THE LIFE and TIMES of HASTINGS ELWIN OR ELWYN (1777–1852) and HIS CRITICAL ROLE in FOUNDING the BATH LITERARY and SCIENTIFIC INSTITUTION in 1823 by H.S

Total Page:16

File Type:pdf, Size:1020Kb

THE LIFE and TIMES of HASTINGS ELWIN OR ELWYN (1777–1852) and HIS CRITICAL ROLE in FOUNDING the BATH LITERARY and SCIENTIFIC INSTITUTION in 1823 by H.S THE GEOLOGICAL CURATOR VOLUME 8, NO. 4 CONTENTS THE LIFE AND TIMES OF HASTINGS ELWIN OR ELWYN (1777–1852) AND HIS CRITICAL ROLE IN FOUNDING THE BATH LITERARY AND SCIENTIFIC INSTITUTION IN 1823 by H.S. Torrens.......................................................................................................................................................141 THE COLLECTIONS OF GEORGE GARDNER (1810–1849) FROM THE SANTANA FORMATION (CRETACEOUS) OF NORTHEAST BRAZIL by J.R. Nudds and J. Washington Evans...................................................................................................................169 COMMENT AND RESPONSE ON ‘BIOEROSION, PREPARATION AND CURATION’ Comment by S.K. Donovan, C. Hensley and D.N. Lewis..........................................................................................177 Response by J.D. Radley.........................................................................................................................................179 THE JURASSIC OF WARWICKSHIRE: PERSPECTIVES ON COLLECTING by J.D. Radley.........................................................................................................................................................181 LOST & FOUND.........................................................................................................................................................189 BOOK REVIEW.........................................................................................................................................................190 GEOLOGICAL CURATORS’ GROUP - 30TH ANNUAL GENERAL MEETING.................................................191 ERRATA: STATE & STATUS 2001 REPORT THE GEOLOGICAL CURATOR 8(3) [2005]..................................199 THE GEOLOGICAL CURATORS’ GROUP 2006 MEMBERSHIP APPLICATION/RENEWAL FORM...........201 GEOLOGICAL CURATORS’ GROUP - December 2005 -139- -140- THE LIFE AND TIMES OF HASTINGS ELWIN OR ELWYN (1777– 1852) AND HIS CRITICAL ROLE IN FOUNDING THE BATH LITERARY AND SCIENTIFIC INSTITUTION IN 1823 by Hugh S. Torrens Torrens, H.S. 2005. The life and times of Hastings Elwin or Elwyn (1777–1852) and his critical role in founding the Bath Literary and Scientific Institution in 1823. The Geological Curator 8(4): 141–168. H.S. Torrens, Lower Mill Cottage, Furnace Lane, Madeley, Crewe, Cheshire, CW3 9EU, U.K. Revised version received 10th August 2005. For Stella Whyberd Pierce—in gratitude. 1753. It was that same museum which purchased Smith’s rock and fossil collections between 1815 and “It is to be wished, if for nothing else but the 1818. Smith’s realisation of the importance of using honour of Bath, that so valuable a gift [as this fossils to identify those strata which contained them Institution], transmitted from a generation almost led to museums all round the world filling with such passed away, should not perish in the hands of a collections. That same date was also chosen to “call race less alive to its value and importance” (Hunter attention to the BRLSI’s wonderful collections” 1853, 72). (Catchpole 2004, 47), since no museum had more filled up with fossils and rocks than their’s in Bath. Introduction The City of Bath was enrolled, in 1987, as one of the The Bath Literary and Scientific Institution, United Kingdom’s first World Heritage sites. It was (hereafter—BLSI, or from 1837, when it acquired the ninth here, listed by UNESCO (2003). However further royal patronage—BRLSI), has an important, such a culturally important city now has some strange if complex, history. As one direct result of its ‘cultural legacies’. There was particularly fierce foundation, the claim was first made there, by Rev. opposition from Bath’s rate-payers, where rates were, Joseph Hunter (1783–1861), that “Bath may justly be and still are, famously low, to the Public Libraries regarded as the cradle of English geology” (Hunter Act of 1850. This was rejected in Bath four times and 1827a, 14). The initiation of the study of Bath’s so any Bath Public Library and Art Gallery could geology by William Smith (1769–1839), from 1791, only be finally adopted in 1900 (Kelly 1977, 81-84). and its subsequent encouragement there by the BLSI, The museological history of