Nautilus: Biology, Systematics, and Paleobiology As Viewed from 2015
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CEPHALOPODS 688 Cephalopods
click for previous page CEPHALOPODS 688 Cephalopods Introduction and GeneralINTRODUCTION Remarks AND GENERAL REMARKS by M.C. Dunning, M.D. Norman, and A.L. Reid iving cephalopods include nautiluses, bobtail and bottle squids, pygmy cuttlefishes, cuttlefishes, Lsquids, and octopuses. While they may not be as diverse a group as other molluscs or as the bony fishes in terms of number of species (about 600 cephalopod species described worldwide), they are very abundant and some reach large sizes. Hence they are of considerable ecological and commercial fisheries importance globally and in the Western Central Pacific. Remarks on MajorREMARKS Groups of CommercialON MAJOR Importance GROUPS OF COMMERCIAL IMPORTANCE Nautiluses (Family Nautilidae) Nautiluses are the only living cephalopods with an external shell throughout their life cycle. This shell is divided into chambers by a large number of septae and provides buoyancy to the animal. The animal is housed in the newest chamber. A muscular hood on the dorsal side helps close the aperture when the animal is withdrawn into the shell. Nautiluses have primitive eyes filled with seawater and without lenses. They have arms that are whip-like tentacles arranged in a double crown surrounding the mouth. Although they have no suckers on these arms, mucus associated with them is adherent. Nautiluses are restricted to deeper continental shelf and slope waters of the Indo-West Pacific and are caught by artisanal fishers using baited traps set on the bottom. The flesh is used for food and the shell for the souvenir trade. Specimens are also caught for live export for use in home aquaria and for research purposes. -
Nautiloid Shell Morphology
MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOWER STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOIVER 1964 STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS EXOFFICIO THEHONORABLEJACKM.CAMPBELL ................................ Governor of New Mexico LEONARDDELAY() ................................................... Superintendent of Public Instruction APPOINTEDMEMBERS WILLIAM G. ABBOTT ................................ ................................ ............................... Hobbs EUGENE L. COULSON, M.D ................................................................. Socorro THOMASM.CRAMER ................................ ................................ ................... Carlsbad EVA M. LARRAZOLO (Mrs. Paul F.) ................................................. Albuquerque RICHARDM.ZIMMERLY ................................ ................................ ....... Socorro Published February 1 o, 1964 For Sale by the New Mexico Bureau of Mines & Mineral Resources Campus Station, Socorro, N. Mex.—Price $2.50 Contents Page ABSTRACT ....................................................................................................................................................... 1 INTRODUCTION -
Late Cretaceous Nautilid Beaks from Near-Shore/Shallow Water Deposits of the Bohemian Cretaceous Basin (Czech Republic)
Acta Geologica Polonica , Vol. 60 (2010), No. 3, pp. 417 –428 Late Cretaceous nautilid beaks from near-shore/shallow water deposits of the Bohemian Cretaceous Basin (Czech Republic) MaRtiN KošťáK 1, RadeK VodRážKa 1,2 , Jiří FRaNK 1, MaRtiN MazuCh 1 aNd JaRosLaV MaReK 1 1Institute of Geology and Palaeontology, Faculty of Science, Charles University in Prague, 128 43 Czech Republic. E-mail: [email protected] 2Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic aBstRaCt: Košťák, M., Vodrážka, R., Frank, J., Mazuch, M. and Marek, J. 2010. Late Cretaceous nautilid beaks from near- shore/shallow water deposits of the Bohemian Cretaceous Basin (Czech Republic). Acta Geologica Polonica , 60 (3), 417 –428 . Warszawa. More than 30 isolated nautilid jaws have been discovered in washed samples of late Cretaceous (turonian) near- shore/shallow water deposits located in the southern part of the Bohemian Cretaceous Basin (BCB). upper and lower jaws discovered in genetically-similar early turonian deposits are described