DOCSLIB.ORG

Ammoniten Mitteljura.Pdf

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Ammoniten Mitteljura.Pdf Lytoceratidae Lytocerataceae LYTOCERATINA: Phylloceratidae Phyllocerataceae PHYLLOCERATINA: informations from Schlegelmilch, R. (1998) jurassic of southern germany. Biostratigraphical data combined by Biostratigraphic distribution of subclass ammonoidea in the middle zusammengestellt nach Angaben aus Schlegelmilch, R. (1998) süddeutschen Mitteljura. Biostratigraphisch Verbreitungsdaten Biostratigraphische Verbreitung der Unterklasse Ammonoidea im Pachylytoceras Pachylytoceras Pachylytoceras Lytoceras Calliphylloceras Lytoceras Lytoceras Sowerbyceras Sowerbyceras Sowerbyceras Holycophylloceras Calliphylloceras Partschiceras taeniatum dilucidum torulosum penicillatum bajociense eudesianum amplum subtortisulcatum ovale antecedens zignodianum disputabile esulcatum 2 (5) 2 (3,4) 2 (2) 1 (8) 1 (2) 2 (1) 1 (9) 1 (7) 1 (6) 1 (5) 1 (4) 1 (3) 1 (1) + + + + + Mittlerer Jura / middle jurassic al 1a alpha + + Unter-Aalenium al 1b beta + al 2a Ober-Aalenium al 2b bj 1a gamma Unter-Bajocium bj 1b bj 1c + + + delta bj 2 + + + Mittel-Bajocium bj 3a1 + + + bj3a2 + + + Ober-Bajocium bj3a3 epsilon + + + bj 3b + + + bj 3c + + + bt 1a + + + Unter-Bathonium bt 1b + + bt 2a + + Mittel-Bathonium bt 2b + + bt 2c + + bt 3a + + Ober-Bathonium bt 3b + + bt 3c + + cl 1a + + Unter-Callovium cl 1b + + + + + cl 2a zeta + + + + + Mittel-Callovium cl 2b + + + + + + cl 3a + + + + + + Ober-Callovium cl 3b Oberer Jura / upper jurassic ox 1a Unter-Oxfordium ox 1b ox 1c alpha Mittel-Oxfordium ox 1d Ober-Oxfordium ox 1e ox 1f ox 2a beta ox 2b ki 1a gamma 1 Unter-Kimmeridgium ki 1b gamma 2 ki 1c gamma 3 ki 1d ki 2a delta Mittel-Kimmeridgium ki 2b ki 3a epsilon Ober-Kimmeridgium ki 3b ki 4 zeta1 ki 5 zeta2 ti 1a zeta 3 Unter-Tithon ti 1b ti 1c Oppeliidae Tmetoceratidae Planammatoceras Hammatoceratinae Hammatoceratidae Hammatocerataceae AMMONITINA: informations from Schlegelmilch, R. (1998) jurassic of southern germany. Biostratigraphical data combined by Biostratigraphic distribution of subclass ammonoidea in the middle zusammengestellt nach Angaben aus Schlegelmilch, R. (1998) süddeutschen Mitteljura. Biostratigraphisch Verbreitungsdaten Biostratigraphische Verbreitung der Unterklasse Ammonoidea im Tmetoceras Erycites Hammatoceras Eudmetoceras Eudmetoceras Planammatoceras (?) Hammatoceras Hammatoceras Pachylytoceras planiforme scissum labrosus sieboldi euaptetum amplectens auerbachense insignoides diadematoides trapeza 3 (5) 4 (1) 2 (6) 4 (3) 4 (2) 3 (4) 3 (3) 3 (2) 3 (1) nicht bekannt + + + Mittlerer Jura / middle jurassic al 1a alpha + Unter-Aalenium al 1b beta + + + al 2a Ober-Aalenium + + + + + al 2b + + + bj 1a gamma + + + Unter-Bajocium bj 1b + + bj 1c delta bj 2 Mittel-Bajocium bj 3a1 bj3a2 Ober-Bajocium bj3a3 epsilon bj 3b bj 3c bt 1a Unter-Bathonium