THE ANATOMY of NEOPILINA GALATHEAE LEMCHE. 1957 (Molluscs Tryblidiacea)
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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 -
Monoplacophoran Limpet
16 McLean: Monoplacophoran Limpet FIGURES 17-21. Neopilinid radular ribbons, magnifications adjusted to show a similar number of teeth rows. FIGURE 17, Vema (Vema) ewingi. intact ribbon with teeth aligned (LACM 65-11, 6200 m. 110 mi. W of Callao. Pern. R/V ANTON BRUUN, 24 November 1965). FIGURE 18, Vema (Vema) ewingi. another portion of same ribbon with lateral teeth turned to the side. FIGURE 19. Neopilina veleronis. intact ribbon of paratype, teeth not aligned (AHF 603, 2730-2769 m, 30 mi. W of Natividad Island. Baja California, Mexico). FIGURE 20, Vema (Laevipilina) hyalina new species, intact ribbon with teeth aligned, focused on shafts of lateral teeth (LACM 19148). FIGURE 21, Vema (Laevipilina) hyalina, same ribbon, focused on fringe of first marginal teeth. instead of the highly reduced condition in these two species. Al- small-sized species have similar teeth. Radular differences among though the first lateral of N. veleronis is somewhat larger than it the species examined are quantitative rather than qualitative, sup- is in the other two species, that of V. hyalina is still the larger. porting placement of the four species in the same family. A study The fringed first marginal of V. hyalina is much broader than in of the radulae of the other three living species of neopilinids N. veleronis. Only in V. hyalina is the fringed tooth so broad that should reveal further specific differences. it overlaps the opposite member in the central part of the ribbon. The radula of neopilinid monoplacophorans is very similar to The second and third laterals of V. -
Morphology and Systematic Position of Tryhlidium Canadense Whiteaves
Morphology and systematic position of Tryblidium canadense Whiteaves, 1884 (Mollusca) from the Silurian of North America JOHNS. PEEL Peel, J. S.: Morphology and systematic position of Tryblidium Canadense Whiteaves, 1884 (Mollusca) from the Silurian of North America. Bull. geol. Soc. Denmark, vol. 38, pp. 43-51. Copenhagen, April 25th, 1990. https://doi.org/10.37570/bgsd-1990-38-04 The nomenclative history of Tryblidium canadense Whiteaves, 1884, a large, oval, univalved mollusc originally described from the Silurian Guelph Formation of Ontario, is reviewed. Following comparison to Archinace/la Ulrich & Scofield, 1897, in which genus it has generally been placed for almost a century, Whiteaves' species is redescribed and assigned to a new gastropod genus, Guelphinace/la. John S. Peel, Geological Survey of Greenland, Oster Voldgade JO, 1350 Copenhagen K, Denmark. February 10th, 1989. Whiteaves (1884) described a single internal the sub-apical wall. He commented that the mould of a large (45 mm), oval, univalved mol structure seemed to be a single continuous mus lusc from the Guelph Formation (Silurian) of cular impression and not two separate depres Hespeler, Ontario, Canada as Tryblidium Cana sions, as suggested by Lindstrom (1884), al dense (Fig. 1). Uncertainty surrounding its sys though he did not refer directly to the latter's tematic position developed immediately when description. He made no reference to the thin Lindstrom (1884) questioned the assignment to dorsal band which Lindstrom (1884) had consid the genus Tryblidium -
The Slit Bearing Nacreous Archaeogastropoda of the Triassic Tropical Reefs in the St
Berliner paläobiologische Abhandlungen 10 5-47 Berlin 2009-11-11 The slit bearing nacreous Archaeogastropoda of the Triassic tropical reefs in the St. Cassian Formation with evaluation of the taxonomic value of the selenizone Klaus Bandel Abstract: Many Archaeogastropoda with nacreous shell from St. Cassian Formation have a slit in the outer lip that gives rise to a selenizone. The primary objective of this study is to analyze family level characters, provide a revision of some generic classifications and compare with species living today. Members of twelve families are recognized with the Lancedellidae n. fam., Rhaphistomellidae n. fam., Pseudowortheniellidae n. fam., Pseudoschizogoniidae n. fam., Wortheniellidae n. fam. newly defined. While the organization of the aperture and the shell structure is similar to that of the living Pleurotomariidae, morphology of the early ontogenetic shell and size and shape of the adult shell distinguish the Late Triassic slit bearing Archae- gastropoda from these. In the reef environment of the tropical Tethys Ocean such Archaeogastropoda were much more diverse than modern representatives of that group from the tropical Indo-Pacific Ocean. Here Haliotis, Seguenzia and Fossarina represent living nacreous gastropods with slit and are compared to the fossil species. All three have distinct shape and arrangement of the teeth in their radula that is not related to that of the Pleurotomariidae and also differs among each other. The family Fossarinidae n. fam. and the new genera Pseudowortheniella and Rinaldoella are defined, and a new species Campbellospira missouriensis is described. Zusammenfassung: In der St. Cassian-Formation kommen zahlreiche Arten der Archaeogastropoda vor, die eine perlmutterige Schale mit Schlitz in der Außenlippe haben, welcher zu einem Schlitzband führt. -
