The Mineralogy of Mudrocks from the Lias Group of England
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REFERENCES REFERENCES G. REFERENCES Fastnet Basin, offshore southwest Ireland. Journal of Micropalaeontology, 5, 19-29. AINSWORTH, N. R. & RILEY, L. A. 2010. Triassic to Middle Jurassic stratigraphy of the Kerr McGee 97/12-1 exploration ABBOTTS, I. 1991. United Kingdom oil and gas fields, 25 years commemorative volume. Memoir of the Geological Society well, offshore southern England. Marine & Petroleum Geology, 27, 853-894. of London, No.14. AINSWORTH, N. R., HORTON, N. F. & PENNEY, R. A. 1985. Lower Cretaceous micropalaeontology of the Fastnet ACTLABS. 2018. Report on 10 Ar-Ar analyses carried out as part of project IS16/04. IS16_04_ActLabs_raddatingrpt_Ar- Basin, offshore southwest Ireland. Marine & Petroleum Geology, 2, 341-349. Ar.xlsx. [Copy included within the Digital Addenda of this Atlas] AINSWORTH, N. R., BAILEY, H. W., GUEINN, K. J., RILEY, L. A., CARTER, J. & GILLIS, E. 2014. Revised AGNINI, C., FORNACIARI, E., RAFFI, I., CATANZARITI, R., PÄLIKE, H., BACKMAN, J. & RIO, D. 2014. stratigraphic framework of the Labrador Margin through integrated biostratigraphic and seismic interpretation, Biozonation and biochronology of Paleogene calcareous nannofossils from low and middle latitudes. Newsletters on Offshore Newfoundland and Labrador. Abstracts of the 4th Atlantic Conjugate Margins Conference. Go Deep: Back Stratigraphy, 47/2, 131–181. to the Source, 89-90. AINSWORTH, N. R. 1985. Upper Jurassic and Lower Cretaceous Ostracoda from the Fastnet Basin, offshore southwest AINSWORTH, N. R., BRAHAM, W., GREGORY, F. J., JOHNSON, B & KING, C. 1998a. A proposed latest Triassic to Ireland. Irish Journal of Earth Sciences. 7, 15-33. earliest Cretaceous microfossil biozonation for the English Channel and its adjacent areas. -
A Mysterious Giant Ichthyosaur from the Lowermost Jurassic of Wales
A mysterious giant ichthyosaur from the lowermost Jurassic of Wales JEREMY E. MARTIN, PEGGY VINCENT, GUILLAUME SUAN, TOM SHARPE, PETER HODGES, MATT WILLIAMS, CINDY HOWELLS, and VALENTIN FISCHER Ichthyosaurs rapidly diversified and colonised a wide range vians may challenge our understanding of their evolutionary of ecological niches during the Early and Middle Triassic history. period, but experienced a major decline in diversity near the Here we describe a radius of exceptional size, collected at end of the Triassic. Timing and causes of this demise and the Penarth on the coast of south Wales near Cardiff, UK. This subsequent rapid radiation of the diverse, but less disparate, specimen is comparable in morphology and size to the radius parvipelvian ichthyosaurs are still unknown, notably be- of shastasaurids, and it is likely that it comes from a strati- cause of inadequate sampling in strata of latest Triassic age. graphic horizon considerably younger than the last definite Here, we describe an exceptionally large radius from Lower occurrence of this family, the middle Norian (Motani 2005), Jurassic deposits at Penarth near Cardiff, south Wales (UK) although remains attributable to shastasaurid-like forms from the morphology of which places it within the giant Triassic the Rhaetian of France were mentioned by Bardet et al. (1999) shastasaurids. A tentative total body size estimate, based on and very recently by Fischer et al. (2014). a regression analysis of various complete ichthyosaur skele- Institutional abbreviations.—BRLSI, Bath Royal Literary tons, yields a value of 12–15 m. The specimen is substantially and Scientific Institution, Bath, UK; NHM, Natural History younger than any previously reported last known occur- Museum, London, UK; NMW, National Museum of Wales, rences of shastasaurids and implies a Lazarus range in the Cardiff, UK; SMNS, Staatliches Museum für Naturkunde, lowermost Jurassic for this ichthyosaur morphotype. -
