DOCSLIB.ORG

Bbm:978-3-8274-3099-1/1.Pdf

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Bbm:978-3-8274-3099-1/1.Pdf 4 Bildtafeln Soweit nicht anders vermerkt, sind aile Aufnahmen in natiirlicher GroBe wiedergegeben. Die Aufnahmen wurden, wenn nicht anders angegeben, vom Verfasser gemacht. Tafel 1 1 Phylloceras (Phylloceras) heterophyllum (SOW.), flachgedriicktes Exemplar aus dem oberen Posidonienschiefer, Holzmaden bei Goppingen; Slg. des Verf., freundlicherweise iiberlassen von Herrn ]. Fischer, Holzmaden; x 0,23 2 Phylloceras (Phylloceras) heterophyllum (SOW.), Lias E, Altdorf bei Niirnberg; Slg. des Verf., freundlicherweise iiberlassen von Herrn G. Engelhardt, Niirnberg 3 Phylloceras (Phylloceras) supraliasicum POMP., LT, oberer Lias S, Reutlingen; Orig. zu Am. heterophyllus SQU. 1885, Taf. 40, Fig. 2; IGPT, Ce 5/4012; x 0,5 4 Phylloceras (Zetoceras) zetes (D'ORB.), Lias 0, Reutlingen; Slg. R. Flaig, Unterensingen bei Niirtingen 5 Sowerbyceras tortisulcoides (QU.), LT, Lias 8, Eislingen/Fils; Orig. zu QU. 1885, Taf. 43, Fig. 15; SMNS; x 2 6 Sowerbyceras tortisulcoides (QU.), Lias 0, Lindenhof bei Schwabisch Gmiind; Slg. F. Sauter, Aalen; x 2 7 Holcophylloceras calypso (D'ORB).), oberer Lias, La Verpilliere bei Lyon (Frankreich); IGPT, 148411 112 Tafel 2 1 Tragophylloceras numismale (POMP.), Lias y, Niirtingen; SMNS 2 Tragophylloceras numismale (POMP.), Lias y, Kirchheim/Teck; Orig. zu POMP. 1893, Taf. 3, Fig. 3, HT von Phylloceras elteni POMP.; SMNS 3 Tragophylloceras paucicostatum (POMP.), HT, Lias y, Kirchheim/Teck; Orig. zu POMP. 1893, Taf. 3, Fig. 2; SMNS 4 Tragophylloceras undulatum (SMITH), Lias y, Fundort unbekannt; IGPT, 148412 5 Tragophylloceras ibex (QU.), Lias y, Niirtingen; Slg. R. Flaig. Unterensingen bei Niirtingen 6 Holcolytoceras nodostrictum (QU.), HT, Lias y, Gomaringen-Hinterweiler bei Tiibingen; Orig. zu QU. 1885, Taf. 33, Fig. 20; SMNS; x 2 7 Holcolytoceras raui WIEDMANN, HT, Lias y, Gomaringen-Hinterweiler bei Tiibingen; Orig. zu WIEDMANN 1970, Taf. 5, Fig. 5; IGPT, 1373/4; x 2 8 Lytoceras fimbriatum (SOW.), Lias y, Heiningen, Krs. Goppingen; Orig. zu Am.lineatus interruptus QU. 1885, Taf. 39, Fig. 8; SMNS 9 Lytoceras fimbriatum (SOW.), Lias y, Dijon (Frankreich); Slg. des Verf. 10 Lytoceras aequistriatum POMP., mittlerer Lias, Fundort unbekannt; Orig. zu POMP. 1896, Taf. 9, Fig. 2; IGPT, Ce P/9/2 114 Tafel 3 1 Lytoceras aequistriatum POMP., HT, Lias y, Reutlingen-Sondelfingen; Orig. zu QU. 1885, Taf. 39, Fig. 6; aus POMP. 1896, Taf. 8, Fig.1 2 Lytoceras salebrosum POMP., LT, Lias ylb, Balingen-Erzingen; Orig. zu