5. the Pesciara-Monte Postale Fossil-Lagerstätte: 2. Fishes and Other Vertebrates
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Zoology Marine Ornamental Fish Biodiversity of West Bengal ABSTRACT
Research Paper Volume : 4 | Issue : 8 | Aug 2015 • ISSN No 2277 - 8179 Zoology Marine Ornamental Fish Biodiversity of KEYWORDS : Marine fish, ornamental, West Bengal diversity, West Bengal. Principal Scientist and Scientist-in-Charge, ICAR-Central Institute of Fisheries Education, Dr. B. K. Mahapatra Salt Lake City, Kolkata-700091, India Director and Vice-Chancellor, ICAR-Central Institute of Fisheries Education, Versova, Dr. W. S. Lakra Mumbai- 400 061, India ABSTRACT The State of West Bengal, India endowed with 158 km coast line for marine water resources with inshore, up-shore areas and continental shelf of Bay of Bengal form an important fishery resource and also possesses a rich wealth of indigenous marine ornamental fishes.The present study recorded a total of 113 marine ornamental fish species, belonging to 75 genera under 45 families and 10 orders.Order Perciformes is represented by a maximum of 26 families having 79 species under 49 genera followed by Tetraodontiformes (5 family; 9 genus and 10 species), Scorpaeniformes (2 family; 3 genus and 6 species), Anguilliformes (2 family; 3 genus and 4 species), Syngnathiformes (2 family; 3 genus and 3 species), Pleuronectiformes (2 family; 2 genus and 4 species), Siluriformes (2 family; 2 genus and 3 species), Beloniformes (2 family; 2 genus and 2 species), Lophiformes (1 family; 1 genus and 1 species), Beryciformes(1 family; 1 genus and 1 species). Introduction Table 1: List of Marine ornamental fishes of West Bengal Ornamental fishery, which started centuries back as a hobby, ORDER 1: PERCIFORMES has now started taking the shape of a multi-billion dollar in- dustry. -
Order BERYCIFORMES ANOPLOGASTRIDAE Fangtooths (Ogrefish) by J.A
click for previous page 1178 Bony Fishes Order BERYCIFORMES ANOPLOGASTRIDAE Fangtooths (ogrefish) by J.A. Moore, Florida Atlantic University, USA iagnostic characters: Small (to about 160 mm standard length) beryciform fishes.Body short, deep, and Dcompressed, tapering to narrow peduncle. Head large (1/3 standard length). Eye smaller than snout length in adults, but larger than snout length in juveniles. Mouth very large and oblique, jaws extend be- hind eye in adults; 1 supramaxilla. Bands of villiform teeth in juveniles are replaced with large fangs on dentary and premaxilla in adults; vomer and palatines toothless. Deep sensory canals separated by ser- rated ridges; very large parietal and preopercular spines in juveniles of one species, all disappearing with age. Gill rakers as clusters of teeth on gill arch in adults (lath-like in juveniles). No true fin spines; single, long-based dorsal fin with 16 to 20 rays; anal fin very short-based with 7 to 9 soft rays; caudal fin emarginate; pectoral fins with 13 to 16 soft rays; pelvic fins with 7 soft rays. Scales small, non-overlapping, spinose, goblet-shaped in adults; lateral line an open groove partially bridged by scales; no enlarged ventral keel scutes. Colour: entirely dark brown or black in adults. Habitat, biology, and fisheries: Meso- to bathypelagic, at depths of 75 to 5 000 m. Carnivores, with juveniles feeding on mainly crustaceans and adults mainly on fishes. May sometimes swim in small groups. Uncommon deep-sea fishes of no commercial importance. Remarks: The family was revised recently by Kotlyar (1986) and contains 1 genus with 2 species throughout the tropical and temperate latitudes. -
§4-71-6.5 LIST of CONDITIONALLY APPROVED ANIMALS November
§4-71-6.5 LIST OF CONDITIONALLY APPROVED ANIMALS November 28, 2006 SCIENTIFIC NAME COMMON NAME INVERTEBRATES PHYLUM Annelida CLASS Oligochaeta ORDER Plesiopora FAMILY Tubificidae Tubifex (all species in genus) worm, tubifex PHYLUM Arthropoda CLASS Crustacea ORDER Anostraca FAMILY Artemiidae Artemia (all species in genus) shrimp, brine ORDER Cladocera FAMILY Daphnidae Daphnia (all species in genus) flea, water ORDER Decapoda FAMILY Atelecyclidae Erimacrus isenbeckii crab, horsehair FAMILY Cancridae Cancer antennarius crab, California rock Cancer anthonyi crab, yellowstone Cancer borealis crab, Jonah Cancer magister crab, dungeness Cancer productus crab, rock (red) FAMILY Geryonidae Geryon affinis crab, golden FAMILY Lithodidae Paralithodes camtschatica crab, Alaskan king FAMILY Majidae Chionocetes bairdi crab, snow