Genetic Diversity, Biogeography and the Morpho-Genetic Relationship in Extant Planktonic Foraminifera

Total Page:16

File Type:pdf, Size:1020Kb

Genetic Diversity, Biogeography and the Morpho-Genetic Relationship in Extant Planktonic Foraminifera Genetic diversity, biogeography and the morpho-genetic relationship in extant planktonic foraminifera Dissertation zur Erlangung des Doktorgrades in den Naturwissenschaften (Dr. rer. nat.) im Fachbereich Geowissenschaften der Universität Bremen vorgelegt von Agnes Katharina Maria Weiner Bremen, Mai 2014 1. Gutachter: Prof. Dr. Michal Kucera, MARUM – Zentrum für marine Umweltwissenschaften, Universität Bremen, Deutschland 2. Gutachter: Prof. Dr. Kate Darling, School of GeoSciences, University of Edinburgh and School of Geography and GeoSciences, University of St Andrews, Großbritannien Datum der Abgabe: 05.05.2014 Datum der Verteidigung: 11.07.2014 (Photos on title page: WG Kucera) PREFACE Preface The present PhD thesis was prepared at the Department of Geosciences at the University of Tübingen and the MARUM – Center for Marine Environmental Sciences at the University of Bremen, Germany. The work was financed by the “Landesgraduiertenförderung Baden- Württemberg” and by grant KU 2259/19 from the Deutsche Forschungsgemeinschaft (DFG) as part of the OPOCA project. Planktonic foraminifera samples for genetic analysis were collected and processed during five research expeditions to the Mediterranean Sea, Atlantic, South China Sea and the Southern Pacific on the research vessels R/V MARIA S. MERIAN (cruise MSM15/5), R/V POSEIDON (cruises P411 and P413) and R/V SONNE (cruises SO221 and SO226/3). In addi- tion, four research stays were carried out at the marine laboratories at Villefranche sur Mer, France, the Interuniversity Institute in Eilat, Israel, the Estación Costera de Investigaciones Marinas in Las Cruces, Chile and the Isla Magueyes Laboratories in La Parguera, Puerto Rico. The visits to the marine stations in Chile and Israel were financed by the EU FP7 research infrastructure initiative ASSEMBLE and the field trip to Puerto Rico was part of the OPOCA DFG project. The obtained planktonic foraminifera dataset was enlarged with samples from the collections of the working group and from various coauthors, as indicated for each study separately. The eight chapters of this thesis comprise four research papers dealing with the genetic diversity, biogeography and a potential correlation of morphology and genetics in living planktonic foraminifera. Chapter 1 introduces the model organisms from a biological as well as paleontological perspective. It describes the marker gene that is used in the genetic analysis of planktonic foraminifera and elaborates the problem of cryptic diversity within the traditional morphospecies. The following section presents different modes of speci- ation and biogeographical distribution patterns that can be found in plankton organisms. Chapter 2 outlines the motivation and major research questions of this thesis and Chapter 3 describes the methods applied in the molecular analysis of planktonic foraminifera. Chapters 4–7 include the actual case studies that were carried out in the framework of this thesis, in the form of published or submitted research papers and Chapter 8 presents a general conclusion on the results of the studies and an outlook for future work. 3 EXTANT PLANKTONIC FORAMINIFERA 4 CONTENTS Table of Contents Abstract 07 Zusammenfassung 19 Chapter 1: Introduction 11 1.1. The biology of extant planktonic foraminifera 11 1.2. The fossil record of planktonic foraminifera 15 1.3. Genetic diversity of planktonic foraminifera 18 1.4. Speciation and biogeographic distribution patterns in plankton 24 Chapter 2: Motivation and Objectives 29 Chapter 3: Methods applied in single-cell foraminifera genetics 31 3.1. Sampling of planktonic foraminifera 31 3.2. Culturing of planktonic foraminifera 32 3.3. DNA extraction