WITSML Lithology Object Usage Guide
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Western North Greenland (Laurentia)
BULLETIN OF THE GEOLOGICAL SOCIETY OF DENMARK · VOL. 69 · 2021 Trilobite fauna of the Telt Bugt Formation (Cambrian Series 2–Miaolingian Series), western North Greenland (Laurentia) JOHN S. PEEL Peel, J.S. 2021. Trilobite fauna of the Telt Bugt Formation (Cambrian Series 2–Mi- aolingian Series), western North Greenland (Laurentia). Bulletin of the Geological Society of Denmark, Vol. 69, pp. 1–33. ISSN 2245-7070. https://doi.org/10.37570/bgsd-2021-69-01 Trilobites dominantly of middle Cambrian (Miaolingian Series, Wuliuan Stage) Geological Society of Denmark age are described from the Telt Bugt Formation of Daugaard-Jensen Land, western https://2dgf.dk North Greenland (Laurentia), which is a correlative of the Cape Wood Formation of Inglefield Land and Ellesmere Island, Nunavut. Four biozones are recognised in Received 6 July 2020 Daugaard-Jensen Land, representing the Delamaran and Topazan regional stages Accepted in revised form of the western USA. The basal Plagiura–Poliella Biozone, with Mexicella cf. robusta, 16 December 2020 Kochiella, Fieldaspis? and Plagiura?, straddles the Cambrian Series 2–Miaolingian Series Published online 20 January 2021 boundary. It is overlain by the Mexicella mexicana Biozone, recognised for the first time in Greenland, with rare specimens of Caborcella arrojosensis. The Glossopleura walcotti © 2021 the authors. Re-use of material is Biozone, with Glossopleura, Clavaspidella and Polypleuraspis, dominates the succes- permitted, provided this work is cited. sion in eastern Daugaard-Jensen Land but is seemingly not represented in the type Creative Commons License CC BY: section in western outcrops, likely reflecting the drastic thinning of the formation https://creativecommons.org/licenses/by/4.0/ towards the north-west. -
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. -
Proposed Global Standard Stratotype-Section And
PROPOSED GLOBAL STANDARD STRATOTYPE-SECTION AND POINT FOR THE DRUMIAN STAGE (CAMBRIAN) Prepared for the International Subcommission on Cambrian Stratigraphy by: Loren E. Babcock School of Earth Sciences The Ohio State University, 125 South Oval Mall Columbus, OH 43210, USA [email protected] Richard A. Robison Department of Geology, University of Kansas Lawrence, KS 66045, USA [email protected] Margaret N. Rees Department of Geoscience University of Nevada, Las Vegas Las Vegas, NV 89145, USA [email protected] Peng Shanchi Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences 39 East Beijing Road, Nanjing 210008, China [email protected] Matthew R. Saltzman School of Earth Sciences The Ohio State University, 125 South Oval Mall Columbus, OH 43210, USA [email protected] 31 July 2006 CONTENTS Introduction …………………………………………………………………………. 2 Proposal: Stratotype Ridge, Drum Mountains (Millard County, Utah, USA) as the GSSP for the base of the Drumian Stage ……………………………………………………. 3 1. Stratigraphic rank of the boundary …………………..…………………………… 3 2. Proposed GSSP – geography and physical geology ……………………………… 3 2.1. Geographic location …………………………………………………...….. 3 2.2. Geological location ………………..……………………...…………...….. 4 2.3. Location of level and specific point ……………………..……………...… 4 2.4. Stratigraphic completeness ………………...……………………………… 5 2.5. Thickness and stratigraphic extent …………………...……………...……. 5 2.6. Provisions for conservation, protection, and accessibility ……………..…. 5 3. Motivation for selection of the boundary level and of the potential stratotype section ………………………………………………………………………………. 6 3.1. Principal correlation event (marker) at GSSP level ………...…………..… 6 3.2. Potential stratotype section …………………………………………....….. 7 3.3. Demonstration of regional and global correlation ………………………... 8 3.3.1. Agnostoid trilobite biostratigraphy ………………………………… 9 3.3.2. Polymerid trilobite biostratigraphy …………....…………….……. -
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. -
Durham Research Online
Durham Research Online Deposited in DRO: 14 September 2016 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Zhang, X.-G. and Smith, M.R. and Yang, J. and Hou, J.-B. (2016) 'Onychophoran-like musculature in a phosphatized Cambrian lobopodian.', Biology letters., 12 (9). p. 20160492. Further information on publisher's website: http://rsbl.royalsocietypublishing.org/ Publisher's copyright statement: 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 https://dro.dur.ac.uk Submitted to Biology Letters Onychophoran -like musculature in a phosphatized Cambrian lobopodian Journal:For Biology Review Letters Only Manuscript ID RSBL-2016-0492.R2 Article Type: Research Date Submitted by the Author: 23-Aug-2016 Complete List of Authors: Zhang, Xi-guang; Yunnan University, Key Laboratory for Palaeobiology; Smith, Martin; Durham University Yang, Jie; Yunnan University, The Key Laboratory for Palaeobiology Hou, Jin-bo; Yunnan University Subject: Evolution < BIOLOGY, Palaeontology < BIOLOGY Categories: Palaeontology Keywords: lobopodians, muscle, evolution, taphonomy, phylogenetics http://mc.manuscriptcentral.com/bl Page 1 of 14 Submitted to Biology Letters 1 Onychophoran-like musculature in a phosphatized Cambrian 2 lobopodian 3 4 Xi-Guang Zhang 1*, Martin R. -
