Stratigraphy, Structure, and Economic Geology of the Iliamna Quadrangle, Alaska
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Danise Et Al 2020 Gondwana Research.Docx.Pdf
University of Plymouth PEARL https://pearl.plymouth.ac.uk Faculty of Science and Engineering School of Geography, Earth and Environmental Sciences 2020-06 Isotopic evidence for partial geochemical decoupling between a Jurassic epicontinental sea and the open ocean Danise, S http://hdl.handle.net/10026.1/15995 10.1016/j.gr.2019.12.011 Gondwana Research Elsevier BV All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. Please cite as: Danise, S., Price, G.D., Alberti, M., Holland S.M. 2020 Isotopic evidence for partial geochemical decoupling between a Jurassic epicontinental sea and the open ocean. Gondwana Research, 82, 97–107. Isotopic evidence for partial geochemical decoupling between a Jurassic epicontinental sea and the open ocean Silvia Danise a,b,⁎, Gregory D. Price a, Matthias Alberti c, Steven M. Holland d a School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, Devon PL4 8AA, UK b Dipartimento di Sicenze della Terra, Università degli Studi di Firenze, via La Pira 4, 50121 Firenze, Italy c Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Straße 10, 24118 Kiel, Germany d Department of Geology, University of Georgia, Athens, GA 30602-2501, USA a b s t r a c t Article history: Received 21 October 2019 Received in revised form 20 December 2019 Accepted 20 December 2019 Available online 30 January 2020 Handling Editor: A. -
Sequence Stratigraphic Expression of Flexural Subsidence: Middle
SEQUENCE STRATIGRAPHIC EXPRESSION OF FLEXURAL SUBSIDENCE: MIDDLE JURASSIC TWIN CREEK LIMESTONE, WYOMING, U.S.A. by BOLTON HOWES (Under the Direction of Steve Holland) ABSTRACT In southwestern Wyoming, the Bajocian to Callovian Twin Creek Limestone records the incipient deposition on a foreland basin in the Sundance Seaway. The sequence stratigraphy of the Twin Creek Limestone is described in the Wyoming Range of southwestern Wyoming, and the geometry of the foreland basin is described mathematically based on estimates flexural rigidity of the underlying crust and the subsidence caused by a thrust load in central Idaho. Four depositional sequences are described. These sequences are correlated to the Bighorn Basin based on existing biostratigraphic correlations and descriptions of the sequence stratigraphic architecture of Middle Jurassic strata in the Bighorn Basin. Modeling of the flexural subsidence of the foreland basin indicates that to account for the geometry of the foreland basin some form of long-wavelength subsidence must be superimposed on the flexural subsidence associated with the thrust load in central Idaho. INDEX WORDS: carbonate rocks; Jurassic; foreland basin; sequence stratigraphy SEQUENCE STRATIGRAPHIC EXPRESSION OF FLEXURAL SUBSIDENCE: MIDDLE JURASSIC TWIN CREEK LIMESTONE, WYOMING, U.S.A. By BOLTON HOWES B.A., Macalester College, 2015 A Thesis Submitted to the Graduate Faculty of The University of Georgia in Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE ATHENS, GEORGIA 2017 © 2017 Bolton Howes All Rights Reserved SEQUENCE STRATIGRAPHIC EXPRESSION OF FLEXURAL SUBSIDENCE: MIDDLE JURASSIC TWIN CREEK LIMESTONE, WYOMING, U.S.A. by BOLTON HOWES Major Professor: Steven M. Holland Committee: L. Bruce Railsback David S. -
Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) 163-211 ©Geol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 1993 Band/Volume: 136 Autor(en)/Author(s): Meister Christian, Böhm Florian Artikel/Article: Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) 163-211 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Jb. Geol. B.-A. ISSN 0016-7800 Band 136 S.163-211 Wien, Juli 1993 Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) By CHRISTIAN MEISTER & FLORIAN BÖHM *) With 14 Text-Figures and 9 Plates Oslerreich Salzburg Oberöslerreich Nördliche Kalkalpen Lias Ammoniten Oslerreichische Karle 1. 50.000 Biostratigraphie BI/1l1er94, 95, 96,126 Palaeogeographie Contents Zusammenfassung 163 Abstract. .. 