Upper Ordovician Conodont Biostratigraphy and Revised Lithostratigraphy and Geological Map, Akpatok Island, Ungava Bay, Nunavut
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Conodonts in Ordovician Biostratigraphy
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Archivio istituzionale della ricerca - Università di Modena e Reggio Emilia 1 Conodonts in Ordovician biostratigraphy STIG M. BERGSTRÖM AND ANNALISA FERRETTI Conodonts in Ordovician biostratigraphy The long time interval after Pander’s (1856) original conodont study can in terms of Ordovician conodont biostratigraphic research be subdivided into three periods, namely the Pioneer Period (1856-1955), the Transition Period (1955-1971), and the Modern Period (1971-Recent). During the pre-1920s, the few published conodont investigations were restricted to Europe and North America and were not concerned about the potential use of conodonts as guide fossils. Although primarily of taxonomic nature, the pioneer studies by Branson & Mehl, Stauffer, and Furnish during the 1930s represent the beginning of the use of conodonts in Ordovician biostratigraphy. However, no formal zones were introduced until Lindström (1955) proposed four conodont zones in the Lower Ordovician of Sweden, which marks the end of the Pioneer Period. Because Lindström’s zone classification was not followed by similar work outside Baltoscandia, the time interval up to the late 1960s can be regarded as a Transition Period. A milestone symposium volume, entitled ‘Conodont Biostratigraphy’ and published in 1971, 2 summarized much new information on Ordovician conodont biostratigraphy and is taken as the beginning of the Modern Period of Ordovician conodont biostratigraphy. In this volume, the Baltoscandic Ordovician was subdivided into named conodont zones whereas the North American Ordovician succession was classified into a series of lettered or numbered Faunas. Although most of the latter did not receive zone names until 1984, this classification has been used widely in North America. -
Early Silurian Oceanic Episodes and Events
Journal of the Geological Society, London, Vol. 150, 1993, pp. 501-513, 3 figs. Printed in Northern Ireland Early Silurian oceanic episodes and events R. J. ALDRIDGE l, L. JEPPSSON 2 & K. J. DORNING 3 1Department of Geology, The University, Leicester LE1 7RH, UK 2Department of Historical Geology and Palaeontology, SiSlvegatan 13, S-223 62 Lund, Sweden 3pallab Research, 58 Robertson Road, Sheffield $6 5DX, UK Abstract: Biotic cycles in the early Silurian correlate broadly with postulated sea-level changes, but are better explained by a model that involves episodic changes in oceanic state. Primo episodes were characterized by cool high-latitude climates, cold oceanic bottom waters, and high nutrient supply which supported abundant and diverse planktonic communities. Secundo episodes were characterized by warmer high-latitude climates, salinity-dense oceanic bottom waters, low diversity planktonic communities, and carbonate formation in shallow waters. Extinction events occurred between primo and secundo episodes, with stepwise extinctions of taxa reflecting fluctuating conditions during the transition period. The pattern of turnover shown by conodont faunas, together with sedimentological information and data from other fossil groups, permit the identification of two cycles in the Llandovery to earliest Weniock interval. The episodes and events within these cycles are named: the Spirodden Secundo episode, the Jong Primo episode, the Sandvika event, the Malm#ykalven Secundo episode, the Snipklint Primo episode, and the lreviken event. Oceanic and climatic cyclicity is being increasingly semblages (Johnson et al. 1991b, p. 145). Using this recognized in the geological record, and linked to major and approach, they were able to detect four cycles within the minor sedimentological and biotic fluctuations. -
