The Year 2000 Classification of the Agglutinated Foraminifera
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Warm Water Benthic Foraminifera Document The
Boise State University ScholarWorks Geosciences Faculty Publications and Presentations Department of Geosciences 11-15-2014 Warm Water Benthic Foraminifera Document the Pennsylvanian-permian Warming and Cooling Events – The Record from the Western Pangea Tropical Shelves Vladimir Davydov Boise State University Publication Information Davydov, Vladimir. (2014). "Warm Water Benthic Foraminifera Document the Pennsylvanian-permian Warming and Cooling Events – The Record from the Western Pangea Tropical Shelves". Palaeogeography, Palaeoclimatology, Palaeoecology, 414, 284-295. http://dx.doi.org/10.1016/j.palaeo.2014.09.013 NOTICE: this is the author’s version of a work that was accepted for publication in Palaeogeography, Palaeoclimatology, Palaeoecology. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Palaeogeography, Palaeoclimatology, Palaeoecology, (In Press). doi: 10.1016/j.palaeo.2014.09.013 This is an author-produced, peer-reviewed version of this article. The final, definitive version of this document can be found online at Palaeogeography, Palaeoclimatology, Palaeoecology, published by Elsevier. Copyright restrictions may apply. doi: 10.1016/ j.palaeo.2014.09.013 1 Vladimir Davydov Warm water benthic foraminifera document the Pennsylvanian-Permian warming and cooling events – the record from the Western Pangea tropical shelves Permian Research Institute, Boise State University and Kazan (Volga Region) Federal University , Russia; 1910 University Drive, Department of Geosciences, Boise State University, Boise, Idaho, USA; [email protected]; fax: (208) 4264061. ABSTRACT. Shallow warm water benthic foraminifera (SWWBF), including all larger fusulinids (symbiont-bearing benthic foraminifera), are among the best indicators of paleoclimate and paleogeography in the Carboniferous and Permian. -
Emplacement of the Jurassic Mirdita Ophiolites (Southern Albania): Evidence from Associated Clastic and Carbonate Sediments
Int J Earth Sci (Geol Rundsch) (2012) 101:1535–1558 DOI 10.1007/s00531-010-0603-5 ORIGINAL PAPER Emplacement of the Jurassic Mirdita ophiolites (southern Albania): evidence from associated clastic and carbonate sediments Alastair H. F. Robertson • Corina Ionescu • Volker Hoeck • Friedrich Koller • Kujtim Onuzi • Ioan I. Bucur • Dashamir Ghega Received: 9 March 2010 / Accepted: 15 September 2010 / Published online: 11 November 2010 Ó Springer-Verlag 2010 Abstract Sedimentology can shed light on the emplace- bearing pelagic carbonates of latest (?) Jurassic-Berrasian ment of oceanic lithosphere (i.e. ophiolites) onto continental age. Similar calpionellid limestones elsewhere (N Albania; crust and post-emplacement settings. An example chosen N Greece) post-date the regional ophiolite emplacement. At here is the well-exposed Jurassic Mirdita ophiolite in one locality in S Albania (Voskopoja), calpionellid lime- southern Albania. Successions studied in five different stones are gradationally underlain by thick ophiolite-derived ophiolitic massifs (Voskopoja, Luniku, Shpati, Rehove and breccias (containing both ultramafic and mafic clasts) that Morava) document variable depositional processes and were derived by mass wasting of subaqueous fault scarps palaeoenvironments in the light of evidence from compara- during or soon after the latest stages of ophiolite emplace- ble settings elsewhere (e.g. N Albania; N Greece). Ophiolitic ment. An intercalation of serpentinite-rich debris flows at extrusive rocks (pillow basalts and lava breccias) locally this locality is indicative of mobilisation of hydrated oceanic retain an intact cover of oceanic radiolarian chert (in the ultramafic rocks. Some of the ophiolite-derived conglom- Shpati massif). Elsewhere, ophiolite-derived clastics typi- erates (e.g. -