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. -
PHYLOGENY and DISTRIBUTION by LARS E
[Papers in Palaeontology, 2019, pp. 1–17] CAMBRIAN RHYNCHONELLIFORM NISUSIOID BRACHIOPODS: PHYLOGENY AND DISTRIBUTION by LARS E. HOLMER1,2 , MOHAMMAD-REZA KEBRIA-EE ZADEH3, LEONID E. POPOV4, MANSOUREH GHOBADI POUR2,4,5,J.JAVIERALVARO 6, VACHIK HAIRAPETIAN7 and ZHIFEI ZHANG1 1Shaanxi Key Laboratory of Early Life & Environments, State Key Laboratory for Continental Dynamics, Northwest University, Xi’an, 710069, China 2Department of Earth Sciences, Palaeobiology, SE-752 36, Uppsala, Sweden; [email protected] 3Department of Geology, Payame Noor University, Semnan, Iran; [email protected] 4Department of Earth Sciences, National Museum of Wales, Cathays Park, Cardiff, CF10 3NP, UK; [email protected] 5Department of Geology, Faculty of Sciences, Golestan University, Gorgan, 49138-15739, Iran; [email protected] 6Instituto de Geociencias (CSIC-UCM), Dr. Severo Ochoa 7, Madrid, 28040, Spain; [email protected] 7Department of Geology, Khorasgan (Isfahan) Branch, Islamic Azad University, PO Box 81595-158, Isfahan, Iran; [email protected] Typescript received 18 July 2018; accepted in revised form 6 November 2018 Abstract: A comprehensive review and phylogenetic analy- an early separation of the lineages of spinose and non-spi- sis of genera and species presently assigned to the rhyn- nose nisusiids. The non-spinose nisusiids probably evolved chonelliform superfamily Nisusioidea and family Nisusiidae in Laurentia by the end of Cambrian Series 4. The new suggests that this short-lived but important group of bra- nisusiid genus Bellistrophia is described. The new species chiopods first appeared in peri-Gondwana during the second Nisusia multicostata represents the first documented rhyn- half of the Cambrian Series 2, before going extinct by the chonelliform (kutorginide) brachiopod from the Miaolingian end of Drumian times. -
Revised Sequence Stratigraphy of the Ordovician of Baltoscandia …………………………………………… 20 Druzhinina, O
Baltic Stratigraphical Association Department of Geology, Faculty of Geography and Earth Sciences, University of Latvia Natural History Museum of Latvia THE EIGHTH BALTIC STRATIGRAPHICAL CONFERENCE ABSTRACTS Edited by E. Lukševičs, Ģ. Stinkulis and J. Vasiļkova Rīga, 2011 The Eigth Baltic Stratigraphical Conference 28 August – 1 September 2011, Latvia Abstracts Edited by E. Lukševičs, Ģ. Stinkulis and J. Vasiļkova Scientific Committee: Organisers: Prof. Algimantas Grigelis (Vilnius) Baltic Stratigraphical Association Dr. Olle Hints (Tallinn) Department of Geology, University of Latvia Dr. Alexander Ivanov (St. Petersburg) Natural History Museum of Latvia Prof. Leszek Marks (Warsaw) Northern Vidzeme Geopark Prof. Tõnu Meidla (Tartu) Dr. Jonas Satkūnas (Vilnius) Prof. Valdis Segliņš (Riga) Prof. Vitālijs Zelčs (Chairman, Riga) Recommended reference to this publication Ceriņa, A. 2011. Plant macrofossil assemblages from the Eemian-Weichselian deposits of Latvia and problems of their interpretation. In: Lukševičs, E., Stinkulis, Ģ. and Vasiļkova, J. (eds). The Eighth Baltic Stratigraphical Conference. Abstracts. University of Latvia, Riga. P. 18. The Conference has special sessions of IGCP Project No 591 “The Early to Middle Palaeozoic Revolution” and IGCP Project No 596 “Climate change and biodiversity patterns in the Mid-Palaeozoic (Early Devonian to Late Carboniferous)”. See more information at http://igcl591.org. Electronic version can be downloaded at www.geo.lu.lv/8bsc Hard copies can be obtained from: Department of Geology, Faculty of Geography and Earth Sciences, University of Latvia Raiņa Boulevard 19, Riga LV-1586, Latvia E-mail: [email protected] ISBN 978-9984-45-383-5 Riga, 2011 2 Preface Baltic co-operation in regional stratigraphy is active since the foundation of the Baltic Regional Stratigraphical Commission (BRSC) in 1969 (Grigelis, this volume). -
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. -
Permophiles International Commission on Stratigraphy
