International Stratigraphic Chart

Total Page:16

File Type:pdf, Size:1020Kb

International Stratigraphic Chart INTERNATIONAL STRATIGRAPHIC CHART ICS International Commission on Stratigraphy Ma Ma Ma Ma Era Era Era Era Age Age Age Age Age Eon Eon Age Eon Age Eon Stage Stage Stage GSSP GSSP GSSA GSSP GSSP Series Epoch Series Epoch Series Epoch Period Period Period Period System System System System Erathem Erathem Erathem Erathem Eonothem Eonothem Eonothem 145.5 ±4.0 Eonothem 359.2 ±2.5 542 Holocene Tithonian Famennian Ediacaran 0.0117 150.8 ±4.0 Upper 374.5 ±2.6 Neo- ~635 Upper Upper Kimmeridgian Frasnian Cryogenian 0.126 ~ 155.6 385.3 ±2.6 proterozoic 850 “Ionian” Oxfordian Givetian Tonian Pleistocene 0.781 161.2 ±4.0 Middle 391.8 ±2.7 1000 Calabrian Callovian Eifelian Stenian Quaternary 1.806 164.7 ±4.0 397.5 ±2.7 Meso- 1200 Gelasian Bathonian Emsian Ectasian proterozoic 2.588 Middle 167.7 ±3.5 Devonian 407.0 ±2.8 1400 Piacenzian Bajocian Lower Pragian Calymmian Pliocene 3.600 171.6 ±3.0 411.2 ±2.8 1600 Zanclean Aalenian Lochkovian Statherian Jurassic 5.332 175.6 ±2.0 416.0 ±2.8 Proterozoic 1800 Messinian Toarcian Pridoli Paleo- Orosirian 7.246 183.0 ±1.5 418.7 ±2.7 2050 Tortonian Pliensbachian Ludfordian proterozoic Rhyacian 11.608 Lower 189.6 ±1.5 Ludlow 421.3 ±2.6 2300 Serravallian Sinemurian Gorstian Siderian Miocene 13.82 196.5 ±1.0 422.9 ±2.5 2500 Neogene Langhian Hettangian Homerian 15.97 199.6 ±0.6 Wenlock 426.2 ±2.4 Neoarchean Burdigalian M e s o z i c Rhaetian Sheinwoodian 20.43 203.6 ±1.5 428.2 ±2.3 2800 Aquitanian Upper Norian Silurian Telychian 23.03 216.5 ±2.0 436.0 ±1.9 P r e c a m b i n P Mesoarchean C e n o z i c Chattian Carnian Llandovery Aeronian Oligocene 28.4 ±0.1 ~ 228.7 439.0 ±1.8 3200 Rupelian Ladinian Rhuddanian 33.9 ±0.1 Middle 237.0 ±2.0 443.7 ±1.5 Paleoarchean Priabonian Anisian Archean Triassic Hirnantian 37.2 ±0.1 ~ 245.9 445.6 ±1.5 3600 Bartonian Olenekian Upper Katian Eocene 40.4 ±0.2 Lower ~ 249.5 455.8 ±1.6 Eoarchean Lutetian Induan Sandbian 48.6 ±0.2 251.0 ±0.4 460.9 ±1.6 4000 Ypresian Changhsingian a l e o z i c P Darriwilian 55.8 ±0.2 468.1 ±1.6 P h a n e r o z i c P h a n e r o z i c P Lopingian 253.8 ±0.7 h a n e r o z i c P Middle Hadean (informal) Paleogene Thanetian Wuchiapingian Dapingian 58.7 ±0.2 260.4 ±0.7 471.8 ±1.6 ~4600 Paleocene Selandian Capitanian Ordovician Floian ~ 61.1 265.8 ±0.7 Lower 478.6 ±1.7 Subdivisions of the global geologic record are Danian Guadalupian Wordian Tremadocian 268.0 ±0.7 formally defined by their lower boundary. Each unit 65.5 ±0.3 488.3 ±1.7 of the Phanerozoic (~542 Ma to Present) and the Maastrichtian Roadian Stage 10 70.6 ±0.6 270.6 ±0.7 ~ 492 * base of Ediacaran are defined by a basal Global Campanian Kungurian Furongian Stage 9 Boundary Stratotype Section and Point (GSSP ), 83.5 ±0.7 Permian 275.6 ±0.7 ~ 496 * whereas Precambrian units are formally subdivided Santonian Artinskian Paibian by absolute age (Global Standard Stratigraphic Age, Upper 85.8 ±0.7 Cisuralian 284.4 ±0.7 ~ 499 Coniacian Sakmarian Guzhangian GSSA). Details of each GSSP are posted on the ~ 88.6 294.6 ±0.8 ~ 503 ICS website (www.stratigraphy.org). Turonian Asselian Series 3 Drumian Numerical ages of the unit