WOGOGOB 2007. 9Th Meeting of the Working Group on Ordovician

Total Page:16

File Type:pdf, Size:1020Kb

WOGOGOB 2007. 9Th Meeting of the Working Group on Ordovician SGURapporter och meddelanden 128 Rapporter och meddelanden 128 WOGOGOB 2007 9th meeting of the Working Group on Ordovician Geology of Baltoscandia Field guide and Abstracts Jan Ove Ebbestad, Linda Wickström & Anette Högström (eds.) WOGOGOB2007 9th– meeting the of Working Groupon Ordovician Geology Baltoscandia of Rapporter och meddelanden 128 WOGOGOB 2007 9th meeting of the Working Group on Ordovician Geology of Baltoscandia IGCP503 Ordovician Palaeogeography and Palaeoclimate Regional Meeting 2007 August 17th–20st, Rättvik, Sweden Field guide and Abstracts Jan Ove R. Ebbestad, Linda M. Wickström & Anette E.S. Högström (eds.) Sveriges geologiska undersökning 2007 ISSN 0349­2176 ISBN 978­91­7158­788­6 Cover photo: Composite photo showing (upper part, photo by J.O.R. Ebbestad) the east flank of the Osmundsberget quarry in the Siljan District, Dalarna with the Kullsberg Limestone to the right, followed by transition beds of the Fjäcka Shale equivalent, and the flank facies Boda Limestone to the left; (lower part, photo by L.M. Wickström), river section at Sladderforsen, River Långan, with folded and thrusted beds of ramp facies sediments (Isön Limestone). WOGOGOB 2007 logo: The design follows the WOGOGOB 2004 layout, with the text and trilobite motif added by J.O.R. Ebbestad. The outline represents the cranidium of the trilobiteTetralichas planifrons (Ange­ lin, 1854) from the Katian Kullsberg Limestone in the Siljan District, Dalarna, Sweden. © Sveriges geologiska undersökning Layout: Jeanette Bergman Weihed, SGU Tryck: Elanders Tofters, Östervåla 2007 Contents Preface ............................................................................................................................................................... 5 WOGOGOB – How it began ................................................................................................................................ 6 Maurits Lindström Ordovician of the Siljan District, Sweden......................................................................................................... 7 Jan Ove R. Ebbestad & Anette E.S. Högström Structural setting ........................................................................................................................................................ 7 Earliest history of research ........................................................................................................................................ 7 The stratigraphic succession...................................................................................................................................... 9 The Ordovician conodont biostratigraphy in the Siljan region, south-central Sweden: a brief review of an international reference standard .............................. 26 Stig M. Bergström Previous conodont studies in the Siljan region ................................................................................................... .28 Conodont biostratigraphy in upper Darriwilian–Hirnantian sections ......................................................... .30 13 Relations to δ C chemostratigraphy .................................................................................................................... .39 Concluding remarks ................................................................................................................................................. .41 Ordovician of the Storsjön Area ...................................................................................................................... 41 Linda M. Wickström Previous work ............................................................................................................................................................ 41 Geological setting .................................................................................................................................................... 42 Faunas ................................................................................................................................................................... 43 The Lockne crater .................................................................................................................................................. 45 Maurits Lindström Stratigraphic succession ..................................................................................................................................... 49 Linda M. Wickström, Åsa M. Frisk & Maurits Lindström Locality descriptions, the Siljan District ........................................................................................................ 52 Jan Ove R. Ebbestad & Anette E.S. Högström Stop 1. Amtjärn quarry ............................................................................................................................................ 52 Stop 2. “Fjäckan” ..................................................................................................................................................... 54 Stop 3. Osmundsberget .......................................................................................................................................... 54 Stop 4. Solberga ....................................................................................................................................................... 57 Stop 5. Jutjärn .......................................................................................................................................................... 58 Locality descriptions, the Storsjön Area ....................................................................................................... 