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New and Poorly Known Perisphinctoidea (Ammonitina) from the Upper Tithonian of Le Chouet (Drôme, SE France)
Volumina Jurassica, 2014, Xii (1): 113–128 New and poorly known Perisphinctoidea (Ammonitina) from the Upper Tithonian of Le Chouet (Drôme, SE France) Luc G. BULOT1, Camille FRAU2, William A.P. WIMBLEDON3 Key words: Ammonoidea, Ataxioceratidae, Himalayitidae, Neocomitidae, Upper Tithonian, Le Chouet, South-East France. Abstract. The aim of this paper is to document the ammonite fauna of the upper part of the Late Tithonian collected at the key section of Le Chouet (Drôme, SE France). Emphasis is laid on new and poorly known Ataxioceratidae, Himalayitidae and Neocomitidae from the upper part of the Tithonian. Among the Ataxioceratidae, a new account on the taxonomy and relationship between Paraulacosphinctes Schindewolf and Moravisphinctes Tavera is presented. Regarding the Himalayitidae, the range and content of Micracanthoceras Spath is discussed and two new genera are introduced: Ardesciella gen. nov., for a group of Mediterranean ammonites that is homoeomorphic with the Andean genus Corongoceras Spath, and Pratumidiscus gen. nov. for a specimen that shows morphological similarities with the Boreal genera Riasanites Spath and Riasanella Mitta. Finally, the occurrence of Neocomitidae in the uppermost Tithonian is documented by the presence of the reputedly Berriasian genera Busnardoiceras Tavera and Pseudargentiniceras Spath. INTRODUCTION known Perisphinctoidea from the Upper Tithonian of this reference section. Additional data on the Himalayitidae in- The unique character of the ammonite fauna of Le Chouet cluding the description and discussion of Boughdiriella (near Les Près, Drôme, France) (Fig. 1) has already been chouetensis gen. nov. sp. nov. are to be published elsewhere outlined by Le Hégarat (1973), but, so far, only a handful of (Frau et al., 2014). -
Sülfür Throughout Geological Time in Balkan Peninsula**
Mineral Res. Expl. Bul.. 123-124. 1-12, 2002 SÜLFÜR THROUGHOUT GEOLOGİCAL TIME IN BALKAN PENINSULA** Radule POPOVİC* ABSTRACT.- During investigations for a long time it has been remarked that the oldest metallogenic epochs in Balkan Peninsula include a limited number of, occurrences with sülfür as one of the chief chemical elements. Thus it could be said that in these epochs the deposits with sulphur compounds either have not been formed or in some cases there were only rare showings. So, for instance with the Grenvilian epoch, according to date know- ledge, only one occurrence in Pelagonids (Nezilovo) could be associated. In the Baikalian metallogenic epoch, characterized by formation of greenschists in western Macedonian only traces of sulfide mineralizations, then one deposit of lead, zinc and copper sulfides, as well as one pyrite impregnation in the larger Popcevo - Dojran area (eastern Macedonia), exhibiting sülfür content less than 0,11% are present. In contrast to Pelagonian-Rhodopean massif, in the Green complex (Vlasina) of eastern Serbia numerous deposits and occurrences of pyrite and lead, zinc and copper sulfides are present, indicating a more remarkable sülfür yield in this district during Baikalian metallogenic epoch. Thanks to this fact it could be estimated this epoch to be much more enriched in sülfür in Balkan Peninsula, compared with the Grenvilian epoch. In the next epochs (Caledonian and Hercynian) the sülfür yield had become more and more intensive. This is especially related to the phytlitic volcanogenic-sedimentary origin formation of western Macedonian. in which fifteen deposits and occurrences of lead. zinc, copper and molybdenum sulfides have been registered, indicating numerous richer and poorer, certainly irregular pyrite impregnations. -