A New Species of the Conodont Genus Siphonodella Branson & Mehl
Estonian Journal of Earth Sciences, 2017, 66, 4, 188–192 https://doi.org/10.3176/earth.2017.15 A new species of the conodont genus Siphonodella Branson & Mehl (late Tournaisian) Andrey V. Zhuravlev Institute of Geology Komi SC, UrB RAS, Pervomayskaya 54, 167000 Syktyvkar, Russia; [email protected] Received 3 April 2017, accepted 6 June 2017, available online 16 October 2017 Abstract. A new upper Tournaisian (Lower Carboniferous) siphonodellid conodont species Siphonodella carinata n. sp. is described. The material comes from the shallow-water carbonate sediments of the Pechora Swell (Timan-Pechora region or NE of European Russia). The co-occurrence of conodonts Hindeodus cristulus (Youngquist & Miller), Bispathodus stabilis (Branson & Mehl) Morphotype 1, Polygnathus longiposticus Branson & Mehl and Pseudopolygnathus nodomarginatus (Branson) suggests the late Tournaisian (Lower Siphonodella crenulata Zone) age of the deposits. Morphologically the new species is similar to Siphonodella semichatovae Kononova & Lipnjagov and S. ludmilae Zhuravlev & Plotitsyn, but differs in possessing three rostral ridges at the late stages of ontogeny and Class III symmetry. The presence of the shallow-water siphonodellids Siphonodella bella Kononova & Migdisova and S. quasinuda Gagiev, Kononova & Pazuhin in the upper part of the Tournaisian is detected for the first time. Key words: Conodonta, new species, Siphonodella carinata n. sp., Lower Carboniferous, Tournaisian. INTRODUCTION platform and a wide pseudokeel or depressed keel at the aboral side of Pa elements. Traditionally species of the genus Siphonodella are used The shallow-water siphonodellids of the Chinese for biostratigraphy of the lower part of the Tournaisian branch appeared in the earliest Tournaisian and ranged (Sandberg et al. 1978; Ji 1985; Ji & Ziegler 1992; up to the late Tournaisian (Ji & Ziegler 1992). -
Conodont Stratigraphy of a Highly Tectonised Silurian-Devonian Section in the San Basilio Area (SE Sardinia, Italy)
Bollettino della Societa Paleontologica Italiana 40 (3), 2001 ISSN 0375-7633 Modena, Dicembre 2001 Conodont stratigraphy of a highly tectonised Silurian-Devonian section in the San Basilio area (SE Sardinia, Italy) Carlo CORRADINI F rancesco LEONE Alfredo Loi Enrico SERPAGLI Dipartimento del Museo di Paleobiologia Dipartimento di Scienze della Terra Dipartimento del Museo di Paleobiologia e dell'Orto Botanico Universita di Cagliari e dell'Orto Botanico Universidt di Modena e Reggio Emilia Universita di Modena e Reggio Emilia KEYWORDS- Conodonts, Biostratigraphy, Tectonics, Silurian, Devonian, SE Sardinia. ABSTRACT- Several conodont species belonging to five "late Silurian biozones (Ancoradella ploeckensis, Polygnathoides siluricus, Ozarkodina crispa, Ozarkodina remscheidensis, Oulodus elegans detortus) and four Early and Late Devonian biozones (delta, pesavis, kitabicus-excavatus and Late rhenana) allow a better interpretation of stratigraphy and tectonics of the San Basilio area in western Gerrei. Frasnian sediments are documented for the first time in SE Sardinia. RIASSUNTO- [Stratigrafia a conodonti di una sezione forremente tettonizzata di eta Siluriano-Devoniano nell'area di San Basilio (Sardegna SE)] - Grazie alla biostratigrafia a conodonti viene interpretata la complessa tettonica di una sezione nell'area di San Basilio (Sardegna sud-orientale) e viene ricostruita la successione originaria. Sono documentate cinque biozone a conodonti del Siluriano superiore (Ancoradella eioeckensis, Polygnathoides siluricus, Ozarkodina crispa, -
Atlantic Walrus Odobenus Rosmarus Rosmarus
