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Recent Benthic Foraminifera from the Itaipu Lagoon, Rio De Janeiro (Southeastern Brazil)
12 5 1959 the journal of biodiversity data 15 September 2016 Check List LISTS OF SPECIES Check List 12(5): 1959, 15 September 2016 doi: http://dx.doi.org/10.15560/12.5.1959 ISSN 1809-127X © 2016 Check List and Authors Recent benthic foraminifera from the Itaipu Lagoon, Rio de Janeiro (southeastern Brazil) Débora Raposo1*, Vanessa Laut2, Iara Clemente3, Virginia Martins3, Fabrizio Frontalini4, Frederico Silva5, Maria Lúcia Lorini6, Rafael Fortes6 and Lazaro Laut1 1 Laboratório de Micropaleontologia (LabMicro), Universidade Federal do Estado do Rio de Janeiro – UNIRIO. Avenida Pasteur 458, Urca, Rio de Janeiro, CEP 22290-240, RJ, Brazil 2 Universidade Federal Fluminense (UFF), Instituto de Biologia Marinha, Outeiro São João Batista, s/nº, Niterói, Rio de Janeiro, CEP 24001-970, RJ, Brazil 3 Universidade do Estado do Rio de Janeiro (UERJ). Rua São Francisco Xavier, 524, Maracanã, Rio de Janeiro, CEP 20550-900, RJ, Brazil 4 DiSTeVA, Università degli Studi di Urbino “Carlo Bo”, Campus Scientifico Enrico Mattei. Località Crocicchia, 61029 Urbino, Italy 5 Laboratório de Palinofácies e Fácies Orgânicas (LAFO), Universidade Federal do Rio de Janeiro (UFRJ). Avenida Pedro Calmon, 550, Cidade Universitária, Rio de Janeiro, CEP 21941-901, RJ, Brazil 6 Laboratório de Ecologia Bêntica, Universidade Federal do Estado do Rio de Janeiro – UNIRIO. Avenida Pasteur 458, Urca, Rio de Janeiro, CEP 22290-240, RJ, Brazil * Corresponding author. E-mail: [email protected] Abstract: Itaipu Lagoon is located near the mouth of There are many advantages of applying foraminifera Guanabara Bay and has great importance for recreation to environmental monitoring when compared with to the city of Niterói, Rio de Janeiro state, Brazil. -
New Insights Into the Behavioural Ecology of Intertidal Foraminifera
Journal of Foraminiferal Research, v. 45, no. 4, p. 390–401, October 2015 THE DEVIL LIES IN DETAILS: NEW INSIGHTS INTO THE BEHAVIOURAL ECOLOGY OF INTERTIDAL FORAMINIFERA LAURENT SEURONT1,3 AND VINCENT M. P. BOUCHET2 ABSTRACT To validate in-situ observations, living foraminifera have The motion behaviour of three species of intertidal been used in the laboratory for nearly a century (e.g., Myers, foraminifera, Ammonia tepida, Cribroelphidium excavatum 1935; Le Calvez, 1938; Jepps, 1942; Arnold, 1953). In contrast, and Haynesina germanica, was investigated continuously in the the understanding of the behavioural ecology of foraminifera laboratory. We first infer the presence of geotactic and is still in its infancy, despite a fair amount of work related to phototactic responses. Significant geotactic responses were their vertical and horizontal rates of movement (Arnold, 1953, observed for all three species; A. tepida was found to be 1974; Zmiri et al., 1974; Severin & Erskian, 1981; Severin negatively geotactic while C. excavatum and H. germanica et al., 1982; Severin, 1987; Kitazato, 1988; Wetmore, 1988; showed positive geotaxis. In contrast, no response to light was Weinberg, 1991; Anderson et al., 1991; Bornmalm et al., 1997; ever observed. The detailed nature of motility, investigated in Manley & Shaw, 1997; Bernhard, 2000; Gross, 2000; Khare & terms of both geometric and stochastic complexity of their Nigam, 2000). motion behaviour, was consistently characterised by a strong Negative geotaxis is by far the most widely reported inter-specific, inter-individual and intra-individual variability. behavioural property among foraminifera (Murray, 1963, Specifically, A. tepida and H. germanica were characterised by 1979, 1991; Richter, 1964; Lee et al., 1969; Moodley, 1990), an intensive search behaviour (they explore their environment which has been routinely used to separate them from the slowly with straighter trajectories), while C. -
The Metabolic Response of Ubiquitous Benthic Foraminifera (Ammonia Tepida)
