North American Stratigraphic Code1
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Do Gssps Render Dual Time-Rock/Time Classification and Nomenclature Redundant?
Do GSSPs render dual time-rock/time classification and nomenclature redundant? Ismael Ferrusquía-Villafranca1 Robert M. Easton2 and Donald E. Owen3 1Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Coyoacán, México, DF, MEX, 45100, e-mail: [email protected] 2Ontario Geological Survey, Precambrian Geoscience Section, 933 Ramsey Lake Road, B7064 Sudbury, Ontario P3E 6B5, e-mail: [email protected] 3Department of Geology, Lamar University, Beaumont, Texas 77710, e-mail: [email protected] ABSTRACT: The Geological Society of London Proposal for “…ending the distinction between the dual stratigraphic terminology of time-rock units (of chronostratigraphy) and geologic time units (of geochronology). The long held, but widely misunderstood distinc- tion between these two essentially parallel time scales has been rendered unnecessary by the adoption of the global stratotype sections and points (GSSP-golden spike) principle in defining intervals of geologic time within rock strata.” Our review of stratigraphic princi- ples, concepts, models and paradigms through history clearly shows that the GSL Proposal is flawed and if adopted will be of disservice to the stratigraphic community. We recommend the continued use of the dual stratigraphic terminology of chronostratigraphy and geochronology for the following reasons: (1) time-rock (chronostratigraphic) and geologic time (geochronologic) units are conceptually different; (2) the subtended time-rock’s unit space between its “golden spiked-marked” -
Geological Processes and Evolution
GEOLOGICAL PROCESSES AND EVOLUTION J.W. HEAD1, R. GREELEY2, M.P. GOLOMBEK3, W.K. HARTMANN4, E. HAUBER5, R. JAUMANN5, P. MASSON6, G. NEUKUM5, L.E. NYQUIST7 and M.H. CARR8 1Department of Geological Sciences, Brown University, Providence, RI 02912 USA 2Department of Geology, Arizona State University, Tempe, AZ 85287 USA 3Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109 USA 4Planetary Science Institute, Tucson, AZ 85705 USA 5DLR Institute of Space Sensor Technology and Planetary Exploration, Rutherfordstrasse 2, 12484 Berlin-Aldershof, Germany 6University of Paris-Sud, 91405, Orsay Cedex France 7Johnson Space Center, Houston TX 77058 USA 8US Geological Survey, Branch of Astrogeological Studies, 345 Middlefield Road, Menlo Park, CA 94025 USA Received:14 February 2001; accepted:12 March 2001 Abstract. Geological mapping and establishment of stratigraphic relationships provides an overview of geological processes operating on Mars and how they have varied in time and space. Impact craters and basins shaped the crust in earliest history and as their importance declined, evidence of extensive regional volcanism emerged during the Late Noachian. Regional volcanism characterized the Early Hesperian and subsequent to that time, volcanism was largely centered at Tharsis and Elysium, con- tinuing until the recent geological past. The Tharsis region appears to have been largely constructed by the Late Noachian, and represents a series of tectonic and volcanic centers. Globally distributed structural features representing contraction characterize the middle Hesperian. Water-related pro- cesses involve the formation of valley networks in the Late Noachian and into the Hesperian, an ice sheet at the south pole in the middle Hesperian, and outflow channels and possible standing bodies of water in the northern lowlands in the Late Hesperian and into the Amazonian. -
The Astronomical Theory of Climate and the Age of the Brunhes-Matuyama Magnetic Reversal
EPSL ELSEVIER Earth and Planetary Science Letters 126 (1994) 91-108 The astronomical theory of climate and the age of the Brunhes-Matuyama magnetic reversal Franck C. Bassinot a,1, Laurent D. Labeyrie b, Edith Vincent a, Xavier Quidelleur c Nicholas J. Shackleton d, Yves Lancelot a a Laboratoire de Gdologie du Quaternaire, CNRS-Luminy, Case 907, 13288 Marseille cddex 09, France b Centre des Faibles Radioactivit&, CNRS/CEA, Avenue de la Terrasse, BP 1, 91198 Gif-sur-Yvette, France c Institut de Physique du Globe, Laboratoire de Pal~omagn&isme, 4 Place Jussieu, 75252 Paris c~dex 05, France d Department of Quaternary Research, The Godwin Laboratory, Free School Lane, Cambridge CB2 3RS, UK Received 3 November 1993; revision accepted 30 May 1994 Abstract Below oxygen isotope stage 16, the orbitally derived time-scale developed by Shackleton et al. [1] from ODP site 677 in the equatorial Pacific differs significantly from previous ones [e.g., 2-5], yielding estimated ages for the last Earth magnetic reversals that are 5-7% older than the K/Ar values [6-8] but are in good agreement with recent Ar/Ar dating [9-11]. These results suggest that in the lower Brunhes and upper Matuyama chronozones most deep-sea climatic records retrieved so far apparently missed or misinterpreted several oscillations predicted by the astronomical theory of climate. To test this hypothesis, we studied a high-resolution oxygen isotope record from giant piston core MD900963 (Maldives area, tropical Indian Ocean) in which precession-related oscillations in t~180 are particularly well expressed, owing to the superimposition of a local salinity signal on the global ice volume signal [12]. -
