The Holostratigraphy of the Albian Stage (Lower Cretaceous) of the United Kingdom and Its Continental Shelf

Total Page:16

File Type:pdf, Size:1020Kb

The Holostratigraphy of the Albian Stage (Lower Cretaceous) of the United Kingdom and Its Continental Shelf The holostratigraphy of the Albian Stage (Lower Cretaceous) of the United Kingdom and its continental shelf Holostrat Research Report RR/06/01 HOW TO NAVIGATE THIS DOCUMENT Bookmarks The main elements of the table of contents are book- marked enabling direct links to be followed to the principal section headings and sub-headings, figures, plates and tables irrespective of which part of the document the user is viewing. In addition, the report contains links: from the principal section and subsection headings back to the contents page, from each reference to a figure, plate or table directly to the corresponding figure, plate or table, from each figure, plate or table caption to the first place that figure, plate or table is mentioned in the text and from each page number back to the contents page. RETURN TO CONTENTS PAGE BRITISH GEOLOGICAL SURVEY RESEARCH REPORT RR/06/01 The holostratigraphy of the Albian Stage (Lower Cretaceous) of the United Kingdom and its continental The National Grid and other Ordnance Survey data are used with the permission of the shelf Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2006. Key words I P Wilkinson Albian; Holostrat; Lower Cretaceous Front cover Folkestone Warren, Kent. Slipped and fallen masses of Chalk and Gault overlying the Gault outcrop. Bibliographical reference Wilkinson, I P. 2006. The holostratigraphy of the Albian Stage (Lower Cretaceous) of the United Kingdom and its continental shelf. British Geological Survey Research Report RR/06/01 124 pp. ISBN 0 85272 442 1 Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. Maps and diagrams in this book use topography based on Ordnance Survey mapping. © NERC 2006. All rights reserved. Keyworth, Nottingham British Geological Survey 2006 BRITISH GEOLOGICAL SURVEY British Geological Survey offices The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham, Edinburgh and London; see contact ຜ 0115–936 3100 Fax 0115–936 3200 details below or shop online at www.geologyshop.com e-mail: [email protected] www.bgs.ac.uk The London Information Office also maintains a reference collec- Online shop: www.geologyshop.com tion of BGS publications including maps for consultation. Murchison House, West Mains Road, Edinburgh EH9 3LA The Survey publishes an annual catalogue of its maps and other ຜ 0131–667 1000 Fax 0131–668 2683 publications; this catalogue is available from any of the BGS Sales e-mail: [email protected] Desks. London Information Office at the Natural History Museum The British Geological Survey carries out the geological survey of (Earth Galleries), Exhibition Road, South Kensington, London Great Britain and Northern Ireland (the latter is an agency service SW7 2DE for the government of Northern Ireland), and of the surrounding ຜ 020–7589 4090 Fax 020–7584 8270 continental shelf, as well as its basic research projects. It also ຜ 020–7942 5344/45 e-mail: [email protected] undertakes programmes of British technical aid in geology in developing countries as arranged by the Department for Forde House, Park Five Business Centre, Harrier Way, International Development and other agencies. Sowton, Exeter, Devon EX2 7HU ຜ 01392–445271 Fax 01392–445371 The British Geological Survey is a component body of the Natural Environment Research Council. Geological Survey of Northern Ireland, Colby House, Stranmillis Court, Belfast BT9 5BF ຜ 028–9038 8462 Fax 028–9038 8461 Maclean Building, Crowmarsh