The Silurian Hypothesis: Would It Be Possible to Detect an Industrial
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Gender and the Quest in British Science Fiction Television CRITICAL EXPLORATIONS in SCIENCE FICTION and FANTASY (A Series Edited by Donald E
Gender and the Quest in British Science Fiction Television CRITICAL EXPLORATIONS IN SCIENCE FICTION AND FANTASY (a series edited by Donald E. Palumbo and C.W. Sullivan III) 1 Worlds Apart? Dualism and Transgression in Contemporary Female Dystopias (Dunja M. Mohr, 2005) 2 Tolkien and Shakespeare: Essays on Shared Themes and Language (ed. Janet Brennan Croft, 2007) 3 Culture, Identities and Technology in the Star Wars Films: Essays on the Two Trilogies (ed. Carl Silvio, Tony M. Vinci, 2007) 4 The Influence of Star Trek on Television, Film and Culture (ed. Lincoln Geraghty, 2008) 5 Hugo Gernsback and the Century of Science Fiction (Gary Westfahl, 2007) 6 One Earth, One People: The Mythopoeic Fantasy Series of Ursula K. Le Guin, Lloyd Alexander, Madeleine L’Engle and Orson Scott Card (Marek Oziewicz, 2008) 7 The Evolution of Tolkien’s Mythology: A Study of the History of Middle-earth (Elizabeth A. Whittingham, 2008) 8 H. Beam Piper: A Biography (John F. Carr, 2008) 9 Dreams and Nightmares: Science and Technology in Myth and Fiction (Mordecai Roshwald, 2008) 10 Lilith in a New Light: Essays on the George MacDonald Fantasy Novel (ed. Lucas H. Harriman, 2008) 11 Feminist Narrative and the Supernatural: The Function of Fantastic Devices in Seven Recent Novels (Katherine J. Weese, 2008) 12 The Science of Fiction and the Fiction of Science: Collected Essays on SF Storytelling and the Gnostic Imagination (Frank McConnell, ed. Gary Westfahl, 2009) 13 Kim Stanley Robinson Maps the Unimaginable: Critical Essays (ed. William J. Burling, 2009) 14 The Inter-Galactic Playground: A Critical Study of Children’s and Teens’ Science Fiction (Farah Mendlesohn, 2009) 15 Science Fiction from Québec: A Postcolonial Study (Amy J. -
Climate Instability and Tipping Points in the Late Devonian
Archived version from NCDOCKS Institutional Repository – http://libres.uncg.edu/ir/asu/ Sarah K. Carmichael, Johnny A. Waters, Cameron J. Batchelor, Drew M. Coleman, Thomas J. Suttner, Erika Kido, L.M. Moore, and Leona Chadimová, (2015) Climate instability and tipping points in the Late Devonian: Detection of the Hangenberg Event in an open oceanic island arc in the Central Asian Orogenic Belt, Gondwana Research The copy of record is available from Elsevier (18 March 2015), ISSN 1342-937X, http://dx.doi.org/10.1016/j.gr.2015.02.009. Climate instability and tipping points in the Late Devonian: Detection of the Hangenberg Event in an open oceanic island arc in the Central Asian Orogenic Belt Sarah K. Carmichael a,*, Johnny A. Waters a, Cameron J. Batchelor a, Drew M. Coleman b, Thomas J. Suttner c, Erika Kido c, L. McCain Moore a, and Leona Chadimová d Article history: a Department of Geology, Appalachian State University, Boone, NC 28608, USA Received 31 October 2014 b Department of Geological Sciences, University of North Carolina - Chapel Hill, Received in revised form 6 Feb 2015 Chapel Hill, NC 27599-3315, USA Accepted 13 February 2015 Handling Editor: W.J. Xiao c Karl-Franzens-University of Graz, Institute for Earth Sciences (Geology & Paleontology), Heinrichstrasse 26, A-8010 Graz, Austria Keywords: d Institute of Geology ASCR, v.v.i., Rozvojova 269, 165 00 Prague 6, Czech Republic Devonian–Carboniferous Chemostratigraphy Central Asian Orogenic Belt * Corresponding author at: ASU Box 32067, Appalachian State University, Boone, NC 28608, USA. West Junggar Tel.: +1 828 262 8471. E-mail address: [email protected] (S.K. -
Revised Correlation of Silurian Provincial Series of North America with Global and Regional Chronostratigraphic Units 13 and D Ccarb Chemostratigraphy