Am. lineatus QU. 1885, Taf. 39, Fig. 10; SMNS 3 Lytoceras ceratophagum (QU.), Lias £, Altdorf bei Niirnberg; SMNS 4 Lytoceras cornucopia (Y. & B.), oberer Lias, La Verpilliere bei Lyon (Frankreich); SMNS; x 0,5 5 Lytoceras sublineatum (OPP.), LT, oberes Untertoarcium, Milhaul Aveyron (Frankreich); Orig. zu OPP. 1862, Taf. 43, Fig. 4; BSPG 6 Lytoceras jurense (ZIETEN), Lias " Bisingen/Hohenzollern; Slg. R. Flaig, Unterensingen bei Niirtingen; x 0,75 7 Derolytoceras tortum (QU.), LT, Lias b, Heiningen, Krs. Goppingen; Orig. zu Am. lineatus tortus QU. 1885, Taf. 39, Fig. 12; SMNS; x 2 116 4 Tafel 4 1 Lytoceras siemensi (DENCKMANN), LT, «Posidonienschiefer», Klein Sisbeck bei Helrnstedt; aus DENCKMANN 1887, Taf. 1, Fig. 8; x 0,5 2 Alocolytoceras germaini (D'ORB.), Lias ~, Reutlingen; Orig. zu Am. jurensis interruptus QU. 1885, Taf. 47, Fig. 6; IGPT, Ce 5/4716 3 Alocolytoceras coarctatum (POMP.), Lias~, Reutlingen; Orig. zu Am. interruptus striatus QU. 1885, Taf. 48, Fig. 6; IGPT, Ce 5/48/6 4 Alocolytoceras irregulare (POMP.), Lias ~, Holzrnaden; Orig. zu POMP. 1896, Taf. 11, Fig. 7; IGPT, Ce Plll/7 5 Alocolytoceras irregulare (POMP.), Lias ~, Holzrnaden; Orig. zu POMP. 1896, Taf. 11, Fig. 10; IGPT; Ce PIl1/10 6 Alocolytoceras rugiferum (POMP.), LT, Lias ~, Goppingen-St.Gotthardt; Orig. zu POMP. 1896, Taf. 11, Fig. 1; IGPT, Ce PI 11 11 7 Alocolytoceras rugiferum (POMP.), Lias ~, Bargau; Slg. des Verf. 8 Alocolytoceras wrighti (BUCKM.), Lias ~, Aalen-Weidenfeld; Slg. des Verf. 9 Pleurolytoceras hircinum (SCHLOTH), Lias ~, Neurnarkt/Oberpf.; Slg. des Verf.; x 2 10 Pleurolytoceras propehircinum (KRUMBECK), oberster Lias ~, Pretzfeld bei Forchheirn/Oberfranken; Orig. zu Lytoceras subhircinum KRUMBECK, 1976 vorn Verf. zurn LT bestirnrnt (bisher nicht abgebildet); IGPEN, Slg. KRUMBECK 11 Neophyllites brevicellatus (POMP.), Lias a (Psilonotenbank), Tiibingen; Orig. zu Am. psilonotus nanus QU. 1882, Taf. 1, Fig. lOa; IGPT, Ce 5/1110; x 2 12 Neophyllites antecedens LANGE, HT, unterster Lias a «<Planorbis-Subzone»), Drove bei Diiren; aus LANGE 1941, Taf. 1, Fig. 2 13 Psilophyllites hagenowii (DUNKER), unterster Lias, Halberstadt; Orig. zu QU. 1882, Taf. 1, Fig. 18; IGPT, Ce 5/1/18 14 Psiloceras (Psiloceras) planorbis (SOW.), unterer Lias a, Wiirtternberg; Slg. des Verf. 15 Psiloceras (Psiloceras) plicatulum (POMP.), Lias a (Psilonotenbank), Bebenhausen bei Tiibingen; Orig. zu Am. psilonotus plicatulus QU. 1882, Taf. 1, Fig. 11; IGPT, Ce 5/1/11 118 Tafel 5 1 Psiloceras (Psiloceras) becki (M. SCHMIDT), LT, Lias a (Psilonotenkalk), Bebenhausen bei Tiibingen; Orig. zu