boundaries in the 93.6 ±0.8 299.0 ±0.8 ~ 506.5 Phanerozoic are subject to revision. Some stages Cenomanian Gzhelian Stage 5 within the Cambrian will be formally named upon 99.6 ±0.9 Upper 303.4 ±0.9 ~ 510 * international agreement on their GSSP limits. Most P a l e o z i c P Albian Kasimovian Cambrian Stage 4 112.0 ±1.0 307.2 ±1.0 Series 2 ~ 515 * sub-Series boundaries (e.g., Middle and Upper Aptian Penn- Middle Moscovian Stage 3 Aptian) are not formally defined. Cretaceous 125.0 ±1.0 sylvanian 311.7 ±1.1 ~ 521 * M e s o z i c Colors are according to the Commission for the Barremian Lower Bashkirian Stage 2 Geological Map of the World (www.cgmw.org). Lower 130.0 ±1.5 318.1 ±1.3 Terreneuvian ~ 528 * Hauterivian Upper Serpukhovian Fortunian The listed numerical ages are from 'A Geologic ~ 133.9 328.3 ±1.6 542.0 ±1.0 Time Scale 2004', by F.M. Gradstein, J.G. Ogg, Valanginian Middle Visean This chart was drafted by Gabi Ogg. Intra Cambrian unit ages A.G. Smith, et al. (2004; Cambridge University Press) 140.2 ±3.0 Carboniferous 345.3 ±2.1 Missis- sippian with * are informal, and awaiting ratified definitions. and “The Concise Geologic Time Scale” by J.G. Ogg, Berriasian Lower Tournaisian 145.5 ±4.0 359.2 ±2.5 Copyright © 2010 International Commission on Stratigraphy G. Ogg and F.M. Gradstein (2008). Sept. 2010.
Recommended publications
  • And Ordovician (Sardic) Felsic Magmatic Events in South-Western Europe: Underplating of Hot Mafic Magmas Linked to the Opening of the Rheic Ocean
    Solid Earth, 11, 2377–2409, 2020 https://doi.org/10.5194/se-11-2377-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Comparative geochemical study on Furongian–earliest Ordovician (Toledanian) and Ordovician (Sardic) felsic magmatic events in south-western Europe: underplating of hot mafic magmas linked to the opening of the Rheic Ocean J. Javier Álvaro1, Teresa Sánchez-García2, Claudia Puddu3, Josep Maria Casas4, Alejandro Díez-Montes5, Montserrat Liesa6, and Giacomo Oggiano7 1Instituto de Geociencias (CSIC-UCM), Dr. Severo Ochoa 7, 28040 Madrid, Spain 2Instituto Geológico y Minero de España, Ríos Rosas 23, 28003 Madrid, Spain 3Dpt. Ciencias de la Tierra, Universidad de Zaragoza, 50009 Zaragoza, Spain 4Dpt. de Dinàmica de la Terra i de l’Oceà, Universitat de Barcelona, Martí Franquès s/n, 08028 Barcelona, Spain 5Instituto Geológico y Minero de España, Plaza de la Constitución 1, 37001 Salamanca, Spain 6Dpt. de Mineralogia, Petrologia i Geologia aplicada, Universitat de Barcelona, Martí Franquès s/n, 08028 Barcelona, Spain 7Dipartimento di Scienze della Natura e del Territorio, 07100 Sassari, Italy Correspondence: J. Javier Álvaro ([email protected]) Received: 1 April 2020 – Discussion started: 20 April 2020 Revised: 14 October 2020 – Accepted: 19 October 2020 – Published: 11 December 2020 Abstract. A geochemical comparison of early Palaeo- neither metamorphism nor penetrative deformation; on the zoic felsic magmatic episodes throughout the south- contrary, their unconformities are associated with foliation- western European margin of Gondwana is made and in- free open folds subsequently affected by the Variscan defor- cludes (i) Furongian–Early Ordovician (Toledanian) activ- mation.
