For a Better Characterization of the Fossil Pelagic Record: Molecular, Biogeographical and Ecological Diversity of Planctonic Fo
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Article 57 (Protozoa 8)
THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS ARTICLE 57 (PROTOZOA 8) LATE NEOGENE PLANKTONIC FORAMINIFERS IN THE CARIBBEAN, GULF OF MEXICO, AND ITALIAN STRATOTYPES JAMES L. LAMB AND JOHN H. BEARD Esso Production Research Company, Houston, Texas The University of Kansas Paleontological Institute HAROLD NORMAN FISK MEMORIAL PAPERS Humble Oil & Refining Company THE UNIVERSITY OF KANSAS PUBLICATIONS FEBRUARY 10, 1972 THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS Article 57 (Protozoa 8), 67 Pages, 25 Figures, 36 Plates, 2 Tables LATE NEOGENE PLANKTONIC FORAMINIFERS IN THE CARIBBEAN, GULF OF MEXICO, AND ITALIAN STRATOTYPES JAMES L. LAMB AND JOHN H. BEARD Esso Production Research Company, Houston, Texas CONTENTS PAGE PAGE ABSTRACT 7 Sphaeroidinello psis sphaeroides Subzone 45 Pliocene 45 INTRODUCTION 7 Globorotalia margaritae Zone 45 Acknowledgments 8 Globorotalia multicamerata Subzone 45 PLANKTONIC SUCCESSION WITHIN STANDARD Pulleniatina primalis Subzone 45 REFERENCE SECTIONS 8 Pulleniatina obliquiloculata Zone 46 Italy 8 Pleistocene 46 General 8 Globorotalia truncatulinoides Zone 46 Tortonian Stage (late Miocene) 8 Globorotalia tosaensis Subzone 46 Messinian Stage (late Miocene) 11 Globo quadrina dutertrei Subzone 46 Tabianian, Plaisancian, and Astian Stages Pulleniatina finalis Subzone 46 (early, middle, and late Pliocene) 13 Holocene 46 Calabrian Stage (early Pleistocene) 17 Globorotalia tumida Zone 46 Le CasteIla section 20 Summary of Italian late Neogene planktonic SYSTEMATIC PALEONTOLOGY 47 succession 25 Candeina D ' ORBIGNY 47 Caribbean and Gulf of Mexico 26 C. nitida D ' ORBIGNY 47 General 26 Globigerina D ' ORBIGNY 47 No. 1 Cubagua, Venezuela 28 G. bulloides D ' ORBIGNY 47 Coastal Group, Jamaica, West Indies 31 G. nepenthes TODD 47 Sigsbee Knolls core, central Gulf of Mexico 32 G. -
Палеонтологічний Збірник 2020. № 52. С. 23–36
ПАЛЕОНТОЛОГІЧНИЙ ЗБІРНИК PALEONTOLOGICAL REVIEW 2020. № 52. С. 23–36 2020. N 52. P. 23–36 GLOBOROTALIA MENARDII (D’ORBIGNY, 1826) PARKER, JONES & BRADY, 1865 (ПЛАНКТОННІ ФОРАМІНІФЕРИ , МІОЦЕН , ПОДІЛЛЯ): ІСТОРІЯ ТА СУЧАСНИЙ СТАН (КОМЕНТАРІ ДО ТАКСОНОМІЇ , НОМЕНКЛАТУРИ І ФІЛОГЕНІЇ ) Я. Тузяк . Львівський національний університет імені Івана Франка , вул . М. Грушевського , 4, 79005 Львів , Україна e-mail: [email protected] Уперше для ранньосарматських відкладів ( буглівські верстви , міоцен ) терито- рії Поділля ( Західна Україна ) наведено монографічний опис одного з біомаркерів еко- зони Globorotalia menardii–Anomalinoides dividens–Spirolina austriaca . З’ясовано її та- ксономічне положення і філогенетичні зв ’язки . Визначено , що подія морфологічної зміни у будові скелетів Globorotalia menardii має глобальне значення із діахронним зміщенням у часі з тенденцією до омолодження і залежить від змін умов навколиш- нього середовища . Еволюційна мінливість цього таксону полягає у виявленні різно- маніття морфологічних параметрів скелетів ( розмір черепашки , висота спіралі , кіль- кість камер в останньому оберті , наявність чи відсутність кіля , шипів та ін .) від Се- редземномор ’я, тропічної Атлантики до східної частини тропічної зони Тихого й Ін- дійського океанів за останні 13 млн років . В екоінтервалі ( буглівські верстви , с. Ван- жулів ) цей вид виявлено у вигляді двох генерацій : 1 – пізньобаденська , черепашка дрібних розмірів (0.47 мм ), з меншою кількістю камер в останньому оберті (6–7,5), з кілем , оснащеним шипами , стінка -
The Planktonic Protist Interactome: Where Do We Stand After a Century of Research?