M. SCHMIDT 1925, Taf. 1, Fig. 1; SMNS 2 Psiloceras (Psiloceras) calliphylloides POMP., HT, Lias a (Planorbis-Zone), Bebenhausen bei Tiibingen; Orig. zu POMP. 1893, Taf. 5, Fig. 3; IGPT, Ce P/5/3 3 Psiloceras (Psiloceras) distinctum POMP., HT, Lias a, Tiibingen; Orig. zu Am. johnstoni QU. 1882, Taf. 1, Fig. 20; IGPT, Ce 5/1/20 4 Psiloceras (Psiloceras) tenerum (NEUMAYR), unterster Lias, Fonsjoch/ Achensee; Slg. des Verf. 5 Psiloceras (Curviceras) subangulare (OPP.), unterster Lias, Balingen; SMNS (Slg. WAIDELICH) 6 Psiloceras (Curviceras) capraibex POMP., HT, Lias a (Bucklandi-Zone), Jettenburg bei Tiibingen; Orig. zu POMP. 1893, Taf. 5, Fig. 6; IGPT, Ce P/5/6 7 Psiloceras (Caloceras) johnstoni (SOW.), Lias a 1, Tiibingen; Orig. zu Am. psilonotus plicatus QU. 1882, Taf. 1, Fig. 13; IGPT, Ce 5/1/13 8 Psiloceras (Caloceras) johnstoni (SOW.), unterster Lias, Robin Hood's Bay/Yorkshire (England); HT von Am. belcheri SIMPSON; WM 101 9 Psiloceras (Discamphiceras) megastoma (GUMBEL), unterer Lias, Breitenberg (Osterreich. Alpen); Orig. zu BLIND 1963, Taf. 2, Fig. 2; IGPT, 1136/21 10 Psiloceras (Discamphiceras) longipontinum (0. FRAAS), HT, unterer Lias (Planorbis-Zone), Langenbriicken bei Bruchsal; Orig. zu OPP. 1862, Taf. 41, Fig. 1; SMNS 120 Tafel 6 1 Psiloceras (Discamphiceras) nuertingense HOLLAND, HT, Lias, Niirtingen; Orig. zu HOLLAND 1900, Taf. 9, Fig. 1; SMNS; x 0,6 2 Psiloceras (Discamphiceras) harpoptychum HOLLAND, LT, unterster Lias, Niirtingen; Orig. zu HOLLAND 1900, Taf. 8, Fig. 1; SMNS 3 Saxoceras pseudalpinum (POMP.), HT, Lias a (Angulata-Zone), Stuttgart-Vaihingen; Orig. zu POMP., 1893, Taf. 5, Fig. 4; SMNS 4 Schlotheimia angulata (SCHL.), Lias a 2, Oldentrup bei Bielefeld; IGPT, 119115 5 Schlotheimia angulata densicostata LANGE, Lias a 2, Oldentrup bei Bielefeld; Orig. zu BUDWILL 1960, Taf. 18, Fig. 6; IGPT, 1191117 6 Schlotheimia striatissima (QU.), HT, unterer Lias a (Oolithenbank), Bebenhausen bei Tiibingen; Orig. zu QU. 1882, Taf. 3, Fig. 2; IGPT, Ce 5/3/2 7 Schlotheimia polyeides LANGE, Lias a, Mogglingen/Ostalbkreis; Slg. G. Hagele, Ulm/Donau 122 Tafel 7 1 Saxoceras schroederi (LANGE) (extrem weitnabliges Exemplar), Lias a 1, Ttibingen-Pfrondorf; Orig. zu ALTMANN 1964; IGPT, 1266/381 2 Schlotheimia angulosa LANGE, Lias a 2 (Angulata-Zone), Steinlacke, Nordwestdeutschland; aus LANGE 1951, Taf. 4, Fig. 5 3 Schlotheimia depressa (WAHNER), Lias a, Stuttgart-Vaihingen; Orig. zu Am. angulatus depressus QU. 1882, Taf. 2, Fig. 1; IGPT, Ce 5/2/1; x 0,6 4 Schlotheimia depressa (WAHNER), Lisa a «<unmittelbar tiber der