Review of the West Dorset Coast Fossil Collecting Code of Conduct, and Recording Scheme 1999 to 2010
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Congregational Chapel's Graveyard
https://www.lymeregismuseum.co.uk/research Congregational Chapel Coombe Street, Lyme Regis The Search for a Graveyard Graham Davies, July 2021 The Dinosaurland Fossil Museum in Coombe Street, Lyme Regis, occupies a grade I listed building, a former Congregational (more recently, United Reform) Chapel which closed its doors to religious services in 1985. The Congregational (Independent) Church was formed in Lyme in 1662 following the ejection of the vicar, the Rev A Short, for non-compliance with the Act of Uniformity. He subsequently held services in his own house in Church Street and elsewhere, but was constantly hounded by the authorities. He died in 1697. In 1734 the Rev J Whitty became the new minister and under his guidance a chapel was built in Coombe Street in 1755. Dinosaurland, June 2013 In 2012, research team members, Diane Shaw, Derek Perrey and Graham Davies reviewed the Museum’s Congregational Chapel archives. They found a reference to a ‘curious little graveyard’ on the Lynch, belonging to the Congregational Chapel. In 1841, on behalf of the Chapel, a piece of ground, with two cottages on it (ref 192, 1841 tithe map), situated on the Lynch, was purchased by Mr Theophilus B Goddard from Mr Fowler, of the Hart Inn, at a price of £250. Extensive alterations were made to the cottages, and the part to be used as the burial ground was walled off from the rest. Mr Goddard hoped the Church would repay him his £250 through rents, burial fees and subscriptions. Through lack of subscriptions, Mr Goddard was set free by the Church in 1873 to dispose of the cottages as he saw fit, leaving them the graveyard. -
Excursion to Lyme Regis, Easter, 1906
320 EXCURSION TO LYME REGIS, EASTER, 1906. pebbles and bed NO.3 seemed, however, to be below their place. The succession seemed, however,to be as above, and, if that be so, the beds below bed I are probably Bagshot Beds. "The pit at the lower level has been already noticed in our Proceedings; cj. H. W. Monckton and R. S. Herries 'On some Bagshot Pebble Beds and Pebble Gravel,' Proc. Ceol. Assoc., vol. xi, p. 13, at p. 22. The pit has been worked farther back, and the clay is now in consequence thicker. Less of the under lying sand is exposed than it was in June, 1888. "The casts of shells which occur in this sand were not abundant, but several were found by members of the party on a small heap of sand at the bottom of the pit." Similarly disturbed strata were again observed in the excavation for the new reservoir close by. A few minutes were then profitably spent in examining Fryerning Church, and its carved Twelfth Century font, etc. At the Spread Eagle a welcome tea awaited the party, which, after thanking the Director, returned by the 7.55 p.m. train to London. REFERENCES. Geological Survey Map, Sheet 1 (Drift). 1889. WHITAKER, W.-I< Geology of London," vol. i, pp. 259, 266. &c. 1889. MONCKTON, H. W., and HERRIES, R. S.-I< On Some Bagshot Pebble Beds and Pebble Gravel," Proc, Geo], Assoc., vol, xi, p. 13. 1904. SALTER, A. E.-" On the Superficial Deposits of Central and Southern England," Proc. Ceo!. Assoc., vol. -
Springs and Seepages of Wessex Lyme Regis Invertebrate Survey
Springs and Seepages of Wessex Lyme Regis Invertebrate Survey Andy Godfrey March 2012 1 Andy Godfrey Invertebrate Consultant 90 Bence Lane Darton Barnsley South Yorkshire S75 5DA Tel: 01226 384022 Mobile: 07502 364511 Email: [email protected] 2 Contents Summary ........................................................................................................................................4 1. Introduction .............................................................................................................................5 2. Location ..................................................................................................................................5 3. Methodology............................................................................................................................5 3.1. Aquatic survey method ....................................................................................................5 3.2. Terrestrial survey method ................................................................................................5 3.3. Recording of environmental variables..............................................................................6 3.4. Identification ....................................................................................................................6 3.5. Assessment .....................................................................................................................6 4. Selection of survey sites..........................................................................................................6 -
A Mysterious Giant Ichthyosaur from the Lowermost Jurassic of Wales
A mysterious giant ichthyosaur from the lowermost Jurassic of Wales JEREMY E. MARTIN, PEGGY VINCENT, GUILLAUME SUAN, TOM SHARPE, PETER HODGES, MATT WILLIAMS, CINDY HOWELLS, and VALENTIN FISCHER Ichthyosaurs rapidly diversified and colonised a wide range vians may challenge our understanding of their evolutionary of ecological niches during the Early and Middle Triassic history. period, but experienced a major decline in diversity near the Here we describe a radius of exceptional size, collected at end of the Triassic. Timing and causes of this demise and the Penarth on the coast of south Wales near Cardiff, UK. This subsequent rapid radiation of the diverse, but less disparate, specimen is comparable in morphology and size to the radius parvipelvian ichthyosaurs are still unknown, notably be- of shastasaurids, and it is likely that it comes from a strati- cause of inadequate sampling in strata of latest Triassic age. graphic horizon considerably younger than the last definite Here, we describe an exceptionally large radius from Lower occurrence of this family, the middle Norian (Motani 2005), Jurassic deposits at Penarth near Cardiff, south Wales (UK) although remains attributable to shastasaurid-like forms from the morphology of which places it within the giant Triassic the Rhaetian of France were mentioned by Bardet et al. (1999) shastasaurids. A tentative total body size estimate, based on and very recently by Fischer et al. (2014). a regression analysis of various complete ichthyosaur skele- Institutional abbreviations.—BRLSI, Bath Royal Literary tons, yields a value of 12–15 m. The specimen is substantially and Scientific Institution, Bath, UK; NHM, Natural History younger than any previously reported last known occur- Museum, London, UK; NMW, National Museum of Wales, rences of shastasaurids and implies a Lazarus range in the Cardiff, UK; SMNS, Staatliches Museum für Naturkunde, lowermost Jurassic for this ichthyosaur morphotype. -
St Michael's House, 7 Pound Street
St Michael’s House, 7 Pound Street Graham Davies and Richard Wells May 2020 The house is set back from the roadside and adjacent properties on the Pound Street hill in Lyme Regis. Of Regency origin, the house underwent a Victorian makeover followed by further changes in the 20th/21st centuries. Initially a private house for almost a hundred years it became an hotel for most of the 20th century before being converted into flats in 2004. The Rev Michael Babbs bought the house in 1818. Did he name the house Mount Nebo or was it the earlier owner and/or builder? 2018 The Rev Babbs (1743-1831) came from London to Lyme Regis as a curate in 1792. He was accompanied by his daughters, Elizabeth and Mary Ann, and their step-mother, his second wife Mary. He rented the recently built house, Belle Vue (today’s Kersbrook), in Pound Road from Samuel Coade and was tenant there for the next 30 years. He served under four different vicars and seemed content to act as a perpetual curate at the Parish Church of St Michael the Archangel. He was a gentleman of additional means. The parish records show him to be a very busy clergyman, well known, not only in society, but to all classes of people in the community. He was described by his sexton, John Upjohn, as ‘a nice gentleman who wrote like copperplate’. It is not known when the house was built, by whom, and from whom it was purchased in 1818. Annotated survey What is known: 1. -