Geology of the Yorkshire Coast 4. Staithes
05/03/2013 Geology of the Yorkshire Coast Dr Liam Herringshaw - [email protected] 4. Staithes – of Sand and Iron Early Jurassic Staithes Sandstone Formation Cleveland Ironstone Formation 1 05/03/2013 Staithes to Old Nab Simplified cliff section Rocks get younger towards south and east: RMF-SSF-CIF-WMF 2 05/03/2013 Staithes Sandstone Formation •Early Jurassic: Middle Pliensbachian Key features Sandstones with cross-stratification Burrowed siltstones 3 05/03/2013 Hummocky cross-stratification Fine-grained storm deposits 4 05/03/2013 Burrowed siltstones •After each storm, organic-rich silts deposited in quieter conditions Cleveland Ironstone Formation Transition from SSF to CIF, Penny Nab 5 05/03/2013 Oolitic ironstones Cleveland Ironstone Formation Modern oolites Warm, wave-agitated waters 6 05/03/2013 Stratigraphy Fossils 7 05/03/2013 Old Nab Ironstone burrows 8 05/03/2013 Siderite – iron carbonate Grows in sediment Needs low oxygen, low-sulphide conditions with iron and calcium Normally grey; turns red when oxidized Cleveland ironstone environment Fossils = marine conditions Ooids = high energy environment Primary iron-rich ooids = iron-rich waters Burrow scratches = firm sediments Shallow sea, wave-agitated, lots of runoff from land (with iron-rich soils?) 9 05/03/2013 Jet-powered Whitby Early Jurassic Whitby Mudstone Formation Grey Shales Black Shales Alum Shales Whitby Mudstone Formation 10 05/03/2013 Whitby Mudstone Formation Late Early Jurassic – Toarcian 5 subdivisions, mostly muddy Common features - sediments Finely laminated, -
Hydrogeological Field Guide to the Wessex Basin
Hydrogeological Field Guide to the Wessex Basin Technical Report IR/00/77 R Tyler-Whittle, P Shand, K J Griffiths and W M Edmunds This page is blank BRITISH GEOLOGICAL SURVEY Natural Environment Research Council TECHNICAL REPORT IR/00/77 Hydrogeology Series Technical Report IR/00/77 Hydrogeological Field Guide to the Wessex Basin R Tyler-Whittle, P Shand, K J Griffiths and W M Edmunds This report was prepared for an EU BASELINE fieldtrip. Bibliographic Reference Tyler-Whittle R, Shand P, Griffiths K J and Edmunds W M, 2000 Hydrogeological Field Guide to the Wessex Basin British Geological Survey Report IR/00/77 NERC copyright 2000 British Geological Survey Keyworth, Nottinghamshire BRITISH GEOLOGICAL SURVEY BRITISH GEOLOGICAL SURVEY KEYWORTH NOTTINGHAM NG12 5GG UNITED KINGDOM TEL (0115) 9363100 FAX (0115) 9363200 DOCUMENT TITLE AND AUTHOR LIST Hydrogeological Field Guide to the Wessex Basin R Tyler-Whittle, P Shand, K J Griffiths and W M Edmunds CLIENT CLIENT REPORT # BGS REPORT# IR/00/77 CLIENT CONTRACT REF BGS PROJECT CODE CLASSIFICATION Restricted SIGNATURE DATE SIGNATURE DATE PREPARED BY CO-AUTHOR (Lead Author) CO-AUTHOR CO-AUTHOR PEER REVIEWED BY CO-AUTHOR CHECKED BY CO-AUTHOR (Project Manager or deputy) CO-AUTHOR APPROVED BY CO-AUTHOR (Project Director or senior staff) CO-AUTHOR APPROVED BY OS Copyright (Hydrogeology acknowledged Group Manager) Assistant Director Layout checked by clearance (if reqd) BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from Keyworth, Nottingham NG12 5GG the BGS Sales Desk at the Survey headquarters, ☎ 0115-936 3100 Telex 378173 BGSKEY G Keyworth, Nottingham. The more popular maps and Fax 0115-936 3200 books may be purchased from BGS-approved stockists Murchison House, West Mains Road, Edinburgh, EH9 3LA and agents and over the counter at the Bookshop, Gallery ☎ 37, Natural History Museum, Cromwell Road, (Earth 0131-667 1000 Telex 727343 SEISED G Fax 0131-668 2683 Galleries), London. -
A Model for the Evolution of the Weald Basin
