Belemnite Palaeo-Proxies and Dating of Mesozoic Carbonates
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Jurassic Coast Fossil Acquisition Strategy Consultation Report
Jurassic Coast World Heritage Site Fossil acquisition strategy for the Jurassic Coast- Consultation Document A study to identify ways to safeguard important scientific fossils from the Dorset and East Devon Coast World Heritage Site – prepared by Weightman Associates and Hidden Horizons on behalf of the Jurassic Coast Team, Dorset County Council p Jurassic Coast World Heritage Site Fossil acquisition strategy for the Jurassic Coast CONTENTS 1. INTRODUCTION…………………………………………………………………………………2 2. BACKGROUND…………………………………………………………………………………..2 3. SPECIFIC ISSUES………………………………………..……………………………………….5 4. CONSULTATION WITH STAKEHOLDERS………………………………………………5 5. DISCUSSION……………………………………………………………………………………..11 6. CONCLUSIONS…………………………..……………………………………………………..14 7. ACKNOWLEDGEMENTS…………………………………………………………………....14 8. APPENDIX..……………………………………………………………………………………...14 1 JURASSIC COAST FOSSIL ACQUISITION STRATEGY 1. Introduction The aim of this project is to identify ways to safeguard important scientific fossils from the Dorset and East Devon Coast World Heritage Site. The identification of placements in accredited museums would enable intellectual access for scientific study and education. Two consulting companies Weightman Associates and Hidden Horizons have been commissioned to undertake this Project. Weightman Associates is a partnership of Gill Weightman and Alan Weightman; they have been in partnership for twenty years working on museum and geology projects. Hidden Horizons Ltd is a museum and heritage consultancy formed in 2013 by Will Watts. When UNESCO granted World Heritage status to the Dorset and East Devon Coast in 2001 it recognised the importance of the Site’s geology and geomorphology. The Jurassic Coast Management Plan 2014-2019 has as one of its aims to “To Conserve and enhance the Site and its setting for science, education and public enjoyment” and the Plan states that a critical success factor is “An increase in the number of scientifically important fossils found along the site that are acquired by or loaned back to local accredited museums”. -
191010 Appendix A, Item 18. PDF 2 MB
Appendix A Consultation on Proposed Dog- Related Public Spaces Protection Order There are a number of existing dog-related Public Spaces Protection Orders (‘PSPOs’) across the Dorset Council area. These were introduced by the former District and Borough Councils which have now become part of the new unitary Dorset Council. Some of these Orders will soon naturally expire and the council is taking the opportunity to consolidate them into one. The intention is that the new Order will provide clarity and consistency across the area for dog owners and non-owners alike about dog controls on public open spaces. We are required to consult with the public and other stakeholders on the content of new or revised PSPOs. This may see changes to the previous Orders dependent upon the views expressed. Councillors will make the final decision on the controls to be included in the new Order, having regard to the feedback received during the consultation. The views of residents, visitors and businesses are therefore very important and a period of consultation will run for 12 weeks finishing at 4.30pm on Friday ADD DATE. To have your say, please complete this short survey, it should take about 15 minutes or less for the 34 questions related to the proposal and a further 6 ‘about you’. Results will be published on the consultation tracker after the closing date. Information on the current dog-related Public Spaces Protection Orders is available to view at: East Dorset: https://www.dorsetcouncil.gov.uk/environmental-health/dog-warden-service/dog-control- -
Seatown Regeneration Project