Bath is equally complex, after Smith was in his northern English exile, was to because of the City’s dependence on ‘attracting have important museological consequences. A Bath tourists’ to keep the rates low. The history of the newspaper item dated 29 June 1929 (copy preserved BLSI/BRLSI Museum, by many decades the oldest in in T.S. Cotterell’s copy of Bather (1926), Bath Bath, but which is not ‘a tourist attraction’, is thus of Reference Library) reported how particular importance, although it fails to receive the citizens of Bath could not have a worthier notice in recent histories (e.g. Davis and Bonsall object to maintain, and their efforts should 1996). certainly be directed to the upkeep of this historic A more recent author has, rightly, claimed this is institution, which has been termed both ‘the Finest because Bath’s recent heritage-mongers have been Geological Museum outside London’ and to be antipathetic to local science and its history. ‘an institution whose opening date is uncertain’. There was no sign of a twentieth-century swing Such statements prompted the choice of 7 June 2003 [here] towards the sciences; indeed, quite the to launch the BRLSI’s reprint of the 1844 Memoirs of opposite appears to be the case. Any attempt, William Smith LL.D.. This was the 250th anniversary such as that of Williams and Stoddart (1978), to of the establishment of the British Museum on 7 June create a counter-hagiography of [Bath] scientists -141- and engineers was seemingly doomed to failure. married a London solicitor, Alexander Gordon However, during the nineteenth century science (c.1772–1854 —see Gentleman’s Magazine, February enjoyed considerable kudos in Bath, a position 1855, 221). The son of these latter, of the same name, reflected in the establishment of the prestigious also migrated to Sydney in 1857 where he died in Literary and Scientific Institution, whose Rooms 1903—(see Australian Dictionary of Biography and were opened in 1825, and which proceeded to Foster 1887–1891, vol. 1, 80). acquire... several scientific collections (Borsay 2000, 139). Hastings Elwin (or Elwyn) Senior (1742– Hastings Elwin junior’s vital role in the founding of 1833) this important institution is thus both critical and too Elwin senior is a similarly forgotten figure like his long forgotten. The Geological Curators’ Group has confusingly homonymous son. The only clues, but now campaigned for over 30 years, for the better which have considerable relevance to Hastings Elwin protection of its important collections (see Copp, junior’s later career as museum-builder and collector, Pickford and Torrens 1975 and Parker 1978). A are the several references to a “Mr Elwin” or “Elwyn” jubilee publication on the Institution’s history failed as art-collector and connoisseur in Georgian England. to mention him (Spender 1875). A recent piece by For example, he was listed, merely as “Elwyn”, by Jane Coates (the Institution’s then archivist) did note the German curator Gustav Waagen (1794–1868) in a new display which included material on the 1838, as among “founding fathers of the institution, notably Hastings Elwin” (Coates 2003, 4). But conclusive evidence of the most distinguished [such] collectors in his part in establishing this institution has never been England since 1792, who, by diffusing the most properly revealed, nor have details of his biography admirable works of art in their century, have or his distant fate. conferred upon it a lasting benefit (Waagen 1838, vol. 1, 57). It is extraordinary how some categories of people have fallen through the historical ‘net’ more than He is also listed in Joseph Farington’s diaries between others. I have already made this point in relation to 1797 and 1809 (Garlick and Macintyre 1979; Cave mineral surveyors (Torrens 2002). Their profession 1982). He is identified no further than ‘Hastings was often highly itinerant. Such itineracy becomes a Elwin’ in their index; but he is certain, in view of major problem for their biographical record and is these dates, to be Hastings Elwin senior. Fritz Lugt also one main reason why Hastings Elwin, of Norfolk, (1938) records details of five of the Catalogues of art Antigua, Bath and Australia, has fallen into near- he, as both Hastings Elwin or Elwyn, auctioned in complete historical anonymity. A second reason is London between 1787 and 1811 (Lugt nos 4242 of that Hastings Elwin, although twice married, had no 1787, 5263 of 1794, 7101 of 1806, 7791 of 1810 and children, through whom any memory, or archive, of 7918 of 1811). Lugt (1953) records another such