Xenosphinctes N. Gen. (Ataxioceratidae, Lithacoceratinae), a New Rare Ammonite Genus from the Lower Tithonian (Hybonotum Zone) of SW Germany
VOLUMINA JURASSICA, 2017, XV: 155–160 DOI: 10.5604/01.3001.0010.7170 Xenosphinctes n. gen. (Ataxioceratidae, Lithacoceratinae), a new rare ammonite genus from the Lower Tithonian (Hybonotum Zone) of SW Germany Armin SCHERZINGER1, Günter SCHWEIGERT2 Key words: ammonites, Xenosphinctes berkai, Early Tithonian, biostratigraphy, Germany. Abstract. The new monotypic ammonite genus Xenosphinctes (type species: Xenosphinctes berkai n. sp.) is established. It is recorded from the Upper Jurassic, Early Tithonian, Hybonotum Zone, Riedense Subzone, eigeltingense α horizon from the Talmühle, N of Engen, Baden-Württemberg, SW Germany. INTRODUCTION AMMONITE FAUNA OF THE EIGELTINGENSE α HORIZON The Hangende-Bankkalke Formation is the youngest formation in the Upper Jurassic of Swabia. Its base is usual- The first comprehensive review of ammonites from the ly formed by an unconformity with a marked change in li- uppermost Jurassic in Swabia was provided by Berckhemer thology from coarse-grained bioclastic limestones or marl- & Hölder (1959). However, therein the focus was on the am- stones to pure mudstones (Schweigert, 1996). Its type monite fauna of the Late Kimmeridgian Beckeri Zone, and locality is an abandoned limestone quarry near the village of only very few taxa from higher levels have been reported. Eigeltingen, and its base is best exposed in a nearby section Ohmert & Zeiss (1980) started with a description of the am- along a railroad cut, NW of the Talmühle hamlet (Fig. 1). monite fauna of the Hangende-Bankkalke Formation in the The most abundant macrofossils in these basal parts of the western part of the Swabian Alb. On that occasion several formation are ammonites. Many of them are fragmented due important taxa from the basal part of this formation which to predation, but some of them are quite well-preserved as are typical of the former eigeltingense horizon were intro- steinkerns with superimposed sculpture of the outer shell. -
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. -
Upper Jurassicelower Cretaceous Stratigraphy in South-Eastern Tibet: a Comparison with the Western Himalayas
Author's personal copy Cretaceous Research 29 (2008) 301e315 www.elsevier.com/locate/CretRes Upper JurassiceLower Cretaceous stratigraphy in south-eastern Tibet: a comparison with the western Himalayas Xiumian Hu a,*, Luba Jansa b, Chengshan Wang c a State Key Laboratory of Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, China b Department of Earth Sciences, Dalhousie University, Halifax B3H 3J5, Canada c Geological Centre for Tibetan Plateau, China University of Geosciences, Beijing 100083, P.R. China Received 24 January 2007; accepted in revised form 14 May 2007 Available online 28 November 2007 Abstract Lithostratigraphic studies of the Upper JurassiceLower Cretaceous sedimentary successions exposed in the TingrieGyangze area, south- eastern Tibet resulted in the establishment of a revised stratigraphic framework. A major crustal fault separates the southern Tibetan sedimentary successions into a Southern Zone and a Northern Zone. The Upper JurassiceLower Cretaceous strata of the Southern Zone are subdivided into the Menkadun Formation (Oxfordian, Kimmeridgian, up to lower Upper Tithonian), the Gucuo Formation (Upper Tithonian to Lower Albian) and the overlying Dongshan Formation (Upper Albian). The Gucuo Formation is further subdivided into a quartz arenite unit, which is overlain by a shale unit, in turn overlain by a volcaniclastic sandstone unit. The youngest cluster of detrital zircon absolute age data (127.7 Æ 1.8 Ma) from the lower part of the volcaniclastic unit of the Gucuo Formation place the volcanic event before the Late Barremian. In the Northern Zone, the Upper JurassiceLower Cretaceous strata have been subdivided into four formations: the Zhera Formation (Upper Jurassic), the Weimei Formation (Tithonian), the Rilang Formation (?Berriasian) and the Gyabula Formation (? post-Valanginian). -