‘Saving Seatown for the Future’: Seatown Regeneration Project Strengths Weaknesses Close to A35 main Trunk Road & easy reach of Narrow & tortuous vehicular access from A 35; public transport service leads to congestion at peak times, with few and no Accommodation available at Caravan Park at proper passing places Seatown and other facilities in Chideock Access used by cars and towed touring caravans Local Shop in caravan site which adds to difficulties. Attractive coastal location No coach access or parking which restricts visitor Access to the Beach and Jurassic Coast World market Heritage Restricted access and turning at Seatown and Area of Outstanding Natural Beauty conflict with pedestrians & residents Geology & Fossil collecting Unauthorised parking on double yellow lines in Main access point for Golden Cap [Iconic summer causing congestion and blocking of road symbol of WHS & Highest Point of South Coast] for service and emergency vehicles Access to SW Coast Path to both directions & No enforcement of parking restrictions National Trust land; attractive landscape & Car Park has fixed ‘All Day’ fee [£4] nature areas No short stay parking so some visitors put Visitor facilities Pub, Car Park, ice cream kiosk & off/frustrated & insufficient parking at peak times toilets close to beach Car park liable to flooding Good quality pub Car park closes at sunset and is not open until Safe off road parking 9:30 AM, controlled by covenant. Outside these Clean beach & water times; essentially no parking at Seatown after No night time light pollution on beach sunset in summer. Area protected from development; comparatively Access to beach is unclear and difficult in places; unspoilt no clear and effective signage; access over rock Popular fishing location armour dangerous Much used destination for all levels of education Facilities for disabled people are limited; notably Bridleway for pedestrians links Seatown with parking spaces & no safe access to beach Chideock. -
Malcolm T. Sanders, Jérémie Bardin, Mohammed Benzaggagh & Fabrizio Cecca
Early Toarcian (Jurassic) belemnites from northeastern Gondwana (South Riffian ridges, Morocco) Malcolm T. Sanders, Jérémie Bardin, Mohammed Benzaggagh & Fabrizio Cecca Paläontologische Zeitschrift Scientific Contributions to Palaeontology ISSN 0031-0220 Paläontol Z DOI 10.1007/s12542-013-0214-0 1 23 Your article is protected by copyright and all rights are held exclusively by Springer- Verlag Berlin Heidelberg. This e-offprint is for personal use only and shall not be self- archived in electronic repositories. If you wish to self-archive your article, please use the accepted manuscript version for posting on your own website. You may further deposit the accepted manuscript version in any repository, provided it is only made publicly available 12 months after official publication or later and provided acknowledgement is given to the original source of publication and a link is inserted to the published article on Springer's website. The link must be accompanied by the following text: "The final publication is available at link.springer.com”. 1 23 Author's personal copy Pala¨ontol Z DOI 10.1007/s12542-013-0214-0 RESEARCH PAPER Early Toarcian (Jurassic) belemnites from northeastern Gondwana (South Riffian ridges, Morocco) Malcolm T. Sanders • Je´re´mie Bardin • Mohammed Benzaggagh • Fabrizio Cecca Received: 3 May 2013 / Accepted: 30 October 2013 Ó Springer-Verlag Berlin Heidelberg 2013 Abstract A belemnite fauna collected in the lowermost post-date the earliest Toarcian Polymorphum—Tenuicost- Toarcian succession that crops out near Moulay Idriss atum Chronozone. However, records of Early Jurassic be- (northern Morocco) is studied in this article. This is the first lemnites are still too sparse to recognize the establishment palaeontological study of Early Toarcian belemnites from of provincialism and the timing of its onset. -
Chesil Beach and Adjacent Area: Outline of Existing Data And
INTERNAL DOCUMENT 94 GHESIL BEA.CH AHD ADJACENT AEEA- OUTLINE OF EXISTING DATA AND SUGGESTIONS FOR FUTURE RESEARCH Report to the Dorset County Council and ¥essex Water Authority [This document should not be cited in a published bibliography, and is supplied for the use of the recipient only]. INSTITUTE OF \ OCEAN a GRAPHIC SCIENCES INSTITUTE OF OCEANOGRAPHIC SCIENCES Wormley, Godalming, Surrey, GU8 BUB. (042-879-4141) (Director: Dr. A. 8. Laughton) Bidston Observatory, Crossway, Birkenhead, Taunton, Merseyside, L43 7RA. Somerset, TA1 2DW. (051-652-2396) (0823-86211) (Assistant Director: Dr. D. E. Cartwright) (Assistant Director: M.J. Tucker) OUTLIETE OP EXISTING MTA AND SUGGESTIONS FOR FUTURE RESEARCH Report to the Dorset CoTxnty Council and ¥essex Water Authority P GARR Internal Document No 94 Institute of Oceanographic Sciences Crossway Taunton Somerset June 198O CONTENTS Page SUMMARY 1 1. INTRODUCTION " 2 2. EXISTING PUBLISHED DATA 2 3. OTHER SOURCES OF DATA 4 3*1 Offshore 4 3.2 Wave data; computed and observed 5 3.3 Beach Sections 6 3.4 Gravel extraction 7 3.5 Tracer experiments and littoral drift 8 3.6 Additional sources 8 4. VALIDITY OF DATA 9 5. THE BEACH AS A FINITE RESOURCE 11 5.1 Introduction 11 5.2 Mechanism of replacement 11 5.3 Conclusions 12 5.4 Further research 12 6. IMPLICATIONS OF DATA ON SEA. DEFENCES, CO&ST PROTECTION 14 WORK AM) GRAVEL EXTRACTION 7. CONCLUSIONS 16 ACKNOWLEDGMENTS 19 REFERENCES TABLES APPENDICES FIGURES TABLES 1. Nature Conservancy beach sections availability* 1965-68 2. Dorset County Council " ; 1955—59 3. " " " " .. " " ; 1974-78 4. -
