Jurassic Rhynchonellids Internal Structures and Taxonomic Revisions SERIES PUBLICATIONS of the SMITHSONIAN INSTITUTION
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
G. Arthur Cooper
G. ARTHUR COOPER SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY • NUMBER 65 SERIES PUBLICATIONS OF THE SMITHSONIAN INSTITUTION Emphasis upon publication as a means of "diffusing knowledge" was expressed by the first Secretary of the Smithsonian. In his formal plan for the Institution, Joseph Henry outlined a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge.' This theme of basic research has been adhered to through the years by thousands of titles issued in series publications under the Smithsonian imprint, commencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Contributions to Anthropotogy Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to the h/larine Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Folklife Studies Smithsonian Studies in Air and Space Smithsonian Studies in History and Technology In these series, the Institution publishes small papers and full-scale monographs that report the research and collections of its various museums and bureaux or of professional colleagues in the world of science and scholarship. The publications are distributed by mailing lists to libraries, universities, and similar institutions throughout the worid. Papers or monographs submitted for series publication are received by the Smithsonian Institution Press, subject to its own review for format and style, only through departments of the various Smithsonian museums or bureaux, where the manuscripts are given substantive review. -
New Document
ANNUAL STATEMENT OF RESERVES 2016 AKER BP ASA Annual Statement of Reserves 2016 Annual Statement of Reserves 2016 Table of Contents 1 Classification of Reserves and Contingent Resources 1 2 Reserves, Developed and Non-Developed 2 3 Description of Reserves 5 3.1 Producing Assets 5 3.1.1 Alvheim and Viper/Kobra (PL036, Pl088BS, PL203) 5 3.1.2 Vilje (PL036D) 7 3.1.3 Volund (PL150) 8 3.1.4 Bøyla (PL340) 9 3.1.5 Atla (PL102C) 11 3.1.6 Jette (PL027D), PL169C, PL504) 11 3.1.7 Jotun (PL027B, PL203B) 12 3.1.8 Varg (PL038) 12 3.1.9 Ivar Aasen Unit and Hanz (Pl001B, PL028B, PL242, PL338BS, PL457) 13 3.1.10 Valhall (PL006B, PL033B) 15 3.1.11 Hod (PL033) 16 3.1.12 Ula (PL019) 17 3.1.13 Tambar (PL065) 19 3.1.14 Tambar East (PL065, PL300, PL019B) 20 3.1.15 Skarv/Snadd (PL262, PL159, PL212B, PL212) 21 3.2 Development Projects 22 3.2.1 Johan Sverdrup (PL265, PL501, PL502; Pl501B) 22 3.2.2 Gina Krog (PL029B) 25 3.2.3 Oda (PL405) 26 4 Contingent Resources 28 5 Management’s Discussion and Analysis 34 Annual Statement of Reserves 2016 List of Figures 1.1 SPE reserves and recourses classification systen .................................................................... 1 3.1 Alvheim and Viper/Kobra Location Map.................................................................................... 5 3.2 Vilje location map ...................................................................................................................... 7 3.3 Volund location map.................................................................................................................. 8 3.4 Bøyla location map.................................................................................................................. 10 3.5 Ivar Aasen Unit and Hanz location map.................................................................................. 13 3.6 Valhall and Hod location map................................................................................................. -