164 Resume 164 1. Introduction 164 2. Geographical and Geological Framework 164 3. Lithological Description and Qualitative/Quantitative Ammonite Distributions 165 3.1. Schmiedwirt Quarry 165 3.2. Breitenberg Quarry 166 3.3. Rotkogel Outcrop 166 3.4. Rötelstein Outcrop 168 4. Systematic Palaeontology 169 PhylioceratinaARKELL 1950 171 LytoceratinaHYATT1889 174 Ammonitina HYATT 1889 175 5. Biostratigraphical Framework 184 5.1. Sinemurian 184 5.1.1. Early Sinemurian 184 5.1.2. Late Sinemurian 184 5.2. Pliensbachian 184 5.2.1. Early Pliensbachian (Carixian) 184 5.2.2. Late Pliensbachian (Domerian) 186 5.3. Toarcian 186 6. Faunal Composition and Palaeogeographical Remarks 189 7. Conclusion 190 Acknowledgements 190 References 208 Oberostalpine Liasammoniten aus der Adnetformation (Nördlichen Kalkalpen) Zusammenfassung Das Oberostalpin spielt eine Schlüsselrolle für das Verständnis der Verteilungsmuster der jurassischen Ammonitenfaunen und für die Fixierung genauer biostratigraphischer Korrelationen zwischen Tethyaler und Euroborealer Faunenprovinz. -
Cp-2020-99-Manuscript-Version2.Pdf
Million-year-scale alternation of warm-humid and semi-arid periods as a mid-latitude climate mode in the Early Jurassic (Late Sinemurian, Laurasian Seaway) 5 Thomas Munier1,2, Jean-François Deconinck1, Pierre Pellenard1, Stephen P. Hesselbo3, James B. Riding4, Clemens V. Ullmann3, Cédric Bougeault1, Mathilde Mercuzot5, Anne-Lise Santoni1, Émilia Huret6, Philippe Landrein6 10 1 Biogéosciences, UMR 6282, uB/CNRS, Université Bourgogne Franche-Comté, 6 Boulevard Gabriel, 21000 Dijon, France. 2 ISTeP, UMR 7193, SU/CNRS, Sorbonne Université, 4 Place Jussieu, 75005 Paris, France. 3 Camborne School of Mines and the Environment and Sustainability Institute, University of Exeter, Penryn Campus, Penryn, Cornwall TR10 9FE, UK. 4 British Geological Survey, Keyworth, Nottingham NG12 5GG, UK. 15 5 Géosciences Rennes, UMR 6118, UR/CNRS, Université Rennes 1, Campus de Beaulieu, CS 74205 35042 Rennes cedex, France. 6 Agence Nationale pour la gestion des déchets radioactifs, Centre de Meuse/Haute-Marne, RD 960, 55290 Bure, France. Correspondence to: Thomas Munier ([email protected]) 20 Abstract. Clay mineral and stable isotope (C, O) data are reported from the upper Sinemurian (Lower Jurassic) of the Cardigan Bay Basin (Llanbedr [Mochras Farm] borehole, northwest Wales) and the Paris Basin (Montcornet borehole, northern France) to highlight the prevailing environmental and climatic conditions. In both basins, located at similar palaeolatitudes of 30– 35°N, the clay mineral assemblages comprise chlorite, illite, illite-smectite mixed-layers (R1 I-S), smectite, and kaolinite in various proportions. Because the influence of burial diagenesis and authigenesis is negligible in both boreholes, the clay 25 minerals are interpreted to be derived from the erosion of the Caledonian and Variscan massifs, including their basement and pedogenic cover. -
By Robert L. Detterman-"
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Mesozoic blogeography of southern Alaska with implications for the paleogeography By Robert L. Detterman-"- Open-File Report 88-662 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS. Menlo Park, California CONTENTS Introducti on.................................................... 1 Tectonostratigraphic terranes...................................2 Biogeography....................................................3 Triassic biogeography........................................4 Jurassic biogeography........................................5 Hettangian................................................5 Sinemurian................................................5 Pliensbachian.............................................6 Toarcian..................................................6 Middle Jurassic...........................................7 Aalenian..................................................7 Bajoci an..................................................7 Bathonian.................................................8 Callovlan.................................................8 Oxfordian, Kimmeridgian, and Tithonian....................8 Cretaceous...................................................9 Berriasian and Valanginian...............................10 Hauterivian and Barremian................................10 -
Dimorphinites (Ammonoidea, Jurassic, Upper Bajocian) in the Precordillera of Northern Chile
