Nelson, 1968 Ammonites

Total Page:16

File Type:pdf, Size:1020Kb

Nelson, 1968 Ammonites J. Soc.Biblphy nat. Hist.(r968) 5 (r): 1-18. Ammonites: Ammon's Horns into Cephalopods* By CLIFFORD M. NELSON Departmentof Palaeontology, tJniversityof Califomia,Berkeley. Ammonites, unlike the living pearly and papernautili, have yet to be gracedby the poerry of a Holmesl or a Pope2and are lesswidely known outsidepaleontological fields; how- ever, their esthetics,abundance, widespread distribution, and the legendsassociated with these geologically useful extinct cephalopodshave captured the literary attentions of Scott, Schiller, and Goethe. Ammonites, or more recently ammonoids,3 like many other long-known fossils, although not always understoodas to their nature and origins, have been associatedwith necromancy, myths, legends,and history sinceLate Paleolithic times. SixJurassicspeci- mensfrom SolutreanIII at Forneaudu Diable, Bourdeilles,France have perforatedcenters and may have formed a necklacesomewhat like one found in a Bronze Agelocality near Gravesendin Kent, fashionedbyjoining naturally vented Cretaceoussponges.a A number of markings which appearto be glyphs of some sort follow the curve of the ourer whorl of an ammonite from the French Magdaleniansand may have been usedin magic rituals similar to those of the North American Blackfoot Indians. As ammonires seemed to resemblesleeping bison to theseindians, they were called "iniskim" or buffalo stonesand hence were the central objectsin the sacredbundles used in the sympathetic magic for coiralling bison.6As talismans,they occur in the pouches of Navajo shamans.TJurassic ammonoids from the Himalayas are used as amulets throughout India and as fetish symbols in Hindu temples where they are: . ._,rggarded as the embodimentof the god Vishnu,and spouse of the basilplant. They are called"salagrams" or "salagrama"[after the ancient village]. A draughtofthe waterin which oneofthe sacredammonites has been steeped is supposedto washaway sin and secure temporal weifare.8 'was " Ammonite" ,e literally " stoneof Ammon ", derived from the resemblanceof the crenulatedwhorls of thesefossils to the ram's horns sacredto the ancientEgyptian deity Amun, or to those worn by him on his ram-headedefiigies or rhose of Zeus(Jupiter)- Ammon, his Greek and Roman amalgams.l0The ". ites" sufiixis aremnatrt of th. ideasconcerning the non-organic nature of fossils,added to the namesof objectswhich were thought to only resembleliving organismsor rheir parrs and were not rheir actual remains. To the ancient Egyptians, Amun1l originally representedthe dynamic force "air" or "wind", the universalbreath oflife which animatedall things. From obscurebeginnings in Thebesduring the Old Kingdom, he achievednational prominenceby associationwith the successfulTheban dynasts,and by the Eighteenth Dynasty, universality, with all the attributesofthe previouscreator deities,when merged with solarRe asAmun-Re, "King of the Gods".12The bestknown ofhis many oraclesis that at OasisSiwa13 in the Western Desert some 35o miles west-south-west of modern Cairo. Through contact with the Cyrenian Hellenesbeginning in the sixth century n.c., Amun was merged with Zeus,and from the Museumof Palaeontology,University of California,Berkeley. ilontribution 7 2 AMMONITES: AMMON'S HORNS INTO CEPHALOPODS the Oracle of Zeus-Ammon becamefamous throughout the Greek world.la After that of Apollo at Delphi, Siwa and Dodona in Epirus were the leading authoritiesin Hellenic affairs for centuries.Siwa, however, was an Egyptian oracle for Greeks-the principal native augur being at Buto in the Delta.ls Demigods and heroes,kings and princes,all visited or consultedthe oracle during its prominence.l6First among thesewas Alexander the Great,who arrived at Siwa in 33 r n.c. a{ter amiraculousjourneyfrom the coast.l7As pharaohand "son of Ammon" he after wards wore the sacredram's horns tied to a {illet so that they appearedto grow from his hair. Diadochi coinageshows him thus; he becameknown to legendas "Alexander of the Two Horns."18 In time thesehorns were associatedwith the divine attributesof royalty in Successorkingdoms and the Roman Empire.tn By late Hellenistic times the fame of the "Horns of Ammon" ensured their associationwith the oddly crenulated curved fossilscommon in certain parts of the Mediterraneanbasin. Pliny the Elder reGrs to them as: ...'Hammonis cornu' or'horn of Ammon,'which is amongthe mostsacred stones of Ethiopia,has a goldenyellow colourand is shapedlike a ram'shorn. This stoneis guaranteed to ensurewithout fail dreamsthat r,villcome true.20 Pliny later treatsprecious stoneswhich derive their namesfrom animals,by color or likencss(Chapter 7z). Although he was familiar with the argonaut, and presumably by reading Aristotle with the nautilus, in view of the decline of