GLOUCESTERSHIRE. MID 397 Marks Rev
COURT DIRECTORY.] GLOUCESTERSHIRE. MID 397 Marks Rev. Ro'bert B.A. The ;Vicarage, Mason Henry, Windrush, Burford ,Mayer L. G. H. 120 London rd.Glo'str Norton, Gloucester R.8.0. (Oxon) Maynard Miss, Loughton villa, Great Marling Sir William Henry bart. D.L., Mason Misses, Beacon house, New st. Western road, Cheltenham J.P. Stanley park, Selsley, 'Stroud Painswick, Stroud Mayne Rev. William John, Vicarage, Marling Col. Walter Eentley J.P. Clan- Mason Mrs. Park street, Stow·on-the- Poulton, Fairford 8.0 na, A;.vIDgton, Lydney Wold S.O Mayne Edward, Orchard street, Wot- Marling ~laj. Pereival Scrope V.C., Massey Mrs. Westbourne villa, GIou- ton-under-Edge J.P. Stanley park. Selsley, Stroud cester TOad, Cheltenham Mnyne Richd. Cutwell hill, Tetbury Mrarling Charles Murray M.A. Stanley MassJ1 Capt. Godfrey Lennox Eyre, Mayo Benjamin Pleydell,Vine Tree cot. park, Selsley, Stroud Uley lodge, Dursley tage, Rodley, Newnham ~larling Samuel Stanley J.P. Stanley Massy-Dawson Mrs. Coombe bank,Slad Mayo W. P. 30 Midland Il'd. Gloucester park, Selsley, Stroud road, Stroud Mayos Thomas, 2 Bayshill parade, St. Marling William John Paley M.A.Stan- Master Digby C. Elm gro. Cirencester George?s road, Cheltenham ley park, 8elsley, Stroud Master Mrs. A. Elm gtrO'Ve,Cirencestr Maysey Mrs. 26 Kingsholm rd.Glo'ster Marment James, 6 Glenfall terrace, Master Thomas William Chester D.L., Meadows H. Sutgrove, Tuffiey, Glo'str All Saints' road, Cheltenham J.P. Knole park,Almondsbury R.S.O Meadows Miss, Longborough, Moreton- Marmont Arthur C. Northfields, Inch- Mast~r Thomas William Chester, jun. -
Systematics of the Middle Jurassic Heteromorphic Ammonites
UDC 564. 53 . 01 SYSTEMATICS OF THE MIDDLE JURASSIC HETEROMORPHIC AMMONITES N. V. Besnosov and V. V. Kutuzova All-Union Scientific Research Petroleum Geologic Exploration Institute (VSEGEI) ABSTRACT: The stratigraphic distribution, phylogenetic relationships, and systema tics of the Middle Jurassic heteromorphic ammonites and their relationship to the monomorphic ammonites are considered. Sulcohamitoides gen. nov. and Ga�antiana as a�jani sp. nov. are described. * * * The vast majority of Middle Jurassic heteromorphic ammonites are shells with a spiral developing early in one plane, all the way to the formation of a straight tube in the outer part of the phragmocone and in the living chamber. They are also characterized by reduction of the U and I lobes in ontogenesis, manifested to a greater or lesser degree, and by only slight dissection of their lobes and saddles. The following generic names of the Jurassic heteromorphs are given in the lite rature. A�cuce�as Potonie, 1929, for which the family Arcuceratidae Arkell, 1950 has been proposed. This genus is based on a single species, A. ma�thae Potonie, from the Pliensbachian of Germany, the only specimen of which has been lost. Repeated searches at the type locality have been unsuccessful. It has been suggested that the dating is erroneous, or that the species and genus are based not on a heteromor phic ammonite, but on acrinoid stem. Apso��oce�as Hyatt, 1900, occurs in the lower half of the subfu�catum zone of the Upper-Bajocian and has usually been combined with Spi�oce�as Quenstedt, 1858, from which it differs in its less reduced U and I lobes and its finer sculpture. -
"Subfurcaten-Schichten" (Bajocium, Niortense-Zone) in Nordwestdeutschland