and molecular analysis 33 Chapter 4: First case study: Vertical niche partitioning between cryptic sibling species of a cosmopolitan marine planktonic protist. Molecular Ecology 35 Chapter 5: Second case study: The cryptic and the apparent reversed: lack of genetic differentiation within the morphologically diverse plexus of the planktonic foraminifer Globigerinoides sacculifer. Paleobiology 49 Chapter 6: Third case study: Phylogeography of the tropical planktonic foraminifera lineage Globigerinella reveals isolation inconsistent with passive dispersal by ocean currents. PLoS ONE 71 Chapter 7: Fourth case study: Genetic and morphometric evidence for parallel evolution of the Globigerinella calida morphotypes. Marine Micropaleontology 85 Chapter 8: Concluding remarks and Perspectives 119 8.1. Implications of the results 119 8.2. Remaining limitations 125 8.3. Future perspectives 126 References 129 Acknowledgements 141 Erklärung 143 5 EXTANT PLANKTONIC FORAMINIFERA 6 ABSTRACT Abstract The fossil record of planktonic foraminifera grants this group an exceptional position among marine microplankton. Foraminifera have a long tradition as proxies for the reconstruction of past ocean and climate conditions and therefore, the fossilized shells are very well studied, including evolutionary processes and phylogenetic relationships since their origin in the Jurassic. For their classification, the morphological species concept has been applied, which distinguishes about 50 different species among the modern representatives, based on the ultrastructure of their calcite shells. With the application of molecular genetic approaches on living planktonic foraminifera, the classical species concept has been challenged by the discovery of a large number of cryptic species “hidden” within the morphospecies. The total amount of cryptic diversity and its distribution between the different morphospecies, however, are still not completely resolved. In contrast to the mainly cosmopolitan occur- rences of the morphospecies, many of the cryptic species exhibit differentiated distribution patterns in the ocean, marked by local adaptations to environmental factors. A morphological separation of the sibling species, however, proved very difficult and was so far only possible after detailed morphometric studies. The present thesis aims at contributing to the ongoing research on living planktonic foraminifera, by studying the genetic diversity within three selected morphospecies, the biogeographical distribution patterns of their cryptic species and the relationship between genetic and morphological variability. The study on Hastigerina pelagica examined its genetic diversity and biogeographical dis- tribution in the Mediterranean Sea, Atlantic, Caribbean Sea and the Western Pacific. Only three already known cryptic species were discovered and they were shown to exhibit a global distribution in the ocean, but vertical segregation in the water column. For the analysis of Globigerinoides sacculifer, a high number of samples from around the world was amassed, including all different morphotypes of this highly variable plexus, that were, however, revealed to be genetically completely homogenous. The third species that was chosen for analysis was Globigerinella siphonifera that is marked by a high genetic as well as morphological variability. The examination of a large number of samples allowed the com- plete resolution of its cryptic diversity and a separation of the plexus into three species. Despite an extensive sampling effort, the number of newly detected cryptic species from these studies was unexpectedly low. This indicates that for the well-studied morpho- species most cryptic species might by now be detected and that genetic variability is not even prevalent in all morphospecies. The results presented in this thesis further imply that the amount of genetic diversity cannot be predicted from the characteristics