Gifford, Wallingford, Oxfordshire OX10 8BB ຜ 01491–838800 Fax 01491–692345 Columbus House, Greenmeadow Springs, Tongwynlais, Cardiff, CF15 7NE ຜ 029–2052 1962 Fax 029–2052 1963 Parent Body Natural Environment Research Council, Polaris House, North Star Avenue, Swindon, Wiltshire SN2 1EU ຜ 01793–411500 Fax 01793–411501 ii Contents 1 The Albian Stage 1 5.33 Holostratigraphical event ALB 33 81 1.1 Definition 1 5.34 Holostratigraphical event ALB 34 81 1.2 Author 1 5.35 Holostratigraphical event ALB 35 81 1.3 Derivation of name 1 5.36 Holostratigraphical event ALB 36 81 1.4 Original reference localities 1 5.37 Holostratigraphical event ALB 37 81 1.5 Synonyms 1 6 Albian localities in the United Kingdom 82 1.6 Substages 1 6.1 Speeton Clay Formation (‘A’ Beds) 82 1.7 British lithostratigraphical units 1 6.2 Carstone Formation 82 2 Lithostratigraphy 4 6.3 Folkestone Formation 85 2.1 North Sea Basin 4 6.4 Sandrock Formation 90 2.2 Onshore England 8 6.5 Lower Greensand Formation (Bedchester 3 Biostratigraphy 61 Sands Member) 91 3.1 Ammonite biostratigraphy 61 6.6 Gault Formation (Eastern England: 3.2 Belemnite biostratigraphy 65 Bedfordshire–Norfolk) 92 3.3 Calcareous nannofossil biostratigraphy 66 6.7 Gault Formation (Southern England: 3.4 Dinoflagellate cyst biostratigraphy 69 Dorset–Kent) 97 3.5 Foraminiferida biostratigraphy 71 6.8 Gault Formation (‘Junction Beds’ Member) 102 3.6 Ostracod biostratigraphy 74 6.9 Hunstanton Formation 103 6.10 Upper Greensand Formation 109 4 Other stratigraphical methods 77 6.11 Cambridge Greensand Formation 117 4.1 Chemostratigraphy 77 References 4.2 Geophysical methods 77 118 4.3 Magnetostratigraphy 77 4.4 Sequence stratigraphy 78 TABLES 4.5 Selected references 78 5 Holostratigraphical events of the Albian Stage 79 1 Biostratigraphical correlation of the Speeton ‘A’ beds 5.1 Holostratigraphical event ALB 1 79 (Mitchell and Underwood, 1999) 10 5.2 Holostratigraphical event ALB 2 79 2 Correlation of the Hunstanton Formation at Speeton, 5.3 Holostratigraphical event ALB 3 79 South Ferribly and Hunstanton with the Gault of East 5.4 Holostratigraphical event ALB 4 79 Anglian 41 5.5 Holostratigraphical event ALB 5 79 3 Subdivision of the Upper Greensand on the Isle of 5.6 Holostratigraphical event ALB 6 79 Wight after Jukes-Brown and Hill (1900) 50 5.7 Holostratigraphical event ALB 7 79 4 Correlation of the Upper Greensand in Devon and 5.8 Holostratigraphical event ALB 8 79 Dorset 50 5.9 Holostratigraphical event ALB 9 79 5.10 Holostratigraphical event ALB 10 79 5.11 Holostratigraphical event ALB 11 79 FIGURES 5.12 Holostratigraphical event ALB 12 79 5.13 Holostratigraphical event ALB 13 79 1 Distribution of Albian sediments at outcrop 2 5.14 Holostratigraphical event ALB 14 79 2 The Albian holostratigraphical scheme at end of report 5.15 Holostratigraphical event ALB 15 80 3 Correlation of the Albian formations in the North Sea 5.16 Holostratigraphical event ALB 16 80 Basin 4 5.17 Holostratigraphical event ALB 17 80 4 The Albian sequence of the North Sea: Wick 5.18 Holostratigraphical event ALB 18 80 Sandstone, Carrack and Radby formations 5 5.19 Holostratigraphical event ALB 19 80 5 Correlation of the Radby, Carrack and Wick sandstone 5.20 Holostratigraphical event ALB 20 80 formations in the North Sea Basin (after Johnson and 5.21 Holostratigraphical event ALB 21 80 Lott, 1993) 7 5.22 Holostratigraphical event ALB 22 80 6 ‘A Beds’ Member of the Speeton Clay Formation at 5.23 Holostratigraphical event ALB 23 80 Reighton 9 5.24 Holostratigraphical event ALB 24 80 7 The Carstone at Hunstanton 11 5.25 Holostratigraphical event ALB 25 80 8 Lower unit of the Folkestone Formation, East Cliff, 5.26 Holostratigraphical