Revised correlation of Silurian Provincial Series of North America with global and regional chronostratigraphic units 13 and d Ccarb chemostratigraphy BRADLEY D. CRAMER, CARLTON E. BRETT, MICHAEL J. MELCHIN, PEEP MA¨ NNIK, MARK A. KLEFF- NER, PATRICK I. MCLAUGHLIN, DAVID K. LOYDELL, AXEL MUNNECKE, LENNART JEPPSSON, CARLO CORRADINI, FRANK R. BRUNTON AND MATTHEW R. SALTZMAN Cramer, B.D., Brett, C.E., Melchin, M.J., Ma¨nnik, P., Kleffner, M.A., McLaughlin, P.I., Loydell, D.K., Munnecke, A., Jeppsson, L., Corradini, C., Brunton, F.R. & Saltzman, M.R. 2011: Revised correlation of Silurian Provincial Series of North America with global 13 and regional chronostratigraphic units and d Ccarb chemostratigraphy. Lethaia,Vol.44, pp. 185–202. Recent revisions to the biostratigraphic and chronostratigraphic assignment of strata from the type area of the Niagaran Provincial Series (a regional chronostratigraphic unit) have demonstrated the need to revise the chronostratigraphic correlation of the Silurian System of North America. Recently, the working group to restudy the base of the Wen- lock Series has developed an extremely high-resolution global chronostratigraphy for the Telychian and Sheinwoodian stages by integrating graptolite and conodont biostratigra- 13 phy with carbonate carbon isotope (d Ccarb) chemostratigraphy. This improved global chronostratigraphy has required such significant chronostratigraphic revisions to the North American succession that much of the Silurian System in North America is cur- rently in a state of flux and needs further refinement. This report serves as an update of the progress on recalibrating the global chronostratigraphic correlation of North Ameri- can Provincial Series and Stage boundaries in their type area. -
The Geologic Time Scale Is the Eon
Exploring Geologic Time Poster Illustrated Teacher's Guide #35-1145 Paper #35-1146 Laminated Background Geologic Time Scale Basics The history of the Earth covers a vast expanse of time, so scientists divide it into smaller sections that are associ- ated with particular events that have occurred in the past.The approximate time range of each time span is shown on the poster.The largest time span of the geologic time scale is the eon. It is an indefinitely long period of time that contains at least two eras. Geologic time is divided into two eons.The more ancient eon is called the Precambrian, and the more recent is the Phanerozoic. Each eon is subdivided into smaller spans called eras.The Precambrian eon is divided from most ancient into the Hadean era, Archean era, and Proterozoic era. See Figure 1. Precambrian Eon Proterozoic Era 2500 - 550 million years ago Archaean Era 3800 - 2500 million years ago Hadean Era 4600 - 3800 million years ago Figure 1. Eras of the Precambrian Eon Single-celled and simple multicelled organisms first developed during the Precambrian eon. There are many fos- sils from this time because the sea-dwelling creatures were trapped in sediments and preserved. The Phanerozoic eon is subdivided into three eras – the Paleozoic era, Mesozoic era, and Cenozoic era. An era is often divided into several smaller time spans called periods. For example, the Paleozoic era is divided into the Cambrian, Ordovician, Silurian, Devonian, Carboniferous,and Permian periods. Paleozoic Era Permian Period 300 - 250 million years ago Carboniferous Period 350 - 300 million years ago Devonian Period 400 - 350 million years ago Silurian Period 450 - 400 million years ago Ordovician Period 500 - 450 million years ago Cambrian Period 550 - 500 million years ago Figure 2. -
(Silurian) Anoxic Palaeo-Depressions at the Western Margin of the Murzuq Basin (Southwest Libya), Based on Gamma-Ray Spectrometry in Surface Exposures
GeoArabia, Vol. 11, No. 3, 2006 Gulf PetroLink, Bahrain Identification of early Llandovery (Silurian) anoxic palaeo-depressions at the western margin of the Murzuq Basin (southwest Libya), based on gamma-ray spectrometry in surface exposures Nuri Fello, Sebastian Lüning, Petr Štorch and Jonathan Redfern ABSTRACT Following the melting of the Gondwanan icecap and the resulting postglacial sea- level rise, organic-rich shales were deposited in shelfal palaeo-depressions across North Africa and Arabia during the latest Ordovician to earliest Silurian. The unit is absent on palaeohighs that were flooded only later when the anoxic event had already ended. The regional distribution of the Silurian black shale is now well-known for the subsurface of the central parts of the Murzuq Basin, in Libya, where many exploration wells have been drilled and where the shale represents the main hydrocarbon source rock. On well logs, the Silurian black shale is easily recognisable due to increased uranium concentrations and, therefore, elevated gamma-ray values. The uranium in the shales “precipitated” under oxygen- reduced conditions and generally a linear relationship between uranium and organic content is developed. The distribution of the Silurian organic-rich shales in the outcrop belts surrounding the Murzuq Basin has been long unknown because Saharan surface weathering has commonly destroyed the organic matter and black colour of the shales, making it complicated to identify the previously organic-rich unit in the field. In an attempt to distinguish (previously) organic-rich from organically lean shales at outcrop, seven sections that straddle the Ordovician-Silurian boundary were measured by portable gamma-ray spectrometer along the outcrops of the western margin of the Murzuq Basin. -