DIMORPHINITES (AMMONOIDEA, JURASSIC, UPPER BAJOCIAN) IN THE PRECORDILLERA OF NORTHERN CHILE SIXTO R. FERNA´ NDEZ-LO´ PEZ1 AND GUILLERMO B. CHONG DIAZ2 1Departamento de Paleontologı´a, Facultad de Ciencias Geolo´gicas (UCM) and Instituto de Geologı´a Econo´mica (CSIC-UCM), Madrid 28040, Spain, ,[email protected].; and 2Departamento de Ciencias Geolo´gicas, Universidad Cato´lica del Norte, Antofagasta, Chile, ,[email protected]. This pdf file is licensed for distribution in the form of electronic reprints and by way of personal or institu- tional websites authorized by the author(s). A copyright license has been purchased to make this possible. Journal of Paleontology, 85(3), 2011, p. 395–405 Copyright ’ 2011, The Paleontological Society 0022-3360/11/0085-0395$03.00 DIMORPHINITES (AMMONOIDEA, JURASSIC, UPPER BAJOCIAN) IN THE PRECORDILLERA OF NORTHERN CHILE SIXTO R. FERNA´ NDEZ-LO´ PEZ1 AND GUILLERMO B. CHONG DIAZ2 1Departamento de Paleontologı´a, Facultad de Ciencias Geolo´gicas (UCM) and Instituto de Geologı´a Econo´mica (CSIC-UCM), Madrid 28040, Spain, ,[email protected].; and 2Departamento de Ciencias Geolo´gicas, Universidad Cato´lica del Norte, Antofagasta, Chile, ,[email protected]. ABSTRACT—A new upper Bajocian ammonite assemblage containing the morphoceratids Dimorphinites dimorphus (d’Orbigny) and Vigoriceras defrancei (d’Orbigny) is reported from the circum-Pacific area. These ammonites were found at the top of the Torcazas Formation, in the Quebrada San Pedro area, Precordillera of northern Chile. Taphonomic, systematic, and paleobiogeographic data confirm these dimorphs were part of indigenous populations within the Tarapaca Basin, belonging to the same demic biospecies: Dimorphinites defrancei (d’Orbigny). -
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Palaeontologia Electronica http://palaeo-electronica.org NEW MIDDLE AND UPPER JURASSIC BELEMNITE ASSEMBLAGES FROM WEST ANTARCTICA (LATADY GROUP, ELLSWORTH LAND): TAXONOMY AND PALEOBIOGEOGRAPHY A. Brian Challinor and Dan C.H. Hikuroa A. Brian Chalinor. Department of Earth Sciences, University of Waikato, Private Bag 3105, Hamilton, New Zealand. [email protected] Dan C.H. Hikuroa. Department of Geology, University of Auckland, Private Bag 92019, Auckland, New Zealand (corresponding author). [email protected] ABSTRACT Six belemnite genera and up to 24 species (some informal) represented mainly by moulds are recorded from the Middle and Late Jurassic Latady Group, Ellsworth Land, West Antarctica. Belemnopsis and Hibolithes are moderately abundant, Dicoelites, Duvalia, Produvalia, Pachyduvalia, and Rhopaloteuthis are rare. The assemblages are best described as: a sparse aff. Brevibelus-Hibolithes fauna (Bajocian); a Belemnopsis fauna with rare Hibolithes, Duvaliidae and Dicoelitidae (late Bathonian-Oxfordian); and a more abundant fauna of Belemnopsis and Hibolithes, with less common Duvaliidae (Kimmeridgian-Tithonian). The Duvaliidae and short grooved Hibolithes likely migrated from Madagascar to Ellsworth Land via a trans-Gondwana seaway. Most Hibolithes are endemic to the region; they resemble and may be in part conspecific with the New Zealand Hibolithes arkelli-H. marwicki group (middle Tithonian). They appeared first in Ellsworth Land and migrated to New Zealand. The Belemnopsis are also endemic. One group resembles the New Zealand Belemnopsis annae-B. stevensi-B. keari group of the New Zealand Heterian Stage (Callovian to Kimmeridgian) and may have appeared first in Ellsworth Land. A second group of small robust Belemnopsis resem- bles broadly similar forms from the early Callovian and Kimmeridgian of New Zealand. -