the Ionian ideasof temporal perspectiveby this time, it is unrealisticto expect an analogy with the ammonites.These remainedCornu ammonis until the end ofthe controversyover the organic nature offossils. Solinus, obviously referring to Pliny's description, first mentions the occurrence of ammonitesat Siwa: . Betweenthis Towne [Cyrene]and the Templeof Anmton,are fourehundred miles, harde by the Templeis a fountaincconsecrated to the Sunne,which with the moistureof his water byndeththe ground,and hardnethashes also into a clod, wherin (not without wonder)the placeglittreth rounde about none otherwysethan if it were the greenefields. There is also gatheredthe stone called Ammons horne. For it is sowarpped and crooked that it is shapedlike a Ramshorne. It is bright asgold. Beeing layde under a manneshead when he sleepeth,it is said to representunto him heavenlydreams.2l unfortunately the geology of the oasisdoes not support this association;all its outcrops are of Miocene or younger age.The nearestCretaceous exposures, the youngest rocks in which ammonites occur, are rio miles drstant.2zThis indicatesthat despitethe classical sourcesthe name originated in a generalcontext rather than through occurrencesof the fossilsat Siwa. No meaningful additions to the classicalknowledge of ammonites seem to have been 'Where made prior to the work of the sixteenth-centuryRenaissance naturalists. Ammonis cornu,or one of its variant names,occurs in the medieval lapidariesthe entriesare para- phrasesof Pliny.23Camillo Leonardi's The Mirror of Stones,which in one senserepresents a culmination of the lapidary tradition at the beginningscf the "geological" renaissarlce, contains a description that is strikingly Plinyesque: . Hammonis,is a Stoneof a gold Colour,and is numberedamong the mostsacred Gems. It hasthe shapeof a Ram'sHorn, andis foundtnEthiopia.If a manputs himself in a Postureof Contemplation,it givesthe Mind a Representationof all divine Things.2a AMMONITES: AMMON'S HORNS INTO CEPHALOPODS 3 Agricola's De lt{aturaFossilium2s well illustratesthe effect of the Renaissanceon the geologicalsciences. His mineralogy,based on the physicalcharacters of "fossils",26is free of much of the magical and mythical propertiesand spuriousinformation that character- izesthe earlierlapidaries. Here Ammonisclrnufrom Marienburg is a mineral coveredwith golden armaturct,hard and striated, which imitates a horn.27 Agricola views theseand other stonesas the products of a lapidifying juice, although not necessarilyorganic in nature.28 The lavish useof woodcuts (which had beensupplemented by the useof etchingsafter the middle of the fifteenth century) characterizesmany of Agricola's works; there are some 3oo in De Re Metallicaalone. The use of illustrations for scientific description per- vadesthe treatisesof the sixteenth-centurynatural historians.2eThus the first iliustrations (of varying quality) of many fossils,including ammonires, occur in Konrad Gesner's30 celebratedmineralogical treatise De Rerum Fossilium.Therc is a curious mixture of the organic and inorganic in his rendering of amrnonites. The Cornu serpentisof the four- teenth chapterare describedas Concheaemarinae, stones that imitar. or r.r.rrrble marine animals, along with a fossil fish, a crab (" Pagaruslapideus"), and heart urchins (" Echini marini") that had easilyrecognizable living analogues.Another ammonire is figured and discussedin the following chapter: stoneswhich imitate serpentsand insects.This evolute ammonite,whose coiling type would now be termed "serpenticone",without its wider body whorl and with earlier whorls of rather equal height, must have seemeda perGct petrified serpent to Gesner, and unlike the other conchs which somewhat resembled I'Jautilus.Gesner also describesand illustrates a cidaroid echinoderm as a serpenregg (" auumanguinum"),31 although such".ggr " were correctiyidentified by his "orrt.-por- ary Palissy.32Gesner treats living cephalopodsin the fourth volume of Historia Anima- lium,tncluding in his discussioninformation from the studiesof the FrenchmenGuillaume Rondelet and Pierre Belon, whose ecological view of "poissons" includes these creatures.33l-Jnfortunately they did not discussfossil fish and seemto have hedged on the nature of the fossil invertebratesthey did consider. One of the seventreatises bound with Gesner'sDe Rerum Fossilir,tmis the catalogueof the personalcabinet of Johann Kentmann,34who actually edited the volume. The effect of cataioguesof this type and those of the museumsthat closely followed, nearly all of which included specimensof ammonites, was to popularize the study of lithology throughout Europe during the seventeenthcentury. Fossilscould be cataloguedand pre- servedwith relative easeby the virtuosi, discussedand exchangedwith their fellows, and used to impresstheir friends.
