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A Brief History of Christ Church MEDIEVAL PERIOD
A Brief History of Christ Church MEDIEVAL PERIOD Christ Church was founded in 1546, and there had been a college here since 1525, but prior to the Dissolution of the monasteries, the site was occupied by a priory dedicated to the memory of St Frideswide, the patron saint of both university and city. St Frideswide, a noble Saxon lady, founded a nunnery for herself as head and for twelve more noble virgin ladies sometime towards the end of the seventh century. She was, however, pursued by Algar, prince of Leicester, for her hand in marriage. She refused his frequent approaches which became more and more desperate. Frideswide and her ladies, forewarned miraculously of yet another attempt by Algar, fled up river to hide. She stayed away some years, settling at Binsey, where she performed healing miracles. On returning to Oxford, Frideswide found that Algar was as persistent as ever, laying siege to the town in order to capture his bride. Frideswide called down blindness on Algar who eventually repented of his ways, and left Frideswide to her devotions. Frideswide died in about 737, and was canonised in 1480. Long before this, though, pilgrims came to her shrine in the priory church which was now populated by Augustinian canons. Nothing remains of Frideswide’s nunnery, and little - just a few stones - of the Saxon church but the cathedral and the buildings around the cloister are the oldest on the site. Her story is pictured in cartoon form by Burne-Jones in one of the windows in the cathedral. One of the gifts made to the priory was the meadow between Christ Church and the Thames and Cherwell rivers; Lady Montacute gave the land to maintain her chantry which lay in the Lady Chapel close to St Frideswide’s shrine. -
PROGRAMME ABSTRACTS AGM Papers
The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia, Spain PROGRAMME ABSTRACTS AGM papers Palaeontological Association 6 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia The programme and abstracts for the 63rd Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. An easy-to-navigate pocket guide to the Meeting is also available to delegates. Venue The Annual Meeting will take place in the faculties of Philosophy and Philology on the Blasco Ibañez Campus of the University of Valencia. The Symposium will take place in the Salon Actos Manuel Sanchis Guarner in the Faculty of Philology. The main meeting will take place in this and a nearby lecture theatre (Salon Actos, Faculty of Philosophy). There is a Metro stop just a few metres from the campus that connects with the centre of the city in 5-10 minutes (Line 3-Facultats). Alternatively, the campus is a 20-25 minute walk from the ‘old town’. Registration Registration will be possible before and during the Symposium at the entrance to the Salon Actos in the Faculty of Philosophy. During the main meeting the registration desk will continue to be available in the Faculty of Philosophy. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. It is therefore expected that you prepare to speak for no more than 12 minutes to allow time for questions and switching between presenters. We have a number of parallel sessions in nearby lecture theatres so timing will be especially important. -
Lee-Riding-2018.Pdf
Earth-Science Reviews 181 (2018) 98–121 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Marine oxygenation, lithistid sponges, and the early history of Paleozoic T skeletal reefs ⁎ Jeong-Hyun Leea, , Robert Ridingb a Department of Geology and Earth Environmental Sciences, Chungnam National University, Daejeon 34134, Republic of Korea b Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996, USA ARTICLE INFO ABSTRACT Keywords: Microbial carbonates were major components of early Paleozoic reefs until coral-stromatoporoid-bryozoan reefs Cambrian appeared in the mid-Ordovician. Microbial reefs were augmented by archaeocyath sponges for ~15 Myr in the Reef gap early Cambrian, by lithistid sponges for the remaining ~25 Myr of the Cambrian, and then by lithistid, calathiid Dysoxia and pulchrilaminid sponges for the first ~25 Myr of the Ordovician. The factors responsible