    [Show full text]
  • Sandbian) K-Bentonites in Oslo, Norway T ⁎ Eirik G
    Palaeogeography, Palaeoclimatology, Palaeoecology 520 (2019) 203–213 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo A new age model for the Ordovician (Sandbian) K-bentonites in Oslo, Norway T ⁎ Eirik G. Balloa, , Lars Eivind Auglanda, Øyvind Hammerb, Henrik H. Svensena a Centre for Earth Evolution and Dynamics (CEED), University of Oslo, Pb. 1028, 0316 Oslo, Norway b Natural History Museum, University of Oslo, Pb. 1172, 0318 Oslo, Norway ARTICLE INFO ABSTRACT Keywords: During the Late Ordovician, large explosive volcanic eruptions deposited worldwide K-bentonites, including the Chronostratigraphy Millbrig and Deicke K-bentonites in North America and the Kinnekulle K-bentonite in Scandinavia. We have Sandbian-Katian boundary studied a classical locality in Oslo containing one of the most complete sections of K-bentonites in Europe. U-Pb dating In a 53 m section of Sandbian age, we discovered 33 individual K-bentonite beds, the most notable beds being Milankovitch the Kinnekulle and the upper Grimstorp K-bentonite. Magnetic susceptibility (MS) measurements on two in- Age model tervals show significant periodicity peaks interpreted as Milankovitch cycles and thus astronomically forced Kinnekulle changes in sediment supply and composition. These cycles fit remarkably well with both the expected Milankovitch periodicities for the Ordovician as well as the radiometric ages presented in this study and may represent one of the most convincing demonstrations of Milankovitch cycles from the lower Paleozoic so far. Five of the K-bentonites have been dated by high-precision chemical abrasion-thermal ionization mass spectrometry (CA-TIMS) U-Pb zircon geochronology, where the Kinnekulle K-bentonite gives an age of 454.06 ± 0.43 Ma.
    [Show full text]
  • SILURIAN TIMES NEWSLETTER of the INTERNATIONAL SUBCOMMISSION on SILURIAN STRATIGRAPHY (ISSS) (INTERNATIONAL COMMISSION on STRATIGRAPHY, ICS) No
    SILURIAN TIMES NEWSLETTER OF THE INTERNATIONAL SUBCOMMISSION ON SILURIAN STRATIGRAPHY (ISSS) (INTERNATIONAL COMMISSION ON STRATIGRAPHY, ICS) No. 27 (for 2019) Edited by ZHAN Renbin INTERNATIONAL UNION OF GEOLOGICAL SCIENCES President: CHENG Qiuming (Canada) Vice-Presidents: Kristine ASCH (Germany) William CAVAZZA (Italy) Secretary General: Stanley C. FINNEY (USA) Treasurer: Hiroshi KITAZATO (Japan) INTERNATIONAL COMMISSION ON STRATIGRAPHY Chairman: David A.T. HARPER (UK) Vice-Chairman: Brian T. HUBER (USA) Secretary General: Philip GIBBARD (UK) SUBCOMMISSION ON SILURIAN STRATIGRAPHY Chairman: Petr ŠTORCH (Czech Republic) Vice-Chairman: Carlo CORRADINI (Italy) Secretary: ZHAN Renbin (China) Other titular members: Anna ANTOSHKINA (Russia) Carlton E. BRETT (USA) Bradley CRAMER (USA) David HOLLOWAY (Australia) Jisuo JIN (Canada) Anna KOZŁOWSKA (Poland) Jiří KŘÍŽ (Czech Republic) David K. LOYDELL (UK) Peep MÄNNIK (Estonia) Michael J. MELCHIN (Canada) Axel MUNNECKE (Germany) Silvio PERALTA (Argentina) Thijs VANDENBROUCKE (Belgium) WANG Yi (China) Živilė ŽIGAITĖ (Lithuania) Silurian Subcommission website: http://silurian.stratigraphy.org 1 CONTENTS CHAIRMAN’S CORNER 3 ANNUAL REPORT OF SILURIAN SUBCOMMISSION FOR 2019 7 INTERNATIONAL COMMISSION ON STRATGRAPHY STATUTES 15 REPORTS OF ACTIVITIES IN 2019 25 1. Report on