58 Linda M. Wickström, Åsa M. Frisk & Peter Dahlqvist Stop 6. Lockne crater (crater trail) ........................................................................................................................ 58 Stop 7. Brunflo area................................................................................................................................................. 60 Stop 8. Rannåsen ..................................................................................................................................................... 60 Stop 9 Österulvsås, Kälom ...................................................................................................................................... 61 Acknowledgements ............................................................................................................................................. 62 Contact details of contributing authors (in alphabetical order) .......................................................... 63 References ............................................................................................................................................................. 63 Abstracts ............................................................................................................................................................. 79 The organizing committee warmly thanks the following: Preface Last year WOGOGOB (WOrking Group on Ordovician Geology of Baltoscandia) turned 20 years, and the 9th meeting this year in Rättvik in the Siljan District celebrates this occasion. WOGOGOB was instigated by Maurits Lindström in 1986, and the history is chronicled briefly below. The meeting has over the years developed into one of the more important forums for integrated Baltoscandian research and collaboration, along with The Baltic Stratigraphic Conference and Lundadagarna. WOGOGOB 2007 is a field meeting, with excursions in the Siljan District and the Östersund area. The reason behind the choice of Rättvik and Östersund as the place for this gathering is twofold. Firstly the Sil­ jan District has a central place in Ordovician geology of Baltoscandia and indeed world wide. We are here thinking of reference sections for units in Sweden, standard conodont zones and even global palaeoclimate changes (e.g. the Boda event). Jämtland is central in WOGOGOB’s history as the area served as a meeting place for the intial meeting in 1986, and more recently renewed stratigraphical and sedimentological studies have demonstrated the importance of this area in regional geology. WOGOGOB 2007 is unique in that it brings together palaeontologists, sedimentologists, geochemists and stratigraphers with research efforts directed at the Ordovician of Baltoscandia primarily, but also with wider ramifications for Ordovician geology. The meeting is held in collaboration with, and is a contribution to IGCP project 503, Ordovician Palaeogeography and Palaeoclimate, which aims to develop a better under­ standing of the environmental changes that influenced the Ordovician biodiversification, the end­Ordovician extinction and the Silurian radiation (http://sarv.gi.ee./igcp503). WOGOGOB 2007 also serves as the Baltic regional team meeting for IGCP 503. Jan Ove R. Ebbestad, Linda M. Wickström, and Anette E.S. Högström (Editors) Rapporter.&.meddelanden.128 5 WOGOGOB – How it began Maurits Lindström WOGOGOB was born at 18.00 hrs on May 31, 1985. Although it was declared dead by a couple of truly knowledgeable people a few days before and after this date, its survival into a third decade may be due, among other things, to the circumstance that a sufficient number of people would not just let such a quaint acronym expire. It stands for Working Group on Ordovician Geology of Baltoscandia. The idea of WOGOGOB was presented to a meeting of Palaeontologisk Klub (DGF) in Copenhagen on
Recommended publications
  • Trilobites of the Hagastrand Member (Tøyen Formation, Lowermost Arenig) from the Oslo Region, Norway. Part Il: Remaining Non-Asaphid Groups
    Trilobites of the Hagastrand Member (Tøyen Formation, lowermost Arenig) from the Oslo Region, Norway. Part Il: Remaining non-asaphid groups OLE A. HOEL Hoel, O. A.: Trilobites of the Hagastrand Member (Tøyen Formation, lowermost Arenig) from the Oslo Region, Norway. Part Il: remaining non-asaphid groups. Norsk Geologisk Tidsskrift, Vol. 79, pp. 259-280. Oslo 1999. ISSN 0029-196X. This is Part Il of a two-part description of the trilobite fauna of the Hagastrand Member (Tøyen Formation) in the Oslo, Eiker­ Sandsvær, Modum and Mjøsa areas. In this part, the non-asaphid trilobites are described, while the asaphid species have been described previously. The history and status of the Tremadoc-Arenig Boundary problem is also reviewed, and I have found no reason to insert a Hunnebergian Series between the Tremadoc and the Arenig series, as has been suggested by some workers. Descriptions of the localities yielding this special trilobite fauna are provided. Most of the 22 trilobite species found in the Hagastrand Member also occur in Sweden. The 12 non-asaphid trilobites described herein belong to the families Metagnostidae, Shumardiidae, Remopleurididae, Nileidae, Cyclopygidae, Raphiophoridae, Alsataspididae and Pliomeridae. One new species is described; Robergiella tjemviki n. sp. Ole A. Hoel, Paleontologisk Museum, Sars gate l, N-0562 Oslo, Norway. Introduction contemporaneous platform deposits in Sweden are domi­ nated by a condensed limestone succession. In Norway, the The Tremadoc-Arenig Boundary interval is a crucial point Tøyen Formation is divided into two members: the lower in the evolution of several invertebrate groups, especially among the graptolites and the trilobites. In the graptolites, this change consisted most significantly in the loss of bithekae and a strong increase in diversity.
