The Ostracod a Neglected Little Crustacean
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Baseline Assessment of the Lake Ohrid Region - Albania
TOWARDS STRENGTHENED GOVERNANCE OF THE SHARED TRANSBOUNDARY NATURAL AND CULTURAL HERITAGE OF THE LAKE OHRID REGION Baseline Assessment of the Lake Ohrid region - Albania IUCN – ICOMOS joint draft report January 2016 Contents ........................................................................................................................................................................... i A. Executive Summary ................................................................................................................................... 1 B. The study area ........................................................................................................................................... 5 B.1 The physical environment ............................................................................................................. 5 B.2 The biotic environment ................................................................................................................. 7 B.3 Cultural Settings ............................................................................................................................ 0 C. Heritage values and resources/ attributes ................................................................................................ 6 C.1 Natural heritage values and resources ......................................................................................... 6 C.2 Cultural heritage values and resources....................................................................................... 12 D. -
Volume 2, Chapter 10-2: Arthropods: Crustacea
Glime, J. M. 2017. Arthropods: Crustacea – Ostracoda and Amphipoda. Chapt. 10-2. In: Glime, J. M. Bryophyte Ecology. Volume 2. 10-2-1 Bryological Interaction. Ebook sponsored by Michigan Technological University and the International Association of Bryologists. Last updated 19 July 2020 and available at <http://digitalcommons.mtu.edu/bryophyte-ecology2/>. CHAPTER 10-2 ARTHROPODS: CRUSTACEA – OSTRACODA AND AMPHPODA TABLE OF CONTENTS CLASS OSTRACODA ..................................................................................................................................... 10-2-2 Adaptations ................................................................................................................................................ 10-2-3 Swimming to Crawling ....................................................................................................................... 10-2-3 Reproduction ....................................................................................................................................... 10-2-3 Habitats ...................................................................................................................................................... 10-2-3 Terrestrial ............................................................................................................................................ 10-2-3 Peat Bogs ............................................................................................................................................ 10-2-4 Aquatic ............................................................................................................................................... -
Crustacea: Ostracoda) in Three Temporary Ponds
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by RERO DOC Digital Library Hydrobiologia (2009) 636:219–232 DOI 10.1007/s10750-009-9952-0 PRIMARY RESEARCH PAPER Dynamics of sexual and parthenogenetic populations of Eucypris virens (Crustacea: Ostracoda) in three temporary ponds Maria Joa˜o Fernandes Martins • Jochen Vandekerkhove • Francesc Mezquita • Olivier Schmit • Juan Rueda • Giampaolo Rossetti • Tadeusz Namiotko Received: 20 May 2009 / Revised: 13 September 2009 / Accepted: 15 September 2009 / Published online: 19 October 2009 Ó Springer Science+Business Media B.V. 2009 Abstract Eucypris virens is a freshwater ostracod This renders the species a potentially valuable in which both sexual reproduction and partheno- model organism to study the ‘queen of evolutionary genesis occur. Sympatric coexistence of both problems’, i.e. why sex is so successful despite its reproductive modes is known in zones of overlap. costs (paradox of sex). In order to maximally exploit this potential, a broad knowledge of the species’ ecology is essential, including an under- standing of its life history and population dynam- ics. Here, the phenology of the species was Electronic supplementary material The online version of followed in three temporary ponds through monthly this article (doi:10.1007/s10750-009-9952-0) contains (Spain) or fortnightly (Poland) samplings, through- supplementary material, which is available to authorized users. out an inundation period. This study confirms the wide ecological tolerances of E. virens. Although Handling editor: K. Martens the species is generally assumed to be univoltine, M. J. F. Martins (&) Á J. Vandekerkhove Á T. Namiotko two hatching periods were observed in the Spanish Laboratory of Limnozoology, Department of Genetics, sites. -
