DEEP HISTORY COAST Economic Plan
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
PDF Viewing Archiving 300
Bull. Soc. belge Géol., Paléont., Hydrol. T. 79 fasc. 2 pp. 167-174 Bruxelles 1970 Bull. Belg. Ver. Geol., Paleont., Hydrol. V. 79 deel 2 blz. 167-174 Brussel 1970 MAMMALS OF THE CRAG AND FOREST BED B. McW1LLIAMs SuMMARY. In the Red and Norwich Crags mastodonts gradually give way to the southern elephant, large caballine horses and deer of the Euctenoceros group become common. Large rodents are represented by Castor, Trogontherium and rarely Hystrix; small forms include species of Mimomys. Carnivores include hyaena, sabre-toothed cat, leopard, polecat, otter, bear, seal and walrus. The Cromer Forest Bed Series had steppe and forest forms of the southern elephant and the mastodont has been lost. Severa! species of giant deer become widespread and among the many rodents are a. number of voles which develop rootless cheek teeth. The mole is common. Warmth indicators include a monkey, and more commonly hippopotamus. Possible indicators of cold include glutton and musk ox. Rhinoceros is widespread, and it is a time of rapid evolution for the elk. Carnivores include hyaena, bear, glutton, polecat, marten, wold and seal. The interpretation of mammalian finds from is represented by bones which resemble the the Crags and Forest Bed is not an easy mole remains but are about twice their size. matter. A proportion of the remains have been derived from eatlier horizons, others are Order Primates discovered loose in modern coastal deposits, and early collectors often kept inadequate The order is represented at this period m records. Owing to the uncertain processes of England by a single record of Macaca sp., the fossilisation or inadequate collecting there are distal end of a teft humerus from a sandy many gaps in our knowledge of the mammal horizon of the Cromerian at West Runton, ian faunas of these times. -
On the Occurrence of the Scimitar-Toothed Cat, Homotherium Latidens (Carnivora; Felidae), at Kents Cavern, England
Journal of Archaeological Science 40 (2013) 1629e1635 Contents lists available at SciVerse ScienceDirect Journal of Archaeological Science journal homepage: http://www.elsevier.com/locate/jas On the occurrence of the scimitar-toothed cat, Homotherium latidens (Carnivora; Felidae), at Kents Cavern, England Donald A. McFarlane a,*, Joyce Lundberg b a W.M. Keck Science Center, The Claremont Colleges, 925 North Mills Avenue, Claremont, CA 91711, USA b Department of Geography and Environmental Studies, Carleton University, Ottawa, ON K1S 5B6, Canada article info abstract Article history: Teeth of Homotherium latidens recovered from late Pleistocene sediments, Kents Cavern, England have Received 10 July 2012 long been the source of controversy. H. latidens is conspicuously absent from other late Pleistocene cave Received in revised form deposits in Britain, and is widely thought to have been extirpated from the region during the isotope 19 October 2012 stage 10 glacial period. Here we present high spatial resolution analyses of fluorine and uranium uptake Accepted 25 October 2012 profiles in teeth of three species from the same cave. The H. latidens tooth is clearly distinguished from the unambiguously provenanced Late Pleistocene hyaena and Middle Pleistocene cave bear teeth. These Keywords: results are consistent with the theory that the H. latidens teeth originated at an exogenous location, were Quaternary Cave probably transported to Kents Cavern as Palaeolithic trade goods, and were buried in Kents Cavern in Palaeontology Palaeolithic times. Fluorine Ó 2012 Elsevier Ltd. All rights reserved. Uranium Palaeolithic 1. Introduction latest marine isotope stage (MIS) 12 or earliest MIS 11 age (Lundberg and McFarlane, 2007). The Breccia has also yielded Kents1 Cavern, located on the southwest coast of England in human artifacts (Lowe, 1916) of late Cromerian (MIS 13) age which a suburb of the town of Torquay (50.4677 N, 3.5028 W, Fig. -
IPSWICH GEOLOGICAL GROUP August 1966 BULLETIN No. 1