Recommended publications
  • Felix Gradstein, Lames Ogg and Alan Smith 18 the Jurassic Period J
    Felix Gradstein, lames ogg and Alan smith 18 The Jurassic Period J. G. OGG iographic distribution of Jurassic GSSPs that have been ratified (ye Table 18.1 for more extensive listing). GSSPs for the honds) or are candidates (squares) on a mid-Jurassic map base-Jurassic, Late Jurassic stages, and some Middle Jurassic stages PNS in January 2004; see Table 2.3). Overlaps in Europe have are undefined. The projection center is at 30" E to place the center kured some GSSPs, and not all candidate sections are indicated of the continents in the center of the map. basaurs dominated theland surface. Ammonites are themain fossils neously considered his unit to he older. Alexander Brongniart rmrrelatingmarine deposits. Pangea supercontinent began to break (1829) coined the term "Terrains Jurassiques" when correlat- h md at the end of the Middle Jurassic the Central Atlantic was ing the "Jura Kalkstein" to the Lower Oolite Series (now as- m. Organic-rich sediments in several locations eventually became signed to Middle Jurassic) of the British succession. Leopold t source rocks helping to fuel modern civilization. von Buch (1839) established a three-fold subdivision for the Jurassic. The basic framework of von Buch has been retained as the three Jurassic series, although the nomenclature has var- 8.1 HISTORY AND SUBDIVISIONS ied (Black-Brown-White, Lias-Dogger-Malm, and currently L1.1 Overview of the Jurassic Lower-Middle-Upper). The immense wealth of fossils, particularly ammonites, in hc term "Jura Kalkstein" was applied by Alexander von the Jurassic strata of Britain, France, German5 and Switzer- bmholdt (1799) to a series ofcarhonate shelfdeposits exposed land was a magnet for innovative geologists, and modern con- the mountainous Jura region of northernmost Switzerland, cepts of hiostratigraphy, chronostratigraphy, correlation, and d he first recognized that these strata were distinct from paleogeography grew out of their studies.
    [Show full text]
  • Myth and Reality in the Battle Between the Pygmies and the Cranes in the Greek and Roman Worlds
    ARTÍCULOS Gerión. Revista de historia Antigua ISSN: 0213-0181 http://dx.doi.org/10.5209/GERI.56960 Myth and Reality in the Battle between the Pygmies and the Cranes in the Greek and Roman Worlds Asher Ovadiah1; Sonia Mucznik2 Recibido: 19 de septiembre de 2016 / Aceptado: 23 de marzo de 2017 Abstract. Ancient writers, such as Homer, Aesop, Hecataeus of Miletus, Herodotus, Aristotle, Philostratus, Pliny the Elder, Juvenal and others have often referred to the enmity and struggle between the Pygmies and the Cranes. It seems that this folk-tale was conveyed to the Greeks through Egyptian sources. Greek and Roman visual works of art depict the Pygmies fighting against the vigorous and violent attack of the birds, which in some cases was vicious. This article sets out to examine the reasons for the literary and artistic portrayals of the Battle between the Pygmies and the Cranes (Geranomachy) in the context of the migration of the cranes in the autumn from the Caucasus (Scythian plains) to Central (Equatorial) Africa. In addition, an attempt will be made to clarify whether the literary sources and visual works of art reflect myth and/or reality. Keywords: Egypt; Ethiopia; Geranomachy; Migration; Nile; Scythia; Trojans. [en] Mito y realidad en la batalla entre los pigmeos y las grullas en el mundo griego y romano Resumen. Escritores antiguos, tales como Homero, Esopo, Hecateo de Mileto, Herodoto, Aristóteles, Filóstrato, Plinio el Viejo, Juvenal y otros se refirieron frecuentemente a la enemistad y guerra entre los pigmeos y las grullas. Es posible que este cuento popular fuese transmitido a los griegos a través de fuentes egipcias.
