A New Integrated Approach to Taxonomy: the Fusion of Molecular and Morphological Systematics with Type Material in Benthic Foraminifera
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Tsunami-Generated Rafting of Foraminifera Across the North Pacific Ocean
Aquatic Invasions (2018) Volume 13, Issue 1: 17–30 DOI: https://doi.org/10.3391/ai.2018.13.1.03 © 2018 The Author(s). Journal compilation © 2018 REABIC Special Issue: Transoceanic Dispersal of Marine Life from Japan to North America and the Hawaiian Islands as a Result of the Japanese Earthquake and Tsunami of 2011 Research Article Tsunami-generated rafting of foraminifera across the North Pacific Ocean Kenneth L. Finger University of California Museum of Paleontology, Valley Life Sciences Building – 1101, Berkeley, CA 94720-4780, USA E-mail: [email protected] Received: 9 February 2017 / Accepted: 12 December 2017 / Published online: 15 February 2018 Handling editor: James T. Carlton Co-Editors’ Note: This is one of the papers from the special issue of Aquatic Invasions on “Transoceanic Dispersal of Marine Life from Japan to North America and the Hawaiian Islands as a Result of the Japanese Earthquake and Tsunami of 2011." The special issue was supported by funding provided by the Ministry of the Environment (MOE) of the Government of Japan through the North Pacific Marine Science Organization (PICES). Abstract This is the first report of long-distance transoceanic dispersal of coastal, shallow-water benthic foraminifera by ocean rafting, documenting survival and reproduction for up to four years. Fouling was sampled on rafted items (set adrift by the Tohoku tsunami that struck northeastern Honshu in March 2011) landing in North America and the Hawaiian Islands. Seventeen species of shallow-water benthic foraminifera were recovered from these debris objects. Eleven species are regarded as having been acquired in Japan, while two additional species (Planogypsina squamiformis (Chapman, 1901) and Homotrema rubra (Lamarck, 1816)) were obtained in the Indo-Pacific as those objects drifted into shallow tropical waters before turning north and east to North America. -
Elphidium Williamsoni
QUANTIFICATION OF THE EFFECTS OF OCEAN ACIDIFICATION ON BENTHIC FORAMINIFERA Luis Fabricio Guamán Guevara A Thesis Submitted for the Degree of PhD at the University of St Andrews 2019 Full metadata for this thesis is available in St Andrews Research Repository at: http://research-repository.st-andrews.ac.uk/ Please use this identifier to cite or link to this thesis: http://hdl.handle.net/10023/17792 This item is protected by original copyright This item is licensed under a Creative Commons License https://creativecommons.org/licenses/by-nc-nd/4.0 Quantification of the effects of ocean acidification on benthic foraminifera Luis Fabricio Guamán Guevara This thesis is submitted in partial fulfilment for the degree of Doctor of Philosophy (PhD) at the University of St Andrews October 2018 Candidate's declaration I, Luis Fabricio Guaman Guevara, do hereby certify that this thesis, submitted for the degree of PhD, which is approximately 53,000 words in length, has been written by me, and that it is the record of work carried out by me, or principally by myself in collaboration with others as acknowledged, and that it has not been submitted in any previous application for any degree. I was admitted as a research student at the University of St Andrews in November 2014. I received funding from an organisation or institution and have acknowledged the funder(s) in the full text of my thesis. Date Signature of candidate Supervisor's declaration I hereby certify that the candidate has fulfilled the conditions of the Resolution and Regulations appropriate for the degree of PhD in the University of St Andrews and that the candidate is qualified to submit this thesis in application for that degree. -
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 -
Global Change Stress on Symbiont- Bearing Benthic Foraminifera