event ALB 26 80 Folkestone 13 5.27 Holostratigraphical event ALB 27 80 9 Upper part of the Folkestone Formation at Baker’s 5.28 Holostratigraphical event ALB 28 81 Gap, East Cliff, Folkestone 14 5.29 Holostratigraphical event ALB 29 81 10 Correlation of the upper unit of the Folkestone 5.30 Holostratigraphical event ALB 30 81 Formation in the south-east England 15 5.31 Holostratigraphical event ALB 31 81 11 Upper part of the Folkestone Formation at Parrat’s Pit, 5.32 Holostratigraphical event ALB 32 81 Wreccles 16 iii 12 Lower part of the Folkestone Formation in south-east 28 Correlation of the Gault and Upper Greensand (UGS) England 17 formations in the Isle of Wight and English Channel 13 Upper part of the Folkestone Formation at Squerryes by means of density (DT) logs 35 Main Pit, Westerham, Kent 18 29 The Gault of Church Farm Borehole, Shaftesbury 36 14 Lithostratigraphy of the Sandrock Formation at 30 The Gault of Rookley Brick Pit, Isle of Wight 37 Rochen End to Blackgang Chine, Chale Bay, Isle of 31 Locality map of the Leighton Buzzard area showing Wight 20 the localities from which the Junction Beds and Gault 15 The Sandrock Formation at Compton Bay 21 have been described 38 16 The position of the Bedchester Sands Member near 32 Junction Beds around Leighton Buzzard 39 Bedchester 23 33 The Hunstanton Formation at Speeton, Yorkshire 42 17 Correlation of the Gault of the reference section of the 34 The Hunstanton Formation at seven localities in Mundford ‘C’ Borehole with other sequences of East Norfolk and Lincolnshire 43 Anglia and the relationship between macrofossil and 35 The Foxmould, Whitecliff Chert and Bindon ostracod biostratigraphy 24 Sandstone members of the Upper Greensand 18 Stratigraphy of the Gault at Copt Point, Folkestone 25 Formation of Devon, Dorset and Somerset 45 19 Locality map of East Anglia and Lincolnshire 36 Distribution of the Upper Greensand Formation,
Recommended publications
  • M25 and M26 Economic Case Study
    M25 M26 Connectivity 21/06/2016 Reference number 103712 ECONOMIC CASE STUDY FINAL REPORT M25 M26 CONNECTIVITY ECONOMIC CASE STUDY IDENTIFICATION TABLE Client/Project Kent County Council owner Project M25 M26 Connectivity Study Economic Case Study Type of document Final Report Date 21/06/2016 File name M25M26 Report 2c (final).docx Reference number 103712 Number of pages 83 APPROVAL Version Name Date Modifications Ian Wilkinson, Author 07/04/2016 John Stephens Ian Wilkinson, 1 Checked by 07/04/2016 Version 1 Draft for client David Carter consideration Approved David Carter 07/04/2016 by Ian Wilkinson, Version 2 Report including client Author John Stephens, 21/06/2016 feedback: incorporating minor expansion on reporting of scheme David Carter costs, wider consideration of Ian Wilkinson, GIF/SHMA issues and dependent Checked by 21/06/2016 David Carter housing case, as well as minor 2c drafting points Version 2a/b including a few further snagging corrections and other minor Approved changes David Carter 21/06/2016 by Version 2c incorporating final comments from KCC and the study working group TABLE OF CONTENTS SUMMARY 6 BACKGROUND AND EXISTING STUDIES 6 HIGHWAY MODEL REVIEW 6 HIGHWAY OUTCOMES 7 WIDER ECONOMIC BENEFITS 10 OVERALL VALUE FOR MONEY CASE 10 LOCAL STAKEHOLDER CONSULTATION 11 CONCLUSIONS 12 1. INTRODUCTION 14 1.1 OVERVIEW 14 1.2 BACKGROUND PROVIDED BY KENT COUNTY COUNCIL (WITH SOME MINOR ADAPTATION) 15 1.3 DATA PROVISION 18 2. QUALITATIVE REVIEW 22 2.1 POLICY CONTEXT 22 2.2 ECONOMIC/VALUE FOR MONEY CASE AND WIDER BUSINESS CASE DELIVERY 23 3. HIGHWAY MODEL REVIEW 26 3.1 INTRODUCTION AND MODEL ROBUSTNESS 26 3.2 HIGHWAY MODEL REVIEW AND ACTIONS 26 3.3 HIGHWAY MODEL VALIDATION 30 4.
