Seismic Characterization of the Zechstein Carbonates in the Dutch Northern Offshore

Total Page:16

File Type:pdf, Size:1020Kb

Seismic Characterization of the Zechstein Carbonates in the Dutch Northern Offshore Seismic characterization of the Zechstein carbonates in the Dutch northern offshore Sjoerd Tolsma1 (Author) Prof. Dr. Jan de Jager1 (First supervisor) Bastiaan jaarsma2 (Second Supervisor) 1 Utrecht University, Netherlands 2 EBN, Utrecht, Netherlands June, 2014 MSc. Thesis: Earth, Life and Climate SEISMIC CHARACTERIZATION OF THE ZECHSTEIN CARBONATES IN THE DUTCH NORTHERN OFFSHORE Sjoerd Tolsma, 2014 2 SEISMIC CHARACTERIZATION OF THE ZECHSTEIN CARBONATES IN THE DUTCH NORTHERN OFFSHORE Sjoerd Tolsma, 2014 Contents 1.0 Abstract ....................................................................................................................................... 5 2.0 Introduction ................................................................................................................................ 7 3.0 Geological & Tectonic History of the Netherlands .................................................................... 9 3.1 Study area structural elements ............................................................................................. 21 4.0 Zechstein lithological description ............................................................................................ 25 4.1 Zechstein 1 cycle.................................................................................................................... 27 4.2 Zechstein 2 cycle.................................................................................................................... 29 4.3 Zechstein 3 cycle.................................................................................................................... 33 4.4 Zechstein 4 cycle.................................................................................................................... 36 4.5 Zechstein 5 cycle.................................................................................................................... 36 4.6 The Zechstein Upper Claystone Formation ........................................................................... 36 4.7 Zechstein build-up distribution ............................................................................................. 36 5.0 Proven Zechstein platform areas ............................................................................................. 37 6.0 Possibilities for Zechstein build-ups in the northern Dutch offshore .................................... 41 7.0 Methods .................................................................................................................................... 47 7.1 Seismic interpretation ........................................................................................................... 48 7.2 Synthetics .............................................................................................................................. 49 7.3 Time – depth conversion ....................................................................................................... 49 8.0 Results ....................................................................................................................................... 53 9.0 Zechstein seismic character in real data .................................................................................. 55 9.1 Petrophysical description ...................................................................................................... 55 9.2 Conclusions on the petrophysical description ...................................................................... 62 9.3 Zechstein well synthetics ....................................................................................................... 63 9.4 Discussion & Conclusions ...................................................................................................... 71 9.5 Zechstein seismic character on seismic ................................................................................. 77 9.6 Discussion & Conclusions ...................................................................................................... 79 9.7 Base Zechstein amplitude map ............................................................................................. 79 9.8 Conclusions ............................................................................................................................ 82 10.0 Seismic interpretation .............................................................................................................. 83 10.1 DEF survey ............................................................................................................................. 83 10.2 TerraCube .............................................................................................................................. 84 10.3 2D Lines ..................................................................................................................................... 86 3 SEISMIC CHARACTERIZATION OF THE ZECHSTEIN CARBONATES IN THE DUTCH NORTHERN OFFSHORE Sjoerd Tolsma, 2014 10.4 Velocity model results ........................................................................................................... 86 10.5 Zechstein thickness map ....................................................................................................... 87 10.6 Base Zechstein amplitude map ............................................................................................. 88 10.7 DEF survey ............................................................................................................................. 