    [Show full text]
  • Ichthyosauria, Parvipelvia) from the Lower Jurassic of the Atacama Desert, Northern Chile T
    Journal of South American Earth Sciences 98 (2020) 102459 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames First temnodontosaurid (Ichthyosauria, Parvipelvia) from the Lower Jurassic of the Atacama Desert, northern Chile T ∗ Rodrigo A. Oteroa,b,c, , Patricio Sepúlvedad a Red Paleontológica U-Chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Av. Las Palmeras, 3425, Santiago, Chile b Consultora Paleosuchus Ltda, Huelén 165 Oficina C, Providencia, Santiago, Chile c Museo de Historia Natural y Cultural del Desierto de Atacama, Parque El Loa S/n, Calama, Chile d GeoBlast S.A, Antonio Bellet 444, Oficina 120, Providencia, Santiago, Chile ARTICLE INFO ABSTRACT Keywords: We describe fragmentary ichthyosaur skull remains of a single individual recovered from Lower Jurassic marine Ichthyosauria strata in northern Chile. The preserved teeth display distinctive features such as a very long, robust and coarsely Lower jurassic infolded roots; as well as low, labio-lingually compressed, large triangular crowns with carinae. Dental features south Pangea are consistent with those of the genus Temnodontosaurus, previously known in the Lower Jurassic of Europe. This Paleobiogeography find represent the first record of a temnodontosaurid ichthyosaur in the southern hemisphere, reinforcing a pattern of faunal interchange between the northern Tethys and southern Panthalassa, prior to the separation of Palabras clave: Laurasia and Gondwana, and before the full establishment of the Caribbean Seway. Ichthyosauria Jurásico Inferior Pangea sur RESUMEN Paleobiogeografía Describimos restos craneales fragmentarios de ictiosaurio pertenecientes a un único individuo, recuperado desde estratos marinos del Jurásico Inferior del norte de Chile.
    [Show full text]
  • Parte Seconda Bibliotheca Collinsiana, Seu Catalogus Librorum Antonji Collins Armigeri Ordine Alphabetico Digestus
    Parte seconda Bibliotheca Collinsiana, seu Catalogus Librorum Antonji Collins Armigeri ordine alphabetico digestus Avvertenza La biblioteca non è solo il luogo della tua memoria, dove conservi quel che hai letto, ma il luogo della memoria universale, dove un giorno, nel momento fata- le, potrai trovare quello che altri hanno letto prima di te. Umberto Eco, La memoria vegetale e altri scritti di bibliografia, Milano, Rovello, 2006 Si propone qui un’edizione del catalogo manoscritto della collezione libra- ria di Anthony Collins,1 la cui prima compilazione egli completò nel 1720.2 Nei nove anni successivi tuttavia Collins ampliò enormemente la sua biblioteca, sin quasi a raddoppiarne il numero delle opere. Annotò i nuovi titoli sulle pagine pari del suo catalogo che aveva accortamente riservato a successive integrazio- ni. Dispose le nuove inserzioni in corrispondenza degli autori già schedati, attento a preservare il più possibile l’ordine alfabetico. Questo tuttavia è talora impreciso e discontinuo.3 Le inesattezze, che ricorrono più frequentemente fra i titoli di inclusione più tarda, devono imputarsi alla difficoltà crescente di annotare nel giusto ordine le ingenti e continue acquisizioni. Sono altresì rico- noscibili abrasioni e cancellature ed in alcuni casi, forse per esigenze di spazio, oppure per sostituire i titoli espunti, i lemmi della prima stesura sono frammez- zati da titoli pubblicati in date successive al 1720.4 In appendice al catalogo, due liste confuse di titoli, per la più parte anonimi, si svolgono l’una nelle pagi- ne dispari e l’altra in quelle pari del volume.5 Agli anonimi seguono sparsi altri 1 Sono molto grato a Francesca Gallori e Barbara Maria Graf per aver contribuito alla revi- sione della mia trascrizione con dedizione e generosità.
