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THE CONCESIO FORMATION of the LOMBARDIAN RIFTED BASIN (Southern ALPS, Rtaly)
Rivista Italiana di Paleontologia e Stratigrafia volume tul numero I pagrne 49-64 ApriÌe 1996 THE CONCESIO FORMATION OF THE LOMBARDIAN RIFTED BASIN (souTHERN ALPS, rTALY). STRATIGRAPHY OF A JURASSIC CALCAREOUS TURBIDITE UNIT RICCARDO BERSEZIO, FABRIZIO FELLETTI, FRANCESCA LOZAR & MARCO RUGGERI Key-uords: calcareous turbidites, Jurassic, Lombardian Basin, downcurrent (westwards) and upsection by sheet-like calcarenite Southern Alps. stratigraphy. syn-ri[t sediments. units, very similar to depositional lobes, then by a basin plain facies association. Close to the Aalenian - Bajocian boundary the resulting Riassunto. La Formazione di Concesio è costituita da due lito- thinning and fining upwards megasequence was sealed by hemipelagic somi torbiditici, grosso modo corrispondenti ai membri dei Calcari marlstones, followed upsection by a basin plain facies association of Nocciola e dei Calcari Medoloidi (Auct.), che si svilupparono da sud- pelagic turbidites and pelagites. This second unit developed as a re- est verso nord-ovest, tra il Toarciano inferiore ed il Batoniano inferio- sponse of a major flooding event recorded by drowning of the re nel Bacino Sebino, la porzione orientale del Bacino Lombardo. platform succession of the Trento platform. I[ corpo torbiditìco inferiore (Toarciano-Aaleniano), alimenta- Turbidite deposition came to end before the Bathonian; du- to dall'erosione del margine di una piattaforma carbonatica e del suo ring this time interval sediment starvation and bottom current rewor- substrato, si configura come un prisma cuneiforme che termina sopra- king occurred throughout the Sebino Basin, slightly predating the corrente al bordo occidentale dell'alto strutturale del Botticino. Esso turnover to siliceous pelagic sedimentation (radiolarites of the Selcife- si chiude sottocorrente in relazione di onlap sul margine fagliato ro Group). -
A New Early Jurassic Marine Locality from Southwestern Chubut Basin, Argentina
Andean Geology 42 (3): 349-363. September, 2015 Andean Geology doi: 10.5027/andgeoV42n3-a0410.5027/andgeoV40n2-a?? www.andeangeology.cl A new Early Jurassic marine locality from southwestern Chubut Basin, Argentina * S. Mariel Ferrari1, Santiago Bessone1 1 Centro Nacional Patagónico (CENPAT), Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Boulevard A. Brown 2915, Puerto Madryn 9120, Chubut, Argentina. [email protected]; [email protected] * Corresponding author: [email protected] ABSTRACT. A shallow marine invertebrate association is reported from a new Early Jurassic locality namely La Casilda, which is situated in the southwestern region of the Chubut Basin (Patagonia, Argentina). The marine deposits of La Casilda are located in the Río Genoa valley and bear a diverse invertebrate fauna including bivalves, gastropods, brachiopods, echinoderms and corals. A preliminary taxonomic analysis of the invertebrate fauna suggests that La Casilda deposits belong to the Mulanguiñeu Formation of late Pliensbachian-early Toarcian age, and may be coeval with those from the marine localities previously sampled in other regions of the Río Genoa valley. The preliminary results of a biodiversity analysis displayed that La Casilda is one of the most diverse localities at the Chubut Basin and could be assigned to the biofacies at the mixed siliciclastic-carbonate ramp proposed for the marine Early Jurassic at the Andean Basin of northern Chile. The evolution of the marine transgression during the early Pliensbachian-early Toarcian is also interpreted here in a time scale based on ammonite faunas, giving a preliminary temporal reconstruction of the entire Chubut Basin. Keywords: Invertebrates, La Casilda, Mulanguiñeu Formation, Chubut Basin, Argentina. -