in detail herein. the nautilid jaw appa - ratuses comprise rhyncholites (upper jaws) assigned to Nautilorhynchus simplex (Fritsch), and conchorhynchs (lower jaws) assigned to Conchorhynchus cretaceus Fritsch. some rhyncholites show signs of abrasion and corrosion, and may also form a substrate for sessile organisms. in one specimen, signs of acid digestion in the stomach of a preda - tor were recognized. N. simplex is synonymized with “ Rhyncholithus ” bohemicus (till), “ R.” curvatus ” (till), “ R”. rectus (till) and “ R” . curtus (till). the significant morphological variability observed in N. simplex is supported by biometric data. although the jaws were not found associated with body chambers, it is inferred from the extremely low nautilid biodiversity across the Cenomanian/turonian boundary interval in the BCB, and from the range and rel - ative abundance of the only early turonian nautilid taxon present, that the jaws are probably referable to the genus Eutrephoceras hyatt and specifically to the common and long-ranging species E. -
THE NAUTILUS [Vol
2 2 THE NAUTILUS [Vol. 69 (1) separated from each other by five centimeters. The snail was expanded with its head oriented away from the clam. When placed on the sand, the clam showed no activity during the next 30 minutes after which observations were discontinued. All but the lower (anterior) end of the body of the clam was covered by an envelope of slime secreted by the foot of the snail. It seems clear that P. duplicatus capturesEnsis directus by approaching it below the surface of the substratum and by ir ritating the lower portion so that it retreats upward. The snail then coats the razor clam with an envelope of slime which ap pears to have anesthetic properties. Successful capture proba bly depends on the ability of the snail to maintain contact with its prey until anesthesia takes place. ON THE OCCURRENCE OF THE NUDIBRANCH ALDERIA MODESTA (LOVÉN, 1844) ON THE CENTRAL CALIFORNIAN COAST By CADET HAND and JOAN STEINBERG Department of Zoology, University of California, Berkeley Alderia modesta (Loven, 1844) has long been known from the coasts of northern Europe. It has been recorded from as far north as the Trondheim Fjord in Norway (Norman, 1893), south to Skibbereen in Ireland (Allman, 1845) and on the French coast (Gollien, 1929). Therefore, it has been of con siderable interest to us to find well-established populations of an Alderia in two localities on the central Californian coast. Through the kindness of Monsieur G. Van Put of the Royal Institute of Natural Sciences of Belgium in Brussels and Dr. -
'Cenoceras Islands' in the Blue Lias Formation (Lower Jurassic)
FOSSIL IMPRINT • vol. 75 • 2019 • no. 1 • pp. 108–119 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) ‘CENOCERAS ISLANDS’ IN THE BLUE LIAS FORMATION (LOWER JURASSIC) OF WEST SOMERSET, UK: NAUTILID DOMINANCE AND INFLUENCE ON BENTHIC FAUNAS DAVID H. EVANS1, *, ANDY H. KING2 1 Stratigrapher, Natural England, Rivers House, East Quay, Bridgwater, Somerset, TA6 4YS UK; e-mail: [email protected]. 2 Director & Principal Geologist, Geckoella Ltd, Suite 323, 7 Bridge Street, Taunton, Somerset, TA1 1TG UK; e-mail: [email protected]. * corresponding author Evans, D. H., King, A. H. (2019): ‘Cenoceras islands’ in the Blue Lias Formation (Lower Jurassic) of West Somerset, UK: nautilid dominance and influence on benthic faunas. – Fossil Imprint, 75(1): 108–119, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on-line). Abstract: Substantial numbers of the nautilid Cenoceras occur in a stratigraphically limited horizon within the upper part of the Lower Jurassic (Sinemurian Stage) Blue Lias Formation at Watchet on the West Somerset Coast (United Kingdom). Individual nautilid conchs are associated with clusters of encrusting organisms (sclerobionts) forming ‘islands’ that may have been raised slightly above the surrounding substrate. Despite the relatively large numbers of nautilid conchs involved, detailed investigation of their preservation suggests that their accumulation reflects a reduction in sedimentation rates rather than an influx of empty conches or moribund animals. Throughout those horizons in which nautilids are present in relative abundance, the remains of ammonites are subordinate or rare. The reason for this unclear, and preferential dissolution of ammonite conchs during their burial does seem to provide a satisfactory solution to the problem. -