of a morpho- species. The correlation of morphological traits with genetic variability appeared to be possible to some extent in the studied morphospecies, however, generally speaking, mor- phology and genetics of planktonic foraminifera appear to evolve rather independently of each other. The biogeographical distribution patterns of the cryptic species of the studied morphospecies speak for a prevalence of large scale dispersal and gene flow in planktonic foraminifera, while at the same time possibilities are given for the establishment of 7 EXTANT PLANKTONIC FORAMINIFERA reproductive isolation, such as in the vertical dimension in the water column or by local adaptations to different ecological parameters. 8 ZUSAMMENFASSUNG Zusammenfassung Der fossile Befund planktonischer Foraminiferen verleiht dieser Organismengruppe eine außergewöhnliche Position innerhalb des marinen Mikroplanktons. Ihre Nutzung als Proxies für die Rekonstruktion vergangener Ozean- und Klimabedingungen hat eine lange Tradition, was zur Folge hat, dass ihre fossilisierten Schalen sehr gut untersucht und ihre Evolution und phylogenetischen Verhältnisse seit ihres ersten Auftretens im Jura genau bekannt sind. Für die Klassifikation der Arten wurde das morphologische Artkonzept zu Grunde gelegt, das die modernen Vertreter basierend auf der Struktur ihrer kalzitischen Schale in ca. 50 Arten unterteilt. Die Anwendung molekulargenetischer Methoden an planktonischen Foraminiferen stellte das klassische Artkonzept allerdings in Frage, da eine große Zahl kryptischer Arten innerhalb der morphologischen Arten entdeckt wurde. Das komplette Ausmaß dieser kryptischen Diversität sowie seine Verteilung zwischen den morphologischen Arten konnten bisher nicht im Detail geklärt werden. Im Gegensatz zu den morphologischen Arten, die sich größtenteils durch eine globale Verbreitung aus- zeichnen, weisen die kryptischen Arten eher differenzierte Verbreitungsmuster
Recommended publications
  • 20. Infome Variabilidad Climatica 2019
    ASPECTOS BIO-OCEANOGRÁFICOS OBSERVADOS EN DOS ESTACIONES 10 MILLAS COSTA AFUERA, DURANTE EL 2019 INTRODUCCIÓN El Instituto Nacional de Pesca (INP) a través de su programa Variabilidad Climática monitorea de manera mensual las condiciones oceanográficas (físico, químicas y biológicas) de dos estaciones ubicadas 10 millas fuera de la costa ecuatoriana; Puerto López y Salinas (Figura 1). El objetivo principal de este programa es analizar los procesos oceanográficos presentes en los ecosistemas marino-costeros, tomando en cuenta las variaciones espacio-temporales y productividad del océano. De esta manera, se busca relacionar la información obtenida durante las campañas con la distribución, abundancia y biomasa de los recursos pesqueros de interés comercial del país. El mar es un entorno dinámico, influenciado por la geografía del fondo marino y por el clima, de acuerdo a Riley & Chester (1989), los elementos nutritivos, se detectan en el mar en bajas y constantes concentraciones, puesto que las actividades de los organismos vivos produce solo un cambio pequeño o indetectable en su concentración, pero también son los responsables de la eliminación o excreción de cantidades considerables de micronutrientes en relación con la cantidad total presente; para Cushing et al., (1975), las concentraciones registrada de nutrientes, son consecuencia del proceso de producción y no a la inversa, cuya investigación tiene el carácter de una regresión inacabable. Estos constituyentes presentan una marcada variabilidad, la cual restringe la dinámica de exportaciones de nutrientes y carbono orgánico del margen costero ( Helmke et.al., 2005) estableciendo patrones diferentes de distribución que favorecerán la acumulación de nutrientes o la dispersión de los mismos, condiciones influenciadas por los cambios estacionales del viento, situación topográfica, y del sistema de intercambio y/o mezcla con la capa subsuperficial.