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SINEMURIAN (EARLY JURASSIC) STRATIGRAPHY AT LAST CREEK, BRITISH COLUMBIA AND FIVE CARD DRAW, NEVADA: PALEONTOLOGY AND ENVIRONMENTAL IMPLICATIONS by PENGFEI HOU M.Sc., China University of Petroleum (Beijing), 2012 B.Sc., China University of Geosciences (Beijing), 2009 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE in THE FACULTY OF GRADUATE AND POSTDOCTORAL STUDIES (Geological Sciences) THE UNIVERSITY OF BRITISH COLUMBIA (Vancouver) August 2014 © Pengfei Hou, 2014 ABSTRACT Over 400 ammonite specimens were collected from the Last Creek Formation in Last Creek, British Columbia and the Sunrise Formation in Five Card Draw, Nevada. A detailed taxonomic study from the Involutum Zone to the lower part of the Harbledownense Zone of the Sinemurian is presented. At least 38 species are identified and described, distributed amongst 15 genera and 5 families. Three species are introduced as new: Tipperoceras n. sp. A, Tmaegoceras obesus n. sp., Arnioceras n. sp. A. Also, Echioceratidae gen. et sp. indet. is tentatively introduced as a new species and genus. The following zones of the current Sinemurian zonation for western North America (Taylor et al., 2001) can be recognized, based on the stratigraphical distribution of the taxa identified, namely the Involutum, Leslei, Carinatum and Harbledownense zones in ascending order. The Jamesi Zone placed between the last two by Taylor et al. (2001) cannot be recognized in the study areas in either Canada or the United States and therefore it is removed from the current zonation scheme. A revised zonation and definition of the zones, with precise correlation to the primary standard northwest European zonation, are provided. -
Oxfordian and Late Callovian Ammonite Faunas and Biostratigraphy of the Neuquén-Mendoza and Tarapacá Basins (Jurassic, Ammonoidea, Western South-America)
Boletín del Instituto de Fisiografía y Geología 76(1-2), 2006. OXFORDIAN AND LATE CALLOVIAN AMMONITE FAUNAS AND BIOSTRATIGRAPHY OF THE NEUQUÉN-MENDOZA AND TARAPACÁ BASINS (JURASSIC, AMMONOIDEA, WESTERN SOUTH-AMERICA) Horacio PARENT Boletín Parent H., 2006. Oxfordian and late Callovian ammonite faunas and biostratigraphy of the Neuquén-Mendoza del Instituto de and Tarapacá basins (Jurassic, Ammonoidea, western South-America). Boletín del Instituto de Fisiografía y Fisiografía y Geología Geología 76(1-2): 1-70. Rosario, 01-10-2006. ISSN 1666-115X. Abstract.- During the Jurassic Period in the western border of Gondwana settled the Neuquén-Mendoza and Tarapacá basins, separated by the “Antofagasta Land”. In these basins there is a thick record of marine rocks with ammonites of the interval late Callovian-late Oxfordian (considering the Oxfordian/Kimmeridgian boundary at the base of the Platynota Zone of the primary international chronostratigraphic scale). The rocks of this interval are included in the Lotena, La Manga, Barda Negra (subsurface) and Auquilco formations. The ammonite faunas of the Neuquén-Mendoza Basin, their stratigraphic distribution and their relationships with those of the Tarapacá Basin and other regions of the world were poorly known in this interval of the Jurassic. In this report are presented the results of the first comprehensive study of the ammonite faunas and their biostratigraphy in these basins. The name Araucanian Sea is here introduced for the marine system of the Neuquén-Mendoza Basin, and Tarapacá Sea for the marine system of the homonymous basin. A new formal biostratigraphic classification is introduced for the Neuquén-Mendoza Basin, based on the revision of all the antecedents published, description of several species of ammonites and analysis of their succession. -
Middle Jurassic, Bajocian, Bathonian, Ammonitina, Biostratigraphy, Biochronology, Andes, South-America, Chile
FERNANDEZ-LOPEZ S., CHONG G., QUINZIO L.A. & WILKE H.G. 1994. The Upper Bajocian and Bathonian in the Cordillera de Domeyko, North-Chilean Precordillera : sedimentological and biostratigraphical results. [Le Ba jocien superieur et le Bathonien de la CordiIIere de Domeyko, PrecordilIere Nord-Chilienne : resultats sedimento logiques et biostratigraphiquesl. ABSTRACT The Jurassic ammonites of the CordiIIera de Domeyko have been studied in several monographies. The classic memoirs of Steinmann (1881), Tornquist (1898), Burckhardt (1903) and Stehn (1923) are particularly relevant. However, the biostratigraphic problems concerning stage boundaries arisen only in recent dates. New sedimentolo gical and biostratigraphical data have been obtained in relation to the BajocianlBathonian of this region. Several sections have been studied in two separate areas : Caracoles and Sierra de Varas. More than one thousand ammonites were collected in situ from these localities. Facies analysis shows that sedimentation during Late Bajocian and Bathonian occurs in a marine environment