Chionocetes opilio crab, snow 1 CONDITIONAL ANIMAL LIST §4-71-6.5 SCIENTIFIC NAME COMMON NAME Chionocetes tanneri crab, snow FAMILY Nephropidae Homarus (all species in genus) lobster, true FAMILY Palaemonidae Macrobrachium lar shrimp, freshwater Macrobrachium rosenbergi prawn, giant long-legged FAMILY Palinuridae Jasus (all species in genus) crayfish, saltwater; lobster Panulirus argus lobster, Atlantic spiny Panulirus longipes femoristriga crayfish, saltwater Panulirus pencillatus lobster, spiny FAMILY Portunidae Callinectes sapidus crab, blue Scylla serrata crab, Samoan; serrate, swimming FAMILY Raninidae Ranina ranina crab, spanner; red frog, Hawaiian CLASS Insecta ORDER Coleoptera FAMILY Tenebrionidae Tenebrio molitor mealworm, -
Annotated Checklist of Fossil Fishes from the Smoky Hill Chalk of the Niobrara Chalk (Upper Cretaceous) in Kansas
Lucas, S. G. and Sullivan, R.M., eds., 2006, Late Cretaceous vertebrates from the Western Interior. New Mexico Museum of Natural History and Science Bulletin 35. 193 ANNOTATED CHECKLIST OF FOSSIL FISHES FROM THE SMOKY HILL CHALK OF THE NIOBRARA CHALK (UPPER CRETACEOUS) IN KANSAS KENSHU SHIMADA1 AND CHRISTOPHER FIELITZ2 1Environmental Science Program and Department of Biological Sciences, DePaul University,2325 North Clifton Avenue, Chicago, Illinois 60614; and Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601;2Department of Biology, Emory & Henry College, P.O. Box 947, Emory, Virginia 24327 Abstract—The Smoky Hill Chalk Member of the Niobrara Chalk is an Upper Cretaceous marine deposit found in Kansas and adjacent states in North America. The rock, which was formed under the Western Interior Sea, has a long history of yielding spectacular fossil marine vertebrates, including fishes. Here, we present an annotated taxo- nomic list of fossil fishes (= non-tetrapod vertebrates) described from the Smoky Hill Chalk based on published records. Our study shows that there are a total of 643 referable paleoichthyological specimens from the Smoky Hill Chalk documented in literature of which 133 belong to chondrichthyans and 510 to osteichthyans. These 643 specimens support the occurrence of a minimum of 70 species, comprising at least 16 chondrichthyans and 54 osteichthyans. Of these 70 species, 44 are represented by type specimens from the Smoky Hill Chalk. However, it must be noted that the fossil record of Niobrara fishes shows evidence of preservation, collecting, and research biases, and that the paleofauna is a time-averaged assemblage over five million years of chalk deposition. -
The Adductor Pectoral Fin Muscle of Micropogonias Furnieri (Perciformes
ZOOLOGIA 33(6): e20160101 ISSN 1984-4689 (online) www.scielo.br/zool MORPHOLOGY AND PHYSIOLOGY The adductor pectoral fin muscle ofMicropogonias furnieri (Perciformes: Sciaenidae): a morphological and histochemical study María Sol Hernández1, María Victoria Longo1*, Clelia Viviana Devincenti1 & Alcira Ofelia Díaz1 1Instituto de Investigaciones Marinas y Costeras (IIMyC), Departamento de Biología, FCEyN, CONICET, Universidad Nacional de Mar del Plata. Funes 3250, 3° piso, (7600) Mar del Plata, Argentina. *Corresponding author. E-mail: [email protected] ABSTRACT. The adductor pectoral fin muscle in post-spawning females of the white croakerMicropogonias furnieri (Desmarest, 1823) is described from a morphological, histochemical and morphometric perspectives. A description of the morphological characteristics was conducted after dissections in different layers, down to the deep layer. Five muscles were found: superficial, medial, radial and deep adductors, and dorsal arrector. Their fibers were studied after applying histochemical techniques: succinic dehydrogenase (SDH) to reveal mitochondria, periodic acid-Schiff (PAS) for glycogen, Sudan black for lipids, myosin adenosinetriphosphatase (mATPase) to reveal the types of fibers, and modified mATPase to evidence the capillaries. Fiber diameters were measured and the number of capillaries was counted. Fiber subtypes named small, medium and large were found within red, pink and white fibers, the latter prevailing. Staining homogeneity was observed in white fibers after alkaline pre-incubations. The number of capillaries decreased from red to white fibers. Due to the prevalence of white fibers, the adductor muscle of the pectoral fins appears to be capable of rapid and discontinuous movements, which are important to body stabilization during subcarangiform swimming. The homogenous staining of white fibers observed in this research corresponds to the post-spawning gonad stage studied. -