Victorian Popular Science and Deep Time in “The Golden Key”
“Down the Winding Stair”: Victorian Popular Science and Deep Time in “The Golden Key” Geoffrey Reiter t is sometimes tempting to call George MacDonald’s fantasies “timeless”I and leave it at that. Such is certainly the case with MacDonald’s mystical fairy tale “The Golden Key.” Much of the criticism pertaining to this work has focused on its more “timeless” elements, such as its intrinsic literary quality or its philosophical and theological underpinnings. And these elements are not only important, they truly are the most fundamental elements needed for a full understanding of “The Golden Key.” But it is also important to remember that MacDonald did not write in a vacuum, that he was in fact interested in and engaged with many of the pressing issues of his day. At heart always a preacher, MacDonald could not help but interact with these issues, not only in his more openly didactic realistic novels, but even in his “timeless” fantasies. In the Victorian period, an era of discovery and exploration, the natural sciences were beginning to come into their own as distinct and valuable sources of knowledge. John Pridmore, examining MacDonald’s view of nature, suggests that MacDonald saw it as serving a function parallel to the fairy tale or fantastic story; it may be interpreted from the perspective of Christian theism, though such an interpretation is not necessary (7). Björn Sundmark similarly argues that in his works “MacDonald does not contradict science, nor does he press a theistic interpretation onto his readers” (13). David L. Neuhouser has concluded more assertively that while MacDonald was certainly no advocate of scientific pursuits for their own sake, he believed science could be of interest when examined under the aegis of a loving God (10). -
Calendar Year Age Estimates of Allerød-Younger Dryas Sea-Level
JOURNAL OF QUATERNARY SCIENCE (2004) 19(5) 443–464 Copyright ß 2004 John Wiley & Sons, Ltd. Published online in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/jqs.846 Calendar year age estimates of Allerød–Younger Dryas sea-level oscillations at Os, western Norway ØYSTEIN S. LOHNE,1,2* STEIN BONDEVIK,3 JAN MANGERUD1,2 and HANS SCHRADER1 1 Department of Earth Science, Alle´gaten 41, N-5007 Bergen, Norway 2 The Bjerknes Centre for Climate Research, University of Bergen, Norway 3 Department of Geology, University of Tromsø, Dramsveien 201, N-9037 Tromsø, Norway Lohne, Ø. S., Bondevik, S., Mangerud, J. and Schrader, H. 2004. Calendar year age estimates of Allerød—Younger Dryas sea-level oscillations at Os, western Norway. J. Quaternary Sci., Vol. 19 pp. 443–464. ISSN 0267-8179. Received 30 September 2003; Revised 2 February 2004; Accepted 17 February 2004 ABSTRACT: A detailed shoreline displacement curve documents the Younger Dryas transgression in western Norway. The relative sea-level rise was more than 9 m in an area which subsequently experienced an emergence of almost 60 m. The sea-level curve is based on the stratigraphy of six isolation basins with bedrock thresholds. Effort has been made to establish an accurate chronology using a calendar year time-scale by 14C wiggle matching and the use of time synchronic markers (the Vedde Ash Bed and the post-glacial rise in Betula (birch) pollen). The sea-level curve demonstrates that the Younger Dryas transgression started close to the Allerød–Younger Dryas transition and that the high stand was reached only 200 yr before the Younger Dryas–Holocene boundary. -
All These Fantastic Cultures? Research History and Regionalization in the Late Palaeolithic Tanged Point Cultures of Eastern Europe