    [Show full text]
  • General Index
    Cambridge University Press 978-1-107-03398-6 - Man and Animal in Severan Rome: The Literary Imagination of Claudius Aelianus Steven D. Smith Index More information General index Achilles Tatius 5, 6, 31, 47, 49, 56, 95, 213, Atalante 10, 253, 254, 261, 262, 263, 265, 266, 265 267, 268 Aeneas 69, 92, 94, 95, 97 Atargatis 135 Aeschylus 91, 227 Athena 107, 125, 155 Aesop 6, 260 Athenaeus 47, 49, 58, 150, 207, 212, 254 aitnaios 108, 109, 181 Athenians 8, 16, 29, 30, 31, 33, 34, 35, 41, 45, 58, akolasia 41, 43, 183, 279 77, 79, 109, 176, 199, 200, 202, 205, 206, 207, Alciphron 30, 33, 41, 45, 213 210, 227, 251, 252, 253 Alexander of Mundos 129 Athens 55, 60, 79 Alexander Severus 22, 72, 160, 216, 250, 251 Augustus 18, 75, 76, 77, 86, 98, 126, 139, 156, 161, Alexander the Great 58, 79, 109, 162, 165, 168, 170, 215, 216, 234, 238 170, 171, 177, 215, 217, 221, 241, 249 Aulus Gellius 47, 59, 203, 224, 229 Alexandria 23, 47, 48, 49, 149, 160, 162, 163, 164, Aurelian 127 168, 203 Anacreon 20 baboons 151 Androkles 81, 229, 230, 231, 232, 235, 236, 237, Bakhtin, Mikhail 136 247 Barthes, Roland 6 anthias 163, 164 bears 128, 191, 220, 234, 252, 261 ants 96, 250 bees 10, 33, 34, 36, 38, 45, 109, 113, 181, 186, 217, apes 181 218, 219, 220, 221, 222, 223, 224, 225, 242, 246 apheleia 20 beetles 14, 44 Aphrodite 34, 55, 122, 123, 125, 141, 150, 180, 207, Bhabha, Homi 85 210, 255, 256, 259, 260, 263, 267 boars 2, 40, 46, 250, 263 Apion 22, 118, 130, 149, 229, 231, 232 Brisson, Luc 194, 196 Apollo 38, 122, 123, 124, 125, 131, 140, 144, 155, 157, 175, 242, 272
    [Show full text]
  • PDF (Español (España))
    Revista Mexicana de Ciencias Geológicas,Caracterización v. 22, núm. de una 1, 2005,nueva p.localidad 97-114 fosilífera, Temapá Hidalgo 97 Caracterización de una nueva localidad fosilífera del Jurásico Inferior con crinoides y amonites en el centro-oriente de México (Temapá, Hidalgo) Carlos Esquivel-Macías1,*, Rita G. León-Olvera2 y Kinardo Flores-Castro3 1 Centro de Investigaciones Biológicas, Universidad Autónoma de Hidalgo, 42184 Pachuca, México. 2 Investigadora Independiente. Presa Salinillas 17-B-106, Colonia Irrigación, 11200 México D.F., México. 3 Centro de Investigaciones en Ciencias de la Tierra, Universidad Autónoma de Hidalgo, 42184 Pachuca, México. * [email protected] RESUMEN El grupo Huayacocotla es conocido por medio de diversos estudios geológicos y paleontológicos. En el presente trabajo se reporta por primera vez una fauna de amonites (Paltechioceras cf. mexicanum, P. rothpletzi, Ortechioceras incaguasiense, Coroniceras? (Metophioceras) aff. conybeari auct., Phylloceras sp., Sulciferites? cf. stenorhynchus) e isocrínidos bentónicos (Isocrinidae) y pseudoplanctónicos (Pentacrinitidae). Estos últimos representan nuevos registros para sedimentos sinemurianos de México. Se consideran los supuestos hábitos de vida para las familias a las que pertenecen las especies de amonites, como dato de referencia sobre el ambiente de depósito. En este afloramiento también se encuentra el bivalvo Posidontis semiplicata y un gasterópodo no identificado. Hay tres tipos de asociaciones fósiles que se encuentran repetidamente en las capas del afloramiento Temapá, perteneciente a la Formación Despí, de tal forma que es posible reconocerlas (1) por la diferencia de diámetro de los amonites que las componen; (2) por la diferente composición faunística entre ellas, que se demuestra con la aplicación del índice de Simpson; y (3) por el grado de fragmentación de las conchas.