bt 1b bt 2a Mittel-Bathonium bt 2b bt 2c bt 3a Ober-Bathonium bt 3b bt 3c cl 1a Unter-Callovium cl 1b cl 2a zeta Mittel-Callovium cl 2b cl 3a Ober-Callovium cl 3b Oberer Jura / upper jurassic ox 1a Unter-Oxfordium ox 1b ox 1c alpha Mittel-Oxfordium ox 1d Ober-Oxfordium ox 1e ox 1f ox 2a beta ox 2b ki 1a gamma 1 Unter-Kimmeridgium ki 1b gamma 2 ki 1c gamma 3 ki 1d ki 2a delta Mittel-Kimmeridgium ki 2b ki 3a epsilon Ober-Kimmeridgium ki 3b ki 4 zeta1 ki 5 zeta2 ti 1a zeta 3 Unter-Tithon ti 1b ti 1c Hecticoceratinae Oppeliinae informations from Schlegelmilch, R. (1998) jurassic of southern germany. Biostratigraphical data combined by Biostratigraphic distribution of subclass ammonoidea in the middle zusammengestellt nach Angaben aus Schlegelmilch, R. (1998) süddeutschen Mitteljura. Biostratigraphisch Verbreitungsdaten Biostratigraphische Verbreitung der Unterklasse Ammonoidea im Hecticoceras (Hecticoceras) Eohecticoceras Eohecticoceras Prohecticoceras Oecotraustes (Paroecotraustes) Oecotraustes (Paroecotraustes) Oecotraustes (Oecotraustes) Oecotraustes (Oecotraustes) Oecotraustes (Oecotraustes) Oecotraustes (Oecotraustes) Oxycerites Oxycerites Oxycerites Oxycerites Oxycerites Oxycerites Oppelia hecticum biflexuosum primaevum retrocostatum maubeugei juscus decipiens pygmaeus bradleyi nivernensis subcostarius orbis oxus seebachi yeovilensis aspidoides subradiata 6 (2) 6 (1) 5 (13) 5 (12) 5 (11) 5 (10) 5 (9) 5 (8) 5 (7) 5 (6) 5 (5) 5 (4) 5 (3) 5 (2) 5 (1) 4 (5) 4 (4) Mittlerer Jura / middle jurassic al 1a alpha Unter-Aalenium al 1b beta al 2a Ober-Aalenium al 2b bj 1a gamma Unter-Bajocium bj 1b + bj 1c + delta bj 2 + Mittel-Bajocium bj 3a1 + bj3a2 + Ober-Bajocium bj3a3 epsilon bj 3b + bj 3c + + + + + + + + bt 1a Unter-Bathonium bt 1b bt 2a + Mittel-Bathonium bt 2b + bt 2c + + + bt 3a + + Ober-Bathonium bt 3b + bt 3c + + cl 1a + + Unter-Callovium cl 1b + cl 2a zeta + Mittel-Callovium cl 2b + cl 3a + Ober-Callovium cl 3b Oberer Jura / upper jurassic ox 1a Unter-Oxfordium ox 1b ox 1c alpha Mittel-Oxfordium ox 1d Ober-Oxfordium ox 1e ox 1f ox 2a beta ox 2b ki 1a gamma 1 Unter-Kimmeridgium ki 1b gamma 2 ki 1c gamma 3 ki 1d ki 2a delta Mittel-Kimmeridgium ki 2b ki 3a epsilon Ober-Kimmeridgium ki 3b ki 4 zeta1 ki 5 zeta2 ti 1a zeta 3 Unter-Tithon ti 1b ti 1c Hecticoceras (Putealiceras) Hecticoceras (Brightia) informations from Schlegelmilch, R. (1998) jurassic of southern germany. Biostratigraphical data combined by Biostratigraphic distribution of subclass ammonoidea in the middle zusammengestellt nach Angaben aus Schlegelmilch, R. (1998) süddeutschen Mitteljura. Biostratigraphisch Verbreitungsdaten Biostratigraphische Verbreitung der Unterklasse Ammonoidea im Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) Hecticoceras (Brightia) Hecticoceras (Brightia) Hecticoceras (Brightia) Hecticoceras (Brightia) Hecticoceras (Brightia) Hecticoceras (Brightia) Hecticoceras (Brightia) Hecticoceras (Chanasia) Hecticoceras (Chanasia ?) Hecticoceras (Chanasia) Hecticoceras (Chanasia) Hecticoceras (Chanasia) Hecticoceras (Zieteniceras ?) Hecticoceras (Zieteniceras) Hecticoceras (Zieteniceras) Hecticoceras (Zieteniceras) Hecticoceras (Zieteniceras) Hecticoceras (Zieteniceras) Hecticoceras (Zieteniceras) Hecticoceras (Hecticoceras) Hecticoceras (Hecticoceras) punctatum exile nodosum thalheimense punctatum arcuatum punctatum salvadorii difforme tenuinodosum solinophorum prorsosinuatum solinophorum nodosum recurvum nodosum anomalum parallelum keilbergense perlatum aureum inflatum balinense karpinskyi sarasini evolutum tuberculatum zieteni hecticum posterius hecticum boginense 7 (12) 7 (11) 7 (10) 7 (9) 7 (8) 7 (7) 7 (6) 7 (5) 7 (4) 7 (3) 7 (2) 7 (1) 6 (15) 6 (14) 6 (13) 6 (12) 6 (11) 6 (10) 6 (9) 6 (8) 6 (7) 6 (6) 6 (5) 6 (4) 6 (3) Mittlerer Jura / middle jurassic al 1a alpha Unter-Aalenium al 1b beta al 2a Ober-Aalenium al 2b bj 1a gamma Unter-Bajocium bj 1b bj 1c delta bj 2 Mittel-Bajocium bj 3a1 bj3a2 Ober-Bajocium bj3a3 epsilon bj 3b bj 3c bt 1a Unter-Bathonium bt 1b bt 2a Mittel-Bathonium bt 2b bt 2c bt 3a Ober-Bathonium bt 3b bt 3c + + + + + + + + + + cl 1a + + + + + + + + + + + Unter-Callovium cl 1b + + + + + + + + + + ! + + + + + + + cl 2a zeta + + + + + + + + ! + + + + + + + Mittel-Callovium cl 2b + + + + + + + + + cl 3a + + + + + + + + + Ober-Callovium cl 3b Oberer Jura / upper jurassic ox 1a Unter-Oxfordium ox 1b ox 1c alpha Mittel-Oxfordium ox 1d Ober-Oxfordium ox 1e ox 1f ox 2a beta ox 2b ki 1a gamma 1 Unter-Kimmeridgium ki 1b gamma 2 ki 1c gamma 3 ki 1d ki 2a delta Mittel-Kimmeridgium ki 2b ki 3a epsilon Ober-Kimmeridgium ki 3b ki 4 zeta1 ki 5 zeta2 ti 1a zeta 3 Unter-Tithon ti 1b ti 1c Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) informations from Schlegelmilch, R. (1998) jurassic of southern germany. Biostratigraphical data combined by Biostratigraphic distribution of subclass ammonoidea in the middle zusammengestellt nach Angaben aus Schlegelmilch, R. (1998) süddeutschen Mitteljura. Biostratigraphisch Verbreitungsdaten Biostratigraphische Verbreitung der Unterklasse Ammonoidea im Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Lunuloceras) Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) Hecticoceras (Putealiceras) schloenbachi fallax nodosulcatum orbignyi frederici submatheyi michailowense paulowi lunula lunuloides sinuicostatum lunuloides gigas brightii pseudopunctatum subnodosum metomphalum multicostatum metomphalum rossiense robustum inaequifurcatum krakoviense svevum douvillei arkelli 8 (18) 8 (17) 8 (16) 8 (15) 8 (14) 8 (13) 8 (12) 8 (11) 8 (10) 8 (9) 8 (8) 8 (7) 8 (6) 8 (5) 8 (4) 8 (3) 8 (2) 8 (1) 7 (18) 7 (17) 7 (16) 7 (15) 7 (14) 7 (13) Mittlerer Jura / middle jurassic al 1a alpha Unter-Aalenium al 1b beta al 2a Ober-Aalenium al 