European Journal of Archaeology 23 (2) 2020, 162–185 This is an Open Access article, distributed under the terms of the Creative Commons Attribution- NonCommercial-ShareAlike licence (http://creativecommons.org/licenses/by-nc-sa/4.0/), which permits non- commercial re-use, distribution, and reproduction in any medium, provided the same Creative Commons licence is included and the original work is properly cited. The written permission of Cambridge University Press must be obtained for commercial re-use. All these Fantastic Cultures? Research History and Regionalization in the Late Palaeolithic Tanged Point Cultures of Eastern Europe 1 2 3 LIVIJA IVANOVAITĖ ,KAMIL SERWATKA ,CHRISTIAN STEVEN HOGGARD , 4 5 FLORIAN SAUER AND FELIX RIEDE 1Museum of Copenhagen, Denmark 2Archaeological and Ethnographic Museum of Łódź, Poland 3University of Southampton, United Kingdom 4University of Cologne, Köln, Germany 5Aarhus University, Højbjerg, Denmark The Late Glacial, that is the period from the first pronounced warming after the Last Glacial Maximum to the beginning of the Holocene (c. 16,000–11,700 cal BP), is traditionally viewed as a time when northern Europe was being recolonized and Late Palaeolithic cultures diversified. These cultures are characterized by particular artefact types, or the co-occurrence or specific relative frequencies of these. In north-eastern Europe, numerous cultures have been proposed on the basis of supposedly different tanged points. This practice of naming new cultural units based on these perceived differences has been repeatedly critiqued, but robust alternatives have rarely been offered. Here, we review the taxonomic landscape of Late Palaeolithic large tanged point cultures in eastern Europe as currently envisaged, which leads us to be cautious about the epistemological validity of many of the constituent groups. -
Geochronology Database for Central Colorado
Geochronology Database for Central Colorado Data Series 489 U.S. Department of the Interior U.S. Geological Survey Geochronology Database for Central Colorado By T.L. Klein, K.V. Evans, and E.H. DeWitt Data Series 489 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: T.L. Klein, K.V. Evans, and E.H. DeWitt, 2009, Geochronology database for central Colorado: U.S. Geological Survey Data Series 489, 13 p. iii Contents Abstract ...........................................................................................................................................................1 Introduction.....................................................................................................................................................1 -
Soils in the Geologic Record
in the Geologic Record 2021 Soils Planner Natural Resources Conservation Service Words From the Deputy Chief Soils are essential for life on Earth. They are the source of nutrients for plants, the medium that stores and releases water to plants, and the material in which plants anchor to the Earth’s surface. Soils filter pollutants and thereby purify water, store atmospheric carbon and thereby reduce greenhouse gasses, and support structures and thereby provide the foundation on which civilization erects buildings and constructs roads. Given the vast On February 2, 2020, the USDA, Natural importance of soil, it’s no wonder that the U.S. Government has Resources Conservation Service (NRCS) an agency, NRCS, devoted to preserving this essential resource. welcomed Dr. Luis “Louie” Tupas as the NRCS Deputy Chief for Soil Science and Resource Less widely recognized than the value of soil in maintaining Assessment. Dr. Tupas brings knowledge and experience of global change and climate impacts life is the importance of the knowledge gained from soils in the on agriculture, forestry, and other landscapes to the geologic record. Fossil soils, or “paleosols,” help us understand NRCS. He has been with USDA since 2004. the history of the Earth. This planner focuses on these soils in the geologic record. It provides examples of how paleosols can retain Dr. Tupas, a career member of the Senior Executive Service since 2014, served as the Deputy Director information about climates and ecosystems of the prehistoric for Bioenergy, Climate, and Environment, the Acting past. By understanding this deep history, we can obtain a better Deputy Director for Food Science and Nutrition, and understanding of modern climate, current biodiversity, and the Director for International Programs at USDA, ongoing soil formation and destruction. -
Career Stage, Time Spent on the Road, and Truckload Driver Attitudes