the ISSS business meeting 2019 25 2. Report on the 15th International Symposium on Early/Lower Vertebrates 28 3. Report on the 13th International Symposium on the Ordovician System in conjunction with the 3rd Annual Meeting of IGCP 653 32 GUIDELINES FOR THE ISSS AWARD: KOREN' AWARD 33 ANNOUNCEMENTS OF MEETINGS and ACTIVITIES 34 1. Lithological Meeting: GEOLOGY OF REEFS 34 SILURIAN RESEARCH 2019: NEWS FROM THE MEMBERS 36 RECENT PUBLICATIONS ON THE SILURIAN RESEARCH 67 MEMBERSHIP NEWS 77 1. List of all Silurian workers and interested colleagues 77 2.
    [Show full text]
  • University of Birmingham Carbon Isotope (13Ccarb) and Facies
    University of Birmingham Carbon isotope (13Ccarb) and facies variability at the Wenlock-Ludlow boundary (Silurian) of the Midland Platform, UK Blain, John Allan; Wheeley, James; Ray, David DOI: 10.1139/cjes-2015-0194 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Blain, JA, Wheeley, J & Ray, D 2016, 'Carbon isotope (13Ccarb) and facies variability at the Wenlock-Ludlow boundary (Silurian) of the Midland Platform, UK', Canadian Journal of Earth Science. https://doi.org/10.1139/cjes-2015-0194 Link to publication on Research at Birmingham portal Publisher Rights Statement: Publisher Version of Record available at: http://dx.doi.org/10.1139/cjes-2015-0194 Validated Feb 2016 General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document.
    [Show full text]
  • Polar Front Shift and Atmospheric CO During the Glacial Maximum of the Early Paleozoic Icehouse
    Polar front shift and atmospheric CO2 during the glacial maximum of the Early Paleozoic Icehouse Thijs R. A. Vandenbrouckea,b,c,1,2, Howard A. Armstronga,1, Mark Williamsd,e,1, Florentin Parisf, Jan A. Zalasiewiczd, Koen Sabbeg, Jaak Nõlvakh, Thomas J. Challandsa,i, Jacques Verniersb, and Thomas Servaisc aPalaeoClimate Group, Department of Earth Sciences, Durham University, Science Labs, Durham, DH1 3LE, United Kingdom; bResearch Unit Palaeontology, Department of Geology, Ghent University, Krijgslaan 281-S8, 9000 Ghent, Belgium; cGéosystèmes, Université Lille 1, Formation de Recherche en Evolution 3298 du Centre National de la Recherche Scientifique, Avenue Paul Langevin, bâtiment SN5, 59655 Villeneuve d’Ascq Cedex, France; dDepartment of Geology, University of Leicester, University Road, Leicester, LE1 7RH, United Kingdom; eBritish Geological Survey, Kingsley Dunham Centre, Keyworth, NG12 5GG, United Kingdom; fGéosciences, Université de Rennes I, Unité Mixte de Recherche 6118 du Centre National de la Recherche Scientifique, Campus de Beaulieu, 35042 Rennes-cedex, France; gProtistology and Aquatic Ecology, Department of Biology, Ghent University, Krijgslaan 281-S8, 9000 Ghent, Belgium; hInstitute of Geology, Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia; and iTotal E&P UK Limited, Geoscience Research Centre, Crawpeel Road, Aberdeen AB12 3FG, United Kingdom Edited by Jeffrey Kiehl, National Center for Atmospheric Research, Boulder, CO, and accepted by the Editorial Board July 1, 2010 (received for review March 16, 2010) Our new data address the paradox of Late Ordovician glaciation PAL (5). A GCM experiment parameterized with the same p × under supposedly high CO2 (8 to 22 PAL: preindustrial atmo- pCO2 value, high relative sea level, and a modern equator-to-pole spheric level).