    [Show full text]
  • Article (PDF, 3250
    Mitt. Mus. Nat.kd. Berl., Geowiss. Reihe 5 (2002) 105-120 10.11.2002 Atractocybeloides, eine kleinwuchsige Trilobitengattung aus baltoskandischen Geschieben und ihrem Anstehenden Hans-Hartmut Krueger * Mit 6 Abbildungen und 3 Tafeln Zusammenfassung Aus mittel- bis oberordovizischen Geschieben werden funf Taxa der kleinwuchsigen Trilobitengattung Atractocybeloides vorge- stellt, davon die beiden neuen Arten Atractocybeloides nebeni n. SP. und Atractocybeloides oepiki n. sp. Die Gattung wurde 1991 an Fragmenten aufgestellt. Sie hat sich in der Aseri-Stufe aus Cybele entwickelt. Neue Funde und das reichhaltige Material aus der Sammlung Rhebergen, in der auch fast vollstandige Panzerhemden von A. berneri enthalten sind, ermoglich- ten eine Rekonstruktion. ,Weiterhin wird die aus Nonvegen beschriebene Art Atractopyge gracilis der Gattung Atractocybel- oides zugeordnet. GroBe Ahnlichkeiten bestehen zur ungefahr gleichaltrigen nordamerikanischen kleinwiichsigen Gattung Cy- beloides. Schliisselworter: Trilobita, Atractocybeloides, Geschiebe, Ordovizium. Abstract Five taxa of the small trilobite genus Atractocybeloides are presented from Middle to Late Ordovician erratic boulders, includ- ing the new species Atractocybeloides nebeni n. sp. and Atractocybeloides oepiki n. sp. The genus was errected in 1991 on the basis of fragmentary material. It evolved from Cybele during Aseri-zone times. A reconstruction is made possible due to new finds and the rich material from the Rhebergen collection, including nearly complete cuticles of A. berneri. Furthermore, Atructopyge gracilis from Norway is assigned to Atractocybeloides. Strong similarities exist to the roughly coeval, small trilo- bite genus Cybeloides, which is known from North America. Key words: Trilobita, Atructocybeloides, erratic boulders, Ordovician. Einleitung tung vereinigt auf ihrem Cranidium Merkmale von Cybele, Atractopyge und Cybeloides. 1991 Durch ihren kleinen Wuchs und die seltenen, wurde die neue Gattung Atructocybeloides mit sparlichen Reste in bestimmten oberordovizi- zwei neuen Arten, A.