Annelids, Arthropods, Molluscs 2. Very Diverse, Mostly Marine B. Characteristics 1
Molluscs A. Introduction 1. Three big Protostome Phyla - Annelids, Arthropods, Molluscs 2. Very diverse, mostly marine B. Characteristics 1. Bilateral symmetrical, unsegmented with definite head 2. Muscular foot 3. Mantle - mantle cavity a. Secretes shell - Calcium carbonate 4. Ciliated epithelium 5. Coelom reduced - around heart 6. Open circulatory system 7. Gaseous exchange by gills, lung, or just body surface 8. Metanephridia - empty into mantle cavity C. Body Plan 1. Generalized mollusc a. Mantle - secreted shell b. Mantle - cavity has gills - posterior - location important 2. Head-foot a. Head - 1. Radula - rasping tongue a. Mostly for scraping - snails b. Some (Cone shells) modified to a dart and poison b. Foot - Variously modified 1. Ventral sole-like structure - movement 2. May be shaped for burrowing 3. Shell 1. Made of Calcium Carbonate Molluscs 2. Three layers a. Periostracum - organic layer - not always visible b. Prismatic layer - prim-shaped crystals of calcium carbonate 1. Secreted by gladular margin of mantle 2. Grows as animal grows c. Nacreous layer 1. Continuously secreted by mantle on interior of shell 2. Pearls 4. Reproduction a. Larval stages 1. Trochophore - first stage to hatch from egg 2. Veliger - planktonic larva of most marine snails and bivalves a. Beginnings of foot, shell and mantle D. Classes - problem of segmentation - is it the original body plan - have molluscs lost segementation? 1. Monoplacophora - genus Neopilina a. Serial repetition in body form b. Single shell c. Interesting story of discovery 2. Polyplacophora - chitons a. Segmented shell - plates b. Multiple gills down side of body - not like generalized plan c. Rock dwellers that use radula to scrape algae off rocks 3. -
Mollusca, Archaeogastropoda) from the Northeastern Pacific
Zoologica Scripta, Vol. 25, No. 1, pp. 35-49, 1996 Pergamon Elsevier Science Ltd © 1996 The Norwegian Academy of Science and Letters Printed in Great Britain. All rights reserved 0300-3256(95)00015-1 0300-3256/96 $ 15.00 + 0.00 Anatomy and systematics of bathyphytophilid limpets (Mollusca, Archaeogastropoda) from the northeastern Pacific GERHARD HASZPRUNAR and JAMES H. McLEAN Accepted 28 September 1995 Haszprunar, G. & McLean, J. H. 1995. Anatomy and systematics of bathyphytophilid limpets (Mollusca, Archaeogastropoda) from the northeastern Pacific.—Zool. Scr. 25: 35^9. Bathyphytophilus diegensis sp. n. is described on basis of shell and radula characters. The radula of another species of Bathyphytophilus is illustrated, but the species is not described since the shell is unknown. Both species feed on detached blades of the surfgrass Phyllospadix carried by turbidity currents into continental slope depths in the San Diego Trough. The anatomy of B. diegensis was investigated by means of semithin serial sectioning and graphic reconstruction. The shell is limpet like; the protoconch resembles that of pseudococculinids and other lepetelloids. The radula is a distinctive, highly modified rhipidoglossate type with close similarities to the lepetellid radula. The anatomy falls well into the lepetelloid bauplan and is in general similar to that of Pseudococculini- dae and Pyropeltidae. Apomorphic features are the presence of gill-leaflets at both sides of the pallial roof (shared with certain pseudococculinids), the lack of jaws, and in particular many enigmatic pouches (bacterial chambers?) which open into the posterior oesophagus. Autapomor- phic characters of shell, radula and anatomy confirm the placement of Bathyphytophilus (with Aenigmabonus) in a distinct family, Bathyphytophilidae Moskalev, 1978. -
Four New Pseudococculinid Limpets Collected by the Deep-Submersible Alvin in the Eastern Pacific By