88 10.12TerraCube ................................................................................................................................. 96 11.0 Discussion ................................................................................................................................ 109 11.1 Development of the E02-02 platform ................................................................................. 109 11.2 Zechstein structures – DEF area .......................................................................................... 111 11.6 Zechstein structures – TerraCube area ............................................................................... 119 12.0 Zechstein platform distribution map ................................................................................... 127 12.1 Influence of paleowind direction ........................................................................................ 129 13.0 Conclusions ............................................................................................................................. 131 14.0 References ............................................................................................................................... 133 15.0 Appendices .............................................................................................................................. 135 4 SEISMIC CHARACTERIZATION OF THE ZECHSTEIN CARBONATES IN THE DUTCH NORTHERN OFFSHORE Sjoerd Tolsma, 2014 1.0 Abstract The presence of Zechstein carbonate platform facies is often controlled by the pre-existing paleo- geography and commonly occur on uplifted fault blocks and along the margins of the Southern Permian Basin. Present day Zechstein distribution maps suggest that these platform facies are absent along the margins of the Elbow Spit High in the Dutch northern offshore, while based on the general geological setting their presence might be expected. Only several Dutch and UK wells have drilled the Zechstein or older formations in the study area. Well E02-02 and A16-01 have strong positive indicators for the presence of Zechstein platform facies, with good reservoir characteristics. Well E02-02 drilled a Zechstein platform structure, which was confirmed by a side-wall core sample. A16- 01 found stromatolites along the SW margin of the Elbow Spit High, indicating a shallow water environment. Therefore it cannot be ruled out that platform facies exists in a large area along the margins of the Elbow Spit High. This has been investigated with the use of seismic data. First, seismic and petrophysical data will be used to characterize the Zechstein on seismic. That will be used, together with Zechstein analogues from the North-East Netherlands, to identify potential Zechstein platform structures. Second, top and base Zechstein is mapped in great detail and in specific areas the top Zechstein-3 Anhydrite Member is mapped as well. The identified potential Zechstein platform structures are then compared and compared to the proven E02-02 platform. The results show that the Zechstein Group contains several characteristic seismic properties that can be used to identify potential Zechstein platform structure, since a low amplitude seems to correlate with Zechstein platform structures. This study illustrates that Zechstein platform facies exists along the western and eastern margins of the Elbow Spit High, away from the wells that encountered this facies. A modified Zechstein distribution map has been proposed showing the areas with Zechstein platform facies along the Elbow Spit High. This map is based on the identified Zechstein platform structures and well data in the study area. Also a new area with possible Zechstein platform facies is proposed, that roughly correlates with the Step High. Acknowledgements I would like to express my gratitude to Bastiaan Jaarsma (EBN), my supervisor, for his patient guidance, enthusiastic encouragement and useful critiques on this research. I would also like to thank prof.
Recommended publications
  • A Late Permian Ichthyofauna from the Zechstein Basin, Lithuania-Latvia Region
    bioRxiv preprint doi: https://doi.org/10.1101/554998; this version posted February 20, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. 1 A late Permian ichthyofauna from the Zechstein Basin, Lithuania-Latvia Region 2 3 Darja Dankina-Beyer1*, Andrej Spiridonov1,4, Ģirts Stinkulis2, Esther Manzanares3, 4 Sigitas Radzevičius1 5 6 1 Department of Geology and Mineralogy, Vilnius University, Vilnius, Lithuania 7 2 Chairman of Bedrock Geology, Faculty of Geography and Earth Sciences, University 8 of Latvia, Riga, Latvia 9 3 Department of Botany and Geology, University of Valencia, Valencia, Spain 10 4 Laboratory of Bedrock Geology, Nature Research Centre, Vilnius, Lithuania 11 12 *[email protected] (DD-B) 13 14 Abstract 15 The late Permian is a transformative time, which ended in one of the most 16 significant extinction events in Earth’s history. Fish assemblages are a major 17 component of marine foods webs. The macroevolution and biogeographic patterns of 18 late Permian fish are currently insufficiently known. In this contribution, the late Permian 19 fish fauna from Kūmas quarry (southern Latvia) is described for the first time. As a 20 result, the studied late Permian Latvian assemblage consisted of isolated 21 chondrichthyan teeth of Helodus sp., ?Acrodus sp., ?Omanoselache sp. and 22 euselachian type dermal denticles as well as many osteichthyan scales of the 23 Haplolepidae and Elonichthydae; numerous teeth of Palaeoniscus, rare teeth findings of 1 bioRxiv preprint doi: https://doi.org/10.1101/554998; this version posted February 20, 2019.