sale his multi-faceted, widely spread, activities might of 1 June 1833 (Lugt no. 13325) by a mystery W.B. have been maintained. Elwyn who must be the Oxford educated barrister Dr William Brame Elwyn (c.1744–1841) but who came Elwin’s origins and birth from a different Canterbury family. Hastings senior was also active in art circles in London as a purchaser, Hastings Elwin was born on 8 March 1777, a fact and agent for the sale, of expensive paintings by, for only revealed on the far-away foot stone of what little example, Rubens, Van Dyke and others. He was also survives of his grave in Sydney, New South Wales. a major purchaser at the Fonthill House, Wiltshire He was the eldest son of the London barrister Hastings sale in August 1807 of two Vernet
Recommended publications
  • Heim Gallery Records, 1965-1991
    http://oac.cdlib.org/findaid/ark:/13030/kt5779r8sb No online items Finding aid for the Heim Gallery records, 1965-1991 Finding aid prepared by Isabella Zuralski. Finding aid for the Heim Gallery 910004 1 records, 1965-1991 Descriptive Summary Title: Heim Gallery records Date (inclusive): 1965-1991 Number: 910004 Creator/Collector: Heim Gallery Physical Description: 120.0 linear feet(271 boxes) Repository: The Getty Research Institute Special Collections 1200 Getty Center Drive, Suite 1100 Los Angeles, California, 90049-1688 (310) 440-7390 Abstract: London gallery directed by Andrew Ciechanowieck. Records include extensive correspondence with museums, galleries, collectors, and other colleagues in Europe and the United States. Photographs document paintings, drawings, sculptures, and decorative art sold and exhibited by, and offered to the gallery. Stock and financial records trace acquisitions and sales. Request Materials: Request access to the physical materials described in this inventory through the catalog record for this collection. Click here for the access policy . Language: Collection material is in English Biographical / Historical Note Heim Gallery London began in June 1966 with François Heim (from Galerie Heim, Paris, begun 1954) and Andrew S. Ciechanowiecki as partners. Ciechanowiecki served as director in London while Heim remained in France. The emphasis of the gallery was Old Master paintings, especially French of the 15th - 18th century, Italian paintings of all periods, and sculpture (marble, terracotta and bronze) from the Renaissance to the 19th century. The gallery was known for its scholarly exhibitions and catalogs. Between 1966 and 1989 the gallery presented exhibitions two to three times a year. The gallery did business with museums and individual clients in Europe and the United States.
    [Show full text]
  • III MRSS Dokembriy.Indd
    ФЕДЕРАЛЬНОЕ АГЕНТСТВО ПО НЕДРОПОЛЬЗОВАНИЮ ВСЕРОССИЙСКИЙ НАУЧНО-ИССЛЕДОВАТЕЛЬСКИЙ ГЕОЛОГИЧЕСКИЙ ИНСТИТУТ им. А. П. КАРПИНСКОГО MЕЖВЕДОМСТВЕННЫЙ СТРАТИГРАФИЧЕСКИЙ КОМИТЕТ РОССИИ РЕШЕНИЯ Третьего Межведомственного регионального стратиграфического совещания по докембрию, палеозою и мезозою Северо-Востока России (Санкт-Петербург, 2002) Издательство ВСЕГЕИ Санкт-Петербург – 2009 УДК 551.71/.72+551.73/.78 (925.17+925.16) Решения Третьего межведомственного регионального стратиграфического совещания по докембрию, палеозою и мезозою Северо-Востока России (Санкт-Петербург, 2002) / Ред. Т. Н. Корень, Г. В. Котляр. СПб.: Изд-во ВСЕГЕИ, 2009. 268 с. ISBN 978-5-93761-135-2 Публикуется Постановление МСК по стратиграфи- ческим схемам докембрия, палеозоя и мезозоя Северо- Востока России и объяснительные записки к ним. Схемы в настоящем издании представлены в электронном виде (на диске), прилагаемом к Решениям. Схемы и объяснительные записки к ним могут быть ис- пользованы при составлении и ревизии листов ГГК-200/2 и ГГК-1000/3, а также геологических карт масштабов 1 : 2 500 000 и 1 : 5 000 000 в рамках международных проек- тов по территории Азиатского континента. Схемы – 15 (на диске), список литературы 516 назв. Редакторы Т. Н. Корень, Г. В. Котляр © Всероссийский научно-исследовательский геологический институт им. А. П. Карпин- ского, 2009 © Межведомственный стратиграфический ко- митет России, 2009 ISBN 978-5-93761-135-2 © Коллектив авторов, 2009 ПРЕДИСЛОВИЕ Третье межведомственное региональное стратиграфическое совещание (3-е СВ МРСС) по докембрию, палеозою и мезозою Северо-Востока Рос- сии проходило 4–6 декабря 2002 г. в Санкт-Петербурге. Совещание было организовано ВСЕГЕИ, в его работе приняли участие более 70 производ- ственных организаций и институтов МПР РФ, высших учебных заведений и научно-исследовательских институтов РАН. Оргкомитет 3-го СВ МРСС: Т.
