Anatomy & Physiology
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
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. -
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 -
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. -
Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park
Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park By Linda Sue Lassiter1, Justin S. Tweet2, Frederick A. Sundberg3, John R. Foster4, and P. J. Bergman5 1Northern Arizona University Department of Biological Sciences Flagstaff, Arizona 2National Park Service 9149 79th Street S. Cottage Grove, Minnesota 55016 3Museum of Northern Arizona Research Associate Flagstaff, Arizona 4Utah Field House of Natural History State Park Museum Vernal, Utah 5Northern Arizona University Flagstaff, Arizona Introduction As impressive as the Grand Canyon is to any observer from the rim, the river, or even from space, these cliffs and slopes are much more than an array of colors above the serpentine majesty of the Colorado River. The erosive forces of the Colorado River and feeder streams took millions of years to carve more than 290 million years of Paleozoic Era rocks. These exposures of Paleozoic Era sediments constitute 85% of the almost 5,000 km2 (1,903 mi2) of the Grand Canyon National Park (GRCA) and reveal important chronologic information on marine paleoecologies of the past. This expanse of both spatial and temporal coverage is unrivaled anywhere else on our planet. While many visitors stand on the rim and peer down into the abyss of the carved canyon depths, few realize that they are also staring at the history of life from almost 520 million years ago (Ma) where the Paleozoic rocks cover the great unconformity (Karlstrom et al. 2018) to 270 Ma at the top (Sorauf and Billingsley 1991). The Paleozoic rocks visible from the South Rim Visitors Center, are mostly from marine and some fluvial sediment deposits (Figure 5-1). -
Contributions Cushman Foundation Foraminiferal Research
CONTRIBUTIONS FROM THE CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH VOLUME XVII, Part 2 April, 1966 Contents PAGE No. 314. Depth at which Foraminifera can Survive in Sediments Esteban Boltovskoy 43 No. 315. Annotated bibliography of Paleozoic nOnfusulinid Foraminifera, Addendum 3 Donald F. Toomey ........................................................... 1....................................................................................... 46 No. 316. On some Recent Foraminifera from the Faeroe Islands, Denmark Drew Haman ...................................................................... .................................................................. ......................................... 67 No. 317. Quinqueloculina neosigmoilinoides, new name for Quinqueloculina sigmoili- noides Vella, preoccupied James P. Kennett ................................ .. .......... .................................. 71 Recent Literature on the Foraminifera Ruth Todd .......................................................................................... 72 1966 FRIEDA BILLlNGS CUSHMAN (October 20, 1880 - March 21, 1966) The numerous students and paleontologists who have worked at the Cushman Labora wry for Foraminiferal Research, Sharon, Massachusetts, will be saddened to learn of the ath of Mrs. Frieda Billings Cushman. Mrs. Cushman published no papers as an author, ut she made num'eI:ous indirect and important contributions to the study of Foraminifera. \ 5 the wife of the late Joseph Augustine Cushman, the founder and director of the Cush -
Contributions Cushman Foundation Foraminiferal
CONTRIBUTIONS FROM THE CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH VOLUME XVI, Part 2 April, 1965 Contents PAOB No. 296. A note on some Recent Foraminifera from northwest Iceland T. D. Adams and 1. Frampton ............................................................................ ................ ............................................................. 55 No. 297. The Foraminifera in a sample dredged from the vicinity of Salisbury Island, Durban Bay, South Africa A. D. Albani ....................................................................................... 60 No. 298. Observations on some Recent Florida Bay Foraminifera George W. Lynts 67 No. 299. Some observations on Recent foraminifers from Venezuela: Part I George A. Seiglie ............................................................................................................................. ............. ............. .................... 70 No. 300. Fusulinids from the Cyathophyllum Limestone, central Vestspitsbergen Charles A. Ross ................................................................................................................ ........................:: ................ .. ................... .. 74 Recent Literature on the Foraminifera Ruth Todd ........................................................: ................................. 87 1965 CO NTRIBUTIONS FROM THE CUSHMAN F OUN D AT[ON F OR F OR A MI N IFERAL RESE ARCH 55 CONTRIBUTIONS FROM THE CUSHMAN FOUNDATION FOR FORAMINIFERAL RESEARCH VOLUME XVI, PART 2, APRIL, 1965 296. A NOTE ON SOME -
