DOCSLIB.ORG

Planktonic Forami- Nifera

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Planktonic Forami- Nifera CONTRI BUTIONS FROM THE CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH Volume XV (1964) Editor ROBERT M . KLEINPELL 1964 CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH. INC. 1964 PATRONS RS. JOS EPH A. CUSHMAN, Sharon, Massachusetts ARTHUR N. DUSENBURY, JR., 19 Sherman Ave., White Plains, New York WALDO L. SCHMITT, U . S. National Museum, Washington, D .C. SUN OIL COMPANY, Dallas, Texas FELLOWS HAROLD V. ANDERSEN, Louisiana State University, Baton Rouge, Louisiana HARRY W. ANISGARD, Humble Oil & Refg. Co., New Orleans, Louisiana ORVILLE L. BANDY, Univ. Southern California, Los Angeles, California C. LOTHROP BARTLETT, 842 East Drive, Beaumont, Texas R. STANLEY BECK, 621 Truxtun, Bakersfield , California LER6y E. BECKER , R. D. I, Spencer, Indiana NOEL BROWN, JR. , Humble Oil & Refg. Co., Houston, Texas JAMES BUSH , II T Research lnst. , Chicago, Illinois RICHARD CIFELLI, U. S. National Museum, Washington, D .C. DANA K. CLARK, 112 Cherry St., Seattle, Washington W. STORRS COLE, Cornell University, Ithaca, New York G. ARTHUR COOPER, U. S. National Museum, Washington, D.C. RAYMOND C. DOUGLASS, U. S. National Museum, Washington, D.C. RONALD ECHOLS, Univ. Southern California, Los Angeles, California M . A. FURRER, Dominion Oil Co., Port-of-Spain, Trinidad J. B. GARRETT, JR. , Pan American Petroleum Corp., Houston, Texas GEOLOGISCH-PALAONTOLOGISCHES INST., Univ. Kiel, Kiel, Germany JOSEPH J. GRAHAM, Stanford University, Stanford, California GEORG E L. HARRINGTON, 850 Webster St., Palo Alto, California HOLLIS D. HEDB ERG, 118 Liberty Place, Princeton, New Jersey LLOYD G. HEN BEST, U . S. Geological Survey, Washington, D.C. HUMBLE OIL and REFINING Co., Houston, Texas MRS. F. H. KIERSTEAD, Smith College, Northampton, Massachusetts ROBERT M. KLEINPELL, 5959 Margarido Drive, Oakland, California H. G. KUGLER, Natural History Museum, Basel, Switzerland A. R. LOEBLlCH, JR. , c/ o California Research Corp., La Habra, California DONALD H . LOKKE, East Texas State College, Commerce, Texas DORIS L. Low, U. S. Geological Survey, Washington, D.C. DONALD A. MY ERS, Federal Center, Denver, Co!orado ENRICO F. DINAPOLI, Via G. A . Guttani 14, Rome, Italy KATHERINE V . W. PALMER, Paleontological Research Institution, Ithaca, New York FRANCES L. PARK ER, Scripps Institution of Oceanography, La Jolla, California SETEMBRINO PETRI, University of Sao Paulo, Brazil FRED B PH LEGER, Scripps Institution of Oceanography, La Jolla, California MORTON POLUGAR, Standard Oil Co. of California, Oildale, California C. M. QUIGLEY, 5303 Brae Burn Drive, Bellaire, Texas K. NORMAN SACHS, U. S. National Museum, Washington, D.C. F. MARION SETZER, 536 College St., Bellaire, Texas LEO W. STACH, 255 Beaconsfield Parade, Victoria, Australia CHARLES R. STELCK, University of Alberta, Edmonton, Canada HANS E. THALMANN, P. O. Box 4407, Stanford, California M. RUTH TODD, U. S. Geological Survey, Washington, D.C. DONALD F. TOOMEY, Pan American Petroleum Corp., Tulsa, Oklahoma UNIVERSITAT GRAZ, Geologisch-PalaeontologisChes Institut, Graz, Austria JAMES A. WATERS, 308 Shadywood Lane, Seagoville, Texas R. T. D. WICKENDEN, Geological Survey of Canada, Calgary, Canada VIRGIL WINKLER, c/o Creole Petroleum Corp., Caracas, Venezuela A. E. WIRZ, 1 D Ardmore Park, Singapore, Malaya GORDON A. YOUNG, c/o Mene Grande Oil Co., Caracas, Venezuela INDEX TO VOLUME XV, 1964 A history of the holotype, ontogeny and dimorphism of Globorotaloides turgida (Finlay). By D. Graham Jenkins ... ....................................... ........................... 