Order BERYCIFORMES ANOPLOGASTRIDAE Anoplogaster
click for previous page 2210 Bony Fishes Order BERYCIFORMES ANOPLOGASTRIDAE Fangtooths by J.R. Paxton iagnostic characters: Small (to 16 cm) Dberyciform fishes, body short, deep, and compressed. Head large, steep; deep mu- cous cavities on top of head separated by serrated crests; very large temporal and pre- opercular spines and smaller orbital (frontal) spine in juveniles of one species, all disap- pearing with age. Eyes smaller than snout length in adults (but larger than snout length in juveniles). Mouth very large, jaws extending far behind eye in adults; one supramaxilla. Teeth as large fangs in pre- maxilla and dentary; vomer and palatine toothless. Gill rakers as gill teeth in adults (elongate, lath-like in juveniles). No fin spines; dorsal fin long based, roughly in middle of body, with 16 to 20 rays; anal fin short-based, far posterior, with 7 to 9 rays; pelvic fin abdominal in juveniles, becoming subthoracic with age, with 7 rays; pectoral fin with 13 to 16 rays. Scales small, non-overlap- ping, spinose, cup-shaped in adults; lateral line an open groove partly covered by scales. No light organs. Total vertebrae 25 to 28. Colour: brown-black in adults. Habitat, biology, and fisheries: Meso- and bathypelagic. Distinctive caulolepis juvenile stage, with greatly enlarged head spines in one species. Feeding mode as carnivores on crustaceans as juveniles and on fishes as adults. Rare deepsea fishes of no commercial importance. Remarks: One genus with 2 species throughout the world ocean in tropical and temperate latitudes. The family was revised by Kotlyar (1986). Similar families occurring in the area Diretmidae: No fangs, jaw teeth small, in bands; anal fin with 18 to 24 rays. -
Geo-Eco-Trop., 2020, 44, 1: 161-174 Osteology and Phylogenetic Relationships of Gregoriopycnodus Bassanii Gen. Nov., a Pycnodon
Geo-Eco-Trop., 2020, 44, 1: 161-174 Osteology and phylogenetic relationships of Gregoriopycnodus bassanii gen. nov., a pycnodont fish (Pycnodontidae) from the marine Albian (Lower Cretaceous) of Pietraroja (southern Italy) Ostéologie et relations phylogénétiques de Gregoriopycnodus bassanii gen. nov., un poisson pycnodonte (Pycnodontidae) de l’Albien marin (Crétacé inférieur) de Pietraroja (Italie du Sud) Louis TAVERNE 1, Luigi CAPASSO 2 & Maria DEL RE 3 Résumé: L’ostéologie et les relations phylogénétiques de Gregoriopycnodus bassanii gen. nov., un poisson pycnodonte de l’Albien marin (Crétacé inférieur) de l’Italie du Sud, sont étudiées en détails. Ce genre fossile appartient à la famille des Pycnodontidae, comme le montre la présence d’un peniculus branchu sur le pariétal. Gregoriopycnodus diffère des autres genres de la famille par son préfrontal court, en forme de plaque et qui est partiellement soudé au mésethmoïde. Au sein de la famille, la position systématique de Gregoriopycnodus est intermédiaire entre celle de Tepexichthys et Costapycnodus, d’une part, et celle de Proscinetes, d’autre part. Mots-clés: Pycnodontiformes, Pycnodontidae, Gregoriopycnodus bassanii gen. nov., ostéologie, phylogénie, Albien marin, Italie du Sud Abstract: The osteology and the phylogenetic relationships of Gregoriopycnodus bassanii gen. nov., a pycnodont fish from the marine Albian (Lower Cretaceous) of Pietraroja (southern Italy), are studied in details. This fossil genus belongs to the family Pycnodontidae, as shown by the presence of a branched peniculus on the parietal. Gregoriopycnodus differs from the other genera of the family by its short and plate-like prefrontral that is partly fused to the mesethmoid. Within the family, the systematic position of Gregoriopycnodus is intermediate between that of Tepexichthys and Costapycnodus, on the one hand, and that of Proscinetes, on the other hand. -
Fishes of Terengganu East Coast of Malay Peninsula, Malaysia Ii Iii