    [Show full text]
  • On the Barremian - Lower Albian Stratigraphy of Colombia
    On the Barremian - lower Albian stratigraphy of Colombia Philip J. Hoedemaeker Hoedemaeker, Ph.J. 2004. On the Barremian-lower Albian stratigraphy of Colombia. Scripta Geologica, 128: 3-15, 3 figs., Leiden, December 2004. Ph.J. Hoedemaeker, Department of Palaeontology, Nationaal Natuurhistorisch Museum, P.O. Box 9517, 2300 RA Leiden, The Netherlands (e-mail: [email protected]). Key words – stratigraphy, Barremian, Aptian, depositional sequences, Colombia. The biostratigraphy and sequence stratigraphy of the Barremian deposits, and the biostratigraphy of the Aptian deposits in the Villa de Leyva area in Colombia are briefly described. Contents Introduction ....................................................................................................................................................... 3 Barremian ............................................................................................................................................................ 4 Barremian sequence stratigraphy ............................................................................................................ 6 Aptian ................................................................................................................................................................. 11 Lowermost Albian ........................................................................................................................................ 13 Conclusions ....................................................................................................................................................
    [Show full text]
  • 71 Bus Time Schedule & Line Route
    71 bus time schedule & line map 71 Chichester View In Website Mode The 71 bus line (Chichester) has 2 routes. For regular weekdays, their operation hours are: (1) Chichester: 9:30 AM (2) Storrington: 1:00 PM Use the Moovit App to ƒnd the closest 71 bus station near you and ƒnd out when is the next 71 bus arriving. Direction: Chichester 71 bus Time Schedule 64 stops Chichester Route Timetable: VIEW LINE SCHEDULE Sunday Not Operational Monday Not Operational Bus Station, Storrington Old Mill Drive, Storrington Tuesday Not Operational Old Mill Drive, Storrington Wednesday 9:30 AM Fryern Road, Storrington Thursday Not Operational Friday Not Operational Nightingale Lane, Storrington Puttick Close, Storrington Saturday Not Operational Mead Lane, Storrington Sullington Copse, Storrington Oak Close, Storrington And Sullington Civil Parish 71 bus Info Direction: Chichester Rydon College, Storrington Stops: 64 Trip Duration: 74 min Greenhurst Lane, Abingworth Line Summary: Bus Station, Storrington, Old Mill Drive, Storrington, Fryern Road, Storrington, Jackets Hill, Abingworth Nightingale Lane, Storrington, Mead Lane, Storrington, Sullington Copse, Storrington, Rydon High Bar Lane, Abingworth College, Storrington, Greenhurst Lane, Abingworth, Jackets Hill, Abingworth, High Bar Lane, Abingworth, Woodlands Cottages, Thakeham Civil Parish South Hill Barn, Thakeham, Town House Farm, South Hill Barn, Thakeham Thakeham, Goffsland Farm, Thakeham, Picketty Cottages, West Chiltington, Lower Voakes Farm, Town House Farm, Thakeham West Chiltington, East Street,
    [Show full text]
  • Local Plan Review Issues and Options Consultation 2018 Summary of Responses and Proposed Next Steps
    Local Plan Review Issues and Options Consultation 2018 Summary of responses and proposed next steps September 2018 Left Blank on Purpose CONTENTS Page Built up Area Boundary (BUAB) (in alphabetical order) 1 Conversion of Existing Agricultural Buildings/ Rural Development 24 Countryside Protection 29 Economy / Economic Development Strategy 30 Employment Sites 51 General 80 Key Employment Areas (KEAs) 86 Local Planning Context 102 Other 106 Rural Economic Development 114 Rural Workers Accommodation 120 Secondary Settlements (in alphabetical order) 126 Sustainable Rural Development 158 Tourism 160 Horsham District Council Local Plan Review Issues and Options Consultation 2018 Summary of Responses and Proposed Next Steps Agent For: Topic Area Summary of Comment Nature of Next steps Site reference comment Surname Organisation Respondent No Respondent 8 Woolley BUAB – Ashington Amend Ashington Built Up Area Boundary to Object Comments noted and the include Church Farm House, Church Lane. following action will be The private drive from Church Lane to the undertaken: Ashington property is already included. Site is adjacent Built Up Area Boundary to central areas of the village and therefore will be reviewed directly relates to the built form rather than the countryside. 97 Carey BUAB - Ashington Land immediately north of the village is Observation Comments noted and the Ashington characterised by low/medium density housing following action will be served by B2133. It has a strong physical undertaken: Ashington connectivity with the existing settlement of Built Up Area Boundary Ashington. Consideration should be given to will be reviewed creating a more extensive review of the proposed Built Up Area Boundary taking into account the level of housing identified in the Housing Needs Assessment undertaken as part of the Ashington Neighbourhood Plan.