GLOBAL CHANGE STRESS ON SYMBIONT- BEARING BENTHIC FORAMINIFERA Dissertation zur Erlangung des Doktorgrades in den Naturwissenschaften (Dr. rer. nat.) vorgelegt von Christiane Schmidt Bremen, Januar 2015 GLOBAL CHANGE STRESS ON SYMBIONT- BEARING BENTHIC FORAMINIFERA Dissertation zur Erlangung des Doktorgrades in den Naturwissenschaften (Dr. rer. nat.) im Fachbereich Geowissenschaften der Universität Bremen vorgelegt von Christiane Schmidt Bremen, Januar 2015 1. Gutachter: Professor Dr. Michal Kucera, Mikropaläontologie, Zentrum für Marine Umweltwissenschaften, MARUM, Universität Bremen 2. Gutachter: Professor Dr. Kai Bischof, Marine Botanik, Universität Bremen Datum der Verteidigung: 18. März 2015 1 Contents Zusammenfassung................................................................................................................ 5 Summary............................................................................................................................... 9 1. Introduction ...................................................................................................................11 1.1. The ecology of symbiont-bearing benthic foraminifera............................................11 1.2. The Identity and diversity of symbionts in benthic foraminifera ...............................15 1.3. Bleaching in symbiont-bearing foraminifera............................................................17 1.4. Combined effects of global change ........................................................................20 1.5. Culturing -
Preliminary Foraminiferal Survey in Chichiriviche De La Costa, Vargas, Venezuela
Revista Brasileira de Paleontologia, 24(2):90–103, Abril/Junho 2021 A Journal of the Brazilian Society of Paleontology doi:10.4072/rbp.2021.2.02 PRELIMINARY FORAMINIFERAL SURVEY IN CHICHIRIVICHE DE LA COSTA, VARGAS, VENEZUELA HUMBERTO CARVAJAL-CHITTY & SANDRA NAVARRO Departamento de Estudios Ambientales, Laboratorio de Bioestratigrafía, Universidad Simón Bolívar. Valle de Sartenejas, Caracas, Venezuela. [email protected], [email protected] ABSTRACT – A preliminary study of the composition and community structure of the foraminifera of Chichiriviche de La Costa (Vargas, Venezuela) is presented. A total of 105 species were found in samples from 10 to 40 meter-depth, and their abundance quantified in a carbonate prone area almost pristine in environmental conditions. The general composition varies in all the samples: at 10 m, Miliolida dominates the assemblages but, as it gets deeper, Rotaliida takes control of the general composition. The Shannon Wiener diversity index follows species richness along the depth profile, meanwhile the FORAM index has a higher value at 20 m and its lowest at 40 m. Variations in the P/(P+B) ratio and high number of rare species are documented and a correspondence multivariate analysis was performed in order to visualize the general community structure. These results could set some basic information that will be useful for management programs associated with the coral reef in Chichiriviche de La Costa, which is the principal focus for diver’s schools and tourism and could help the local communities to a better understanding of their ecosystem values at this location at Vargas State, Venezuela. Keywords: Miliolida, Rotaliida, foraminiferal assemblages, FORAM index, Caribbean continental shelf. -
The Evolution of Early Foraminifera
The evolution of early Foraminifera Jan Pawlowski†‡, Maria Holzmann†,Ce´ dric Berney†, Jose´ Fahrni†, Andrew J. Gooday§, Tomas Cedhagen¶, Andrea Haburaʈ, and Samuel S. Bowserʈ †Department of Zoology and Animal Biology, University of Geneva, Sciences III, 1211 Geneva 4, Switzerland; §Southampton Oceanography Centre, Empress Dock, European Way, Southampton SO14 3ZH, United Kingdom; ¶Department of Marine Ecology, University of Aarhus, Finlandsgade 14, DK-8200 Aarhus N, Denmark; and ʈWadsworth Center, New York State Department of Health, P.O. Box 509, Albany, NY 12201 Communicated by W. A. Berggren, Woods Hole Oceanographic Institution, Woods Hole, MA, August 11, 2003 (received for review January 30, 2003) Fossil Foraminifera appear in the Early Cambrian, at about the same loculus