Die Allgäu-Schichten (Jura-Fleckenmergel) Zwischen Wettersteingebirge Und Rhein
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Jb. Geol. B. A. Bd. 108 S. 1—114 Wien, Juni 1965 Die Allgäu-Schichten (Jura-Fleckenmergel) zwischen Wettersteingebirge und Rhein Von Volker JACOBSHAGEN (Marburg/Lahn) *) (Mit 3 Abbildungen, 2 Tabellen, 5 Phototafeln und 8 Tafeln) Zusammenfassung In den Nördlichen Kalkalpen westlich vom Wetterstein-Gebirge wurden die Allgäu- Schichten (Jura-Fleckenmergel) nach dem Vorwiegen kalkiger oder mergeliger Gesteine durchweg in drei Abteilungen gegliedert: A. Ältere Allgäu-Schichten (Unter- bis Mittellias), kalkreich. B. Mittlere Allgäu-Schichten (unterer Oberlias), mergelreioh. C. Jüngere Allgäu-Schichten (oberer Oberlias und Dogger), kalkreich. Diese Abteilungen konnten gebietsweise jedoch noch in mehrere Gruppen unterteilt werden. Die in der Schichtfolge beobachteten Faziestypen werden kurz charakterisiert und genetisch gedeutet. Nach Mächtigkeits- und Fazies-Verteilung wird dann ein paläo- geographischer Überblick für die einzelnen Abteilungen entworfen. Fragen der Groß- tektonik, unter anderem das Problem Deckenbau oder gebundene Tektonik, können daran überprüft werden. Abschließend werden die Beziehungen der Allgäu-Schichten zum mediterranen und mitteleuropäischen Jura behandelt. Inhalt Vorwort 2 I. Erforschungsgeschichte 3 II. Stratigraphie 5 Zur Nomenklatur 5 Die Gliederung 6 Schichtenfolge 6 A. Ältere Allgäu-Schichten 7 1. Rätikon, Davenna-Gruppe 8 2. Lechtaler Alpen 10 3. Nördliche Vorarlberger Kalkalpen 25 4. Allgäuer Alpen 28 5. Hohenschwangauer und Ammergauer Alpen 38 *) Adresse des Autors: Geologisch-Paläontologisches Institut der Universität Mar burg/Lahn, Deutschhausstraße 10. ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at 2 B. Mittlere Allgäu-Schiohten 40 1. Kätikon, Davenna-Gruppe 43 2. Lechtaler Alpen 43 3. Nördliche Vorarlberger Kalkalpen 46 4. Allgäuer Alpen 46 5. Hohenschwangauer und Ammergauer Alpen 50 C. -
Marine Sediments from the Southern Sierra Madre Oriental
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Blau, Joachim; Meister, Christian; Schmidt-Effing, Reinhard; Villaseñor, Ana B. A new fossiliferous site of Lower Liassic (Upper Sinemurian) marine sediments from the southern Sierra Madre Oriental (Puebla, Mexico): ammonite fauna, biostratigraphy, and description of Ectocentrites hillebrandti new species Revista Mexicana de Ciencias Geológicas, vol. 25, núm. 3, 2008, pp. 402-407 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57225303 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 402 RevistaBlau etMexicana al. de Ciencias Geológicas, v. 25, núm. 3, 2008, p. 402-407 A new fossiliferous site of Lower Liassic (Upper Sinemurian) marine sediments from the southern Sierra Madre Oriental (Puebla, Mexico): ammonite fauna, biostratigraphy, and description of Ectocentrites hillebrandti new species Joachim Blau1,*, Christian Meister2, Reinhard Schmidt-Effi ng3, and Ana B. Villaseñor4 1 Feldbergstrasse 5, D-61191 Rosbach-Rodheim, Germany. 2 Muséum d’Histoire Naturelle, Département de Géologie et Paléontologie, 1 Rte de Malagnou, CP. 6434, CH-1211 Genève 6, Switzerland. 3 Institut für Geologie und Paläontologie, Hans-Meerwein-Strasse 11a, D-35032 Marburg, Germany. 4 Instituto de Geología, Departamento de Paleontología, Ciudad Universitaria, 04510, México, D.F., Mexico. * [email protected] ABSTRACT We describe ammonites from a newly discovered, fossil-bearing, marine Liassic locality (Lower Jurassic, Huayacocotla Fm.) in the vicinity of the Zongozotla Municipality (southern Sierra Madre Oriental) in the northern part of Puebla State (Mexico). -