Psilonotenbanb), Ttibingen; Orig. zu «Riesenpsilonot» QU 1882, Taf. 3, Fig. 1; IGPT, Ce 5/3/1; x 0,3 5 Schlotheimia hoelderi LANGE, HT, Lias a (untere Arietenschichten), Stuttgart-Vaihingen; Orig. zu HOLDER 1936, Taf. 1, Fig. 2; SMNS; x 2 6 Angulaticeras ventricosum (SOW.), unterer Lias, Coregna bei Spezia (Italien); aus CANAVARl1882, Taf. 18, Fig. 10 7 Angulaticeras angulatoides (QU.), HT, Lias a 3 (Bucklandi-Zone), Balingen-Endingen; aus QU 1882, Taf. 3, Fig. 8 8 Angulaticeras angulatoides (QU.), Lias a (untere Arietenschichten), Stuttgart-Vaihingen; IGPT, 1484/3 124 Tafel 8 1 Schlotheimia germanica LANGE, Lias a 2, Oldentrup bei Bielefeld; Orig. zu BUDWILL 1960, Taf. 19, Fig. 2; IGPT, 1191149 2 Schlotheimia intermedia POMP., unterer Lias a, Balingen-Endingen; Orig. zu Am. angulatus intermedius gigas QU. 1882, Taf. 4, Fig. 1; IGPT, Ce 5/411; x 0,18 3 Angulaticeras ventricosum (SOW.), unterer Lias (Rotiforme-Horizont), Hinter-Mandling bei Radstadt (Osterreich); aus WAH­ NER 1886, Taf. 23, Fig. 11; x 0,8 4 Angulaticeras marmoreum (OPP.), Lias a, Stuttgart-Vaihingen; MSSG; x 0,8 5 Angulaticeras lacunatum (]. BUCKMAN), Lias ~, Hechingen; IGPT, 1484/4; x 2 6 Angulaticeras rump ens (OPP.), Lias ~, Goppingen-Bezgenried; Orig. zu Am. lacunatus rotundus QU. 1884, Taf. 22, Fig. 6; IGPT, Ce 5/22/6; x 2 7 Angulaticeras sulcatum (SIMPSON), HT, unterer Lias, Robin Hood's Bay/Yorkshire (England); WM 743; x 2 8 Angulaticeras sulcatum (SIMPSON), Lias ~, Dewangen bei Aalen; Slg. des Verf.; x 2 126 Tafel 9 1 Angulaticeras charmassei (D'ORB.), Lias lX, Stuttgart-Vaihingen; Orig. zu Am. angulatus compressus QU. 1882, Taf. 2, Fig. 2; IGPT, Ce 51212; x 0,6 2 Angulaticeras martinischmidti (LANGE), unterer Lias lX, Fundort unbekannt; Orig. zu Am. angulatus compressus gigas QU. 1882, Taf. 4, Fig. 2; IGPT, Ce 5/412; x 0,3 3 Angulaticeras deletum (CANAVARI), Oberes Sinemurium (Oxynotum-Zone), Fundort unbekannt; aus WRIGHT 1882, Taf. 56, Fig. 16-18 (HT von Angulaticeras dumortieri) 4 Angulaticeras boucaultianum (D'ORB.), HT, unterer Lias, (Arcuatenkalk), Champlong bei Semur (Frankreich); aus D'ORB. 1844, Taf. 90; x 0,67 5 Angulaticeras densilobatum (POMP.), Lias ~ (Raricostatum-Zone), Goppingen; Orig. zu POMP. 1893, Tat. 6, Fig. 1; IGPT, Ce PI6/1 128 Tafel 10 1 Alsatites laqueus (QU.), HT, Lias a, Bebenhausen bei Tiibingen; Orig. zu QU. 1882, Taf. 1, Fig. 14; IGPT, Ce 5/1/14 2 Alsatites quedlinburgensis LANGE, HT, unterer Lias, Quedlinburg; Orig. zu Am. d. laqueus QU. 1882, Taf. 1, Fig. 15; IGPT, Ce 5/1/15 3 Alsatites sironotus (QU.), HT, Lias a (Oolithenbank), DuBlingen (Wiirtt.); Orig.