94366148005.Pdf
Boletín de la Sociedad Geológica Mexicana ISSN: 1405-3322 Sociedad Geológica Mexicana, A.C. Omaña, Lourdes; López-Doncel, Rubén; Torres, José Ramón; Alencaster, Gloria; López-Caballero, Iriliana Mid-late Cenomanian larger benthic foraminifers from the El Abra Formation W Valles-San Luis Potosi Platform, central-eastern Mexico: Taxonomy, biostratigraphy and paleoenvironmental implications Boletín de la Sociedad Geológica Mexicana, vol. 71, no. 3, 2019, September-December, pp. 691-725 Sociedad Geológica Mexicana, A.C. DOI: https://doi.org/10.18268/BSGM2019v71n3a5 Available in: https://www.redalyc.org/articulo.oa?id=94366148005 How to cite Complete issue Scientific Information System Redalyc More information about this article Network of Scientific Journals from Latin America and the Caribbean, Spain and Journal's webpage in redalyc.org Portugal Project academic non-profit, developed under the open access initiative Boletín de la Sociedad Geológica Mexicana / 2019 / 691 Mid–late Cenomanian larger benthic foraminifers from the El Abra Formation W Valles-San Luis Potosi Platform, central–eastern Mexico: Taxonomy, biostratigraphy and paleoenvironmental implications Lourdes Omaña, Rubén López-Doncel, José Ramón Torres, Gloria Alencaster, Iriliana López-Caballero ABSTRACT Lourdes Omaña ABSTRACT RESUMEN Gloria Alencaster lomanya@geología.unam.mx The Valles–San Luis Potosí Platform is La Plataforma Valles–San Luis Potosí es parte de Departamento de Paleontologia, Instituto de part of an extensive carbonate platform un sistema de plataformas extenso que se encon- Geologia, Universidad Nacional Autonoma system that rimmed the ancestral Gulf traba bordeando el antiguo Golfo de México en el de Mexico, Ciudad Universitaria, Coyoacan, of Mexico during the middle (Albian) Albiano hasta el Cretácico Superior. -
Geologic Report for the Navarin Basin Planning Area, Bering Sea, A1 Aska
OCS Report MMS 85-0045 Geologic Report for the Navarin Basin Planning Area, Bering Sea, A1 aska Ronald F. Turner Gary C. Martin Tabe 0. Flett David A. Steffy edited by Ronald F. Turner United States Department of the Interior Mineral s Management Service Alaska OCS Region Any use of trade names is for descriptive purposes only and does not constitute endorsement of these products by the Minerals Management Service. Engl ish-Metric Conversion (The following table gives the factors used to convert English units to metric units.) -- - -- - - - - -- multiply English units by to obtain metric units feet meters miles (statute) ki1 ometers acres hectares barrel s (U .S. petrol eum) 1i ters cubic meters inches centimeters pounds per gallon grams per cubic centimeter knots kilometers per hour miles per hour kilometers per hour square miles square ki1 ometers To convert from Fahrenheit (OF) to Celsius (OC), subtract 32 then divide by 1.8, - Abbreviations and Acronyms AAPG Arneri can As soci ati on of Petroleum Geol ogi sts aff. affinis (to have affinities with) APD Appl icdL ior~for Permit to Drill ARC0 Atlantic Richfield Company BHT Bottom Hole Temperature bop. before present BS R Bottom-Simulati ng Ref lector C carbon OC degrees Celsius CDP common depth point cf. confer (to be compared with) Co. Company c ommun . communication COST Continental Offshore Stratigraphic Test 0 darcy, darci es D downthrown DS T Drill Stem Test e, E early, Early E east Abbreviations and Acronyms--Continued EA Environmental Assessment ed . edi tor(s ) , edited by " F degrees Fahrenheit fig. figure ft. -
