New Data from Monoplacophora and a Carefully-Curated Dataset Resolve Molluscan Relationships Kevin M
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27-60, 1999 Redescription Problematic Alpine Oxychilus
BASTERIA, 63: 27-60, 1999 Redescription of two problematic Alpine Oxychilus: O. adamii (Westerlund, 1886) and O. polygyra (Pollonera, 1885) (Pulmonata, Zonitidae) F. Giusti & G. Manganelli Dipartimento di Biologia Evolutiva dell'Universita di Siena, Via P.A. Mattioli 4, 1-53100 Siena, Italy of The taxonomic and nomenclatural status Oxychilus adamii (Westerlund, 1886) and O. polygyra is (Pollonera, 1885) revised. These two, very similar species are tentatively assigned to Mediterranean of characterized absent short a ‘subgenus’ Oxychilus by (1) or very flagellum; (2) penial retractor inserted where epiphallus ends and proximal penis begins; (3) internal ornamentation of penis of and of of consisting pleats rows papillae, some which or all with apical thorn; (4) short slender epiphallus internally with series of transverse crests on one side and a few longitudinal the pleats on other; (5) mucous gland forming muff of glandular tissue, denser and yellower around distal portion of free oviduct; (6) and short mesocone on the central tooth. O. adamii is medium-sized shell 16.1 ± 1.0 distinguished by a (diameter mm) and very small papillae withoutapical thorn covering the initialportion of the proximal penis. O. polygyra is distinguished small shell 10.4 ± 0.5 and by a (diameter mm) large papillae with an evident cuticularized The with apical thorn covering the initial portion of the proximal penis. paper concludes a review of the current status of the Oxychilus taxonomy, including main problems and some tentative solutions to be verified in the context of individual revisions. words: Key Gastropoda, Pulmonata, Zonitidae, Oxychilus, taxonomy, nomenclature, Italy. INTRODUCTION Ten species of Oxychilus Fitzinger, 1833, are reported from the Alps: O. -
Nail Anatomy and Physiology for the Clinician 1
Nail Anatomy and Physiology for the Clinician 1 The nails have several important uses, which are as they are produced and remain stored during easily appreciable when the nails are absent or growth. they lose their function. The most evident use of It is therefore important to know how the fi ngernails is to be an ornament of the hand, but healthy nail appears and how it is formed, in we must not underestimate other important func- order to detect signs of pathology and understand tions, such as the protective value of the nail plate their pathogenesis. against trauma to the underlying distal phalanx, its counterpressure effect to the pulp important for walking and for tactile sensation, the scratch- 1.1 Nail Anatomy ing function, and the importance of fi ngernails and Physiology for manipulation of small objects. The nails can also provide information about What we call “nail” is the nail plate, the fi nal part the person’s work, habits, and health status, as of the activity of 4 epithelia that proliferate and several well-known nail features are a clue to sys- differentiate in a specifi c manner, in order to form temic diseases. Abnormal nails due to biting or and protect a healthy nail plate [1 ]. The “nail onychotillomania give clues to the person’s emo- unit” (Fig. 1.1 ) is composed by: tional/psychiatric status. Nail samples are uti- • Nail matrix: responsible for nail plate production lized for forensic and toxicology analysis, as • Nail folds: responsible for protection of the several substances are deposited in the nail plate nail matrix Proximal nail fold Nail plate Fig. -
The Impact of Hydraulic Blade Dredging on a Benthic Megafaunal Community in the Clyde Sea Area, Scotland