117 American Mid-Tertiary miogypsinid Foraminifera: classification and zonation. By W. Storrs Cole 138 Applin, Esther R. : Some Middle Eocene, Lower Eocene, and Paleocene foraminiferal faunas from west Florida ...... ................... ..................................................................................... ..................... ... .... ................... 45 Bandy, Orville L. : The type of Globigerina quadrUobata d'Orbigny 36 Bandy, Orville L.: The type of Globorotalia crassata (Cushman) .. 34 Benthonic Foraminifera of the Chukchi Sea. By Susan C. Cooper 79 Christiansen, Bengt 0 .: Normania cOllfertum from the Oslo Fiord in Norway ............................... .................. 135 Cole, W. Storrs: American Mid-Tertiary miogypsinid Foraminifera: classification and zonation ...... 138 Cooper, Susan C.: Benthonic Foraminifera of the Chukchi Sea ..... 79 Distribution of Foraminifera off the southern Atlantic Coast of the United States. By James A. Wilcoxon ................................... ........................................... ................. Gaudryilla koreaellsis, a new name for Gal/dryilla COllvexa Cushman, 1911. By N. de B. Horni- brook ....... ...................... ..................................... ..................................... .. ......................... .... ................... ..................... .. 38 Hornibrook, N. de B.: Gal/dryilla koreaellsis, a new name for Gal/dryilla cOllvexa Cushman, 1911 38 Jenkins, D. Graham: A history of the holotype, ontogeny and dimorphism of Globorotaloides tur- gida (Finlay) .. .. .... ................................ .................................... ................... ....... ..... .......... ................... 117 Jenkins, D. Graham: Location of the Pliocene-Pleistocene boundary ............................................ 25 Jenkins, D. Graham: Preliminary account of the type Aquitanian-Burdigalian planktonic Forami- nifera ...................... .......................................................................................... .................. ................................................... 28 Living planktonic Foraminifera collected along an east-west traverse in the north Pacific. By A. Barrett Smith ...................... ........................................................ ... .............................................................................. ...................... 131 Location of the Pliocene-Pleistocene Boundary. By D. Graham Jenkins ....... .... ........................... 25 Loeblich, Alfred R., Jr. and Helen Tappan: Stability of foraminiferal nomenclature ...... 30 Low, Doris: Redescription of A Il omalina eaglefordellsis Moreman .................................................................... 122 Lutze, Gerhard F.: Statistical investigations on the variability of Bolivilla argentea Cushman 105 Normallia cOllfertum from the Oslo Fiord in Norway. By Bengt O. Christiansen ........................... 135 Preliminary account of the type Aquitanian-Burdigalian planktonic Foraminifera. By D. Graham Jenkins .......... ............................ ........................... .. ................................. ... ................... ... ............................... ..................... 28 Recent literature on the Foraminifera. By Ruth Todd ..... 39, 73, 124, 151 Redescription of A Il omalina eaglefordellsis Moreman. By Doris Low ................... 122 Smith, A. Barrett: Living planktonic Foraminifera collected along an east-west traverse in the north Pacific ............................................ ....................................... ................... .............................. 131 Some Middle Eocene, Lower Eocene, and Paleocene foraminiferal faunas from west Florida. By Esther R. Applin ..... ..................................................... ...................... .................. .......... .. .................. .. ................. 