    [Show full text]
  • USGS Professional Paper 1739-E
    Studies by the U.S. Geological Survey in Alaska, 2006 U.S. Geological Survey Professional Paper 1739–E A Major Unconformity Between Permian and Triassic Strata at Cape Kekurnoi, Alaska Peninsula: Old and New Observations on Stratigraphy and Hydrocarbon Potential By Robert B. Blodgett1 and Bryan Sralla2 Abstract reconnaissance and oil and gas prospecting dating back to the early 1900s. The impetus for early geologic interest came from A major angular unconformity separates carbonates the recognition of several broad surface anticlines, along with and shales of the Upper Triassic Kamishak Formation from active oil and gas seeps emerging from Jurassic sandstone and an underlying unnamed sequence of Permian agglomerate, siltstone cropping out along the axis of the anticlines. volcaniclastic rocks (sandstone), and limestone near Puale Bay The internal company report by Hanna and others (1937) on the Alaska Peninsula. For the first time, we photographi- makes it apparent that the thick succession of Upper Trias- cally document the angular unconformity in outcrop, as clearly sic carbonates exposed between Puale and Alinchak Bays exposed in a seacliff ~1.3 mi (2.1 km) west of Cape Kekurnoi on the Pacific side of the Alaska Peninsula, directly across in the Karluk C–4 and C–5 1:63,360-scale quadrangles. This Shelikof Strait from Kodiak Island, Alaska (fig. 1), was of unconformity is also documented by examination of core primary interest early on as an exploration target. Work by chips, ditch cuttings, and (or) open-hole electrical logs in two the Standard Oil Co. of California during the 1930s, along deep oil-and-gas-exploration wells (Humble Oil & Refining with encouragement by the famous Alaska oil prospector Co.’s Bear Creek No.
    [Show full text]
  • Characteristic Jurassic Mollusks from Northern Alaska
    Characteristic Jurassic Mollusks From Northern Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-D Characteristic Jurassic Mollusks From Northern Alaska By RALPH W. IMLAY A SHORTER CONTRIBUTION TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-D A study showing that the northern Alaskan faunal succession agrees with that elsewhere in the Boreal region and in other parts of North America and in northwest Europe UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1955 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - BMMH§ts (paper cover) Price $1.00 CONTENTS Page Abstract_________________ 69 Introduction _________________ 69 Biologic analysis____________ 69 Stratigraphic summary. _______ 70 Ages of fossils________________ 73 Comparisons with other faunas. 75 Ecological considerations___ _ 75 Geographic distribution____. 78 Summary of results ___________ 81 Systematic descriptions__ _. 82 Literature cited____________ 92 Index_____________________ 95 ILLUSTRATIONS [Plates &-13 follow Index] PLATE 8. Inoceramus and Gryphaea 9. Aucella 10. Amaltheus, Dactylioceras, "Arietites," Phylloceras, and Posidonia 11. Ludwigella, Dactylioceras, and Harpoceras. 12. Pseudocadoceras, Arcticoceras, Amoeboceras, Tmetoceras, Coeloceras, and Pseudolioceras 13. Reineckeia, Erycites, and Cylindroteuthis. Page FIGXTKE 20. Index map showing Jurassic fossil collection localities in northern Alaska.
    [Show full text]
  • Note on the Ammonite — Bearing Beds in the Various Localities of Turkey - Part One: Ankara Region
    NOTE ON THE AMMONITE — BEARING BEDS IN THE VARIOUS LOCALITIES OF TURKEY - PART ONE: ANKARA REGION Mükerrem TÜRKÜNAL Mineral Research and Exploration Institute of Turkey INTRODUCTION While working on «The Mono- graphic Revision of the Ammonites Fa- una of Turkey» (to be published later), the author has prepared a note on the Ammonite-bearing beds of Turkey. In this note are assembled the data of the available literature on this subject with the listing of fossil names as given by the authors; the synonyms are given here only for a few well-known species. In the Monography, each of these fos- sils will be fully discussed and all the synonyms of the fossils will be given. In the present note, we are beginning with the beds of the Ankara region. The other localities will be the subject of the following notes. LOCALITY : ANKARA In this district, there are several beds known from the early works. The most important ones will be listed below. A - Balkuyumcu. — In 1887, Tchihatcheff (10) studied first this Jurassic outcrop and found concave-fractured limestone. This limestone contains : A. tortisulcatus (= Sowerbyceras tortisulcatum D'Orb.) A. ardennensis (= Peltoceratoides ardennensis D'Orb.) A. plicatilis (= Perisphenctes plicatilis Sow.) A. tatricus (= Phyllocefas tatricum (Pusch) ?) Age. — Oxfordian. 68 Mükerrem TÜRKÜNAL B - Kesiktaş. — Pompeckj (7), in 1897, made a detailed study of the Juras- sic of Ankara. In his book, he mentioned these fossils : Arietites cf. rotator Reynes A. cf. latesulcatus Quens. Aegoceras sp. aff. brevispinae Sow. Phylloceras alontinum frondosum Reynes Ph. hebertinum Reynes His fossil locality must be wrong. Because, according to several authors, no Jurassic series were encountered in the given locality.