    [Show full text]
  • ALBIAN AMMONITES of POLAND (Plates 1—25)
    PALAEONTOLOGIA POLQNICA mm ■'Ъ-Ь POL T S H ACADEMY OF SCIENCES INSTITUTE OF PALEOBIOLOGY PALAEONTOLOGIA POLONICA—No. 50, 1990 t h e a l b ia w AMMONITES OF POLAND (AMQNITY ALBU POLS К I) BY RYSZARD MARCINOWSKI AND JOST WIEDMANN (WITH 27 TEXT-FIGURES, 7 TABLES AND 25 PLATES) WARSZAWA —KRAKÔW 1990 PANSTWOWE WYDAWNICTWO NAUKOWE KEDAKTOR — EDITOR JOZEP KA2MIERCZAK 2ASTEPCA HEDAKTOHA _ ASSISTANT EDITOR m AôDAlenA BÛRSUK-BIALYNICKA Adres Redakcjl — Address of the Editorial Office Zaklad Paleobiologij Polska Akademia Nauk 02-089 Warszawa, AI. 2w irki i Wigury 93 KOREKTA Zespol © Copyright by Panstwowe Wydawnictwo Naukowe Warszawa — Krakôw 1990 ISBN 83-01-09176-2 ISSN 0078-8562 Panstwowe Wydawnielwo Naukowe — Oddzial w Krakowie Wydanie 1, Naklad 670 + 65 cgz. Ark. wyd. 15. Ark. druk. 6 + 25 wkladek + 5 wklejek. Papier offset, sat. Ill kl. 120 g. Oddano do skiadania w sierpniu 1988 r. Podpisano do druku w pazdzierniku 1990 r. Druk ukoriczono w listopadzie 1990 r. Zara. 475/87 Drukarnia Uniwersytetu Jagielloriskiego w Krakowie In Memory of Professor Edward Passendorfer (1894— 1984) RYSZARD MARCINOWSKI and JOST WIEDMANN THE ALBIAN AMMONITES OF POLAND (Plates 1—25) MARCINOWSKI, R. and WIEDMANN, J.: The Albian ammonites of Poland. Palaeonlologia Polonica, 50, 3—94, 1990. Taxonomic and ecological analysis of the ammonite assemblages, as well as their general paleogeographical setting, indicate that the Albian deposits in the Polish part of the Central European Basin accumulated under shallow or extremely shallow marine conditions, while those of the High-Tatra Swell were deposited in an open sea environment. The Boreal character of the ammonite faunas in the epicontinental area of Poland and the Tethyan character of those in the Tatra Mountains are evident in the composition of the analyzed assemblages.
    [Show full text]
  • Lineages, Splits and Divergence Challenge Whether the Terms Anagenesis and Cladogenesis Are Necessary
    Biological Journal of the Linnean Society, 2015, , – . With 2 figures. Lineages, splits and divergence challenge whether the terms anagenesis and cladogenesis are necessary FELIX VAUX*, STEVEN A. TREWICK and MARY MORGAN-RICHARDS Ecology Group, Institute of Agriculture and Environment, Massey University, Palmerston North, New Zealand Received 3 June 2015; revised 22 July 2015; accepted for publication 22 July 2015 Using the framework of evolutionary lineages to separate the process of evolution and classification of species, we observe that ‘anagenesis’ and ‘cladogenesis’ are unnecessary terms. The terms have changed significantly in meaning over time, and current usage is inconsistent and vague across many different disciplines. The most popular definition of cladogenesis is the splitting of evolutionary lineages (cessation of gene flow), whereas anagenesis is evolutionary change between splits. Cladogenesis (and lineage-splitting) is also regularly made synonymous with speciation. This definition is misleading as lineage-splitting is prolific during evolution and because palaeontological studies provide no direct estimate of gene flow. The terms also fail to incorporate speciation without being arbitrary or relative, and the focus upon lineage-splitting ignores the importance of divergence, hybridization, extinction and informative value (i.e. what is helpful to describe as a taxon) for species classification. We conclude and demonstrate that evolution and species diversity can be considered with greater clarity using simpler, more transparent terms than anagenesis and cladogenesis. Describing evolution and taxonomic classification can be straightforward, and there is no need to ‘make words mean so many different things’. © 2015 The Linnean Society of London, Biological Journal of the Linnean Society, 2015, 00, 000–000.