    [Show full text]
  • Developing a Geological Framework
    21/2/12 GeolFrameworkPaper_postreview_v2acceptchanges_editorcomments New insights from 3D geological models at analogue CO2 storage sites in Lincolnshire and eastern Scotland, UK. Alison Monaghan1*, Jonathan Ford2, Antoni Milodowski2, David McInroy1, Timothy Pharaoh2, Jeremy Rushton2, Mike Browne1, Anthony Cooper2, Andrew Hulbert2 and Bruce Napier2 1 British Geological Survey, Murchison House, West Mains Road, Edinburgh, EH9 3LA, UK. 2 British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham, NG12 5GG, UK. * Corresponding author (email [email protected] (Approx.15,600 words in total, 25 figures) SUMMARY: Subsurface 3D geological models of aquifer and seal rock systems from two contrasting analogue sites have been created as the first step in an investigation into methodologies for geological storage of carbon dioxide in saline aquifers. Development of the models illustrates the utility of an integrated approach using digital techniques and expert geological knowledge to further geological understanding. The models visualize a faulted, gently dipping Permo-Triassic succession in Lincolnshire and a complex faulted and folded Devono-Carboniferous succession in eastern Scotland. The Permo-Triassic is present in the Lincolnshire model to depths of -2 km OD, and includes the aquifers of the Sherwood Sandstone and Rotliegendes groups. Model-derived thickness maps test and refine Permian palaeogeography, such as the location of a carbonate reef and its associated seaward slope, and the identification of aeolian dunes. Analysis of borehole core samples established average 2D porosity values for the Rotliegendes (16%) and Sherwood Sandstone (20%) groups, and the Zechstein (5%) and Mercia Mudstone (<10%) groups, which are favourable for aquifer and seal units respectively. Core sample analysis has revealed a complex but well understood diagenetic history.
    [Show full text]
  • Hydrocarbon Plays from West Poland: Zechstein Limestone and Main Dolomite
    Hydrocarbon Plays from West Poland: Zechstein Limestone and Main Dolomite Paweł Zdanowski & Tomasz Solarski PGNiG SA (Polish Oli & Gas Company), Exploration and Production Branch Underexplored Plays - Part III 31-X-2018 & 01-XI-2018 Stavanger Hydrocarbon Plays from West Poland: Zechstein Limestone (Ca1) and Main Dolomite (Ca2) Presentation outline: Palaeogeography of Zechstein • Southern Permian Basin and Northern Permian Basin • Correlation of carbonate units between SBP and NPB Zechstein Limestone (Brońsko Gas Field) • Hydrocarbon Play. • Pattern Recognition from Seismic. Main Dolomite (BMB and LMG oil & gas fields) • Hydrocarbon Play. • Pattern Recognition from Seismic. • Analysis of Seismic Attributes. • Seismic Modeling. Late Permian Paleogeography from Blakely (2014) Tucker, 2016 After Scotese, 2002 European Southern Permian Basin Zechstein Sea Connected to Pantalassa Ocean 2000km to N/NE. Possible connection to Paleo-Tethys through the Polish Sub-Basin to the SE ?? Palaeo-latitude: 10-20°. Climate extremely arid. After Scotese, 2012 Sketch map of Permian sedimentary basin in north-west Europe Dziękuję za uwagę Stavanger Warsaw Millennium Atlas: Petroleum Geology of the Central and Northern North Sea, 2003 Polish Zechstein Basin ….stratigraphy Leine Na2 A2 Stassfurt Ca2 A1g Na1 A1d Werra Ca1 Wagner & Peryt. 1997 Słowakiewicz & Mikołajewski, 2009 Tucker, 2016 Comparison of the Zechstein development of the NPB with the classic SPB Evans et al. 2003 Madeleine et al. 2018 Zechstein Limestone – Ca1 (≈ Argyll Carbonate Member) Zechstein basin, showing the position of the Brandenburg-Wolsztyn-Pogorzela palaeo-High Basin facies of the Zechstein Limestone in Poland, showing the occurrence of isolated reefs related to the Brandenburg-Wolsztyn-Pogorzela palaeo-High. isolated reefs (rimmed platform) Peryt et al.