    [Show full text]
  • Trace Fossils from the Baltoscandian Erratic Boulders in Sw Poland
    Annales Societatis Geologorum Poloniae (2017), vol. 87: 229–257 doi: https://doi.org/10.14241/asgp.2017.014 TRACE FOSSILS FROM THE BALTOSCANDIAN ERRATIC BOULDERS IN SW POLAND Alina CHRZĄSTEK & Kamil PLUTA Institute of Geological Sciences, Wrocław University; Maksa Borna 9, 50-204 Wrocław, Poland e-mails: [email protected], [email protected] Chrząstek, A. & Pluta, K, 2017. Trace fossils from the Baltoscandian erratic boulders in SW Poland. Annales Societatis Geologorum Poloniae, 87: 229–257. Abstract: Many well preserved trace fossils were found in erratic boulders and the fossils preserved in them, occurring in the Pleistocene glacial deposits of the Fore-Sudetic Block (Mokrzeszów Quarry, Świebodzice outcrop). They include burrows (Arachnostega gastrochaenae, Balanoglossites isp., ?Balanoglossites isp., ?Chondrites isp., Diplocraterion isp., Phycodes isp., Planolites isp., ?Rosselia isp., Skolithos linearis, Thalassinoides isp., root traces) and borings ?Gastrochaenolites isp., Maeandropolydora isp., Oichnus isp., Osprioneides kamp- to, ?Palaeosabella isp., Talpina isp., Teredolites isp., Trypanites weisei, Trypanites isp., ?Trypanites isp., and an unidentified polychaete boring in corals. The boulders, Cambrian to Neogene (Miocene) in age, mainly came from Scandinavia and the Baltic region. The majority of the trace fossils come from the Ordovician Orthoceratite Limestone, which is exposed mainly in southern and central Sweden, western Russia and Estonia, and also in Norway (Oslo Region). The most interesting discovery in these deposits is the occurrence of Arachnostega gastrochaenae in the Ordovician trilobites (?Megistaspis sp. and Asaphus sp.), cephalopods and hyolithids. This is the first report ofArachnostega on a trilobite (?Megistaspis) from Sweden. So far, this ichnotaxon was described on trilobites from Baltoscandia only from the St.
    [Show full text]
  • Kliinikumi Uued Ravikor- Pused Said 12. Novembril Nurgakivi
    1000 neerusiirdamist! Üks A4 Patsiendi ootustest Kokkuvõte LK 2-3 LK 4 tervishoiule LK 6-7 abiarstidest LK 11 SISELEHT nr 157 november 2013 www.kliinikum.ee/leht UUDIS Kliinikumi uued ravikor- HIVi ja hepatiitide testimine ja nõus- pused said 12. novembril tamine noortele Tartu linnavalitsuse tervis- hoiuosakond korraldab nurgakivi. koostöös Tartu Ülikooli Kliinikumi infektsiooni- kontrolli teenistusega Tartu Ülikooli Kliinikumi Maarjamõisa meditsiinilinnaku teises ehitusjärgus Tartu linna kõrgkoolides rajatakse kolm uut ravikorpust. ning kutsehariduskeskuses Fotod: Andres Tennus HIVi ja hepatiitide tasuta ja anonüümse testimise ning nõustamise. Testimised toimuvad: • 4. novembril kell 9.00- 12.00 Tartu Ülikooli pea- hoones, Ülikooli 18, audi- toorium 140. • 5. novembril kell 9.00- 12.00 Eesti Maaülikooli Metsamajas, ruum 2A9 • 6. novembril kell 9.00- 12.00 Tartu Kutseharidus- keskuses, Kopli 1, ruum C164 • 11. novembril kell 9.00- 12.00 Tartu Ülikooli pea- hoones, Ülikooli 18, audi- Meditsiinilinnaku teise etapi ca 32,4 miljonit eurot. vana, täna ei ole see enam pel- toorium 140 üks tähtsamaid eesmärke on Meditsiinilinnaku J-, K- ja galt kivi. • 14. novembril kell 9.00- moodsa onkoloogiakeskuse L-korpused projekteerivad Louvris säilitatakse kaht 12.00 Tartu Kutseharidus- rajamine, mille keerukaim osa AW2-arkkitehdit Oy ja OÜ terrakota silindrit, mis on lei- keskuses, Põllu 11c, kab 5 on kiiritusraviosakond. Samu- Civen ning ehitavad AS Ehi- tud Lagashi linna varemetest • 25. novembril kell 10.00- ti luuakse kaasaegne taristu si- tusfirma Rand ja Tuulberg toonasest lõuna Babülooniast 13.00 Tartu Tervishoiu Kõrgkoolis, Nooruse 5, sekliinikule, silmakliinikule, ning OÜ Astlanda Ehitus. ja on pärit umbes aastast 2125 ruum 208 kardiokirurgia osakonnale. Maarjamõisa meditsiinilin- ekr.