A model for the evolution of the Weald Basin DAVID L. HANSEN, DEREK J. BLUNDELL & S0REN B. NIELSEN Hansen, D.L., Blundell, D.J. & Nielsen, S.B. 2002-12-02. A Model for the evolution of the Weald Basin. Bulletin of the Geological Society of Denmark, Vol. 49, pp. 109-118. Copenhagen. https://doi.org/10.37570/bgsd-2003-49-09 The Weald Basin developed through the Jurassic-Lower Cretaceous as an extensional basin founded upon E-W trending low-angle faults that were probably Variscan thrusts, subsequently reactivated as normal faults. Later, the basin was inverted and uplifted into a broad dome, whilst the London Basin to the north, and the Hampshire-Dieppe Basin to the south, subsided as flanking basins during the late Palaeocene-Eocene. Seismic sections across the Weald indicate that inversion resulted from north-directed stress. A stratigraphic reconstruction based on a N-S profile across the Weald and flanking basins serves as a template for a forward, 2D thermo-mechanical model that simulates the evolution of the Weald Basin through crustal extension and its inversion, and subsidence of the flanking basins, through compression. The model provides a physical explanation for this sequence of events, requiring a region of crust of reduced strength relative to its flanks. This weak region is the location of crustal-scale Variscan thrusts that have been reactivated subsequently. The strong crust on the flanks is essential for the development of flanking basins during inversion and uplift of the Weald. Keywords: Basin inversion, lithosphere, thermo-mechanical modelling, finite elements, visco-elas tic-plastic, sedimentation, erosion. -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
The Strawberry Bank Lagerstätte Reveals Insights Into Early Jurassic Lifematt Williams, Michael J
XXX10.1144/jgs2014-144M. Williams et al.Early Jurassic Strawberry Bank Lagerstätte 2015 Downloaded from http://jgs.lyellcollection.org/ by guest on September 27, 2021 2014-144review-articleReview focus10.1144/jgs2014-144The Strawberry Bank Lagerstätte reveals insights into Early Jurassic lifeMatt Williams, Michael J. Benton &, Andrew Ross Review focus Journal of the Geological Society Published Online First doi:10.1144/jgs2014-144 The Strawberry Bank Lagerstätte reveals insights into Early Jurassic life Matt Williams1, Michael J. Benton2* & Andrew Ross3 1 Bath Royal Literary and Scientific Institution, 16–18 Queen Square, Bath BA1 2HN, UK 2 School of Earth Sciences, University of Bristol, Bristol BS8 2BU, UK 3 National Museum of Scotland, Chambers Street, Edinburgh EH1 1JF, UK * Correspondence: [email protected] Abstract: The Strawberry Bank Lagerstätte provides a rich insight into Early Jurassic marine vertebrate life, revealing exquisite anatomical detail of marine reptiles and large pachycormid fishes thanks to exceptional preservation, and especially the uncrushed, 3D nature of the fossils. The site documents a fauna of Early Jurassic nektonic marine animals (five species of fishes, one species of marine crocodilian, two species of ichthyosaurs, cephalopods and crustaceans), but also over 20 spe- cies of insects. Unlike other fossil sites of similar age, the 3D preservation at Strawberry Bank provides unique evidence on palatal and braincase structures in the fishes and reptiles. The age of the site is important, documenting a marine ecosystem during recovery from the end-Triassic mass extinction, but also exactly coincident with the height of the Toarcian Oceanic Anoxic Event, a further time of turmoil in evolution. -
'Cenoceras Islands' in the Blue Lias Formation (Lower Jurassic)