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. -
The Revised Classification of Eukaryotes
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/231610049 The Revised Classification of Eukaryotes Article in Journal of Eukaryotic Microbiology · September 2012 DOI: 10.1111/j.1550-7408.2012.00644.x · Source: PubMed CITATIONS READS 961 2,825 25 authors, including: Sina M Adl Alastair Simpson University of Saskatchewan Dalhousie University 118 PUBLICATIONS 8,522 CITATIONS 264 PUBLICATIONS 10,739 CITATIONS SEE PROFILE SEE PROFILE Christopher E Lane David Bass University of Rhode Island Natural History Museum, London 82 PUBLICATIONS 6,233 CITATIONS 464 PUBLICATIONS 7,765 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Biodiversity and ecology of soil taste amoeba View project Predator control of diversity View project All content following this page was uploaded by Smirnov Alexey on 25 October 2017. The user has requested enhancement of the downloaded file. The Journal of Published by the International Society of Eukaryotic Microbiology Protistologists J. Eukaryot. Microbiol., 59(5), 2012 pp. 429–493 © 2012 The Author(s) Journal of Eukaryotic Microbiology © 2012 International Society of Protistologists DOI: 10.1111/j.1550-7408.2012.00644.x The Revised Classification of Eukaryotes SINA M. ADL,a,b ALASTAIR G. B. SIMPSON,b CHRISTOPHER E. LANE,c JULIUS LUKESˇ,d DAVID BASS,e SAMUEL S. BOWSER,f MATTHEW W. BROWN,g FABIEN BURKI,h MICAH DUNTHORN,i VLADIMIR HAMPL,j AARON HEISS,b MONA HOPPENRATH,k ENRIQUE LARA,l LINE LE GALL,m DENIS H. LYNN,n,1 HILARY MCMANUS,o EDWARD A. D. -
A Case for Verella/Eofusulina Discrimination
SPANISH J OURNAL OF P ALAEONTOLOGY Demarcation problem in fusuline classifi cation: A case for Verella/Eofusulina discrimination Katsumi UENO1,2* & Elisa VILLA 2 1 Department of Earth System Science, Fukuoka University, Fukuoka 814-0180, Japan; [email protected] 2 Departamento de Geología, Universidad de Oviedo, c/ Jesús Arias de Velasco, s/n, 33005 Oviedo, Spain; [email protected] * Corresponding author Ueno, K. & Villa, E. 2018. Demarcation problem in fusuline classifi cation: A case for Verella/Eofusulina discrimination. [Problemas en la clasifi cación de fusulinas: el ejemplo de la distinción entre Verella y Eofusulina ]. Spanish Journal of Palaeontology, 33 (1), 215-230. Manuscript received 4 December 2017 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 5 March 2018 ABSTRACT RESUMEN The eofusulinin genera Verella and Eofusulina formed an La evolución de Verella hacia Eofusulina presenta un gran important lineage among fusulines to defi ne the Bashkirian/ interés para caracterizar paleontológicamente el intervalo Moscovian transitional interval in the Pennsylvanian (Upper de transición entre los pisos Bashkiriense y Moscoviense Carboniferous) subsystem. We studied morphologies of (Pensilvánico/Carbonífero superior). En este trabajo hemos Verella transiens , a highly evolved form in the genus, and estudiado detalladamente la morfología de Verella transiens , the fi rst Eofusulina species from the Los Tornos section in especie avanzada de este género, en ejemplares procedentes the Cantabrian Zone of northern -
High European Sauropod Dinosaur Diversity During Jurassic–Cretaceous Transition in Riodeva (Teruel, Spain)