45 Stability of foraminiferal nomenclature. By Alfred R. Loeblich, Jr. and Helen Tappan ........................... 30 Statistical investigations on the variability of Bolivina argelltea Cushman. By Gerhard F. Lutze ...... 105 The type of Globigerilla ql/adrUobata d'Orbigny. By Orville L. Bandy ... 36 The type of Globorotalia crassata (Cushman). By Orville L. Bandy .. 34 Todd, Ruth : Recent literature on the Foraminifera ........................ 39, 73, 124, 151 Wilcoxon, James A.: Distribution of Foraminifera off the southern Atlantic Coast of the United States ...................... ........................................ ................................. ....................................... ............................................ 1 CONTRIBUTIONS FROM THE CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH 1 CONTRIBUTIONS FROM THE CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH VOLUME XV, PART 1, JANUARY, 1964 275. DISTRIBUTION OF FORAMINIFERA OFF THE SOUTHERN ATLANTIC COAST OF THE UNITED STATES JAMES A. WILCOXON University of Southern California, Los Angeles, California! ABSTRACT Previous Work The Foraminifera from 98 s ta tions - intertidal zone to a depth of 1000 fms . - between Cape H a tte ras a nd Very little work has been done with the Forami­ the Florida S traits were s tudied. The Gulf Stream appar­ nifera from the southeast coastal area of the United ently restricts the bent honic specimens to the continental States. In 1920 Cushman undertook to describe the shelf and upper s lope, s ince f ew a re found deeper. The Foraminifera of the Atlantic Ocean with particular deeper benthonic specim ens ma y ha ve been dis placed from reference to the area adjacent to the coast of the sha llowe r w ater ; pla nktonic s pec imens are common. The number o f species inc reases with depth to the ou ter s helf , United States and the Caribbean Sea. This work was w ith a renaceous forms most common from 15-52 m. POl' primarily descriptive. Norton (1930) contributed an celaneous forms are m ost abundant nearshore, H yaline important study concerned with ecologic trends
Load more

Recommended publications
  • Foraminifera • Foraminifers Are Found in All Marine Environments
    Foraminifera • Foraminifers are found in all marine environments. Some are adapted to brackish water. There are none in fresh water. Two life modes are recognized: • Benthic . These are forms that live on the sea floor, either on the surface of the sediment (epifauna) or buried in it (infauna). • Planktonic . These are forms which float passively, moved only by currents but capable of vertica migration. Some planktonic foraminifers (their largest dimension on the order of a half-millimeter). Small benthic foraminifers (their largest dimension on the order of a half-centimeter). Some large benthic foraminifers (their largest dimension on the order of a centimeter). Planktonic Foraminifera Globigerina bulloides Globorotalia menardii d'Orbigny (Parker, Jones and Brady) Pliocene-Recent Pliocene-Recent Globigerina bulloides d'Orbigny Hantkenina alabamensis Cushman, 1927 Pliocene-Recent Eocene Globigerinoides ruber Pseudohastigerina micra d'Orbigny (Cole, 1927) Miocene-Recent Eocene-Oligocene Globorotalia inflata Globorotalia cerro- d'Orbigny azulensis Cole, 1928 Pliocene-Recent Eocene Globorotalia menardii Parasubbotina (Parker, Jones and pseudobulloides Brady) (Plummer, 1926) Pliocene-Recent Lower-Middle Palaeocene Planktonic Foraminifera Racemiguembelina Subbotina triloculinoides fructicosa (Egger) (Plummer, 1926) Middle-Uppper lower-upper Palaeocene Maastrichtian (Upper Cretaceous) Pseudotextularia elegans (Rzehak) Abathomphalus mayaroensis (Bolli) Campanian- Maastrichtian (Upper Upper Maastrichtian Cretaceous (Upper Cretaceous) Hedbergella