FOSSIL IMPRINT • vol. 75 • 2019 • no. 1 • pp. 108–119 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) ‘CENOCERAS ISLANDS’ IN THE BLUE LIAS FORMATION (LOWER JURASSIC) OF WEST SOMERSET, UK: NAUTILID DOMINANCE AND INFLUENCE ON BENTHIC FAUNAS DAVID H. EVANS1, *, ANDY H. KING2 1 Stratigrapher, Natural England, Rivers House, East Quay, Bridgwater, Somerset, TA6 4YS UK; e-mail: [email protected]. 2 Director & Principal Geologist, Geckoella Ltd, Suite 323, 7 Bridge Street, Taunton, Somerset, TA1 1TG UK; e-mail: [email protected]. * corresponding author Evans, D. H., King, A. H. (2019): ‘Cenoceras islands’ in the Blue Lias Formation (Lower Jurassic) of West Somerset, UK: nautilid dominance and influence on benthic faunas. – Fossil Imprint, 75(1): 108–119, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on-line). Abstract: Substantial numbers of the nautilid Cenoceras occur in a stratigraphically limited horizon within the upper part of the Lower Jurassic (Sinemurian Stage) Blue Lias Formation at Watchet on the West Somerset Coast (United Kingdom). Individual nautilid conchs are associated with clusters of encrusting organisms (sclerobionts) forming ‘islands’ that may have been raised slightly above the surrounding substrate. Despite the relatively large numbers of nautilid conchs involved, detailed investigation of their preservation suggests that their accumulation reflects a reduction in sedimentation rates rather than an influx of empty conches or moribund animals. Throughout those horizons in which nautilids are present in relative abundance, the remains of ammonites are subordinate or rare. The reason for this unclear, and preferential dissolution of ammonite conchs during their burial does seem to provide a satisfactory solution to the problem. -
Natural Hydraulic Fractures in the Wessex Basin, SW England: Widespread Distribution, Composition and History Alain Zanella, Peter Robert Cobbold, Tony Boassen
Natural hydraulic fractures in the Wessex Basin, SW England: widespread distribution, composition and history Alain Zanella, Peter Robert Cobbold, Tony Boassen To cite this version: Alain Zanella, Peter Robert Cobbold, Tony Boassen. Natural hydraulic fractures in the Wessex Basin, SW England: widespread distribution, composition and history. Marine and Petroleum Geology, Elsevier, 2015, 68 (Part A), pp.438-448. 10.1016/j.marpetgeo.2015.09.005. insu-01200780 HAL Id: insu-01200780 https://hal-insu.archives-ouvertes.fr/insu-01200780 Submitted on 18 Sep 2015 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. ACCEPTED MANUSCRIPT Natural hydraulic fractures in the Wessex Basin, SW England: widespread distribution, composition and history A. Zanella 1, 2 *, P.R. Cobbold 1 and T. Boassen 4 1Géosciences-Rennes (UMR-6118), CNRS et Université de Rennes 1, Campus de Beaulieu, 35042 Rennes Cedex, France 2L.P.G., CNRS UMR 6112, Université du Maine, Faculté des Sciences, 72085 Le Mans Cedex 9, France 4 Statoil ASA Research Centre, NO-7005 Trondheim, Norway *Corresponding author, e-mail: [email protected] Abstract Bedding-parallel veins of fibrous calcite ('beef') are historical in the Wessex Basin. -
Geology of the Shepton Mallet Area (Somerset)
Geology of the Shepton Mallet area (Somerset) Integrated Geological Surveys (South) Internal Report IR/03/94 BRITISH GEOLOGICAL SURVEY INTERNAL REPORT IR/03/00 Geology of the Shepton Mallet area (Somerset) C R Bristow and D T Donovan Contributor H C Ivimey-Cook (Jurassic biostratigraphy) The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Ordnance Survey licence number GD 272191/1999 Key words Somerset, Jurassic. Subject index Bibliographical reference BRISTOW, C R and DONOVAN, D T. 2003. Geology of the Shepton Mallet area (Somerset). British Geological Survey Internal Report, IR/03/00. 52pp. © NERC 2003 Keyworth, Nottingham British Geological Survey 2003 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation. Shop online at: www.thebgs.co.uk The Survey publishes an annual catalogue of its maps and other publications; this catalogue is available from any of the BGS Sales Murchison House, West Mains Road, Edinburgh EH9 3LA Desks. 0131-667 1000 Fax 0131-668 2683 The British Geological Survey carries out the geological survey of e-mail: [email protected] Great Britain and Northern Ireland (the latter as an agency service for the government of Northern Ireland), and of the London Information Office at the Natural History Museum surrounding continental shelf, as well as its basic research (Earth Galleries), Exhibition Road, South Kensington, London projects. -