    [Show full text]
  • Form and Function of F-Actin During Biomineralization Revealed from Live Experiments on Foraminifera
    Form and function of F-actin during biomineralization revealed from live experiments on foraminifera Jarosław Tyszkaa,1, Ulf Bickmeyerb, Markus Raitzschc,d, Jelle Bijmac, Karina Kaczmarekc, Antje Mewesc, Paweł Topae, and Max Jansef aResearch Centre in Kraków, Institute of Geological Sciences, Polish Academy of Sciences, 31-002 Kraków, Poland; bEcological Chemistry, Alfred-Wegener- Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570 Bremerhaven, Germany; cMarine Biogeosciences, Alfred-Wegener-Institut Helmholtz- Zentrum für Polar- und Meeresforschung, D-27570 Bremerhaven, Germany; dInstitut für Mineralogie, Leibniz Universität Hannover, 30167 Hannover, Germany; eDepartment of Computer Science, AGH University of Science and Technology, 30-052, Kraków, Poland; and fBurgers’ Ocean, Royal Burgers’ Zoo, 6816 SH Arnhem, The Netherlands Edited by Lia Addadi, Weizmann Institute of Science, Rehovot, Israel, and approved January 23, 2019 (received for review June 15, 2018) Although the emergence of complex biomineralized forms has Pioneers who studied living foraminifera described that been investigated for over a century, still little is known on how chamber formation was progressing on what they called “active single cells control morphology of skeletal structures, such as matrix” (15, 16). Hottinger (1) suggested that foraminiferal frustules, shells, spicules, or scales. We have run experiments on chamber morphology depended on the length of rhizopodia the shell formation in foraminifera, unicellular, mainly marine (branching pseudopodia) extruded from the previous chamber organisms that can build shells by successive additions of chambers. and supported by microtubular cytoskeleton. Recent investiga- We used live imaging to discover that all stages of chamber/shell tions on theoretical models of foraminiferal morphogenesis implied formation are controlled by dedicated actin-driven pseudopodial structures.
    [Show full text]
  • 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.
    [Show full text]
  • 1 1 Diversity and Spatial Patterns Of
    1 1 Diversity and spatial patterns of foraminiferal assemblages in the eastern Clarion– 2 Clipperton Zone (abyssal eastern equatorial Pacific) 3 4 5 6 7 Aurélie Goineaua, Andrew J Gooday* 8 9 10 11 National Oceanography Centre, Southampton, University of Southampton Waterfront Campus, 12 European Way, Southampton SO14 3ZH, UK 13 14 15 16 17 18 a Present address: 1, Rue du Champ de Foire, 44530 Guenrouët, France 19 20 *Corresponding author. E-mail address: [email protected] (A.J. Gooday) 21 22 2 24 Abstract 25 Foraminifera are a major component of the abyssal meiofauna in parts of the eastern Pacific 26 Clarion-Clipperton Zone (CCZ) licensed by the International Seabed Authority for polymetallic 27 nodule exploration. We analysed the diversity and distribution of stained (‘live’) and unstained 28 (dead) assemblages (0-1 cm layer, >150-µm sieve fraction) in megacorer samples from 11 sites 29 (water depths 4051 - 4235 m) within three 30 x 30 km ‘strata’ in the United Kingdom 1 (UK1 30 Strata A and B; 5 and 3 samples, respectively) and Ocean Minerals Singapore (3 samples) 31 license areas and separated by distances of up to 28 km within a stratum and 224 km between 32 strata. Foraminiferal assemblage density, diversity and composition at the higher 33 taxon/morphogroup level were largely consistent between samples. Stained assemblages were 34 dominated (>86%) by single-chambered monothalamids, mainly spheres, tubes, komokiaceans 35 and forms that are difficult to categorise morphologically. Hormosinaceans were the most 36 common multichambered group (~10%), while calcareous taxa (mainly rotaliids) represented 37 only ~3.5% of stained tests.