    [Show full text]
  • Deep Sea Drilling Project Initial Reports Volume 6
    39. PLANKTONIC MICROFOSSIL BIOSTRATIGRAPHY OF THE NORTHWESTERN PACIFIC OCEAN David Bukry1, U.S. Geological Survey, La Jolla, California, Robert G. Douglas, Case Western Reserve University, Cleveland, Ohio, Stanley A. Kling, Cities Service Oil Company, Tulsa, Oklahoma, and Valeri Krasheninnikov, Academy of Sciences of the U.S.S.R., Moscow CONTENTS Page Page Introduction 1253 Regional Correlation 1281 Zonal Comparison 1254 Calcareous Nannoplankton 1281 Planktonic Foraminifera, Mesozoic 1281 Upper Cretaceous-Paleocene Boundary 1255 California 1281 Paleocene-Eocene Boundary 1259 Japan 1285 Eocene-Oligocene Boundary 1259 West Pacific 1286 Oligocene-Miocene Boundary 1259 Australia 1287 Miocene-Pliocene Boundary 1260 Planktonic Foraminifera, Cenozoic 1288 Pliocene-Pleistocene Boundary 1261 Solomon Islands 1288 Zonal Summary 1261 Mariana Islands 1288 The Philippines 1288 Paleoecology 1261 Taiwan 1289 Calcareous Nannoplankton 1261 Japan 1289 Radiolaria 1267 Kamchatka Penisula 1290 California 1290 Preservation 1267 Radiolaria 1291 Calcareous Nannoplankton 1267 Sedimentation Rates 1291 Foraminifera 1269 Relationship to Acoustostratigraphy 1294 Radiolaria 1279 References 1296 INTRODUCTION A comparison of zonal units of calcareous nannoplank- ton, foraminifera, and radiolarians in the same strata Biostratigraphic evidence obtained from the north- shows only few cases of exact coincidence of zonal western Pacific Ocean as a result of coring carried out limits, especially if coincidences at the top or bottom by the Glomar Challenger during Leg 6 of the Deep of the standard 9-meter coring runs are dismissed as Sea Drilling Project from Hawaii to Guam is considered artificially induced owing to gaps in sediment recovery. here mainly from the standpoint of three dominant Exact coincidence of zonal limits within coring runs marine planktonic microfossil groups—calcareous nan- are most notable for the Upper Paleocene sediment of noplankton, foraminifers, and radiolarians.
    [Show full text]
  • International Symposium on Foraminifera FORAMS 2014 Chile, 19-24 January 2014
    International Symposium on Foraminifera FORAMS 2014 Chile, 19-24 January 2014 Abstract Volume Edited by: Margarita Marchant & Tatiana Hromic International Symposium on Foraminifera FORAMS 2014 Chile, 19–24 January 2014 Abstract Volume Edited by: Margarita Marchant & Tatiana Hromic Grzybowski Foundation, 2014 International Symposium on Foraminifera FORAMS 2014, Chile 19–24 January 2014 Abstract Volume Edited by: Margarita Marchant Universidad de Concepción, Concepción, Chile and Tatiana Hromic Universidad de Magallanes, Punta Arenas, Chile Published by The Grzybowski Foundation Grzybowski Foundation Special Publication No. 20 First published in 2014 by the Grzybowski Foundation a charitable scientific foundation which associates itself with the Geological Society of Poland, founded in 1992. The Grzybowski Foundation promotes and supports education and research in the field of Micropalaeontology through its Library (located at the Geological Museum of the Jagiellonian University), Special Publications, Student Grant-in-Aid Programme, Conferences (the MIKRO- and IWAF- meetings), and by organising symposia at other scientific meetings. Visit our website: www.gf.tmsoc.org Grzybowski Foundation Special Publications Editorial Board (2012-2016): M.A. Gasiński (PL) M.A. Kaminski (GB/KSA) M. Kučera (D) E. Platon (Utah) P. Sikora (Texas) R. Coccioni (Italy) J. Van Couvering (NY) P. Geroch (CA) M. Bubík (Cz.Rep) S. Filipescu (Romania) L. Alegret (Spain) S. Crespo de Cabrera (Kuwait) J. Nagy (Norway) J. Pawłowski (Switz.) J. Hohenegger (Austria) C.