Load more

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]
  • ALBIAN AMMONITES of POLAND (Plates 1—25)
    PALAEONTOLOGIA POLQNICA mm ■'Ъ-Ь POL T S H ACADEMY OF SCIENCES INSTITUTE OF PALEOBIOLOGY PALAEONTOLOGIA POLONICA—No. 50, 1990 t h e a l b ia w AMMONITES OF POLAND (AMQNITY ALBU POLS К I) BY RYSZARD MARCINOWSKI AND JOST WIEDMANN (WITH 27 TEXT-FIGURES, 7 TABLES AND 25 PLATES) WARSZAWA —KRAKÔW 1990 PANSTWOWE WYDAWNICTWO NAUKOWE KEDAKTOR — EDITOR JOZEP KA2MIERCZAK 2ASTEPCA HEDAKTOHA _ ASSISTANT EDITOR m AôDAlenA BÛRSUK-BIALYNICKA Adres Redakcjl — Address of the Editorial Office Zaklad Paleobiologij Polska Akademia Nauk 02-089 Warszawa, AI. 2w irki i Wigury 93 KOREKTA Zespol © Copyright by Panstwowe Wydawnictwo Naukowe Warszawa — Krakôw 1990 ISBN 83-01-09176-2 ISSN 0078-8562 Panstwowe Wydawnielwo Naukowe — Oddzial w Krakowie Wydanie 1, Naklad 670 + 65 cgz. Ark. wyd. 15. Ark. druk. 6 + 25 wkladek + 5 wklejek. Papier offset, sat. Ill kl. 120 g. Oddano do skiadania w sierpniu 1988 r. Podpisano do druku w pazdzierniku 1990 r. Druk ukoriczono w listopadzie 1990 r. Zara. 475/87 Drukarnia Uniwersytetu Jagielloriskiego w Krakowie In Memory of Professor Edward Passendorfer (1894— 1984) RYSZARD MARCINOWSKI and JOST WIEDMANN THE ALBIAN AMMONITES OF POLAND (Plates 1—25) MARCINOWSKI, R. and WIEDMANN, J.: The Albian ammonites of Poland. Palaeonlologia Polonica, 50, 3—94, 1990. Taxonomic and ecological analysis of the ammonite assemblages, as well as their general paleogeographical setting, indicate that the Albian deposits in the Polish part of the Central European Basin accumulated under shallow or extremely shallow marine conditions, while those of the High-Tatra Swell were deposited in an open sea environment. The Boreal character of the ammonite faunas in the epicontinental area of Poland and the Tethyan character of those in the Tatra Mountains are evident in the composition of the analyzed assemblages.
