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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. -
Origin and Beyond
EVOLUTION ORIGIN ANDBEYOND Gould, who alerted him to the fact the Galapagos finches ORIGIN AND BEYOND were distinct but closely related species. Darwin investigated ALFRED RUSSEL WALLACE (1823–1913) the breeding and artificial selection of domesticated animals, and learned about species, time, and the fossil record from despite the inspiration and wealth of data he had gathered during his years aboard the Alfred Russel Wallace was a school teacher and naturalist who gave up teaching the anatomist Richard Owen, who had worked on many of to earn his living as a professional collector of exotic plants and animals from beagle, darwin took many years to formulate his theory and ready it for publication – Darwin’s vertebrate specimens and, in 1842, had “invented” the tropics. He collected extensively in South America, and from 1854 in the so long, in fact, that he was almost beaten to publication. nevertheless, when it dinosaurs as a separate category of reptiles. islands of the Malay archipelago. From these experiences, Wallace realized By 1842, Darwin’s evolutionary ideas were sufficiently emerged, darwin’s work had a profound effect. that species exist in variant advanced for him to produce a 35-page sketch and, by forms and that changes in 1844, a 250-page synthesis, a copy of which he sent in 1847 the environment could lead During a long life, Charles After his five-year round the world voyage, Darwin arrived Darwin saw himself largely as a geologist, and published to the botanist, Joseph Dalton Hooker. This trusted friend to the loss of any ill-adapted Darwin wrote numerous back at the family home in Shrewsbury on 5 October 1836. -
Gorgonopsia: Rubidgeinae) with Implications for the Identity of This Species
Rediscovery of the holotype of Clelandina major Broom, 1948 (Gorgonopsia: Rubidgeinae) with implications for the identity of this species Christian F. Kammerer North Carolina Museum of Natural Sciences, 11 W. Jones Street, Raleigh, North Carolina 27604, U.S.A., and Evolutionary Studies Institute, University of the Witwatersrand, Private Bag 3, WITS, Johannesburg, 2050 South Africa E-mail: [email protected] Received 7 November 2017. Accepted 8 December 2017 No specimen number was given for the holotype of the rubidgeine gorgonopsian species Clelandina major Broom, 1948 in its original description. Historically, a specimen in the Rubidge Collection (RC 94) was considered to represent Broom’s type specimen for C. major. However, recent study has revealed that the holotype of C. major is in fact a different specimen in the McGregor Museum in Kimberley (MMK 5031). The morphology of this specimen is consistent with the genus Clelandina, contra work based on RC 94 that considered C. major referable to Aelurognathus. Clelandina major is here considered synonymous with the type species Clelandina rubidgei. MMK 5031 represents only the fifth known specimen of this rare and unusual gorgonopsian. Keywords: Synapsida, Therapsida, Gorgonopsia, Permian, holotype, taxonomy. Palaeontologia africana 2017. ©2017 Christian F.Kammerer. This is an open-access article published under the Creative Commons Attribution 4.0 Unported License (CC BY4.0). To view a copy of the license, please visit http://creativecommons.org/licenses/by/4.0/. This license permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. The article is permanently archived at: http://wiredspace.wits.ac.za/handle/10539/23480 INTRODUCTION provided no specimen numbers for the holotypes of Clelandina is one of the rarest and most unusual C. -
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 -
Foraminifera (Forams) in Both the Protozoa Kingdom Or 1) Order Fusilinida (Fusilinids) the Protista Kingdom and You Will Find Variation in the Books
