- vided herein. Selachians from the early Eocene horizons of this deposit represent the southernmost Paleogene occurrences in the fossil record, and are represented by isolated teeth belonging to orectolobiforms, lamniforms, carcharhiniforms, squatiniforms and pristiophoriforms.