    [Show full text]
  • South and North Barents Triassic-Jurassic Total Petroleum System of the Russian Offshore Arctic
    U. S. Department of the Interior U. S. Geological Survey South and North Barents Triassic-Jurassic Total Petroleum System of the Russian Offshore Arctic On-Line Edition by Sandra J. Lindquist1 Open-File Report 99-50-N This report is preliminary and has not been reviewed for conformity with the U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1999 1 Consulting Geologist, Contractor to U. S. Geological Survey, Denver, Colorado Page 1 of 22 South and North Barents Triassic-Jurassic Total Petroleum System of the Russian Offshore Arctic2 Sandra J. Lindquist, Consulting Geologist Contractor to the U.S. Geological Survey, Denver, CO October, 1999 FOREWORD This report was prepared as part of the World Energy Project of the U.S. Geological Survey. In the project, the world was divided into 8 regions and 937 geologic provinces. The provinces have been ranked according to the discovered oil and gas volumes within each (Klett and others, 1997). Then, 76 "priority" provinces (exclusive of the U.S. and chosen for their high ranking) and 26 "boutique" provinces (exclusive of the U.S. and chosen for their anticipated petroleum richness or special regional economic importance) were selected for appraisal of oil and gas resources. The petroleum geology of these priority and boutique provinces is described in this series of reports. A detailed report containing the assessment results will be available separately, if such results are not reported herein. The priority South Barents Basin Province ranks 35th in the world, exclusive of the U.S.
    [Show full text]
  • Available Generic Names for Trilobites
    AVAILABLE GENERIC NAMES FOR TRILOBITES P.A. JELL AND J.M. ADRAIN Jell, P.A. & Adrain, J.M. 30 8 2002: Available generic names for trilobites. Memoirs of the Queensland Museum 48(2): 331-553. Brisbane. ISSN0079-8835. Aconsolidated list of available generic names introduced since the beginning of the binomial nomenclature system for trilobites is presented for the first time. Each entry is accompanied by the author and date of availability, by the name of the type species, by a lithostratigraphic or biostratigraphic and geographic reference for the type species, by a family assignment and by an age indication of the type species at the Period level (e.g. MCAM, LDEV). A second listing of these names is taxonomically arranged in families with the families listed alphabetically, higher level classification being outside the scope of this work. We also provide a list of names that have apparently been applied to trilobites but which remain nomina nuda within the ICZN definition. Peter A. Jell, Queensland Museum, PO Box 3300, South Brisbane, Queensland 4101, Australia; Jonathan M. Adrain, Department of Geoscience, 121 Trowbridge Hall, Univ- ersity of Iowa, Iowa City, Iowa 52242, USA; 1 August 2002. p Trilobites, generic names, checklist. Trilobite fossils attracted the attention of could find. This list was copied on an early spirit humans in different parts of the world from the stencil machine to some 20 or more trilobite very beginning, probably even prehistoric times. workers around the world, principally those who In the 1700s various European natural historians would author the 1959 Treatise edition. Weller began systematic study of living and fossil also drew on this compilation for his Presidential organisms including trilobites.
    [Show full text]
  • Strophomenide and Orthotetide Silurian Brachiopods from the Baltic Region, with Particular Reference to Lithuanian Boreholes
    Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes PETRAS MUSTEIKIS and L. ROBIN M. COCKS Musteikis, P. and Cocks, L.R.M. 2004. Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes. Acta Palaeontologica Polonica 49 (3): 455–482. Epeiric seas covered the east and west parts of the old craton of Baltica in the Silurian and brachiopods formed a major part of the benthic macrofauna throughout Silurian times (Llandovery to Pridoli). The orders Strophomenida and Orthotetida are conspicuous components of the brachiopod fauna, and thus the genera and species of the superfamilies Plec− tambonitoidea, Strophomenoidea, and Chilidiopsoidea, which occur in the Silurian of Baltica are reviewed and reidentified in turn, and their individual distributions are assessed within the numerous boreholes of the East Baltic, particularly Lithua− nia, and attributed to benthic assemblages. The commonest plectambonitoids are Eoplectodonta(Eoplectodonta)(6spe− cies), Leangella (2 species), and Jonesea (2 species); rarer forms include Aegiria and Eoplectodonta (Ygerodiscus), for which the new species E. (Y.) bella is erected from the Lithuanian Wenlock. Eight strophomenoid families occur; the rare Leptaenoideidae only in Gotland (Leptaenoidea, Liljevallia). Strophomenidae are represented by Katastrophomena (4 spe− cies), and Pentlandina (2 species); Bellimurina (Cyphomenoidea) is only from Oslo and Gotland. Rafinesquinidae include widespread Leptaena (at least 11 species) and Lepidoleptaena (2 species) with Scamnomena and Crassitestella known only from Gotland and Oslo. In the Amphistrophiidae Amphistrophia is widespread, and Eoamphistrophia, Eocymostrophia, and Mesodouvillina are rare. In the Leptostrophiidae Mesoleptostrophia, Brachyprion,andProtomegastrophia are com− mon, but Eomegastrophia, Eostropheodonta, Erinostrophia,andPalaeoleptostrophia are only recorded from the west in the Baltica Silurian.