    [Show full text]
  • Kemsing Walk 8 Also Use Ordnance Survey Map: 4 ¡ 3 9 Stile Gate View Stile ¡ ¡ Take Care Take 10 2 1 ¡ 0.5 1 0.5 ¡ 11 12 Miles Kilometres 0 N
    Walk Overview Distance: 6.5 miles /10.4 kms Start /Finish: Centre of the village of Kemsing Stiles: 18 Gates: 6 Terrain: Field paths and tracks with some steep slopes Views: Magnificent views across the Weald of Kent Toilets: At Kemsing village car park Refreshments: pubs and shops in Kemsing. Pub at Heaverham When you’re out walking in the countryside, please respect the Countryside Code. Be safe – plan ahead and follow any arrows or signs Leave gates and property as you find them Protect plants and animals, and take your litter home Keep dogs under close control Consider other people By car: From A25 at Seal follow signs to Kemsing Parking: Free car park in centre of village Train: Kemsing station is 2.5 miles from village on the London Victoria to Maidstone East line Train enquiries tel 08457 484950 This challenging 6.5 mile route passes through the beautiful village of Kemsing and offers walkers magnificent views across the Weald of Kent. Bus: Buses 431/432 go through the village The village of Kemsing was first recorded in AD 822 and is a fascinating Traveline 0870 200 2233 start point for the walk. The Church of St Mary the Virgin dates from 1060 and features a Norman Font. The walk ascends and decends the North Downs and paths can be muddy and slippery after rain. Route Description 1 From the Car Park in Kemsing Village 8 Cross straight over the minor road and walk eastwards along Heaverham Road. keep heading westwards along the path. Turn right along a path opposite Church 2 9 Turn left and immediately right again at Lane and continue across open farmland Cotman's Ash Lane still on the National towards Crowdleham.
    [Show full text]
  • A CRITICAL EVALUATION of the LOWER-MIDDLE PALAEOLITHIC ARCHAEOLOGICAL RECORD of the CHALK UPLANDS of NORTHWEST EUROPE Lesley
    A CRITICAL EVALUATION OF THE LOWER-MIDDLE PALAEOLITHIC ARCHAEOLOGICAL RECORD OF THE CHALK UPLANDS OF NORTHWEST EUROPE The Chilterns, Pegsdon, Bedfordshire (photograph L. Blundell) Lesley Blundell UCL Thesis submitted for the degree of PhD September 2019 2 I, Lesley Blundell, confirm that the work presented in this thesis is my own. Where information has been derived from other sources, I confirm that this has been indicated in the thesis. Signed: 3 4 Abstract Our understanding of early human behaviour has always been and continues to be predicated on an archaeological record unevenly distributed in space and time. More than 80% of British Lower-Middle Palaeolithic findspots were discovered during the late 19th/early 20th centuries, the majority from lowland fluvial contexts. Within the British planning process and some academic research, the resultant findspot distributions are taken at face value, with insufficient consideration of possible bias resulting from variables operating on their creation. This leads to areas of landscape outside the river valleys being considered to have only limited archaeological potential. This thesis was conceived as an attempt to analyse the findspot data of the Lower-Middle Palaeolithic record of the Chalk uplands of southeast Britain and northern France within a framework complex enough to allow bias in the formation of findspot distribution patterns and artefact preservation/discovery opportunities to be identified and scrutinised more closely. Taking a dynamic, landscape = record approach, this research explores the potential influence of geomorphology, 19th/early 20th century industrialisation and antiquarian collecting on the creation of the Lower- Middle Palaeolithic record through the opportunities created for artefact preservation and release.