A Pterosaur from the Toarcian (Early Jurassic) of the Ardennes (Northeastern France) Eric Buffetaut, Bernard Gibout, Danielle Drouin
A pterosaur from the Toarcian (Early Jurassic) of the Ardennes (northeastern France) Eric Buffetaut, Bernard Gibout, Danielle Drouin To cite this version: Eric Buffetaut, Bernard Gibout, Danielle Drouin. A pterosaur from the Toarcian (Early Jurassic) of the Ardennes (northeastern France). Carnets de Geologie, Carnets de Geologie, 2009, CG2010 (L01), pp.1-6. hal-00458144 HAL Id: hal-00458144 https://hal.archives-ouvertes.fr/hal-00458144 Submitted on 19 Feb 2010 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. Carnets de Géologie / Notebooks on Geology - Letter 2010/01 (CG2010_L01) A pterosaur from the Toarcian (Early Jurassic) of the Ardennes (northeastern France) [Un ptérosaure dans le Toarcien (Jurassique inférieur) des Ardennes (NE de la France)] 1 Eric BUFFETAUT 2 Bernard GIBOUT 3 Danielle DROUIN Abstract: A pterosaur tibia-fibula is described from Toarcian shales ("Marne de Flize") near the city of Charleville-Mézières (Ardennes, northeastern France). The morphology of this element, especially the reduced fibula partially fused to the tibia, suggests that it belongs to the rhamphorhynchid Dorygnathus, which is well represented in the Toarcian Posidonienschiefer of Germany and has also been reported from the Toarcian of Nancy (eastern France). -
Synthe,Sis of Calcareous Nannofossil Events in Tethyan Lower and Middle Jurassic Successions
Rivista Italiana di Paleontologìa e Stratigrafia SYNTHE,SIS OF CALCAREOUS NANNOFOSSIL EVENTS IN TETHYAN LOWER AND MIDDLE JURASSIC SUCCESSIONS EMANUELA MATTIOLIl 8. ELISABETTA ERBA2 Recebed March 18, /999; accepted September 2t, 1999 Key-uords: Calcareous nannofossils, biostratigraphl', Lower posto per l'intervallo Hettangiano-Batoniano sono srxri disrinti 4/ and Middie Juriissic, Te thys, Mcdrtcrrancan Province. eventi principàI basati su t;rxa resistcnti alla diagenesi e comuni, 17 eventi basati su taxa rari raa ubiqtiitari, e 12 eventi potenziaL che Abstact. This paper is a synthesis of calcareous nannofossil richiedono ulterrori controlli:r causa di problerni tassonomici e dis- biostretigrephy' for the Lower and Middle Jurassic of the Mediter- tribuzione sporadica. Vienc inoitre proposto per l'area retide:ì LÌno ranean Province based on several sections from Northern and Central schema biostratigrafico consistentc in i1 zone e 15 sorrozone Italy. Nannofossil events rvere calibrated n'ith ammonite biostratigra- La biostratigrafia propost:r é stara confronrate con recenti sin- phy and, when necessary ammonite-controlled sections in South East tesi biostratigrafiche conpilate per Portogallo, Marocco, Svizzera e ii Fr;rnce were incorporated. Data derive from previously published bio- Regno Boreale e sono stati ìnclividuatr 2Z er.enti riproducibili nelle strxtigrxphies and unpublished data of the authors. varie regioni. Il diacronisrno di rnolti bio-orizzontr é, e nostro awrso, 'I'he large data-set allowed estirnates of reliability and repro- apparente e dovuto essenzialmcnte elle diverse zoneziom ad Anmoni- ducibilitl' of single events. As r result, in the Hetr:rngran-Bathonian ti utilizzate in varie aree. In Italia/Francia, é possibile ottenere un' alta interval x.e propose 4/ nain events based on diagenesis-resistant and risoluzione stratigrafica per l'inten'allo Pliensbachiano-Baiociano. -
A Synoptic Review of the Vertebrate Fauna from the “Green Series