    [Show full text]
  • 001-012 Primeras Páginas
    PUBLICACIONES DEL INSTITUTO GEOLÓGICO Y MINERO DE ESPAÑA Serie: CUADERNOS DEL MUSEO GEOMINERO. Nº 9 ADVANCES IN TRILOBITE RESEARCH ADVANCES IN TRILOBITE RESEARCH IN ADVANCES ADVANCES IN TRILOBITE RESEARCH IN ADVANCES planeta tierra Editors: I. Rábano, R. Gozalo and Ciencias de la Tierra para la Sociedad D. García-Bellido 9 788478 407590 MINISTERIO MINISTERIO DE CIENCIA DE CIENCIA E INNOVACIÓN E INNOVACIÓN ADVANCES IN TRILOBITE RESEARCH Editors: I. Rábano, R. Gozalo and D. García-Bellido Instituto Geológico y Minero de España Madrid, 2008 Serie: CUADERNOS DEL MUSEO GEOMINERO, Nº 9 INTERNATIONAL TRILOBITE CONFERENCE (4. 2008. Toledo) Advances in trilobite research: Fourth International Trilobite Conference, Toledo, June,16-24, 2008 / I. Rábano, R. Gozalo and D. García-Bellido, eds.- Madrid: Instituto Geológico y Minero de España, 2008. 448 pgs; ils; 24 cm .- (Cuadernos del Museo Geominero; 9) ISBN 978-84-7840-759-0 1. Fauna trilobites. 2. Congreso. I. Instituto Geológico y Minero de España, ed. II. Rábano,I., ed. III Gozalo, R., ed. IV. García-Bellido, D., ed. 562 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage and retrieval system now known or to be invented, without permission in writing from the publisher. References to this volume: It is suggested that either of the following alternatives should be used for future bibliographic references to the whole or part of this volume: Rábano, I., Gozalo, R. and García-Bellido, D. (eds.) 2008. Advances in trilobite research. Cuadernos del Museo Geominero, 9.
    [Show full text]
  • The Viruan (Middle Ordovician) of Öland
    The Viruan (Middle Ordovician) of Öland By Valdar Jaanusson ABSTRACT.-The stratigraphy and lithology of the Viruan (Middle Ordovician) Iimestones of the bed-rock of Öland are described based on three bares and on field work in the outcrop area. A combined litho- and bio-stratigraphic classification (termed topo-stratigraphic) is introduced for the described sequence. The names of the Estonian stages (Aserian, Lasnamägian, Uhakuan, and Kukrusean) are used as chrono-stratigraphic references instead of the previous Swedish names of the units of stage category (Platyurus, Schroeteri, Crassicauda, and Ludibundus, re­ spectivcly). New topo-stratigraphic divisions are Segerstad Limestone (of Aserian age), Skärlöv, Seby, and Folkeslunda Limestones (of Lasnamägian age), Furudal, Källa, and Persnäs Lime­ stones (of Uhakuan age), and Dalby Limestone (of Kukrusean age in the bed-rock of Öland). The Aserian Lasnamägian topo-stratigraphic divisions have the same lithological characteris­ and tics throughout Öland. The Uhakuan beds are developed as calcilutites (Furudal Limestone) on southern Öland continuing as a tongue (Källa Limestone) on northern Öland. The middle and upper part of the Uhakuan beds of northern Öland consist of calcarenites (Persnäs Limestone) lithologically indistiguishable from the Kukrusean Dalby Limestone which forms the bed-rock only on northern Öland. Within the Segerstad Limestone two zones are distinguished (z. of Angelinoceras latum and z. of Illaenus planifrons).H ouvr ' s zones of Lituites discors, L. lituus, and L. perfectus are of Lasna­ mägian age, and their stratigraphic position and fauna! characteristics are described. Contents Introduction . 207 Methods .............. 209 Classification of the Viruan rocks of Öland 2I2 Historical survey . 2I9 Taxonornie and nomenclatural notes 22I Viruan rocks of northern Öland .