    [Show full text]
  • GEOLOGIC TIME SCALE V
    GSA GEOLOGIC TIME SCALE v. 4.0 CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST HIST. ANOM. (Ma) ANOM. CHRON. CHRO HOLOCENE 1 C1 QUATER- 0.01 30 C30 66.0 541 CALABRIAN NARY PLEISTOCENE* 1.8 31 C31 MAASTRICHTIAN 252 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 Lopin- 254 32 C32 72.1 635 2A C2A PIACENZIAN WUCHIAPINGIAN PLIOCENE 3.6 gian 33 260 260 3 ZANCLEAN CAPITANIAN NEOPRO- 5 C3 CAMPANIAN Guada- 265 750 CRYOGENIAN 5.3 80 C33 WORDIAN TEROZOIC 3A MESSINIAN LATE lupian 269 C3A 83.6 ROADIAN 272 850 7.2 SANTONIAN 4 KUNGURIAN C4 86.3 279 TONIAN CONIACIAN 280 4A Cisura- C4A TORTONIAN 90 89.8 1000 1000 PERMIAN ARTINSKIAN 10 5 TURONIAN lian C5 93.9 290 SAKMARIAN STENIAN 11.6 CENOMANIAN 296 SERRAVALLIAN 34 C34 ASSELIAN 299 5A 100 100 300 GZHELIAN 1200 C5A 13.8 LATE 304 KASIMOVIAN 307 1250 MESOPRO- 15 LANGHIAN ECTASIAN 5B C5B ALBIAN MIDDLE MOSCOVIAN 16.0 TEROZOIC 5C C5C 110 VANIAN 315 PENNSYL- 1400 EARLY 5D C5D MIOCENE 113 320 BASHKIRIAN 323 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 1500 CALYMMIAN 6 C6 APTIAN LATE 20 120 331 6A C6A 20.4 EARLY 1600 M0r 126 6B C6B AQUITANIAN M1 340 MIDDLE VISEAN MISSIS- M3 BARREMIAN SIPPIAN STATHERIAN C6C 23.0 6C 130 M5 CRETACEOUS 131 347 1750 HAUTERIVIAN 7 C7 CARBONIFEROUS EARLY TOURNAISIAN 1800 M10 134 25 7A C7A 359 8 C8 CHATTIAN VALANGINIAN M12 360 140 M14 139 FAMENNIAN OROSIRIAN 9 C9 M16 28.1 M18 BERRIASIAN 2000 PROTEROZOIC 10 C10 LATE
    [Show full text]
  • (Terreneuvian) Blue Clay in the Northern Baltic Palaeobasin
    Estonian Journal of Earth Sciences, 2020, 69, 4, 200–213 https://doi.org/10.3176/earth.2020.14 Illitization of the lower Cambrian (Terreneuvian) Blue Clay in the northern Baltic Palaeobasin Kalle Kirsimäe, Peeter Somelar and Argo Jõeleht Department of Geology, University of Tartu, Ravila 14A, 50411 Tartu, Estonia; [email protected] Received 9 July 2020, accepted 2 September 2020, available online 11 November 2020 Abstract. The clay mineral composition of the lower Cambrian (Terreneuvian) Blue Clay (BC) in the northern Baltic Palaeobasin was studied. The proportion of illite in mixed­layer illite­smectite in the BC increases gradually from ca 85% in northern Estonia to ca 92% in central Latvia with the present burial depth increasing from a few hundred metres to ca 1000 m. The high level of illitization suggests a mature diagenetic grade of the sediments, which is typically achieved with burial at several kilometres. However, uncompact nature and thermally immature organic material suggest only shallow burial and maximum palaeotemperatures not exceeding 50 °C. The smectite­to­illite transformation in the BC was described using a kinetic modelling to assess the constraints on burial­driven illitization. Modelling results show that the present illitization level is possible to achieve by assuming burial during the Devonian to Permian prior to the erosion in the Mesozoic. The thickness of eroded sediments in the northern part of the basin was in this case only about 400–800 m. The smectite­to­illite transformation process in the BC in the northern Baltic Palaeobasin was controlled rather by time than by temperature.
