389. Distribution and Ecology of Benthonic Foraminifera in the Sediments of the Andaman Sea W
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Recent and Quaternary Foraminifera Collected Around New Caledonia
Plates 6/1 & 6/2 Recent and Quaternary foraminifera collected around New Caledonia Jean-Pierre DEBENAY 1 & Guy CABIOCH 2 1 UPRES EA, Universite d'Angers, 2 Bd Lavoisiere, 49045, Angers cedex, France 2 Institut de Recherche pour Developpement, UR 055, Paliotropique, Centre IRD, BPA5, 98848 Noumea cedex, Nouvelle-Caledonie [email protected] Abstract The compilation of the works carried out on Recent and Quaternary foraminifera collected in the waters surrounding New Caledonia allowed us to identify 574 species. These species are listed according to the classification of Loeblish & Tappan (1988), updated for the Recent species by Debenay et al. (1996). Their affinity with microfaunas from other regions is briefly discussed. Resume La compilation des travaux sur les foramini:feres actuels et quaternaires recoltes dans les eaux entourant la Nouvelle-Caledonie nous a permis de repertorier 574 especes. Ces especes sont presen tees selon la classification de Loeblish & Tappan (1988), mise ajour pour les especes actuelles par Debenay et al. (1996). Leur affinite avec les microfaunes d'autres regions est discutee brievement. Introduction The first study about foraminifera from the southwestern Pacific near New Caledonia was carried out by Brady (1884) during the voyage of H.M.S. Challenger (1873-1876), updated by Barker (1960), The nearest station was station 177, near Vanuatu (16°45'S-168°5'E). However, studies concerning directly New Caledonia began much later, with partial and local inventories in coastal samples (Gambini,1958, 1959; Renaud-Debyser, 1965; Toulouse, 1965, 1966). Samples of recent and fossil sediments collected during the Singer-Polignac mission (1960-1965) were further used for several studies of foraminiferal assemblages (Coudray & Margerel, 1974; Coudray, 1976; Margerel, 1981). -
Tasmanian Tertiary Foraminifera
Papers and Proceedings of the Royal Society of Tasmania, Volume 108 (ms. received 16.3.1973) TASMANIAN TERTIARY FORAMINIFERA Part 1. Textulariina, Miliolina, Nodosariacea by Patrick G. Quilty West Australian Petroleum Pty. Limited, Perth, W.A. (with four plates) ABSTRACT Foraminifera of the Suborders Textulariina and Miliolina and the Superfamily Nodosariacea are recorded from samples of all known Tasmanian marine Oligo-Miocene sections. Thirteen species of agglutinated foraminifera are identified specifically and one category is left in open nomenclature. Thirty species of porcellanous foraminifera (including CrenuZostomina banksi n. gen., n. sp.) are recorded and there are eight open categories. The Nodosariacea is represented by 63 identified species (including Lagena tasmaniae n. sp.) and 10 categories in open nomenclature. Information on each species includes original citation, synonymy of Australian identifications, remarks where necessary and occurrence and age in Tasmania. All identified forms are figured. INTRODUCTION AND ACKNOWLEDGEMENTS The stratigraphy of the Tasmanian Tertiary Marine succession has been reviewed by Quilty (1972). The results noted in that paper are based on foraminiferal studies conducted at the University of Tasmania. Localities, sample numbers etc., mentioned here are detailed further in Quilty (op. cit.) and this paper should be read in company with that paper. This paper is the first of a projected series of three papers documenting the Tasmanian Tertiary foraminifera. Classification adopted in these papers follows closely that proposed by Loeblich and Tappan (1964a) and reviewed by them (1964b) but differs in minor respects which will be indicated where necessary. Quilty (op. cit.) noted that the first record of Tasmanian Tertiary foraminifera was by Goddard and Jensen (1907). -
TEXTULARIID and MILIOLID FORAMINIFERA from a 50-CM CORE SEGMENT from the ARABIAN SEA 1Nimmy, P
