VIMERCATE a Cura Di: R

Total Page:16

File Type:pdf, Size:1020Kb

VIMERCATE a Cura Di: R 1 I S P R A Istituto Superiore per la Protezione e la Ricerca Ambientale SERVIZIO GEOLOGICO D’ITALIA Organo Cartografico dello Stato (legge n°68 del 2.2.1960) NOTE ILLUSTRATIVE della CARTA GEOLOGICA D’ITALIA alla scala 1:50.000 foglio 097 VIMERCATE a cura di: R. Bersezio(1), A. Bini(1), R. Gelati(1), C. Ferliga (2), I. Rigamonti (3), A. Strini (1) con contributi di: A. Rovida(4), G.P. Beretta(1), I. Premoli Silva(1), G. Scardia(5), D. Sciunnach(2), F. Torri(3) (1) Dipartimento di Scienze della Terra, Università di Milano (2) Regione Lombardia (3) Consulente di Regione Lombardia (4) INGV - Milano (5) CNR - IDPA - Milano Ente realizzatore: 2 Direttori del Servizio Geologico d’Italia - ISPRA: C. Campobasso Responsabile del Progetto CARG per il Servizio Geologico d’Italia - ISPRA: F. Galluzzo Direttori della Direzione Generale competente - Regione Lombardia: R. Compiani, M. Presbitero, M. Rossetti, M. Nova, B. Mori, P.I. Baccolo Dirigenti della struttura competente - Regione Lombardia: M. Presbitero, B. Mori, R. Laffi, A. De Luigi, M. Cassin, N. Padovan, D. Fossati e A. Biancardi Responsabili del Progetto CARG per Regione Lombardia: M. Presbitero, A. Piccin Coordinatore scientifico: A. Gregnanin PER IL SERVIZIO GEOLOGICO D’ITALIA - ISPRA Revisione scientifica: R. M. Pichezzi, E. Chiarini, L. Martarelli Coordinamento cartografico: D. Tacchia (coord.), S. Falcetti Revisione informatizzazione dei dati geologici: L. Battaglini, R. Carta, R. M. Pichezzi (ASC) Coordinamento editoriale ed allestimento per la stampa: D. Tacchia, S. Falcetti PER REGIONE LOMBARDIA Coordinamento editoriale e allestimento cartografico: G. B. Siletto, M. Credali Informatizzazione dei dati geologici: coordinamento e direzione lavori: G. B. Siletto, M. Credali informatizzazione: S. Racchetti, F. Torri, F. Mandozzi, M. Cetti, G. Tucci collaudo: a cura di Lombardia Informatica S.P.A Allestimento cartografico per la stampa della Banca Dati a cura di Gestione tecnico-amministrativa del Progetto CARG: M.T. Lettieri (Servizio Geologico d’Italia - ISPRA) G. Mannucci, N. Padovan, A. Piccin, G.B. Siletto, M. Credali e P. Belotti (Regione Lombardia) Si ringraziano i componenti del precedente Comitato Geologico per il loro contributo scientifico 3 I. INTRODUZIONE .......................................................................................................... 7 1. - CRITERI ADOTTATI ........................................................................... 9 1.1 – UNITÀ DISTINTE IN BASE AL BACINO DI APPARTENENZA ...................................... 9 1.2 – UNITÀ NON DISTINTE IN BASE AL BACINO DI APPARTENENZA ............................. 11 II. STUDI PRECEDENTI ................................................................................................ 15 1. - CARTOGRAFIA GEOLOGICA ......................................................... 15 2. - LETTERATURA PRECEDENTE ....................................................... 17 III. INQUADRAMENTO GEOLOGICO ......................................................................... 27 1. - QUADRO GEOLOGICO E STRUTTURALE .................................... 27 2. - DATI DI SOTTOSUOLO .................................................................... 36 3. - SISMICITÀ E CENNI DI NEOTETTONICA ..................................... 41 IV. CARATTERI GEOMORFOLOGICI ........................................................................ 43 V. STRATIGRAFIA ......................................................................................................... 49 1. - LA SUCCESSIONE MESOZOICA PRE-RIFT............................................................ 49 1.1 - DOLOMIA PRINCIPALE (DPR) ........................................................................... 49 1.2 - GRUPPO DELL‟ARALALTA ................................................................................. 50 1.2.1. - Dolomie zonate (DZN) ................................................................................ 51 1.2.2. - Calcare di Zorzino (ZOR) .......................................................................... 51 1.3 - ARGILLITE DI RIVA DI SOLTO (ARS) ................................................................ 52 1.4 - CALCARE DI ZU (ZUU) .................................................................................... 56 1.5 - FORMAZIONE DELL‟ALBENZA (ALZ) ............................................................... 62 1.6 - CALCARE DI SEDRINA (SED) ............................................................................ 