    [Show full text]
  • (Floian) Conodont Fauna from the Eastern Cordillera of Peru (Central Andean Basin) Geologica Acta: an International Earth Science Journal, Vol
    Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España GUTIÉRREZ-MARCO, J.C.; ALBANESI, G.L.; SARMIENTO, G.N.; CARLOTTO, V. An Early Ordovician (Floian) Conodont Fauna from the Eastern Cordillera of Peru (Central Andean Basin) Geologica Acta: an international earth science journal, vol. 6, núm. 2, junio, 2008, pp. 147-160 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50513115004 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.6, Nº 2, June 2008, 147-160 DOI: 10.1344/105.000000248 Available online at www.geologica-acta.com An Early Ordovician (Floian) Conodont Fauna from the Eastern Cordillera of Peru (Central Andean Basin) 1 2 1 3,4 J.C. GUTIÉRREZ-MARCO G.L. ALBANESI G.N. SARMIENTO and V. CARLOTTO 1 Instituto de Geología Económica (CSIC-UCM). Facultad de Ciencias Geológicas 28040 Madrid, Spain. Gutiérrez-Marco E-mail: [email protected] Sarmiento E-mail: [email protected] 2 CONICET-CICTERRA, Museo de Paleontología Facultad de Ciencias Exactas, Físicas y Naturales, Universidad Nacional de Córdoba Casilla de Correo 1598, 5000 Córdoba, Argentina. E-mail: [email protected] 3 INGEMMET Avenida Canadá 1740, San Borja, Lima, Peru. E-mail: [email protected] 4 Departamento de Geología, Universidad Nacional San Antonio Abad del Cusco Avda. de la Cultura 733, Cuzco, Perú ABSTRACT Late Floian conodonts are recorded from a thin limestone lens intercalated in the lower part of the San José For- mation at the Carcel Puncco section (Inambari River), Eastern Cordillera of Peru.