2b bj 1a gamma Unter-Bajocium bj 1b bj 1c delta bj 2 Mittel-Bajocium bj 3a1 bj3a2 Ober-Bajocium bj3a3 epsilon bj 3b bj 3c bt 1a Unter-Bathonium bt 1b bt 2a Mittel-Bathonium bt 2b bt 2c bt 3a Ober-Bathonium bt 3b bt 3c + + + + + + + + + + + + + + + cl 1a + + + + + + + + + + + + + + + Unter-Callovium cl 1b + + + + + + + + + + + + + + + + + + + + + + + cl 2a zeta + + + + + + + + + + + + + + + + + + + + + + + Mittel-Callovium cl 2b + + + + + + + + + + + + + + + + + + + + + cl 3a + + + + + + + + + + + + + + + + + + + + + Ober-Callovium cl 3b Oberer Jura / upper jurassic ox 1a Unter-Oxfordium ox 1b ox 1c alpha Mittel-Oxfordium
Load more

Recommended publications
  • 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.................................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • "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.
    [Show full text]
  • 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.
    [Show full text]
  • Földtani Közlöny
    Földtani Közlöny A MAGYARHONI FÖLDTANI TÁRSULAT FOLYÓIRATA БЮЛЛЕТЕНЬ ВЕНГЕРСКОГО ГЕОЛОГИЧЕСКОГО ОБЩЕСТВА BULLETIN DE LA SOCIÉTÉ GÉOLOGIQUE DE HONGRIE ZEITSCHRIFT DER UNGARISCHEN GEOLOGISCHEN GESELLSCHAFT BULLETIN OF THE HUNGARIAN GEOLOGICAL SOCIETY T. 105. No. 2. (1975) FÖLDTANI KÖZLÖNY A MAGYARHONI FÖLDTANI TÁRSULAT FOLYÓIRATA 105. KÖTET TARTALOMJEGYZÉK - СОДЕРЖАНИЕ - CONTENU ÉRTEKEZÉSEK — НАУЧНЫЕ СТАТЬИ - MEMOIRES DE. STEGENA L.—DE. GÉCZY В.—HORVÁTH F.: A Pannon-medence késő-kainozóos fejlődése — Evolution néogénique récente du Bassin pannonique 101—123 DR. GÉCZY В.: A magyar őslénytan időszerű problémái 124—128 KOVÁTS L.—DR. NAGY L.: Ujabb észlelések a szilikogén porok DTA vizsgálatában 129—142 NÉMETH MÁRTA: Ujabb mészalgák a Bükk-hegységi középsőkarbonból — Neuere Kalkalgen aus dem Mittel­ karbon des Bükk-Gebirges in Nordungarn 143—154 DR. SIDO MÁRIA: A tatai formáció Foraminiferái (felsőapti) — The Foraminifera of Tata Formation (Upper Aptian) 155—187 DR. В ALDI T. — BÁLDINÉ ВЕКЕ MÁRIA—HORVÁTH MÁRIA—NAGYMAROSI A. —BALOGH K. — SÓS EDIT: Adatok a magyarországi kiscelli agyag abszolút és relatív korához — On the Radiometric Age and the Biostratigraphic Position of the Kiscell Clay in Hungary 188—192 SINGH А. К.: A talajgeokémiai vizsgálatok, mint alkalmazható geokémiai kutató-módszer a rózsabányai területen — Soil analysis as a method of geochemical prospecting in Nagybörzsöny ore deposit, Hungary 193—207 GALÁCZ A.: Bajóci szelvények az Északi Bakonyból — Coupes bajociennes dans le Bakony Septentrional 208—219 DR. T. KOVÁCS G.: A Duna—Tisza köze déli részének miocén képződményei — Das Miozän im Südteil des Donau—Theiss-Zwischenstromlandes 220—236 HÍREK, ISMERTETÉSEK — СООБЩЕНИЯ, РЕЦЕНЗИИ — NOTICES, REVUE BIBLIOGRA­ PHIQUE 237—247 TÁRSULATI ÜGYEK — ДЕЛА ОБЩЕСТВА - AFFAIRES DE LA SOCIÉTÉ 248-255 ÉRTEKEZÉSEK Földtani Közlöny, Bull, of the Hungarian Oeol.