CAREER STAGE, TIME SPENT ON THE ROAD, AND TRUCKLOAD DRIVER ATTITUDES James C. McElroy Julene M. Rodriguez Gene C. Griffin Paula C. Morrow Michael G. Wilson UGPTI Staff Paper No. 113 May 1993 Career Stage, Time Spent on the Road, And Truckload Driver Attitudes1 James C. McElroy, Department of Management Iowa State University Julene M. Rodriguez and Gene C. Griffin Upper Great Plains Transportation Institute North Dakota State University Paula C. Morrow Industrial Relations Center Iowa State University Michael G. Wilson Iowa State University Address correspondence to: James C. McElroy, Chair Departments of Management, Marketing, and Transportation & Logistics Iowa State University 300 Carver Hall Ames, Iowa 50011 1The authors would like to thank their respective institutions for support, Drs. Ben Allen, Michael Crum, Richard Poist, and David Shrock for their comments and suggestions and Brenda Lantz for her assistance with data analysis. TABLE OF CONTENTS Page CAREER STAGE, TIME SPENT ON THE ROAD, AND TRUCKLOAD DRIVER ATTITUDES ......................................... 1 Determinants of Work-Related Attitudes ......................................... 2 Propositions ................................................................ 3 Method ................................................................... 3 Sample ................................................................ 3 Independent Variables ...................................................... 4 Dependent Variables ....................................................... 4 Research -
(Foram in Ifers, Algae) and Stratigraphy, Carboniferous
MicropaIeontoIogicaI Zonation (Foramin ifers, Algae) and Stratigraphy, Carboniferous Peratrovich Formation, Southeastern Alaska By BERNARD L. MAMET, SYLVIE PINARD, and AUGUSTUS K. ARMSTRONG U.S. GEOLOGICAL SURVEY BULLETIN 2031 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Text and illustrations edited by Mary Lou Callas Line drawings prepared by B.L. Mamet and Stephen Scott Layout and design by Lisa Baserga UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Mamet, Bernard L. Micropaleontological zonation (foraminifers, algae) and stratigraphy, Carboniferous Peratrovich Formation, southeastern Alaska / by Bernard L. Mamet, Sylvie Pinard, and Augustus K. Armstrong. p. cm.-(U.S. Geological Survey bulletin ; 2031) Includes bibtiographical references. 1. Geology, Stratigraphic-Carboniferous. 2. Geology-Alaska-Prince of Wales Island. 3. Foraminifera, Fossil-Alaska-Prince of Wales Island. 4. Algae, Fossil-Alaska-Prince of Wales Island. 5. Paleontology- Carboniferous. 6. Paleontology-Alaska-Prince of Wales Island. I. Pinard, Sylvie. II. Armstrong, Augustus K. Ill. Title. IV. Series. QE75.B9 no. 2031 [QE671I 557.3 s--dc20 [551.7'5'097982] 92-32905 CIP CONTENTS Abstract -
International Chronostratigraphic Chart
INTERNATIONAL CHRONOSTRATIGRAPHIC CHART www.stratigraphy.org International Commission on Stratigraphy v 2015/01 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 ~ 720 Pleistocene 0.781 372.2 ±1.6 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 11.63 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 -
What Is the Zuni Sandstone Today
What is the ZuniSandstone Today -- 100 Years AfterDutton? A Discussion andReview of JurassicStratigraphy in West-Central New Mexico NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES OPEN-FILE REPORT 174 by Orin J. Anderson New MexicoBureau of Minesand Mineral Resources 1983 Contents Introduction P. 1 Discussion P. 3 Todilto Limestone - Navajo Sandstone P- 5 San Rafael Group Defined P. 8 Glen CanyonGroup Defined P. 9 MorrisonFormation Subdivided p. 14 Cow SpringsSandstone p. 17 1956 Memorandum from C. H. Dane p. 22 Zuni Sandstone Redefined p. 26 Summary p. 28 ReferencesCited p. 30 Figures Fig. 1 Index map of study area Fig. 2 Stratigraphic nomenclature and correlationchart- 1885 to present Fig. 3 Measured section at type locality of Zuni Sandstone (inside back cover) Fig. 4 Stratigraphiccross-section-Dakota and Zuni sandstones, showing southward thinning of Zuni Sandstone (inside back cover) WHAT IS THE ZUNISANDSTONE TODAY -- 100 YEARS AFTER DUTTON? A DISCUSSION AND REVIEW OF JURASSICSTRATIGRAPHY IN WEST-CENTRAL NEW MEXICO Introduction The massivesequence(s) of light colored, cross bedded sandstonesthat underliethe Dakota Sandstone (Upper Cretaceous) in west-central New Mexico and northeasternArizona were first described and namedby CaptainClarence E. Dutton ofthe U. S. Army Ordinance Corps. His reportentitled "Mount Taylor and the Zuni Plateau"(Dutton, 1885) contains an account of the stratigraphy and structure of those two areas and theimmediately surrounding region(the Zuni Plateau is thepresent day Zuni uplift). In thereport he described a "massive bright redsandstone" that overlies the "basal Triassediments" (the present day ChinleFormation) in theFort Wingate area; this unit henamed "provisionally"the Wingate Sandstone. Overlyingthe Wingate Dutton recognized "a series ofsandstones and sandy shales .....