www.ijcrt.org © 2018 IJCRT | Volume 6, Issue 2 April 2018 | ISSN: 2320-2882 TEXTULARIID AND MILIOLID FORAMINIFERA FROM A 50-CM CORE SEGMENT FROM THE ARABIAN SEA 1Nimmy, P. M., 1*Rajeshwara Rao, N., 1Nandita Nandan, T., 2Neelavannan, K. and 2Hussain, S. M. 1Department of Applied Geology and 2Department of Geology University of Madras, Guindy Campus, Chennai 600 025, India Abstract: The Arabian Sea is one of the most productive regions of the world ocean and hence has been the focus of attention of micropaleontologists from all over the world. A 5.4-m gravity core was retrieved onboard the CRV Sagar Kanya from off Goa, Arabian Sea, and its uppermost 50 cm examined for foraminifers. The systematic paleontology of textulariid and miliolid foraminifera from this core segment is presented with relevant remarks and comments on their ecology and distribution. Keywords: Foraminifera; Taxonomy; Textulariids; Miliolids; Ecology; Arabian Sea. Introduction: The seasonal reversal of the winds caused by the alternate heating and cooling of the Tibet Plateau controls the circulation in the Arabian Sea. It has, therefore, been extensively studied with respect to diverse aspects of both benthic and planktic foraminifers. Between June and September (summer), offshore Ekman transport and intense upwelling along the Oman and Somalia margins (Shi et al., 2000) are caused by the strong south-westerly winds that blow across the Arabian Sea. This upwelling process brings cold, nutrient-rich waters from a few hundred meters depth to the surface and considerably increases the biological productivity in the euphotic zone, making the Arabian Sea one of the most productive regions of the world ocean (Qasim, 1977). -
Contributions Cushman Foundation Foraminiferal
CONTRIBUTIONS FROM THE CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH VOLUME XIX, Part 4 October, 1968 Contents No. 352. Acceleration of the Evolutionary Rate in the Orbulina Lineage I D. Graham Jenkins ....................................................................................................................................................... _. ___ 133 'No. 353. A New Genus of the Haplophragmoidinae from Malaysia D. S. Dhillon ,- 140 No. 354. Late Eocene and Early Oligocene Planktonic Foraminifera from Port Eliz , abeth and Cape Foulwind, New Zealand M. S. Srinivasan .:, ........ _.... _....... __ 142 No. 355. The Genus Sigmoilopsis Finlay 1947 from Cardigan Bay, Wales. Keith Atkinson ..................... .. ...................... .......... ........ ................................................................................ _...... ___ 160 No. 356. Preliminary Report on Some Littoral Foraminifera from Tomales Bay, California Don Maurer ............... ...... ................ ................................................................... _.. ___ 163 No. 357. A Taxonomic Note on Massilina carinata (Fornasini, 1905) Keith Atkinson 165 No. 358. A New Species of Pseudoguembelina from the Upper Cretaceous ~ Texas G. C. Esker, ill .............................................................................................................................................. __ 168 No. 359. Designation of a Lectotype of Globotruncana rosetta (Carsey) G. C. Esker, ill ......................... ............................................ -
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. -
The Benthic Foraminifer Stomatorbina Binkhorsti (Reuss, 1862): Taxonomic Review and Ecological Insights
Austrian Journal of Earth Sciences Vienna 2019 Volume 112/2 195-206 DOI: 10.17738/ajes.2019.0011 The benthic foraminifer Stomatorbina binkhorsti (Reuss, 1862): Taxonomic review and ecological insights Felix SCHLAGINTWEIT1,* & Sylvain RIGAUD2 1) Lerchenauerstr. 167, 80935 München, Germany 2) Asian School of the Environment, 62 Nanyang Drive, 637459 Singapore *) Corresponding author: [email protected] KEYWORDS Benthic foraminifera, composite wall, Palaeocene, Juvenarium, Kambühel Formation, Lower Austria Abstract The benthic foraminifer Rosalina binkhorsti Reuss, 1862, was cosmopolitan in Late Cretaceous to early Paleogene shal- low-water seas. It possesses a distinctive composite wall made of a continuous, agglutinated layer discontinuously covered by secondary hyaline outer deposits. Its taxonomic position, phylogeny, morphology, wall structure, and compo- sition have been debated for a long time. Based on abundant, well-preserved material from the Danian of the Kambühel Formation in the Northern Calcareous Alps, Austria, we identify elements in the here emended species Stomatorbina binkhorsti which support a strong affinity to the order Textulariida, within the genus Stomatorbina Dorreen, 1948. Usually regarded as free (non-fixing), S. binkhorsti is here illustrated attached to small bioclasts in high-energy carbonate settings. The attached specimens are juvenile forms with a wall covered by massive hyaline deposits. This observation suggests that secondary lamellar parts added to the wall may have served for stabilisation or fixation to the substrate. Rosalina binkhorsti Reuss, 1862, war eine in den Flachwassermeeren der Oberkreide und des frühen Paläogens kos- mopolitische benthonische Foraminifere. Sie besitzt eine zusammengesetzte Wand, bestehend aus einer kontinuierlichen agglutinierten Lage welche diskontinuierlich von äusseren sekundär-hyalinen Abschnitten bedeckt ist. -