A synoptic review of the vertebrate fauna from the “Green Series” (Toarcian) of northeastern Germany with descriptions of new taxa: A contribution to the knowledge of Early Jurassic vertebrate palaeobiodiversity patterns I n a u g u r a l d i s s e r t a t i o n zur Erlangung des akademischen Grades eines Doktors der Naturwissenschaften (Dr. rer. nat.) der Mathematisch-Naturwissenschaftlichen Fakultät der Ernst-Moritz-Arndt-Universität Greifswald vorgelegt von Sebastian Stumpf geboren am 9. Oktober 1986 in Berlin-Hellersdorf Greifswald, Februar 2017 Dekan: Prof. Dr. Werner Weitschies 1. Gutachter: Prof. Dr. Ingelore Hinz-Schallreuter 2. Gutachter: Prof. Dr. Paul Martin Sander Tag des Promotionskolloquiums: 22. Juni 2017 2 Content 1. Introduction .................................................................................................................................. 4 2. Geological and Stratigraphic Framework .................................................................................... 5 3. Material and Methods ................................................................................................................... 8 4. Results and Conclusions ............................................................................................................... 9 4.1 Dinosaurs .................................................................................................................................. 10 4.2 Marine Reptiles ....................................................................................................................... -
Non-Marine Carbon-Isotope Stratigraphy of the Triassic-Jurassic
Earth-Science Reviews 210 (2020) 103383 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Review article Non-marine carbon-isotope stratigraphy of the Triassic-Jurassic transition in T the Polish Basin and its relationships to organic carbon preservation, pCO2 and palaeotemperature ⁎ Grzegorz Pieńkowskia, , Stephen P. Hesselbob, Maria Barbackac,e, Melanie J. Lengd,f a Polish Geological Institute – National Research Institute, Rakowiecka 4, PL-00-975 Warszawa, Poland b Camborne School of Mines and Environment and Sustainability Institute, University of Exeter, Penryn TR10 9FE, UK c W. Szafer Institute of Botany, PAN, ul. Lubicz 46, PL- 31-512 Kraków, Poland d National Environmental Isotope Facility, British Geological Survey, Nottingham NG12 5GG, UK e Department of Botany, Hungarian Natural History Museum, H-1476 Budapest, P.O. Box 222, Hungary f Centre for Environmental Geochemistry, School of Biosciences, University of Nottingham, LE12 5RD, UK ARTICLE INFO ABSTRACT 13 Keywords: New carbon-isotope data obtained from homogenous organic material (separated microfossil wood; δ Cwood) Chemostratigraphy from the upper Rhaetian and entire Lower Jurassic permit chemostratigraphic correlation of these marginal/ Correlation non-marine deposits with the biostratigraphically well-constrained Llanbedr (Mochras Farm) core in N Wales Paralic facies and other marine profiles, supported by sequence stratigraphic correlation and biostratigraphical markers. Palaeoclimate 13 Statistically significant (Rs = 0.61) positive exponential correlation between δ Cwood values and continental Carbon isotopes 13 TOC (TOCcont) concentrations occurs and can be defined empirically by equation. Changes of δ Cwood observed 13 in C3 plants depends on δ CO2 of atmosphere and can be modulated by other factors such as pCO2 causing fractionation (enrichment in 12C) of C isotopes in source C3 plants and, to lesser extent, by soil moisture content. -
A New Stratigraphic Scheme for the Early Jurassic of Northern Switzerland