    [Show full text]
  • 3D Seismic Reflection Data Reveal Syn-Depositional Halokinesis in The
    This manuscript is a EarthArxiv preprint and had been submitted for publication in the AAPG Bulletin. Please note that this manuscript has not been peer-reviewed. Subsequent versions of this manuscript may, thus, have slightly different content. If accepted, the final version of this manuscript will be available via the “Peer-reviewed Publication DOI” link on the right- hand side of this webpage. Please feel free to contact any of the authors directly; We welcome your feedback. 1 3D seismic reflection data reveal syn-depositional halokinesis in the 2 Zechstein Supergroup (Lopingian), Central North Sea, UK 3 Amir Joffe 1*, Christopher A-L. Jackson2, Leonardo M. Pichel3 4 1. Basins Research Group (BRG), Department of Earth Science and Engineering, Imperial 5 College London, South Kensington Campus, SW7 2BP, UK 6 2. Department of Earth and Environmental Sciences, The University of Manchester, 7 Williamson Building, Oxford Road, Manchester, M13 9PL, UK 8 3. Department of Earth Science, University of Bergen, Allégaten 41, 5007, Bergen, 9 Norway 10 Abstract 11 Salt tectonics is typically caused by the flow of mobile evaporites in response to post- 12 depositional gravity gliding and/or differential loading by overburden sediments. This situation 13 is considerably more complex near the margins of salt basins, where carbonate and clastic rocks 14 may be deposited at the same time and interbedded with, more mobile, evaporite strata. In these 15 cases, syn-depositional salt flow may occur due to density differences in the deposited 16 lithologies, although our understanding of this process and related produces is relatively poor. 17 We here use 3D seismic reflection and borehole data from the Devil’s Hole Horst, West Central 18 Shelf, offshore UK to understand the genesis, geometry and kinematic of intra-Zechstein 19 Supergroup (Lopingian) minibasins and their effect on post-depositional salt deformation.
    [Show full text]
  • Induced Seismicity of the Groningen Gas Field: History and Recent Developments K
    Induced seismicity of the Groningen gas field: History and recent developments K. van Thienen-Visser1 and J. N. Breunese1 Abstract For the large Groningen field, the first seismic event was Induced seismicity of the Groningen gas field is caused by recorded in 1991. The largest magnitude was an ML 3.6 event the production of gas. Because of the large areal extent of the on 16 August 2012. Even though the magnitude of the event reservoir, the long history of depletion, and the available data sets was, seismologically speaking, not high, intensities as high as VI (which exist as a result of consequences and public unrest caused were observed because of the shallow depth of the event (3 km, by induced seismicity), the field presents a valuable case for i.e., reservoir depth) and the soft surface soils in the area (TNO, studying the relationships among geologic, flow-dynamic, geo- 2013a), causing damage to houses in the area. mechanical, and seismological models. Gas production from the Until 2012, a maximum magnitude of 3.9, with a probabil- Groningen field started in 1963. Induced seismicity of the field ity of exceedance of 16% (van Eck et al., 2006), was seen as the first was recorded in 1991 (ML 2.4). During the subsequent 10 upper size limit for induced seismicity in the north of the Nether- years, induced seismicity stayed at a rate of about five events (ML lands. However, since 2003, seismicity in the field has increased ≥ 1.5) per year. Starting in 2003, the number of events and mag- in number and magnitude.