Development of the Eocene Elko Basin, Northeastern Nevada: Implications for Paleogeography and Regional Tectonism
DEVELOPMENT OF THE EOCENE ELKO BASIN, NORTHEASTERN NEVADA: IMPLICATIONS FOR PALEOGEOGRAPHY AND REGIONAL TECTONISM by SIMON RICHARD HAYNES B.Sc, Brock University, 1998 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE in THE FACULTY OF GRADUATE STUDIES (Department of Earth and Ocean Sciences) We accept this thesis as conforming _tQ the required standard THE UNIVERSITY OF BRITISH COLUMBIA April 2003 © Simon Richard Haynes, 2003 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. < Department of \z~<xc ^Qp^rs SOA<S>C-> QS_2> The University of British Columbia Vancouver, Canada ABSTRACT Middle to late Eocene sedimentary and volcanic rocks in northeastern Nevada document the formation of broad lakes, two periods of crustal extension, and provide compelling evidence that the Carlin trend was a topographic high during a major phase of gold formation. The Eocene Elko Formation consists of alluvial-lacustrine rocks that were deposited into a broad, extensional basin between the present-day Ruby Mountains-East Humboldt Range metamorphic core complex and the Tuscarora Mountains. The rocks are divided into the lacustrine-dominated, longer-lived, eastern Elko Basin, and the alluvial braidplain facies of the shorter-lived western Elko Basin. -
Crustacea, Malacostraca)*
SCI. MAR., 63 (Supl. 1): 261-274 SCIENTIA MARINA 1999 MAGELLAN-ANTARCTIC: ECOSYSTEMS THAT DRIFTED APART. W.E. ARNTZ and C. RÍOS (eds.) On the origin and evolution of Antarctic Peracarida (Crustacea, Malacostraca)* ANGELIKA BRANDT Zoological Institute and Zoological Museum, Martin-Luther-King-Platz 3, D-20146 Hamburg, Germany Dedicated to Jürgen Sieg, who silently died in 1996. He inspired this research with his important account of the zoogeography of the Antarctic Tanaidacea. SUMMARY: The early separation of Gondwana and the subsequent isolation of Antarctica caused a long evolutionary his- tory of its fauna. Both, long environmental stability over millions of years and habitat heterogeneity, due to an abundance of sessile suspension feeders on the continental shelf, favoured evolutionary processes of “preadapted“ taxa, like for exam- ple the Peracarida. This taxon performs brood protection and this might be one of the most important reasons why it is very successful (i.e. abundant and diverse) in most terrestrial and aquatic environments, with some species even occupying deserts. The extinction of many decapod crustaceans in the Cenozoic might have allowed the Peracarida to find and use free ecological niches. Therefore the palaeogeographic, palaeoclimatologic, and palaeo-hydrographic changes since the Palaeocene (at least since about 60 Ma ago) and the evolutionary success of some peracarid taxa (e.g. Amphipoda, Isopo- da) led to the evolution of many endemic species in the Antarctic. Based on a phylogenetic analysis of the Antarctic Tanaidacea, Sieg (1988) demonstrated that the tanaid fauna of the Antarctic is mainly represented by phylogenetically younger taxa, and data from other crustacean taxa led Sieg (1988) to conclude that the recent Antarctic crustacean fauna must be comparatively young. -
Late Pleistocene to Recent Ostracod Assemblages from the Western Black Sea Ian Boomer, Francois Guichard, Gilles Lericolais
Late Pleistocene to recent ostracod assemblages from the western Black Sea Ian Boomer, Francois Guichard, Gilles Lericolais To cite this version: Ian Boomer, Francois Guichard, Gilles Lericolais. Late Pleistocene to recent ostracod assemblages from the western Black Sea. Journal of Micropalaeontology, Geological Society, 2010, 29 (2), pp.119- 133. 10.1144/0262-821X10-003. hal-03199895 HAL Id: hal-03199895 https://hal.archives-ouvertes.fr/hal-03199895 Submitted on 1 Jul 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. Journal of Micropalaeontology, 29: 119–133. 0262-821X/10 $15.00 2010 The Micropalaeontological Society Late Pleistocene to Recent ostracod assemblages from the western Black Sea IAN BOOMER1,*, FRANCOIS GUICHARD2 & GILLES LERICOLAIS3 1School of Geography, Earth & Environmental Sciences, University of Birmingham Birmingham B15 2TT, UK 2Laboratoire des Sciences du Climat et de l’Environnement (LSCE, CEA-CNRS-UVSQ) Avenue de la Terrasse, 91198 Gif sur Yvette, France 3IFREMER, Centre de Brest, Géosciences Marines, Laboratoire Environnements Sédimentaires BP70, F-29280 Plouzané cedex, France *Corresponding author (e-mail: [email protected]) ABSTRACT – During the last glacial phase the Black Sea basin was isolated from the world’s oceans due to the lowering of global sea-levels. -
The Taxonomy and Biogeography of Macrofaunal Ostracod Crustaceans