RESEARCH ARTICLE Surviving anoxia in marine sediments: The metabolic response of ubiquitous benthic foraminifera (Ammonia tepida) Charlotte LeKieffre1*, Jorge E. Spangenberg2, Guillaume Mabilleau3, SteÂphane Escrig1, Anders Meibom1,4*, Emmanuelle Geslin5* 1 Laboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique FeÂdeÂrale de Lausanne (EPFL), Lausanne, Switzerland, 2 Stable Isotope and Organic Geochemistry Laboratories, Institute of Earth Surface Dynamics (IDYST), University of Lausanne, a1111111111 Lausanne, Switzerland, 3 Service commun d'imageries et d'analyses microscopiques (SCIAM), Institut de a1111111111 Biologie en SanteÂ, University of Angers, Angers, France, 4 Center for Advanced Surface Analysis, Institute of a1111111111 Earth Sciences, University of Lausanne, Lausanne, Switzerland, 5 UMR CNRS 6112 - LPG-BIAF, University a1111111111 of Angers, Angers, France a1111111111 * [email protected] (CL); [email protected] (AM); [email protected] (EG) Abstract OPEN ACCESS High input of organic carbon and/or slowly renewing bottom waters frequently create periods Citation: LeKieffre C, Spangenberg JE, Mabilleau G, Escrig S, Meibom A, Geslin E (2017) Surviving with low dissolved oxygen concentrations on continental shelves and in coastal areas; such anoxia in marine sediments: The metabolic events can have strong impacts on benthic ecosystems. Among the meiofauna living in these response of ubiquitous benthic foraminifera environments, benthic foraminifera are often the most tolerant to low oxygen levels. Indeed, (Ammonia tepida). PLoS ONE 12(5): e0177604. https://doi.org/10.1371/journal.pone.0177604 some species are able to survive complete anoxia for weeks to months. One known mecha- nism for this, observed in several species, is denitrification. For other species, a state of Editor: Bo Thamdrup, University of Southern Denmark, DENMARK highly reduced metabolism, essentially a state of dormancy, has been proposed but never demonstrated. -
Next-Generation Environmental Diversity Surveys of Foraminifera: Preparing the Future Jan Pawlowski, Franck Lejzerowicz, Philippe Esling
Next-Generation Environmental Diversity Surveys of Foraminifera: Preparing the Future Jan Pawlowski, Franck Lejzerowicz, Philippe Esling To cite this version: Jan Pawlowski, Franck Lejzerowicz, Philippe Esling. Next-Generation Environmental Diversity Sur- veys of Foraminifera: Preparing the Future . Biological Bulletin, Marine Biological Laboratory, 2014, 227 (2), pp.93-106. 10.1086/BBLv227n2p93. hal-01577891 HAL Id: hal-01577891 https://hal.archives-ouvertes.fr/hal-01577891 Submitted on 28 Aug 2017 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. See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/268789818 Next-Generation Environmental Diversity Surveys of Foraminifera: Preparing the Future Article in Biological Bulletin · October 2014 Source: PubMed CITATIONS READS 26 41 3 authors: Jan Pawlowski Franck Lejzerowicz University of Geneva University of Geneva 422 PUBLICATIONS 11,852 CITATIONS 42 PUBLICATIONS 451 CITATIONS SEE PROFILE SEE PROFILE Philippe Esling Institut de Recherche et Coordination Acoust… 24 PUBLICATIONS 551 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: UniEuk View project KuramBio II (Kuril Kamchatka Biodiversity Studies II) View project All content following this page was uploaded by Jan Pawlowski on 30 December 2015. -
Systematic Paleontology, Distribution and Abundance of Cenozoic Benthic Foraminifera from Kish Island, Persian Gulf, Iran
Journal of the Persian Gulf (Marine Science)/Vol. 8/No. 28/ June 2017/22/19-40 Systematic Paleontology, Distribution and Abundance of Cenozoic Benthic Foraminifera from Kish Island, Persian Gulf, Iran Fahimeh Hosseinpour1, Ali Asghar Aryaei1*, Morteza Taherpour-Khalil-Abad2 1- Department of Geology, Mashhad Branch, Islamic Azad University, Mashhad, Iran 2- Young Researchers and Elite Club, Mashhad Branch, Islamic Azad University, Mashhad, Iran Received: January 2017 Accepted: June 2017 © 2017 Journal of the Persian Gulf. All rights reserved. Abstract Foraminifera are one of the most important fossil microorganisms in the Persian Gulf. During micropaleontological investigations in 5 sampling stations around the Kish Island, 14 genera and 15 species of dead Cenozoic benthic foraminifera were determined and described. Next to these assemblages, other organisms, such as microgastropods and spines of echinids were also looked into. In this study, the statistical analysis of foraminiferal distribution was done in one depth-zone (60-150 m and compared with the Australian-Iran Jaya Continental margin depth- zone. Keywords: Foraminifera, Distribution analysis, Kish Island, Persian Gulf, Iran Downloaded from jpg.inio.ac.ir at 9:20 IRST on Monday October 4th 2021 1. Introduction approximately 226000 km2. Its average depth is about 35 m, and it attains its maximum depth about Persian Gulf is the location of phenomenal 100 m near its entrance - the Straits of Hormuz (for hydrocarbon reserves and an area of the world where more details see details in Seibold and Vollbrecht, the oil industry is engaged in intense hydrocarbon 1969; Seibold and Ulrich 1970). It is virtually exploration and extraction. -