Imray Supplement
Shell Channel Pilot 8th Edition 2017 ISBN 978 184623 700 3 Supplement No.2 May 2019 This supplement contains amendments and corrections sent Erratum in by a number of cruising yachtsmen and women, in addition to those culled from official sources such as Notices IMPORTANT to Mariners. Positions and waypoints The captions for all Tidal stream diagrams for All positions and waypoints are to datum WGS84. They are Portland Bill on pages 147 –9 relate incorrectly to included to help locating place, features and transits. Do HW Dover. This should be corrected in all not rely on them alone for safe navigation. instances to HW Plymouth . Bearings and lights Any bearings are given in degrees True and from seaward. The diagrams themselves are otherwise correct. The characteristics of lights may be changed during the The implications of this are critical and should not lifetime of this book and they should be checked against the latest edition of the UK Admiralty List of Lights. be ignored. Note Where lights have been modified in the text do please Please see following pages remember to alter them on the appropriate plan(s). This supplement is cumulative and the latest information is Page 27 River Stour entrance plan marked in blue . See amended plan. Page 43 Brighton Depths Reports are in (May 2019) that depths are now even more restricted. One metre draught 2 hours either side of LW is the official version. Page 296 Honfleur Lock access Amend to HW+2 to HW. It is advisable to check with the lock keeper on VHF Ch17 prior to arrival. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Vol 10, Issue 4, December 2011
MMAAGGAAZZIINNEE OOFF TTHHEE GGEEOOLLOOGGIISSTTSS’’ AASSSSOOCCIIAATTIIOONN VVoolluummee 1100 NNoo.. 44 DDeecceemmbbeerr 22001111 The Association Future Lectures FESTIVAL OF GEOLOGY Nominations Required Field Trip to France part 2 October Lecture Weald Clay Field Trip Curry Fund Report Circular GA Two-Day Meeting Rockwatch News Rockwatch Young Writer Sher-rock Holmes Geology of NE Churches 1 Winners of Photographic Competition Magazine of the Geologists’ Association Volume 10 No. 4, 2011 CONTENTS Published by the Geologists’ Association. Four issues per year. ISSN 1476-7600 Production team: JOHN CROCKER, Paula Carey, John 3 The Association Cosgrove, Vanessa Harley, Jon Trevelyan, 4 Future Lectures Chris Woolston 5 FESTIVAL OF GEOLOGY Printed by City Print, Milton Keynes 6 Nominations Required 7 Field Trip to France part 2 The GEOLOGISTS’ ASSOCIATION does not accept any responsibility for views and opinions expressed by 11 October Lecture individual authors in this magazine. 12 Weald Clay Field Trip 13 Curry Fund Report The Geologists’ Association 14 Circular The Association, founded in 1858, exists to foster the progress and diffusion of the science of geology, and to encourage 20 GA Two-Day Meeting research and the development of new methods. It holds meetings 23 Rockwatch News for the reading of papers and the delivery of lectures, organises museum demonstrations, publishes Proceedings and Guides, and 25 Rockwatch Young Writer conducts field meetings. Annual Subscriptions for 2012 are £40.00, Associates £30.00, 27 Sher-rock Holmes Joint Members £58.00, Students £18.00. 28 Geology of NE Churches 1 For forms of Proposal for Membership and further information, apply to the Executive Secretary, The Geologists’ Association, 31 Kite Flying or Fossil Hunting? Burlington House, Piccadilly, London W1J 0DU. -
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 -
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.