Permophiles International Commission on Stratigraphy Newsletter of the Subcommission on Permian Stratigraphy Number 66 Supplement 1 ISSN 1684 – 5927 August 2018 Permophiles Issue #66 Supplement 1 8th INTERNATIONAL BRACHIOPOD CONGRESS Brachiopods in a changing planet: from the past to the future Milano 11-14 September 2018 GENERAL CHAIRS Lucia Angiolini, Università di Milano, Italy Renato Posenato, Università di Ferrara, Italy ORGANIZING COMMITTEE Chair: Gaia Crippa, Università di Milano, Italy Valentina Brandolese, Università di Ferrara, Italy Claudio Garbelli, Nanjing Institute of Geology and Palaeontology, China Daniela Henkel, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany Marco Romanin, Polish Academy of Science, Warsaw, Poland Facheng Ye, Università di Milano, Italy SCIENTIFIC COMMITTEE Fernando Álvarez Martínez, Universidad de Oviedo, Spain Lucia Angiolini, Università di Milano, Italy Uwe Brand, Brock University, Canada Sandra J. Carlson, University of California, Davis, United States Maggie Cusack, University of Stirling, United Kingdom Anton Eisenhauer, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany David A.T. Harper, Durham University, United Kingdom Lars Holmer, Uppsala University, Sweden Fernando Garcia Joral, Complutense University of Madrid, Spain Carsten Lüter, Museum für Naturkunde, Berlin, Germany Alberto Pérez-Huerta, University of Alabama, United States Renato Posenato, Università di Ferrara, Italy Shuzhong Shen, Nanjing Institute of Geology and Palaeontology, China 1 Permophiles Issue #66 Supplement -
Annual Meeting 2011
The Palaeontological Association 55th Annual Meeting 17th–20th December 2011 Plymouth University PROGRAMME and ABSTRACTS Palaeontological Association 2 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 55th Annual Meeting 17th–20th December 2011 School of Geography, Earth and Environmental Sciences, Plymouth University The programme and abstracts for the 55th Annual Meeting of the Palaeontological Association are outlined after the following summary of the meeting. Venue The meeting will take place on the campus of Plymouth University. Directions to the University and a campus map can be found at <http://www.plymouth.ac.uk/location>. The opening symposium and the main oral sessions will be held in the Sherwell Centre, located on North Hill, on the east side of campus. Accommodation Delegates need to make their own arrangements for accommodation. Plymouth has a large number of hotels, guesthouses and hostels at a variety of prices, most of which are within ~1km of the University campus (hotels with PL1 or PL4 postcodes are closest). More information on these can be found through the usual channels, and a useful starting point is the website <http://www.visitplymouth.co.uk/site/where-to-stay>. In addition, we have organised discount rates at the Jury’s Inn, Exeter Street, which is located ~500m from the conference venue. A maximum of 100 rooms have been reserved, and will be allocated on a first-come-first-served basis. Further information can be found on the Association’s website. Travel Transport into Plymouth can be achieved via a variety of means. Travel by train from London Paddington to Plymouth takes between three and four hours depending on the time of day and the number of stops. -
(Re)Proposal of Three Cambrian Subsystems and Their Geochronology
Article 273 by Ed Landing1*, Gerd Geyer2, Mark D. Schmitz3, Thomas Wotte4, and Artem Kouchinsky5 (Re)proposal of three Cambrian Subsystems and their Geochronology 1 New York State Museum, 222 Madison Avenue, Albany, NY, USA; *Corresponding author, E-mail: [email protected] 2 Lehrstuhl für Geodynamik und Geomaterialforschung, Institut für Geographie und Geologie, Bayerische Julius-Maximilians Universität Würzburg, Am Hubland, D-97074 Würzburg, Germany 3 Department of Geosciences, Boise State University, 1910 University Drive, Boise, Idaho 83725, USA 4 Department of Palaeontology, TU Bergakademie Freiberg, Bernhard-von-Cotta-Straße, D-09599 Freiberg, Germany 5 Department of Palaeontology, Swedish Museum of Natural History, Box 50007, SE-104 05, Stockholm, Sweden (Received: April 29, 2020; Revised accepted: September 24, 2020) https://doi.org/10.18814/epiiugs/2020/020088 The Cambrian is anomalous among geological systems 2018). Following work by the International Subcommission on Cam- as many reports divide it into three divisions of indetermi- brian Stratigraphy (ISCS), these key biotic developments can be related nate rank. This use of “lower”, “middle”, and “upper” has to the chronostratigraphic subdivision of the Cambrian System into been a convenient way to subdivide the Cambrian despite four global series and ten stages (e.g., Babcock, 2005; Babcock and agreement it consists of four global series. Traditional divi- Peng, 2007) complemented by an increasingly precise U-Pb (numeri- sions of the system into regional series (Lower, Middle, cal) geochronology (Fig. 1). This decision at the 2004 ISCS meeting Upper) reflected local biotic developments not interpro- meant that the traditional subdivisions of the Cambrian into regional “Lower,” “Middle,” and “Upper” series (discussed below) were no lon- vincially correlatable with any precision.