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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 -
Palaeoecology and Palaeoenvironments of the Middle Jurassic to Lowermost Cretaceous Agardhfjellet Formation (Bathonian–Ryazanian), Spitsbergen, Svalbard
NORWEGIAN JOURNAL OF GEOLOGY Vol 99 Nr. 1 https://dx.doi.org/10.17850/njg99-1-02 Palaeoecology and palaeoenvironments of the Middle Jurassic to lowermost Cretaceous Agardhfjellet Formation (Bathonian–Ryazanian), Spitsbergen, Svalbard Maayke J. Koevoets1, Øyvind Hammer1 & Crispin T.S. Little2 1Natural History Museum, University of Oslo, P.O. Box 1172 Blindern, 0318 Oslo, Norway. 2School of Earth and Environment, University of Leeds, Leeds LS2 9JT, United Kingdom. E-mail corresponding author (Maayke J. Koevoets): [email protected] We describe the invertebrate assemblages in the Middle Jurassic to lowermost Cretaceous of the Agardhfjellet Formation present in the DH2 rock-core material of Central Spitsbergen (Svalbard). Previous studies of the Agardhfjellet Formation do not accurately reflect the distribution of invertebrates throughout the unit as they were limited to sampling discontinuous intervals at outcrop. The rock-core material shows the benthic bivalve fauna to reflect dysoxic, but not anoxic environments for the Oxfordian–Lower Kimmeridgian interval with sporadic monospecific assemblages of epifaunal bivalves, and more favourable conditions in the Volgian, with major increases in abundance and diversity of Hartwellia sp. assemblages. Overall, the new information from cores shows that abundance, diversity and stratigraphic continuity of the fossil record in the Upper Jurassic of Spitsbergen are considerably higher than indicated in outcrop studies. The inferred life positions and feeding habits of the benthic fauna refine our understanding of the depositional environments of the Agardhfjellet Formation. The pattern of occurrence of the bivalve genera is correlated with published studies of Arctic localities in East Greenland and northern Siberia and shows similarities in palaeoecology with the former but not the latter. -
Crustacea : Decapoda : Erymidae) Dans Le Jurassique
Première occurrence d’Enoploclytia M’Coy, 1849 (Crustacea : Decapoda : Erymidae) dans le Jurassique First occurence of Enoploclytia M’Coy, 1849 (Crustacea: Decapoda: Erymidae) in the Jurassic Julien Devillez Muséum national d’Histoire naturelle, Paris Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (CR2P, UMR 7207), Sorbonne Universités, MNHN, UPMC, CNRS, 57 rue Cuvier F-75005 Paris (France) [email protected] Sylvain Charbonnier Muséum national d’Histoire naturelle, Paris Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (CR2P, UMR 7207), Sorbonne Universités, MNHN, UPMC, CNRS, 57 rue Cuvier F-75005 Paris (France) [email protected] Jean-Philippe Pezy Normandie Univ, UNICAEN, CNRS, M2C, 14000 CAEN, France [email protected] RÉSUMÉ Parmi les Erymidae Van Straelen, 1925, connus dès le Permien supérieur (Changhsingien) et répandus au Jurassique, le genre Enoploclytia M’Coy, 1849 passe pour être apparu tardivement en raison de son absence avant le Crétacé. Jusqu’à présent, le plus ancien représentant était E. augustobonae Devillez, Charbonnier, Hyžný & Leroy, 2016 du Crétacé inférieur (Barrémien) de l’est du bassin de Paris (France). Cependant, un nouveau fossile récolté en Normandie (France), présentant une architecture des sillons de la carapace typique d’Enoploclytia, atteste de la présence du genre dès le Jurassique supérieur (Oxfordien). MOTS CLÉS Crustacé, Erymidae, France, homard, Jurassique, Mésozoïque, Normandie. ABSTRACT Among the Erymidae Van Straelen, 1925, known as early as the Late Permian (Changhsingian) and widespread in the Jurassic, the genus Enoploclytia M’Coy, 1849 seems to have a late appearance because of its lack before the Cretaceous. Until now, the oldest representative was E. -
The Middle Oxfordian to Lowermost Kimmeridgian Ammonite