Giant Pacific Octopus (Enteroctopus Dofleini) Care Manual
Giant Pacific Octopus Insert Photo within this space (Enteroctopus dofleini) Care Manual CREATED BY AZA Aquatic Invertebrate Taxonomic Advisory Group IN ASSOCIATION WITH AZA Animal Welfare Committee Giant Pacific Octopus (Enteroctopus dofleini) Care Manual Giant Pacific Octopus (Enteroctopus dofleini) Care Manual Published by the Association of Zoos and Aquariums in association with the AZA Animal Welfare Committee Formal Citation: AZA Aquatic Invertebrate Taxon Advisory Group (AITAG) (2014). Giant Pacific Octopus (Enteroctopus dofleini) Care Manual. Association of Zoos and Aquariums, Silver Spring, MD. Original Completion Date: September 2014 Dedication: This work is dedicated to the memory of Roland C. Anderson, who passed away suddenly before its completion. No one person is more responsible for advancing and elevating the state of husbandry of this species, and we hope his lifelong body of work will inspire the next generation of aquarists towards the same ideals. Authors and Significant Contributors: Barrett L. Christie, The Dallas Zoo and Children’s Aquarium at Fair Park, AITAG Steering Committee Alan Peters, Smithsonian Institution, National Zoological Park, AITAG Steering Committee Gregory J. Barord, City University of New York, AITAG Advisor Mark J. Rehling, Cleveland Metroparks Zoo Roland C. Anderson, PhD Reviewers: Mike Brittsan, Columbus Zoo and Aquarium Paula Carlson, Dallas World Aquarium Marie Collins, Sea Life Aquarium Carlsbad David DeNardo, New York Aquarium Joshua Frey Sr., Downtown Aquarium Houston Jay Hemdal, Toledo -
Geology of the Shepton Mallet Area (Somerset)
Geology of the Shepton Mallet area (Somerset) Integrated Geological Surveys (South) Internal Report IR/03/94 BRITISH GEOLOGICAL SURVEY INTERNAL REPORT IR/03/00 Geology of the Shepton Mallet area (Somerset) C R Bristow and D T Donovan Contributor H C Ivimey-Cook (Jurassic biostratigraphy) The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Ordnance Survey licence number GD 272191/1999 Key words Somerset, Jurassic. Subject index Bibliographical reference BRISTOW, C R and DONOVAN, D T. 2003. Geology of the Shepton Mallet area (Somerset). British Geological Survey Internal Report, IR/03/00. 52pp. © NERC 2003 Keyworth, Nottingham British Geological Survey 2003 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation. Shop online at: www.thebgs.co.uk The Survey publishes an annual catalogue of its maps and other publications; this catalogue is available from any of the BGS Sales Murchison House, West Mains Road, Edinburgh EH9 3LA Desks. 0131-667 1000 Fax 0131-668 2683 The British Geological Survey carries out the geological survey of e-mail: [email protected] Great Britain and Northern Ireland (the latter as an agency service for the government of Northern Ireland), and of the London Information Office at the Natural History Museum surrounding continental shelf, as well as its basic research (Earth Galleries), Exhibition Road, South Kensington, London projects. -
Late Cretaceous Nautilid Juveniles of Cymatoceras Reussi and Eutrephoceras Aff
SBORNÍK NÁRODNÍHO MUZEA V PRAZE ACTA MUSEI NATIONALIS PRAGAE Řada B – Přírodní vědy • sv. 70 • 2014 • čís. 3–4 • s. 143–152 Series B – Historia Naturalis • vol. 70 • 2014 • no. 3–4 • pp. 143–152 LATE CRETACEOUS NAUTILID JUVENILES OF CYMATOCERAS REUSSI AND EUTREPHOCERAS AFF. SUBLAEVIGATUM – SCARCE FOSSILS UNDER RISK OF PYRITE DEGRADATION JIŘÍ FRANK JAN SKLENÁŘ BORIS EKRT National Museum, Department of Palaeontology, Václavské náměstí 68, 115 74 Praha 1, the Czech Republic; e-mails: [email protected]; [email protected]; [email protected] Frank, J., Sklenář, J. Ekrt, B. (2014): Late Cretaceous nautilid juveniles of Cymatoceras reussi and Eutrephoceras aff. sublaevigatum – scarce fossils under risk of pyrite degradation. – Acta Mus. Nat. Pragae, Ser. B, Hist. Nat., 70(3-4): 143–152, Praha. ISSN 1804-6479. Abstract. The syntype collection of “Nautilus reussi” has been subject to a detailed