THE VELIGER © CMS, Inc., 1991 The Veliger 34(l):38-47 (January 2, 1991) Four New Pseudococculinid Limpets Collected by the Deep-Submersible Alvin in the Eastern Pacific by JAMES H. McLEAN Los Angeles County Museum of Natural History, 900 Exposition Boulevard, Los Angeles, California 90007, USA Abstract. Four new species of Pseudococculinidae collected with the deep-submersible Alvin are described. One species represents a new monotypic genus, Punctabyssia, and two represent new sub genera: Dictyabyssia (of Caymanabyssia Moskalev, 1976) and Gordabyssia (of Amphiplica Haszprunar 1988). New species are: Punctabyssia tibbettsi and Caymanabyssia (Dictyabyssia) fosteri, both from the same piece of wood at abyssal depths on the East Pacific Rise Axis near 12°N, and two from abyssal depths on the Gorda Ridge off northern California, Caymanabyssia (Caymanabyssia) vandoverae and Amphiplica (Gordabyssia) gordensis. The latter is the first member of the family to be recovered from sulfide crust in the hydrothermal-vent habitat. New character states for the radula and protoconch are defined for the new genus Punctabyssia. INTRODUCTION of hydrothermal vents, and another from sulfide crust pro duced by hydrothermal vents. The latter species represents The cocculiniform limpets include a number of deep-sea a new monotypic subgenus and is the first member of the families in which there is an association with biogenic family restricted to the hydrothermal-vent habitat. substrates (for review see HASZPRUNAR, 1988b). Until re cently the only method by which these limpets have been Recent work on the systematics and anatomy of the recovered has been by chance trawling of pieces of wood pseudococculinid limpets (MOSKALEV, 1976; HICKMAN, or other biogenic substrates. -
Keeping a Lid on It: Muscle Scars and the Mystery of the Mobergellidae
1 Keeping a lid on it: muscle scars and the mystery of the 2 Mobergellidae 3 4 TIMOTHY P. TOPPER1,2* and CHRISTIAN B. SKOVSTED1 5 6 1Department of Palaeobiology, Swedish Museum of Natural History, P.O. Box 50007, 7 SE-104 05, Stockholm, Sweden. 8 2Palaeoecosystems Group, Department of Earth Sciences, Durham University, Durham 9 DH1 3LE, UK. 10 11 Mobergellans were one of the first Cambrian skeletal groups to be recognized yet have 12 long remained one of the most problematic in terms of biological function and affinity. 13 Typified by a disc-shaped, phosphatic sclerite the most distinctive character of the 14 group is a prominent set of internal scars, interpreted as representing sites of former 15 muscle attachment. Predominantly based on muscle scar distribution, mobergellans 16 have been compared to brachiopods, bivalves and monoplacophorans, however a 17 recurring theory that the sclerites acted as operculum remains untested. Rather than 18 correlate the number of muscle scars between taxa, here we focus on the percentage of 19 the inner surface shell area that the scars constitute. We investigate two mobergellan 20 species, Mobergella holsti and Discinella micans comparing the Cambrian taxa with the 21 muscle scars of a variety of extant and fossil marine invertebrate taxa to test if the 22 mobergellan muscle attachment area is compatible with an interpretation as operculum. 23 The only skeletal elements in our study with a comparable muscle attachment 24 percentage are gastropod opercula. Complemented with additional morphological 25 information, our analysis supports the theory that mobergellan sclerites acted as an 26 operculum presumably from a tube-living organism. -
Deep-Water Buccinidae (Gastropoda: Neogastropoda) from Sunken Wood, Vents and Seeps: Molecular Phylogeny and Taxonomy Yu.I
Deep-water Buccinidae (Gastropoda: Neogastropoda) from sunken wood, vents and seeps: molecular phylogeny and taxonomy Yu.I. Kantor, N. Puillandre, K. Fraussen, A.E. Fedosov, P. Bouchet To cite this version: Yu.I. Kantor, N. Puillandre, K. Fraussen, A.E. Fedosov, P. Bouchet. Deep-water Buccinidae (Gas- tropoda: Neogastropoda) from sunken wood, vents and seeps: molecular phylogeny and taxonomy. Journal of the Marine Biological Association of the UK, Cambridge University Press (CUP), 2013, 93 (8), pp.2177-2195. 10.1017/S0025315413000672. hal-02458197 HAL Id: hal-02458197 https://hal.archives-ouvertes.fr/hal-02458197 Submitted on 28 Jan 2020 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. Deep-water Buccinidae (Gastropoda: Neogastropoda) from sunken wood, vents and seeps: Molecular phylogeny and taxonomy KANTOR YU.I.1, PUILLANDRE N.2, FRAUSSEN K.3, FEDOSOV A.E.1, BOUCHET P.2 1 A.N. Severtzov Institute of Ecology and Evolution of Russian Academy of Sciences, Leninski Prosp. 33, Moscow 119071, Russia, 2 Muséum National d’Histoire Naturelle, Departement Systematique et Evolution, UMR 7138, 43, Rue Cuvier, 75231 Paris, France, 3 Leuvensestraat 25, B–3200 Aarschot, Belgium ABSTRACT Buccinidae - like other canivorous and predatory molluscs - are generally considered to be occasional visitors or rare colonizers in deep-sea biogenic habitats. -
Studies on Molluscan Shells: Contributions from Microscopic and Analytical Methods