Volumina Jurassica, 2010, Viii: 5–48 The Middle Oxfordian to lowermost Kimmeridgian ammonite succession at Mikhalenino (Kostroma District) of the Russian Platform, and its stratigraphical and palaeobiogeographical importance Ewa GŁOWNIAK1, Dmitry N. KISELEV2, Mikhail ROGOV3, Andrzej WIERZBOWSKI1, John K. WRIGHT4 Key words: ammonites, biostratigraphy, Boreal zonation, Subboreal zonation, Submediterranean zonation, correlation, Oxfordian/ Kimmeridgian boundary. Abstract. The Mikhalenino section on the Russian Platform has yielded numerous ammonites from the Middle and Upper Oxfordian and lowermost Kimmeridgian, collected bed by bed. The ammonites belong mostly to the Boreal family Cardioceratidae, but also to the Sub- boreal family Aulacostephanidae; additionally at some levels there were collected various Submediterranean ammonites (Perisphinctidae, Oppeliidae and Aspidoceratidae). The co-occurrence of ammonites representative of different faunal provinces makes possible recognition of the Boreal, Subboreal, and partly also Submediterranean standard zonations. In consequence, it is possible to make a close correlation between these zonal schemes. The Oxfordian/Kimmeridgian boundary at the Pseudocordata/Baylei zonal boundary of the Subboreal zonal scheme corresponds precisely to the Rosenkrantzi/Bauhini zonal boundary. This boundary of the stages defined well faunistically in the Flodigarry section (Isle of Skye, Scotland) and proposed as a candidate for the uniform Oxfordian/Kimmeridgian boundary, can be also recognized in the Russian sec- tion studied. The boundary can be traced in the Mikhalenino section using the same criteria as used at Staffin: the appearance of the first representatives of Pictonia [M]–Prorasenia [m] (Subboreal), and the first appearance of Amoeboceras (Plasmatites) (Boreal). This indi- cates the large correlation potential of the boundary defined in this way. The research on the Mikhalenino section has provided the new palaeontological findings described in this study. -
2. General Index
Downloaded from http://pygs.lyellcollection.org/ by guest on September 29, 2021 2. General Index abandoned river courses. Vale of York 40,223-32 anhydrite 50.78.79,81,86,88.143-54 Abbey Crags, Knaresborough Gorge 46,290 Anisocardiu tenera (Antiquicyprina) loweana 39, 117, 130, 131.738-9 Acadian 46,175 ff.; 50,255-65 anisotropy of vitrinites 39,515-26 acanthite 46,135 ankerite 50,87 Acanthodiacrodium cf. simplex 42,412-3 annelida, in Yorkshire Museum 41,402 Acanthodiacrodium rotundatum 45.124 antimony, trace element in galena 44,153 Acanthodiacrodium cf. tumidum 45,124 apatite 44,438 Acanthopleuroceras sp. 42, 152-3 apatite fission-track palaeotemperatures. north-west England 50,95-9 accretionary lapilli, Cwm Clwyd Tuff 39,201,206-7,209,215-6 Apatocythere (Apatocythere) simulans 45, 243 Acheulian handaxes 41,89,94-5 Apedale Fault 50. 196," 198 acid intrusions, Ordovician and Caledonian, geochemical characteristics aplites. Whin Sill 47,251 of 39,33-57 Apollo's Coppice, Shropshire 50,193 acritarchs. Arenig 42. 405 Arachinidiuin smithii 42, 213 acritarchs, Ordovician 47,271-4 Araucarites phillipsii 45,287 acritarchs,Tremadoc 38 45-55; 45,123-7 archaeology, Lincolnshire 41.75 ff. Actinocamax plenus 40,586 Arcomva unioniformis 39.117.133, 134, 138 Acton Reynald Hall, Shropshire 50,193,198,199,200,202,204 Arcow"45,19ff.' adamellite (Threlkeld Microgranite) 40,211-22 Arcow Wood Quarry 39,169,446,448,455,459,470-1 aegirine 44,356 arctic-alpine flora. Teesdale 40.206 aeolian deposition, Devensian loess 40,31 ff. Arenicolites 41,416,436-7 aeolian deposition. Permian 40,54.55 Arenobulirnina advena 45,240 aeolian sands, Permian 45, 11-18 Arenobulimina chapmani 45,240 aeolian sedimentation, Sherwood Sandstone Group 50,68-71 Arenobulirnina macfadyeni 45, 240 aeromagnetic modelling, west Cumbria 50,103-12 arfvedsonite 44,356 aeromagnetic survey, eastern England 46,313,335—41 argentopyrite 46, 134-5 aeromagnetic survey, Norfolk 46.313 Arniocreas fulcaries 42, 150-1 Africa, North, Devonian of 40,277-8 arsenic 44,431 ff. -
The Upper Jurassic of Europe: Its Subdivision and Correlation