    [Show full text]
  • Paleozoic Rocks Antelope Valley Eureka and Nye Counties Nevada
    :It k 'I! ' Paleozoic Rocks Antelope Valley Eureka and Nye Counties Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 423 Paleozoic Rocks of Antelope Valley Eureka and Nye Counties Nevada By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 423 P,rinciples of stratigraphy applied in descriptive study of the Central Great Basin Paleozoic column UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page Silurian system ____________________________________ _ Abstract------------------------------------------- 1 36 Introduction. _____________________________________ _ 2 General features-------------------------------- 36 Geologic setting ______________ ------ ___ --------- 2 Roberts Mountains formation ___________________ _ 37 History of investigation ________________________ _ 5 Lone Mountain dolomite ______ ---_-------------- 39 Purpose and scope _____________ -- ______ ------ --- 6 Devonian system ______________ ---- __ - _- ___ - _------- 41 Acknowledgments ______________________________ _ 6 General features _____________ - ___________ -_----- 41 Geologic structure as related to stratigraphy __________ _ 6 Western Helderberg age limestones of the Monitor Paleontologic studies ______ ..:. _______ ~ ________________ _ 9 · Range ______ - _.- ___ --------------------------- 42 The Paleozoic column at Antelope Valley
    [Show full text]
  • Distribution of the Middle Ordovician Copenhagen Formation and Its Trilobites in Nevada
    Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada By REUBEN JAMES ROSS, JR., and FREDERICK C. SHAW GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Descriptions of Middle Ordovician trilobites belonging to 21 genera contribute to correlations between similar strata in Nevada) California) and 0 klahoma UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. lVIOR TON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 78-190301 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 70 cents (paper cover) Stock Number 2401-2109 CONTENTS Page Page Abstract ______________________________ -------------------------------------------------- 1 Descriptions of trilobites __________________________________________________ _ 14 Introduction ________________________________________________________________________ _ 1 Genus T1·iarth1·us Green, 1832 .... ------------------------------ 14 Previous investigations _____________________________________________ _ 1 Genus Carrickia Tripp, 1965 ____________________________________ _ 14 Acknowledgments-------------------------------------------------------· 1 Genus Hypodicranotus Whittington, 1952 _____________ _ 15 Geographic occurrences of the Copenhagen Genus Robergia Wiman, 1905·----------------------------------
    [Show full text]
  • Diversity and Biostratigraphic Utility of Ordovician Brachiopods in the East Baltic.', Estonian Journal of Earth Sciences., 67 (3)
    Durham Research Online Deposited in DRO: 11 June 2018 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Hints, L. and Harper, D.A.T. and Pa§skevi§cius,J. (2018) 'Diversity and biostratigraphic utility of Ordovician brachiopods in the East Baltic.', Estonian journal of earth sciences., 67 (3). pp. 176-191. Further information on publisher's website: https://doi.org/10.3176/earth.2018.14 Publisher's copyright statement: c 2018 Authors. This is an Open Access article distributed under the terms and conditions of the Creative Commons Attribution 4.0 International Licence (http://creativecommons.org/licenses/by/4.0). Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 http://dro.dur.ac.uk Estonian Journal of Earth Sciences, 2018, 67, 3, 176–191 https://doi.org/10.3176/earth.2018.14 Diversity and biostratigraphic utility of Ordovician brachiopods in the East Baltic Linda Hintsa, David A.
    [Show full text]