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Представители Семейства Bochianitidae (Ammonoidea) Из Нижнего Мела Горного Крыма © 2008 Г
ПАЛЕОНТОЛОГИЧЕСКИЙ ЖУРНАЛ, 2008, № 5, с. 18-26 УДК 564.5:551.76(477.9) ПРЕДСТАВИТЕЛИ СЕМЕЙСТВА BOCHIANITIDAE (AMMONOIDEA) ИЗ НИЖНЕГО МЕЛА ГОРНОГО КРЫМА © 2008 г. В. В. Аркадьев Санкт-Петербургский государственный университет e-mail: [email protected] Поступила в редакцию 10.04.2007 г. Принята к печати 21.06.2007 г. Приведены результаты ревизии гетероморфньгх аммонитов семейства Bochianitidae из нижнего ме ла Горного Крыма. Автором подтверждена валидность рода Janenschites, выделенного из рода Bo- chianites. Из берриаса Горного Крыма описаны виды Bochianites neocomiensis (d'Orbigny), В. goubech- ensis Mandov, В. levis sp. nov. и В. crymensis sp. nov., из нижнего баррема - виды Janenschites oosteri (Sarasin et Schondelmayer) и J. incisus sp. nov. Бохианиты, появившись в начале берриаса в южных обла стях (Африка, Крым), в валанжине и готериве распространились в северные районы Западной Европы. Гетероморфные аммониты рода Bochianites тарктиды (Kelly, 1995; Lomas, 1999) и Новой Гви¬ редко встречаются в нижнемеловых отложениях неи (Benson, 1923). Горного Крыма. До настоящего времени из этого В последнее время вид В. cf. neocomiensis най региона было описано лишь два вида - Bochianites ден в пограничных отложениях валанжина - готе- oosteri и В. neocomiensis (Каракаш, 1907). Между рива Большого Кавказа (Захаров и др., 2006). тем, представители этого рода занимают значи¬ Крымские бохианиты после Н.И. Каракаша тельное место в нижнемеловых (в частности (1907) никем не изучались. Этот исследователь верхневаланжинских) аммонитовых комплексах виды B. neocomiensis и В. oosteri определил и опи¬ западной части Тетической области (Сесса, 1998; сал из красных известняков разреза на р. Кача в Lukeneder, 2005). Географическое распростране¬ Горном Крыму. Е.Ю. Барабошкин (1997) данный ние рода Bochianites чрезвычайно широкое. -
Symposium I: Evolution O the Depositional Systems
9 SYMPOSIUM I: EVOLUTION O THE DEPOSITIONAL SYSTEMS MINERALOGICAL CHARACTERIZATION increase of siliciclastic sedimentation with the progressive shallow- O LYSCH SEQUENCES O THE SE ALPS ing of the basin from deep-sea to delta facies. In the Vipava lysch (VI) carbonates are predominant. In the lysch of Brkini (BK) the AND OUTER DINARIDES (NE ITALY, mineral content is similar to that of the coeval sandstones in the JB. SLOVENIA, CROATIA) Dolomite appears only in the molasse samples. In the Istrian Basin (IB) no clear trend is noticed. In the western part the siliciclastic material content is higher than in the eastern part (ig. 2). A. ALBERTI1, D. LENAZ 1, . PRINCIVALLE 1 As for heavy minerals, Cr-spinel, garnet (pyralspite and gran- and G. TUNIS 2 dite series), zircon, tourmaline, rutile, pyrite, chloritoid, pyroxene (opx and cpx), staurolite and amphibole were identified, but their 1Dipartimento di Scienze della Terra, Via Weiss 8, 34127 Trieste, Italy 2Dipartimento di Scienze Geologiche, Ambientali e Marine, Via Weiss 2, 34127 Trieste, Italy; *[email protected] Key words: lysch, X-ray powder diffraction, heavy mineral assemblage, source areas. Introduction An extensive lysch complex of Late Cretaceous to Early Ter- tiary age outcrops in north-eastern Italy, western Slovenia and Is- tria (Croatia) (ig. 1). The rock sequences belong to different dep- ositional basins and have different ages. Sedimentation in the basins of the northern part of the complex (Slovenia and riuli) occurred from the Maastrichtian to Middle Eocene (Engel 1974; Tunis & Venturini 1989), while in the southern part (Trieste, SW Slovenia and Istria) it took place from the Middle to Late Eocene (Marincic et al. -
Stratigraphic Constraints on the Late Jurassic–Cretaceous Paleotectonic Interpretations of the Placetas Belt in Cuba, in C