Swiss J Geosci (2011) 104:97–146 DOI 10.1007/s00015-011-0057-1 The Staffelegg Formation: a new stratigraphic scheme for the Early Jurassic of northern Switzerland Achim G. Reisdorf • Andreas Wetzel • Rudolf Schlatter • Peter Jordan Received: 20 March 2010 / Accepted: 10 January 2011 / Published online: 3 May 2011 Ó Swiss Geological Society 2011 Abstract The deposits of the Early Jurassic in northern sediments in northern Switzerland between the Doubs Switzerland accumulated in the relatively slowly subsiding River and Mt. Weissenstein in the west and the Randen transition zone between the southwestern part of the Hills located north of the city of Schaffhausen in the east. Swabian basin and the eastern part of the Paris basin under The Staffelegg Formation starts within the Planorbis zone fully marine conditions. Terrigenous fine-grained deposits of the Hettangian. The upper boundary to the overlying dominate, but calcarenitic and phosphorit-rich strata are Aalenian Opalinus-Ton is diachronous. The lithostrati- intercalated. The total thickness varies between 25 and graphic names previously in use have been replaced by 50 m. In the eastern and central parts of N Switzerland, new ones, in accordance within the rules of lithostrati- sediments Sinemurian in age constitute about 90% of the graphic nomenclature. The Staffelegg Formation comprises total thickness. To the West, however, in the Mont Terri 11 members and 9 beds. Several of these beds are impor- area, Pliensbachian and Toarcian deposits form 70% of the tant correlation horizons in terms of allostratigraphy. Some total thickness. Stratigraphic gaps occur on a local to of them correspond to strata or erosional unconformities regional scale throughout N Switzerland. -
Applications of Palaeontology: Techniques and Case Studies Robert Wynn Jones Index More Information
Cambridge University Press 978-1-107-00523-5 - Applications of Palaeontology: Techniques and Case Studies Robert Wynn Jones Index More information Index Bold type indicates figures. Abathomphalus 2.6 Alveolophragmium (Reticulophragmium) anoxia, anoxic environments, events 125, Abdur Reef Limestone 334 4.6 126, 160, 215, 223–4, 278 Abies 192 Alveovalvulina 129, 286, 5.37 Antarctica 100, 267, 306 Abundance 153, 154 Amacuro member 5.47 Antarcticycas 100 Acadoparadoxides 39 Amaltheus 2.14 Antedon 115 Acanthinula 107, 333 Amaurolithus 2.4 Anthocyrtidium 2.7 Acanthocircus 99 Amazon fan 138, 208, 211 Anthracoceras 109, 305 Acarinina 2.6 AZTI Marine Biotic Index (AMBI) 313 Anthraconauta 305, 7.2 Acaste 112 Ammoastuta 126 Anthraconia 305, 7.2 accelerator mass spectrometry (AMS) Ammobaculites 126, 2.33, 3.3, 5.21 Anthracosia 7.2 68, 309 Ammodiscus 129, 2.33, 3.3, 5.23 Anthracomya 305 Acheulian, culture 198, 333, 334, 337 Ammolagena 5.23 Anthracosphaerium 7.2 acritarchs 15–16, 18–9, 95–6, 2.1, 3.1–3.2 Ammomarginulina 126, 5.23 Antler basin 105 Acropora 134, 135, 314 Ammonia 126, 129, 326, 5.37 Apectodinium 180, 5.22 Acrosphaera 99 ammonites 2.14–2.17, 2.30, 5.9 Apodemus 188, 10.2 Acroteuthis 152 ammonoids 34, 108–10, 2.1, 2.12, 3.1 Appalachian basin 302 Actinocamax 111, 2.18 Ammotium 126 Apringia 105 Actinocyclus 2.3 amphibians 53–5, 118, 2.1, 3.1 Aquilapollenites 100, 149 Adentognathus 105 Amphirhopalon 2.7 Aquitaine basin 182 Adercotryma 2.33, 5.23 Amphisorus 126, 3.10 Aqra Limestone formation 220 Adipicola 141 Amphistegina 127, 3.10 Arab formation -
Jurassic (170 - 199 Ma Time-Slice) Time