i Fishes of Terengganu East coast of Malay Peninsula, Malaysia ii iii Edited by Mizuki Matsunuma, Hiroyuki Motomura, Keiichi Matsuura, Noor Azhar M. Shazili and Mohd Azmi Ambak Photographed by Masatoshi Meguro and Mizuki Matsunuma iv Copy Right © 2011 by the National Museum of Nature and Science, Universiti Malaysia Terengganu and Kagoshima University Museum All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means without prior written permission from the publisher. Copyrights of the specimen photographs are held by the Kagoshima Uni- versity Museum. For bibliographic purposes this book should be cited as follows: Matsunuma, M., H. Motomura, K. Matsuura, N. A. M. Shazili and M. A. Ambak (eds.). 2011 (Nov.). Fishes of Terengganu – east coast of Malay Peninsula, Malaysia. National Museum of Nature and Science, Universiti Malaysia Terengganu and Kagoshima University Museum, ix + 251 pages. ISBN 978-4-87803-036-9 Corresponding editor: Hiroyuki Motomura (e-mail: [email protected]) v Preface Tropical seas in Southeast Asian countries are well known for their rich fish diversity found in various environments such as beautiful coral reefs, mud flats, sandy beaches, mangroves, and estuaries around river mouths. The South China Sea is a major water body containing a large and diverse fish fauna. However, many areas of the South China Sea, particularly in Malaysia and Vietnam, have been poorly studied in terms of fish taxonomy and diversity. Local fish scientists and students have frequently faced difficulty when try- ing to identify fishes in their home countries. During the International Training Program of the Japan Society for Promotion of Science (ITP of JSPS), two graduate students of Kagoshima University, Mr. -
Offshore Marine Actinopterygian Assemblages from the Maastrichtian–Paleogene of the Pindos Unit in Eurytania, Greece Thodoris Argyriou, Donald Davesne
Offshore marine actinopterygian assemblages from the Maastrichtian–Paleogene of the Pindos Unit in Eurytania, Greece Thodoris Argyriou, Donald Davesne To cite this version: Thodoris Argyriou, Donald Davesne. Offshore marine actinopterygian assemblages from the Maastrichtian–Paleogene of the Pindos Unit in Eurytania, Greece. PeerJ, PeerJ, 2021, 9, pp.e10676. 10.7717/peerj.10676. hal-03121049 HAL Id: hal-03121049 https://hal.sorbonne-universite.fr/hal-03121049 Submitted on 26 Jan 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Offshore marine actinopterygian assemblages from the Maastrichtian–Paleogene of the Pindos Unit in Eurytania, Greece Thodoris Argyriou1 and Donald Davesne2,3 1 UMR 7207 (MNHN—Sorbonne Université—CNRS) Centre de Recherche en Paléontologie, Museum National d’Histoire naturelle, Paris, France 2 Department of Earth Sciences, University of Oxford, Oxford, UK 3 UMR 7205 (MNHN—Sorbonne Université—CNRS—EPHE), Institut de Systématique, Évolution, Biodiversité, Museum National d’Histoire naturelle, Paris, France ABSTRACT The fossil record of marine ray-finned fishes (Actinopterygii) from the time interval surrounding the Cretaceous–Paleogene (K–Pg) extinction is scarce at a global scale, hampering our understanding of the impact, patterns and processes of extinction and recovery in the marine realm, and its role in the evolution of modern marine ichthyofaunas. -
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. -
Carboniferous Formations and Faunas of Central Montana
Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________ -
Downloaded for Five Nuclear Genes 243 (KIAA1239, MYH6, RIPK4, RAG1, SH3PX3), and Four Mitochondrial Genes (12S, 16S, 244 COX1 and CYTB)
bioRxiv preprint doi: https://doi.org/10.1101/247304; this version posted March 26, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 2 How the Central American Seaway and 3 an ancient northern passage affected 4 flatfish diversification 5 6 Lisa Byrne1, François Chapleau1, and Stéphane Aris-Brosou*,1,2 7 8 1Department of Biology, University of Ottawa, Ottawa, ON, CANADA 9 2Department of Mathematics & Statistics, University of Ottawa, Ottawa, ON, CANADA 10 11 *Corresponding author: E-mail: [email protected] 12 1 bioRxiv preprint doi: https://doi.org/10.1101/247304; this version posted March 26, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 13 Abstract 14 While the natural history of flatfish has been debated for decades, the mode of 15 diversification of this biologically and economically important group has never been 16 elucidated. To address this question, we assembled the largest molecular data set to date, 17 covering > 300 species (out of ca. 800 extant), from 13 of the 14 known families over 18 nine genes, and employed relaxed molecular clocks to uncover their patterns of 19 diversification. As the fossil record of flatfish is contentious, we used sister species 20 distributed on both sides of the American continent to calibrate clock models based on 21 the closure of the Central American Seaway (CAS), and on their current species range.