revision resulting in confirmation of at least provisional validity of the species represented by a single juvenile specimen. This species, restricted now to the Late Coniacian, is inserted into the genus Cymatoceras Hyatt, 1884. The rest of the collection differs from the original description and is left separately as Eutrephoceras aff. sublaevi- gatum, being considered juveniles of the species. The lithology, geographic and stratigraphic position of the type locality of Cymatoceras reussi (FRITSCH IN FRITSCH ET SCHLÖNBACH, 1872) as well as the other sites are discussed here. The valuable material is endangered due to pyrite degradation as relics of this unstable sulphide are still at present hidden in the secondary limonitic material. The degradation products cause volumetric expansion resulting in formation of crevices and loss of integrity. -
Spisula Solidissima) Using a Spatially Northeastern Continental Shelf of the United States
300 Abstract—The commercially valu- able Atlantic surfclam (Spisula so- Management strategy evaluation for the Atlantic lidissima) is harvested along the surfclam (Spisula solidissima) using a spatially northeastern continental shelf of the United States. Its range has con- explicit, vessel-based fisheries model tracted and shifted north, driven by warmer bottom water temperatures. 1 Declining landings per unit of effort Kelsey M. Kuykendall (contact author) (LPUE) in the Mid-Atlantic Bight Eric N. Powell1 (MAB) is one result. Declining stock John M. Klinck2 abundance and LPUE suggest that 1 overfishing may be occurring off Paula T. Moreno New Jersey. A management strategy Robert T. Leaf1 evaluation (MSE) for the Atlantic surfclam is implemented to evalu- Email address for contact author: [email protected] ate rotating closures to enhance At- lantic surfclam productivity and in- 1 Gulf Coast Research Laboratory crease fishery viability in the MAB. The University of Southern Mississippi Active agents of the MSE model 703 East Beach Drive are individual fishing vessels with Ocean Springs, Mississippi 39564 performance and quota constraints 2 Center for Coastal Physical Oceanography influenced by captains’ behavior Department of Ocean, Earth, and Atmospheric Sciences over a spatially varying population. 4111 Monarch Way, 3rd Floor Management alternatives include Old Dominion University 2 rules regarding closure locations Norfolk, Virginia 23529 and 3 rules regarding closure du- rations. Simulations showed that stock biomass increased, up to 17%, under most alternative strategies in relation to estimated stock biomass under present-day management, and The Atlantic surfclam (Spisula solid- ally not found where average bottom LPUE increased under most alterna- issima) is an economically valuable temperatures exceed 25°C (Cargnelli tive strategies, by up to 21%. -
Trans-Tethyan Correlation
Acta Geologica Polonica, Vol. 67 (2017), No. 1, pp. 75–108 DOI: 10.1515/agp-2017-0005 Trans-Tethyan correlation of the Lower–Middle Cenomanian boundary interval; southern England (Southerham, near Lewes, Sussex) and Douar el Khiana, northeastern Algeria WILLIAM J. KENNEDY1 and ANDREW S. GALE2 1Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW, and Department of Earth Sciences, South Parks Road, Oxford OX1 3AN, United Kingdom. E-mail: [email protected] 2Department of Earth and Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, United Kingdom. E-mail: [email protected] ABSTRACT: Kennedy, W.J. and Gale, A.S. 2017. Trans-Tethyan correlation of the Lower–Middle Cenomanian boundary interval; southern England (Southerham, near Lewes, Sussex) and Douar el Khiana, northeastern Algeria. Acta Geologica Polonica, 67 (1), 75–108. Warszawa. A 480 m section of marls with widely separated levels of nodular limestone in the Fahdene Formation north of Bou Khadra in Tebessa Province, northeastern Algeria, spans the Lower/Middle Cenomanian boundary. A total of 30 ammonite species are present, of which two: Forbesiceras reversum and Calycoceras (Newboldiceras) algeriense are new. The fauna allows recognition of the Northwest European upper Lower Cenomanian Mantelliceras dixoni Zone, the succeeding lower Middle Cenomanian Cunningtoniceras inerme Zone, the Acanthoceras rhotomagense Zone and its subzones of Turrilites costatus and Turrilites acutus. The sequence of index species occurs in the same order in both north-eastern Tunisia and the Southerham Grey Pit in Sussex (and indeed elsewhere in North- west Europe), indicating these to be robust assemblage zones and subzones that can be recognised on both the north and south sides of the Tethys. -