Osnabrücker naturwiss. Mitt. 5Abb.,4Taf. Osnabrück, Dez. 1992 Die Faunenhorizonte der "Subfurcaten-Schichten" (Bajocium, Niortense-Zone) in Nordwestdeutschland mit5 Abbildungen und 4 Tafeln Matthias Metz' Kurzfassung: Aufgrund neuer Aufschlüsse der "Subfurcaten-Schichten" (Bajocium, Niortense- Zone) in Nordwestdeutschland ist es möglich, die Schichtenfolge in Ammonitenfaunen-Horizonte zu untergliedern. Eine paläontologische Revision der Ammonitengattung Strenoceras HYATTmit den Untergattungen Strenoceras HYATT(m) und Garantiana HYATT(M) wird durchgeführt. [The faunal horizons of the "Subfurcaten-Schichten" (Bajocian, Niortense-Zone) in Northwest Germany) Abstract: Because of new exposures in the "Subfurcaten-Schichten" (Bajocian, Niortense- Zone) in Northwest Germany it is possible to subdivide the sequence in ammonite faunal hori- zons. A palaeontological revision of the genus Strenoceras HYATTwith the subgenus Strenoceras HYATT(m) and Garantiana HYATT(M) is executed. 1 Einleitung und historischer Überblick U Die ersten Hinweise auf die .Bifurcaten-Schichten" (= "Subfurcaten-Schichten ) fin- den sich bereits in den Veröffentlichungen von TRENKNER(1872; 1877) und POELMANN (1912) über die Juravorkommen in Osnabrück-Hellern. Im Wiehengebirge konnten LOHMANN(1909) bei Bad Essen und v. SEE (1910) an der Porta Westfalica die Schich- ten ebenfalls nachweisen. Der Begriff "Schichten oder Zone der Parkinsonia subturcete" wurde erstmals von SCHROEDER(1905) verwendet, der zahlreiche Vorkommen in Nordwestdeutschland beschrieb. Die paläontologische Erforschung ihrer Ammonitenfauna wurde von MAscKE (1907) und BENTZ (1924) mit dem aus dem Brauneisenoolith-Bergbau von Lindenbruch und Harlingerode (Harz-Vorland) gewonnenen Ammonitenmaterial begonnen. Demgegenüber sind die "Subfurcaten-SchichtenU im Bereich des Teuto- burger Waldes in toniger Fazies ausgebildet. Die wichtigsten Aufschlüsse waren die Tongruben von Bielefeld-Bethel (heute verfüllt). ALTHoFF (1914; 1922; 1928; 1938) veröffentlichte zahlreiche Profilaufnahmen. -
Mechanics Unlocks the Morphogenetic Puzzle of Interlocking Bivalved Shells
Mechanics unlocks the morphogenetic puzzle of interlocking bivalved shells Derek E. Moultona,1 , Alain Gorielya , and Regis´ Chiratb aMathematical Institute, University of Oxford, Oxford, OX2 6GG, United Kingdom; and bCNRS 5276, LGL-TPE (Le Laboratoire de Geologie´ de Lyon: Terre, Planetes,` Environnement), Universite´ Lyon 1, 69622 Villeurbanne Cedex, France Edited by Sean H. Rice, Texas Tech University, Lubbock, TX, and accepted by Editorial Board Member David Jablonski November 11, 2019 (received for review September 24, 2019) Brachiopods and mollusks are 2 shell-bearing phyla that diverged tal events causing shell injuries. Yet, in all cases the interlocking from a common shell-less ancestor more than 540 million years ago. of the 2 shell edges is tightly maintained. These observations Brachiopods and bivalve mollusks have also convergently evolved imply that the interlocking pattern emerges as the result of epi- a bivalved shell that displays an apparently mundane, yet strik- genetic interactions modulating the behavior of the secreting ing feature from a developmental point of view: When the shell mantle during shell development. is closed, the 2 valve edges meet each other in a commissure that Here, we provide a geometric and mechanical explanation forms a continuum with no gaps or overlaps despite the fact that for this morphological trait based on a detailed analysis of the each valve, secreted by 2 mantle lobes, may present antisymmet- shell geometry during growth and the physical interaction of the ric ornamental patterns of varying regularity and size. Interlock- shell-secreting soft mantle with both the rigid shell edge and ing is maintained throughout the entirety of development, even the opposing mantle lobe. -