IPSWICH GEOLOGICAL GROUP August 1966 BULLETIN No. 1 Contents Author Title Pages H. E. P. Spencer Geographic and Geological Notes on the Ipswich District 1-3 Coast Erosion S. J. J. MacFarlane The Crag Exposure to the West of the Water Tower on Rushmere 5-6 Heath R. A. D. Markham Marsupites from the Gipping Valley Chalk 6 R. A. D. Markham Note of some Crag fossils in the Museum of the Geology 6 Department of Birmingham University R. A. D. Markham Illustrations of some common Crag fossils 8-10 C. Holcombe & Section through junction of Red and Coralline Crags, ‘The Rocks’, 10-11 R. M. Ramsholt Bibliography: Paramoudra Club Bulletin 11 & 13 R. M. Hoxne Palaeoliths (John Frere) 14-15 R. M. Strata identified by organised fossils (William Smith) 15 R. M. Bibliography: Proceedings of the Prehistoric Society of East Anglia 16-19 C. Allen Fossils collected from the London Clay, 1963 19-20 R. M. Simplified table of local strata 20 R. Markham An excavation in the Coralline Crag at Tattingstone 21-23 R. A. D. Markham Waldringfield Crag 24-25 R. A. D. Markham Notes on Weavers Pit, Tuddenham St. Martin 25-27 R. A. D. Markham Acknowledgement and publication details 27 IPSWICH GEOLOGICAL GROUP August 1966 BULLETIN No. 1 GEOGRAPHIC AND GEOLOGICAL NOTES ON THE IPSWICH DISTRICT By H. E. P. Spencer, F.G.S. East Suffolk has beds of sand and clay deposited during the closing chapters of the series of geological epochs. In the region there are probably the greatest number of formations to be found in any such limited area. -
Pleistocene Small Cave Bear (Ursus Rossicus) from the South Siberia, Russia Un Pequeño Oso De Las Cavernas (Ursus Rossicus) Del Sur De Siberia, Rusia
Cadernos Lab. Xeolóxico de Laxe ISSN: 0213-4497 Coruña. 2001. Vol. 26, pp. 373-398 Pleistocene small cave bear (Ursus rossicus) from the South Siberia, Russia Un pequeño Oso de las Cavernas (Ursus rossicus) del Sur de Siberia, Rusia BARYSHNIKOV, G.1, FORONOVA, I.2 AB S T R A C T The skull, mandibles and cheek teeth of U. rossicus from four localities of the South Siberia are examined. This species inhabited the steppe regions in early Middle and Late Pleistocene. By odontological characters it is more close to U. r. rossicus from Krasnodar, than to U. rossicus uralensis from Kizel Cave in Ural. Discriminant analysis, based on measurements of lower cheek teeth of the cave bears from seven sites of Europe and Siberia, demonstrated that U. rossicus most resembles morphometrically U. savini. As a result of cladistic analysis employed 17 characters of skull, limb bones, and dentition, the phylogenetic tree has been obtained for 7 species of the genus Ur s u s . A four species of the cave bears are included in the subgenus Spelearctos: U. savini, U. rossicus, U. denin - geri and U. spelaeus. Key words: cave bears, Ur s u s , Siberia, Pleistocene, evolution (1) Zoological Institute, Russian Academy of Sciences, Universitetskaya naberezhnaya 1, 199034 St. Petersburg, Russia; e-mail: [email protected] (2) Institute of Geology, Siberian Branch of Russian Academy of Sciences, pr. Akad. Koptiuga 3, 630090 Novosibirsk, Russia; e-mail: [email protected] 374 BARYSHNIKOV & FORONOVA CAD. LAB. XEOL. LAXE 26 (2001) INTRODUCTION V E R E S H C H A G I N & T I K H O N O V, 1994; BA RY S H N I K O V , 1995). -
Geological Landscapes of the Norfolk Coast
Geological Landscapes of the Norfolk Coast Introducing five areas of striking geodiversity in the Norfolk Coast Area of Outstanding Natural Beauty Dersingham National Nature Reserve CONTENTS [clicking on relevant content lines will take you straight to the page] 1.0 Introduction---------------------------------------------------------------------------------------- 3 2.0 An overview of the Geodiversity of the Norfolk Coast Area of Outstanding Natural Beauty ------------------------------------------------------------------------------------ 4 3.0 Geological Landscapes------------------------------------------------------------------------ 7 3.1 WEST NORFOLK SANDSTONES ------------------------------------------------------ 7 3.2 HUNSTANTON GLACIAL----------------------------------------------------------------10 3.3 NORTH NORFOLK COASTAL ---------------------------------------------------------13 3.4 CROMER RIDGE ---------------------------------------------------------------------------18 3.5 EAST NORFOLK COASTAL ------------------------------------------------------------22 APPENDIX 1 – Summary of Geological Stratigraphy in the Norfolk Coast Area of Outstanding Natural Beauty-----------------------------------------------------------------25 APPENDIX 2 – Glossary -------------------------------------------------------------------------------27 APPENDIX 3 Geodiversity Characterisation & Conservation------------------------30 A3.1 WEST NORFOLK SANDSTONES Conservation and enhancement --------32 A3.2 HUNSTANTON GLACIAL Conservation and enhancement -