    [Show full text]
  • The Space-Time Relationship of Taxonomic Diversity and Morphological Disparity in the Middle Jurassic Ammonite Radiation ⁎ Sébastien Moyne A, , Pascal Neige B
    Palaeogeography, Palaeoclimatology, Palaeoecology 248 (2007) 82–95 www.elsevier.com/locate/palaeo The space-time relationship of taxonomic diversity and morphological disparity in the Middle Jurassic ammonite radiation ⁎ Sébastien Moyne a, , Pascal Neige b a Centre de Sédimentologie-Paléontologie and FRE CNRS 2761, Université de Provence, Bâtiment de Sciences Naturelles, Case 67, Place Victor Hugo, F-13 331 Marseille cedex 3, France b Centre des Sciences de la Terre and UMR CNRS 5561 Biogéosciences, Université de Bourgogne, 6 bd Gabriel, F-21000 Dijon, France Received 9 May 2006; received in revised form 17 October 2006; accepted 24 November 2006 Abstract The Middle Jurassic ammonite radiation (from the late Aalenian to the end of the mid-Bathonian) is traced using combined analyses of morphological disparity and taxonomic diversity. The global signals of disparity and diversity are compared. These signals are then broken down by paleogeographical provinces to detect any heterogeneity in the radiation. An examination of the global signals reveals three biodiversity crises (discordances between signals) where morphological disparity grows while taxonomic diversity declines. The subdivision of the signals indicates the radiation was heterogeneous between provinces: the global signal is an aggregate of signals from each province. The three biological crises have different paleogeographical signatures: the first is visible in a few provinces only while the other two are visible in most provinces. First-order crises can be distinguished from second-order ones by studying the number of paleogeographical provinces affected. © 2006 Elsevier B.V. All rights reserved. Keywords: Paleogeography; Morphological disparity; Taxonomic diversity; Ammonites; Jurassic 1. Introduction groups of taxa with equal diversity may display very different morphological variability.
    [Show full text]
  • Saint-Julien-En- Genevois, Résulte Du Même Type De Déformation
    SAINT-JULIEN-EN­ GENEVOIS M DONZEAU. R WERNLI. J CHAROLLAIS. G MONJUVENT SAINT-JULIEN-EN-GENEVOIS La carle géologique à 1/50000 SAINT-JULIEN-EN-GENEVOIS est LHG recouverte par les coupures suivantes ~SHGN de la Carle géologique de ta France à 1/80000 --=:-- SIGN au sud-ouest: NANTUA (N° 160) SIEGN au sud-est. ANNECY (N" 160 bis) -.SNHGS au nord-ouest: SAINlCLAUDE iN° 149) DtPARTEMENT Dt; l'imEAIEuA OE l'ENVIRONNEMENT otPAATEMENT OE L1NTERIEUR liT DES IoJ'fAIAES REGIONALES SERVICE MYllflOI-OG>OOE ET au nord-est: THONON (N" 150) SERVICE (;,t,NTOtlAL DE GtOl-OO'E DE GENE~E GEOl-OGIOl)E " ...nONAl ,,",_Son__ CH '~"GE_I·SI.OSSE """"""'IlE""" SUISSE -- ._<:- MINISTÈRE DE L'ÉCONOMIE, --- -- DES FINANCeS ET DE L'INOUSTRIE '...JULIEN _.. BAGM· SERVICE GEOlOGIOUE NATIONAL "-- -- BP 6009· ~5060 ORLI"ANS CEOEX 2· FRANce BRGt,; _.- -- --, NOTICE EXPLICATIVE DE LA FEUILLE SAINT-JULIEN-EN-GENEVOIS À 1/50 000 par M. DONZEAU, R. WERNLI, J. CHAROLLAIS, G. MONJUVENT 1997 Editions du BRGM Service géologique national Références bibliographiques. Toute référence en bibliographie à ce document doit être faite de la façon suivante : pour la carte : DONZEAU M., WERNLIR., CHAROLLAIS J., MONJUVENTG. (1997) — Carte géol. France (1/50 000), feuille Saint-Julien-en-Genevois (653). Orléans : BRGM. Notice explicative par M. Donzeau, R. Wernli, J. Charollais, G. Monjuvent (1997), 144 p. pour la notice : DONZEAU M., WERNLI R., CHAROLLAIS J., MONJUVENT G. (1997) — Notice explicative, Carte géol. France (1/50 000), feuille Saint-Julien-en-Genevois (653). Orléans : BRGM, 144 p. Carte géologique par M. Donzeau, R. Wernli, J.