Les Brachiopodes De La Collection Eudes-Deslongchamps Du Muséum De Gaillac (Tarn)
Les Carnets natures, 2014, vol. 1 Les Brachiopodes de la collection Eudes-Deslongchamps Du muséum de Gaillac (Tarn) Yves ALMéRAS, Michel COUGNON, Bernard GUIBBERT & Philippe FAURé Yves Alméras : Université Claude-Bernard-Lyon 1, Département des Sciences de la Terre, Campus universitaire de la Doua, bâtiment Géode, 2 rue Raphaël Dubois, 69622 Villeurbanne Cedex, France. E-mail : yves.almeras0827@ orange.fr Michel Cougnon : E-mail : [email protected] Bernard Guibbert : E-mail : [email protected] Philippe Fauré : Muséum d’Histoire naturelle de Toulouse, allées Jules Guesdes, F-31000 Toulouse. E-mail : [email protected] Résumé Les collections du Musée de Gaillac renferment un important fond de fossiles provenant du Jurassique de Normandie. Ceux-ci furent recueillis à la fin du 19ème siècle par le Dr. Philadelphe Thomas profitant de ses bonnes relations avec le paléontologue normand Eugène Eudes-Deslongchamps. On y trouve en particulier un important lot de Brachiopodes déterminés et étiquetés par cet éminent spécialiste des Brachiopodes jurassiques. La disparition de la collection originale du Musée de Caen sous les bombes des alliés en 1944 en fait toute la valeur car les collections du Musée de Gaillac renferment un certain nombre de topotypes (ou néotypes) éventuels. La présente publication donne une brève description des espèces de Brachiopodes jurassiques conservées à Gaillac. Ces descriptions sont précédées d’une synonymie précisant la diagnose originale de chaque espèce, ainsi que la référence à une récente publication, ce qui permet au lecteur de retrouver toutes les données relatives à ces espèces (variabilité morphologique, caractères internes, âges et répartitions géographiques, principales figurations par les auteurs successifs). -
Ammonites and Stratigraphy of the Upper Bajocian Garantiana Garantiana Zone in the Interfluve Between the Kuban and Urup Rivers (Northern Caucasus) V
ISSN 0031-0301, Paleontological Journal, 2019, Vol. 53, No. 11, pp. 1188–1202. © Pleiades Publishing, Ltd., 2019. Ammonites and Stratigraphy of the Upper Bajocian Garantiana garantiana Zone in the Interfluve between the Kuban and Urup Rivers (Northern Caucasus) V. V. Mittaa, b, * aBorissiak Paleontological Institute, Russian Academy of Sciences, Moscow, 117647 Russia bCherepovets State University, Cherepovets, 162600 Russia *e-mail: [email protected] Received March 12, 2019; revised March 29, 2019; accepted April 1, 2019 Abstract—This paper presents the results of the study of the Upper Bajocian Garantiana garantiana Zone (Middle Jurassic) and characteristic ammonites in sections of the basin of the Kuban River (Karachay-Cher- kessia). The assemblage contains species of the genera Garantiana, Pseudogarantiana, Paragarantiana, Djanaliparkinsonia (all family Stephanoceratidae) and Vermisphinctes (family Perisphinctidae). A section of the Garantiana Zone on the Kyafar River contains (from bottom to top) Beds with Djanaliparkinsonia alanica (also recognized on the Kuban River), Beds with Garantiana subgaranti and Beds with Paragarantiana, approximately corresponding to the Dichotoma, Garantiana, and Tetragona subzones of the standard scale. Garantiana subgaranti Wetzel and Vermisphinctes martiusii (d’Orbigny) are described. Prorsisphinctes Buck- man, 1921 is proposed as a junior