to become globular or tubular, or by the development of time as the first skeletonized metazoans. However, due to the spiral growth (12). The evolution of spiral tests led to the inadequate preservation of early unilocular (single-chambered) formation of internal septae through the development of con- foraminiferal tests and difficulties in their identification, the evo- strictions in the spiral tubular chamber and hence the appear- lution of early foraminifers is poorly understood. By using molec- ance of multilocular forms. ular data from a wide range of extant naked and testate unilocular Because of their poor preservation and the difficulties in- species, we demonstrate that a large radiation of nonfossilized volved in their identification, the unilocular noncalcareous for- unilocular Foraminifera preceded the diversification of multilocular aminifers are largely ignored in paleontological studies. In a lineages during the Carboniferous. Within this radiation, similar previous study, we used molecular data to reveal the presence of test morphologies and wall types developed several times inde- naked foraminifers, perhaps resembling those that lived before pendently. -
This Article Was Published in an Elsevier Journal. the Attached Copy Is Furnished to the Author for Non-Commercial Research
This article was published in an Elsevier journal. The attached copy is furnished to the author for non-commercial research and education use, including for instruction at the author’s institution, sharing with colleagues and providing to institution administration. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Available online at www.sciencedirect.com Marine Micropaleontology 66 (2008) 233–246 www.elsevier.com/locate/marmicro Molecular phylogeny of Rotaliida (Foraminifera) based on complete small subunit rDNA sequences ⁎ Magali Schweizer a,b, , Jan Pawlowski c, Tanja J. Kouwenhoven a, Jackie Guiard c, Bert van der Zwaan a,d a Department of Earth Sciences, Utrecht University, The Netherlands b Geological Institute, ETH Zurich, Switzerland c Department of Zoology and Animal Biology, University of Geneva, Switzerland d Department of Biogeology, Radboud University Nijmegen, The Netherlands Received 18 May 2007; received in revised form 8 October 2007; accepted 9 October 2007 Abstract The traditional morphology-based classification of Rotaliida was recently challenged by molecular phylogenetic studies based on partial small subunit (SSU) rDNA sequences. These studies revealed some unexpected groupings of rotaliid genera. However, the support for the new clades was rather weak, mainly because of the limited length of the analysed fragment. -
Deep-Water Biogenic Sediment Off the Coast of Florida
Deep-Water Biogenic Sediment off the Coast of Florida by Claudio L. Zuccarelli A Thesis Submitted to the Faculty of The Charles E. Schmidt College of Science In Partial Fulfillment of the Requirements for the Degree of Master of Science Florida Atlantic University Boca Raton, FL May 2017 Copyright 2017 by Claudio L. Zuccarelli ii Abstract Author: Claudio L. Zuccarelli Title: Deep-Water Biogenic Sediment off the Coast of Florida Institution: Florida Atlantic University Thesis Advisor: Dr. Anton Oleinik Degree: Master of Science Year: 2017 Biogenic “oozes” are pelagic sediments that are composed of > 30% carbonate microfossils and are estimated to cover about 50% of the ocean floor, which accounts for about 67% of calcium carbonate in oceanic surface sediments worldwide. These deposits exhibit diverse assemblages of planktonic microfossils and contribute significantly to the overall sediment supply and function of Florida’s deep-water regions. However, the composition and distribution of biogenic sediment deposits along these regions remains poorly documented. Seafloor surface sediments have been collected in situ via Johnson- Sea-Link I submersible along four of Florida’s deep-water regions during a joint research cruise between Harbor Branch Oceanographic Institute (HBOI) and Florida Atlantic University (FAU). Sedimentological analyses of the taxonomy, species diversity, and sedimentation dynamics reveal a complex interconnected development system of Florida’s deep-water habitats. Results disclose characteristic microfossil assemblages of planktonic foraminiferal ooze off the South West Florida Shelf, a foraminiferal-pteropod ooze through the Straits iv of Florida, and pteropod ooze deposits off Florida’s east coast. The distribution of the biogenic ooze deposits is attributed to factors such as oceanographic surface production, surface and bottom currents, off-bank transport, and deep-water sediment drifts. -