Kingdom – Protozoa or Protista Note: Forams have been included Phylum – Foraminifera (Forams) in both the Protozoa kingdom or 1) Order Fusilinida (Fusilinids) the Protista kingdom and you will find variation in the books. 2) Genus Nummulites Forams are small (usually less than 1 mm) shelled aquatic species. There are over 10,000 known species. Most are benthic and marine, but pelagic and fresh-water species do exist. The larger forams are excellent index fossils for both age and environment for much of geologic time as their form and structure continuously evolved. They are used in oil industry research in understanding geologic environment of drilled strata. Fusulinida is an extinct order of Foraminifera that lived from the Silurian until the Permian Periods of the Paleozoic Era. They tests (shells) were composed of tightly packed microgranular calcite. Genus Nummulites - A genus of relatively large (0.5-2 inches) modern recent forams found in Eocene to Miocene rocks. The Top pyramids in Egypt are constructed of fossiliferous limestone full view of Nummulites Horizontally bisected 1 inch Kingdom – ANIMALIA 3) Genus Astraeospongia Phylum – Porifera (Sponges) 4) Genus Hydnoceras Sponges are the simplest of animals, lacking tissues or organs. However, sponge cells are integrated and organized for filter feeding, waste deposal, reproduction, and secreting a calcite base that fixes the anchors the animal to substrate. The skeletal structure is often comprised of silica and forms protective spicules. Sponges get their name from the fact that their unicellular food is not taken into a single mouth. It is filtered out of water that passes through many pores, connected by canals, in their bodies. -
Stratigraphic Data of the Middle – Late Permian on Russian Platform Données Stratigraphiques Sur Le Permien Moyen Et Supérieur De La Plate-Forme Russe
Geobios 36 (2003) 533–558 www.elsevier.com/locate/geobio Stratigraphic data of the Middle – Late Permian on Russian Platform Données stratigraphiques sur le Permien moyen et supérieur de la Plate-forme russe Vladimir P. Gorsky a, Ekaterina A. Gusseva a,†, Sylvie Crasquin-Soleau b,*, Jean Broutin c a All-Russian Geological Research Institute (VSEGEI), Sredny pr. 74, St. Petersburg, 199106, Russia b CNRS, FRE2400, université Pierre-et-Marie-Curie, département de géologie sédimentaire, T.15–25, E.4, case 104, 75252 Paris cedex 05, France c Université Pierre-et-Marie-Curie, laboratoire de paléobotanique et paléoécologie, IFR101–CNRS, 12, rue Cuvier, 75005 Paris, France Received 12 November 2001; accepted 2 December 2002 Abstract This paper presents the litho– and biostratigraphic data and correlations of the Middle and Late Permian (Ufimian, Kazanian and Tatarian) on the Russian Platform. The lithological descriptions and the paleontological content (foraminifera, bivalves, ostracods, brachiopods, vertebrates, plants and acritarchs) of the different units are exposed from the Barents Sea up to the Caspian Sea. © 2003 E´ ditions scientifiques et médicales Elsevier SAS. All rights reserved. Résumé Cet article présente les descriptions et les corrélations litho– et biostratigraphiques du Permien moyen et supérieur (Ufimien, Kazanien, Tatarien) de la Plate-forme russe depuis la mer de Barents jusqu’à la mer Caspienne. Les descriptions lithologiques et le contenu paléontologique (foraminifères, bivalves, ostracodes, brachiopodes, vertébrés, plantes et acritarches) des différentes unités sont exposés. © 2003 E´ ditions scientifiques et médicales Elsevier SAS. All rights reserved. Keywords: Stratigraphic data; Correlations; Middle and Late Permian; Russian Platform; Ostracods; Plants Mots clés : Données stratigraphiques ; Corrélations ; Permien moyen et supérieur ; Plate-forme russe ; Ostracodes ; Plantes 1. -
X. Paleontology, Biostratigraphy
BIBLIOGRAPHY OF THE GEOLOGY OF INDONESIA AND SURROUNDING AREAS Edition 7.0, July 2018 J.T. VAN GORSEL X. PALEONTOLOGY, BIOSTRATIGRAPHY www.vangorselslist.com X. PALEONTOLOGY, BIOSTRATIGRAPHY X. PALEONTOLOGY, BIOSTRATIGRAPHY ................................................................................................... 1 X.1. Quaternary-Recent faunas-microfloras and distribution ....................................................................... 60 X.2. Tertiary ............................................................................................................................................. 