subjective synonym of Vermisphinctes Buckman, 1920. Keywords: Upper Bajocian, ammonites, Garantiana, Paragarantiana, Djanaliparkinsonia, Vermisphinctes, biostratigraphy, Northern Caucasus DOI: 10.1134/S0031030119110066 INTRODUCTION lished records of representatives of Garantianinae in the Garantiana Zone in the Northern Caucasus The Garantiana garantiana Zone is located (Ob”yasnitelnaya…, 1973; Yura…, 1992) are not sup- between the Upper Bajocian Strenoceras niortense and ported by figures or collections, and are mostly based Parkinsonia parkinsoni zones of the standard scale and on field identifications. -
The Global Stratotype Sections and Point (GSSP) for the Base of the Jurassic System at Kuhjoch (Karwendel Mountains, Northern Calcareous Alps, Tyrol, Austria)
162 162 Articles by Hillebrandt, A.v.1, Krystyn, L.2, Kürschner, W.M.3, Bonis, N.R.4, Ruhl, M.5, Richoz, S.6, Schobben, M. A. N.12, Urlichs, M.7, Bown, P.R.8, Kment, K.9, McRoberts, C.A.10, Simms, M.11, and Tomãsových, A13 The Global Stratotype Sections and Point (GSSP) for the base of the Jurassic System at Kuhjoch (Karwendel Mountains, Northern Calcareous Alps, Tyrol, Austria) 1 Institut für Angewandte Geowissenschaften, Technische Universität, Ernst-Reuter-Platz 1, 10587 Berlin, Germany. E-mail: [email protected] 2 Department for Palaeontology, Vienna University, Geozentrum, Althansstr. 9, A-1090 Vienna, Austria. E-mail: [email protected] 3 Department of Geosciences and Centre of Earth Evolution and Dynamics (CEED), University of Oslo, PO box 1047, Blindern, 0316 Oslo, Norway. E-mail: [email protected] 4 Shell Global Solutions International B.V., Kessler Park 1, 2288 GS, Rijswijk, the Netherlands. E-mail: [email protected] 5 Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK. E-mail: [email protected] 6 Commission for the Palaeontological and Stratigraphical Research of Austria, Austrian Academy of Sciences c/o Institut of Earth Sciences, Graz University, Heinrichstraße 26, 8010 Graz, Austria. E-mail: [email protected] 7 Staatliches Museum für Naturkunde, Rosenstein 1, 70191 Stuttgart, Germany. E-mail: [email protected] 8 Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK. E-mail: [email protected] 9 Lenggrieser Str. -
Amberley Ridge
AMBERLEY RIDGE MINCHINHAMPTON COMMON . GLOUCESTERSHIRE GL5 5DB COLBURN ALL IN THE DETAIL AMBERLEY RIDGE is an exclusive new development of very desirae 3, 4 and 5 bedrm homes ideay located on e edge of Minchinhampton Common SELSLEY COMMON RODBOROUGH COMMON 2 RODBOROUGH COMMON MINCHINHAMPTON COMMON 3 COLBURN THE MARKET HOUSE, TETBURY THE COMPANY Colburn is recognised as an independent local Colburn works hard to keep ahead of the game developer who cares intensely about the tradition producing highly specified homes of exceptional Colburn is an established residential development and character of its build locations and who takes quality. Their ‘special touches’ and attention to company based near Stroud, Gloucestershire, pride in their reputation for planning and detail make their homes original, individual which for the past 30 years has specialised producing small developments of outstanding style, and highly appreciated by the more discerning in numerous challenging and highly original design and quality. New bespoke house type styles home owner. developments located throughout the southwest are designed and created for each development to including the counties of Gloucestershire, Colburn is conscious of their responsibility to the respond naturally to the surroundings in which they Somerset, Avon, Wiltshire and Herefordshire. environment, taking great pride in their dedication are situated, be that city, town or country. to sustainable building. They have proved it is The Company has a renowned reputation for possible to reduce the impact on the environment not only building new homes of the highest quality WHY BUY A COLBURN HOME? without cutting corners on quality or design, homes and specification, but also planning and producing Colburn is an established local developer with a to be proud of, homes for the future. -