    [Show full text]
  • 196. ECOLOGY of LIVING PLANKTONIC FORAMINIFERA in the NORTH and EQUATORIAL PACIFIC Oceanl JOHN S
    CONTRIBUTIONS FROM THE CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH 25 CONTRIBUTIONS FROM THE CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH VOLUME X, PART 2, APRIL, 1959 196. ECOLOGY OF LIVING PLANKTONIC FORAMINIFERA IN THE NORTH AND EQUATORIAL PACIFIC OCEANl JOHN S. BRADSHAW Scripps Institution of Oceanography, La Jolla, California ABSTRACT the results. James Moriarty drafted many of the Planktonic Foraminifera were examined from over 700 ill ustra tions. plankton tows taken at more than 400 stations in the North and equatorial Pacific Ocean. Twenty-seven species PREVIOUS WORK IN THE PACIFIC OCEAN were identified and their frequencies determined. Most specimens occur in the upper 100 m of water. The Work on the ecology of planktonic Foraminifera in species appear to be randomly distributed throughout the the North Pacific has lagged behind that in the At- upper levels with no indication of layering of the abun- lantic. Most of the papers include descriptions of dant species. bottom specimens dredged near oceanic islands but The planktonic Foraminifera in the North and equato- give little pertinent information about environmental rial Pacific can be grouped into four faunas: a cold-water fauna. a transition fauna. and two warm-water faunas. rei a tionships. The regions they inhabit appear to be differentiated by The first systematic sampling of living planktonic characteristic temperature and salinity values. The cold- Foraminifera in the Pacific was carried out by the water fauna is. limited to the area occupied by the Sub- CHALLENGER in 1874. Forty-five plankton sam- arctic Water mass while the warm-water faunas are found throughout the region occupied by the Equatorial ples, scattered throughout the North and South Pacific, and Central water masses.
    [Show full text]
  • Mining Morphological Evolution in Microfossils Using Volume Density Diagrams
    Palaeontologia Electronica palaeo-electronica.org Mining morphological evolution in microfossils using volume density diagrams Michael W. Knappertsbusch and Yannick Mary ABSTRACT A technique is explored to visualize series of bivariate morphometric measure- ments of microfossil shells through geological time with the help of 3D-animated vol- ume-density distributions. Visualization tests were performed using two existing and published sets of morphometric data, i.e., the Neogene coccolithophorid group Calcid- iscus leptoporus-Calcidiscus macintyrei and the planktonic foraminifera plexus of Glo- borotalia menardii. The technique converts series of downcore bivariate morphometric shell data into a continuous frequency distribution, which can be investigated with the help of a graphical data mining tool called Voxler from Golden Software. This tool allowed us to compose and animate complex subsurface structures raised from mor- phometric measurements of microfossils, and so provides an intuitive, comprehensive insight into the structure and dynamics of complicated evolutionary patterns. With upcoming future large morphometric data sets for oceanic microfossils, this instructive illustration method may hopefully serve to raise more interest in studying topics like morphological evolution, speciation and advances to achieve more universial species concepts needed so strongly in paleontology. An important conclusion from the experi- ments is that the structure of size frequency distribution through time shows a stronger differentiation into separate morphotype clusters in the coccolith example than in the case of the investigated planktonic foraminifers. The difference between the groups is explained by the differences in ontogenetic shell growth between the alga C. leptopo- rus and the foraminifer G. menardii. These differences have implications for morpho- type classification and evolutionary research by means of morphometry with coccolithophorids and foraminifers.