Chordates (Phylum Chordata)
A short story Leathem Mehaffey, III, Fall 201993 The First Chordates (Phylum Chordata) • Chordates (our phylum) first appeared in the Cambrian, 525MYA. 94 Invertebrates, Chordates and Vertebrates • Invertebrates are all animals not chordates • Generally invertebrates, if they have hearts, have dorsal hearts; if they have a nervous system it is usually ventral. • All vertebrates are chordates, but not all chordates are vertebrates. • Chordates: • Dorsal notochord • Dorsal nerve chord • Ventral heart • Post-anal tail • Vertebrates: Amphioxus: archetypal chordate • Dorsal spinal column (articulated) and skeleton 95 Origin of the Chordates 96 Haikouichthys Myllokunmingia Note the rounded extension to Possibly the oldest the head bearing sensory vertebrate: showed gill organs bars and primitive vertebral elements Early and primitive agnathan vertebrates of the Early Cambrian (530MYA) Pikaia Note: these organisms were less Primitive chordate, than an inch long. similar to Amphioxus 97 The Cambrian/Ordovician Extinction • Somewhere around 488 million years ago something happened to cause a change in the fauna of the earth, heralding the beginning of the Ordovician Period. • Rather than one catastrophe, the late-Cambrian extinction seems to be a series of smaller extinction events. • Historically the change in fauna (mostly trilobites as the index species) was thought to be due to excessive warmth and low oxygen. • But some current findings point to an oxygen spike due perhaps to continental drift into the tropics, driving rapid speciation and consequent replacement of old with new organisms. 98 Welcome to the Ordovician YOU ARE HERE 99 The Ordovician Sea, 488 million years 100 ago The Ordovician Period lasted almost 45 million years, from 489 to 444 MYA. -
Jahrbuch Der Geologischen Bundesanstalt
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 2018 Band/Volume: 158 Autor(en)/Author(s): Schönlaub Hans-Peter Artikel/Article: Review of the Devonian/Carboniferous boundary in the Carnic Alps 29- 47 JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb. Geol. B.-A. ISSN 0016–7800 Band 158 Heft 1–4 S. 29–47 Wien, Dezember 2018 Review of the Devonian/Carboniferous boundary in the Carnic Alps HANS P. SCHÖNLAUB* 16 Text-Figures Österreichische Karte 1:50.000 Italy BMN / UTM Carnic Alps 197 Kötschach / NL 33-04-09 Oberdrauburg Devonian 197 Kötschach / NL 33-04-10 Kötschach-Mauthen Carboniferous Conodonts Hangenberg Crisis Contents Abstract ................................................................................................ 29 Zusammenfassung ........................................................................................ 30 Current knowledge ........................................................................................ 30 Review of sedimentary and tectonic history ..................................................................... 32 Important stratigraphic markers .............................................................................. 32 Middle and Upper Ordovician ............................................................................. 32 Silurian .............................................................................................. 32 Devonian............................................................................................ -
Doctor Who and the Creation of a Non-Gendered Hero Archetype