Talexirhynchia, a New Rhynchonellid Genus from the Jurassic Ethiopian Province of Jordan
Talexirhynchia, a new rhynchonellid genus from the Jurassic Ethiopian Province of Jordan Howard R. Feldman, Mena Schemm- Gregory, Mark A. Wilson & Fayez Ahmad Paläontologische Zeitschrift Scientific Contributions to Palaeontology ISSN 0031-0220 Paläontol Z DOI 10.1007/s12542-013-0216-y 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/s12542-013-0216-y RESEARCH PAPER Talexirhynchia, a new rhynchonellid genus from the Jurassic Ethiopian Province of Jordan Howard R. Feldman • Mena Schemm-Gregory • Mark A. Wilson • Fayez Ahmad Received: 30 May 2013 / Accepted: 28 November 2013 Ó Springer-Verlag Berlin Heidelberg 2013 Abstract A new genus and species of a rhynchonellide scattered on a limy substrate, such as shells and rocks, brachiopod from the Jurassic of Jordan, Talexirhynchia could have served as an attachment site for juveniles. With kadishi gen. et sp. nov., is described. -
Paléobiologie
REVUE DE VOLUME 35 (2 ) – 2016 PALÉOBIOLOGIE Une institution Ville de Genève www.museum-geneve.ch Revue de Paléobiologie, Genève (décembre 2016) 35 (2): 385-416 ISSN 0253-6730 Die Brachiopoden der Klippendecke (Préalpes médianes) in den Préalpes romandes der Südwestschweiz, des Chablais und der zentralschweizerischen Klippen: eine Übersicht und paläogeographische Beziehungen Heinz SULSER Paläontologisches Institut und Museum der Universität Zürich, Karl Schmid-Str. 4, CH-8006 Zürich. E-Mail: [email protected] Zusammenfassung Die Kenntnis der Brachiopoden der Préalpes romandes in der Südwestschweiz (Kantone Bern, Freiburg und Waadt), des fränzösi- schen Chablais und der Klippenregion der Zentralschweiz beruht zum grossen Teil auf den klassischen Arbeiten früherer Autoren. Die Brachiopoden kommen fast ausschliesslich in der Klippendecke (Préalpes médianes) vor. Die Klippendecke besteht aus einer nahezu lückenlosen Abfolge von mesozoischen Sedimenten. In fast allen stratigraphischen Stufen kommen Brachiopoden vor, doch mit unter- schiedlicher Häufigkeit und Frequenz. In der vorliegenden Arbeit werden über 60 Arten der Ordnungen Rhynchonellida, Spiriferinida und Terebratulida diskutiert. Zwei neue Arten (Septaliphoria felberi nov. sp., Aulacothyris maendlii nov. sp.) aus dem Dogger der My- then werden beschrieben. Obwohl die von älteren Autoren aufgestellten Arten neu untersucht und teilweise revidiert werden müssen, ist der besondere Charakter dieser Brachiopoden offensichtlich. In der Trias lassen sich die Brachiopoden mit Vorkommen in ganz Europa vergleichen. Im späten Dogger und Malm zeigen sich deutliche Analogien zu Formen der Ost- und Südalpen. Die Brachiopoden der Mytilus-Schichten sind eher endemisch. Im frühen und mittleren Lias erscheint eine gemischte Fauna mit Arten aus Jura und Alpen. Diese Affinitäten passen recht gut in den gegebenen tektonischen Rahmen: nach der Trennung des Kontinents Pangaea in einen euro- päischen Nord- und afrikanischen Südteil am Ende der Trias entstanden in der Bruchzone Mikrokontinente (Ostalpen, Briançonnais).