    [Show full text]
  • REGIONAL GEOLOGY by Graham K. Lott
    CHAPTER II REGIONAL GEOLOGY by Graham K. Lott The ‘quarrying’ and use of local stone in Notting- the Triassic comprises a thick succession of non- hamshire, for both building and decorative purposes, marine, green-grey to reddish brown sandstones, dates back to Roman times. However, the lithological siltstones and mudstones, the latter including thinly units that characterise the geological succession interbedded, grey-green, dolomitic, very fine grained within the county contain only a few beds of stone sandstones (known locally as skerry). In contrast, the suitable for these purposes. This lack of indigenous early Jurassic marine succession is only sporadically stone useful for decorative carving is reflected in the exposed along the northern edge of the low-lying composition of the suite of carved stone fragments Vale of Belvoir and comprises a succession of grey that have been studied as part of this Corpus project. limestones and mudstones (Lias Group). The eastern By far the majority of the stones examined consist part of the county is locally blanketed by extensive of lithologies (primarily sandstones and limestones) tracts of glacial and alluvial sediments (unconsolidated sourced from outside the county border. sands, gravels, clays and muds) of Quaternary age. carboniferous THE GEOLOGY OF NOTTINGHAMSHIRE Pennine Coal Measures Group Nottinghamshire has a relatively simple geological The Carboniferous rocks that crop out in the west of succession comprising a sequence of eastwards- the county form part of the Pennine Coal Measures dipping sedimentary rock units whose outcrops Group. This succession is best known economically extend from north to south across the county (see for its coal reserves but also contains a number of Fig.
    [Show full text]
  • Geology of the Groningen Field – an Overview
    Netherlands Journal of Geosciences — Geologie en Mijnbouw |96 – 5 | s3–s15 | 2017 doi:10.1017/njg.2017.22 Geology of the Groningen field – an overview JandeJager1,∗ & Clemens Visser2 1 Nassaukade 42, 2281 XD Rijswijk, the Netherlands 2 Nederlandse Aardolie Maatschappij B.V., Schepersmaat 2, 9405 TA Assen, the Netherlands ∗ Corresponding author. Email: [email protected] Manuscript received: 27 February 2017, accepted: 21 July 2017 Abstract After more than half a century of production and with some 350 wells, the Groningen gas field must be one of the best-studied gas fields in the world. Initially, it was considered to be relatively simple and behaving like one big tank. Now that it is entering a phase of declining production it has become clear that many subtleties are not fully understood yet. Prediction and management of subsidence and induced earth tremors require a detailed understanding of the field geology. In addition, an optimum gas recovery is only possible if details of, for example, reservoir quality distribution and faulting, that did not appear relevant before, are well understood. The large Groningen field comprises a structurally high block during much of its history, probably already from Devonian times onwards. The desert sandstones of the Rotliegend reservoir exhibit a strong south-to-north proximal–distal relationship. Whilst diagenesis has in many fields led to deterioration of reservoir properties, this effect is small in the Groningen field. The field is dipping to the north, and bounded by a series ofnormal faults in the west, south and east. Almost all faults are normal extensional faults, but locally inverse reactivation has led to small pop-up structures.
    [Show full text]
  • Geology of Gas and Oil Under the Netherlands
    Geology of Gas and Oil under the Netherlands Geology of Gas and Oil under the Netherlands Selection of papers presented at the 1993 International Conference of the American Association of Petroleum Geologists, held in The Hague Edited by H.E. Rondeel Institute of Earth Sciences, Vrije Unlversiteit, Amsterdam, the Netherlands D.A.J. Batjes The Hague, the Netherlands W.H. Nieuwenhuijs Delft University of Technology, Delft, the Netherlands The Royal Geological and Mining Society of the Netherlands· KNGMG Kluwer Academic Publishers DORDRECHT I BDSTON I LONDON Library of Congress Cataloging-in-Publication Data Geology of gas and 011 under the Netherlands I edlted by H.E. Rondeel. D.A.J. BatjBS and W.H. Nleuwenhuljs. p. em. 1. Natural gas--Geology--Netherlands. 2. Petroleu.--Geology­ -Netherlands. I. Rondeel. H. E. II. Batjes. D. A. J. III. Nl euwenhu 1 jS. W. H. TN897.N4G46 1996 553.2'85'09492--de20 95-25226 ISBN-13: 978-94-010-6541-2 e-ISBN-13: 978-94-009-0121-6 DOl: 10.1007/978-94-009-0121-6 Published by Kluwer Academic Publishers, P.O. Box 17, 3300 AA Dordrecht, The Netherlands Kluwer Academic Publishers incorporates the publishing programmes of D. Reidel, Martinus Nijhoff, Dr W. Junk and MTP Press. Sold and distributed in the U.S.A. and Canada by Kluwer Academic Publishers, 101 Philip Drive, Norwell, MA 02061, U.S.A. In all other countries, sold and distributed by Kluwer Academic Publishers Group, P.O. Box 322, 3300 AH Dordrecht, The Netherlands Printed on acid-free paper All rights reserved ©1996 Kluwer Academic Publishers Softcover reprint of the hardcover 1st edition 1996 No part of the material protected by this copyright notice may be reproduced or utiHzed in any form or by any means, electronic or mechanical, including photocopying, recording or by any information storage and retrieval system, without written permission from the copyright owner.