    [Show full text]
  • DID JOSHUA REYNOLDS PAINT HIS PICTURES? Matthew C
    DID JOSHUA REYNOLDS PAINT HIS PICTURES? Matthew C. Hunter Did Joshua Reynolds Paint His Pictures? The Transatlantic Work of Picturing in an Age of Chymical Reproduction In the spring of 1787, King George III visited the Royal Academy of Arts at Somerset House on the Strand in London’s West End. The king had come to see the first series of the Seven Sacraments painted by Nicolas Poussin (1594–1665) for Roman patron Cassiano dal Pozzo in the later 1630s. It was Poussin’s Extreme Unction (ca. 1638–1640) (fig. 1) that won the king’s particular praise.1 Below a coffered ceiling, Poussin depicts two trains of mourners converging in a darkened interior as a priest administers last rites to the dying man recumbent on a low bed. Light enters from the left in the elongated taper borne by a barefoot acolyte in a flowing, scarlet robe. It filters in peristaltic motion along the back wall where a projecting, circular molding describes somber totality. Ritual fluids proceed from the right, passing in relay from the cerulean pitcher on the illuminated tripod table to a green-garbed youth then to the gold flagon for which the central bearded elder reaches, to be rubbed as oily film on the invalid’s eyelids. Secured for twenty-first century eyes through a spectacular fund-raising campaign in 2013 by Cambridge’s Fitzwilliam Museum, Poussin’s picture had been put before the king in the 1780s by no less spirited means. Working for Charles Manners, fourth Duke of Rutland, a Scottish antiquarian named James Byres had Poussin’s Joshua Reynolds, Sacraments exported from Rome and shipped to London where they Diana (Sackville), Viscountess Crosbie were cleaned and exhibited under the auspices of Royal Academy (detail, see fig.
    [Show full text]
  • 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.
    [Show full text]
  • Paper Palaces: the Topham Collection As a Source for British Neo-Classicism
    Paper Palaces: the Topham Collection as a source for British Neo-Classicism Adriano Aymonino with Lucy Gwynn and Mirco Modolo Front cover image: Francesco Bartoli, Drawing of decorative mosaics in the vaulting of S. Costanza, c. 1720-25 (see cat. no. 25) Inside cover image: Francesco Bartoli, Drawing of an ancient ceiling from the Palatine, 1721 (see cat. no. 15) Paper Palaces: the Topham Collection as a source for British Neo-Classicism The Verey Gallery, Eton College May - November 2013 Curated by Lucy Gwynn & Adriano Aymonino Accompanied by the Conference: A Window on Antiquity: the Topham Collection at Eton College, 17th May 2013 Catalogue written by Adriano Aymonino with Lucy Gwynn and Mirco Modolo This catalogue is dedicated to the memory of Louisa M. Connor Bulman Contents Many people have given their support to the production of both the exhibition Foreword 4 Section 2 16 and this catalogue, and we would like in particular to thank: Lord Waldegrave of North Hill Robert Adam and his antiquarian sources The Tavolozza Foundation The Humanities Research Institute, the University of Buckingham Introduction 5 Section 3 22 the rationale for the exhibition Robert Adam, the Topham Collection and Country Life Magazine Francesco Bartoli Sir Francis Dashwood Richard Topham & Eton 6 by Lucy Gwynn The National Trust Section 4 40 The Topham Collection’s broader influence: Savills (UK) Limited Catalogue Charles Cameron and other Neo-Classical architects and decorators The authors would also like to thank Frances Sands for the fruitful discussion on the different hands in the Adam drawings; Jeremy Howard and Eleanor Davey for their Cataloguing Notes 8 help and support; Charlotte Villiers and Dennis Wallis for their patience and exquisite Notes 47 contribution in photography and design, Charlotte Villiers for the coordination of the exhibition, Pat McNeaney for his inexhaustible enthusiasm and skill, the Eton College Section 1 10 Buildings Department and Vario Press.