Dorset and East Devon Coast for Inclusion in the World Heritage List
Nomination of the Dorset and East Devon Coast for inclusion in the World Heritage List © Dorset County Council 2000 Dorset County Council, Devon County Council and the Dorset Coast Forum June 2000 Published by Dorset County Council on behalf of Dorset County Council, Devon County Council and the Dorset Coast Forum. Publication of this nomination has been supported by English Nature and the Countryside Agency, and has been advised by the Joint Nature Conservation Committee and the British Geological Survey. Maps reproduced from Ordnance Survey maps with the permission of the Controller of HMSO. © Crown Copyright. All rights reserved. Licence Number: LA 076 570. Maps and diagrams reproduced/derived from British Geological Survey material with the permission of the British Geological Survey. © NERC. All rights reserved. Permit Number: IPR/4-2. Design and production by Sillson Communications +44 (0)1929 552233. Cover: Duria antiquior (A more ancient Dorset) by Henry De la Beche, c. 1830. The first published reconstruction of a past environment, based on the Lower Jurassic rocks and fossils of the Dorset and East Devon Coast. © Dorset County Council 2000 In April 1999 the Government announced that the Dorset and East Devon Coast would be one of the twenty-five cultural and natural sites to be included on the United Kingdom’s new Tentative List of sites for future nomination for World Heritage status. Eighteen sites from the United Kingdom and its Overseas Territories have already been inscribed on the World Heritage List, although only two other natural sites within the UK, St Kilda and the Giant’s Causeway, have been granted this status to date. -
Lulworth Cove Circular Via Tyneham and Durdle Door Lulworth Cove Circular – Wool Station Start and Finish
Lulworth Cove Circular via Tyneham and Durdle Door Lulworth Cove Circular – Wool Station Start and Finish 1st walk check 2nd walk check 3rd walk check 1st walk check 2nd walk check 3rd walk check 24th July 2019 Current status Document last updated Tuesday, 27th August 2019 This document and information herein are copyrighted to Saturday Walkers’ Club. If you are interested in printing or displaying any of this material, Saturday Walkers’ Club grants permission to use, copy, and distribute this document delivered from this World Wide Web server with the following conditions: • The document will not be edited or abridged, and the material will be produced exactly as it appears. Modification of the material or use of it for any other purpose is a violation of our copyright and other proprietary rights. • Reproduction of this document is for free distribution and will not be sold. • This permission is granted for a one-time distribution. • All copies, links, or pages of the documents must carry the following copyright notice and this permission notice: Saturday Walkers’ Club, Copyright © 2008-2019, used with permission. All rights reserved. www.walkingclub.org.uk This walk has been checked as noted above, however the publisher cannot accept responsibility for any problems encountered by readers. Lulworth Cove Circular via Tyneham and Durdle Door Start & Finish: Lulworth Cove bus stop Lulworth Cove bus stop, map reference SY 822 800, is 178 km south west of Charing Cross, 16m above sea level and in Dorset. Length: 22.2 km (13.8 mi). Cumulative ascent/descent: 974m. For a shorter walk and an Alternative Start or Finish at Wool Station, see below Walk options. -
An Inventory of Belemnites Documented in Six Us National Parks in Alaska