COSEWIC Assessment and Update Status Report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada SPECIAL CONCERN 2006 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION ENDANGERED WILDLIFE DES ESPÈCES EN PÉRIL IN CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2006. COSEWIC assessment and update status report on the Atlantic walrus Odobenus rosmarus rosmarus in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. ix + 65 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous reports: COSEWIC 2000. COSEWIC assessment and status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vi + 23 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Richard, P. 1987. COSEWIC status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-23 pp. Production note: COSEWIC would like to acknowledge D.B. Stewart for writing the status report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada, prepared under contract with Environment Canada, overseen and edited by Andrew Trites, Co-chair, COSEWIC Marine Mammals Species Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: (819) 997-4991 / (819) 953-3215 Fax: (819) 994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Évaluation et Rapport de situation du COSEPAC sur la situation du morse de l'Atlantique (Odobenus rosmarus rosmarus) au Canada – Mise à jour. -
Annual Report of the Eastern Artic Marine Investigations for 1949
C ONF IDENT IA L FISHERIES RESEARCH BOARD OF CANADA ANNUAL REPORT OF EASTERN ARCTIC FISHERIES INVESTIGATION FOR 1949 OTTAWA DECEMBER , 1949. Eastern Arctic Fisheries Inv'estigation, 1949, The Cruise of the "CALANUS", 1949. M. J.Dunbar I. Introduction and Summary. The terms of reference of these investetions are (1) to study the physical and biological oceanography of the eastern arctic and (2) to discover, if possible, marine resources which may be developed by and for the native population, Results obtained in Ungava bay during the 1949 season are listed in Dr. Dunbar's report, under these headings: (1) a. Sections were made from Burwell to Akpatok, from Akpatok to Payne bay, and from Akpatok to the mouth of the Koksoak river. Salinities, temperatures and oxygen concentrations were measured (the salinities not yet determined at time of writing). The sections were made in mid-July and one section, that from Payne bay to Akpatok, was repeated late in August in order to show the changes during the summer months* b, Echo-sounder tracks were recorded and kept from regions in Ungava bay where soundings are very incomplete, c. The study of the biology and distribution of the plankton, benthos and littoral fauna was continued, by the addition to the already large collections (from 1947 and 1948) of material from deeper water and from other areas than were possible to reach in the first two seasons. An effort was also made to collect micro-organisms by centrifuging methods. d. Experimental fishing for codfish, shark and flatfish, by hand line and by long lino trawl was continued. -
Uria Lomvia) and Black-Legged Kittiwakes (Rissa Tridactyla
A First Count of Thick-billed Murres ( Uria lomvia ) and Black-legged Kittiwakes ( Rissa tridactyla ) Breeding on Bylot Island ANTHONY J. G ASTON 1, 4 , MARC -A NDRÉ CYR 2, and KIERAN O’D ONOVAN 3 1Science and Technology Branch, Environment and Climate Change Canada, Carleton University, Ottawa, Ontario K1A 0H3 Canada 2Canadian Wildlife Service, Environment and Climate Change Canada, Place Vincent Massey, 351 St. Joseph Boulevard, Gatineau, Quebec K1A 0H3 Canada 3308a Klukshu Avenue, Whitehorse, Yukon Y1A 3Y1 Canada 4Corresponding author: [email protected] Gaston, Anthony J., Marc-André Cyr, and Kieran O’Donovan. 