    [Show full text]
  • Chapter 2 Physical Characteristics of the Study Area
    CHAPTER 2 PHYSICAL CHARACTERISTICS OF THE STUDY AREA 2.1. Location of study area The study area incorporates part of north Hertfordshire, south and mid- Bedfordshire as well as the southwest corner of Cambridgeshire and lies approximately 40 km north of London (Figure 1.1). Coverage of the area by British Geological Survey (BGS) 1:50,000 map sheets is shown in Figure 2.1. 2.2. Bedrock geology The strikes of the solid geological formations are approximately northeast- southwest across the study area (Figure 2.2). The solid geological succession is shown in Table 2.1. To the northwest of the Chiltern Hills the Gault Clay forms a rich agricultural landscape, representing a continuation of the Vale of Aylesbury. Beyond this, running approximately from Bow Brickhill (SP915343) to Gamlingay (TL234525) is a discontinuous ridge formed by the Woburn Sands Formation, part of the Lower Greensand. This prominent ‘Greensand Ridge’, rising to 170 m O.D. at Bow Brickhill, separates the Cretaceous clays from the Jurassic Oxford and Ampthill Clays to the northwest. The oldest formation is recorded in a borehole (TL23NE1) at Ashwell (TL286390), where Devonian strata were reached at a depth of 186.54 m, i.e. 93 m below O.D. (Smith, 1992). Lying just beyond the northern boundary of the present study area, north of the River Ouse, a borehole (TL15NE2) at Wyboston (TL175572) penetrated Ordovician rocks of Tremadoc age at a depth of approximately 230 m (Moorlock et al ., 2003). The Oxford Clay of the Upper Jurassic represents the oldest formation outcropping within the study area.
    [Show full text]
  • Las Especies Del Orden Trigonioida En El Cretácico De Chile
    U N I V E R S I D A D D E C O N C E P C I Ó N DEPARTAMENTO DE CIENCIAS DE LA TIERRA 10° CONGRESO GEOLÓGICO CHILENO 2003 LAS ESPECIES DEL ORDEN TRIGONIOIDA EN EL CRETÁCICO DE CHILE PÉREZ D’A., E. 1 Y REYES, R. 2 1Servicio Nacional de Geología y Minería, Ada. Santa María 0104, Providencia, Santiago, Chile [email protected] 2Avda. Diego Portales 936, Departamento 6 (recreo) Viña del Mar, Chile CLASIFICACIÓN DEL ORDEN TRIGONIOIDA EN EL CRETÁCICO DE CHILE Orden Trigonioida Dall, 1899 Suborden Trigoniina Dall, 1899 Superfamilia Trigoniacea Lamarck, 1819 Familia Trigoniidae Lamarck, 1819 Subfamilia Trigoniinae Lamarck, 1819 Género Trigonia Bruguière, 1789 T. carinata Agassiz, 1840, Titoniano inferior-Barremiano (?), Zonas de Windhauseniceras internispinosum, Corongoceras alternans y Substeuroceras koeneni (Titoniano medio y superior), Cuyaniceras transgrediens y Spiticeras (Kilianiceras) damesi (Berriasiano superior), Holcoptychites neuquensis (Hauteriviano medio; Reyes y Pérez, 1978), [Titoniano superior, Zona de Substeueroceras koeneni, Hauteriviano inferior-medio, Zonas de Lyticoceras pseudoregale y Holcoptychites neuquensis; Leanza, 1993]; T. aliexpandita Leanza y Garate, 1983, [Hauteriviano inferior-medio, Zonas de Lyticoceras pseudoregale y Holcoptychites neuquensis; Leanza, 1993]. Familia Neotrigoniidae Kobayashi, 1954 Subfamilia Nototrigoniinae Skwarko, 1963 Género Pacitrigonia Marwick, 1932 P. hanetiana (d’Orbigny, 1842), Campaniano (Reyes y Pérez, 1979), Campaniano superior- Maastrichtiano inferior (Pérez y Reyes, 1978); P. ecplecta (Wilckens, 1905), Campaniano- Maastrichtiano; Pérez y Reyes, 1978), P. regina (Wilckens, 1910), Campaniano inferior (alto)- Maastrichtiano inferior (Pérez y Reyes, 1978). Suborden Myophorellina Cooper, 1991 Superfamilia Myophorellacea Kobayashi, 1954 Familia Myophorellidae, Kobayashi, 1954 Subfamilia Myophorellinae Kobayashi, 1954 Género Mediterraneotrigonia Nakano, 1974 Todas las contribuciones fueron proporcionados directamente por los autores y su contenido es de su exclusiva responsabilidad.