Patterns of Preglacial Sedimentation and Glaciotectonic Deformation Within
Published in Proceedings of the Geologist’s Association, 2009, Volume 120, pages 34-48. Patterns of preglacial sedimentation and glaciotectonic deformation within early Middle Pleistocene sediments at Sidestrand, north Norfolk, UK Jonathan R. Lee1,2 Abstract Middle Pleistocene preglacial and glacial sediments are described from Sidestrand in north Norfolk, UK. The sequence consists of estuarine and fluvial deposits of the Wroxham Crag and Cromer Forest‐bed formations that were deposited by, and adjacent to, a major river system that drained northern and central England during the ‘Cromerian Complex’. These preglacial sediments were subsequently overridden and partially tectonised during a glaciation that deposited till of the Happisburgh Formation associated with the first lowland glaciation of eastern England. Detailed examination of the stratigraphy and structural evolution of the sequence reveals that glaciotectonic rafts of Sidestrand Unio Bed material, a regionally important biostratigraphic marker horizon, have been remobilised and partially mixed with other lithologies whilst being transported and emplaced further up‐sequence by glaciotetconic processes. Caution should therefore be exercised when examining this deposit for biostratigraphic and palaeoenvironmental purposes to ensure that sampling is from in situ material. Key words: Pleistocene, East Anglia, preglacial, glaciotectonic. 1British Geological Survey, Keyworth, Nottingham, NG12 5GG. Email: [email protected] 2Department of Geography, Royal Holloway, University of London, -
Runton, Norfolk, England)
Cranium, jrg. 9, no. 2, pag. 77-84, augustus 1992 The Pleistocene Vertebrate Faunas of West Runton, Norfolk, England A.J. Stuart Summary the Norfolk is the fossil vertebrate the Cromer Forest Bed For- West Runton, on coast, most important single locality of marine fauna mation. The Lower Pleistocene (Pre-Pastonian and Pastonian stages) ’crags’ have yielded a sparse inclu- ding Mammuthus meridionalis, Mimomys pliocaenicus, and M. blanci. The fluvial of the West Runton Cromerian have organic deposits Freshwater Bed, type site, produced an exceptionally rich early MiddlePleistocene vertebrate assemblage, comprising: 8 fish taxa; 5 amphibians; 3 reptiles; several birds; and 43 mammals. The mammals include: voles Mimomys savini and and Pliomys episcopalis; extinct beaver Trogontherium cuvieri; monkey Macaca sylvanus, mammoth Mammuthus cf. meridionalis, rhinoceros Dicerorhinus etruscus, and giant deer Megaloceros verticornis. Pollen and macrofossils show that this fauna lived in association with forest in the first half of plant regional temperate the temperate stage. Samenvatting West Runton, aan de Norfolk kust in Engeland, is de meest belangrijke vindplaats van vertebratenfossielen afkomstig uit de Cromer Forest Bed Formatie. In de Vroeg Pleistocene (Pre-Pastonien en Pastonien stages) mariene ’crags’ zijn een klein aantal M. relatief zoogdierresten van o.a. Mammuthus meridionalis, Mimomys pliocaenicus en blanci verzameld. de Freshwater hebben De organische, fluviatiele afzettingen van West Runton Bed, type-lokaliteit van het Cromerien, Midden vertebratenfauna 8 5 een buitengewoon rijke vroeg Pleistocene opgeleverd met soorten vissen, soorten amphi- biën, 3 soorten reptielen, meerdere vogels en 43 soorten zoogdieren. De zoogdierfauna bevat o.a. woelmuizen Mimomys en de bever de de mammoet savini Pliomys episcopalis, uitgestorven Trogontherium cuvieri, aap Macaca sylvanus, Mam- cf. -
Ice-Rafted Erratics with Early Middle Pleistocene Shallow Marine
