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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. -
Late Eocene and Early Oligocene) of the Hampshire Basin
Cainozoic Research, 4(1-2), pp. 27-39, February 2006 The Neritidae of the Solent Group (Late Eocene and Early Oligocene) of the Hampshire Basin M.F. Symonds The Cottage in the Park, Ashtead Park, Ashtead, Surrey KT21 1LE, United Kingdom Received 1 June 2003; revised version accepted 7 March 2005 Gastropods of the family Neritidae in the Solent Group of the Hampshire Basin, southern England are reviewed and two previously unde- scribed taxa are described. New genus: Pseudodostia. New species: Clithon (Pictoneritina) cranmorensis and Clithon (Vittoclithon) headonensis. Neotypes designated for Neritina planulata Edwards, 1866 and Neritina tristis Forbes, 1856. Amended diagnosis: subgenus Vittoclithon. New combinations: Pseudodostia aperta (J. de C. Sowerby, 1823), Clithon (Pictoneritina) concavus (J. de C. Sowerby, 1823), Clithon (Pictoneritina) planulatus (Edwards, 1866) and Clithon (Pictoneritina) bristowi Wenz, 1929. KEY WORDS: Mollusca, Gastropoda, Neritidae, Palaeogene, Hampshire Basin. Introduction Systematic Palaeontology Family Neritidae Rafinesque, 1815 Although the number of species of Neritidae in the Solent Genus Pseudodostia gen. nov. Group is rather limited, specimens are common at certain horizons and they have received the attention of numerous Type species — Nerita aperta J. de C. Sowerby, 1825. Eo- authors in the past. In particular Curry (1960, 265-270) cene, Headon Hill Formation. dealt in detail with the taxonomy of Theodoxus concavus (J. de C. Sowerby, 1823), Theodoxus planulatus (Edwards, Derivatio nominis — The name reflects the close resem- 1866) and Theodoxus bristowi Wenz, 1929. The purpose of blance between the shell of the type species of this genus this paper is to update Curry’s work and to cover additional and that of Nerita crepidularia Lamarck, 1822, the type species. -
Tayside, Central and Fife Tayside, Central and Fife
Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland. -
Distribution of Landslides and Geotechnical Properties Within the Hampshire Basin
Distribution of landslides and geotechnical properties within the Hampshire Basin Kwanjai Yuangdetkla, Andy Gibson & Malcolm Whitworth University of Portsmouth, Portsmouth, UK Claire Foster, David Entwisle & Catherine Pennington British Geological Survey, Nottingham UK ABSTRACT This paper outlines the sedimentary sequences and geotechnical properties of the Hampshire Basin, a basin of filled with 700 m of Palaeogene clays, silts, sands and limestones in southern England. The paper presents results so far of a study to synthesize relevant geological and geotechnical data and relate these to the nature of the landslides in this basin. The study has found that stratigraphic sequences and geotechnical properties vary considerably across the basin owing to basin morphology and depositional environments which are correspond to complex paleogeography and tectonic movements during the Tertiary. Over-consolidated clays with low residual shear strengths are extensive on moderately steep slopes and prone to landsliding, especially on over-steepened coastal sections. Landslides vary from mudflows through mudslides, rotational landslides and minor falls. Landslide characteristics are strongly influenced by lithology but gradient appears to be the controlling factor in many cases. The presences of weak strata (clays, lignite, laminated layers), the pre-existing shear surface, the lithological interface (sand overlying clay) play important roles to locally control the position of the shear surface and the type of movements. At a basin scale, inland landslides are associated with the development of drainage system during and since the Tertiary. 1 INTRODUCTION structures trend east-west or northeast-southwest (Melville and Freshney, 1982). Locally, the complex 2 The Hampshire Basin underlies 3 400km of the mainland reactivation of basement faulting has produced many of Southern England and the northern half of the nearby local structures forming gentle hills and valleys such as Isle of Wight (Figure 1). -
Lihoreau-Et-Al.Merged-PDF-Proo