for mid–late Hypoxia Cambrian microbial-lithistid sponge reef dominance remain unclear. Although oxygen increase appears to have Lithistid sponge-microbial reef significantly contributed to the early Cambrian ‘Explosion’ of marine animal life, it was followed by a prolonged period dominated by ‘greenhouse’ conditions, as sea-level rose and CO2 increased. The mid–late Cambrian was unusually warm, and these elevated temperatures can be expected to have lowered oxygen solubility, and to have promoted widespread thermal stratification resulting in marine dysoxia and hypoxia. Greenhouse condi- tions would also have stimulated carbonate platform development, locally further limiting shallow-water cir- culation. Low marine oxygenation has been linked to episodic extinctions of phytoplankton, trilobites and other metazoans during the mid–late Cambrian. -
Abstract Volume
https://doi.org/10.3301/ABSGI.2019.04 Milano, 2-5 July 2019 ABSTRACT BOOK a cura della Società Geologica Italiana 3rd International Congress on Stratigraphy GENERAL CHAIRS Marco Balini, Università di Milano, Italy Elisabetta Erba, Università di Milano, Italy - past President Società Geologica Italiana 2015-2017 SCIENTIFIC COMMITTEE Adele Bertini, Peter Brack, William Cavazza, Mauro Coltorti, Piero Di Stefano, Annalisa Ferretti, Stanley C. Finney, Fabio Florindo, Fabrizio Galluzzo, Piero Gianolla, David A.T. Harper, Martin J. Head, Thijs van Kolfschoten, Maria Marino, Simonetta Monechi, Giovanni Monegato, Maria Rose Petrizzo, Claudia Principe, Isabella Raffi, Lorenzo Rook ORGANIZING COMMITTEE The Organizing Committee is composed by members of the Department of Earth Sciences “Ardito Desio” and of the Società Geologica Italiana Lucia Angiolini, Cinzia Bottini, Bernardo Carmina, Domenico Cosentino, Fabrizio Felletti, Daniela Germani, Fabio M. Petti, Alessandro Zuccari FIELD TRIP COMMITTEE Fabrizio Berra, Mattia Marini, Maria Letizia Pampaloni, Marcello Tropeano ABSTRACT BOOK EDITORS Fabio M. Petti, Giulia Innamorati, Bernardo Carmina, Daniela Germani Papers, data, figures, maps and any other material published are covered by the copyright own by the Società Geologica Italiana. DISCLAIMER: The Società Geologica Italiana, the Editors are not responsible for the ideas, opinions, and contents of the papers published; the authors of each paper are responsible for the ideas opinions and con- tents published. La Società Geologica Italiana, i curatori scientifici non sono responsabili delle opinioni espresse e delle affermazioni pubblicate negli articoli: l’autore/i è/sono il/i solo/i responsabile/i. ST3.2 Cambrian stratigraphy, events and geochronology Conveners and Chairpersons Per Ahlberg (Lund University, Sweden) Loren E. -
Version 4.Cdr
THE GEOMAGNETIC POLARITY TIME SCALE FOR EARY PALEOZOIC: DATA AND SYNTHESE 1 2 1 Vladimir Pavlov and Yves Gallet 2 Institute of Physics of the Earth, Institut de Physique Russian Academy of Sciences INTRODUCTION EARLY CAMBRIAN: Kirschvink and LONG STANDING CONROVERSY: Constructing the Geomagnetic Polarity Time Scale (GPTS) through the geological history is of crucial importance to address Rozanov, 1984 TWO PRIMARY POLES FOR ONE SIBERIAN PLATFORM? several major issues in Earth sciences, as for instance the long-term evolution of the geodynamo. The GPTS is also an Khramov et al., 1982 important chronological tool allowing one to decipher the age and duration of various geological processes. Moreover, GPTS 509 Ma is widely used in prospecting for commercial minerals and in petroleum geology Kirschvink’s direction OR Khramov’s direction? Series Regiostage . N N The chronology of the geomagnetic polarity reversals since the Upper Jurassic is rather well known thanks to the magnetic Kirschvink and Pisarevsky anomalies recorded in the sea floor. For more ancient epochs our knowledge of the GPTS is still very fragmentary and much Rozanov, 1984 et al., 1997 more uncertain. However significant information has been obtained for several time intervals, in particular for the Triassic and the beginning of the Phanerozoic. Hirnantian Khondelen We will focus our presentation on recent developments made in the determination of the GPTS during the Early Paleozoic P-T Botoma - Toyon Botoma - Botoma - Toyon Botoma - 516 Ma (Siberia) (Cambrian and Ordovician). Siberian APWP Ashgill Epoch 2 Epoch 2 D3-C1 экватор E30° Е90° Е150° Botmoynak Dolborian (Tianshan) Late Ediacarian - Hyperactivity of the Earth magnetic field? Early Cambrian Kirschvink’s pole Early Cambrian O2-O3 Cm3-O1 Khramov’s pole S30° Moyero N Cm2 N N Low (very low?) reversal frequency (Siberia) Pavlov et al., Pavlov et al., 2018 S60° unpubl. -