The taxonomy and biogeography of macrofaunal ostracod crustaceans, with focus on the abyssal benthic Pacific fauna relevant to the CCFZ Ivana Karanovic Hanyang University, Department of Life Science, College of Natural Sciences, Seoul 133-791, Korea University of Tasmania, IMAS, Hobart, TAS, 7001, Australia e-mail: [email protected] Few words about myself Italy(Salerno, 2 years) Serbia (Novi Sad, born) Australia (Perth & Hobart, 10 years) Germany (Hamburg, 2 years) South Korea (Seoul, 3.5 years) • Started working on ostracods 15 years ago • Worked on faunas from all continents (including Antarctica) • and from all environments: from freshwater puddles to deep sea • I don’t particularly like ostracods • I like the fact that ostracods give insight into many aspects of biology General information on ostracods • Named in 1802 by Latreille • Name comes from the Greek óstrakon, meaning shell or tile • Common name in English: “mussel shrimp” or “seed shrimp” • In German it is “Muschelkrebse” • Live in all aquatic habitats on the planet Fossil record Systematics • Previously in the class Maxillopoda • Currently recognized as one of the 7 classes of the phylum Crustacea Currently divided into two subclasses 1. Myodocopa 2. Podocopa Systematics cont. 4a. 1. Subclass Myodocopa 1. Order Myodocopina 2. Order Halocyprida 4b. a) Suborder Halocypridina b) Suborder Cladocopina 2a. Subclass Podocopa 3. Order Platycopida 4. Order Podocopida 4c. a) Suborder Bairdiocopina b) Suborder Cytherocopina 2b. c) Suborder Darwinulocopina d) Suborder Cypridocopina 4d. e) Suborder Sigilliocopina 3. Photo credits: 4e. 1, 2: S.N. Brandao 3: Brandao & Yasuhara 4b, c: D. Keyser 4e: From Maddocks (1972) Morphology a. -
Soft Body Morphology, Dissection and Slide-Preparation of Ostracoda: a Primer
Joannea Geol. Paläont. 11: 327-343 (2011) Soft body morphology, dissection and slide-preparation of Ostracoda: a primer Tadeusz NAMIOTKO, Dan L. DANIELOPOL & Angel BALTANÁS Abstract: Most commonly used techniques for treating ostracod soft body for taxonomi- cal purposes with optical microscopy are described with emphasis on the order Podo- copida. A variety of procedures for pre-treatment, storage, recovery of dried specimens, dissection, temporary and permanent mounting, and staining methods are presented and evaluated. General morphology and terminology of the ostracod appendages are also summarised. Key Words: Ostracoda; Dissection; Mounting; Staining; Appendages; Morphology. 1. Introduction One of best diagnostic and most conspicuous trait of Ostracoda is a bivalved carapace that may completely envelop the whole animal body with limbs. Ostracodologists usu- ally refer to calcified valves as “hard parts”, whereas to the appendages and other in- ternal organs as „soft parts”. The classification of Recent ostracods is based mainly on differences in the soft part morphology which is ordinarily of little use by palaeontolo- gists. However, considering the close functional relationship often existing between the soft and hard parts, each expressing to a considerable extent the morphology of the other, even basic knowledge on the appendages without doubt should help palaeonto- logists to better understand and interpret various features displayed in the valves of the fossil ostracods. Examining living material collected from modern habitats enables pa- laeontologists also to become familiar with intraspecific variability or ecology, which could greatly facilitate both taxonomical and palaeoenvironmental studies. Therefore the morphology and terminology of the soft parts of ostracods is outlined (focusing on limbs) in this primer prior to the description of various laboratory techniques involved in the appendage preparation for optical microscopy. -
On Homology of Arthropod Compound Eyes' "The Eye" Has Long Served As
INTEGR. CotoP. BIOL., 43:522-530 (2003) On Homology of Arthropod Compound Eyes' TODD H. OAKLEY 2 Ecology Evolutioni and Marine Biology, University of California-SantaBarbara, S'anzta Barbara, Califonzia 93106 SyNopsis. Eyes serve as models to understand the evolution of complex traits, with broad implications for the origins of evolutionary novelty. Discussions of eye evolution are relevant at miany taxonomic levels, especially within arthropods where compound eye distribution is perplexing. Either compound eyes were lost numerous times or very similar eyes evolved separately in multiple lineages. Arthropod compound eye homology is possible, especially; between crustaceans and hexapods, which have very similar eye facets and may be sister taxa. However, judging homology only on similarity requires subjective decisions. Regardless of whether compound eyes were present in a common ancestor of arthropods or crustaceans + hexapods, recent phylogenetic evidence suggests that the compound eyes, today present in myodocopid ostracods (Crus- tacea), may have been absent in ostracod ancestors. This pattern is inconsistent with phylogenetic homology. Multiple losses of ostracod eyes are an alternative hypothesis that is statistically improbable and without clear cause. One possible evolutionary process to explain the lack of phylogenetic'homology of ostracod compound eyes is that eyes may evolve by switchback evolution, where genes for lost structures remain dormant and are re-expressed much later in evolution. INTRODUCTION 'the recent evidence for and implications of a poten- "The eye" has long served as a canonical example tially non-homologous arthropod compound eye, un- of a complex trait. In an early design-based argument derstanding the case for compound eye homology is for the existence of God, Paley (1846) used the eye as important. -
E:\Krzymińska Po Recenzji\Sppap29.Vp