    [Show full text]
  • О Некоторых Rarecostites (Parkinsoniidae, Ammonoidea) Зоны Parkinsoni Верхнего Байоса Северного Кавказа © 2017 Г
    ПАЛЕОНТОЛОГИЧЕСКИЙ ЖУРНАЛ, 2017, № 5, с. 13–26 УДК 564.53:551.762.22(470.631) О НЕКОТОРЫХ RARECOSTITES (PARKINSONIIDAE, AMMONOIDEA) ЗОНЫ PARKINSONI ВЕРХНЕГО БАЙОСА СЕВЕРНОГО КАВКАЗА © 2017 г. В. В. Митта Палеонтологический институт им. А.А. Борисяка РАН e-mail: [email protected] Поступила в редакцию 21.09.2016 г. Принята к печати 24.10.2016 г. Приведены результаты изучения аммонитов рода Rarecostites подсемейства Parkinsoniinae из ниж- ней части зоны Parkinsonia parkinsoni верхнего байоса р. Кяфар (бассейн р. Большой Зеленчук, Ка- рачаево-Черкесия). Здесь найдены многочисленные раковины микроконхов R. subarietis (Wetzel). Вслед за А. де Гроссувром (de Grossouvre, 1919) названия R. acris (Wetzel) и R. arietis (Wetzel) предла- гается считать субъективными синонимами R. subarietis, с заменой названия стандартной подзоны Acris на Subarietis. В нижней части разреза найдены также многочисленные микроконхи R. sherstyu- kovi sp. nov. и более редкие макроконхи R. kyafarensis sp. nov. Обсуждаются филогенетические взаи- моотношения видов Rarecostites; приведены описания и изображения перечисленных видов, уста- новлены фаунистические горизонты sherstyukovi и subarietis. DOI: 10.7868/S0031031X17050051 ВВЕДЕНИЕ 200 экз. аммонитов рода Parkinsonia (sensu lato). Аммониты семейства Parkinsoniidae широко Коллекция дополнена сборами любителя палеон- распространены по всей северной периферии тологии М.П. Шерстюкова (Ставрополь, Россия) океана Тетис и являются одной из важнейших из этих же местонахождений. Ниже приводятся групп аммонитов для биостратиграфического
    [Show full text]
  • Annual Statement of Reserves 2020 Contents
    ANNUAL STATEMENT OF RESERVES 2020 CONTENTS 1 Classification of Reserves and Contingent Resources 4 2 Reserves, Developed and Non-Developed 5 3 Description of Reserves 11 3.1 Producing Assets 11 3.1.1 Alvheim (PL036, PL088BS, PL203) 11 3.1.2 Vilje (PL036D) 13 3.1.3 Volund (PL150) 14 3.1.4 Bøyla (PL340) 15 3.1.5 Frosk (PL340) 16 3.1.6 Skogul 17 3.1.7 Ivar Aasen Unit and Hanz (Pl001B, PL028B, PL242, PL338BS, PL457) 17 3.1.8 Valhall (PL006B, PL033B) 19 3.1.9 Hod (PL033) 20 3.1.10 Ula (PL019) 21 3.1.11 Tambar (PL065) 22 3.1.12 Tambar East (PL065, PL300, PL019B) 22 3.1.13 Skarv Unit (PL262, PL159, PL212B, PL212) 23 3.1.14 Ærfugl 24 3.1.15 Johan Sverdrup (PL265, PL501, PL502, PL501B) 25 3.1.16 Oda (PL405) 26 3.1.17 Atla (PL102C) 26 3.1.18 Gina Krog (PL029B) 27 3.2 Development Projects 27 3.2.1 