    [Show full text]
  • International Chronostratigraphic Chart
    INTERNATIONAL CHRONOSTRATIGRAPHIC CHART www.stratigraphy.org International Commission on Stratigraphy v 2018/08 numerical numerical numerical Eonothem numerical Series / Epoch Stage / Age Series / Epoch Stage / Age Series / Epoch Stage / Age GSSP GSSP GSSP GSSP EonothemErathem / Eon System / Era / Period age (Ma) EonothemErathem / Eon System/ Era / Period age (Ma) EonothemErathem / Eon System/ Era / Period age (Ma) / Eon Erathem / Era System / Period GSSA age (Ma) present ~ 145.0 358.9 ± 0.4 541.0 ±1.0 U/L Meghalayan 0.0042 Holocene M Northgrippian 0.0082 Tithonian Ediacaran L/E Greenlandian 152.1 ±0.9 ~ 635 Upper 0.0117 Famennian Neo- 0.126 Upper Kimmeridgian Cryogenian Middle 157.3 ±1.0 Upper proterozoic ~ 720 Pleistocene 0.781 372.2 ±1.6 Calabrian Oxfordian Tonian 1.80 163.5 ±1.0 Frasnian Callovian 1000 Quaternary Gelasian 166.1 ±1.2 2.58 Bathonian 382.7 ±1.6 Stenian Middle 168.3 ±1.3 Piacenzian Bajocian 170.3 ±1.4 Givetian 1200 Pliocene 3.600 Middle 387.7 ±0.8 Meso- Zanclean Aalenian proterozoic Ectasian 5.333 174.1 ±1.0 Eifelian 1400 Messinian Jurassic 393.3 ±1.2 7.246 Toarcian Devonian Calymmian Tortonian 182.7 ±0.7 Emsian 1600 11.63 Pliensbachian Statherian Lower 407.6 ±2.6 Serravallian 13.82 190.8 ±1.0 Lower 1800 Miocene Pragian 410.8 ±2.8 Proterozoic Neogene Sinemurian Langhian 15.97 Orosirian 199.3 ±0.3 Lochkovian Paleo- 2050 Burdigalian Hettangian 201.3 ±0.2 419.2 ±3.2 proterozoic 20.44 Mesozoic Rhaetian Pridoli Rhyacian Aquitanian 423.0 ±2.3 23.03 ~ 208.5 Ludfordian 2300 Cenozoic Chattian Ludlow 425.6 ±0.9 Siderian 27.82 Gorstian
    [Show full text]
  • International Chronostratigraphic Chart
    INTERNATIONAL CHRONOSTRATIGRAPHIC CHART www.stratigraphy.org International Commission on Stratigraphy v 2014/02 numerical numerical numerical Eonothem numerical Series / Epoch Stage / Age Series / Epoch Stage / Age Series / Epoch Stage / Age Erathem / Era System / Period GSSP GSSP age (Ma) GSSP GSSA EonothemErathem / Eon System / Era / Period EonothemErathem / Eon System/ Era / Period age (Ma) EonothemErathem / Eon System/ Era / Period age (Ma) / Eon GSSP age (Ma) present ~ 145.0 358.9 ± 0.4 ~ 541.0 ±1.0 Holocene Ediacaran 0.0117 Tithonian Upper 152.1 ±0.9 Famennian ~ 635 0.126 Upper Kimmeridgian Neo- Cryogenian Middle 157.3 ±1.0 Upper proterozoic Pleistocene 0.781 372.2 ±1.6 850 Calabrian Oxfordian Tonian 1.80 163.5 ±1.0 Frasnian 1000 Callovian 166.1 ±1.2 Quaternary Gelasian 2.58 382.7 ±1.6 Stenian Bathonian 168.3 ±1.3 Piacenzian Middle Bajocian Givetian 1200 Pliocene 3.600 170.3 ±1.4 Middle 387.7 ±0.8 Meso- Zanclean Aalenian proterozoic Ectasian 5.333 174.1 ±1.0 Eifelian 1400 Messinian Jurassic 393.3 ±1.2 7.246 Toarcian Calymmian Tortonian 182.7 ±0.7 Emsian 1600 11.62 Pliensbachian Statherian Lower 407.6 ±2.6 Serravallian 13.82 190.8 ±1.0 Lower 1800 Miocene Pragian 410.8 ±2.8 Langhian Sinemurian Proterozoic Neogene 15.97 Orosirian 199.3 ±0.3 Lochkovian Paleo- Hettangian 2050 Burdigalian 201.3 ±0.2 419.2 ±3.2 proterozoic 20.44 Mesozoic Rhaetian Pridoli Rhyacian Aquitanian 423.0 ±2.3 23.03 ~ 208.5 Ludfordian 2300 Cenozoic Chattian Ludlow 425.6 ±0.9 Siderian 28.1 Gorstian Oligocene Upper Norian 427.4 ±0.5 2500 Rupelian Wenlock Homerian
    [Show full text]
  • Paleogeographic Maps Earth History