Pszczo´łkowski, A., and R. Myczyn´ ski, 2003, Stratigraphic constraints on the Late Jurassic–Cretaceous paleotectonic interpretations of the Placetas belt in Cuba, in C. Bartolini, R. T. Buffler, and J. Blickwede, eds., The Circum-Gulf of Mexico and the Caribbean: Hydrocarbon habitats, basin 25 formation, and plate tectonics: AAPG Memoir 79, p. 545–581. Stratigraphic Constraints on the Late Jurassic–Cretaceous Paleotectonic Interpretations of the Placetas Belt in Cuba Andrzej Pszczo´łkowski Institute of Geological Sciences, Polish Academy of Sciences, Warszawa, Poland Ryszard Myczyn´ski Institute of Geological Sciences, Polish Academy of Sciences, Warszawa, Poland ABSTRACT he Placetas belt in north-central Cuba consists of Late Jurassic–Cretaceous rocks that were highly deformed during the Paleocene to middle Eocene T arc-continent collision. The Late Proterozoic marble and Middle Jurassic granite are covered by the shallow-marine arkosic clastic rocks of late Middle Jurassic(?) or earliest Late Jurassic(?) ages. These arkosic rocks may be older than the transgressive arkosic deposits of the Late Jurassic–earliest Cretaceous Con- stancia Formation. The Berriasian age of the upper part of the Constancia For- mation in some outcrops at Sierra Morena and in the Jarahueca area does not confirm the Late Jurassic (pre-Tithonian) age of all deposits of this unit in the Placetas belt. The Tithonian and Berriasian ammonite assemblages are similar in the Placetas belt of north-central Cuba and the Guaniguanico successions in western Cuba. We conclude that in all paleotectonic interpretations, the Placetas, Camajuanı´, and Guaniguanico stratigraphic successions should be considered as biogeographically and paleogeographically coupled during the Tithonian and the entire Cretaceous. -
Guidebook for the Post-Congress Fieldtrip in the Vocontian Basin, SE France (September 11-13, 2008)
12th Meeting of the International Nannoplankton Association (Lyon, September 7-10, 2008) Guidebook for the post-congress fieldtrip in the Vocontian Basin, SE France (September 11-13, 2008) Emanuela MATTIOLI (special editor), Silvia GARDIN, Fabienne GIRAUD, Davide OLIVERO, Bernard PITTET & Stéphane REBOULET ISBN 978-2-916733-02-9 Dépôt légal à parution Manuscrit en ligne depuis le 7 Septembre 2008 Manuscript online since September 7, 2008 Carnets de Géologie / Notebooks on Geology - Book 2008/01 (CG2008_BOOK_01) Guidebook for the post-congress fieldtrip in the Vocontian Basin, SE France (September 11-13, 2008) Emanuela MATTIOLI (special editor) 1,2, Silvia GARDIN 3, Fabienne GIRAUD 1, Davide OLIVERO 1, Bernard PITTET 1 & Stéphane REBOULET 1 1 UMR 5125 PEPS (CNRS), Université Lyon 1, Campus de la DOUA, Bâtiment Géode, 69622 Villeurbanne Cedex (France) 2 [email protected] 3 UMR 5143 (CNRS), Université Pierre et Marie Curie, Paris 6, 75013 Paris (France) Manuscript online since September 7, 2008 1 Carnets de Géologie / Notebooks on Geology - Book 2008/01 (CG2008_BOOK_01) Chapter 1. The Aalenian-Bajocian northward, with many hiatuses (JAUTÉE, 1984). (Middle Jurassic) of the Digne Basinal facies, represented by marl-limestone alternations, are recorded in the southernmost area areas but in the sector south of the Verdon Davide OLIVERO with the contribution of River a shallow-water platform developed, Emanuela MATTIOLI documented by the occurrence of bioclastic limestones with corals. This development is Geographical and geological context evidence of a progressive extension to the Provence platform southward. The Digne area is located in southeastern France (Fig. 1.1), in the department of "Alpes In the Middle Jurassic, the central part of the de Haute-Provence". -
Jurassic-Cretaceous Tectonic and Depositional Evolution of the Forearc