    [Show full text]
  • Ostracoda and Foraminifera from Paleocene (Olinda Well), Paraíba Basin, Brazilian Northeast
    Anais da Academia Brasileira de Ciências (2017) 89(3): 1443-1463 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201720160768 www.scielo.br/aabc | www.fb.com/aabcjournal Ostracoda and foraminifera from Paleocene (Olinda well), Paraíba Basin, Brazilian Northeast ENELISE K. PIOVESAN¹, ROBBYSON M. MELO¹, FERNANDO M. LOPES², GERSON FAUTH³ and DENIZE S. COSTA³ ¹Laboratório de Geologia Sedimentar e Ambiental/LAGESE, Universidade Federal de Pernambuco, Departamento de Geologia, Centro de Tecnologia e Geociências, Av. Acadêmico Hélio Ramos, s/n, 50740-530 Recife, PE, Brazil ²Instituto Tecnológico de Micropaleontologia/itt Fossil, Universidade do Vale do Rio dos Sinos/UNISINOS, Av. Unisinos, 950, 93022-750 São Leopoldo, RS, Brazil ³PETROBRAS/CENPES/PDEP/BPA, Rua Horácio Macedo, 950, Cidade Universitária, Ilha do Fundão, Prédio 32, 21941-915 Rio de Janeiro, RJ, Brazil Manuscript received on November 7, 2016; accepted for publication on March 16, 2017 ABSTRACT Paleocene ostracods and planktonic foraminifera from the Maria Farinha Formation, Paraíba Basin, are herein presented. Eleven ostracod species were identified in the genera Cytherella Jones, Cytherelloidea Alexander, Eocytheropteron Alexander, Semicytherura Wagner, Paracosta Siddiqui, Buntonia Howe, Soudanella Apostolescu, Leguminocythereis Howe and, probably, Pataviella Liebau. The planktonic foraminifera are represented by the genera Guembelitria Cushman, Parvularugoglobigerina Hofker, Woodringina Loeblich and Tappan, Heterohelix Ehrenberg, Zeauvigerina Finlay, Muricohedbergella Huber and Leckie, and Praemurica Olsson, Hemleben, Berggren and Liu. The ostracods and foraminifera analyzed indicate an inner shelf paleoenvironment for the studied section. Blooms of Guembelitria spp., which indicate either shallow environments or upwelling zones, were also recorded reinforcing previous paleoenvironmental interpretations based on other fossil groups for this basin.
    [Show full text]
  • Cenomanian Turonian Coniacian Santonian Campanian
    walteri aff. aff. spp. spp. imperfectus spp. (prisms) Chronostratigraphy Offshore Norway sp. 1 Geologic Time Scale 2012 Zonation (Gradstein et al., 1999, and this study) Allomorphina halli / pyriformis Sigmoilina antiqua Textularia Gavelinella intermeda gracillima Valvulineria Bulbobaculites problematicus Caudammina ovuloides Nuttallinella florealis Stensioeina granulata polonica Inoceramus Rzehakina minima Rzehakina epigona Fenestrella bellii Gaudryina filiformis Trochamminoides Haplophragmoides Gavelinella usakensis Caudammina ovula Coarse agglutinated spp. LCO dubia Tritaxia Plectorecurvoides alternans Reussella szajnochae Recurvoides Hippocrepina depressa Psammosphaera sphaerical radiolarians Ma Age/Stage Lingulogavelinella jarzevae elegans Lt NCF19 Maastrichtian volutus LCO 70 NCF18 E szajnochae dubia Lt 75 LCO of NCF17 Campanian Deep Water M Agglutinated 80 Foraminifera E bellii NCF16 Lt Inoceramus LCO NCF15 85 Santonian M E polonica NCF14 Lt Coniacian M E Marginotruncana NCF13 90 Lt Turonian M E Dicarinella NCF12 95 Lt brittonensis M NCF11 Cenomanian delrioensis LCO NCF10 E antiqua NCF9 100 Figure 2.8c. Stratigraphic ranges of Upper Cretaceous benthic foraminifera, and miscellaneous index taxa, oshore mid-Norway, with the foraminiferal zonation established in this study. s.l. Chronostratigraphy Offshore Norway Geologic Time Scale 2012 Zonation (Gradstein et al., 1999, and this study) Abathomphalus mayaroensis Pseudotextularia elegans Hedbergella planispira Hedbergella hoelzi Praeglobotruncana delrioensis Praeglobotruncana stephani
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Paper Template