    [Show full text]
  • Phylloceratina (Ammonoidea) Del Pliensbachiano Italiano
    00 o Riv. Ital. Paleont. > n . 2 pp. 193-250 tav. 19-20 Milano 1974 PHYLLOCERATINA (AMMONOIDEA) DEL PLIENSBACHIANO ITALIANO N e r in a F a n t i n i S e s t i n i Abstract. This paper concerns thè conclusive researchs on Pliensbachian Phyllo- ceratina from Italy, among which thè genera Geyeroceras Hyatt, 1900 and Partschiceras Fucini, 1923 were already investigated (Fantini Sestini, 1969, 1971). The fossils were collected in stratigraphic sections from Selva di Zandobbio and Alpe Turati in Lombar- dy and from thè M. Nerone area in thè centrai Apennines. They consist of internai moulds and complete shells. The family Juraphyllitidae is present with genera: Jura- phyllites Miiller, Meneghiniceras Hyatt, Harpophylloceras Spath e Galaticeras Spath. Only four genera of Pliensbachian age can be attributed to thè fam. Phylloceratidae; they are as follows: Phylloceras Suess, 1865 with thè two subgenera Phylloceras s.s. e Zetoceras Kovacs, 1939. Test with ornaments visible at low magnification; internai mould smooth, section elliptical, ovai or sublanceolate; E/L and L/U with or without phylloids (minor subdivisions of folioles). Partschiceras Fucini, 1923 ( = Procliviceras Fucini, 1923; Phyllopachyceras Spath, 1925). Test with well distinct riblets, sometimes with ribs and periumbilical ridges; inter­ nai mould with weak constrictions in thè inner whorls and with very weakly outlined ornaments on thè venter; E/L with phylloids; Hantkeniceras Kovacs, 1939 (= Calaiceras Kovacs, 1939). Test smooth; internai mould smooth with rare weak nearly straight constrictions; L/U with 2/3 folioles jointed at their base. Calliphylloceras Spath, 1927. Test with very well developed riblets along with strong rounded ribs; internai mould smooth with 4 to 8 deep arcuate constrictions; L/U with 2 folioles jointed at their base.
    [Show full text]
  • Schmitz, M. D. 2000. Appendix 2: Radioisotopic Ages Used In
    Appendix 2 Radioisotopic ages used in GTS2020 M.D. SCHMITZ 1285 1286 Appendix 2 GTS GTS Sample Locality Lat-Long Lithostratigraphy Age 6 2s 6 2s Age Type 2020 2012 (Ma) analytical total ID ID Period Epoch Age Quaternary À not compiled Neogene À not compiled Pliocene Miocene Paleogene Oligocene Chattian Pg36 biotite-rich layer; PAC- Pieve d’Accinelli section, 43 35040.41vN, Scaglia Cinerea Fm, 42.3 m above base of 26.57 0.02 0.04 206Pb/238U B2 northeastern Apennines, Italy 12 29034.16vE section Rupelian Pg35 Pg20 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 145.8 m above base 31.41 0.03 0.04 206Pb/238U 145.8, equivalent to GSSP), northeastern Apennines, Italy 12 28003.83vE of section MCA/84-3 Pg34 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 142.8 m above base 31.72 0.02 0.04 206Pb/238U 142.8 GSSP), northeastern Apennines, Italy 12 28003.83vE of section Eocene Priabonian Pg33 Pg19 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 14.7 m above base of 34.50 0.04 0.05 206Pb/238U 14.7, equivalent to Ancona, northeastern Apennines, 13.6011 E section MAS/86-14.7 Italy Pg32 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.9 m above base of 34.68 0.04 0.06 206Pb/238U 12.9 Ancona, northeastern Apennines, 13.6011 E section Italy Pg31 Pg18 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.7 m above base of 34.72 0.02 0.04 206Pb/238U
    [Show full text]
  • Les Ammonites Hettangiennes De L'ancienne Mine De Fer De Beauregard
    Les ammonites hettangiennes de l’ancienne mine de fer de Beauregard (Thoste, Côte-d’Or, France). Jean-Louis Dommergues To cite this version: Jean-Louis Dommergues. Les ammonites hettangiennes de l’ancienne mine de fer de Beauregard (Thoste, Côte-d’Or, France).. Revue de Paléobiologie, Museum d’Histoire Naturelle de la Ville de Geneve, 2012, 31 (1), pp.235-265. hal-00741689 HAL Id: hal-00741689 https://hal.archives-ouvertes.fr/hal-00741689 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. 1661-5468 VOL. 31, N° 1, 2012 Revue de Paléobiologie, Genève (juillet 2012) 31 (1) : 235-265 ISSN 0253-6730 Les ammonites hettangiennes de l’ancienne mine de fer de Beauregard (Thoste, Côte-d’Or, France) Jean-Louis DommerGues1 Résumé La faune d’ammonites provenant de l’ancienne mine de fer de Beauregard (Thoste, Côte-d’Or) est révisée. Seuls neuf spécimens issus de cette localité sont actuellement connus. Ils sont conservés dans les collections du Musée de Semur-en-Auxois, du Muséum national d’Histoire naturelle (Paris) et de l’École Nationale Supérieure des Mines (Université Claude Bernard, Lyon 1).