bioRxiv preprint doi: https://doi.org/10.1101/587352; this version posted May 2, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Bjorbækmo et al., 23.03.2019 – preprint copy - BioRxiv The planktonic protist interactome: where do we stand after a century of research? Marit F. Markussen Bjorbækmo1*, Andreas Evenstad1* and Line Lieblein Røsæg1*, Anders K. Krabberød1**, and Ramiro Logares2,1** 1 University of Oslo, Department of Biosciences, Section for Genetics and Evolutionary Biology (Evogene), Blindernv. 31, N- 0316 Oslo, Norway 2 Institut de Ciències del Mar (CSIC), Passeig Marítim de la Barceloneta, 37-49, ES-08003, Barcelona, Catalonia, Spain * The three authors contributed equally ** Corresponding authors: Ramiro Logares: Institute of Marine Sciences (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003, Barcelona, Catalonia, Spain. Phone: 34-93-2309500; Fax: 34-93-2309555. [email protected] Anders K. Krabberød: University of Oslo, Department of Biosciences, Section for Genetics and Evolutionary Biology (Evogene), Blindernv. 31, N-0316 Oslo, Norway. Phone +47 22845986, Fax: +47 22854726. [email protected] Abstract Microbial interactions are crucial for Earth ecosystem function, yet our knowledge about them is limited and has so far mainly existed as scattered records. Here, we have surveyed the literature involving planktonic protist interactions and gathered the information in a manually curated Protist Interaction DAtabase (PIDA). In total, we have registered ~2,500 ecological interactions from ~500 publications, spanning the last 150 years. -
September 2002
RADI LARIA VOLUME 20 SEPTEMBER 2002 NEWSLETTER OF THE INTERNATIONAL ASSOCIATION OF RADIOLARIAN PALEONTOLOGISTS ISSN: 0297.5270 INTERRAD International Association of Radiolarian Paleontologists A Research Group of the International Paleontological Association Officers of the Association President Past President PETER BAUMBARTNER JOYCE R. BLUEFORD Lausanne, Switzerland California, USA [email protected] [email protected] Secretary Treasurer JONATHAN AITCHISON ELSPETH URQUHART Department of Earth Sciences JOIDES Office University of Hong Kong Department of Geology and Geophysics Pokfulam Road, University of Miami - RSMAS Hong Kong SAR, 4600 Rickenbacker Causeway CHINA Miami FL 33149 Florida Tel: (852) 2859 8047 Fax: (852) 2517 6912 U.S.A. e-mail: [email protected] Tel: 1-305-361-4668 Fax: 1-305-361-4632 Email: [email protected] Working Group Chairmen Paleozoic Cenozoic PATRICIA, WHALEN, U.S.A. ANNIKA SANFILIPPO California, U.S.A. [email protected] [email protected] Mesozoic Recent RIE S. HORI Matsuyama, JAPAN DEMETRIO BOLTOVSKOY Buenos Aires, ARGENTINA [email protected] [email protected] INTERRAD is an international non-profit organization for researchers interested in all aspects of radiolarian taxonomy, palaeobiology, morphology, biostratigraphy, biology, ecology and paleoecology. INTERRAD is a Research Group of the International Paleontological Association (IPA). Since 1978 members of INTERRAD meet every three years to present papers and exchange ideas and materials INTERRAD MEMBERSHIP: The international Association of Radiolarian Paleontologists is open to any one interested on receipt of subscription. The actual fee US $ 15 per year. Membership queries and subscription send to Treasurer. Changes of address can be sent to the Secretary. -
Ocean Drilling Program Scientific Results Volume
Haggerty, J.A., Premoli Suva, L, Rack, R, and McNutt, M.K. (Eds.), 1995 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 144 2. PLANKTONIC FORAMINIFER BIOSTRATIGRAPHY AND THE DEVELOPMENT OF PELAGIC CAPS ON GUYOTS IN THE MARSHALL ISLANDS GROUP1 Paul N. Pearson2 ABSTRACT Five guyots were drilled on Ocean Drilling Program Leg 144, three of which possess thick caps of pelagic sediment. These guyots (Limalok, Site 871; Lo-En, Site 872; and Wodejebato, Site 873) belong to the Marshall Islands group of seamounts. Pelagic sediments of late Oligocene to Holocene age were recovered from them. In each case, the sediment was found to be unconsolidated on recovery and contain very abundant planktonic foraminifers, particularly in the >150-µm size range. Preservation of tests is generally good, with most showing only minor signs of dissolution or recrystallization, although many samples have a high proportion of fragmented material in the fine