Gråsel 27 4 Contingent Resources 28 4.1 Contingent Resources by area 28 4.1.1 The NOAKA Area (North of Alvheim Krafla Askja) 28 4.1.2 Alvheim Area 29 4.1.3 Valhall Area 29 4.1.4 Skarv Area 30 4.1.5 Ula Area 30 4.1.6 Garantiana (PL554) 30 4.1.7 Gohta (PL492) 30 5 Management’s discussion and analysis 31 2 · ANNUAL STATEMENT OF RESERVES · 2020 LIST OF FIGURES Fig. 1.1 SPE reserves and recourses classification system 4 Fig. 3.1 Alvheim and Viper/Kobra location map 11 Fig.
    [Show full text]
  • Ammonites from the Latest Aalenian–Earliest Bathonian of La Baume (Castellane Area, SE France): Palaeontology and Biostratigraphy
    1661-8726/08/030563-16 Swiss J. Geosci. 101 (2008) 563–578 DOI 10.1007/s00015-008-1297-6 Birkhäuser Verlag, Basel, 2008 Ammonites from the latest Aalenian–earliest Bathonian of La Baume (Castellane area, SE France): palaeontology and biostratigraphy KENNETH DE BAETS 1, 2, *, FABRIZIO CECCA 3, MYETTE GUIOMAR 4 & JACQUES VERNIERS 1 Key words: ammonites, Aalenian–Bathonian interval, France, biodiversity, taxonomy, biostratigraphy ABSTRACT Middle Jurassic strata are naturally exposed around the village called La (Parkinsoni Zone) and probably one lower Bathonian Zone (Zigzag Zone) Baume, near Castellane (Alpes de Haute Provence, SE France). We have re- were found. A major gap of both the Niortense Zone and the Garantiana alized both a detailed log and a bed-by-bed sampling for ammonite biostra- Zone, which was not previously described, was detected at the boundary be- tigraphy in a 68 metres thick succession of subpelagic marls and limestones tween members 2 and 3. The main palaeontological interest of the ammonite (“Calcaires à Zoophycos”) that spans the Middle Jurassic from uppermost fauna from La Baume is the richness and diversity of the family Sonniniidae, Aalenian to lowermost Bathonian. The subpelagic succession can be roughly which is the subject of a systematic study and figurated along with some bio- subdivided into three members. Ammonites from the Upper Aalenian Con- stratigraphically significant forms. Biostratigraphical results and open prob- cavum Zone, all Lower Bajocian Zones (Discites Zone, Laeviuscula Zone lems are discussed. including Ovale Subzone, Humpriesianum Zone), one Upper Bajocian Zone Introduction biostratigraphical subdivisions of the geological formations ex- posed. The Jurassic successions in the area of the Réserve Géologique des Alpes de Haute Provence are widely known because of Geological setting the excellent quality of the exposures, the abundance of am- monoids and the easy access.