Illinois State University ISU ReD: Research and eData Theses and Dissertations 10-13-2014 Doctor Who and the Creation of a Non-Gendered Hero Archetype Alessandra J. Pelusi Illinois State University, [email protected] Follow this and additional works at: https://ir.library.illinoisstate.edu/etd Part of the Feminist, Gender, and Sexuality Studies Commons, Film and Media Studies Commons, and the Mass Communication Commons Recommended Citation Pelusi, Alessandra J., "Doctor Who and the Creation of a Non-Gendered Hero Archetype" (2014). Theses and Dissertations. 272. https://ir.library.illinoisstate.edu/etd/272 This Thesis is brought to you for free and open access by ISU ReD: Research and eData. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of ISU ReD: Research and eData. For more information, please contact [email protected]. DOCTOR WHO AND THE CREATION OF A NON-GENDERED HERO ARCHETYPE Alessandra J. Pelusi 85 Pages December 2014 This thesis investigates the ways in which the television program Doctor Who forges a new, non-gendered, hero archetype from the amalgamation of its main characters. In order to demonstrate how this is achieved, I begin with reviewing some of the significant and relevant characters that contribute to this. I then examine the ways in which female and male characters are represented in Doctor Who, including who they are, their relationship with the Doctor, and what major narrative roles they play. I follow this with a discussion of the significance of the companion, including their status as equal to the Doctor. From there, I explore the ways in which the program utilizes existing archetypes by subverting them and disrupting the status quo. -
Doctor Who and the Sea-Devils Ebook, Epub
DOCTOR WHO AND THE SEA-DEVILS PDF, EPUB, EBOOK Malcolm Hulke,Geoffrey Beevers | 1 pages | 01 Apr 2014 | BBC Audio, A Division Of Random House | 9781445824673 | English | London, United Kingdom Doctor Who and the Sea-Devils PDF Book Alternate Versions. Crazy Credits. They could communicate using a form of sound-based telepathy and could use this ability as a weapon by producing a deadly sonic scream. The planet Mondas had lifeforms identical to Sea Devils. Curious, he investigates a sea fortress, where he and Jo are attacked by a sea-adapted bipedal reptile, called a Sea Devil by one witness. Outpost Gallifrey. Doctor Who Live. Telegraphist Bowman Brian Justice Another subspecies of Sea Devil, suggested by the Twelfth Doctor to be a "warrior-class", were larger, faster, and stronger than those that he was familiar with. The Doctor determines to descend in a diving bell to try to make contact with the reptiles. Contrary to common belief, season 10 kicked off in the last week of December — not in , as would be expected. They used terraforming technology to create an earthquake which separated the peninsula from the main land. Season 14 : - Episode Endings The Doctor and Jo head for the sea fort to investigate further. This was the first time stories were produced out of transmission order. Categories :. Scream of the Shalka. Why is the submarine hi-jacked? Commander Mitchell - David Griffin Lt. The Sea Devils infiltrated the school and village on the island by turning the humans into Sea Devils. The interest and quality levels never drop below 9. -
A Lungfish Survivor of the End-Devonian Extinction and an Early Carboniferous Dipnoan
1 A Lungfish survivor of the end-Devonian extinction and an Early Carboniferous dipnoan 2 radiation. 3 4 Tom J. Challands1*, Timothy R. Smithson,2 Jennifer A. Clack2, Carys E. Bennett3, John E. A. 5 Marshall4, Sarah M. Wallace-Johnson5, Henrietta Hill2 6 7 1School of Geosciences, University of Edinburgh, Grant Institute, James Hutton Road, Edinburgh, 8 EH9 3FE, UK. email: [email protected]; tel: +44 (0) 131 650 4849 9 10 2University Museum of Zoology Cambridge, Downing Street, Cambridge CB2 3EJ, UK. 11 12 3Department of Geology, University of Leicester, Leicester LE1 7RH, UK. 13 14 4School of Ocean & Earth Science, University of Southampton, National Oceanography Centre, 15 European Way, University Road, Southampton, SO14 3ZH , UK. 16 17 5Sedgwick Museum, Department of Earth Sciences, University of Cambridge, Downing St., 18 Cambridge CB2 3EQ, UK 1 19 Abstract 20 21 Until recently the immediate aftermath of the Hangenberg event of the Famennian Stage (Upper 22 Devonian) was considered to have decimated sarcopterygian groups, including lungfish, with only 23 two taxa, Occludus romeri and Sagenodus spp., being unequivocally recorded from rocks of 24 Tournaisian age (Mississippian, Early Carboniferous). Recent discoveries of numerous 25 morphologically diverse lungfish tooth plates from southern Scotland and northern England indicate 26 that at least ten dipnoan taxa existed during the earliest Carboniferous. Of these taxa, only two, 27 Xylognathus and Ballgadus, preserve cranial and post-cranial skeletal elements that are yet to be 28 described. Here we present a description of the skull of a new genus and species of lungfish, 29 Limanichthys fraseri gen. -