fraction. Planktonic foraminifer faunas are diverse and consist predominantly of warm-water species. A typically western Pacific fauna occurs throughout the Miocene. Biostratigraphic assignment was generally straightforward except for the bottommost interval of the pelagic caps where severe reworking (sediment mixing) is a common feature. A significant hiatus was found at each site between drowning of the carbonate platform and the onset of pelagic sediment accumulation. Thus, the platforms were apparently swept clean of sediments, with the exception of isolated ponds, until subsidence took the guyots sufficiently deep for sediment to accumulate in large quantities. Backtracking of subsidence paths for each guyot suggests that pelagic cap formation began at depths of between 700 and 1000 mbsl. -
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. -
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 Planktonic Foraminifera of the Jurassic. Part III: Annotated Historical Review and References
Swiss J Palaeontol (2017) 136:273–285 DOI 10.1007/s13358-017-0130-0 The planktonic foraminifera of the Jurassic. Part III: annotated historical review and references Felix M. Gradstein1,2 Received: 21 February 2017 / Accepted: 3 April 2017 / Published online: 7 July 2017 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2017 Abstract Over 70 publications on Jurassic planktonic With few exceptions, Jurassic planktonic foraminifera foraminifera, particularly by East and West European and publications based on thin-sections are not covered in this Canadian micropalaeontologists, are summarized and review. Emphasis is only on thin-section studies that had briefly annotated. It provides an annotated historic over- impact on our understanding of Jurassic planktonic for- view for this poorly understood group of microfossils, aminifera. By the same token, microfossil casts do not going back to 1881 when Haeusler described Globigerina allow study of the taxonomically important wall structure helvetojurassica from the Birmenstorfer Schichten of and sculpture; reference to such studies is limited to few of Oxfordian age in Canton Aargau, Switzerland. historic interest. The first four, presumably planktonic foraminiferal spe- Keywords Jurassic Á Planktonic foraminifera Á Annotated cies from Jurassic strata, were described in the second half of historical review 1881–2015 the nineteenth century: Globigerina liasina from the Middle Lias of France (Terquem and Berthelin 1875), G. helveto- jurassica from the Early Oxfordian of Switzerland (Haeusler Annotated historical overview 1881, 1890) and G. oolithica and G. lobata from the Bajocian of France (Terquem 1883). Some descriptions were from Jurassic planktonic foraminifera have been studied since the internal moulds. It was not until 1958 (see below) that more second half of the nineteen’s century, but it was not until after attention was focused on the occurrences of early planktonic the Second World War that micropalaeontological studies foraminifera, with emphasis on free specimens. -
Northeast Atlantic Late Quaternary Planktic Foraminifera As Primary Productivity and Water Mass Indicators
Northeast Atlantic Late Quaternary planktic Foraminifera as primary productivity and water mass indicators Shirley A. van Kreveld Kreveld, S.A. van. Northeast Atlantic Late Quaternary planktic Foraminifera as primary productivity and water mass indicators. — Scripta Geol., 113: 23-91, 18 figs., 12 pls, Leiden, December 1996. S.A. van Kreveld, Center for Marine Earth Sciences, Institute of Earth Sciences, Free University, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands. Keywords: Planktic Foraminifera, palaeo primary productivity, water mass, Northeast Atlantic. Primary productivity and water mass reconstructions based on planktic Foraminifera reveal distinct interglacial/glacial variations for the past 208 ka in a mid-latitude Northeast Atlantic piston core. Average total planktic foraminiferal absolute frequencies and accumulation rates, which are interpret- ed to reflect primary productivity, are higher in interglacial than in glacial sediments. Low total planktic foraminiferal absolute frequencies and accumulation rates in 'Heinrich layers' are likewise interpreted to show low production of Foraminifera due to low surface ocean fertility. 