A Guide to 1.000 Foraminifera from Southwestern Pacific New Caledonia
Jean-Pierre Debenay A Guide to 1,000 Foraminifera from Southwestern Pacific New Caledonia PUBLICATIONS SCIENTIFIQUES DU MUSÉUM Debenay-1 7/01/13 12:12 Page 1 A Guide to 1,000 Foraminifera from Southwestern Pacific: New Caledonia Debenay-1 7/01/13 12:12 Page 2 Debenay-1 7/01/13 12:12 Page 3 A Guide to 1,000 Foraminifera from Southwestern Pacific: New Caledonia Jean-Pierre Debenay IRD Éditions Institut de recherche pour le développement Marseille Publications Scientifiques du Muséum Muséum national d’Histoire naturelle Paris 2012 Debenay-1 11/01/13 18:14 Page 4 Photos de couverture / Cover photographs p. 1 – © J.-P. Debenay : les foraminifères : une biodiversité aux formes spectaculaires / Foraminifera: a high biodiversity with a spectacular variety of forms p. 4 – © IRD/P. Laboute : îlôt Gi en Nouvelle-Calédonie / Island Gi in New Caledonia Sauf mention particulière, les photos de cet ouvrage sont de l'auteur / Except particular mention, the photos of this book are of the author Préparation éditoriale / Copy-editing Yolande Cavallazzi Maquette intérieure et mise en page / Design and page layout Aline Lugand – Gris Souris Maquette de couverture / Cover design Michelle Saint-Léger Coordination, fabrication / Production coordination Catherine Plasse La loi du 1er juillet 1992 (code de la propriété intellectuelle, première partie) n'autorisant, aux termes des alinéas 2 et 3 de l'article L. 122-5, d'une part, que les « copies ou reproductions strictement réservées à l'usage privé du copiste et non destinées à une utilisation collective » et, d'autre part, que les analyses et les courtes citations dans un but d'exemple et d'illustration, « toute représentation ou reproduction intégrale ou partielle, faite sans le consentement de l'auteur ou de ses ayants droit ou ayants cause, est illicite » (alinéa 1er de l'article L. -
The Revised Classification of Eukaryotes
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/231610049 The Revised Classification of Eukaryotes Article in Journal of Eukaryotic Microbiology · September 2012 DOI: 10.1111/j.1550-7408.2012.00644.x · Source: PubMed CITATIONS READS 961 2,825 25 authors, including: Sina M Adl Alastair Simpson University of Saskatchewan Dalhousie University 118 PUBLICATIONS 8,522 CITATIONS 264 PUBLICATIONS 10,739 CITATIONS SEE PROFILE SEE PROFILE Christopher E Lane David Bass University of Rhode Island Natural History Museum, London 82 PUBLICATIONS 6,233 CITATIONS 464 PUBLICATIONS 7,765 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Biodiversity and ecology of soil taste amoeba View project Predator control of diversity View project All content following this page was uploaded by Smirnov Alexey on 25 October 2017. The user has requested enhancement of the downloaded file. The Journal of Published by the International Society of Eukaryotic Microbiology Protistologists J. Eukaryot. Microbiol., 59(5), 2012 pp. 429–493 © 2012 The Author(s) Journal of Eukaryotic Microbiology © 2012 International Society of Protistologists DOI: 10.1111/j.1550-7408.2012.00644.x The Revised Classification of Eukaryotes SINA M. ADL,a,b ALASTAIR G. B. SIMPSON,b CHRISTOPHER E. LANE,c JULIUS LUKESˇ,d DAVID BASS,e SAMUEL S. BOWSER,f MATTHEW W. BROWN,g FABIEN BURKI,h MICAH DUNTHORN,i VLADIMIR HAMPL,j AARON HEISS,b MONA HOPPENRATH,k ENRIQUE LARA,l LINE LE GALL,m DENIS H. LYNN,n,1 HILARY MCMANUS,o EDWARD A. D. -
23.3 Groups of Protists