The Upper Jurassic of Europe: its subdivision and correlation Arnold Zeiss In the last 40 years, the stratigraphy of the Upper Jurassic of Europe has received much atten- tion and considerable revision; much of the impetus behind this endeavour has stemmed from the work of the International Subcommission on Jurassic Stratigraphy. The Upper Jurassic Series consists of three stages, the Oxfordian, Kimmeridgian and Tithonian which are further subdivided into substages, zones and subzones, primarily on the basis of ammonites. Regional variations between the Mediterranean, Submediterranean and Subboreal provinces are discussed and correlation possibilities indicated. The durations of the Oxfordian, Kimmeridgian and Tithonian Stages are reported to have been 5.3, 3.4 and 6.5 Ma, respectively. This review of the present status of Upper Jurassic stratigraphy aids identification of a num- ber of problems of subdivision and definition of Upper Jurassic stages; in particular these include correlation of the base of the Kimmeridgian and the top of the Tithonian between Submediterranean and Subboreal Europe. Although still primarily based on ammonite stratigraphy, subdivision of the Upper Jurassic is increasingly being refined by the incorporation of other fossil groups; these include both megafossils, such as aptychi, belemnites, bivalves, gastropods, brachiopods, echino- derms, corals, sponges and vertebrates, and microfossils such as foraminifera, radiolaria, ciliata, ostracodes, dinoflagellates, calcareous nannofossils, charophyaceae, dasycladaceae, spores and pollen. Important future developments will depend on the detailed integration of these disparate biostratigraphic data and their precise combination with the abundant new data from sequence stratigraphy, utilising the high degree of stratigraphic resolution offered by certain groups of fos- sils. -
1 the Literature on Triassic, Jurassic and Earliest Cretaceous Dinoflagellate Cysts: Supplement 4 2 3 James B
1 The literature on Triassic, Jurassic and earliest Cretaceous dinoflagellate cysts: supplement 4 2 3 James B. Riding 4 5 British Geological Survey, Environmental Science Centre, Keyworth, Nottingham NG12 6 5GG, United Kingdom 7 8 CONTACT James B. Riding email [email protected] 9 10 ABSTRACT 11 Since the publication of four compilations issued between 2012 and 2019, 93 further 12 published contributions on Triassic, Jurassic and earliest Cretaceous (Berriasian) 13 dinoflagellate cysts from Africa, North America, South America, the Arctic, Australasia, East 14 Europe, West Europe, the Middle East and Russia have been discovered in the literature, or 15 were issued in the last 12 months (i.e. between February 2018 and January 2019). Of these, 16 55 were published during 2018 and 2019, making this period a very productive one. These 17 studies are mostly on the Late Triassic and Early Jurassic of Europe. All the 93 items are 18 listed herein with digital object identifier (doi) numbers where available, as well as a 19 description of each item as a string of keywords. Publications on West Europe comprise 20 31.2% of the total, and items on Africa, the Arctic, Australasia, East Europe and Russia are 21 also significant (15.1%, 6.5%, 7.5%, 9.7% and 14.0% respectively). The least well- 22 represented regions are North America, South America and the Middle East (2.2%, 1.1% and 23 1.1% respectively). 24 25 KEYWORDS dinoflagellate cysts; earliest Cretaceous (Berriasian); Jurassic; literature 26 analysis and compilation; Triassic; worldwide 27 28 29 1. Introduction 30 The literature on Triassic to earliest Cretaceous (Berriasian) dinoflagellate cysts is extensive, 31 and was listed and reviewed by Riding (2012, 2013, 2014, 2019). -
Towards a Consistent Oxfordian-Kimmeridgian Global