Journal of Sea Research 50 (2003) 45–56 www.elsevier.com/locate/seares The impact of hydraulic blade dredging on a benthic megafaunal community in the Clyde Sea area, Scotland C. Hauton*, R.J.A. Atkinson, P.G. Moore University Marine Biological Station Millport (UMBSM), Isle of Cumbrae, Scotland, KA28 0EG, UK Received 4 December 2002; accepted 13 February 2003 Abstract A study was made of the impacts on a benthic megafaunal community of a hydraulic blade dredge fishing for razor clams Ensis spp. within the Clyde Sea area. Damage caused to the target species and the discard collected by the dredge as well as the fauna dislodged by the dredge but left exposed at the surface of the seabed was quantified. The dredge contents and the dislodged fauna were dominated by the burrowing heart urchin Echinocardium cordatum, approximately 60–70% of which survived the fishing process intact. The next most dominant species, the target razor clam species Ensis siliqua and E. arcuatus as well as the common otter shell Lutraria lutraria, did not survive the fishing process as well as E. cordatum, with between 20 and 100% of individuals suffering severe damage in any one dredge haul. Additional experiments were conducted to quantify the reburial capacity of dredged fauna that was returned to the seabed as discard. Approximately 85% of razor clams retained the ability to rapidly rebury into both undredged and dredged sand, as did the majority of those heart urchins Echinocardium cordatum which did not suffer aerial exposure. Individual E. cordatum which were brought to surface in the dredge collecting cage were unable to successfully rebury within three hours of being returned to the seabed. -
1 Crustaceans in Cold Seep Ecosystems: Fossil Record, Geographic Distribution, Taxonomic Composition, 2 and Biology 3 4 Adiël A
1 Crustaceans in cold seep ecosystems: fossil record, geographic distribution, taxonomic composition, 2 and biology 3 4 Adiël A. Klompmaker1, Torrey Nyborg2, Jamie Brezina3 & Yusuke Ando4 5 6 1Department of Integrative Biology & Museum of Paleontology, University of California, Berkeley, 1005 7 Valley Life Sciences Building #3140, Berkeley, CA 94720, USA. Email: [email protected] 8 9 2Department of Earth and Biological Sciences, Loma Linda University, Loma Linda, CA 92354, USA. 10 Email: [email protected] 11 12 3South Dakota School of Mines and Technology, Rapid City, SD 57701, USA. Email: 13 [email protected] 14 15 4Mizunami Fossil Museum, 1-47, Yamanouchi, Akeyo-cho, Mizunami, Gifu, 509-6132, Japan. 16 Email: [email protected] 17 18 This preprint has been submitted for publication in the Topics in Geobiology volume “Ancient Methane 19 Seeps and Cognate Communities”. Specimen figures are excluded in this preprint because permissions 20 were only received for the peer-reviewed publication. 21 22 Introduction 23 24 Crustaceans are abundant inhabitants of today’s cold seep environments (Chevaldonné and Olu 1996; 25 Martin and Haney 2005; Karanovic and Brandão 2015), and could play an important role in structuring 26 seep ecosystems. Cold seeps fluids provide an additional source of energy for various sulfide- and 27 hydrocarbon-harvesting bacteria, often in symbiosis with invertebrates, attracting a variety of other 28 organisms including crustaceans (e.g., Levin 2005; Vanreusel et al. 2009; Vrijenhoek 2013). The 29 percentage of crustaceans of all macrofaunal specimens is highly variable locally in modern seeps, from 30 0–>50% (Dando et al. 1991; Levin et al. -
Mollusca: Polyplacophora: Lepidopleurida)