    History of the Earth Age AGE Eon Era Period Period Epoch Stage Paleogeographic Maps Earth History (Ma) Era (Ma) Holocene Neogene Quaternary* Pleistocene Calabrian/Gelasian Piacenzian 2.6 Cenozoic Pliocene Zanclean Paleogene Messinian 5.3 L Tortonian 100 Cretaceous Serravallian Miocene M Langhian E Burdigalian Jurassic Neogene Aquitanian 200 23 L Chattian Triassic Oligocene E Rupelian Permian 34 Early Neogene 300 L Priabonian Bartonian Carboniferous Cenozoic M Eocene Lutetian 400 Phanerozoic Devonian E Ypresian Silurian Paleogene L Thanetian 56 PaleozoicOrdovician Mesozoic Paleocene M Selandian 500 E Danian Cambrian 66 Maastrichtian Ediacaran 600 Campanian Late Santonian 700 Coniacian Turonian Cenomanian Late Cretaceous 100 800 Cryogenian Albian 900 Neoproterozoic Tonian Cretaceous Aptian Early 1000 Barremian Hauterivian Valanginian 1100 Stenian Berriasian 146 Tithonian Early Cretaceous 1200 Late Kimmeridgian Oxfordian 161 Callovian Mesozoic 1300 Ectasian Bathonian Middle Bajocian Aalenian 176 1400 Toarcian Jurassic Mesoproterozoic Early Pliensbachian 1500 Sinemurian Hettangian Calymmian 200 Rhaetian 1600 Proterozoic Norian Late 1700 Statherian Carnian 228 1800 Ladinian Late Triassic Triassic Middle Anisian 1900 245 Olenekian Orosirian Early Induan Changhsingian 251 2000 Lopingian Wuchiapingian 260 Capitanian Guadalupian Wordian/Roadian 2100 271 Kungurian Paleoproterozoic Rhyacian Artinskian 2200 Permian Cisuralian Sakmarian Middle Permian 2300 Asselian 299 Late Gzhelian Kasimovian 2400 Siderian Middle Moscovian Penn- sylvanian Early Bashkirian
    [Show full text]
  • Ordovician Graptolites from the Basal Part of the Palaeozoic Transgressive Sequence in the Karadere Area, Zonguldak Terrane, NW Turkey
    Estonian Journal of Earth Sciences, 2014, 63, 4, 227–232 doi: 10.3176/earth.2014.23 Ordovician graptolites from the basal part of the Palaeozoic transgressive sequence in the Karadere area, Zonguldak Terrane, NW Turkey M. Cemal Göncüoglua, Valeri Sachanskib, Juan Carlos Gutiérrez-Marcoc and Cengiz Okuyucud a METU, Department of Geological Engineering, 06531 Ankara,Turkey; [email protected] b UMG ‘St. Ivan Rilski’, Department of Geology and Geo-Information, Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria; [email protected] c Instituto de Geociencias (CSIC, UCM), José Antonio Novais 12, 28040 Madrid, Spain; [email protected] d Selcuk University, Department of Geological Engineering, Selcuk University, Konya, Turkey; [email protected] Received 10 June 2014, accepted 15 September 2014 Abstract. The Karadere area to the east of Safranbolu in NW Anatolia is one of the very few localities in Turkey where the contact between the Cadomian basement and the Lower Palaeozoic transgressive succession is well exposed. The Ordovician graptolite Rhabdinopora flabelliformis (Eichwald) ssp. was found in the basal part of the Bakacak Formation, indicating an Early to early Late Tremadocian age for the beginning of the Palaeozoic transgression in the Zonguldak terrane. A few metres above this occurrence, another horizon contains Paradelograptus cf. antiquus (T. S. Hall), which mainly ranges into the Late Tremadocian. Higher up in the Ordovician succession, a new graptolite bed confirms an early Darriwilian (Dw1) age for the middle part of the Karadere Formation with the occurrence of the biozonal index Levisograptus austrodentatus (Harris & Keble) and the first record of Tetragraptus cor (Strandmark) in the area.
    [Show full text]