    [Show full text]
  • Dimerelloid Rhynchonellide Brachiopods in the Lower Jurassic of the Engadine (Canton Graubünden, National Park, Switzerland)
    1661-8726/08/010203–20 Swiss J. Geosci. 101 (2008) 203–222 DOI 10.1007/s00015-008-1250-8 Birkhäuser Verlag, Basel, 2008 Dimerelloid rhynchonellide brachiopods in the Lower Jurassic of the Engadine (Canton Graubünden, National Park, Switzerland) HEINZ SULSER & HEINZ FURRER * Key words: brachiopoda, Sulcirostra, Carapezzia, new species, Lower Jurassic, Austroalpine ABSTRACT ZUSAMMENFASSUNG New brachiopods (Dimerelloidea, Rhynchonellida) from Lower Jurassic Neue Brachiopoden (Dimerelloidea, Rhynchonellida) aus unterjurassischen (?lower Hettangian) hemipelagic sediments of the Swiss National Park in hemipelagischen Sedimenten (?unteres Hettangian) des Schweizerischen Na- south-eastern Engadine are described: Sulcirostra doesseggeri sp. nov. and tionalparks im südöstlichen Engadin werden als Sulcirostra doesseggeri sp. Carapezzia engadinensis sp. nov. Sulcirostra doesseggeri is externally similar to nov. und Carapezzia engadinensis sp. nov. beschrieben. Sulcirostra doesseggeri S. fuggeri (FRAUSCHER 1883), a dubious species, that could not be included in ist äusserlich S. fuggeri (FRAUSCHER 1883) ähnlich, einer zweifelhaften Spezies, a comparative study, because relevant samples no longer exist. A single speci- die nicht in eine vergleichende Untersuchung einbezogen werden konnte, weil men was tentatively assigned to Sulcirostra ?zitteli (BÖSE 1894) by comparison kein relevantes Material mehr vorhanden ist. Ein einzelnes Exemplar wird als of its external morphology with S. zitteli from the type locality. The partly Sulcirostra ?zitteli (BÖSE 1894) bezeichnet, im Vergleich mit der Aussenmor- silicified brachiopods are associated with sponge spicules, radiolarians and phologie von S. zitteli der Typuslokalität. Die teilweise silizifizierten Brachio- crinoid ossicles. Macrofossils are rare: dictyid sponges, gastropods, bivalves, poden waren mit Schwammnadeln, Radiolarien und Crinoiden-Stielgliedern crustaceans, shark teeth and scales of an actinopterygian fish. The Lower Ju- assoziiert.
    [Show full text]
  • Ammonites Marmoreus OPPEL
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Stuttgarter Beiträge Naturkunde Serie B [Paläontologie] Jahr/Year: 1988 Band/Volume: 141_B Autor(en)/Author(s): Bloos Gert Artikel/Article: Ammonites marmoreus OPPEL (Schlotheimiidae) im unteren Lias (angulata-Zone, depressa-Subzone) von Württemberg (Südwestdeutschland) 1-47 " ^ © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at Stuttgarter Beiträge zur Naturkunde Serie B (Geologie und Paläontologie) Herausgeber: Staatliches Museum für Naturkunde, Rosenstein 1, D-7000 Stuttgart 1 Stuttgarter Beitr. Naturk. Ser. B Nr. 141 47S., 12Taf., 11 Abb., 3Tab. Stuttgart, 15. 6. 1988 Ammonites marmoreus Oppel (Schlotheimiidae) im unteren Lias {angulata-Xont^ depressa-Suhzont) von Württemberg (Südwestdeutschland) Ammonites m^armoreus Oppel (Schlotheimiidae) in the lower Lias {angulata Zone, depressa Subzone) of Württemberg (Southwest Germany) _^^ Von Gert Bloos, Stuttgart ^ ^^^ ^ Mit 12 Tafeln, 11 Abbildungen und 3 Tabellen Summary ^=»=%^'^'Aslib The occurrence of the mediterranean spec'ies Ammonites marmoreus Oppel (Schlotheimiidae) in Württemberg - supposed already by Pompeckj 1893 - is verified. A comparison of the 11 stu- died specimens with material of the Eastern Alps yielded no significant differences concerning form, sculpture, and suture line. The differences to Schlotheimia on the one hand and to the charmassei group on the other are shown. There are two main groups within the Schlotheimiidae (not regarded "Waehneroceras" s.L): The one is well known as genus Schlotheimia and the other is here comprised under the name Angulaticeras (including Sulciferites) to which. Ammonites marmoreus belongs. The stratigraphical occurrence of the species in Württemberg Supports the Hettangian age of the marmoreum Zone in the Mediterranean province.