Published in Proceedings of the Geologists’ Association (2011) Possible ice-rafted erratics in late Early to early Middle Pleistocene shallow marine and coastal deposits in northeast Norfolk, UK. Nigel R. Larkina*, Jonathan R. Leeb & E. Rodger Connellc a The Natural History Department, Norfolk Museums and Archaeology Service, Shirehall, Market Avenue, Norwich, Norfolk NR1 3JQ, UK [email protected] b British Geological Survey, Keyworth, Nottingham NG12 5GG, UK [email protected] c Geography and Environment, School of Geosciences, University of Aberdeen, St Mary’s, Elphinstone Road, Aberdeen, AB24 3UF UK [email protected] *Corresponding author: email [email protected] telephone 07973 869613 Abstract Erratic clasts with a mass of up to 15 kg are described from preglacial shallow marine deposits (Wroxham Crag Formation) in northeast Norfolk. Detailed examination of their petrology has enabled them to be provenanced to northern Britain and southern Norway. Their clustered occurrence in coastal sediments in Norfolk is believed to be the product of ice-rafting from glacier incursions into the North Sea from eastern Scotland and southern Norway, and their subsequent grounding and melting within coastal areas of what is now north Norfolk. The precise timing of these restricted glaciations is difficult to determine. However, the relationship of the erratics to the biostratigraphic record and the first major expansion of ice into the North Sea suggest these events occurred during at least one glaciation between the late Early Pleistocene and early Middle Pleistocene (c. 1.1−0.6 Ma). In contrast to the late Middle (Anglian) and Late Pleistocene (Last Glacial Maximum) glaciations, where the North Sea was largely devoid of extensive marine conditions, the presence of far-travelled ice-rafted materials implies that earlier cold stage sea-levels were considerably higher. -
The Norfolk & Norwich
TRANSACTIONS OF THE NORFOLK & NORWICH NATURALISTS' SOCIETY 1# £ Vol.jtf' Part MAY 1979 ISBN 0375 7226 TRANSACTIONS OF THE NORFOLK AND NORWICH NATURALISTS' SOCIETY Volume 25, Part 1 (May 1979) Editor Dr E. A. Ellis CONTENTS Page Some effects of the sea flood at Wells-next-the-sea, 1 1th January, 1978 by P. R. Banham 263 The effects of the storm of 11th January 1978 on Blakeney Point by D.f.B. White 267 Three rare species on the North Norfolk Coast by J. P. Skipworth 270 Birds of the Cromer Forest Bed Series of the East Anglian Pleistocene byC. J. O. Harrison 2 77 A study of Veronica triphyllos L., Veronica praecox All and Veronica vema L. at Weeting Heath Arable Reserve, Norfolk by Anne Bum 287 Norwich bird-seed mixtures and the casual plants of Harford Tip by Nicholas S. Watts and Geoffrey D. Watts 300 1978 Weather Summary by T. B. Norgate 310 Two New Norfolk Roses by E. L. Swann 315 OFFICERS OF THE SOCIETY 1978-79 President: Mr P. J. Trett President Elect: Mr E. T. Daniels 41 Brian Avenue, Norwich Vice-Presidents: P. R. Banham, A. Bull, K. B. Clarke, K. C. Durrant, E. A. Ellis, R. Jones, M. J. Seago, J. A. Steers, E. L. Swann, F. J. Taylor-Page General Secretary: R. E. Baker 25 Southern Reach, Mulbarton, NR14 8BU. Tel. Mulbarton 70609 Assistant Secretary: (Membership and Publications) Ms J. Wakefield Post Office Lane, Saxthorpe, NR11 7BL Assistant Secretary: (Minutes) P. W. Lambley Castle Museum, Norwich Excursion Secretary: Ms J. Robinson 5 Southern Reach, Mulbarton, NR14 8BU. -
The European Descendants of Ursus Etruscus C. Cuvier (Mammalia, Carnivora, Ursidae)
Boletin Geologico y Minero. Vol. 103-4. Ano 1992 (632-642) GEOLOGIA The European descendants of Ursus etruscus C. Cuvier (Mammalia, Carnivora, Ursidae). Por T. DE TORRES PEREZHIDALGO (') ABSTRACT This paper deals with a review of the Pleistocene Bears origin, evolution, and stratigraphical distribution. U. ruscinensis DEP. could be considered the common ancestor of all the European Pleistocene Bears, as the source of two evolutive lineages: one the more conservative, U. mecliterraneus F. MAJOR, and another the more evolved which starts with U. etruscus G. CUV. and gave origin o two evolutive trends: the today vanished speloid one (U. deningeri v. REICH, and U. spelaeus ROS.-HEIN) and the still living artoid one which is represented today in the true brown bear (U. arctos LIN.). U. minimus DEV.-BOUILL. does not constitute a link between U. ruscinensis and U. etruscus: it is a lateral branch, in the general evolutionary schedule, more evolved than U. etruscus. Recent findings of arctoid Ursidae remains in the Iberian Peninsula, ranging from Lower to the Middle (Upper) Pleis tocene, allowed us to think that the general migration southwards of an Asiatic Brown bear population during the Wurm glacial period beginning, superimposed on an authochtonous European Brown bear population (prearctoid): U. prearctos BOULE, which is the probable ancestor of the polar bear [U. maritimus PHIP.). Key words: Ursidae, Phylogeny, Stratigraphy, Pleistocene, Europe. R E S U M E N En este trabajo se revisan el origen, evolucion y distribucion estratigrafica de los osos del Pleistoceno. IS. ruscinensis DEP. puede considerarse como e! ancestro comun: de el derivaria un grupo muy conservador (U. -