    [Show full text]
  • Publikationen Mit Beteiligung Von Mitgliedern Der SKJ Im Druck
    Publikationen mit Beteiligung von Mitgliedern der SKJ im Druck Audo, D., Schweigert, G. & Charbonnier, S. (im Druck): Proeryon, the most widespread and long‐lived genus of Polychelidan lobsters. – Annales de Paléontologie Kutz, M., Dietze, V. & Franz, M. (im Druck): Neue Ammonitenfunde aus der Hauptrogenstein‐ Formation (Mittlerer Jura) vom Tuniberg (Oberrheingraben, SW‐Deutschland). – Jahresberichte und Mitteilungen des oberrheinischen geologischen Vereins Dietze, V. & Schweigert, G. (im Druck): Zwei exotische Ammoniten aus dem Ober‐Aalenium (Mittlerer Jura) von Blumberg‐Achdorf (SW‐Deutschland). – Jahreshefte der Gesellschaft für Naturkunde in Württemberg. Dietze, V., Wannenmacher, N. & Schweigert, G. (im Druck): Die Sauzei‐Zone (Mitteljura, Unter‐Bajocium) im Gebiet des Hohenzollern (Schwäbische Alb, SW‐Deutschland). – Zitteliana Schweigert, G., Scherzinger, A. & Lehmkuhl, A. (2020): Eine „verlorene Formation“ – die jüngsten Weißjura‐Relikte der Schwäbischen Alb. – Jahresberichte und Mitteilungen des oberrheinischen geologischen Vereins 2019 Audo, D. & Schweigert, G. (2019): Das Meereskrokodil Pelagosaurus – Kronjuwel einer Fossiliensammlung. – Fossilien, 36 (1): 4‐7. Dietl, G. (2019): Die Ammonitenfauna der Medea‐Subzone (untere Jason‐Zone, Mittel‐ Callovium) aus dem Ornatenton, mittlere Schwäbische Alb, SW‐Deutschland. – Jh. Ges. Naturkde. Württemberg, 175: 129‐148. Dietl, G. & Niederhöfer, H.‐J. (2019): Ein weiterer Beleg für die Medea‐Subzone (untere Jason‐ Zone, Mittel‐Callovium), und zwar aus dem Wartenbergoolith von Geisingen a. d. Donau, ‐ Jh. Ges. Naturkde. Württemberg, 175: 149‐ 158. Dietze, V. & Wannenmacher, N. (2019): Eine Emileia von der Zollernalb – vom Fund zum wissenschaftlichen Beleg. ‐ Fossilien, 36(1): 44–47. Dietze, V. & Hillebrandt, A. (2019): Lower Bajocian (Middle Jurassic) Ammonites of the Manflas area in Atacama Province, Northern Chile, Part 2: Giebeli Zone. ‐ Zitteliana, 93: 25– 46; München.
    [Show full text]
  • Geologica Hungarica. Series Paleontologica
    STRATIGRAPHY MIDDLE JURASSIC PROFILES IN THE VICINITY OF GYENESPUSZTA To explore the Middle Jurassic sediments available (Text-fig. 2), the staff of the Hungarian Geological Institute carried out diggings on six sites in the vicinity of Gyenespuszta farmstead, northern Bakony Mountains, Hungary (Text-fig. 1). Each profile thus exposed comprises a different rock sequence of different facies and with a different fauna. (For the faunal lists and the profiles, see the Hungarian text.) Profile I The Dachstein Limestone is overlain with a hiatus spanning the entire Middle and Upper Liassic and the Lower Dogger, by red nodular limestone beds (Text-fig. 3), with a fauna characteristic of the Upper Bajocian Parkinsonia parkinsoni Zone. Profile II At the base of the profile (Text-fig. 4) the footwall is represented by lowermost Liassic limestones of Dachstein type that are followed by a thin manganiferous layer with ammonites characteristic of the Toarcian Hildaites serpentinum Zone. This is overlain by the Middle Jurassic ammonitico rosso limestone in which the Middle Bathonian Tulites subcontractus Zone and the Upper Bathonian Prohecticoceras retrocostatus Zone could be identified. The hanging-wall is represented by radio- larites. Profiles III and IV The two profiles have exposed a Middle Jurassic rock suit of similar litho- and biofacies, differing from the other Gyenespuszta profiles. The abundance of Bositra is conspicuous. Both lithology and fauna suggest the presence in Profile III of sediments deposited in a submarine fissure (Q fissure, see W e n d t 1971). Both profiles contain a fauna belonging to the Parkinsoni Zone. Profile V The rock types in this profile (Text-fig.
    [Show full text]