    [Show full text]
  • Paleontological Research of the Mesozoic in Uie Central Zone And
    Západně Karpaty • séria paleontológia (1) • P. 7—23 • GÚDŠ • Bratislava • 1975 Miloš Rakús Hettangian ammonites from the Strážovská hornatina Mts. (West Carpathians) 1 plate (CIV), 10 text-figs, Slovak summary The thorough geological — paleontological research of the Mesozoic in uie central zone and particularly in the Strážovská hornatina mountains resulted in detailed knowledge of the Hettangian Ammonites. Conse­ quently, a summarizing report may be presented on the ammonites. The first, and for considerable time the only published report on the Hettangian Ammonites was that by D. Stúr (1868, p. 378) from the loca­ lity Rakytov (the Velká Fatra mountains), viz A. psilonotus laevis (Q u .) = Psiloceras psilonotum (Quenstedt). Unfortunately, the find has not been repeated so far. Still I suppose that in this case its presence might be regarded as probable, since: a) the species Psiloceras psilonotum is a typical, easily identifiable form, and it is almost impossible to mistake it for another species; b) on the locality Rakytov are well-developed se­ quences of the Upper Triassic (the Rhaetic) to Lower Liassic. Both they yielded rich fauna of lamellibranchiates, so the presence of the Hettan­ gian may be taken for sure there. In the sixties (M. Rakús in M. Mahel 1962; V. Andrusovová —D. Andrusov 1968) published were some reports on the finds of the Hettangian Ammonites from the central zone. In the central zone of the West Carpathians, most Hettangian Ammonites come from the Strá­ žovská hornatina mountains (Central Slovakia). Other finds are from these localities: — the vicinity of Cierna Lehota (text — fig. 1); — Kozinec (text — fig. 2); — Trencianska Teplá.
    [Show full text]
  • Renaissance Diplomacy in Practice: the Case of Gregorio Casali, England’S Ambassador to the Papal Court, 1525-33
    Renaissance diplomacy in practice: the case of Gregorio Casali, England’s ambassador to the papal court, 1525-33 Catherine Lucy Fletcher Royal Holloway, University of London Thesis presented for the award of PhD 1 I confirm that the work contained in this thesis is entirely my own. Catherine Fletcher 23 April 2008 2 Abstract THIS thesis investigates the day-to-day practice of Renaissance diplomacy through a case-study of Gregorio Casali, one of a number of Italians in the Roman diplomatic corps who served foreign princes, in Casali’s case King Henry VIII of England. It outlines and analyses the key elements of the resident ambassador’s role, shifting the focus of study from the traditional emphasis on official negotiations and such formal sites for the exercise of power to consider too informal relationships and arenas for diplomacy. Chapters consider the diplomat’s role in Rome (the most developed diplomatic centre of its day); the relevance of family and friendship networks in Casali’s career; the importance of hospitality and liberality in diplomatic life; gift- giving and ‘bribery’. Drawing on recent scholarship relating to such issues as the house, household and gift-giving, the thesis situates Renaissance diplomacy in its broader social context. It thus contributes to the new trend among historians of diplomacy to adopt methods from social and cultural history, but, in applying the methodology of microhistory, takes this to a new level. As well as raising new questions about the role of the resident ambassador and his interaction with other diplomatic and political actors, the case of Casali and his family draws attention to the important issue of the employment of foreigners in diplomatic service during this period, allowing a consideration of how loyalty was understood and allegiances were managed.