Checklist, Assemblage Composition, and Biogeographic Assessment of Recent Benthic Foraminifera (Protista, Rhizaria) from São Vincente, Cape Verdes
Zootaxa 4731 (2): 151–192 ISSN 1175-5326 (print edition) https://www.mapress.com/j/zt/ Article ZOOTAXA Copyright © 2020 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4731.2.1 http://zoobank.org/urn:lsid:zoobank.org:pub:560FF002-DB8B-405A-8767-09628AEDBF04 Checklist, assemblage composition, and biogeographic assessment of Recent benthic foraminifera (Protista, Rhizaria) from São Vincente, Cape Verdes JOACHIM SCHÖNFELD1,3 & JULIA LÜBBERS2 1GEOMAR Helmholtz-Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany 2Institute of Geosciences, Christian-Albrechts-University, Ludewig-Meyn-Straße 14, 24118 Kiel, Germany 3Corresponding author. E-mail: [email protected] Abstract We describe for the first time subtropical intertidal foraminiferal assemblages from beach sands on São Vincente, Cape Verdes. Sixty-five benthic foraminiferal species were recognised, representing 47 genera, 31 families, and 8 superfamilies. Endemic species were not recognised. The new checklist largely extends an earlier record of nine benthic foraminiferal species from fossil carbonate sands on the island. Bolivina striatula, Rosalina vilardeboana and Millettiana milletti dominated the living (rose Bengal stained) fauna, while Elphidium crispum, Amphistegina gibbosa, Quinqueloculina seminulum, Ammonia tepida, Triloculina rotunda and Glabratella patelliformis dominated the dead assemblages. The living fauna lacks species typical for coarse-grained substrates. Instead, there were species that had a planktonic stage in their life cycle. The living fauna therefore received a substantial contribution of floating species and propagules that may have endured a long transport by surface ocean currents. The dead assemblages largely differed from the living fauna and contained redeposited tests deriving from a rhodolith-mollusc carbonate facies at <20 m water depth. -
Permophiles International Commission on Stratigraphy
Permophiles International Commission on Stratigraphy Newsletter of the Subcommission on Permian Stratigraphy Number 66 Supplement 1 ISSN 1684 – 5927 August 2018 Permophiles Issue #66 Supplement 1 8th INTERNATIONAL BRACHIOPOD CONGRESS Brachiopods in a changing planet: from the past to the future Milano 11-14 September 2018 GENERAL CHAIRS Lucia Angiolini, Università di Milano, Italy Renato Posenato, Università di Ferrara, Italy ORGANIZING COMMITTEE Chair: Gaia Crippa, Università di Milano, Italy Valentina Brandolese, Università di Ferrara, Italy Claudio Garbelli, Nanjing Institute of Geology and Palaeontology, China Daniela Henkel, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany Marco Romanin, Polish Academy of Science, Warsaw, Poland Facheng Ye, Università di Milano, Italy SCIENTIFIC COMMITTEE Fernando Álvarez Martínez, Universidad de Oviedo, Spain Lucia Angiolini, Università di Milano, Italy Uwe Brand, Brock University, Canada Sandra J. Carlson, University of California, Davis, United States Maggie Cusack, University of Stirling, United Kingdom Anton Eisenhauer, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany David A.T. Harper, Durham University, United Kingdom Lars Holmer, Uppsala University, Sweden Fernando Garcia Joral, Complutense University of Madrid, Spain Carsten Lüter, Museum für Naturkunde, Berlin, Germany Alberto Pérez-Huerta, University of Alabama, United States Renato Posenato, Università di Ferrara, Italy Shuzhong Shen, Nanjing Institute of Geology and Palaeontology, China 1 Permophiles Issue #66 Supplement -