Towards a consistent Oxfordian-Kimmeridgian global boundary: current state of knowledge Andrzej Wierzbowski 1, Francois Atrops 2, Jacek Grabowski 1, Mark Hounslow 3, Bronisław A.Matyja 4, Federico Olóriz 5, Kevin Page 6, Horacio Parent 7, Mikhail A. Rogov 8, Günter Schweigert 9, Hubert Wierzbowski 1, John K. Wright 10 1 Polish Geological; Institute – National Research Institute, 4, Rakowiecka Str., 00-975 Warszawa, Poland, e-mail: [email protected] , [email protected] , [email protected] ; 2 UFR Sciences de la Terre, Université Claude-Bernard Lyon 1, 43 bd.du 11 Novembre, 69622 Villeurbanne Cedex, e-mail: francois.atrops@univ- lyon1.fr ; 3CEMP, Lancaster Environment Centre, Lancaster University, UK, e-mail: [email protected] ; 4 Faculty of Geology, University of Warsaw, 93, Żwirki i Wigury Str., 02-089 Warszawa, Poland, e-mail: [email protected] ; 5 Department of Stratigraphy and Paleontology, Faculty of Sciences, University of Granada, Av. Fuentenueva s/n, 1807 Granada, Spain, e-mail: [email protected]; 6 School of Geography, Earth and Environmental Sciences, University of Plymouth, Drakes Circus, Plymouth PL4 8AA, UK, e- mail: [email protected] ; 7 Laboratorio de Paleontologia IFG, FCEIA Universidad Nacional de Rosario, pellegrini 259-0, 2000 Rosario, Argentina, e-mail: [email protected],edu.ar ; 8 Geological Institute of Russian Academy of Sciences, 7, Pyzhevskii Lane, 119017 Moscow, Russia; e-mail: [email protected] ; 9Staatliches Museum für Naturkunde, 1, Rosenstein, 70-191Stuttgart, Germany; e-mail: [email protected] ;10 Department of Earth Sciences, Royal Holloway College, Egham, Surrey, U.K. -
Callovian (Jurassic) Ammonites from the United States and Alaska
Callovian (Jurassic) Ammonites from the United States and Alaska Part 1. Western Interior United States GEOLOGICAL SURVEY PROFESSIONAL PAPER 249-A Callovian (Jurassic) Ammonites from the United States and Alaska Part 1. Western Interior United States By RALPH W. IMLAY GEOLOGICAL SURVEY PROFESSIONAL PAPER 249-A Descriptions and illustrations of cephalopods of Late Jurassic age UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1953 UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Page Abstract -—--—---—-——————_—————__________.._____.„__.______ 1 Ecologic considerations—Continued Introduction --——————————————.._____________._„._.„___ 1 Conditions of deposition—— _.____.__———-——.——— 9 Biologic analysis ——————.——__——._____.___.._____„_„_____ 1 Conglomerate —...— ——————————_.., 9 Stratigraphic summary ———————._.__——____.____________ 4 Sand ——_———————————————— — 9 Faunal zones and correlations————..__————_.._——— 5 Marine siltstone and shale.—————-—_——— 10 Arcticoceras codyense zone..————.._______....——_„ 5 Limestone -——————_.-_————————.——— 10 Gowericeras costidensum zone____—._...„——_.——_——— 7 Other types of sediment———————————— 10 Gowericeras subitum zone————_-.........._..._„„........ 7 Ammonite distribution and associations—————— 11 Kepplerites tychonis zone.__————————_———. 7 Geographic distribution - - ———————————————— 14 Kepplerites mcleami zone.—————„___„..—.............. 7 Summary of results--------———————————————— 17 Comparisons with other faunas————____........„—....„.. 8 Systematic descriptions ———.—_.————————— 18 Ecologic considerations —————————_——.__..._.... 8 References ———————————————————— ———. 34 Sources of sediment———_——.._ _„__..—_———._.. 8 Index -.-—————————.———————-—-—--——— 37 ILLUSTRATIONS [Plates 1-24 follow index] PLATE 1. Xenocephalites and Lilloettia 2-4. Arcticoceras 5. Cosmoceras and Arcticoceras 6,7. Cadoceras 8, 9. -
Jurassica Field Trip Guide and
XIIth Jurassica Conference Field Trip Guide and Abstracts Book April 19–23, 2016, Smolenice, Slovakia Edited by: Jozef Michalík and Kamil Fekete Earth Science Institute, Slovak Academy of Sciences Bratislava 2016 Scientific Committee: Jingeng Sha, Nanjing Inst. of Geol. and Palaeo.; Chinese Academy of Sciences, China Anna Feldman-Olszewska, Polish Geological Institute, Warszawa William A. P. Wimbledon, School of Earth Sciences, University of Bristol, UK Jozef Michalík, Earth Science Institute, Slovak Academy of Sciences, Bratislava Roman Aubrecht, Dep. of Geol. and Palaeontology, Comenius University, Bratislava Jolanta Iwańczuk, Polish Geological Institute, Warszawa Michał Krobicki, Polish Geol. Inst.; AGH Univ. of Science and Technology, Kraków Otília Lintnerová, Dep. of Economic Geology, Comenius University, Bratislava Dušan Plašienka, Dep. of Geol. and Palaeontology, Comenius University, Bratislava Daniela Reháková, Dep. of