International Geology Review ISSN: 0020-6814 (Print) 1938-2839 (Online) Journal homepage: https://tandfonline.com/loi/tigr20 The Byers Basin: Jurassic-Cretaceous tectonic and depositional evolution of the forearc deposits of the South Shetland Islands and its implications for the northern Antarctic Peninsula Joaquin Bastias, Mauricio Calderón, Lea Israel, Francisco Hervé, Richard Spikings, Robert Pankhurst, Paula Castillo, Mark Fanning & Raúl Ugalde To cite this article: Joaquin Bastias, Mauricio Calderón, Lea Israel, Francisco Hervé, Richard Spikings, Robert Pankhurst, Paula Castillo, Mark Fanning & Raúl Ugalde (2019): The Byers Basin: Jurassic-Cretaceous tectonic and depositional evolution of the forearc deposits of the South Shetland Islands and its implications for the northern Antarctic Peninsula, International Geology Review, DOI: 10.1080/00206814.2019.1655669 To link to this article: https://doi.org/10.1080/00206814.2019.1655669 View supplementary material Published online: 21 Aug 2019. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://tandfonline.com/action/journalInformation?journalCode=tigr20 INTERNATIONAL GEOLOGY REVIEW https://doi.org/10.1080/00206814.2019.1655669 ARTICLE The Byers Basin: Jurassic-Cretaceous tectonic and depositional evolution of the forearc deposits of the South Shetland Islands and its implications for the northern Antarctic Peninsula Joaquin Bastias a,b, Mauricio Calderónc, Lea Israela, Francisco Hervéa,c, Richard -
First Record of Duvaliaex. Gr. Lata(Cephalopoda, Coleoidea) From
First record of Duvalia ex. gr. lata (Cephalopoda, Coleiodea) from Mexico 527 BOLETÍN DE LA SOCIEDAD GEOLÓGICA MEXICANA VOLUMEN 65, NÚM. 3, 2013, P. 527-531 D GEOL DA Ó E G I I C C O A S 1904 M 2004 . C EX . ICANA A C i e n A ñ o s First record of Duvalia ex. gr. lata (Cephalopoda, Coleoidea) from Mexico Patrick Zell1,*, Seija Beckmann1, Wolfgang Stinnesbeck1, José Flores-Ventura2 1 Institute for Earth Sciences, Heidelberg University, Im Neuenheimer Feld 234, 69120 Heidelberg, Germany. 2 Santa Engracia 257, Fracc. Santa Elena, Saltillo C.P. 25015, Coahuila, México. * [email protected] Abstract Here we present the first record of the belemniteDuvalia ex. gr. lata (Cephalopoda, Coleoidea) from Mexico. The unique individual, a well-preserved rostrum, was discovered in Early Cretaceous strata of the Sierra de Parras close to Viesca in southwestern Coahuila. Duvalia ex. gr. lata was previously known from the Mediterranean Tethys. Our report extends the paleogeographic distribution of Duvalia to the western hemisphere and supports the hypothesis that the Hispanic Corridor was open during the Early Cretaceous, allowing for marine faunal exchange and migration between the Gulf of Mexico and the European Tethys. Keywords: Duvalia, belemnite, Early Cretaceous, Mexico, Hispanic Corridor. Resumen Se reporta por primera vez el belemnite Duvalia ex. gr. lata (Cephalopoda, Coleoidea) en México. El único ejemplar, un rostro bien preservado, ha sido descubierto en capas del Cretácico Temprano de la Sierra de Parras,en las cercanías de Viesca, en el suroeste de Coahuila. Previamente, se conocía a Duvalia ex. -
Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
Barremian Ammonoids from Serre De Bleyton (Drôme, SE France)
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Annalen des Naturhistorischen Museums in Wien Jahr/Year: 2010 Band/Volume: 112A Autor(en)/Author(s): Lukeneder Alexander Artikel/Article: Barremian ammonoids from Serre de Bleyton (Drôme, SE France). 613- 626 ©Naturhistorisches Museum Wien, download unter www.biologiezentrum.at Ann. Naturhist. Mus. Wien, Serie A 112 613-626 Wien, Juni 2010 Barremian ammonoids from Serre de Bleyton (Drôme, SE France) By Alexander LUKENEDER (With 4 figures) Manuscript submitted on September 18th 2009, the revised manuscript on December 7th 2009 Abstract Barremian ammonoids were collected at the Serre de Bleyton locality in the Department Drôme, SE France. The cephalopod fauna from the “coulées boueuses”, correlated with other macrofossil groups (belemnitoids, brachiopods, crinoids, echinoids etc.) and microfossil data (foraminifera) from the turbiditic unit, indicates Barremian age. The deposition of the allodapic limestones and marls in this interval occurred during depositionally unstable conditions which led to the forma- tion of turbiditic layers. The ammonoid fauna comprises 8 different