The Libycosaurus (Hippopotamoidea, Artiodactyla) intercontinental dispersal event at the early late Miocene revealed by new fossil remains from Kasserine area, Tunisia Fabrice Lihoreau, El Mabrouk Essid, Hayet Khayati Ammar, Laurent Marivaux, Wissem Marzougui, Rodolphe Tabuce, Rim Temani, Monique Vianey-Liaud, Gilles Merzeraud To cite this version: Fabrice Lihoreau, El Mabrouk Essid, Hayet Khayati Ammar, Laurent Marivaux, Wissem Marzougui, et al.. The Libycosaurus (Hippopotamoidea, Artiodactyla) intercontinental dispersal event at the early late Miocene revealed by new fossil remains from Kasserine area, Tunisia. Historical Biology, Taylor & Francis, 2021, 33 (2), pp.146-158. 10.1080/08912963.2019.1596088. hal-02082905 HAL Id: hal-02082905 https://hal.umontpellier.fr/hal-02082905 Submitted on 4 Nov 2020 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. Historical Biology For Peer Review Only The Libycosaurus (Hippopotamoidea, Artiodactyla) intercontinental dispersal event at the early Late Miocene revealed by new fossil remains from Kasserine area, -
Stratigraphical Chart of the United Kingdom: Northern Britain
STRATIGRAPHICAL CHART OF THE UNITED KINGDOM: NORTHERN BRITAIN 1 2 3 4 5 6 7 8 9 10 11 12 BGS Geological Time Chart North-west Approaches/ Northern Isles Northern North Sea Northern Highlands Western Isles & Grampian Midland Valley Central North Sea South of Northern Isle of Man & Northern Hebrides Shelf Inner Hebrides Highlands of Scotland Scotland Ireland northern Irish Sea England Eon Era Series/ Stage/Age age (Ma) Period Epoch System/ Sub-era 0.01 Holocene Late 0.13 Ulster Glacigenic Caledonia Glacigenic Group Caledonia Glacigenic Group Caledonia Glacigenic Group Caledonia Glacigenic Group Caledonia Glacigenic Group Caledonia Glacigenic Group Group Caledonia Glacigenic Group Caledonia Glacigenic Group Britannia Britannia Britannia Britannia Britannia Britannia Britannia Britannia British Coastal British Coastal Catchments British Coastal British Coastal British Coastal British Coastal Benburb Group British Coastal British Coastal Catchments Catchments Catchments Catchments Catchments Catchments Catchments Mid Deposits Group Group Deposits Group Group Deposits Group Deposits Group Group Deposits Group Group Deposits Group Deposits Group Deposits Group Group Albion Group Albion Group Albion Group Albion Glacigenic Group Glacigenic Group Glacigenic Group Glacigenic Group The Geological Society 0.78 Pleistocene* nary Nordland Early Group Quater Scale: 1 cm = 0.5 Ma Compiled by C N Waters 1.8 Nordland Nordland Group Group Cartography by P Lappage L Gelasian Pliocene Residual Buchan Deposits Gravels Formation Piacenzian 2.6 Group 3.6 E Zanclean 5.3 BGS contributors: Messinian 7.2 L Tortonian Britannia M C Akhurst, C A Auton, R P Barnes, A J M Barron, M A E Browne, M T Dean, J D Floyd, M R Gillespie, 11.6 Brassington Cenozoic Serravallian Catchments Miocene M Langhian 13.6 Formation P M Hopson, M Krabbendam, A G Leslie, A A McMillan, D Millward, W I Mitchell, K Smith, D Stephenson, Neogene 16.0 Group P Stone, and C N Waters. -
A Review of the Decapod Crustaceans from the Tertiary of the Isle of Wight, Hampshire, U
Bulletin of the Mizunami Fossil Museum, no. 38 (2012), p. 33–51, 4 pls., 2 figs., 2 tables. 33 © 202, Mizunami Fossil Museum A review of the decapod crustaceans from the Tertiary of the Isle of Wight, Hampshire, U. K, with description of three new species W. J. Quayle* and J. S. H. Collins** * 4, Argyll Street, Ryde, Isle of Wight, Hampsire, England<[email protected]> ** 8, Shaws Cottages, Perry Rise, London, SE23 2QN, and The Natural History Museum, London, SW7 5BD, England Abstract To the known decapod crustaceans of the Tertiary deposits of the Isle of Wight, Hampshire, the Early Eocene species, Basinotopus lamarkii (Desmarest) and Dromilites bucklandi Bell are introduced from the mainland, as are Glyphithyreus wetherelli (Bell), Rhachiosoma bispinosum Woodward, Coeloma (Litoricola) dentate (Woodward), Xanthilites bowerbanki Bell, and Xanthopsis unispinosa (M'Coy), the stratigrahic range of which has been extended to the London Clay on the Island. The development of an anomaly concerning Zanthopsis unispinosa, also present, if not peculiar to the island, is well established. A carapace of Harpactocarcinus sp. from this horizon is the first British record for the genus. Late Eocene species new to the island are Goniocypoda quaylei Crane, Orthakrolophus depressus? (Quayle and Collins) and Typilobus belli Quayle and Collins. Three new genera and species are described from the Late Eocene Headon Hill Formation; a callianassid, Vecticallichirus abditus; a goneplacid, Gonioplacoides minuta, and a hexapodid, Headonipus tuberculosus. New, superior material of the Late Eocene species, Typilobus obscurus Quayle and Collins, from the type locality, Colwell Bay necessitates a new description. A table of all known Tertiary species of decapod crustaceans from the Isle of Wight is appended. -