The Revised Classification of Eukaryotes
Published in Journal of Eukaryotic Microbiology 59, issue 5, 429-514, 2012 which should be used for any reference to this work 1 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. MITCHELL,l SHARON E. MOZLEY-STANRIDGE,p LAURA W. PARFREY,q JAN PAWLOWSKI,r SONJA RUECKERT,s LAURA SHADWICK,t CONRAD L. SCHOCH,u ALEXEY SMIRNOVv and FREDERICK W. SPIEGELt aDepartment of Soil Science, University of Saskatchewan, Saskatoon, SK, S7N 5A8, Canada, and bDepartment of Biology, Dalhousie University, Halifax, NS, B3H 4R2, Canada, and cDepartment of Biological Sciences, University of Rhode Island, Kingston, Rhode Island, 02881, USA, and dBiology Center and Faculty of Sciences, Institute of Parasitology, University of South Bohemia, Cˇeske´ Budeˇjovice, Czech Republic, and eZoology Department, Natural History Museum, London, SW7 5BD, United Kingdom, and fWadsworth Center, New York State Department of Health, Albany, New York, 12201, USA, and gDepartment of Biochemistry, Dalhousie University, Halifax, NS, B3H 4R2, Canada, and hDepartment of Botany, University of British Columbia, Vancouver, BC, V6T 1Z4, Canada, and iDepartment of Ecology, University of Kaiserslautern, 67663, Kaiserslautern, Germany, and jDepartment of Parasitology, Charles University, Prague, 128 43, Praha 2, Czech -
Adl S.M., Simpson A.G.B., Lane C.E., Lukeš J., Bass D., Bowser S.S
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. MITCHELL,l SHARON E. MOZLEY-STANRIDGE,p LAURA W. PARFREY,q JAN PAWLOWSKI,r SONJA RUECKERT,s LAURA SHADWICK,t CONRAD L. SCHOCH,u ALEXEY SMIRNOVv and FREDERICK W. SPIEGELt aDepartment of Soil Science, University of Saskatchewan, Saskatoon, SK, S7N 5A8, Canada, and bDepartment of Biology, Dalhousie University, Halifax, NS, B3H 4R2, Canada, and cDepartment of Biological Sciences, University of Rhode Island, Kingston, Rhode Island, 02881, USA, and dBiology Center and Faculty of Sciences, Institute of Parasitology, University of South Bohemia, Cˇeske´ Budeˇjovice, Czech Republic, and eZoology Department, Natural History Museum, London, SW7 5BD, United Kingdom, and fWadsworth Center, New York State Department of Health, Albany, New York, 12201, USA, and gDepartment of Biochemistry, Dalhousie University, Halifax, NS, B3H 4R2, Canada, and hDepartment of Botany, University of British Columbia, Vancouver, BC, V6T 1Z4, Canada, and iDepartment -
Lab 10-Carboniferous+Perm-Online
Lab 10: Carboniferous/Permian Observations How This Lab Will Work 1. Open a Word doc or similar on your computer 2. At various points I will ask you to answer a question based on the activities in this lab. 3. I will indicate these points by this symbol: Please answer these questions in your Word doc. 4. After you have assembled the answers into your Word doc, go to the course Canvas page. 5. On the module for this week there is a link to TurnItIn. 6. Please upload your document using the TurnInIt. 7. That completes the lab assignment. :) Reminder on Observation Project Please remember that as we go through these, you should be using these fossils to construct your lab observation project, which was detailed last time. Easy to put off, hard to catch up. ;) Topics Today: 1. Introduction to Carboniferous-Permian 2. Phylum Rhizaria: Fusulinida 3. Phylum Bryozoa: Archimedes 4. Phylum Plantae: Glossopteris 5. Phylum Plantae: Lepidodendron 6. Phylum Plantae: Calamites 7. Phylum Arthropoda: Meganeuropsis 8. Phylum Arthropoda: Arthropleura 9. Phylum Chordata: Helicoprion 10. Phylum Chordata: Eryops 11. Phylum Chordata: Dimetrodon 12. Phylum Chordata: Lystrosaurus 13. Phylum Chordata: Gorgonopsia Geology 121 Lab 10: Carboniferous-Permian, page 1 of 7 Introduction to Carboniferous-Permian In today’s lab we’ll look at specimens from the Carboniferous and the Permian. The Carboniferous was period of high O2 and high CO2. It is typically divided in North America into the Mississippian and the Pennsylvanian, so a sketch of today’s time periods looks like this: Permian Pennsylvanian Carboniferous Mississippian These time periods saw developments of some things we haven’t seen before—namely, land animals, foraminifera, and forests of land plants.