No Late Cambrian Shoreline Ice in Laurentia
Comment & Reply COMMENTS AND REPLIES Minnesota clasts; Runkel et al., 2010), or early cement may remain GSA Today soft after burial and be deformed. After burial, the soft clasts Online: , Comments and Replies could be burrowed by trace producers. Published Online: April 2011 Runkel et al. (2010) note that the Jordan sandstone is essentially uncemented with loss of an original cement. Unknown cement/ matrix composition (carbonate/evaporitic, cyanobacterial binding?) make conclusions of ice cementation and cold climate speculative. Without evidence for grounded ice after the Early Cambrian (Landing and MacGabhann, 2010) and subsequent very high No Late Cambrian shoreline ice eustatic levels (Landing, 2007b), the Late Cambrian ocean likely lacked cold water and a thermocline (Landing, 2007b). Thus, an in Laurentia interpretation of Middle–Late Cambrian extinctions by cold water onlap (Runkel et al., 2010) is unlikely; the role of strong regressive- Ed Landing, New York State Museum, 222 Madison Avenue, transgressive couplets and transgressive low oxygen masses Albany, New York, 12230, USA; [email protected] should be considered (e.g., Hallam and Wignall, 1999; Zhuravlev and Wood, 1996). The appearance of marginal trilobites (likely dysoxia adapted) after Cambrian extinctions should be compared Runkel et al. (2010) propose that Late Cambrian cooling led to Cretaceous faunal replacements at non-glacial times with onlap to shoreline ice development in the upper Mississippi River of hypoxic slope water onto platforms (e.g., Jenkyns, 1991). valley. This cooling then led to latest Cambrian biotic turnover and onset of the Ordovician Diversification. (“Lower”/“Early,” Extinction at the Cordylodus proavus (conodont) Zone base is “Middle”/“Middle,” and “Upper”/“Upper” Cambrian are proposed not the onset of the Ordovician Radiation (i.e., Runkel et al., 2010). -
Concordia Theological Monthly
CONCORDIA THEOLOGICAL MONTHLY The Crisis of Theological Historicism and How It May Be Overcome WILHELM MUNDLE Bible Study in the Life of the Church OSCAR E. FEUCHT The Devotional Use of the Bible ' JAMES G. MANZ Homiletics Theological Observer Book Review VOL. xxxm July 1962 No.7 BOOK REVIE\X/ All books 'reviewed in this periodical may be procured from 01' through Concordia Pub lishing House, 3558 South Jefferson Avenue, St. Louis 18, Missouri. THE EV. LUTHERAN CHURCH OF preacher to whom I can take my personal NIGERIA, 1936-1961. By Paul M. problems." Most preachers will find a new Volz. Calabar, Nigeria: Hope Waddell perspective and inspiration for preaching in Press, 1961. Paper. 80 pages. Price not this volume. Some of Jackson's points will given. irritate the Lutheran pastor. All in all, how If is a pleasure to receive this honest and ever, it would be salutary for every preacher straightforward history of the Evangelical to meet the issues raised in this book. Lutheran Church of Nigeria from its be KENNETH H. BREIMEIER ginnings until the present. Full credit is given to the foundations laid by others, THE CARE AND FEEDING OF MINIS notably the Qua Iboe Mission, and the nat TERS. By Kathleen Neill Nyberg. New rad. _ poin.. Jut that the prime desire of York: 1 .. 19do ress, 1.961. 141 pages. the Ibesikpo people was for education and Cloth. $2.50. therefore a teaching church. This book, "from the wife's point of The churches in Nigeria and elsewhere view," is written with exceptional skill and are in Paul Volz's debt for this factual common sense. -
Ediacaran and Cambrian Stratigraphy in Estonia: an Updated Review