    [Show full text]
  • Long-Term Surface Uplift History of the Active Banda Arc- Continent Collision: Depth and Age Analysis of Foraminifera from Rote and Savu Islands, Indonesia
    Brigham Young University BYU ScholarsArchive Theses and Dissertations 2005-07-06 Long-Term Surface Uplift History of the Active Banda Arc- Continent Collision: Depth and Age Analysis of Foraminifera from Rote and Savu Islands, Indonesia Nova Roosmawati Brigham Young University - Provo Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Geology Commons BYU ScholarsArchive Citation Roosmawati, Nova, "Long-Term Surface Uplift History of the Active Banda Arc-Continent Collision: Depth and Age Analysis of Foraminifera from Rote and Savu Islands, Indonesia" (2005). Theses and Dissertations. 559. https://scholarsarchive.byu.edu/etd/559 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. LONG-TERM SURFACE UPLIFT HISTORY OF THE ACTIVE BANDA ARC-CONTINENT COLLISION: DEPTH AND AGE ANALYSIS OF FORAMINIFERA FROM ROTE AND SAVU ISLANDS, INDONESIA by Nova Roosmawati A thesis submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Master of Science Department of Geology Brigham Young University June 2005 BRIGHAM YOUNG UNIVERSITY GRADUATE COMMITTEE APPROVAL of a thesis submitted by Nova Roosmawati This thesis has been read by each member of the following graduate committee and by majority vote has been found to be satisfactory. _________________________
    [Show full text]
  • Shell Injury and Anomalies in Devonian Dacryoconarid Tentaculites
    Unsuccessful predation on Middle Paleozoic plankton: Shell injury and anomalies in Devonian dacryoconarid tentaculites STANISLAVA BERKYOVÁ, JIŘÍ FRÝDA, and PAVEL LUKEŠ Berkyová, S., Frýda, J., and Lukeš, P. 2007. Unsuccessful predation on Middle Paleozoic plankton: Shell injury and anomalies in Devonian dacryoconarid tentaculites. Acta Palaeontologica Polonica 52 (2): 407–412. Anomalous development of shell ornamentation and repaired shell injury in the Early Devonian dacryoconarid tenta− culites are documented and interpreted as either a repaired injury of the shell (evidence of unsuccessful predation ob− scured by recrystallization), or as a result of an anomalous function of the mantle, caused by injury of the soft body. The manner of shell repair, which resembles the way that some modern marine animals, such as mollusks, repair their shells, is discussed. The issue of phylogenetic affinities of tentaculites has been also outlined. These findings represent the first documentation of unsuccessful predation on the Middle Paleozoic plankton. Key words: Tentaculitoidea, predation, shell repair, Devonian. Stanislava Berkyová [[email protected]], Charles University, Faculty of Science, Department of Geology and Pale− ontology, Albertov 6, 128 43 Prague and Czech Geological Survey, Geologicka 6, 150 00 Prague, Czech Republic; Jiří Frýda [[email protected]], Czech Geological Survey, Geologicka 6, 150 00 Prague, Czech Republic; Pavel Lukeš [[email protected]], Třebešovská 66/561, 193 00 Prague, Czech Republic. Introduction cessful predation is an extremely common phenomenon, which is directly manifested by repaired injuries. Shell repair In the last two decades much attention has been paid to pred− has generally been increasing throughout Paleozoic time ator−prey interactions and to the evolutionary significance of (Vermeij 2002).
    [Show full text]
  • Novel Method to Image and Quantify Cogwheel Structures in Foraminiferal Shells
    fevo-08-567231 November 23, 2020 Time: 18:28 # 1 METHODS published: 26 November 2020 doi: 10.3389/fevo.2020.567231 Novel Method to Image and Quantify Cogwheel Structures in Foraminiferal Shells Inge van Dijk1*, Markus Raitzsch2, Geert-Jan A. Brummer3 and Jelle Bijma1 1 Marine Biogeoscience, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany, 2 MARUM–Zentrum für Marine Umweltwissenschaften, Universität Bremen, Bremen, Germany, 3 Department of Ocean Systems, NIOZ Royal Netherlands Institute for Sea Research, Den Burg, Netherlands Most studies designed to better understand biomineralization by foraminifera focus mainly on their shell chemistry in order to retrace processes responsible for element uptake and shell formation. Still, shell formation is a combination of not only chemical and biological processes, but is also limited by structural features. Since the processes involved in the formation of the foraminifera shell remains elusive, new focus has been put on potential structural constraints during shell formation. Revealing structural details of shells of foraminifera might increase our mechanistic understanding of foraminifera calcification, and even explain species-specific differences in element incorporation. Recently, shell structures have been studied in increasingly higher resolution and detail. Edited by: This paper aims to provide new insights on the structural features on foraminifera shells, Anne M. Gothmann, St. Olaf College, United States so-called cogwheels, which can be observed in the shell wall and at its surface. Here, Reviewed by: we present a novel method to image and quantify these cogwheel structures, using field Jan Piotr Goleñ, specimens from different environments and ecological groups, including benthic and Institute of Geological Sciences (PAN), Poland planktonic species.