Micron 40 (2009) 669–690 Contents lists available at ScienceDirect Micron journal homepage: www.elsevier.com/locate/micron Review Studies on molluscan shells: Contributions from microscopic and analytical methods Silvia Maria de Paula, Marina Silveira * Instituto de Fı´sica, Universidade de Sa˜o Paulo, 05508-090 Sa˜o Paulo, SP, Brazil ARTICLE INFO ABSTRACT Article history: Molluscan shells have always attracted the interest of researchers, from biologists to physicists, from Received 25 April 2007 paleontologists to materials scientists. Much information is available at present, on the elaborate Received in revised form 7 May 2009 architecture of the shell, regarding the various Mollusc classes. The crystallographic characterization of Accepted 10 May 2009 the different shell layers, as well as their physical and chemical properties have been the subject of several investigations. In addition, many researches have addressed the characterization of the biological Keywords: component of the shell and the role it plays in the hard exoskeleton assembly, that is, the Mollusca biomineralization process. All these topics have seen great advances in the last two or three decades, Shell microstructures expanding our knowledge on the shell properties, in terms of structure, functions and composition. This Electron microscopy Infrared spectroscopy involved the use of a range of specialized and modern techniques, integrating microscopic methods with X-ray diffraction biochemistry, molecular biology procedures and spectroscopy. However, the factors governing synthesis Electron diffraction of a specific crystalline carbonate phase in any particular layer of the shell and the interplay between organic and inorganic components during the biomineral assembly are still not widely known. This present survey deals with microstructural aspects of molluscan shells, as disclosed through use of scanning electron microscopy and related analytical methods (microanalysis, X-ray diffraction, electron diffraction and infrared spectroscopy). -
Diversity of Animals 355 15 | DIVERSITY of ANIMALS
Concepts of Biology Chapter 15 | Diversity of Animals 355 15 | DIVERSITY OF ANIMALS Figure 15.1 The leaf chameleon (Brookesia micra) was discovered in northern Madagascar in 2012. At just over one inch long, it is the smallest known chameleon. (credit: modification of work by Frank Glaw, et al., PLOS) Chapter Outline 15.1: Features of the Animal Kingdom 15.2: Sponges and Cnidarians 15.3: Flatworms, Nematodes, and Arthropods 15.4: Mollusks and Annelids 15.5: Echinoderms and Chordates 15.6: Vertebrates Introduction While we can easily identify dogs, lizards, fish, spiders, and worms as animals, other animals, such as corals and sponges, might be easily mistaken as plants or some other form of life. Yet scientists have recognized a set of common characteristics shared by all animals, including sponges, jellyfish, sea urchins, and humans. The kingdom Animalia is a group of multicellular Eukarya. Animal evolution began in the ocean over 600 million years ago, with tiny creatures that probably do not resemble any living organism today. Since then, animals have evolved into a highly diverse kingdom. Although over one million currently living species of animals have been identified, scientists are [1] continually discovering more species. The number of described living animal species is estimated to be about 1.4 million, and there may be as many as 6.8 million. Understanding and classifying the variety of living species helps us to better understand how to conserve and benefit from this diversity. The animal classification system characterizes animals based on their anatomy, features of embryological development, and genetic makeup. -
Deep-Sea Video Technology Tracks a Monoplacophoran to the End of Its Trail (Mollusca, Tryblidia)
Deep-sea video technology tracks a monoplacophoran to the end of its trail (Mollusca, Tryblidia) Sigwart, J. D., Wicksten, M. K., Jackson, M. G., & Herrera, S. (2018). Deep-sea video technology tracks a monoplacophoran to the end of its trail (Mollusca, Tryblidia). Marine Biodiversity, 1-8. https://doi.org/10.1007/s12526-018-0860-2 Published in: Marine Biodiversity Document Version: Publisher's PDF, also known as Version of record Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal Publisher rights Copyright 2018 the authors. This is an open access article published under a Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium, provided the author and source are cited. General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:06. Oct. 2021 Deep-sea video technology tracks a monoplacophoran to the end of its trail (Mollusca, Tryblidia) Sigwart, J.