Estonian Journal of Earth Sciences, 2017, 66, 3, 152–160 https://doi.org/10.3176/earth.2017.12 Ediacaran and Cambrian stratigraphy in Estonia: an updated review Tõnu Meidla Department of Geology, Institute of Ecology and Earth Sciences, Faculty of Science and Technology, University of Tartu, Ravila 14a, 50411 Tartu, Estonia; [email protected] Received 18 December 2015, accepted 18 May 2017, available online 6 July 2017 Abstract. Previous late Precambrian and Cambrian correlation charts of Estonia, summarizing the regional stratigraphic nomenclature of the 20th century, date back to 1997. The main aim of this review is updating these charts based on recent advances in the global Precambrian and Cambrian stratigraphy and new data from regions adjacent to Estonia. The term ‘Ediacaran’ is introduced for the latest Precambrian succession in Estonia to replace the formerly used ‘Vendian’. Correlation with the dated sections in adjacent areas suggests that only the latest 7–10 Ma of the Ediacaran is represented in the Estonian succession. The gap between the Ediacaran and Cambrian may be rather substantial. The global fourfold subdivision of the Cambrian System is introduced for Estonia. The lower boundary of Series 2 is drawn at the base of the Sõru Formation and the base of Series 3 slightly above the former lower boundary of the ‘Middle Cambrian’ in the Baltic region, marked by a gap in the Estonian succession. The base of the Furongian is located near the base of the Petseri Formation. Key words: Ediacaran, Cambrian, correlation chart, biozonation, regional stratigraphy, Estonia, East European Craton. INTRODUCTION The latest stratigraphic chart of the Cambrian System in Estonia (Mens & Pirrus 1997b, p. -
The Natural History of Pikes Peak State Park, Clayton County, Iowa ______
THE NATURAL HISTORY OF PIKES PEAK STATE PARK, CLAYTON COUNTY, IOWA ___________________________________________________ edited by Raymond R. Anderson Geological Society of Iowa ______________________________________ November 4, 2000 Guidebook 70 Cover photograph: Photograph of a portion of the boardwalk trail near Bridal Veil Falls in Pikes Peak State Park. The water falls over a ledge of dolomite in the McGregor Member of the Platteville Formation that casts the dark shadow in the center of the photo. THE NATURAL HISTORY OF PIKES PEAK STATE PARK CLAYTON COUNTY, IOWA Edited by: Raymond R. Anderson and Bill J. Bunker Iowa Department Natural Resources Geological Survey Bureau Iowa City, Iowa 52242-1319 with contributions by: Kim Bogenschutz William Green John Pearson Iowa Dept. Natural Resources Office of the State Archaeologist Parks, Rec. & Preserves Division Wildlife Research Station 700 Clinton Street Building Iowa Dept. Natural Resources 1436 255th Street Iowa City IA 52242-1030 Des Moines, IA 50319 Boone, IA 50036 Richard Langel Chris Schneider Scott Carpenter Iowa Dept. Natural Resources Dept. of Geological Sciences Department of Geoscience Geological Survey Bureau Univ. of Texas at Austin The University of Iowa Iowa City, IA 52242-1319 Austin, TX 78712 Iowa City, IA 52242-1379 John Lindell Elizabeth Smith Norlene Emerson U.S. Fish & Wildlife Service Department of Geosciences Dept. of Geology & Geophysics Upper Mississippi Refuge University of Massachusetts University of Wisconsin- Madison McGregor District Office Amherst, MA 01003 Madison WI 53706 McGregor, IA 52157 Stephanie Tassier-Surine Jim Farnsworth Greg A. Ludvigson Iowa Dept. Natural Resources Parks, Rec. & Preserves Division Iowa Dept. Natural Resources Geological Survey Bureau Iowa Dept. -
Subcommission on Cambrian Stratigraphy
International Commission on Stratigraphy Subcommission on Cambrian Stratigraphy ANNUAL REPORT 2020 1. TITLE OF CONSTITUENT BODY International Subcommission on Cambrian Stratigraphy Prepared by: Dr. Anna ŻYLIŃSKA, Secretary, [email protected] Prof. Per AHLBERG, Chair, [email protected] Prof. Loren E. BABCOCK, Chair 2016–2020, [email protected]. Date: 22 November 2020 2. OVERALL OBJECTIVES AND FIT WITHIN IUGS SCIENCE POLICY 2.a. Mission Statement The Subcommission is the primary body for facilitation of international communication and scientific cooperation on Cambrian stratigraphy. 2.b. Goals The two principal goals of the Subcommission are: 1) To develop a global stage-level and series-level chronostratigraphic classification of the Cambrian System. 2) To complete and publish regional and global correlation charts for the Cambrian System. 