I.—Geology, Chemical, Physical, and Stratighaphical. by Joseph
158 Reviews—Prof. Prestwich's Geology, Vol. II. II.—DIE GATTUNG Saurodon, Hays. By Prof. Dr. W. DAMES. Ibid. pp. 72—78. URING the investigation of the teeth of Titanichthys, Dr. Dames D was led to study the semi-barbed teeth from the European Chalk originally referred by Agassiz to the American genus and species Saurodon Leanus, Hays. The result is an interesting resume of the varied fate of the fossils in question at the hands of different palae- ontologists. Their resemblance to the teeth of the Trichiuridse is dis- cussed, and full references are given to the several descriptions and figures. It is unfortunate, however, that Hays' original memoir has not been consulted, nor yet the most important contributions of Leidy (Trans. Amer. Phil. Soc. vol. xi.) and E. T. Newton (Quart. Journ. Geol. Soc. vol. xxxiv.). The latter authors have shown that the European fossils are certainly not referable to Sanrocephalue • (of which Saurodon is a synonym), and those from the English Chalk are named Cimolichthys levesiensis. A. S. W. E, IE "V I IE "W S. I.—GEOLOGY, CHEMICAL, PHYSICAL, AND STKATIGHAPHICAL. By JOSEPH PRESTWICH, M.A., F.E.S., F.G.S. In Two Volumes. Vol. II. STBATIGEAPHICAL AND PHYSICAL. Eoyal 8vo. pp. xxviii. and 606, with Geological Map of Europe, and numerous Illustra- tions. (Oxford, at the Clarendon Press, 1888.) TF the number of geological papers published every year in J_ various parts of the globe were taken as a measure of the increase of our knowledge, our sentiments on the subject might fitly find utterance in the word " Prodigious ! " Nevertheless, while this great " talus heap of geological literature," as it has been rather irreverently termed, may at times produce a feeling of dismay and oppression, yet we may derive comfort from the thought that in due course of time the leading facts and the general results of this mass of information are tabulated and expounded in the larger Text-Books and Manuals. -
Proglacial to Subglacial Progressive Deformation And
Progressive proglacial to subglacial deformation and syntectonic sedimentation at the margins of the Mid-Pleistocene British Ice Sheet: evidence from north Norfolk, UK. Emrys Phillips 1*, Jonathan R. Lee 2,3, Helen Burke 2 1British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, Scotland, UK 2British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK 3Department of Geography, Royal Holloway, University of London, Egham, Surrey, TW20 0EX, UK. *corresponding author telephone: +44 (0)131-667-1000 fax: +44 (0)131-668-2683 e-mail: [email protected] Abstract Detailed analysis and interpretation of the stratigraphy and structures developed within polydeformed sediments exposed in the coastal section between West Runton and Sheringham (eastern England) has allowed the characterisation of the glacitectonic signature associated with the advance of a major Mid-Pleistocene (Anglian) ice sheet. The sequence of pre-glacial deposits and glacial sediments laid-down during earlier southerly directed ice advances (D1-D2) are deformed and disrupted by an ice advance from the west/southwest that marks a major change in ice flow dynamics in northern East Anglia. The simplest interpretation of this deformation event (D3) is in terms of a progressive proglacial to subglacial deformation model. Proglacial deformation occurred in-advance of the ice margin and was dominated by thrusting. Positive topographic features which developed above the propagating thrusts controlled sediment dispersal patterns within outwash sandur, leading to the formation of small sub-basins between these morainic ridges. The accretion of the wedge- shaped, proglacial thrust moraines to the main push moraine formed at the margin of the advancing glacier may have temporarily stalled forward motion of the ice.