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. -
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). -
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. -
Paleoambiental Interpretations of Middle Pleistocene with Benthic
UNIVERSIDADE DO VALE DO RIO DOS SINOS - UNISINOS UNIDADE ACADÊMICA DE GRADUAÇÃO CURSO DE CIÊNCIAS BIOLÓGICAS - BACHARELADO MICAEL LUÃ BERGAMASCHI INTERPRETAÇÕES PALEOAMBIENTAIS DO PLEISTOCENO MÉDIO COM BASE EM FORAMINÍFEROS BENTÔNICOS DA BACIA DE SANTOS – BRASIL SÃO LEOPOLDO 2012 Micael Luã Bergamaschi INTERPRETAÇÕES PALEOAMBIENTAIS DO PLEISTOCENO MÉDIO COM BASE EM FORAMINÍFEROS BENTÔNICOS DA BACIA DE SANTOS – BRASIL Trabalho de Conclusão de Curso apresentado como requisito parcial para a obtenção do título de Bacharel em Ciências Biológicas, pelo Curso de Ciências Biológicas da Universidade do Vale do Rio dos Sinos - UNISINOS Orientador: Prof. Dr. Itamar Ivo Leipnitz São Leopoldo 2012 Aos meus pais, Cláudia e Fernando. Presentes nos momentos de eclipse e luz em minha vida. AGRADECIMENTOS Ao finalizar este estudo e concluir mais uma etapa em minha vida, gostaria de agradecer àqueles que colaboraram de diversas e significativas maneiras no desenvolvimento e evolução deste trabalho: Ao meu orientador, Itamar Ivo Leipnitz, que sempre me incentivou, apoiou e abriu portas na minha jovem caminhada ao longo destes anos que venho me dedicando aos estudos com foraminíferos. Aos pesquisadores e amigos, Carolina Jardim Leão e Fabricio Ferreira, pela oportunidade, ideias e ensinamentos passados, contribuindo para a realização deste trabalho e motivação para muitos outros que estão por vir. À Petrobras por ter cedido as amostras para execução deste trabalho. Aos colegas do Instituto Tecnológico de Micropaleontologia (ITT Fossil – Unisinos), pelo suporte técnico de fundamental importância. Pelas risadas e diversos momentos de descontração. Aos amigos da Biologia, pelos momentos de diversão e discussões biológicas, que de forma direta ou indireta contribuíram para a conclusão deste trabalho. -
Systematic Paleontology and Distribution of Late Eocene Benthic
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Systematic paleontology and distribution of late Eocene benthic forap.inifers from northwestern Oregon and southwestern Washington by Kristin McDougall Open-File Report 81-109 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature Systematic paleontology and distribution of late Eocene benthic foraminifers from northwestern Oregon and southwestern Washington by Kristin McDougall Introduction The purpose of this report is to document the data used in "Paleoeco- logical evaluation of late Eocene biostratigraphic zonations of the Pacific coast of North America" (McDougall, 1980). Two forms of documentation are presented: 1) systematic paleontology, and 2) fauna! distribution charts. Sample localities and stratigraphic information were given in an earlier report (McDougall, 1979). Since consistent application of zoological nomenclature and species concepts were important in resolving biostratigraphic problems considerable attention has been given to the systematic paleontology. Classification of the benthic foraminifers follows that of Loeblich and Tappan (1964). Classifi cation of the planktic foraminifers is after Poore (personal commun., 1976). Synonymies given in the following section include reference to the original description and to pertinent West Coast studies. Illustrated specimens and assemblage slides are on file at the U.S. National Museum (USNM numbers are referenced). Slides borrowed from oil companies have been returned to the respective companies. The occurrence of specimens is listed at the end of the species discussion and the reader is referred to the appropriate faunal distribution chart and species' number on the chart. The occurrence and abundance of species within the sections is indicated by the faunal distribution charts. -
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.