CORE Metadata, citation and similar papers at core.ac.uk Provided by RERO DOC Digital Library [Palaeontology, Vol. 52, Part 5, 2009, pp. 1009–1027] HIGH EUROPEAN SAUROPOD DINOSAUR DIVERSITY DURING JURASSIC–CRETACEOUS TRANSITION IN RIODEVA (TERUEL, SPAIN) by RAFAEL ROYO-TORRES*, ALBERTO COBOS*, LUIS LUQUE*, AINARA ABERASTURI*, , EDUARDO ESPI´LEZ*, IGNACIO FIERRO*, ANA GONZA´ LEZ*, LUIS MAMPEL* and LUIS ALCALA´ * *Fundacio´n Conjunto Paleontolo´gico de Teruel-Dino´polis. Avda. Sagunto s ⁄ n. E-44002 Teruel, Spain; e-mail: [email protected] Escuela Taller de Restauracio´n Paleontolo´gica II del Gobierno de Arago´n. Avda. Sagunto s ⁄ n. E-44002 Teruel, Spain Typescript received 13 December 2007; accepted in revised form 3 November 2008 Abstract: Up to now, more than 40 dinosaur sites have (CPT-1074) referring to the Diplodocidae clade. New been found in the latest Jurassic – earliest Cretaceous remains from the RD-28, RD-41 and RD-43 sites, of the sedimentary outcrops (Villar del Arzobispo Formation) of same age, among which there are caudal vertebrae, are Riodeva (Iberian Range, Spain). Those already excavated, assigned to Macronaria. New sauropod footprints from the as well as other findings, provide a large and diverse Villar del Arzobispo Formation complete the extraordinary number of sauropod remains, suggesting a great diversity sauropod record coming to light in the area. The inclusion for this group in the Iberian Peninsula during this time. of other sauropods from different contemporaneous expo- Vertebrae and ischial remains from Riodevan site RD-13 sures in Teruel within the Turiasauria clade adds new evi- are assigned to Turiasaurus riodevensis (a species described dence of a great diversity of sauropods in Iberia during in RD-10, Barrihonda site), which is part of the the Jurassic–Cretaceous transition. -
Redalyc.Microfossils, Paleoenvironments And
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Filkorn, Harry F.; Scott, Robert W. Microfossils, paleoenvironments and biostratigraphy of the Mal Paso Formation (Cretaceous, upper Albian), State of Guerrero, Mexico Revista Mexicana de Ciencias Geológicas, vol. 28, núm. 1, 2011, pp. 175-191 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57220090013 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de CienciasMicrofossils, Geológicas, paleoenvironments v. 28, núm. 1, 2011, and p. biostratigraphy 175-191 of the Mal Paso Formation 175 Microfossils, paleoenvironments and biostratigraphy of the Mal Paso Formation (Cretaceous, upper Albian), State of Guerrero, Mexico Harry F. Filkorn1,* and Robert W. Scott2 1 Physics and Planetary Sciences Department, Los Angeles Pierce College, 6201 Winnetka Avenue, Woodland Hills, California 91371 USA. 2 Precision Stratigraphy Associates and University of Tulsa, 149 West Ridge Road, Cleveland, Oklahoma 74020, USA. * fi[email protected] ABSTRACT Microfossils from an outcrop of the coral reef and rudist-bearing calcareous upper member of the Mal Paso Formation just north of Chumbítaro, State of Michoacán, Mexico, indicate a deepening trend and transition from nearshore through outer shelf depositional environments upward through the sampled stratigraphic interval. The microbiota is mostly composed of species of calcareous algae and foraminifera. The identified calcareous algae are: Pseudolithothamnium album Pfender, 1936; Cayeuxia kurdistanensis Elliott, 1957; Acicularia americana Konishi and Epis, 1962; and Dissocladella sp. -
The Classification of Lower Organisms