120 X.3. Jurassic- Cretaceous ........................................................................................................................ 161 X.4. Triassic ............................................................................................................................................ 171 X.5. Paleozoic ......................................................................................................................................... 179 X.6. Quaternary Hominids, Mammals and associated stratigraphy ........................................................... 191 This chapter X of the Bibliography 7.0 contains 288 pages with >2150 papers. These are mainly papers of a more general or regional nature. Numerous additional paleontological papers that deal with faunas/ floras from specific localities are listed under those areas in this Bibliography. It is organized in six sub-chapters: - X.1 on modern and sub-recent -
Pelycosauria Y Therapsida
Pelycosauria y Therapsida Los amniotos pueden dividirse en dos líneas principales: Los synapsidos (de quienes provienen los mamíferos) y los Sauropsidos (de quienes provienen “rep;les” y aves). Los Synápsidos poseen una apertura (fenestra) en el cráneo, detrás del ojo, debajo de la unión entre los huesos postorbital y escamoso. Comparten un ancestro en común más reciente con un mamífero que con una lagar;ja. Filogené;camente, no pertenecen a rep;lia, pero a la mayoría se les conoce como “rep;les semejantes a mamíferos” Anapsida Synapsida Diapsida “Parapsida” o “Euryapsida” (Diapsida modificados) SYNAPSIDA: -COMPARTEN UN ACMR CON MAMÍFEROS QUE CON REPTILES -FENESTRA TEMPORAL, BAJO POSTORBITAL-ESCAMOSO -REGION OCCIPITAL POSTERIORMENTE INCLINADA (NO VERTICAL) -SUPRATEMPORAL SE CONECTA AL POSTORBITAL PETROLACOSAURUS ARCHAEOTHYRIS (synapsida) -CENTRALE MEDIAL (MC) BIEN DESARROLLADO EN EL TARSO -PRESENCIA DE DOS HUESOS CORONOIDES (LADO MEDIAL MANDÍBULA) Tradicionalmente se discuten cuatro “tipos fundamnetales” de synapsidos, que en efecto son grupos sucesivamente sucesivamente anidados “Pelycosaurios” (parafilético, se usa para hablar de synapsidos basales) Carbonífero Superior- Terápsidos. Pérmico-Triásico Pérmico. Muy “reptilianos” aún Modificaciones craneales y posturales importantes Cynodontes. Pérmico superior, Triásico Mamíferos. Triásico Muy similares a mamíferos Oído interno tres huesos Dinastías synapsidas Meg Dynasty 1: Pelicosaurios del Pérmico inferior Meg Dynasty 2: Terápsidos del Pérmico superior-Triásico inferior Meg Dynasty 3: Mamíferos del Cenozoico Los primeros synápsidos (basales) se conocen colectivamente como un grupo “parafilético”, los Pelycosaurios (P en la figura) que excluyen a sus descendientes Terápsidos. Los pelycosaurios presentan abundantes dientes en el paladar. Reconstruc;on of Pangaea showing anteosaurid dinocephalians and platyoposaurid temnospondyles during the Middle Permian. Probable dispersal routes are indicated by red arrows. -
Anatomy & Physiology
ANATOMY & PHYSIOLOGY See General Rules, Eye Protection & other Policies on www.soinc.org as they apply to every event. 1. DESCRIPTION: Participants will be assessed on their understanding of the anatomy and physiology for the human Cardiovascular, Lymphatic, and Excretory systems. A TEAM OF UP TO: 2 APPROXIMATE TIME: 50 Minutes 2. EVENT PARAMETERS: Each team may bring one 8.5” x 11” sheet of paper that may contain information on both sides in any form and from any source along with two stand-alone non-programmable, non-graphing calculators. 3. THE COMPETITION: Participants will complete a written test limited to the following topics. Topics listed in italics will only be assessed at the National Tournament. a. CARDIOVASCULAR SYSTEM: i. Anatomy and physiology of the cardiovascular system ii. The Heart - chambers and valves of the heart, electrical stimulation of myocardial tissue, pacemaker tissue, interpreting ECG (EKG) readings on strips iii. Blood Vessels – structure and function of arteries, arterioles, veins, venules, capillaries, including the functionality of Startling’s forces in the capillaries iv. Blood - plasma, hematocrit, red blood cells, oxygen transport, hemoglobin and cooperative binding of oxygen, platelets and blood clotting, regulation of blood plasma volume and acidity, blood typing & basic genetics of ABO, Rh, blood types v. Measurement of the pulse rate and blood pressure with appropriate instrumentation vi. Calculations include systolic and diastolic pressure, mean arterial pressure, stroke volume & cardiac output vii. Effects of exercise, smoking, alcohol, caffeine, and drugs on the cardiovascular system viii. Understand disorders: Congestive Heart Failure, Atrial Fibrillation, Myocardial Infarction, Atherosclerosis, Bradycardia, and Tachycardia ix. -