Geol. and Palaeontology, Comenius University, Bratislava Ján Schlögl, Dep. of Geology and Palaeontology, Comenius University, Bratislava Ján Soták, Earth Science Institute, Slovak Academy of Sciences, Banská Bystrica Vladimír Šimo, Earth Science Institute, Slovak Academy of Sciences, Bratislava Adam Tomašovych, Earth Science Institute, Slovak Academy of Sciences, Bratislava Andrzej Wierzbowski, Polish Geological Institute, Warszawa Organizing Committee: Jozef Michalík, Earth Science Institute, Slovak Academy of Sciences, Bratislava Anna Feldman-Olszewska, Polish Geological Institute, Warszawa Ľubica Puškelová, Earth -
'Sex Reversals' in the Ammonoidea and Their Signi Cance
Another Lesson From Beautiful Monsters: the Case of 'sex Reversals' in the Ammonoidea and Their Signicance Camile Frau ( [email protected] ) Groupement d'Intérêt Paléontologique, Science et Exposition, 35 Impasse lieutenant Daumas 83100 Toulon, France Pierre-Yves Boursicot Research Article Keywords: Ammonoidea, Sexual dimorphism, Intersexuality, Pathology, Jurassic Posted Date: February 2nd, 2021 DOI: https://doi.org/10.21203/rs.3.rs-157754/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Page 1/21 Abstract Background: Expression of a sexual dimorphism is recognised in various fossil groups of molluscs such as the Ammonoidea, an extinct group of shelled cephalopods. During the Mesozoic, the best documented sexual dimorphic examples are seen in the Jurassic superfamily Perisphinctoidea. It is most usually expressed by distinct adult size and apertural modications between the antidimorphs. Putative males (otherwise referred to as microconch) are small in size and develop lappets at the end of the shell while the females (macroconch) are larger and bear a simple peristome. Dubious cases are, however, known in that superfamily. They most often relate to taxonomic biases or lack of diagnostic characters, and some others expose ontogenetic anomalies illustrated by ‘sex reversals’ in the shell morphology and ornamentation. Results: The discovery of two specimens of the Callovian Aspidoceratidae Peltoceras athleta (Phillips), having both female and male features, questions the signicance and causes of ‘sex reversals’ in the Ammonoidea. The two specimens have started with the macroconch ontogeny of Peltoceras athleta, and show an apparent change toward maleness in the adult, as illustrated by their rounded whorl section, ribs retroversion, fading of the tubercles and lappets typical of the microconchs. -
8 International Symposium Cephalopods
8th International Symposium Cephalopods – Present and Past August 30 – September 3, 2010 Abstracts Volume University of Burgundy & CNRS Dijon - France http://www.u-bourgogne.fr/cephalopods/ Honorary Committee Sigurd von Boletzky, DR CNRS - Banyuls-sur-Mer - France Raymond Enay, Prof. University of Lyon Lyon - France Didier Marchand, University of Burgundy Dijon - France Jacques Thierry, Prof. University of Burgundy Dijon - France Scientific committee Giambattista Bello, ARION, Mola di Bari - Italy Vyacheslav Bizikov, Russian Federal Research Institute of Marine Fisheries and Oceanography, Moscou - Russia Christian Klug, Universitaet Zuerich, Zurich - Switzerland Neil. H. Landman, American Museum of Natural History, New York - USA Pascal Neige, University of Burgundy, Dijon - France Isabelle Rouget, University Pierre & Marie Curie, Paris - France Kazushige Tanabe, University of Tokyo, Tokyo - Japan Margareth Yacobuci, Bowling Green State University, Bowling Green - USA Organizing committee Pascal Neige, University of Burgundy – France Isabelle Rouget, University Pierre and Marie Curie – France Alex Bauer, CNRS, University of Burgundy – France Arnaud Brayard, CNRS, University of Burgundy – France Guillaume Dera, University of Burgundy – France Jean-Louis Dommergues, CNRS, University of Burgundy – France Emmanuel Fara, University of Burgundy – France Myette Guiomar, Rserve Gologique de Haute-Provence Digne-les Bains, France Clotilde Hardy, University of Burgundy – France Isabella Kruta, MNHN – France Rémi Laffont, CNRS, University of Burgundy