The Classification of Lower Organisms Ernst Hkinrich Haickei, in 1874 From Rolschc (1906). By permission of Macrae Smith Company. C f3 The Classification of LOWER ORGANISMS By HERBERT FAULKNER COPELAND \ PACIFIC ^.,^,kfi^..^ BOOKS PALO ALTO, CALIFORNIA Copyright 1956 by Herbert F. Copeland Library of Congress Catalog Card Number 56-7944 Published by PACIFIC BOOKS Palo Alto, California Printed and bound in the United States of America CONTENTS Chapter Page I. Introduction 1 II. An Essay on Nomenclature 6 III. Kingdom Mychota 12 Phylum Archezoa 17 Class 1. Schizophyta 18 Order 1. Schizosporea 18 Order 2. Actinomycetalea 24 Order 3. Caulobacterialea 25 Class 2. Myxoschizomycetes 27 Order 1. Myxobactralea 27 Order 2. Spirochaetalea 28 Class 3. Archiplastidea 29 Order 1. Rhodobacteria 31 Order 2. Sphaerotilalea 33 Order 3. Coccogonea 33 Order 4. Gloiophycea 33 IV. Kingdom Protoctista 37 V. Phylum Rhodophyta 40 Class 1. Bangialea 41 Order Bangiacea 41 Class 2. Heterocarpea 44 Order 1. Cryptospermea 47 Order 2. Sphaerococcoidea 47 Order 3. Gelidialea 49 Order 4. Furccllariea 50 Order 5. Coeloblastea 51 Order 6. Floridea 51 VI. Phylum Phaeophyta 53 Class 1. Heterokonta 55 Order 1. Ochromonadalea 57 Order 2. Silicoflagellata 61 Order 3. Vaucheriacea 63 Order 4. Choanoflagellata 67 Order 5. Hyphochytrialea 69 Class 2. Bacillariacea 69 Order 1. Disciformia 73 Order 2. Diatomea 74 Class 3. Oomycetes 76 Order 1. Saprolegnina 77 Order 2. Peronosporina 80 Order 3. Lagenidialea 81 Class 4. Melanophycea 82 Order 1 . Phaeozoosporea 86 Order 2. Sphacelarialea 86 Order 3. Dictyotea 86 Order 4. Sporochnoidea 87 V ly Chapter Page Orders. Cutlerialea 88 Order 6. -
Resumenes XXXI Jornadas Paleontologia.Pdf
XXXI JORNADAS DE PALEONTOLOGÍA Sociedad Española de Paleontología Baeza, 7-10 de octubre de 2015 XXXI JORNADAS DE PALEONTOLOGÍA Sociedad Española de Paleontología Baeza, 7-10 de octubre de 2015 LIBRO DE RESÚMENES Matías Reolid (ed.) Jornadas de Paleontología (31.2015.Baeza) XXXI Jornadas de Paleontología : Baeza, 7-10 de octubre de 2015 : Libro de resúmenes / [Organizan, Sociedad Española de Paleontología…[ et al.] ; Matías Reolid , (ed.) -- Jaén : Servicio de Publicaciones, Universidad de Jaén, 2015. 312 p. ; 17 x 24 cm ISBN 978-84-8439-920-9 1. Paleontología 2. Congresos y conferencias 3. Jaén (Provincia) I. Sociedad Española de Paleontología, org. II. Reolid, Matías, ed.lit . III. Universidad de Jaén. Servicio de Publicaciones, ed. IV. Título. V. Serie 566(460.352(063) XXXI JORNADAS DE PALEONTOLOGÍA Sociedad Española de Paleontología Organizan Departamento de Geología de la Universidad de Jaén Sociedad Española de Paleontología Centro de Estudios Avanzados de Ciencias de la Tierra, Universidad de Jaén Centro de Estudios de Postgrado, Universidad de Jaén Colaboran Universidad Internacional de Andalucía, Sede Antonio Machado, Baeza Diputación de Jaén Comité Español del PICG (IUGS-UNESCO) © Autores © Universidad de Jaén Primera edición, octubre 2015 Diseño y Maquetación Servicio de Publicaciones ISBN 978-84-8439-920-9 Depósito Legal J-372-2015 Edita Publicaciones de la Universidad de Jaén Vicerrectorado de Proyección de la Cultura, Deportes y Responsabilidad Social Campus Las Lagunillas, Edificio Biblioteca 23071 Jaén (España) Teléfono 953 212 355 – Fax 953 212 235 [email protected] Impreso por Gráficas “La Paz” de Torredonjimeno, S. L. Avda. de Jaén, s/n 23650 Torredonjimeno (Jaén) Teléfono 953 571 087 – Fax 953 571 207 Impreso en España / Printed in Spain “Cualquier forma de reproducción, distribución, comunicación pública o transformación de esta obra solo puede ser realizada con la autorización de sus titulares, salvo excepción prevista por la ley.