genera, each apparently represented by a single spe- cies. The assemblage at the Serre de Bleyton section is dominated by ammonoids of the Melchior- ites-type. Ammonitina are the most frequent component (Melchiorites 52%; Holcodiscus 8%), followed by the Phylloceratina (Phyllopachyceras 3% and Hypophylloceras 2%), the Lytoceratina (Protetragonites 15%), and the Ancyloceratina (Anahamulina 10%, Karsteniceras 8% and Mac- roscaphites 2%). The ammonoid fauna consists solely of Mediterranean elements. Keywords: Cephalopoda, Ammonoidea, Barremian, Serre de Bleyton, SE France. Zusammenfassung Ammoniten aus dem Barremium wurden an der Lokalität Serre de Bleyton im Distrikt Drôme, Südost-Frankreich, aufgesammelt. -
Abstract Volume
Subcommission on Cretaceous Stratigraphy (SCS) Second International Symposium on CRETACEOUS STAGE BOUNDARIES Brussels 8 - 16 September 1995 ABSTRACT VOLUME lnstitut royal des Sciences Naturelles de Belgique (I.R.Sc.N.B.) Koninklijk Belgisch lnstituut voor Natuurwetenschappen (K.B.I.N.) Vautierstraot 29, B- 1040 Brussels, BELGIUM Telefox XX- 32-2-646 44 33 Telephone XX- 32-2-627 44 92 JA;· �)I ,., lOOMY. CRETACEOUS STME Jl'lUkliHIU CONTENTS Table of Contents Ill Foreword V Abstracts - papers and posters 1 Reports of the Stage Working Groups 137 - Berriasian 137 - Valanginian 139 - Hauterivian 140 - Barremian 142 - Aptian 144 - Albian 146 - Cenomanian 148 - Tu ronian 150 - Coniacian 153 - Santonian 156 - Campanian 159 - Maastrichtian 162 Abstracts - papers and posters latest arrivals 165 FOREWORD The abstract volume of the Second International Symposium on Cretaceous Stages Boundaries contains reports of the Stage working group chairmen (or to be correct one chairwoman and 11 chairmen) and abstracts of papers (77) and posters (75), represent ing the Cretaceous under most aspects and from almost everywhere on earth. All reports, papers and posters, shall be presented and discussed during the four days of the symposium at the lnstitut royal des Sciences Naturelles/ Koninklijk Belgisch lnstituut voor Natuurwetenschappen in Brussels. We hope that many precise proposals on stage and substage boundaries shall result from these discussions. The organisation of the meeting has only been made possible by generous assistance from the Services Federaux des Affaires Scientifiques, Techniques et Culturelles (Service des Etablissements scientifiques federaux)/ Federate Diensten voor Wetenschappelijke, Technische en Culturele Aangelegenheden (Dienst van de federate wetenschappelijke instellingen) (Brussels), the Nationaal Fends voor Wetenschappelijk Onderzoek (Brus sels), Exekutive der Deutschsprachige Gemeinschaft (Eupen), Societe Generate de Banque (Brussels) and, last but not least, from D. -
Xh Ieuican%Mllisdllm 1Soxftates PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET, NEW YORK 24, N.Y
Xh ieuican%Mllisdllm 1Soxftates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK 24, N.Y. NUMBER 2005 JUNE 15, 1960 Lower Cretaceous Ammonites from Colombia, South America BY OTTO HAAS INTRODUCTION The present paper attempts to summarize the paleontological re- sults of an investigation carried out early in 1956, under the sponsor- ship of International Petroleum (Colombia), Ltd., in the Cordillera Oriental of Colombia for the purpose of clarifying and refining the lower Cretaceous stratigraphy of that region. I am indebted to the company for permission to publish this paper and to utilize photo- graphs made at the company's expense, and to Prof. Gerardo Botero Arango of the Facultad Nacional de Minas of Medellin, Colombia, for permission to describe specimens collected on a field trip of that institution and now deposited in its collections. For the repositories of illustrated specimens, reference is made to the legends of the figures accompanying the present report; there "I.P." indicates the collec- tions of International Petroleum (Colombia), Ltd., in Bogota and "F.N.M." those of the Facultad Nacional de Minas in Medellin. In addition to most of the forms recognized among the abundant ammonites collected in the course of the above investigation, some interesting specimens that had been in the company's collections earlier are also included in the present report. Unfortunately most of the ammonites here described, especially those preserved in shales, are crushed and flattened or otherwise dis- torted; venters can be examined only exceptionally and even more rarely can suture lines be observed. -