The Year 2000 Classification of the Agglutinated Foraminifera
237 The Year 2000 Classification of the Agglutinated Foraminifera MICHAEL A. KAMINSKI Department of Earth Sciences, University College London, Gower Street, London WCIE 6BT, U.K.; and KLFR, 3 Boyne Avenue, Hendon, London, NW4 2JL, U.K. [[email protected]] ABSTRACT A reclassification of the agglutinated foraminifera (subclass Textulariia) is presented, consisting of four orders, 17 suborders, 27 superfamilies, 107 families, 125 subfamilies, and containing a total of 747 valid genera. One order (the Loftusiida Kaminski & Mikhalevich), five suborders (the Verneuilinina Mikhalevich & Kaminski, Nezzazatina, Loftusiina Kaminski & Mikhalevich, Biokovinina, and Orbitolinina), two families (the Syrianidae and the Debarinidae) and five subfamilies (the Polychasmininae, Praesphaerammininae Kaminski & Mikhalevich, Flatschkofeliinae, Gerochellinae and the Scythiolininae Neagu) are new. The classification is modified from the suprageneric scheme used by Loeblich & Tappan (1992), and incorporates all the new genera described up to and including the year 2000. The major differences from the Loeblich & Tappan classification are (1) the use of suborders within the hierarchical classification scheme (2) use of a modified Mikhalevich (1995) suprageneric scheme for the Astrorhizida (3) transfer of the Ammodiscacea to the Astrorhizida (4) restriction of the Lituolida to forms with simple wall structure (5) supression of the order Trochamminida, and (6) inclusion of the Carterinida within the Trochamminacea (7) use of the new order Loftusiida for forms with complex inner structures (8) broadening the definition of the Textulariida to include perforate forms that are initially uniserial or planispiral. Numerous minor corrections have been made based on the recent literature. INTRODUCTION The agglutinated foraminifera constitute a diverse and 25 geologically long-ranging group of organisms. -
ARSTANOSAURUS Species Undescribed AVIMIMUS Portentosus
Dinosaur Casts Specimen List ARSTANOSAURUS species undescribed Meaning of Name: Reptile from Arstan Well Classification: ORNITHOPODA; Hadrosauridae, Hadrosaurinae Age: Late Cretaceous (Santonian) Bayn Shireh Formation, 85 million years ago Locality: Gobi Desert, Peoples' Republic of Mongolia Size: l5cm in length AVIMIMUS portentosus Partial skeleton. In position as if found in field Meaning of Name: Bird Mimic Classification: THEROPODA; relationships uncertain Age: Late Cretaceous (Campanian) Djadokhta Formation, 75 million years ago Locality: Gobi Desert, Peoples' Republic of Mongolia Size: l00cm in length reconstructed Skeleton www.gondwanastudios.com BAGACERATOPS rozhdestvenskyi Meaning of Name: Small horned face Classification: CERATOPSIA; Neoceratopsia; Protoceratopsidae Age: Late Cretaceous (Campanian), Barun Goyot Formation, 75 million years ago Locality: Gobi Desert, Southern Khermin Tsav, Mongolia Size: 3.5cm in length BIARMOSUCHUS tener Meaning of Name: Crocodile from Biarmia, an ancient country in the Perm region. Classification: THERAPSIDA; Eotheriodontia; Family Biarmosuchidae Age: Late Permian, Zone I, 225 million years ago Locality: Ocher, Perm Region, Russia Size: 75cm in length Half skeleton encased in sediment, as found in the field. BULLOCKORNIS planei (Demon Duck of Doom) Meaning of Name: Bird from Bullock Creek Classification: Flightless Bird Age: 12 million years Locality: Northern Territory, Australia Size: 250cm in height www.gondwanastudios.com CATOPSALIS djadochtatherium Meaning of Name: Beast from Djadokhta