    [Show full text]
  • Foraminiferal Analysis Related to Paleoceanographic Changes of Arafura Sea and Surrounding During Holocene
    Bulletin of the Marine Geology, Vol. 33, No. 2, December 2018, pp. 105 to 118 Foraminiferal Analysis Related to Paleoceanographic Changes of Arafura Sea and Surrounding During Holocene Analisis Foraminifera Berkaitan dengan Perubahan Oseanografi Purba di Laut Arafura dan Sekitarnya selama Holosen Luli Gustiantini1, Swasty Aninda Piranti1, Rina Zuraida1, Sangmin Hyun2, Duddy A.S. Ranawijaya1, F. X . H a r k i n z 1 1 Marine Geological Institute of Indonesia, Jl. Junjunan No. 236 Bandung, 40174 Indonesia, Energy and Mineral Resources Research and Development Agency 2 Marine Geology & Geophysics Division, Korea Institute of Ocean Science & Technology (KIOST), 385, Haeyang-ro, Yeo- ngdo-gu, Busan Metropolitan City, 49111 KOREA Corresponding author : [email protected] (Received 26 June 2018; in revised form 04 July 2018 accepted 20 September 2018) ABSTRACT: Arafura Sea is located between Papua and Australia as a part of Sahul Shelf. It is strongly influenced by ITF, ITCZ replacement, monsoon, and ENSO circulation that interplay with local mechanism. To understand the paleoceanographic parameter changes during Holocene, we conducted foraminiferal quantitative analysis from a 152 cm length sediment core (Aru–07), in every 10 cm interval. This sediment core was retrieved from 134o00’33.6” E, 5o55’51.59” S, by RV Geomarin 3 belongs to Marine Geological Institute. Geochronology of the sediment was reconstructed based on 2 AMS 14C age dates, analyzed on organic samples. We identified 129 species of benthic and 24 species of planktonic foraminifera that is dominated by planktonic specimens with average of 53.14%. Predominant species are Globigerina bulloides (16.16%), Globigerinoides ruber (11.18%), and Neogloboquadrina dutertrei (5.65%).
    [Show full text]
  • BOEMRE Web Site Biostratigraphic Chart May 2003
    United States Department of Interior Bureau of Ocean Energy Management, Regulation and Enforcement BOEMRE Biostratigraphic Chart of the Gulf of Mexico Offshore Region, Jurassic to Quaternary Recent through Oligocene Eocene through Jurassic Time Time CHRONOSTRATIGRAPHY BIOSTRATIGRAPHY CHRONOSTRATIGRAPHY BIOSTRATIGRAPHY (mya) BOEMRE (mya) BOEMRE (not to Foraminiferal planktic & benthic regional and Calcareous nannoplanktic regional and CHRONOZONE (not to Planktic & benthic foraminifera & ostracod (O) Calcareous nannoplanktic regional and CHRONOZONE System Subsystem Series Stage System Subsystem Series Stage scale) local markers local markers scale) regional and local markers local markers Holocene Globorotalia inflata 33.70 P Globorotalia cerroazulensis cocoaensis, Discoaster saipanensis, Globorotalia flexuosa Emiliania huxleyi (base of acme) r Hantkenina alabamensis Micrantholithus altus Upper Pontosphaera indooceanica i Textularia hockleyensis Discoaster barbadiensis U Q Sangamon fauna Gephyrocapsa oceanica flood PLU a Globorotalia cerroazulensis pomeroli I p Gephyrocapsa caribbeanica flood b Textularia dibollensis ———0.20——— o p u Helicosphaera inversa o Globigerinatheka tropicalis / mexicana Chiasmolithus consuetus EU n e P M Pseudoemiliania lacunosa "A" n Globigerinatheka semiinvoluta i i r a Globorotalia truncatulinoides coiling change, right-to-left Pseudoemiliania lacunosa "B" i Camerina moodybranchensis, Cribrocentrum reticulatum l d a Gephyrocapsa caribbeanica increase a Camerina jacksonensis e d n PLM t Gephyrocapsa omega n Sphenolithus