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. -
The Geological History of the Isle of Wight
*Manuscript Click here to view linked References The geological history of the Isle of Wight: an overview of the ‘diamond in 1 Britain’s geological crown’ 2 3 4 Abstract 5 6 The geology of the Isle of Wight has attracted both the amateur and professional 7 geologist alike for well over two centuries. It presents a cornucopia of things 8 geological and offers a window into the fascinating story of the geological history and 9 10 landscape development of southern England, as well as an important teaching 11 resource for all levels of study from primary education through to academic research. 12 13 This paper provides a geological framework and a summary of the history of research 14 15 as context for the papers in this issue can be placed. Inevitably, it can only offer a 16 précis of the huge amount of information available, but it is hoped will also give 17 added impetus to further investigation of the literature or, indeed, new research. 18 19 The island offers a field workshop for topics such as lithostratigraphy, sequence 20 21 stratigraphy, tectonics and climate change; studies that are becoming ever more 22 international in their influence. There are 15 Sites of Special Scientific Interest 23 designated because of their geological importance and a number of these are 24 internationally significant. 25 26 27 After a brief discussion on the concealed geology, this paper concentrates on an 28 outline of the near-surface geology on the coast and inland, and introduces a different 29 view on the structure of the Cretaceous and Palaeogene strata. -
Triassic: Seasonal Rivers, Dusty Deserts and Saline Lakes
Triassic: seasonal rivers, dusty deserts and saline lakes Ruffell, A., & Hounslow, M. (2006). Triassic: seasonal rivers, dusty deserts and saline lakes. In P. F. Rawson, & P. Brenchley (Eds.), The Geology of England & Wales. (pp. 295-325). Geological Society of London. Published in: The Geology of England & Wales. Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:28. Sep. 2021 Triassic: seasonal rivers, 13 dusty deserts and saline lakes M. W. HOUNSLOW & A. H. RUFFELL The collision of Siberia and the Kazakstan microplate with European palaeoenvironmental signatures the eastern side of the Fennoscandia continent in the Permian amalgamated the last major continental fragments to produce The Permian witnessed the fragmentation of the core of the the supercontinent Pangaea, which persisted into the Jurassic Variscan Mountains into a number of separate areas, such as the Armorican, Bohemian and Iberian massifs (Fig. -
Central England Regional Geology RWM | Central England Regional Geology
Central England regional geology RWM | Central England Regional Geology Contents 1 Introduction Subregions Central England: summary of the regional geology Available information for this region 2 Rock type Younger sedimentary rocks Older sedimentary rocks 3 Basement rocks Rock structure 4 Groundwater 5 Resources 6 Natural processes Further information 7 - 16 Figures 17 - 18 Glossary Clicking on words in green, such as sedimentary or lava will take the reader to a brief non-technical explanation of that word in the Glossary section. By clicking on the highlighted word in the Glossary, the reader will be taken back to the page they were on. Clicking on words in blue, such as Higher Strength Rock or groundwater will take the reader to a brief talking head video or animation providing a non-technical explanation. For the purposes of this work the BGS only used data which was publicly available at the end of February 2016. The one exception to this was the extent of Oil and Gas Authority licensing which was updated to include data to the end of June 2018. 1 RWM | Central England Regional Geology Introduction This region covers the English Midlands including Northamptonshire, Leicestershire, Rutland, Warwickshire, Staffordshire and West Midlands and parts of Derbyshire, Nottinghamshire, Worcestershire, Cheshire and Shropshire. Subregions To present the conclusions of our work in a concise and accessible way, we have divided the region into 3 subregions (see Figure 1 below). We have selected subregions with broadly similar geological attributes relevant to the safety of a GDF, although there is still considerable variability in each subregion. -
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).