    [Show full text]
  • 3D View of the Base of the Zechstein in the SPBA Area, (Viewed from the South; Red Colours Are Shallow and Blue Indicates the Greatest Depths)
    SPBA-Compleet 22-04-10 13:41 Pagina x 3D view of the base of the Zechstein in the SPBA area, (viewed from the south; red colours are shallow and blue indicates the greatest depths). The section crosses the entire area, a distance of 1525 km. The vertical scale is 1 : 300 000. SPBA-Compleet 22-04-10 13:41 Pagina 1 Chapter 1 — Introduction, stratigraphic framework and mapping Chapter 1 Introduction, stratigraphic framework and mapping Authors Contributors Bibliographic reference Hans Doornenbal (TNO), Oscar Abbink (TNO), Ed Duin (TNO), Michiel Dusar (GSB), Peer Hoth (BGR), United Kingdom: Bruce Napier, Peter Balson, Robert Knox and Susan Stoker, Belgium: Pascal Vancampenhout, Doornenbal, J.C., Abbink, O.A., Duin, E.J.T., Dusar, M., Hoth, P., Jasionowski, M., Lott, G.K., Mathiesen, A., Papiernik, B., Marek Jasionowski (PGI), Graham Lott (BGS), Anders Mathiesen (GEUS), Bartek Papiernik (AGH University Denmark: Torben Bidstrup and Ole Vejbæk, Germany: Gaby Merzbach and Marina Fischer, the Netherlands: Carla Elmers, Peryt, T.M., Veldkamp, J.G. & Wirth, H., 2010. Introduction, stratigraphic framework and mapping. In: Doornenbal, J.C. of Science & Technology), Tadeusz Peryt (PGI), Hans Veldkamp (TNO) and Holger Wirth (BGR) Jenny Hettelaar, Henk Kombrink, Gion Kuper, Erik Simmelink and Boris Webbers, Poland: Marek Hajto, Rafał Kudrewicz, and Stevenson, A.G. (editors): Petroleum Geological Atlas of the Southern Permian Basin Area. EAGE Publications b.v. Grzegorz Machowski and Anna Sowizdzal (Houten): 1-9. 1 Introduction 1.1 Topography and bathymetry In Belgium, geological publications can be found on the GNOSIS website (Generalized Natural Online Sciences Spatial Information System of the federal scientific institutes in Belgium; www.gnosis.be/gnosis/index.jsp).
    [Show full text]
  • B2211 Text Layout.Indd
    Carboniferous-Rotliegend Total Petroleum System Description and Assessment Results Summary By Donald L. Gautier U.S. Geological Survey Bulletin 2211 U.S. Department of the Interior U.S. Geological Survey Carboniferous-Rotliegend Total Petroleum System Description and Assessment Results Summary By Donald L. Gautier U.S. Geological Survey Bulletin 2211 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director U.S. Geological Survey, Reston, Virginia: 2003 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ 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. Although this report is in the public domain, it contains copyrighted materials that are noted in the text. Permission to reproduce those items must be secured from the individual copyright owners. iii Contents Foreword ........................................................................................................................................................ 1 Abstract .......................................................................................................................................................... 2 Introduction ..................................................................................................................................................