    [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]
  • La Col·Lecció Paleontològica Gómez-Alba Del MGB-MCNB
    Treb. Mus. Geol. Barcelona, 19 (2013): 59-149 La col·lecció paleontològica Gómez-Alba del MGB-MCNB Jaume Gallemí1, Vicent Vicedo1, Gregori López2 i Luis Troya2 Abstract GALLEMÍ, J., VICEDO, V., LÓPEZ, G. & TROYA, L. The Gómez-Alba palaeontological collection of the MGB-MCNB. We present the catalogue of the palaeontological collection belonging to the late Dr. Julio Gómez-Alba, former curator of Palaeontology at Barcelona’s Museum of Geology, now integrated in Barcelona’s Natural History Museum Consortium. He proposed the donation of his collection to the city of Barcelona in November 2010 and the Barcelona’s Institute of Culture (ICUB) accepted it on the 11th February 2011. Formed by 4.990 specimens and 25 batches, it is not the col- lection of a palaeontological researcher but that of a general palaeontologist. Many items in this collection were figured in a field guide authored by Gómez-Alba (1988) dealing with the fossils of Spain and Europe. The catalogue is, apart from some minor corrections, the literal transcription of the database originally associated to the collection that –since its acceptation– has neither been updated nor revised. Key words: catalogue, collection, palaeontology, Gómez-Alba, MGB-MCNB. Resumen GALLEMÍ, J., VICEDO, V., LÓPEZ, G. y TROYA, L. La colección paleontológica Gómez-Alba del MGB-MCNB. Se presenta el catálogo de la colección paleontológica que había pertenecido al recientemente fallecido Dr. Julio Gómez-Alba, antiguo conservador de Paleontología del Museo de Geología de Barcelona, actualmente integrado en el Consorcio del Museo de Ciencias Naturales de Barcelona. La propuesta de donación de la colección a la ciudad de Barcelona se realizó en noviembre de 2010 y fue aceptada por el Instituto de Cultura de Barcelona (ICUB) en fecha 11 de febrero de 2011.
    [Show full text]
  • AALENIAN TMETOCERAS (AMMONOIDEA) from IBERIA Taxonomy, Habitats, and Evolution
    AALENIAN TMETOCERAS (AMMONOIDEA) FROM IBERIA Taxonomy, Habitats, and Evolution 1 2 3 S. R. Femandez-L6pez, M. H. Henriques, A. Linares, 1. Sandovae and M. S. Ureta1 'Dept. y UEI de Paleontologia Facultad de Ciencias Geo16gicas (UCM) elnstitutode Geologia Econ6mica (CSIC-UCM) 28040-Madrid, Spain 2Dept. Ci€mcias da Terra Centro de Geociencias Universidade de Coimbra 3049-Coimbra Codex, Portugal 3Dept. de Estratigrafia y Paleontologia Facultad de Ciencias Universidad de Granada 18071 Granada, Spain Abstract Several hundred Aalenian Tmetoceras from the Iberian Peninsula (N Lusitanian Basin, As­ turias, Basque-Cantabrian Basin, NE Cameros, NW Iberian Basin, Aragonese Platform, Tortosa Platform, Castilian Platform, Majorca and Betic Basin) have been reviewed. Two species of Aalenian Tmetoceras have been identified on the basis of morphological, bio­ chronological and palaeobiogeographical data: T. scissum and T. regleyi. T. scissum was dominant among the Tmetoceras populations developed in the Betic and Lusitanian basins during Opalinum, Murchisonae and Bradfordensis biochrons. Popu­ lations coniposed by evolute individuals of T. scissum inhabited shelfal or oceanic envi­ ronments. A chronocline, from rectiradiate and primitive forms to flexicostate and derived forms, can be recognized in these populations of T. scissum. In contrast, shallow epiconti­ nental platforms were inhabited by involute individuals of T. regleyi. This second species was phyletically derived from T. scissum, representing an adaptive radiation from popula­ tions of shelfal or oceanic basins to populations of epicontinental platforms. Asturias L��---:T NW Iberian Basin 14--=--�- Aragonese Platform +--Tortosa Platform 0� q@ Majorca SE Castilian Platform Central Castilian Platform Oriental sector of Median Subbetic Basin 250 km I Central sector with condensed sections of Median Subbetic Basin External Subbetic Basin Central sector with expanded sections of Median Subbetic Basin Figure 1.