Early Jurassic (170 - 199 Ma time-slice) Time ScaLe R Creator CHRONOS Cen Mesozoic Updated by James G. Ogg (Purdue University) and Gabi Ogg to: GEOLOGIC TIME SCALE 2004 (Gradstein, F.M., Ogg, J.G., Smith, A.G., et al., 2004) and The CONCISE GEOLOGIC TIME SCALE (Ogg, J.G., Ogg, G., and Gradstein, F.M., 2008) Paleozoic Sponsored, in part, by: Precambrian ICS Based, in part, on: CENOZOIC-MESOZOIC BIOCHRONOSTRATIGRAPHY: JAN HARDENBOL, JACQUES THIERRY, MARTIN B. FARLEY, THIERRY JACQUIN, PIERRE-CHARLES DE GRACIANSKY, AND PETER R. VAIL,1998. Mesozoic and Cenozoic Sequence Chronostratigraphic Framework of European Basins in: De Graciansky, P.- C., Hardenbol, J., Jacquin, Th., Vail, P. R., and Farley, M. B., eds.; Mesozoic and Cenozoic Sequence Stratigraphy of European Basins, SEPM Special Publication 60. Standard Geo- Ammonites Sequences Ammonites Sequences Smaller Benthic Foraminifers Larger Benthic Foraminifers Calcareous Nannofossils Dinoflagellate Cysts Radiolarians Belemnites Brachiopods Ostracodes Charophytes Stage Age Chronostratigraphy magnetic North Atlantic Tethys Age Polarity Sequences Boreal Sequences T-R Major T-R Period Epoch Stage Substage Boreal Boreal T-R Cycles Tethyan Global, Tethyan Cycles Cycles Zones Tethyan markers Zones Zonal Markers Zonal Markers Zones Boreal Zonal Markers Other Boreal Nannofossils Zones Zonal Markers Other Dinocysts Tethyan Dinocysts Zones Zonal Markers NW Europe Boreal Tethyan Boreal Ostracodes Tethyan Ostracodes Markers Lt. Bajoc. Strenoceras niortense Teloceras banksi Strenoceras niortense Teloceras banksi DSJ14 Lithodinia valensii Belemnopsis Lissajouthyris Lissajouthyris [un-named] 169.8 Stephanolithion speciosum Mancodinium semitabulatum, 169.8 L. galeata mg P., speciosum Durotrigia daveyi, Phallocysta apiciconus matisconensis matisconensis Glyptocythere scitula Teloc. blagdeni Bj3 Telo. blagdeni Bj3 NJ10 Andromeda depressa, G. -
Biostor-118662.Pdf
/v^ GL''i£. The stratigraphy and ammonite fauna of the Upper Lias of Northamptonshire ,^^ UBRAR'' M. K. Howarth Department of Palaeontology, British Museum (Natural History), Cromwell Road, London SW7 5BD Contents Abstract 235 Introduction . 236 Acknowledgements 237 Stratigraphical succession 237 The Yorkshire coast 243 Zonal subdivisions and correlation with Yorkshire 244 Correlations with other areas .... 246 England ....... 246 Southern France, the Alps and Italy . 247 North-eastern Siberia, northern Alaska, arctic Canada, Greenland, Spitzbergen 249 Palaeontology ..... 249 Family Dactylioceratidae Hyatt 249 Genus Dactylioceras Hyatt 252 Subgenus Orthodactylites Buckman 253 Dactylioceras {Orthodactylites) semiannulatum sp. nov. 253 Genus Nodicoeloceras Buckman . 256 Nodicoeloceras crassoides (Young & Bird) 256 Genus Peronoceras Hyatt .... 259 Peronoceras fibulatiim (J. de C. Sowerby) 260 Peronoceras turriculatum (Simpson) 262 Peronoceras subarmatum (Young & Bird) 262 Peronoceras perarmatum (Young & Bird) 263 Genus Zugodactylites Buckman . 264 Zugodactylites braUnianus (d'Orbigny) 268 Zugodactylites rotundiventer Buckman . 273 Zugodactylites thompsoni sp. nov. 274 Zugodactylites pseudobraunianus (Monestier) 276 Genus Porpoceras Buckman 278 Porpoceras vortex (Simpson) 280 References ....... 281 Index ........ 284 Abstract The Upper Lias of Northamptonshire is redescribed from a now obscured exposure of the 3 m of lime- stones and clays, up to the Upper Cephalopod Bed, that could formerly be seen above the Marlstone Rock Bed in a quarry near Byfield, and from Beeby Thompson's descriptions and collections from the overlying 50 m of clays that were exposed in numerous 19th-century brickpits around Northampton. The three lowest subzones of the Upper Lias occur in the top 1 m of the Marlstone Rock Bed. This is overlain by the Transition Bed of Semicelatum Subzone age and the Abnormal Fish Bed of Exaratum Subzone age. -
September 16, 2011: Oh My (Brittle) Stars! Again Ms. Brett and I Drove