    [Show full text]
  • 1 1 2 Combined Sea–Level and Climate Controls on Limestone Formation
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Plymouth Electronic Archive and Research Library 1 2 3 Combined sea–level and climate controls on limestone formation, hiatuses and ammonite 4 preservation in the Blue Lias Formation, South Britain (uppermost Triassic–Lower 5 Jurassic) 6 7 Short title/running head: Sea level and climate controls of the Blue Lias 8 9 Graham P. Weedon1*, Hugh C. Jenkyns2 and Kevin N. Page3 10 11 * Corresponding author 12 1 [email protected], Met Office, Maclean Building, Benson Lane, 13 Crowmarsh Gifford, Wallingford, Oxfordshire, OX10 8BB, UK. 14 2 Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, 15 UK. 16 3 School of Geography, Earth and Environmental Sciences, Plymouth University, Drakes 17 Circus, Plymouth, PL4 8AA, UK. 18 19 20 21 In press: Geological Magazine 22 23 January 2017 24 1 25 Abstract 26 Lithostratigraphic and magnetic-susceptibility logs for four sections in the Blue Lias 27 Formation are combined with a re-assessment of the ammonite biostratigraphy. A Shaw plot 28 correlating the West Somerset coast with the Devon/Dorset coast at Lyme Regis, based on 63 29 common biohorizon picks, together with field evidence, demonstrate that intra-formational 30 hiatuses are common. Compared to laminated shale deposition, the climate associated with 31 light marl is interpreted as both drier and stormier. Storm-related non-deposition favoured 32 initiation of limestone formation near the sediment-water interface. Areas and time intervals 33 with reduced water depths had lower net accumulation rates and developed a greater proportion 34 of limestone.
    [Show full text]
  • Mercury Anomalies and Carbon Isotope Excursions in the Western
    Global and Planetary Change 194 (2020) 103291 Contents lists available at ScienceDirect Global and Planetary Change journal homepage: www.elsevier.com/locate/gloplacha Mercury anomalies and carbon isotope excursions in the western Tethyan T Csővár section support the link between CAMP volcanism and the end- Triassic extinction ⁎ Emma Blanka Kovácsa,b,c,d, , Micha Ruhlc,d,e, Attila Deményf, István Fórizsf, István Hegyif, Zsófia Rita Horváth-Kostkaa, Ferenc Móriczg, Zsolt Vallnera,b, József Pálfya,h a Department of Geology, Eötvös Loránd University, Pázmány Péter sétány 1/C, Budapest H-1117, Hungary b Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Bem tér 18/C, Debrecen H-4026, Hungary c Department of Geology, Trinity College Dublin, The University of Dublin, College Green, Dublin 2, Ireland d Earth Surface Research Laboratory (ESRL), Trinity College Dublin, The University of Dublin, Dublin 2, Dublin, Ireland e Irish Centre for Research in Applied Geosciences (iCRAG), Trinity College Dublin, The University of Dublin, College Green, Dublin 2, Dublin, Ireland f Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences (RCAES), Budaörsi út 45, Budapest H-1112, Hungary g Institute of Mineralogy and Petrology, University of Miskolc, Miskolc-Egyetemváros H-3515, Hungary h MTA–MTM–ELTE Research Group for Paleontology, Pázmány Péter sétány 1/C, Budapest H-1117, Hungary ARTICLE INFO ABSTRACT Keywords: The end-Triassic extinction is one of the major Phanerozoic mass extinctions and it appears to have been linked to Triassic–Jurassic boundary coeval rapid and severe environmental change, thought to be triggered by volcanism in the Central Atlantic stable carbon isotopes Magmatic Province (CAMP).
    [Show full text]
  • The Marine Jurassic of Argentina: a Biostratigraphic Framework
    326 by Alberto C. Riccardi The marine Jurassic of Argentina: a biostratigraphic framework Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina. Email: [email protected] In Argentina the best and most complete marine Juras- sic succession is exposed between 32° and 39° S, along a N-S belt roughly coincident with the border with Chile. Here all stages, except the Kimmeridgian, are represented by marine facies. Ammonites have provided a biostratigraphic framework to date and correlate lithostratigraphic units and sequences, to reconstruct the history of the marine fill, and allow the development of other palaeontological and geological studies. Recent studies on the systematics and/or biostratigra- phy of Andean ammonites have provided the basis for the presentation of a summary of the 45 ammonite zones of the Jurassic of west-central Argentina and to stress its significance in reconstructing the palaeogeographic evolution of that region. Introduction Jurassic rocks in Argentina are present over extensive areas (see Fig- ure 1) and include a large variety of marine and continental facies (see Riccardi et al., 1992). South of 39°S marine Jurassic consists of Pliensbachian-Lower Toarcian and uppermost Jurassic strata, repre- sented respectively in central and southern Patagonia. North of 39°S marine Jurassic is exposed along a N-S belt roughly coincident with the boundary between Argentina and Chile, up to 31°S where it becomes restricted to Chile. The marine Jurassic generally rests unconformably on Upper Triassic (west-central Argentina) and Upper Jurassic vulcanites (southern Patagonia) or on Upper Paleozoic (west-central Patago- nia).
    [Show full text]