'Heinrich layers' are enriched in ice-rafted debris, recording periods of massive iceberg production and rapid melting in the Northeast Atlantic. The dominance of Neogloboquadrina pachyderma (sinistral) in these layers reflects an extension of cold low salinity polar waters. The fresh water along with tur- bidity caused by melting icebergs may account for the low productivity during these events. In contrast, the dominance of Globigerina bulloides, Neogloboquadrina incompta, Globorotalia scitula, Globi- gerinita glutinata, and Globorotalia inflata group in interglacial sediments is interpreted to reflect condi- tions comparable with the present day North Atlantic Current (NAC) waters in the area. In the mod- ern ocean, the Gulf Stream and its extension, the NAC, are driven by seasonally strong westerly winds which induce mixing, supplying nutrients from deep to surface waters. -
Ecology of Foraminifera in Northeastern Gulf of Mexico
Ecology of Foraminifera in Northeastern Gulf of Mexico GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-G This report concerns work done partly on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission Errata: Prof. Paper 27^-G, Ecology of Foraminifera in northeastern Gulf of Mexico. p. 185, 20^4- - Quinqueloculina agglutinata should be Quinqueloculina agglutinans. p. 186 } 20^4- - Textularia barrettii shouild "be Textulariella barrettii. Ecology of Foraminifera in Northeastern Gulf of Mexico By ORVILLE L. BANDY A SHORTER CONTRIBUTION TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-G Frequency distribution oj Recent Foraminifera in the coastal waters of western Florida. This report concerns work done partly on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1956 UNITED STATES DEPARTMENT OF THE INTERIOR Fred A. Seaton, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Page Abstract_________________________________________ 179 Faunal zonation—Continued Introduction______________________________________ 179 Offshore faunal zones—Continued Previous work___--_______-___-____.-_------____-___ 180 Fauna 5 (251-600 feet)_____---_---_ —------- 186 Method of study.----__--___-________-._....-._---__ 181 Planktonic species__________-_-_-__---_-_-_ 186 Faunal zonation__________________________________ -
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 -
Capítulo 6 Foraminíferos Planctónicos: Globigerinina
Micropaleontología (E. Molina, ed., 2004) 127 Capítulo 6 Foraminíferos planctónicos: Globigerinina Eustoquio Molina 6.1. Introducción Globigerinina constituye un suborden de foraminíferos calcíticos hialinos perforados muy abundante en el ecosistema del plancton marino desde el Cretácico, si bien aparecieron en el Jurásico. Al morir, sus pequeñas conchas caen a los fondos oceánicos, conservándose relativamente bien y contribuyendo en gran medida a la formación de rocas sedimentarias pelágicas. La morfología de su concha es muy diagnóstica y, junto a su excelente registro, ha permitido realizar estudios bioestratigráficos muy precisos. Además, en las últimas décadas se ha puesto de manifiesto su gran interés en estudios paleoecológicos y evolutivos. Las primeras descripciones significativas fueron realizadas entre 1826 y 1839 por d'Orbigny, quien los encontró en las arenas de playa y sedimentos marinos de las Islas Canarias, Cuba y América del Sur, pero no descubrió su tipo de vida pelágico. Asimismo, otros naturalistas del siglo XIX, tales como Ehrenberg, Carpenter, Parker y Jones, estudiaron los foraminíferos de sedimentos del Atlántico y asumieron erróneamente que vivían en los fondos oceánicos. Pero en 1867 Owen descubrió su modo de vida planctónico, lo cual fue ignorado hasta que la expedición Challenger (1872-1876) pudo confirmar su descubrimiento. En 1884 Brady, en su informe sobre los foraminíferos dragados en dicha expedición, dio detallada información de la amplia distribución y abundancia de una veintena de especies, aunque pensaba que alguna podía vivir en el fondo. A finales del siglo XIX, Murray analizó más en detalle su distribución latitudinal y muchos rasgos básicos de su biología y ecología. Desde entonces muchos investigadores han precisado la distribución latitudinal y batimétrica de las especies actuales y de la mayor parte de las fósiles, lo cual ha sido de gran utilidad para las reconstrucciones 128 Foraminíferos planctónicos (E.