Life history, patchy distribution, and patchy taxonomy in a shallow- water invertebrate (Mollusca Polyplacophora: Lepidopleurida) Sigwart, J. D., & Chen, C. (2017). Life history, patchy distribution, and patchy taxonomy in a shallow-water invertebrate (Mollusca Polyplacophora: Lepidopleurida). Marine Biodiversity. https://doi.org/10.1007/s12526- 017-0688-1 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 © 2017 The Authors. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http:// creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made 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:08. -
Mollusca: Polyplacophora: Lepidopleurida)
Ruthenica, 2016, vol. 26, No. 3-4: 145-151. © Ruthenica, 2016 Published online September 18, 2016. http: www.ruthenica.com A new South African Leptochiton (Mollusca: Polyplacophora: Lepidopleurida) Boris SIRENKO Zoological Institute, Russian Academy of Sciences, Universitetskaya nab.1, St. Petersburg, 199034, RUSSIAN FEDERATION, e-mail: marine@zin,ru urn:lsid:zoobank.org:pub:4B690F43-F5DC-402A-BFAB-6046A47B1855 ABSTRACT. A new chiton species of the genus Lepto- Systematics chiton is described from the intertidal zone of False Bay, South Africa. The new species is distinguishable Class Polyplacophora Gray, 1821 from other congeneric species by ribbed ventral scales, Subclass Loricata Schumacher, 1817 a wide tail valve and the number of micraesthetes per Order Lepidopleurida Thiele, 1909 each megalaesthete. Family Leptochitonidae Dall, 1889 Genus Leptochiton Gray, 1847 Introduction Type species: Chiton cinereus Montagu, 1803 There are 6 species in genus Leptochiton [L. (non Linnaeus, 1767) = Leptochiton asellus (Gme- sykesi (Sowerby III, 1903), L. chariessa (Bernard, lin, 1791) fide Lovén, 1846, subsequent designation 1963), L. dispersus Kaas 1985, L. permodestus by Gray, 1847. Kaas, 1985; L. meiringae Kaas, 1985 and L. hodg- Genus distribution: Worldwide, Carboniferous- soni (Sirenko, 2000)] [Kaas, 1985; Kaas, Van Belle, Recent. 1985, 1987; Sirenko, 2000, 2015] that inhabit the Leptochiton smirnovi sp. nov. sea floor near South Africa. Five of them live at (Figs 1-6) depths of 70 to 433 m. L. hodgsoni was found in the intertidal zone. This species was originally at- urn:lsid:zoobank.org:act:034AF8DF-EA96-45D5- tributed to the genus Parachiton Thiele, 1909 [Si- 8159-FDAE82365FCC renko, 2000]. However, later, Hiroshi Saito wrote me that the species belongs to the genus Leptochi- Type material. -
Fauna of New Zealand Ko Te Aitanga Pepeke O Aotearoa
aua o ew eaa Ko te Aiaga eeke o Aoeaoa IEEAE SYSEMAICS AISOY GOU EESEAIES O ACAE ESEAC ema acae eseac ico Agicuue & Sciece Cee P O o 9 ico ew eaa K Cosy a M-C aiièe acae eseac Mou Ae eseac Cee iae ag 917 Aucka ew eaa EESEAIE O UIESIIES M Emeso eame o Eomoogy & Aima Ecoogy PO o ico Uiesiy ew eaa EESEAIE O MUSEUMS M ama aua Eiome eame Museum o ew eaa e aa ogaewa O o 7 Weigo ew eaa EESEAIE O OESEAS ISIUIOS awece CSIO iisio o Eomoogy GO o 17 Caea Ciy AC 1 Ausaia SEIES EIO AUA O EW EAA M C ua (ecease ue 199 acae eseac Mou Ae eseac Cee iae ag 917 Aucka ew eaa Fauna of New Zealand Ko te Aitanga Pepeke o Aotearoa Number / Nama 38 Naturalised terrestrial Stylommatophora (Mousca Gasooa Gay M ake acae eseac iae ag 317 amio ew eaa 4 Maaaki Whenua Ρ Ε S S ico Caeuy ew eaa 1999 Coyig © acae eseac ew eaa 1999 o a o is wok coee y coyig may e eouce o coie i ay om o y ay meas (gaic eecoic o mecaica icuig oocoyig ecoig aig iomaio eiea sysems o oewise wiou e wie emissio o e uise Caaoguig i uicaio AKE G Μ (Gay Micae 195— auase eesia Syommaooa (Mousca Gasooa / G Μ ake — ico Caeuy Maaaki Weua ess 1999 (aua o ew eaa ISS 111-533 ; o 3 IS -7-93-5 I ie 11 Seies UC 593(931 eae o uIicaio y e seies eio (a comee y eo Cosy usig comue-ase e ocessig ayou scaig a iig a acae eseac M Ae eseac Cee iae ag 917 Aucka ew eaa Māoi summay e y aco uaau Cosuas Weigo uise y Maaaki Weua ess acae eseac O o ico Caeuy Wesie //wwwmwessco/ ie y G i Weigo o coe eoceas eicuaum (ue a eigo oaa (owe (IIusao G M ake oucio o e coou Iaes was ue y e ew eaIa oey oa ue oeies eseac -