Lucas, S. G., Hunt, A. P. & Lichtig, A. J., 2021, Fossil Record 7. New Mexico Museum of Natural History and Science Bulletin 82. 357 AN INVENTORY OF BELEMNITES DOCUMENTED IN SIX US NATIONAL PARKS IN ALASKA CYNTHIA D. SCHRAER1, DAVID J. SCHRAER2, JUSTIN S. TWEET3, ROBERT B. BLODGETT4, and VINCENT L. SANTUCCI5 15001 Country Club Lane, Anchorage AK 99516; -email: [email protected]; 25001 Country Club Lane, Anchorage AK 99516; -email: [email protected]; 3National Park Service, Geologic Resources Division, 1201 Eye Street, Washington, D.C. 20005; -email: justin_tweet@ nps.gov; 42821 Kingfisher Drive, Anchorage, AK 99502; -email: [email protected];5 National Park Service, Geologic Resources Division, 1849 “C” Street, Washington, D.C. 20240; -email: [email protected] Abstract—Belemnites (order Belemnitida) are an extinct group of coleoid cephalopods, known from the Jurassic and Cretaceous periods. We compiled detailed information on 252 occurrences of belemnites in six National Park Service (NPS) areas in Alaska. This information was based on published literature and maps, unpublished U.S. Geological Survey internal fossil reports (“Examination and Report on Referred Fossils” or E&Rs), the U.S. Geological Survey Mesozoic locality register, the Alaska Paleontological Database, the NPS Paleontology Archives and our own records of belemnites found in museum collections. Few specimens have been identified and many consist of fragments. However, even these suboptimal specimens provide evidence that belemnites are present in given formations and provide direction for future research. Two especially interesting avenues for research concern the time range of belemnites in Alaska. Belemnites are known to have originated in what is now Europe in the Early Jurassic Hettangian and to have a well-documented world-wide distribution in the Early Jurassic Toarcian. -
Field Trip to Osmington Mills, Dorset, March 15Th 2009
Do you like hands-on geology? Try Earthlearningidea www.earthlearningidea.com. We are publishing one new activity every month this year; last year we published one new activity every week so there are lots of innovative hands-on activities - all free to download. Please send us your ideas, comments and suggestions via the blog http://earthlearningidea.blogspot.com or by email [email protected] Figure 6 : formations found near Chapel Stile in the Lake District FIELD TRIP TO also a tuff, this time of the Borrowdale Volcanic OSMINGTON MILLS Series, and the balls seem to be very similar to those of Moel Hebog. Further on, as we ascended DORSET the steep path up the north-east side of Pavey Ark, which is the crag overlooking Stickle Tarn, I came MARCH 15th 2009 across a few larger individual ones, one of which is shown in figure 7 with my son’s boot for size. Elizabeth Devon On a beautiful, very hot day in March, lots of keen geologists gathered in Smugglers Inn car park in Osmington Mills, Dorset. This was a joint field trip with the Dorset branch of the Geologists’ Association and was led by local expert, Alan Holiday. We planned to walk east along the coast from the Smugglers Inn as far as Ringstead. In this section, we were looking at the Upper Jurassic Corallian succession, Diagram 1 , from the Nothe Clay upwards. These rocks date at about 145 million years ago and were deposited Figure 7: A few individual examples on the north-east when Britain was in Mediterranean latitudes, side of Pavey Ark about 35°N. -
Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) 163-211 ©Geol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 1993 Band/Volume: 136 Autor(en)/Author(s): Meister Christian, Böhm Florian Artikel/Article: Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) 163-211 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Jb. Geol. B.-A. ISSN 0016-7800 Band 136 S.163-211 Wien, Juli 1993 Austroalpine Liassic Ammonites from the Adnet Formation (Northern Calcareous Alps) By CHRISTIAN MEISTER & FLORIAN BÖHM *) With 14 Text-Figures and 9 Plates Oslerreich Salzburg Oberöslerreich Nördliche Kalkalpen Lias Ammoniten Oslerreichische Karle 1. 50.000 Biostratigraphie BI/1l1er94, 95, 96,126 Palaeogeographie Contents Zusammenfassung 163 Abstract. .. 