    Short Research Article Foraminiferal Assemblage from the Karai Shale, Uttattur Group, Southern India . ABSTRACT (ARIAL, BOLD, 11 FONT, LEFT ALIGNED, CAPS) To the foraminiferal assemblage from the Karai shale, one hundred and nineteen surface sediment samples were collected systematically. The collected samples (incomplete sentence)were standard micropaleontological techniques. Ninety- eight species of well- preserved foraminifera were obtained from the samples. Of the ninety- eight species, eighty- nine were benthic foraminifera and nine were planktic foraminifera. The specific identification of the foraminifera wasere done after comparing them with those described and illustrated by various workers from the Cretaceous of Southern India. The age of the samples wasere assigned as Albian based on the presence of planktic foraminiferal species viz. Hedbergella delrioensis, Hedbergella planispira, Praeglobotruncana delrioensis, Praeglobotruncana stephani, Planomalina buxtorfi, and Thalmanninella balernaensis. Keywords: Cretaceous, Planktic foraminifera, benthic foraminifera, Albian. 1. INTRODUCTION Foraminifera are unicellular organisms found in all sorts of environments, representing one of the most important groups of marine protists. In light of their incredible fossil record and evolutionary history, foraminifera became the key indices in biostratigraphic, paleoceanographic, and paleoclimatic reconstructions. They are globally used for biostratigraphic subdivision and correlation of sedimentary strata. The Cretaceous has long been recognized as a special episode in the history of the Earth and several of the most important ideas in geology derive from the study of Ccretaceous rocks. The Cretaceous system is classified into two subsystems, the lower stretching up to and including the Albian and the upper comprising the rest. In recent years, Middle or mid- Cretaceous has been recognized, describe the Aptian through Turonian stages, 119-88.5 ma based on Hortland et al.
    [Show full text]
  • Form and Function of F-Actin During Biomineralization Revealed from Live Experiments on Foraminifera
    Form and function of F-actin during biomineralization revealed from live experiments on foraminifera Jarosław Tyszkaa,1, Ulf Bickmeyerb, Markus Raitzschc,d, Jelle Bijmac, Karina Kaczmarekc, Antje Mewesc, Paweł Topae, and Max Jansef aResearch Centre in Kraków, Institute of Geological Sciences, Polish Academy of Sciences, 31-002 Kraków, Poland; bEcological Chemistry, Alfred-Wegener- Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570 Bremerhaven, Germany; cMarine Biogeosciences, Alfred-Wegener-Institut Helmholtz- Zentrum für Polar- und Meeresforschung, D-27570 Bremerhaven, Germany; dInstitut für Mineralogie, Leibniz Universität Hannover, 30167 Hannover, Germany; eDepartment of Computer Science, AGH University of Science and Technology, 30-052, Kraków, Poland; and fBurgers’ Ocean, Royal Burgers’ Zoo, 6816 SH Arnhem, The Netherlands Edited by Lia Addadi, Weizmann Institute of Science, Rehovot, Israel, and approved January 23, 2019 (received for review June 15, 2018) Although the emergence of complex biomineralized forms has Pioneers who studied living foraminifera described that been investigated for over a century, still little is known on how chamber formation was progressing on what they called “active single cells control morphology of skeletal structures, such as matrix” (15, 16). Hottinger (1) suggested that foraminiferal frustules, shells, spicules, or scales. We have run experiments on chamber morphology depended on the length of rhizopodia the shell formation in foraminifera, unicellular, mainly marine (branching pseudopodia) extruded from the previous chamber organisms that can build shells by successive additions of chambers. and supported by microtubular cytoskeleton. Recent investiga- We used live imaging to discover that all stages of chamber/shell tions on theoretical models of foraminiferal morphogenesis implied formation are controlled by dedicated actin-driven pseudopodial structures.