    [Show full text]
  • Paléontologie Au Luxembourg (2) A
    Paléontologie au Luxembourg (2) A. Di Cencio, D. Sadki, R. Weis (eds.) R. Weis D. Sadki, A. Di Cencio, Les ammonites de la Minette Andrea Di Cencio, Driss Sadki, Paléontologie au Luxembourg (2) Luxembourg au Paléontologie Robert Weis (eds.) Ferrantia Travaux scientifiques du Musée national d'histoire naturelle Luxembourg www.mnhn.lu 83 2020 Ferrantia 83 2020 2020 83 Ferrantia est une revue publiée à intervalles non réguliers par le Musée national d’histoire naturelle à Luxembourg. Elle fait suite, avec la même tomaison, aux T M ’ L parus entre 1981 et 1999. Comité de rédaction: Eric Buttini Guy Colling Alain Frantz Thierry Helminger Ben Thuy Mise en page: Romain Bei Design: Thierry Helminger Prix du volume: 20 € Rédaction: Échange: Musée national d’histoire naturelle Exchange MnhnL Rédaction Ferrantia c/o Musée national d’histoire naturelle 25, rue Münster 25, rue Münster L-2160 Luxembourg L-2160 Luxembourg Tél +352 46 22 33 - 1 Tél +352 46 22 33 - 1 Fax +352 46 38 48 Fax +352 46 38 48 Internet: http://www.mnhn.lu/ferrantia/ Internet: http://www.mnhnl.lu/biblio/exchange email: [email protected] email: [email protected] Page de couverture: Bredyia subinsignis (Oppel, 1856), DOU833. Natural History Museum of Luxembourg. Citation: Di Cencio A., Sadki D., Weis R. (eds.) 2020. - Paléontologie au Luxembourg (2) - Les ammonites de la Minette. Ferrantia 83, Musée national d’histoire naturelle, Luxembourg, 129 p. Date de publication: 15 décembre 2020 (réception du manuscrit: 19 mai 2020) Impression: Imprimerie Centrale climatiquement neutre Impression | LU-319-JR8FDJV | www.natureOffice.com Ferrantia est publiée sous la licence Creative Commons BY-NC-ND 3.0 LU.
    [Show full text]
  • Late Jurassic Ammonites from Alaska
    Late Jurassic Ammonites From Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 1190 Late Jurassic Ammonites From Alaska By RALPH W. IMLAY GEOLOGICAL SURVEY PROFESSIONAL PAPER 1190 Studies of the Late jurassic ammonites of Alaska enables fairly close age determinations and correlations to be made with Upper Jurassic ammonite and stratigraphic sequences elsewhere in the world UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress catalog-card No. 81-600164 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page Page Abstract ----------------------------------------- 1 Ages and correlations -----------------------------­ 19 19 Introduction -------------------------------------- 2 Early to early middle Oxfordian --------------­ Biologic analysis _________________________________ _ 14 Late middle Oxfordian to early late Kimmeridgian 20 Latest Kimmeridgian and early Tithonian _____ _ 21 Biostratigraphic summary ------------------------- 14 Late Tithonian ______________________________ _ 21 ~ortheastern Alaska -------------------------­ 14 Ammonite faunal setting --------------------------­ 22 Wrangell Mountains -------------------------- 15 Geographic distribution ---------------------------- 23 Talkeetna Mountains -------------------------­ 17 Systematic descriptions ___________________________ _ 28 Tuxedni Bay-Iniskin Bay area ----------------- 17 References
    [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]
  • 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]