    [Show full text]
  • The Current State of Foraminiferal Research and Future Goals
    International Journal of Paleobiology & Paleontology ISSN: 2642-1283 MEDWIN PUBLISHERS Committed to Create Value for Researchers The Current State of Foraminiferal Research and Future Goals Valeria I Mikhalevich* Review Article Zoological Institute of the Russian Academy of Sciences, Russia Volume 4 Issue 1 Received Date: March 26, 2021 *Corresponding author: Valeria I Mikhalevich, Zoological Institute of the Russian Academy Published Date: May 05, 2021 of Sciences, Universitetskaya Nab., 1, 199034 St. Petersburg, Russia, Email: vm38600@gmail. DOI: 10.23880/ijpbp-16000125 com Abstract An overview is presented of the main achievements in studies of the phylum Foraminifera during the previous few decades, especially the last half of the 20th and the beginning of the 21st centuries, and of the most urgent goals of future studies with Keywords:a special attention Foraminifera; to the problems Morphology; of classification Ecology; as aZoogeography; base for all other Biology; studies. Molecular Studies; Systematics; Previous Achievements; Goals of Future Research Overview of the Most Important sediments was experimentally obtained [9,10]. Achievements in Different Fields of Foraminiferal Research A number of works have been devoted to foraminiferal feeding, their role in the food-chains [11-15], to the other Foraminiferology dates back to 1826, the year of aspects of their biology [16-19], to their symbionts [20-30], d’Orbigny’s publication on this group of organisms. More to the process of growth and formation of the new chambers than 5000 genera and more than 40,000 fossil and 10,000 [17,31-36], Even the problems of foraminifral infestation and recent species have been described so far.
    [Show full text]
  • Guia Para Classificação De Foraminíferos Planctônicos Recentes
    i GUIA PARA CLASSIFICAÇÃO DE FORAMINÍFEROS PLANCTÔNICOS RECENTES iii UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL INSTITUTO DE GEOCIÊNCIAS SANDRO MONTICELLI PETRÓ GUIA PARA CLASSIFICAÇÃO DE FORAMINÍFEROS PLANCTÔNICOS RECENTES IGEO/UFRGS Porto Alegre 2019 UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL Reitor: Rui Vicente Oppermann Vice-Reitor: Jane Fraga Tutikian INSTITUTO DE GEOCIÊNCIAS Diretor: André Sampaio Mexias Vice-Diretor: Nelson Luiz Sambaqui Gruber Capa: Arte do autor (Foraminíferos planctônicos ampliados 15x). Petró, Sandro Monticelli E-mail: [email protected] Petró, Sandro Monticelli Guia para classificação de foraminíferos planctônicos recentes. Sandro Monticelli Petró. - Porto Alegre: IGEO/UFRGS, 2019. [79 f]. il. ISBN: 978-85-61424-72-5 1. Paleontologia. 2. Foraminífero planctônico. I. Título. CDU 563.1 Catalogação na Publicação Biblioteca Instituto de Geociências - UFRGS Renata Cristina Grun CRB 1113/10 Universidade Federal do Rio Grande do Sul - Campus do Vale Av. Bento Gonçalves, 9500 - Porto Alegre - RS - Brasil CEP: 91501-970 / Caixa Postal: 15001. Fone: +55 51 3308-6569 Fax: +55 51 3308-6337 E-mail: [email protected] SUMÁRIO 1. INTRODUÇÃO ........................................................................................ 7 2. CRITÉRIOS GERAIS DE CLASSIFICAÇÃO........................................ 9 3. SISTEMÁTICA DOS FORAMINÍFEROS PLANCTÔNICOS RECENTES ........................................................................................ 13 3.1. Superfamílias de foraminíferos planctônicos recentes ...................
    [Show full text]