September 16, 2011: Oh My (Brittle) Stars! Again Ms. Brett and I drove by many Hochsitz lining area corn fields and showed up right on time at 9 a.m. to meet with our fossil guide, Wolfgang Mages, once again in the Plattenkalk limestone, but this time slightly higher in section, still Tithonian, 146 MYA. Our quarry this time: Sinosura kelheimense and Ophioptera lithographica brittlestars. And once again characteristic of the Solnhofen area, hard digging was required to lay hands on prized fossils. The site had been worked hard by others for quite some time, so Wolfgang found the need to hunt around a bit to locate an accessible portion of the very specific brittlestar bearing layers which were 1.5 cm apart. In the meantime Brett and I messed around splitting slabs on the spoil piles, and in the process I located first the front half of a small fish, then a slab of several brittlestars…nice find, but coming from a spoil pile, it left me no direction in making more similar finds as all the limestone looked the same. FIGS 471-472: Wolfgang Mages and the author this and next page (Site 567) FIG 473: Wolfgang Mages and Ms. Brett (Site 567) FIGS 474-476: The author and Klaus working the pit, this and next 2 pages (Site 567) FIG 477: Partial fish Tharsis dubius (Site 567) This was becoming hard work, and Brett was still sick, so she elected to retire to the Mietwagen. Wolfgang was a hard digger and his example motivated me to do the same, and at about that time another local collector named Klaus showed up with his dog and we all (well maybe not the dog) jumped into a hole in the ground and proceeded to removed cubic meters of overburden to access the brittlestar layers. -
First Record of the Leptonectid Ichthyosaur Eurhinosaurus Longirostris from the Early Jurassic of Switzerland and Its Stratigraphic Framework
Swiss J Geosci (2011) 104:211–224 DOI 10.1007/s00015-011-0069-x First record of the leptonectid ichthyosaur Eurhinosaurus longirostris from the Early Jurassic of Switzerland and its stratigraphic framework Achim G. Reisdorf • Michael W. Maisch • Andreas Wetzel Received: 10 May 2010 / Accepted: 10 July 2011 / Published online: 20 September 2011 Ó Swiss Geological Society 2011 Abstract An incomplete skull of the leptonectid ichthy- ‘‘Posidonienschiefer’’, Early Toarcian) and the extraordi- osaur Eurhinosaurus longirostris found in the Rietheim narily high thickness of the Gross Wolf Member Member (previously ‘‘Posidonienschiefer’’; Toarcian, (previously ‘‘Jurensis-Mergel’’, Late Toarcian). Early Jurassic) of Staffelegg, Canton Aargau, is the first record from Switzerland of this taxon and supports the Keywords Ichthyosauridae Á Lias Á Toarcian Á status of Eurhinosaurus longirostris as a palaeobiogeo- Staffelegg Formation Á Catacoeloceras raquinianum graphic very widespread ichthyosaur species in the Early Toarcian of Western Europe. Being from either the Bifrons or Variabilis zone, it is one of the youngest records of Eurhinosaurus and one of the few diagnostic ichthyosaur Zusammenfassung Von der Staffelegg (Kanton Aargau, finds from this time interval. The partial skull is well N-Schweiz) wird ein unvollsta¨ndiger Scha¨del, des lepto- articulated and preserved three-dimensionally in a car- nectiden Ichthyosauriers Eurhinosaurus longirostris aus bonate concretion. Both the mode of preservation of the dem Rietheim-Member (bisher ‘‘Posidonienschiefer’’, ichthyosaur and an associated ammonoid (Catacoeloceras Toarcium, Fru¨h-Jura) beschrieben. Das Fossil repra¨sentiert raquinianum) provided the age of the concretion, which den ersten Nachweis dieses weitverbreiteten Taxons aus had been collected from scree. Taphocoenosis and der Schweiz und ist auch aufgrund seines stratigraphischen taphonomy show the C.