Paleontological Contributions
THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS May 15, 1970 Paper 47 SIGNIFICANCE OF SUTURES IN PHYLOGENY OF AMMONOIDEA JURGEN KULLMANN AND JOST WIEDMANN Universinit Tubingen, Germany ABSTRACT Because of their complex structure ammonoid sutures offer best possibilities for the recognition of homologies. Sutures comprise a set of individual elements, which may be changed during the course of ontogeny and phylogeny as a result of heterotopy, hetero- morphy, and heterochrony. By means of a morphogenetic symbol terminology, sutural formulas may be established which show the composition of adult sutures as well as their ontogenetic development. WEDEKIND ' S terminology system is preferred because it is the oldest and morphogenetically the most consequent, whereas RUZHENTSEV ' S system seems to be inadequate because of its usage of different symbols for homologous elements. WEDEKIND ' S system includes only five symbols: E (for external lobe), L (for lateral lobe), I (for internal lobe), A (for adventitious lobe), U (for umbilical lobe). Investigations on ontogenetic development show that all taxonomic groups of the entire superorder Ammonoidea can be compared one with another by means of their sutural development, expressed by their sutural formulas. Most of the higher and many of the lower taxa can be solely characterized and arranged in phylogenetic relationship by use of their sutural formulas. INTRODUCTION Today very few ammonoid workers doubt the (e.g., conch shape, sculpture, growth lines) rep- importance of sutures as indication of ammonoid resent less complicated structures; therefore, phylogeny. The considerable advances in our numerous homeomorphs restrict the usefulness of knowledge of ammonoid evolution during recent these features for phylogenetic investigations. -
The Valanginian Olcostephaninae Haug, 1910 (Ammonoidea) from the Andean Lower Cretaceous Chañarcillo Basin, Northern Chile Andean Geology, Vol
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Amaro Mourgues, Francisco; Bulot, Luc G.; Frau, Camille The Valanginian Olcostephaninae Haug, 1910 (Ammonoidea) from the Andean Lower Cretaceous Chañarcillo Basin, Northern Chile Andean Geology, vol. 42, núm. 2, mayo, 2015, pp. 213-236 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173938242004 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Geology 42 (2): 213-236. May, 2015 Andean Geology doi: 10.5027/andgeoV42n2-a04 www.andeangeology.cl The Valanginian Olcostephaninae Haug, 1910 (Ammonoidea) from the Andean Lower Cretaceous Chañarcillo Basin, Northern Chile *Francisco Amaro Mourgues1, 2, Luc G. Bulot3, Camille Frau4 1 IRD-LMTG Observatoire Midi-Pyrénées, 14 Avenue Edouard Belin, 31400 Toulouse, France. 2 Servicio Nacional de Geología y Mineraía, Sección Paleontología y Estratigrafía, Tiltil 1993, Ñuñoa, Santiago, Chile. 3 UMR CNRS 7730 CEREGE, Aix-Marseille Université, Case 67, 3 Place V. Hugo, 13331 Marseille Cédex 03, France. [email protected] 4 9bis Chemin des Poissoniers, 13600 La Ciotat, France. [email protected] * Permanent adress: TERRA IGNOTA. Heritage & Geosciences Consulting, Dr. Cádiz 726, Ñuñoa, Santiago, Chile. [email protected] ABSTRACT. Ammonites of the genus Santafecites Etayo-Serna and subgenus Olcostephanus (Viluceras) Aguirre- Urreta and Rawson are described for the first time from Chile. The succession of Olcostephaninae from the Chañarcillo Basin of northern Chile is described in the light of new collections and revision of historical material.