A Review of Ethnographic and Historically Recorded Dentaliurn Source Locations
FISHINGFOR IVORYWORMS: A REVIEWOF ETHNOGRAPHICAND HISTORICALLY RECORDEDDENTALIUM SOURCE LOCATIONS Andrew John Barton B.A., Simon Fraser University, 1979 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS IN THE DEPARTMENT OF ARCHAEOLOGY Q Andrew John Barton 1994 SIMON FRASER UNIVERSITY Burnaby October, 1994 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means without permission of the author. Name: Andrew John Barton Degree: Master of Arts (Archaeology) Title of Thesis: Fishing for Ivory Worms: A Review of Ethnographic and Historically Recorded Dentaliurn Source Locations Examining Committee: Chairperson: Jack D. Nance - -, David V. Burley Senior Supervisor Associate Professor Richard Inglis External Examiner Department of Aboriginal Affairs Government of British Columbia PARTIAL COPYRIGHT LICENSE I hereby grant to Simon Fraser University the right to lend my thesis or dissertation (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this thesis for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Title of ThesisIDissertation: Fishing for Ivory Worms: A Review of Ethnographic and Historically Recorded Dentalium Source Locations Author: Andrew John Barton Name October 14, 1994 Date This study reviews and examines historic and ethnographic written documents that identify locations where Dentaliurn shells were procured by west coast Native North Americans. -
Mollusca) Found Along the Brazilian Coast, with Two New Synonymies in the Genus Gadila Gray, 1847
Biota Neotrop., vol. 13, no. 2 A commented list of Scaphopoda (Mollusca) found along the Brazilian coast, with two new synonymies in the genus Gadila Gray, 1847 Leonardo Santos de Souza1,2, Isabella Campos Vieira Araújo1 & Carlos Henrique Soares Caetano1 1Departamento de Zoologia, Instituto de Biociências, Universidade Federal do Estado do Rio de Janeiro – UNIRIO, Av. Pasteur, 458, Urca, CEP 22290-240, Rio de Janeiro, RJ, Brasil 2Corresponding author: Leonardo Santos de Souza, e-mail: [email protected] SOUZA, L.S., ARAÚJO, I.C.V. & CAETANO, C.H.S. A commented list of Scaphopoda (Mollusca) found along the Brazilian coast, with two new synonymies in the genus Gadila Gray, 1847. Biota Neotrop. (13)2: http://www.biotaneotropica.org.br/v13n2/en/abstract?inventory+bn03213022013 Abstract: This review aims to present an updated checklist of scaphopods, based mainly on literature database. There is a total of 40 species (six families) for Brazil, including information about the distribution and bathymetric range of each taxon. We propose two synonyms with the aid of morphometry of the shell, for the genus Gadila: G. longa as junior synonym of G. elongata and G. robusta as junior synonym of G. pandionis. Keywords: scaphopods, morphometry, synonyms, distribution, bathymetry. SOUZA, L.S., ARAÚJO, I.C.V. & CAETANO, C.H.S. Lista comentada dos Scaphopoda (Mollusca) encontrados ao longo da costa Brasileira, com duas novas sinonímias no gênero Gadila Gray, 1847. Biota Neotrop. 13(2): http://www.biotaneotropica.org.br/v13n2/pt/abstract?inventory+bn0321302201 Resumo: Uma lista atualizada dos escafópodes da costa brasileira pertencentes a seis famílias é apresentada baseada principalmente em dados da literatura. -