2017. A first count of Thick-billed Murres ( Uria lomvia ) and Black-legged Kittiwakes ( Rissa tridactyla ) breeding on Bylot Island. Canadian Field-Naturalist 131(1): 69 –74. https:// doi.org/10.22621/cfn.v 131i 1.1953 Bylot Island, part of Sirmilik National Park, supports two major breeding colonies of intermingled Thick-billed Murres ( Uria lomvia ) and Black-legged Kittiwakes ( Rissa tridactyla ): at Cape Hay near the northwest tip and at Cape Graham Moore at the opposite end of the island. Although the size of these colonies has been estimated previously, there is no information on how the estimates were made, except for Thick-billed Murres at Cape Hay in 1977, when the numbers were based on sampling only about 30% of the colony. In 2013, high-resolution digital photographs of the whole area of both colonies were taken in July, when most birds were probably incubating eggs. Individual birds were counted on the photographs, and the numbers were corrected for image quality and converted to numbers of breeding pairs based on correction factors from another High Arctic colony. -
Qikiqtani Region Arctic Ocean
OVERVIEW 2017 NUNAVUT MINERAL EXPLORATION, MINING & GEOSCIENCE QIKIQTANI REGION ARCTIC OCEAN OCÉAN ARCTIQUE LEGEND Commodity (Number of Properties) Base Metals, Active (2) Mine, Active (1) Diamonds, Active (2) Quttinirpaaq NP Sanikiluaq Mine, Inactive (2) Gold, Active (1) Areas with Surface and/or Subsurface Restrictions 10 CPMA Caribou Protection Measures Apply ISLANDS Belcher MBS Migratory Bird Sanctuary NP National Park Nares Strait Islands NWA National Wildlife Area - ÉLISABETH Nansen TP Territorial Park WP Wildlife Preserve WS Wildlife Sanctuary Sound ELLESMERE ELIZABETHREINE ISLAND Inuit Owned Lands (Fee simple title) Kane Surface Only LA Agassiz Basin Surface and Subsurface Ice Cap QUEEN Geological Mapping Programs Canada-Nunavut Geoscience Office ÎLES DE Kalaallit Nunaat Boundaries Peary Channel Müller GREENLAND/GROENLAND NLCA1 Nunavut Settlement Area Ice CapAXEL Nunavut Regions HEIBERG ÎLE (DENMARK/DANEMARK) NILCA 2 Nunavik Settlement Area ISLAND James Bay WP Provincial / Territorial D'ELLESMERE James Bay Transportation Routes Massey Sound Twin Islands WS Milne Inlet Tote Road / Proposed Rail Line Hassel Sound Prince of Wales Proposed Steensby Inlet Rail Line Prince Ellef Ringnes Icefield Gustaf Adolf Amund Meliadine Road Island Proposed Nunavut to Manitoba Road Sea Ringnes Eureka Sound Akimiski 1 Akimiski I. NLCA The Nunavut Land Claims Agreement Island Island MBS 2 NILCA The Nunavik Inuit Land Claims Agreement Norwegian Bay Baie James Boatswain Bay MBS ISLANDSHazen Strait Belcher Channel Byam Martin Channel Penny S Grise Fiord -
Conodonts of the Estill Shale and Bisher Formation (Silurian, Southern Ohio): Biostratigraphy and Distribution1
78 M. A. LAMB AND R. L. LOWE Vol. 87 Conodonts of the Estill Shale and Bisher Formation (Silurian, Southern Ohio): Biostratigraphy and Distribution1 MARK A. KLEFFNER, Department of Geology and Mineralogy, The Ohio State University, Columbus, OH 43210 ABSTRACT. Representatives of 20 species of conodonts have been isolated from samples of the Silurian Estill Shale and Bisher Formation at four localities in southern Ohio. The Estill belongs in the amorphognathoides Zone and is late Llandoverian to early Wenlockian. The Estill-Bisher contact is an unconformity. In Adams and southern Highland counties, the Bisher belongs in the middle and upper ranuliformis Zone and is late early to possibly early middle Wenlockian; in northern Highland County the Bisher belongs in the lower ranuliformis Zone and is middle early to late early Wenlockian. The Estill was deposited in a gradually shoaling sea that regressed from Adams and Highland counties in the early Wenlockian. The sea transgressed south- ward across the two counties later in the early Wenlockian and deposited the Bisher in a shallow, subtidal environment. OHIO J. SCI. 87 (3): 78-89, 1987 INTRODUCTION Highland County, Ohio. North of Fleming County, Kentucky, an unconformity separates the Noland and The Estill Shale and overlying Bisher Formation make Estill (Rexroad and Kleffner 1984). up most of the lower Niagaran sequence (Silurian) in The Estill Shale consists predominantly of blue-green, Adams and Highland counties in southern Ohio. The gray-green, green, and brown shale. Shale beds are com- first, and only detailed, published report on conodonts monly blocky or massive in the lower part of the for- from either the Estill or Bisher was by Rexroad and mation and silty and fissile in the upper part. -