Chapter 23 | Protists 639 cysts that are a protective, resting stage. Depending on habitat of the species, the cysts may be particularly resistant to temperature extremes, desiccation, or low pH. This strategy allows certain protists to “wait out” stressors until their environment becomes more favorable for survival or until they are carried (such as by wind, water, or transport on a larger organism) to a different environment, because cysts exhibit virtually no cellular metabolism. Protist life cycles range from simple to extremely elaborate. Certain parasitic protists have complicated life cycles and must infect different host species at different developmental stages to complete their life cycle. Some protists are unicellular in the haploid form and multicellular in the diploid form, a strategy employed by animals. Other protists have multicellular stages in both haploid and diploid forms, a strategy called alternation of generations, analogous to that used by plants. Habitats Nearly all protists exist in some type of aquatic environment, including freshwater and marine environments, damp soil, and even snow. Several protist species are parasites that infect animals or plants. A few protist species live on dead organisms or their wastes, and contribute to their decay. 23.3 | Groups of Protists By the end of this section, you will be able to do the following: • Describe representative protist organisms from each of the six presently recognized supergroups of eukaryotes • Identify the evolutionary relationships of plants, animals, and fungi within the six presently recognized supergroups of eukaryotes • Identify defining features of protists in each of the six supergroups of eukaryotes. In the span of several decades, the Kingdom Protista has been disassembled because sequence analyses have revealed new genetic (and therefore evolutionary) relationships among these eukaryotes. -
Anaerobic Metabolism of Foraminifera Thriving Below the Seafloor 2 3 Authors: William D
bioRxiv preprint doi: https://doi.org/10.1101/2020.03.26.009324; this version posted March 27, 2020. 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 Anaerobic metabolism of Foraminifera thriving below the seafloor 2 3 Authors: William D. Orsi1,2*, Raphaël Morard4, Aurele Vuillemin1, Michael Eitel1, Gert Wörheide1,2,3, 4 Jana Milucka5, Michal Kucera4 5 Affiliations: 6 1. Department of Earth and Environmental Sciences, Paleontology & Geobiology, Ludwig-Maximilians- 7 Universität München, 80333 Munich, Germany. 8 2. GeoBio-CenterLMU, Ludwig-Maximilians-Universität München, 80333 Munich, Germany 9 3. SNSB - Bayerische Staatssammlung für Paläontologie und Geologie, 80333 Munich, Germany 10 4. MARUM – Center for Marine Environmental Sciences, University of Bremen, Germany 11 5. Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Bremen, Germany 12 13 *To whom correspondence should be addressed: [email protected] 14 15 Abstract: Foraminifera are single-celled eukaryotes (protists) of large ecological importance, as well as 16 environmental and paleoenvironmental indicators and biostratigraphic tools. In addition, they are capable 17 of surviving in anoxic marine environments where they represent a major component of the benthic 18 community. However, the cellular adaptations of Foraminifera to the anoxic environment remain poorly 19 constrained. We sampled an oxic-anoxic transition zone in marine sediments from the Namibian shelf, 20 where the genera Bolivina and Stainforthia dominated the Foraminifera community, and use 21 metatranscriptomics to characterize Foraminifera metabolism across the different geochemical 22 conditions. -
Espèces Non Indigènes » En France Métropolitaine
Directive Cadre Stratégie pour le Milieu Marin (DCSMM) Évaluation du descripteur 2 « espèces non indigènes » en France métropolitaine Rapport scientifique pour l’évaluation 2018 au titre de la DCSMM Cécile MASSÉ et Laurent GUÉRIN Pilote scientifique et coordinatrice pour la surveillance de la thématique DCSMM « espèces non indigènes » Museum National d’Histoire Naturelle UMS 2006 PATRIMOINE NATUREL Stations Marines de Dinard et Arcachon 2018 Préambule Ce rapport correspond au livrable « Evaluation DCSMM 2018 : rapport des pilotes scientifiques » des conventions de financement DEB pour l’action pluriannuelle 2014-2017. Ces travaux ont pu être réalisés dans le cadre d’un financement de cette action (DCSMM), via la dotation annuelle du Ministère de l’environnement (MTES) au Muséum Nationale d’Histoire Naturelle (MNHN) Ce rapport met à jour et complète les rapports des travaux antérieurs sur l’évaluation initiale 2012 (Noel P., 2012a, b, c, d et Quemmerais-Amice F., 2012a, b, c, d), en tenant compte de ceux sur la définition et la mise à jour du Bon Etat Ecologique (BEE) (Guérin et al., 2012 ; Massé et Guérin, 2017) et de celui sur la définition des programmes de surveillance et plan d’acquisition de connaissance (Guérin et Lejart, 2013). Le présent rapport ne reprend donc pas tous les éléments déjà publiés dans ces rapports précédents, auxquels il conviendra de se référer pour appréhender pleinement le contexte des travaux menés. Un glossaire et les références des termes utilisés dans le contexte de ce rapport sont fournis au début de ce -