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1 Mobilising molluscan models and genomes in biology 2 Angus Davison1 and Maurine Neiman2 3 1. School of Life Sciences, University Park, University of Nottingham, NG7 2RD, UK 4 2. Department of Biology, University of Iowa, Iowa City, IA, USA and Department of Gender, 5 Women's, and Sexuality Studies, University of Iowa, Iowa, City, IA, USA 6 Abstract 7 Molluscs are amongst the most ancient, diverse, and important of all animal taxa. Even so, 8 no individual mollusc species has emerged as a broadly applied model system in biology. 9 We here make the case that both perceptual and methodological barriers have played a role 10 in the relative neglect of molluscs as research organisms. We then summarize the current 11 application and potential of molluscs and their genomes to address important questions in 12 animal biology, and the state of the field when it comes to the availability of resources such 13 as genome assemblies, cell lines, and other key elements necessary to mobilising the 14 development of molluscan model systems. We conclude by contending that a cohesive 15 research community that works together to elevate multiple molluscan systems to ‘model’ 16 status will create new opportunities in addressing basic and applied biological problems, 17 including general features of animal evolution. 18 Introduction 19 Molluscs are globally important as sources of food, calcium and pearls, and as vectors of 20 human disease. From an evolutionary perspective, molluscs are notable for their remarkable 21 diversity: originating over 500 million years ago, there are over 70,000 extant mollusc 22 species [1], with molluscs present in virtually every ecosystem. -
Spatial Variability in Recruitment of an Infaunal Bivalve
Spatial Variability in Recruitment of an Infaunal Bivalve: Experimental Effects of Predator Exclusion on the Softshell Clam (Mya arenaria L.) along Three Tidal Estuaries in Southern Maine, USA Author(s): Brian F. Beal, Chad R. Coffin, Sara F. Randall, Clint A. Goodenow Jr., Kyle E. Pepperman, Bennett W. Ellis, Cody B. Jourdet and George C. Protopopescu Source: Journal of Shellfish Research, 37(1):1-27. Published By: National Shellfisheries Association https://doi.org/10.2983/035.037.0101 URL: http://www.bioone.org/doi/full/10.2983/035.037.0101 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Journal of Shellfish Research, Vol. 37, No. 1, 1–27, 2018. SPATIAL VARIABILITY IN RECRUITMENT OF AN INFAUNAL BIVALVE: EXPERIMENTAL EFFECTS OF PREDATOR EXCLUSION ON THE SOFTSHELL CLAM (MYA ARENARIA L.) ALONG THREE TIDAL ESTUARIES IN SOUTHERN MAINE, USA 1,2 3 2 3 BRIAN F. -
Geobiological Events in the Ediacaran Period
Geobiological Events in the Ediacaran Period Shuhai Xiao Department of Geosciences, Virginia Tech, Blacksburg, VA 24061, USA NSF; NASA; PRF; NSFC; Virginia Tech Geobiology Group; CAS; UNLV; UCR; ASU; UMD; Amherst; Subcommission of Neoproterozoic Stratigraphy; 1 Goals To review biological (e.g., acanthomorphic acritarchs; animals; rangeomorphs; biomineralizing animals), chemical (e.g., carbon and sulfur isotopes, oxygenation of deep oceans), and climatic (e.g., glaciations) events in the Ediacaran Period; To discuss integration and future directions in Ediacaran geobiology; 2 Knoll and Walter, 1992 • Acanthomorphic acritarchs in early and Ediacara fauna in late Ediacaran Period; • Strong carbon isotope variations; • Varanger-Laplandian glaciation; • What has happened since 1992? 3 Age Constraints: South China (538.2±1.5 Ma) 541 Ma Cambrian Dengying Ediacaran Sinian 551.1±0.7 Ma Doushantuo 632.5±0.5 Ma 635 Ma 635.2±0.6 Ma Nantuo (Tillite) 636 ± 5Ma Cryogenian Nanhuan 654 ± 4Ma Datangpo 663±4 Ma Neoproterozoic Neoproterozoic Jiangkou Group Banxi Group 725±10 Ma Tonian Qingbaikouan 1000 Ma • South China radiometric ages: Condon et al., 2005; Hoffmann et al., 2004; Zhou et al., 2004; Bowring et al., 2007; S. Zhang et al., 2008; Q. Zhang et al., 2008; • Additional ages from Nama Group (Namibia), Conception Group (Newfoundland), and Vendian (White Sea); 4 The Ediacaran Period Ediacara fossils Cambrian 545 Ma Nama assemblage 555 Ma White Sea assemblage 565 Ma Avalon assemblage 575 Ma 585 Ma Doushantuo biota 595 Ma 605 Ma Ediacaran Period 615 Ma