Cause and Consequence of Recurrent Early Jurassic Anoxia Following The
[Palaeontology, Vol. 56, Part 4, 2013, pp. 685–709] MICROBES, MUD AND METHANE: CAUSE AND CONSEQUENCE OF RECURRENT EARLY JURASSIC ANOXIA FOLLOWING THE END-TRIASSIC MASS EXTINCTION by BAS VAN DE SCHOOTBRUGGE1*, AVIV BACHAN2, GUILLAUME SUAN3, SYLVAIN RICHOZ4 and JONATHAN L. PAYNE2 1Palaeo-environmental Dynamics Group, Institute of Geosciences, Goethe University Frankfurt, Altenhofer€ Allee 1, 60438, Frankfurt am Main, Germany; email: [email protected] 2Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Stanford, CA 94305, USA; emails: [email protected], [email protected] 3UMR, CNRS 5276, LGLTPE, Universite Lyon 1, F-69622, Villeurbanne, France; email: [email protected] 4Academy of Sciences, University of Graz, Heinrichstraße 26, 8020, Graz, Austria; email: [email protected] *Corresponding author. Typescript received 19 January 2012; accepted in revised form 23 January 2013 Abstract: The end-Triassic mass extinction (c. 201.6 Ma) Toarcian events are marked by important changes in phyto- was one of the five largest mass-extinction events in the his- plankton assemblages from chromophyte- to chlorophyte- tory of animal life. It was also associated with a dramatic, dominated assemblages within the European Epicontinental long-lasting change in sedimentation style along the margins Seaway. Phytoplankton changes occurred in association with of the Tethys Ocean, from generally organic-matter-poor the establishment of photic-zone euxinia, driven by a general sediments during the -
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”. -
A Revision of the Classification of the Plesiosauria with a Synopsis of the Stratigraphical and Geographical Distribution Of
LUNDS UNIVERSITETS ARSSKRIFT. N. F. Avd. 2. Bd 59. Nr l. KUNGL. FYSIOGRAFISKA SÅLLSKAPETS HANDLINGAR, N. F. Bd 74. Nr 1. A REVISION OF THE CLASSIFICATION OF THE PLESIOSAURIA WITH A SYNOPSIS OF THE STRATIGRAPHICAL AND GEOGRAPHICAL DISTRIBUTION OF THE GROUP BY PER OVE PERSSON LUND C. W. K. GLEER UP Read before the Royal Physiographic Society, February 13, 1963. LUND HÅKAN OHLSSONS BOKTRYCKERI l 9 6 3 l. Introduction The sub-order Plesiosauria is one of the best known of the Mesozoic Reptile groups, but, as emphasized by KuHN (1961, p. 75) and other authors, its classification is still not satisfactory, and needs a thorough revision. The present paper is an attempt at such a revision, and includes also a tabular synopsis of the stratigraphical and geo graphical distribution of the group. Some of the species are discussed in the text (pp. 17-22). The synopsis is completed with seven maps (figs. 2-8, pp. 10-16), a selective synonym list (pp. 41-42), and a list of rejected species (pp. 42-43). Some forms which have been erroneously referred to the Plesiosauria are also briefly mentioned ("Non-Plesiosaurians", p. 43). - The numerals in braekets after the generic and specific names in the text refer to the tabular synopsis, in which the different forms are numbered in successional order. The author has exaroined all material available from Sweden, Australia and Spitzbergen (PERSSON 1954, 1959, 1960, 1962, 1962a); the major part of the material from the British Isles, France, Belgium and Luxembourg; some of the German spec imens; certain specimens from New Zealand, now in the British Museum (see LYDEK KER 1889, pp. -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
'Cenoceras Islands' in the Blue Lias Formation (Lower Jurassic)
FOSSIL IMPRINT • vol. 75 • 2019 • no. 1 • pp. 108–119 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) ‘CENOCERAS ISLANDS’ IN THE BLUE LIAS FORMATION (LOWER JURASSIC) OF WEST SOMERSET, UK: NAUTILID DOMINANCE AND INFLUENCE ON BENTHIC FAUNAS DAVID H. EVANS1, *, ANDY H. KING2 1 Stratigrapher, Natural England, Rivers House, East Quay, Bridgwater, Somerset, TA6 4YS UK; e-mail: [email protected]. 