JARMILA KRZYMIÑSKA, TADEUSZ NAMIOTKO Quaternary Ostracoda of the southern Baltic Sea (Poland) – taxonomy, palaeoecology and stratigraphy Polish Geological Institute Special Papers,29 WARSZAWA 2013 CONTENTS Introduction .....................................................6 Area covered and geological setting .........................................6 History of research on Ostracoda from Quaternary deposits of the Polish part of the Baltic Sea ..........8 Material and methods ...............................................10 Results and discussion ...............................................12 General overwiew on the distribution and diversity of Ostracoda in Late Glacial to Holocene sediments of the studied cores..........................12 An outline of structure of the ostracod carapace and valves .........................20 Pictorial key to Late Glacial and Holocene Ostracoda of the Polish part of the Baltic Sea and its coastal area ..............................................22 Systematic record and description of species .................................26 Hierarchical taxonomic position of genera of Quaternary Ostracoda of the southern Baltic Sea ......26 Description of species ...........................................27 Stratigraphy, distribution and palaeoecology of Ostracoda from the Quaternary of the southern Baltic Sea ...........................................35 Late Glacial and early Holocene fauna ...................................36 Middle and late Holocene fauna ......................................37 Concluding -
Ningaloo Coast World Heritage Nomination: (2008)
Ningaloo Coast Ningaloo Coast © Commonwealth of Australia, January 2010 This work is copyright. Apart from any use as permitted under theCopyright Act 1968, no part may be reproduced by any process without prior written permission from the Commonwealth, available from the Australian Government Department of the Environment, Water, Heritage and the Arts. Published by: Department of the Environment, Water, Heritage and the Arts GPO Box 787 Canberra ACT 2061 National Library of Australia Cataloguing-in-Publication data: Commonwealth of Australia Ningaloo Coast: World Heritage nomination I Australia. Dept. of the Environment, Water, Heritage and the Arts. ISBN 978-1-921733-03-1 Designed by 2B Advertising and Design All images © Department of the Environment, Water, Heritage and the Arts (and associated photographers) unless noted. Front cover image: Photograph Tony Howard © Western Australian Department of the Environment and Conservation Ningaloo Coast ❱ F R O M R eef T O R ange Table of ConTenTs ExEcutivE Summary IV KEy tErmS VII PART 1 IDENTIfICaTION OF THe PRoPeRTY 1 1.A COuntry 2 1.B State, province or region 2 1.C Name of property 2 1.D Geographical coordinates 2 1.E Maps and plans, showing the boundaries of the property 3 1.F Area of nominated property 12 PART 2 DESCRIPTION 13 2.A Description of property 14 2.B History and development 44 PART 3 JUsTIfICaTION FOR INSCRIPTION 53 3.A Criteria under which inscription is proposed (and Justification for inscription under these criteria) 54 Criterion (vii) 56 Criterion (viii) 64 Criterion -
Ostracod Assemblages in the Frasassi Caves and Adjacent Sulfidic Spring and Sentino River in the Northeastern Apennines of Italy
D.E. Peterson, K.L. Finger, S. Iepure, S. Mariani, A. Montanari, and T. Namiotko – Ostracod assemblages in the Frasassi Caves and adjacent sulfidic spring and Sentino River in the northeastern Apennines of Italy. Journal of Cave and Karst Studies, v. 75, no. 1, p. 11– 27. DOI: 10.4311/2011PA0230 OSTRACOD ASSEMBLAGES IN THE FRASASSI CAVES AND ADJACENT SULFIDIC SPRING AND SENTINO RIVER IN THE NORTHEASTERN APENNINES OF ITALY DAWN E. PETERSON1,KENNETH L. FINGER1*,SANDA IEPURE2,SANDRO MARIANI3, ALESSANDRO MONTANARI4, AND TADEUSZ NAMIOTKO5 Abstract: Rich, diverse assemblages comprising a total (live + dead) of twenty-one ostracod species belonging to fifteen genera were recovered from phreatic waters of the hypogenic Frasassi Cave system and the adjacent Frasassi sulfidic spring and Sentino River in the Marche region of the northeastern Apennines of Italy. Specimens were recovered from ten sites, eight of which were in the phreatic waters of the cave system and sampled at different times of the year over a period of five years. Approximately 6900 specimens were recovered, the vast majority of which were disarticulated valves; live ostracods were also collected. The most abundant species in the sulfidic spring and Sentino River were Prionocypris zenkeri, Herpetocypris chevreuxi,andCypridopsis vidua, while the phreatic waters of the cave system were dominated by two putatively new stygobitic species of Mixtacandona and Pseudolimnocythere and a species that was also abundant in the sulfidic spring, Fabaeformiscandona ex gr. F. fabaeformis. Pseudocandona ex gr. P. eremita, likely another new stygobitic species, is recorded for the first time in Italy. The relatively high diversity of the ostracod assemblages at Frasassi could be attributed to the heterogeneity of groundwater and associated habitats or to niche partitioning promoted by the creation of a chemoautotrophic ecosystem based on sulfur-oxidizing bacteria.