    [Show full text]
  • Review of the Pterodactyloid Pterosaur Coloborhynchus 219
    Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie B28 DAVID W. E. HONE & ERIC BUFFETAUT (Eds) Flugsaurier: pterosaur papers in honour of Peter Wellnhofer CONTENTS/INHALT Dedication 3 PETER WELLNHOFER A short history of pterosaur research 7 KEVIN PADIAN Were pterosaur ancestors bipedal or quadrupedal?: Morphometric, functional, and phylogenetic considerations 21 DAVID W. E. HONE & MICHAEL J. BENTON Contrasting supertree and total-evidence methods: the origin of the pterosaurs 35 PAUL M. BARRETT, RICHARD J. BUTLER, NICHOLAS P. EDWARDS & ANDREW R. MILNER Pterosaur distribution in time and space: an atlas 61 LORNA STEEL The palaeohistology of pterosaur bone: an overview 109 S. CHRISTOPHER BENNETT Morphological evolution of the wing of pterosaurs: myology and function 127 MARK P. WITTON A new approach to determining pterosaur body mass and its implications for pterosaur fl ight 143 MICHAEL B. HABIB Comparative evidence for quadrupedal launch in pterosaurs 159 ROSS A. ELGIN, CARLOS A. GRAU, COLIN PALMER, DAVID W. E. HONE, DOUGLAS GREENWELL & MICHAEL J. BENTON Aerodynamic characters of the cranial crest in Pteranodon 167 DAVID M. MARTILL & MARK P. WITTON Catastrophic failure in a pterosaur skull from the Cretaceous Santana Formation of Brazil 175 MARTIN LOCKLEY, JERALD D. HARRIS & LAURA MITCHELL A global overview of pterosaur ichnology: tracksite distribution in space and time 185 DAVID M. UNWIN & D. CHARLES DEEMING Pterosaur eggshell structure and its implications for pterosaur reproductive biology 199 DAVID M. MARTILL, MARK P. WITTON & ANDREW GALE Possible azhdarchoid pterosaur remains from the Coniacian (Late Cretaceous) of England 209 TAISSA RODRIGUES & ALEXANDER W.
    [Show full text]
  • Trigoniidae; Bivalvia) En El Cretacico Superior Del Occidente De La Provincia De La Pampa, Argentina
    DESCRIPCION DE DOS NUEVAS ESPECIES DE PACITRIGONIA MARWICK y AUSTROTRIGONIA SKWARKO (TRIGONIIDAE; BIVALVIA) EN EL CRETACICO SUPERIOR DEL OCCIDENTE DE LA PROVINCIA DE LA PAMPA, ARGENTINA HECTOR A. LEANZA Secretada de Minerfa, CONICET, Avda. Santa Fe 1548, 1060 Sueros Aires SILVIO CASADIO Universidad Nacional de La Pampa, Departamento de Ciencias Naturales Uruguay 151, 6300 Santa Rosa, La Pampa, Argentina RESUMEN Se da a conocer, por primera vez, la presencia de la lamilia Trigoniidae en el Cretácico Superior del occidente de la Provincia de La Pampa, Argentina. En las localidades de Barda Baya y Salitral de La Amarga se ha determinado la presencia de los géneros australes Pacitrigonia Marwick y Austrotrigonia Skwarko a través de dos nuevas especies denominadas P. sobralisp. nov. y A. pampeanasp. nov., respectivamente, así como Pterotrigonia (Rinetrigonia) windhauseniana(Wilckens). En ambas localidades los taxones descritos se encuentran en la Formación Jagüel, en asociación con Eubaculites argentinicus (Weaver) y otros bivalvos y gastrópodos, que permiten su asignación al Maastrichtiano. El género Austrotrigonia Skwarko se cita por primera vez en América del Sur. Palabras claves: Bivalvia, Trigoniidae, Sistemática, Cretácico Superior, Maastrichtiano, Formación Jagüel, Provincia de La Pampa, Argentina. ABSTRACT The occurrence 01 the lamily Trigoniidae (Bivalvia) in the Upper Cretaceous 01 the western part 01 La Pampa Province, Argentina, is reported lorthe lirsttime. At Barda Baya and Salitral de LaAmarga localities, the presence 01 the austral genera Pacitrigonia Marwick and Austrotrigonia Skwarko were recorded, through two new species named P. sobrali sp. nov. and Austrotrigonia pampeana sp. nov. as well as Pterotrigonia (Rinetrigonia) windhauseniana (Wilckens). In both localities the described taxa occur in the Jagüel Formation, in association with Eubaculites argentinicus (Weaver) and other bivalves and gastropods, on the basis 01 which they are assigned to the Maastrichtian.
    [Show full text]