Orbital Pacing and Secular Evolution of the Early Jurassic Carbon Cycle
Orbital pacing and secular evolution of the Early Jurassic carbon cycle Marisa S. Storma,b,1, Stephen P. Hesselboc,d, Hugh C. Jenkynsb, Micha Ruhlb,e, Clemens V. Ullmannc,d, Weimu Xub,f, Melanie J. Lengg,h, James B. Ridingg, and Olga Gorbanenkob aDepartment of Earth Sciences, Stellenbosch University, 7600 Stellenbosch, South Africa; bDepartment of Earth Sciences, University of Oxford, OX1 3AN Oxford, United Kingdom; cCamborne School of Mines, University of Exeter, TR10 9FE Penryn, United Kingdom; dEnvironment and Sustainability Institute, University of Exeter, TR10 9FE Penryn, United Kingdom; eDepartment of Geology, Trinity College Dublin, The University of Dublin, Dublin 2, Ireland; fDepartment of Botany, Trinity College Dublin, The University of Dublin, Dublin 2, Ireland; gEnvironmental Science Centre, British Geological Survey, NG12 5GG Nottingham, United Kingdom; and hSchool of Biosciences, University of Nottingham, LE12 5RD Loughborough, United Kingdom Edited by Lisa Tauxe, University of California San Diego, La Jolla, CA, and approved January 3, 2020 (received for review July 14, 2019) Global perturbations to the Early Jurassic environment (∼201 to where they are recorded as individual shifts or series of shifts ∼174 Ma), notably during the Triassic–Jurassic transition and Toar- within stratigraphically limited sections. Some of these short-term cian Oceanic Anoxic Event, are well studied and largely associated δ13C excursions have been shown to represent changes in the with volcanogenic greenhouse gas emissions released by large supraregional to global carbon cycle, marked by synchronous igneous provinces. The long-term secular evolution, timing, and changes in δ13C in marine and terrestrial organic and inorganic pacing of changes in the Early Jurassic carbon cycle that provide substrates and recorded on a wide geographic extent (e.g., refs. -
The Global Stratotype Sections and Point (GSSP) for the Base of the Jurassic System at Kuhjoch (Karwendel Mountains, Northern Calcareous Alps, Tyrol, Austria)
162 162 Articles by Hillebrandt, A.v.1, Krystyn, L.2, Kürschner, W.M.3, Bonis, N.R.4, Ruhl, M.5, Richoz, S.6, Schobben, M. A. N.12, Urlichs, M.7, Bown, P.R.8, Kment, K.9, McRoberts, C.A.10, Simms, M.11, and Tomãsových, A13 The Global Stratotype Sections and Point (GSSP) for the base of the Jurassic System at Kuhjoch (Karwendel Mountains, Northern Calcareous Alps, Tyrol, Austria) 1 Institut für Angewandte Geowissenschaften, Technische Universität, Ernst-Reuter-Platz 1, 10587 Berlin, Germany. E-mail: [email protected] 2 Department for Palaeontology, Vienna University, Geozentrum, Althansstr. 9, A-1090 Vienna, Austria. E-mail: [email protected] 3 Department of Geosciences and Centre of Earth Evolution and Dynamics (CEED), University of Oslo, PO box 1047, Blindern, 0316 Oslo, Norway. E-mail: [email protected] 4 Shell Global Solutions International B.V., Kessler Park 1, 2288 GS, Rijswijk, the Netherlands. E-mail: [email protected] 5 Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK. E-mail: [email protected] 6 Commission for the Palaeontological and Stratigraphical Research of Austria, Austrian Academy of Sciences c/o Institut of Earth Sciences, Graz University, Heinrichstraße 26, 8010 Graz, Austria. E-mail: [email protected] 7 Staatliches Museum für Naturkunde, Rosenstein 1, 70191 Stuttgart, Germany. E-mail: [email protected] 8 Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK. E-mail: [email protected] 9 Lenggrieser Str.