2.c. Fit within IUGS Science Policy The objectives of the Subcommission fall within three main areas of IUGS policy: 1) The development of an internationally agreed scale of chronostratigraphic units, fully defined by GSSPs where appropriate (stages and series), and related to a hierarchy of units (zones) to maximize relative time resolution within the Cambrian Period. 2) Establishment of frameworks and systems to encourage international collaboration in understanding the evolution of the Earth during the Cambrian Period. 3) Working towards an international policy concerning conservation of geologically and paleontologically important sites such as GSSPs and Fossil-Lagerstätten. 3. ORGANISATION 3.a. Interface with other international projects/groups The Cambrian Subcommission is involved jointly with the Ordovician Subcommission in IGCP Project 653: The onset of the Great Ordovician Biodiversification Event. The Cambrian Subcommission is working jointly with the Ediacaran Subcommission on restudy of the Cambrian base. -
An Annotated Select Bibliography of the Piltdown Forgery
An annotated select bibliography of the Piltdown forgery Informatics Programme Open Report OR/13/047 BRITISH GEOLOGICAL SURVEY INFORMATICS PROGRAMME OPEN REPORT OR/13/47 An annotated select bibliography of the Piltdown forgery Compiled by David G. Bate Keywords Bibliography; Piltdown Man; Eoanthropus dawsoni; Sussex. Map Sheet 319, 1:50 000 scale, Lewes Front cover Hypothetical construction of the head of Piltdown Man, Illustrated London News, 28 December 1912. Bibliographical reference BATE, D. G. 2014. An annotated select bibliography of the Piltdown forgery. British Geological Survey Open Report, OR/13/47, iv,129 pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. © NERC 2014. All rights reserved Keyworth, Nottingham British Geological Survey 2014 BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS shops at British Geological Survey offices Nottingham, Edinburgh, London and Cardiff (Welsh publications only) see contact details below or shop online at www. geologyshop.com BGS Central Enquiries Desk Tel 0115 936 3143 Fax 0115 936 3276 The London Information Office also maintains a reference collection of BGS publications, including maps, for consultation. email [email protected] We publish an annual catalogue of our maps and other publications; this catalogue is available online or from any of the Environmental Science Centre, Keyworth, Nottingham BGS shops. -
WITSML Lithology Object Usage Guide
WITSML Lithology Element Usage Guide For WITSML Version 1.4.1 WITSML The Wellsite Information Transfer Standard Mark-up Language (WITSML) consists of XML data-object Overview definitions and a Web services specification developed to promote the right-time, seamless flow of well data between operators and service companies to speed and enhance decision making. Version: Version 1.01 Abstract This document is a guide for implementing and using the lithology element of the mudLog data-object. This lithology element was significantly modified and released as part of WITSML v1.4.1. Prepared by: WITSML SIG Lithology Sub-team Date published: 18 November 2011 Minor revisions January 2012 Document type: Usage Guide Keywords: Data exchange standard, lithology, data, information, qualifier, matrix cement WITSML Lithology Element Usage Guide Document Information DOCUMENT VERSION: 1.01 DATE: January 2012 Technical Language US English Usage, Intellectual Property Rights, and Copyright The material described in this document was developed by and is the intellectual property of Energistics. Energistics develops material for open, public use so that the material is accessible and can be of maximum value to everyone. Use of the material in this document is governed by the Energistics Intellectual Property Policy document and the Product Licensing Agreement, both of which can be found on the Energistics website, http://www.energistics.org/legal-policies. All Energistics published materials are freely available for public comment and use. Anyone may copy and share the materials but must always acknowledge Energistics as the source. No one may restrict use or dissemination of Energistics materials in any way.