2 Director & Principal Geologist, Geckoella Ltd, Suite 323, 7 Bridge Street, Taunton, Somerset, TA1 1TG UK; e-mail: [email protected]. * corresponding author Evans, D. H., King, A. H. (2019): ‘Cenoceras islands’ in the Blue Lias Formation (Lower Jurassic) of West Somerset, UK: nautilid dominance and influence on benthic faunas. – Fossil Imprint, 75(1): 108–119, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on-line). Abstract: Substantial numbers of the nautilid Cenoceras occur in a stratigraphically limited horizon within the upper part of the Lower Jurassic (Sinemurian Stage) Blue Lias Formation at Watchet on the West Somerset Coast (United Kingdom). Individual nautilid conchs are associated with clusters of encrusting organisms (sclerobionts) forming ‘islands’ that may have been raised slightly above the surrounding substrate. Despite the relatively large numbers of nautilid conchs involved, detailed investigation of their preservation suggests that their accumulation reflects a reduction in sedimentation rates rather than an influx of empty conches or moribund animals. Throughout those horizons in which nautilids are present in relative abundance, the remains of ammonites are subordinate or rare. The reason for this unclear, and preferential dissolution of ammonite conchs during their burial does seem to provide a satisfactory solution to the problem. -
Geology of the Shepton Mallet Area (Somerset)
Geology of the Shepton Mallet area (Somerset) Integrated Geological Surveys (South) Internal Report IR/03/94 BRITISH GEOLOGICAL SURVEY INTERNAL REPORT IR/03/00 Geology of the Shepton Mallet area (Somerset) C R Bristow and D T Donovan Contributor H C Ivimey-Cook (Jurassic biostratigraphy) The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Ordnance Survey licence number GD 272191/1999 Key words Somerset, Jurassic. Subject index Bibliographical reference BRISTOW, C R and DONOVAN, D T. 2003. Geology of the Shepton Mallet area (Somerset). British Geological Survey Internal Report, IR/03/00. 52pp. © NERC 2003 Keyworth, Nottingham British Geological Survey 2003 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation. Shop online at: www.thebgs.co.uk The Survey publishes an annual catalogue of its maps and other publications; this catalogue is available from any of the BGS Sales Murchison House, West Mains Road, Edinburgh EH9 3LA Desks. 0131-667 1000 Fax 0131-668 2683 The British Geological Survey carries out the geological survey of e-mail: [email protected] Great Britain and Northern Ireland (the latter as an agency service for the government of Northern Ireland), and of the London Information Office at the Natural History Museum surrounding continental shelf, as well as its basic research (Earth Galleries), Exhibition Road, South Kensington, London projects. -
Autumn 2009 Free Issue No
Autumn 2009 Free Issue no. 7 no. Issue A mini version of Tower Bridge and a brontosaurus Photo-montage by Tim Heap straddling the water were two of the more tongue-in- be rustic, constructed of timber, appreciably wider with cheek suggestions put to the design team visiting passing places, extended so as to avoid the mud, and to Charmouth on September 10th. Representatives from have an arched elevation similar to the current design. Dorset Engineering Consultancy, the Coastal Ranger team, and the artists, Sans facon, met with District and Parish According to Sans facon, the artists, they do not start from Councillors, adjacent businesses and over 40 locals eager to a preconceived aesthetic: their approach consists of share their thoughts and concerns regarding the understanding a context, from its physical and social replacement footbridge over the Char river. location to the uses and functions of the place. Rather than parachute in ideas or recipes from somewhere else, they People spoke of the natural beauty of the landscape, the aim to utilise and integrate their response ideas within the importance of the geology of the area and the need for a specific quality of the location. The Velator viewing platform new structure that will sit comfortably within its rural they created in Devon (www.sansfacon.co.uk/vel/vel.html) surroundings. The general consensus was that the bridge illustrates this by drawing inspiration from and responding directly to the site and its essence. They will be working in close collaboration with the engineers and the rest of the ‘Palaeontology in Charmouth’ team to develop a joint design.