67 2. - I PRISMI CARBONATICI SIN-RIFT ................................................. 71 2.1 - CALCARE DI MOLTRASIO (MOT) ..................................................................... 71 2.2 - CALCARE DI DOMARO (DOM) ......................................................................... 76 2.3 - FORMAZIONE DI SOGNO (SOG) ........................................................................ 81 2.4 - SUCCESSIONE GIURASSICA RIDOTTA E CONDENSATA (SGX) .............................. 84 3. - LA SUCCESSIONE POST-RIFT ........................................................ 85 3.1 - SELCIFERO LOMBARDO (SM) ........................................................................... 85 3.1.1. - Radiolariti del Selcifero Lombardo (RSL) .................................................. 86 3.1.2. - Rosso ad Aptici (RAP) ................................................................................ 88 3.2 - MAIOLICA (MAI) ............................................................................................. 91 4. - LA SUCCESSIONE CLASTICA CRETACICA DEL BACINO LOMBARDO ............................................................................................. 95 4.1 - MARNA DI BRUNTINO (BRU) ........................................................................... 95 4.2 - SASS DE LA LUNA (SDL) .................................................................................. 98 5. - I SISTEMI TORBIDITICI CENOMANIANI .................................... 101 5.1 - FORMAZIONE DI SORISOLE (FSE) ................................................................... 101 4 6. - I SISTEMI TORBIDITICI ED EMIPELAGICI TURONIANI.......... 105 6.1 - FORMAZIONE DI GAVARNO ............................................................................. 106 6.1.1. - Membro delle peliti nere (GVR1) .............................................................. 106 6.1.2. - Membro delle peliti rosse (GVR2) ............................................................ 108 6.2 - FLYSCH DI PONTIDA (PTD) ............................................................................ 111 7. - I SISTEMI TORBIDITICI CONIACIANO-SANTONIANI ............. 114 7.1 - ARENARIA DI SARNICO (SAR) ........................................................................ 114 7.2 - CONGLOMERATO DI SIRONE (CSH) ................................................................ 116 7.2.1. - Membro di Colle Brianza (CSH1) ............................................................. 120 8. - I SISTEMI TORBIDITICI CAMPANIANI ....................................... 121 8.1 - FLYSCH DI BERGAMO (FBG) .......................................................................... 122 8.1.1. - Megastrato di Missaglia (FBGa) ............................................................... 125 8.1.2. - Membro di Rogeno (FBG1) ....................................................................... 126 8.2 - FORMAZIONE DI BRENNO (BNN) .................................................................... 126 9. - I SISTEMI TORBIDITICI PALEOCENICO-EOCENICI ................. 129 9.1 - FORMAZIONE DI TABIAGO (TAB) ................................................................... 129 9.2 - FORMAZIONE DI CIBRONE (IBR) ..................................................................... 133 10. - SUCCESSIONE NEOGENICO-QUATERNARIA ......................... 138 10.1 - UNITÀ DI SOTTOSUOLO ................................................................................. 138 10.1.1. - Supersintema di Vimercate ...................................................................... 138 10.1.2. - Supersintema di Ronco Briantino ............................................................ 138 10.1.3. - Ceppo di Lomagna .................................................................................. 139 10.2 - UNITÀ DI SUPERFICIE .................................................................................... 141 10.2.1. - Unità del Bacino del Serio ...................................................................... 141 10.2.1.1. -Supersintema di Fiorano (FR) ............................................................ 141 10.2.1.2. - Sintema di Torre Boldone (TBO) ...................................................... 142 10.2.1.3. - Supersintema di Grassobbio (BB) ...................................................... 143 10.2.2. - Unità del Bacino della Morla .................................................................. 143 10.2.2.1. - Supersintema della Morla (OR) ......................................................... 144 10.2.3. - Unità del Bacino del Brembo .................................................................. 145 10.2.3.1. - Conglomerato di Cà della Zogna (CZO) ........................................... 145 10.2.3.2. - Formazione di Almenno Basso (AEO) .............................................. 147 10.2.3.3. - Formazione di Cà Marchi (CMH) ..................................................... 150 10.2.3.4. - Formazione di Tornago (TOG).......................................................... 151 10.2.3.5. - Conglomerato