    [Show full text]
  • Faunal Migration Into the Late Permian Zechstein Basin – Evidence from Bryozoan Palaeobiogeography ⁎ Anne M
    Palaeogeography, Palaeoclimatology, Palaeoecology 251 (2007) 198–209 www.elsevier.com/locate/palaeo Faunal migration into the Late Permian Zechstein Basin – Evidence from bryozoan palaeobiogeography ⁎ Anne M. Sørensen a, Eckart Håkansson a, Lars Stemmerik a,b, a Department of Geography and Geology, University of Copenhagen, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark b Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark Received 24 October 2006; received in revised form 8 March 2007; accepted 19 March 2007 Abstract Late Permian bryozoans from the Wegener Halvø, Ravnefjeld and Schuchert Formations in East Greenland have been investigated. 14 genera are recognised. Integration of the new bryozoan data from the Upper Permian of East Greenland with data on the distribution of Permian bryozoans along the northern margin of Pangea is used to test hypotheses concerning Late Palaeozoic evolution of the North Atlantic region. During the Permian, the Atlantic rift system formed a seaway between Norway and Greenland from the boreal Barents Shelf to the warm and arid Zechstein Basin. This seaway is considered to be the only marine connection to the Zechstein Basin and therefore the only possible migration route for bryozoans to enter the basin. The distribution of Permian bryozoans is largely in keeping with such a connection from the cool Barents Shelf past the East Greenland Basin to the warm Zechstein Basin and also corroborates the change in temperature through this connection. © 2007 Elsevier B.V. All rights reserved. Keywords: Bryozoans; East Greenland; Palaeobiogeography; Permian; Zechstein Basin 1. Introduction Worsley, 2005). This is in concert with global palaeogeo- graphic reconstructions indicating that Pangaea drifted The Upper Palaeozoic successions of the Sverdrup more than 2500 km northward during this time period, so Basin of Arctic Canada and the North Greenland– that the North Greenland–Norwegian Barents Sea area Svalbard–Norwegian Barents Sea area along the northern moved from c.
    [Show full text]
  • Non-Marine Permian Biostratigraphy and Biochronology: an Introduction
    Downloaded from http://sp.lyellcollection.org/ by guest on September 28, 2021 Non-marine Permian biostratigraphy and biochronology: an introduction SPENCER G. LUCAS 1, JOERG W. SCHNEIDER 2 & GIUSSEPE CASSINIS 3 1New Mexico Museum of Natural History and Science, 1801 Mountain Road N. W., Albuquerque, New Mexico 87104-13 Y J, USA (e-mail: [email protected]) 2TU Bergakademie Freiberg, B. v. Cotta-Strasse 2, D-09596 Freiberg, Germany 3pavia University, Earth Science Department, via Ferrata 1, 27100 Pavia, Italy Abstract: The Permian time scale based on marine rocks and fossils is well defined and of global utility, but non-marine Permian biostratigraphy and chronology is in an early phase of development. Non-marine Permian strata are best known from western Europe and the western United States, but significant records are also known from Russia, South Africa, China and Brazil. Global time terms based on non-marine Permian strata, such as Rotliegend, Zechstein, Autunian, Saxonian and Thuringian, are either inadequately defined or poorly characterized and should only be used as lithostratigraphic terms. Macro- and microfloras have long been important in non-marine Permian correlations, but are subject to limitations based on palaeoprovinciality and facies/climatic controls. Charophytes, conchostracans, ostracodes and freshwater bivalves have a potential use in non-marine Permian biostrati- graphy but are limited by their over-split taxonomy and lack of well-established stratigraphic distributions of low-level taxa. Tetrapod footprints provide poor biostratigraphic resolution during the Permian, but tetrapod body fossils and insects provide more detailed biostrati- graphic zonations, especially in the Lower Permian. Numerous radioisotopic ages are available from non-marine Permian sections and need to be more precisely correlated to the global time scale.
    [Show full text]