Information to Users
INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis arxi dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6" x 9" black and white photographic prints are available for any photographs or illustrations appearing In this copy for an additional charge. Contact UMI directly to order. Bell & Howell Information and Learning 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA 800-521-0600 UMI NOTE TO USERS This reproduction is the best copy available. UMI Stratigraphy, Conodont Taxonomy and Biostratigraphy of Upper Cambrian to Lower Silurian Platform to Basin Facies, Northern British Columbia by Leanne Pyle B. Sc., University of Saskatchewan, 1994 A Dissertation Submitted in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY in the School of Earth and Ocean Sciences We accept this dissertation as conforming to the required standard , Supervisor (School of Earth and Ocean Sciences) Dr. -
Canada Topographical
University of Waikato Library: Map Collection Canada: topographical maps 1: 250,000 The Map Collection of the University of Waikato Library contains a comprehensive collection of maps from around the world with detailed coverage of New Zealand and the Pacific : Editions are first unless stated. These maps are held in storage on Level 1 Please ask a librarian if you would like to use one: Coverage of Canadian Provinces Province Covered by sectors On pages Alberta 72-74 and 82-84 pp. 14, 16 British Columbia 82-83, 92-94, 102-104 and 114 pp. 16-20 Manitoba 52-54 and 62-64 pp. 10, 12 New Brunswick 21 and 22 p. 3 Newfoundland and Labrador 01-02, 11, 13-14 and 23-25) pp. 1-4 Northwest Territories 65-66, 75-79, 85-89, 95-99 and 105-107) pp. 12-21 Nova Scotia 11 and 20-210) pp. 2-3 Nunavut 15-16, 25-27, 29, 35-39, 45-49, 55-59, 65-69, 76-79, pp. 3-7, 9-13, 86-87, 120, 340 and 560 15, 21 Ontario 30-32, 40-44 and 52-54 pp. 5, 6, 8-10 Prince Edward Island 11 and 21 p. 2 Quebec 11-14, 21-25 and 31-35 pp. 2-7 Saskatchewan 62-63 and 72-74 pp. 12, 14 Yukon 95,105-106 and 115-117 pp. 18, 20-21 The sector numbers begin in the southeast of Canada: They proceed west and north. 001 Newfoundland 001K Trepassey 3rd ed. 1989 001L St: Lawrence 4th ed. 1989 001M Belleoram 3rd ed. -
ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh. Geol. B.-A. ISSN 0016–7800 ISBN 3-85316-02-6 Band 54 S. 181–199 Wien, Oktober 1999 North Gondwana: Mid-Paleozoic Terranes, Stratigraphy and Biota Editors: R. Feist, J.A. Talent & A. Daurer Early Silurian Conodonts from the Quinton Formation of the Broken River Region (North-Eastern Australia) ANDREW SIMPSON*) 4 Text-Figures and 2 Plates Australia Queensland Silurian Conodonts Stratigraphy Contents Zusammenfassung ...................................................................................................... 181 Abstract ................................................................................................................. 181 1. Introduction ............................................................................................................. 182 2. Geology ................................................................................................................. 182 3. Biostratigraphic Summary ............................................................................................... 183 4. Revision of Stratigraphic Nomenclature ................................................................................... 183 5. Age of Quinton Formation Carbonates .................................................................................... 184 5.1. Top Hut Limestone .................................................................................................. 184 5.2. Tomcat Creek Limestone