Colour Patterns in Early Devonian Cephalopods from the Barrandian Area: Taphonomy and Taxonomy
Colour patterns in Early Devonian cephalopods from the Barrandian Area: Taphonomy and taxonomy VOJTĚCH TUREK Turek, V. 2009. Colour patterns in Early Devonian cephalopods from the Barrandian Area: Taphonomy and taxonomy. Acta Palaeontologica Polonica 54 (3): 491–502. DOI: 10.4202/app.2007.0064. Five cephalopod specimens from the Lower Devonian of Bohemia (Czech Republic) preserve colour patterns. They in− clude two taxonomically undeterminable orthoceratoids and three oncocerid nautiloids assigned to the genus Ptenoceras. The two fragments of orthocone cephalopods from the lowest Devonian strata (Lochkovian, Monograptus uniformis Zone) display colour patterns unusual in orthoceratoids. They have irregular undulating and zigzag strips that are pre− served on counterparts of adapertural regions of specimens flattened in shale, despite their original aragonitic shell having been completely dissolved. These are probably the result of the proteinous pigment inside the shell wall, being substituted during diagenesis by secondary minerals leaving only an altered trace of the original shell. Orthoceratoids from sediments unsuitable for preservation of this feature discussed here thus demonstrate an exceptional case of preservation of colour patterns, not only within Devonian cephalopods but also within other Devonian molluscs. Three specimens of Ptenoceras that preserve colour patterns come from younger Lower Devonian strata. Oblique spiral adaperturally bifurcating bands are preserved in P. alatum from the Pragian and zigzags in P. nudum from the Dalejan. Juvenile specimen of Ptenoceras? sp. from the Pragian exhibits highly undulating transversal bands—a pattern resembling colour markings in some Silu− rian oncocerids. Dark grey wavy lines observed on the superficially abraded adapical part of a phragmocone of nautiloid Pseudorutoceras bolli and interpreted formerly to be colour markings are here reinterpreted as secondary pigmented growth lines. -
Spineless Spineless Rachael Kemp and Jonathan E
Spineless Status and trends of the world’s invertebrates Edited by Ben Collen, Monika Böhm, Rachael Kemp and Jonathan E. M. Baillie Spineless Spineless Status and trends of the world’s invertebrates of the world’s Status and trends Spineless Status and trends of the world’s invertebrates Edited by Ben Collen, Monika Böhm, Rachael Kemp and Jonathan E. M. Baillie Disclaimer The designation of the geographic entities in this report, and the presentation of the material, do not imply the expressions of any opinion on the part of ZSL, IUCN or Wildscreen concerning the legal status of any country, territory, area, or its authorities, or concerning the delimitation of its frontiers or boundaries. Citation Collen B, Böhm M, Kemp R & Baillie JEM (2012) Spineless: status and trends of the world’s invertebrates. Zoological Society of London, United Kingdom ISBN 978-0-900881-68-8 Spineless: status and trends of the world’s invertebrates (paperback) 978-0-900881-70-1 Spineless: status and trends of the world’s invertebrates (online version) Editors Ben Collen, Monika Böhm, Rachael Kemp and Jonathan E. M. Baillie Zoological Society of London Founded in 1826, the Zoological Society of London (ZSL) is an international scientifi c, conservation and educational charity: our key role is the conservation of animals and their habitats. www.zsl.org International Union for Conservation of Nature International Union for Conservation of Nature (IUCN) helps the world fi nd pragmatic solutions to our most pressing environment and development challenges. www.iucn.org Wildscreen Wildscreen is a UK-based charity, whose mission is to use the power of wildlife imagery to inspire the global community to discover, value and protect the natural world.