Kleptoplastidic Benthic Foraminifera from Aphotic Habitats: Insights Into Assimilation of Inorganic C, N, and S Studied with Sub-Cellular Resolution
1 Environmental Microbiology Archimer January 2019, Volume 21, Issue 1, Pages 125-141 http://dx.doi.org/10.1111/1462-2920.14433 http://archimer.ifremer.fr http://archimer.ifremer.fr/doc/00460/57188/ Kleptoplastidic benthic foraminifera from aphotic habitats: Insights into assimilation of inorganic C, N, and S studied with sub-cellular resolution Jauffrais Thierry 1, 2, *, Lekieffre Charlotte 1, 3, Schweizer Magali 1, Geslin Emmanuelle 1, Metzger Edouard 1, Bernhard Joan M. 4, Jesus Bruno 5, 6, Filipsson Helena L. 7, Maire Olivier 8, 9, Meibom Anders 3, 10 1 UMR CNRS 6112 LPG-BIAF; Université d'Angers; 2 Boulevard Lavoisier, 49045 Angers CEDEX 1, France 2 Ifremer, RBE/LEAD; 101 Promenade Roger Laroque, 98897 Nouméa, New Caledonia 3 Laboratory for Biological Geochemistry; School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique Fédérale de Lausanne (EPFL); 1015 Lausanne ,Switzerland 4 Woods Hole Oceanographic Institution; Geology & Geophysics Department; Woods Hole MA ,USA 5 EA2160, Laboratoire Mer Molécules Santé; Université de Nantes; Nantes, France 6 BioISI - Biosystems & Integrative Sciences Institute; Campo Grande University of Lisboa Faculty of Sciences; Lisboa ,Portugal 7 Department of Geology; Lund University; Sölvegatan 12, SE-223 62 Lund, Sweden 8 Univ. Bordeaux; EPOC, UMR 5805, F-33400 Talence, France 9 CNRS, EPOC; UMR 5805, F-33400 Talence, France 10 Center for Advanced Surface Analysis; Institute of Earth Sciences, University of Lausanne; 1015 Lausanne ,Switzerland * Corresponding author : Thierry Jauffrais, email address : [email protected] Abstract : The assimilation of inorganic compounds in foraminiferal metabolism compared to predation or organic matter assimilation is unknown. Here we investigate possible inorganic‐compound assimilation in Nonionellina labradorica, a common kleptoplastidic benthic foraminifer from Arctic and North Atlantic sublittoral regions. -
Taxonomy and Distribution of Meiobenthic Intertidal Foraminifera in the Coastal Tract of Midnapore (East), West Bengal, India
ISSN: 2347-3215 Volume 2 Number 3 (2014) pp. 98-104 www.ijcrar.com Taxonomy and distribution of meiobenthic intertidal foraminifera in the coastal tract of Midnapore (East), West Bengal, India D.Ghosh1, S. Majumdar2 and S.K.Chakraborty1* 1Department of Zoology, Vidyasagar University, Midnapore- 721102, West Bengal, India 2S.D. Marine biological research institute, Sagarisland, West Bengal, 743372, India *Corresponding author KEYWORDS A B S T R A C T Taxonomy and distribution of recent meiobenthic intertidal foraminifera in Rotaliida, the coastal tract of Midnapore District have been studied for a period of two Miliolida, Lituolida, years (March, 2009- February, 2011). A total of 44 meiobenthic foraminiferal Lagenida. species belonging to 22 genera, 17 families, 14 super families and 7 orders has been recorded from the intertidal belts of this coastal environment. Faunal assemblages revealed a dominance of the order Rotaliida (20 species) followed by the order Miliolida (9 species), order Lituolida (7 species), Lagenida (3 species), Trochamminida (2 species), Buliminida (2 species) and order Textulariida (1 species). Asterorotalia trispinosa, A. multispinosa, A. dentata, Ammonia beccarii, A. tepida, Miliammina fusca, Quinqueloculina seminulum, Trochammina inflata, Ammobaculites agglutinans, Elphidium hispidulum, and E. crispum were found to be the most abundant foraminifera recorded from different study sites during different seasons. Introduction Studies on recent benthic foraminifera absolutely rare (Ghosh, 1966; Majumdar et. along the intertidal beach sediments of al., 1996, 1999; Majumdar, 2004). Murray, India were very few. Occurances of recent 2006 had reported intertidal recent benthic benthic foraminifera along the west coast of foraminifera from the West Bengal coast. India has been reported by Bhalla et.