    [Show full text]
  • 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.
    [Show full text]
  • Un Nouveau Genre Et Une Nouvelle Espèce D’Ammonite Micromorphe Dans Le Sinémurien De L’Est De La France (Côte-D’Or)
    Un nouveau genre et une nouvelle espèce d’ammonite micromorphe dans le Sinémurien de l’Est de la France (Côte-d’Or). Jean-Louis Dommergues To cite this version: Jean-Louis Dommergues. Un nouveau genre et une nouvelle espèce d’ammonite micromorphe dans le Sinémurien de l’Est de la France (Côte-d’Or).. Revue de Paléobiologie, Museum d’Histoire Naturelle de la Ville de Geneve, 2015, 34 (1), pp.151-160. 10.5281/zenodo.18905. hal-01184751 HAL Id: hal-01184751 https://hal.archives-ouvertes.fr/hal-01184751 Submitted on 19 Aug 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. REVUE DE VOLUME 34 (1 ) – 2015 PALÉOBIOLOGIE Une institution Ville de Genève www.museum-geneve.ch Revue de Paléobiologie, Genève (juin 2015) 34 (1) : 151-160 ISSN 0253-6730 Un nouveau genre et une nouvelle espèce d’ammonite micromorphe dans le Sinémurien de l’Est de la France (Côte-d’Or) Jean-Louis DOMMERGUES1 1 UFR Sciences de la Vie de la Terre et de l’Environnement, Université de Bourgogne, CNRS/uB, UMR 6282, Biogéo­ sciences Dijon, 6 Boulevard Gabriel, F­21000 Dijon, France.
    [Show full text]
  • PALÄONTOLOGIE Und GEOLOGIE
    BEITRAGE ZUR PALÄONTOLOGIE und GEOLOGIE ÖSTERREICH-UNGARNS und des ORIENTS MITTEILUNGEN DES PALÄONTOLOGISCH EN UND GEOLOGISCHEN INSTITUTES DER UNIVERSITÄT WIEN HERAUSGEGEBEN MIT UNTERSTÜTZUNG DES HOHEN K. K. MINISTERIUMS FÜR KULTUS UND UNTERRICHT VON C A R L D IEN ER , G. v o n ARTHABER, O. PROF. DER PALÄONTOLOGIE A. O. PROF. DER PALÄONTOLOGIE UND F. E. SU ESS, O. PROF. DER GEOLOGIE BAND XXVI MIT XXI TAFELN W IE N und LEIPZIG WILHELM BRAUMÜLLER K. U. K. HOF- UND UNIVERSITÄTS-BUCHHÄNDLER I9<3 INHALT. Heft I und II. Juni 1913. Seile Dr. Otto Haas: Die Fauna des mittleren Lias von Ballino in Südtirol. II. Teil, mit 7 Tafeln (I—V II)..................................................................... ................. I —161 Heft III und IV. März 1914. Dr. Josef Ritter v. Siemiradzki: Die Spongien der polnischen Juraformation. Mit 6 Tafeln, VIII—XIII (I— V I ) ......................................................................................................................... 163—211 Erich Spengler: Nachträge zur Oberkreidefauna des Trichinopoly-Distriktes in Südindien. Mit 2 Tafeln, XIV, XV (I und I I ) ..................................................................... .......................... 213 — 239 Dr. Otto Antonius: Equus Abeli nov. spec. Ein Beitrag zur genaueren Kenntnis unserer Quartärpferde. Mit 6 Tafeln, X V I—XXI (I—V I ) ...................... ...............................241—301 Redigiert von C. Diener, Die Autoren allein sind für Form und Inhalt ihrer Publikationen verantwortlich. DIE FAUNA DES MITTLEREN LIAS VON
    [Show full text]