    [Show full text]
  • Three New Records of Recent Benthic Foraminifera from Korea
    Journal of Species Research 8(4):389-394, 2019 Three new records of recent benthic Foraminifera from Korea Somin Lee and Wonchoel Lee* Department of Life Science, College of Natural Sciences, Hanyang University, Seoul 04763, Republic of Korea *Correspondent: [email protected] Foraminifera are protists that inhabit diverse marine environments and show high abundance and diversity. However, previous studies on foraminifera in Korea mostly focused on geological and paleoecological fields and were conducted in a limited area. Therefore, there is a high possibility for discovering new and unrecor- ded species. Here we describe three newly recorded foraminiferal species from the southwestern part of Jeju Island during a survey on the meiofaunal community, which belongs to three different genera (Ammobaculites, Cylindroclavulina, Saracenaria), three families (Lituolidae, Vaginulinidae, Valvulinidae), and three orders (Lituolida, Textulariida, Vaginulinida): Ammobaculites formosensis Nakamura, 1937, Cylindroclavulina bradyi (Cushman, 1911), and Saracenaria hannoverana (Franke, 1936). These species have been reported from Chinese region in the East China Sea, however this is the first report from Korean waters. Particularly, Cylindroclavulina bradyi is the first report of the genus Cylindroclavulina in Korean waters. The present study supports the diversity of foraminiferal species in Korea, and the necessity of further surveys in Korean waters. Keywords: ‌East China Sea, extant species, Globothalamea, modern foraminifera Ⓒ 2019 National Institute of Biological Resources DOI:10.12651/JSR.2019.8.4.389 INTRODUCTION al., 2000; Woo and Choi, 2006; Woo and Lee, 2006; Woo, 2007; Choi et al., 2010; Jeong et al., 2016). Therefore, a Foraminifera are single-celled amoeboid protists, which high possibility of discovering new and unrecorded spe- inhabit a wide range of marine environments, and show cies is expected, particularly from uninvestigated regions high abundance and species diversity (Sen Gupta, 1999; such as the northeastern coast and open ocean regions.
    [Show full text]
  • Neogene Benthic Foraminifera from the Southern Bering Sea (IODP Expedition 323)
    Palaeontologia Electronica palaeo-electronica.org Neogene benthic foraminifera from the southern Bering Sea (IODP Expedition 323) Eiichi Setoyama and Michael A. Kaminski ABSTRACT This study describes a total of 95 calcareous benthic foraminiferal taxa from the Pliocene–Pleistocene recovered from IODP Hole U1341B in the southern Bering Sea with illustrations produced with an optical microscope and SEM. The benthic foramin- iferal assemblages are mostly dominated by calcareous taxa, and poorly diversified agglutinated forms are rare or often absent, comprising only minor components. Elon- gate, tapered, and/or flattened planispiral infaunal morphotypes are common or domi- nate the assemblages reflecting the persistent high-productivity and hypoxic conditions in the deep Bering Sea. Most of the species found in the cores are long-ranging, but we observe the extinction of several cylindrical forms that disappeared during the mid- Pleistocene Climatic Transition. Eiichi Setoyama. Earth Sciences Department, Research Group of Reservoir Characterization, King Fahd University of Petroleum & Minerals, Dhahran, 31261, Saudi Arabia current address: Energy & Geoscience Institute, University of Utah, 423 Wakara Way, Suite 300, Salt Lake City, Utah 84108, USA [email protected] Michael A. Kaminski. Earth Sciences Department, Research Group of Reservoir Characterization, King Fahd University of Petroleum & Minerals, Dhahran, 31261, Saudi Arabia [email protected] Keywords: Bering Sea; biostratigraphy; foraminifera; palaeoceanography; Pliocene-Pleistocene; taxonomy Submission: 19 February 2014. Acceptance: 1 July 2015 INTRODUCTION the foraminiferal assemblages and palaeoceano- graphic proxies in continuously-cored sections in The Bering Sea is a large, permanently the deeper, southern part of the Bering Sea, with hypoxic deep basin that has a well-developed oxy- an aim toward assessing the effects of climate gen-minimum zone (Takahashi et al., 2011).
    [Show full text]