164 Resume 164 1. Introduction 164 2. Geographical and Geological Framework 164 3. Lithological Description and Qualitative/Quantitative Ammonite Distributions 165 3.1. Schmiedwirt Quarry 165 3.2. Breitenberg Quarry 166 3.3. Rotkogel Outcrop 166 3.4. Rötelstein Outcrop 168 4. Systematic Palaeontology 169 PhylioceratinaARKELL 1950 171 LytoceratinaHYATT1889 174 Ammonitina HYATT 1889 175 5. Biostratigraphical Framework 184 5.1. Sinemurian 184 5.1.1. Early Sinemurian 184 5.1.2. Late Sinemurian 184 5.2. Pliensbachian 184 5.2.1. Early Pliensbachian (Carixian) 184 5.2.2. Late Pliensbachian (Domerian) 186 5.3. Toarcian 186 6. Faunal Composition and Palaeogeographical Remarks 189 7. Conclusion 190 Acknowledgements 190 References 208 Oberostalpine Liasammoniten aus der Adnetformation (Nördlichen Kalkalpen) Zusammenfassung Das Oberostalpin spielt eine Schlüsselrolle für das Verständnis der Verteilungsmuster der jurassischen Ammonitenfaunen und für die Fixierung genauer biostratigraphischer Korrelationen zwischen Tethyaler und Euroborealer Faunenprovinz. -
Belemnite Extinction and the Origin of Modern Cephalopods 35 M.Y. Prior to the Cretaceous−Paleogene Event
Belemnite extinction and the origin of modern cephalopods 35 m.y. prior to the Cretaceous−Paleogene event Yasuhiro Iba1,2*, Jörg Mutterlose1, Kazushige Tanabe3, Shin-ichi Sano4, Akihiro Misaki5, and Kazunobu Terabe6 1Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, 44801, Germany 2Department of Geology and Paleontology, National Museum of Nature and Science, Tokyo 169-0073, Japan 3Department of Earth and Planetary Science, University of Tokyo, Tokyo 113-0033, Japan 4Fukui Prefectural Dinosaur Museum, Fukui 911-8601, Japan 5Kitakyushu Museum of Natural History and Human History, Fukuoka 805-0071, Japan 6Arabian Oil Company, Ltd., Tokyo 140-0002, Japan ABSTRACT determination of the strata studied is based on Belemnites, a very successful group of Mesozoic cephalopods, fl ourished in Cretaceous diagnostic ammonite species. Evaluations of oceans until the Cretaceous−Paleogene event, when they became globally extinct. Following museum collections (Mikasa City Museum, and this event the modern types of cephalopods (squids, cuttlefi sh, octopus) radiated in the Ceno- Kyushu University, Japan; California Academy zoic in all oceans. In the North Pacifi c, however, a turnover from belemnites to the modern of Science, USA) have also been done. Details types of cephalopods about 35 m.y. before the Cretaceous−Paleogene event documents a more of the localities, horizons, and the precise strati- complex evolutionary history of cephalopods than previously thought. Here we show that the graphic ages of Albian belemnites are shown in modern types of cephalopods originated and prospered throughout the Late Cretaceous in Table DR1 in the Data Repository.1 the North Pacifi c. The mid-Cretaceous cephalopod turnover was caused by cooling and the closure of the Bering Strait, which led to a subsequent faunal isolation of this area. -
Deep Sea Drilling Project Initial Reports Volume 27
46. LEG 27 CEPHALOPODA Graeme R. Stevens, New Zealand Geological Survey, Department of Scientific and Industrial Research, Lower Hutt, New Zealand COLEOIDEA frequently develop lines of weakness and hence often BELEMNITIDA break at about the position of the protoconch (Stevens, Family Belemnopsidae 1965b), it is possible that very little of the anterior part cf. Parahibolites, sp. indet. of the stem region has been lost. There is a strong (Plate 1, Figures 1-3) possibility, therefore, that if specimen WM 11629 was a Dimitobelus, the cross-sections would show some sign of Material: One guard (Plate 1, Figure 1). Sample 263- the presence of ventrolateral grooves, or at least the 26-2, 108-110 cm. Cuvier Abyssal Plain, 23°20'S, strongly developed lateral lines that are their con- 1 JO°58'E. Water depth 5065 meters. Sample from 698.5 tinuations posteriorly (Stevens, 1965b, figs. 26 and 29). to 708 meters below the sea floor. Specimen deposited in The cross-sections of specimen WM 11629—circular the World Mollusca Collection, New Zealand in both apical and stem regions—and centrally placed Geological Survey, Lower Hutt, New Zealand. apical line, together tend to deny identification with Specimen WM 11629. Dimitobelidae, as both Peratobelus and Dimitobelus Dimensions: Length of guard: 36 mm; diameter of usually show depressed stem and apical cross-sections guard at anterior end: 7 mm. and eccentric apical line (although the Maestrichtian D. Description: Guard moderately elongate. Length hectori Stevens has circular stem cross-sections and about six times maximum diameter. Outline central apical line). It is concluded, therefore, that the symmetrical and nonhastate.