on a carbonate platform with abundant siliciclastic supply. Facies distribution was controlled by structural segmentation of the platform and processes of differential subsidence. The stratigraphical-sedimentological results together with taphonomical-palaeoecological observations are a diagnostic tool for sequence analysis. The successive ammonite assemblages which were found have allowed the establishment of four biostratigraphic units, spanning the interval from Upper Bajocian to Upper Bathonian. The sedimentological and biostratigraphical results indicate the existence of a regional discontinuity at the base of the Bathonian. KEY-WORDS: MIDDLE JURASSIC, BAJOCIAN, BATHONIAN, AMMONITINA, BIOSTRATIGRAPHY, BIOCHRONOLOGY, ANDES, SOUTH-AMERICA, CHILE. RESUME Les ammonites du Jurassique de la CordiIIere de Domeyko ont ete traitees dans plusieurs monographies, parmi lesqueIIes les memoires classiques de Steinmann (1881), Tornquist (1898), Burckhardt (1903) et Stehn (1923) sont particulierement importants. -
Jurassic and Cretaceous Stratigraphy of the Anabar Area (Arctic Siberia, Laptev Sea Coast) and the Boreal Zonal Standard
Available online at www.sciencedirect.com ScienceDirect Russian Geology and Geophysics 54 (2013) 808–837 www.elsevier.com/locate/rgg Jurassic and Cretaceous stratigraphy of the Anabar area (Arctic Siberia, Laptev Sea coast) and the Boreal zonal standard B.L. Nikitenko a,*, B.N. Shurygin a, V.G. Knyazev b, S.V. Meledina a, O.S. Dzyuba a, N.K. Lebedeva a, E.B. Peshchevitskaya a, L.A. Glinskikh a, A.A. Goryacheva a, S.N. Khafaeva a a A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia b Diamond and Precious Metal Geology Institute, Yakutsk Scientific Center, Siberian Branch of the Russian Academy of Sciences, pr. Lenina 39, Yakutsk, 677891, Russia Received 6 February 2013; accepted 21 February 2013 Abstract Recent integrated studies of Mesozoic reference sections of the Anabar area (northern Middle Siberia, Laptev Sea coast) and the reinterpretation of all the previous data on a modern stratigraphic basis permit considerable improvement of the bio- and lithostratigraphic division and facies zoning of Jurassic and Cretaceous sediments in the region. Analysis of abundant paleontological data allows the development or considerable improvement of zonal scales for ammonites, belemnites, bivalves, foraminifers, ostracods, dinocysts, and terrestrial palynomorphs from several Jurassic and Cretaceous intervals. All the zonal scales have been calibrated against one another and against regional ammonite scale. Reference levels of different scales useful for interregional correlation have been defined and substantiated based on the analysis of lateral distribution of fossils in different regions of the Northern Hemisphere. -
GEOLOGICAL SURVEY PROFESSIONAL PAPER 1148 Early Jurassic Ammonites from Alaska
GEOLOGICAL SURVEY PROFESSIONAL PAPER 1148 Early Jurassic Ammonites from Alaska By RALPH W. IMLAY GEOLOGICAL SURVEY PROFESSIONAL PAPER 1148 Studies of Early Jurassic ammonites from Alaska provide close correlations with Lower Jurassic ammonite zones in Europe and with ammonite successions elsewhere in the world UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Doyle G. Frederick, Acting Director Library of Congress Cataloging in Publication Data Imlay, Ralph Willard, 1908- Early Jurassic ammonites from Alaska. (Geological Survey professional paper ; 1148) Bibliography: p. Supt. of Docs, no.: I 19.16:1148 Includes index. 1. Ammonoidea. 2. Paleontology Jurassic. 3. Paleontology Alaska. I. Title. II. Series. QE807.A51585 564'.53 81-607901 AACR2 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract _____________________________________________——— 1 Introduction ______________________________________________ 2 Biologic analysis ___________________________________________ 2 Biostratigraphic summary _____________________________________ 4 Northern Alaska _________________________________________ 4 East-central Alaska ________________________________________ 6 Southern Alaska _________________________________——————— 7 Wrangell Mountains _____________________________________ 7 Talkeetna Mountains ____________________________________ 7 Chulitna River area _____________________________________