Chamber Arrangement Versus Wall Structure in the High-Rank Phylogenetic Classification of Foraminifera
Editors' choice Chamber arrangement versus wall structure in the high-rank phylogenetic classification of Foraminifera ZOFIA DUBICKA Dubicka, Z. 2019. Chamber arrangement versus wall structure in the high-rank phylogenetic classification of Fora- minifera. Acta Palaeontologica Polonica 64 (1): 1–18. Foraminiferal wall micro/ultra-structures of Recent and well-preserved Jurassic (Bathonian) foraminifers of distinct for- aminiferal high-rank taxonomic groups, Globothalamea (Rotaliida, Robertinida, and Textulariida), Miliolida, Spirillinata and Lagenata, are presented. Both calcite-cemented agglutinated and entirely calcareous foraminiferal walls have been investigated. Original test ultra-structures of Jurassic foraminifers are given for the first time. “Monocrystalline” wall-type which characterizes the class Spirillinata is documented in high resolution imaging. Globothalamea, Lagenata, porcel- aneous representatives of Tubothalamea and Spirillinata display four different major types of wall-structure which may be related to distinct calcification processes. It confirms that these distinct molecular groups evolved separately, probably from single-chambered monothalamids, and independently developed unique wall types. Studied Jurassic simple bilocular taxa, characterized by undivided spiralling or irregular tubes, are composed of miliolid-type needle-shaped crystallites. In turn, spirillinid “monocrystalline” test structure has only been recorded within more complex, multilocular taxa pos- sessing secondary subdivided chambers: Jurassic -
Three Shell Types in Mardinella Daviesi Indicate the Evolution of a Paratrimorphic Life Cycle Among Late Paleocene Soritid Benthic Foraminifera
Three shell types in Mardinella daviesi indicate the evolution of a paratrimorphic life cycle among late Paleocene soritid benthic foraminifera LORENZO CONSORTI, FELIX SCHLAGINTWEIT, and KOOROSH RASHIDI Consorti, L., Schlagintweit, F., and Rashidi, K. 2020. Three shell types in Mardinella daviesi indicate the evolution of a paratrimorphic life cycle among late Paleocene soritid benthic foraminifera. Acta Palaeontologica Polonica 65 (X): xxx–xxx. Soritids are a successful group of larger Foraminifera with several extant representatives that display a complex alterna- tion of generations, the so-called paratrimorphic life cycle. Fossil soritids are abundantly widespread through the geolog- ical record starting from the Albian. The oldest Soritidae possessing annular chambers and cross-wise oblique chamber communications is represented by the Paleocene species Mardinella daviesi. The present paper provides a description of the morphology and anatomy of the three reproductive generations recovered in a Mardinella-rich assemblage from a lower Paleogene shallow-water carbonate succession in SW Iran (Zagros Zone). Comparison among proportion of schizonts vs. gamonts with extant soritids shows that there is an easy match. This would confirm that the paratrimorphic life cycle was successfully adopted by the early soritids to maintain fitness with the environment and to keep a stable mutual relationship with a certain group of endosymbionts. Key words: Foraminifera, Soritidae, reproduction cycle, endosymbionts, Paleogene, Iran. Lorenzo Consorti [[email protected]; [email protected]], Department of Mathematics and Geosciences, University of Trieste. Via Weiss 2, Trieste, Italy. Felix Schlagintweit [[email protected]], Lerchenauerstr. 167, 80935 München, Germany. Koorosh Rashidi [[email protected]], Department of Geology, Yazd University, 89195-741 Yazd, Iran.