Proterozoic Paleozoic Cambrian Ordovician Silurian Devonian
Approximate location of Burley No. 1 well Seismic Stratigraphic Extensional and Thrust Age West Formation or Group Name East Lithology Packages Orogenic Events Sheets Perm. Lower Upper Post-Pottsville rocks, undivided Pottsville Group and Middle post-Pottsville rocks Alleghanian orogeny Penn. Lower Pottsville Group Upper Greenbrier Limestone and Mauch Chunk Group Greenbrier Limestone Miss. Lower Berea Sandstone, Sunbury Shale, and Price Formation Venango Group Venango Group (Formation) Hampshire Formation and Riceville Formation Chagrin Shale Bradford Group Bradford Group Huron Mbr. of Greenland Gap Group the Ohio Shale Upper Salina sheet Acadian orogeny Java Formation Angola Shale Member Devonian West Falls Elk Group Formation Rhinestreet Shale Member Brallier Formation Elk Group Sonyea Formation Genesee Formation Harrell Shale Middle Tully Limestone, Hamilton Group, Marcellus Shale, and Onondaga Limestone Hamilton Group Lower Oriskany Sandstone and Helderberg Group Upper Salina Group (includes salt beds) Salina Group, Tonoloway Limestone, and Wills Creek Formation and Wills Creek Formation Salina Group Paleozoic Lockport Dolomite and Keefer Sandstone McKenzie Limestone and Keefer Sandstone Silurian Rose Hill Formation Lower Reedsville- Tuscarora Sandstone Taconic orogeny Martinsburg Juniata Formation Juniata Formation sheet Oswego Sandstone Upper Reedsville Shale (Utica Shale at base) Reedsville Shale Trenton Limestone Trenton Limestone Black River Limestone Middle Ordovician Knox unconformity Beekmantown Group Beekmantown Group ? Passive continental Lower Rome- margin modified Waynesboro Upper sandstone member of the Copper Ridge Dolomite of the Knox Group by Rome trough sheet Upper extension Copper Ridge Dolomite of the Knox Group Knox Group and Middle pre-Knox rocks Conasauga Group and Rome Formation Cambrian Lower Autochthonous Grenvillian basement Grenvillian Grenvillian basement basement Proterozoic Figure 3.--Correlation chart of Paleozoic and Proterozoic rocks in the study area and associated thrust sheets. -
A Hiatus Obscures the Early Evolution of Modern Lineages of Bony Fishes
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2021 A Hiatus Obscures the Early Evolution of Modern Lineages of Bony Fishes Romano, Carlo Abstract: About half of all vertebrate species today are ray-finned fishes (Actinopterygii), and nearly all of them belong to the Neopterygii (modern ray-fins). The oldest unequivocal neopterygian fossils are known from the Early Triassic. They appear during a time when global fish faunas consisted of mostly cosmopolitan taxa, and contemporary bony fishes belonged mainly to non-neopterygian (“pale- opterygian”) lineages. In the Middle Triassic (Pelsonian substage and later), less than 10 myrs (million years) after the Permian-Triassic boundary mass extinction event (PTBME), neopterygians were already species-rich and trophically diverse, and bony fish faunas were more regionally differentiated compared to the Early Triassic. Still little is known about the early evolution of neopterygians leading up to this first diversity peak. A major factor limiting our understanding of this “Triassic revolution” isaninter- val marked by a very poor fossil record, overlapping with the Spathian (late Olenekian, Early Triassic), Aegean (Early Anisian, Middle Triassic), and Bithynian (early Middle Anisian) substages. Here, I review the fossil record of Early and Middle Triassic marine bony fishes (Actinistia and Actinopterygii) at the substage-level in order to evaluate the impact of this hiatus–named herein the Spathian–Bithynian gap (SBG)–on our understanding of their diversification after the largest mass extinction event of the past. I propose three hypotheses: 1) the SSBE hypothesis, suggesting that most of the Middle Triassic diver- sity appeared in the aftermath of the Smithian-Spathian boundary extinction (SSBE; 2 myrs after the PTBME), 2) the Pelsonian explosion hypothesis, which states that most of the Middle Triassic ichthyo- diversity is the result of a radiation event in the Pelsonian, and 3) the gradual replacement hypothesis, i.e.