Recommended publications
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • Paléobiologie
    REVUE DE VOLUME 36 (1 ) – 2017 PALÉOBIOLOGIE Une institution Ville de Genève www.museum-geneve.ch Revue de Paléobiologie, Genève (juin 2017) 36 (1) : 169-177 ISSN 0253-6730 Nouvelles données sur la paléobiogéographie des genres Septimaniceras Fauré, 2002 et Crassiceras Merla, 1932 (Ammonitina) du Toarcien moyen Romain JATTIOT1, 2, Louis RULLEAU3 & Benjamin LATUTRIE4 1 Paläontologisches Institut und Museum, Universität Zürich, Karl-Schmid Strasse 4, CH-8006 Zürich, Switzerland. E-mail : [email protected] 2 UMR CNRS 6282 Biogéosciences, Univ. Bourgogne Franche-Comté, 6 Boulevard Gabriel, F-21000 Dijon, France. 3 169 chemin de l’Herbetan, F-69380 Chasselay, France. E-mail : [email protected] 4 Institut National de la Recherche Scientifique, Centre Eau Terre Environnement, 490 Rue de la Couronne, G1K 9A9 Québec, Canada. E-Mail : [email protected] Résumé Depuis sa première description, le genre Septimaniceras Fauré, 2002 a été systématiquement considéré comme un genre endémique, avec une répartition géographique limitée à la région des Causses et du Languedoc (France, province nord-ouest européenne). De même, l’espèce Crassiceras bayani (Dumortier, 1874), d’affinités méditerranéennes, était interprétée comme une forme spécifiquement nord-ouest européenne cantonnée au sud-est de la France, et ne dépassant pas la région lyonnaise en latitude nord. Nous décrivons ici les présences inédites des espèces Septimaniceras pseudoyoungi (Guex, 1972) et Crassiceras bayani dans la sous-zone à Variabilis (Toarcien moyen) de la région de Thouars (ouest de la France). En conséquence, nous étendons considérablement la répartition géogra- phique de ces taxons. Au vu de ces nouvelles données, il est probable que le genre Septimaniceras ait été endémique du sud-est de la France dans la partie supérieure de la sous-zone à Bifrons puis ait étendu son aire de distribution jusqu’à la région de Thouars à la base de la zone à Variabilis.
    [Show full text]
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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 .......................................................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • A Review of the Late Jurassic–Early Cretaceous Charophytes from The
    A review of the Late Jurassic–Early Cretaceous charophytes from the northern Aquitaine Basin in south-west France Roch-Alexandre Benoit, Didier Néraudeau, Carles Martin-Closas To cite this version: Roch-Alexandre Benoit, Didier Néraudeau, Carles Martin-Closas. A review of the Late Jurassic– Early Cretaceous charophytes from the northern Aquitaine Basin in south-west France. Cretaceous Research, Elsevier, 2017, 79, pp.199-213. <10.1016/j.cretres.2017.07.009>. <insu-01574653> HAL Id: insu-01574653 https://hal-insu.archives-ouvertes.fr/insu-01574653 Submitted on 16 Aug 2017 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. Accepted Manuscript A review of the Late Jurassic–Early Cretaceous charophytes from the northern Aquitaine Basin in south-west France Roch-Alexandre Benoit, Didier Neraudeau, Carles Martín-Closas PII: S0195-6671(17)30121-0 DOI: 10.1016/j.cretres.2017.07.009 Reference: YCRES 3658 To appear in: Cretaceous Research Received Date: 13 March 2017 Revised Date: 5 July 2017 Accepted Date: 17 July 2017 Please cite this article as: Benoit, R.-A., Neraudeau, D., Martín-Closas, C., A review of the Late Jurassic–Early Cretaceous charophytes from the northern Aquitaine Basin in south-west France, Cretaceous Research (2017), doi: 10.1016/j.cretres.2017.07.009.
    [Show full text]
  • Preservational History of Compressed Jurassic Ammonites from Southern Germany
    N. Jb. Geol. Paliiont. Abh. 152 3 307—356 | Stuttgart, November 1976 Fossildiagenese Nr. 2 0 9 Preservational history of compressed Jurassic ammonites from Southern Germany By A. Seilacher, F. Andalib, G. Dietl and H. Gocht With 20 figures in the text Seilacher, A., Andalib, F., D ietl, G. 8c G ocht, H.: Preservational history of compressed Jurassic ammonites from Southern Germany. — N. Jb. Geol. Paliiont. Abh., 152, 307—356, Stuttgart 1976. Abstract: Preservational features express the varying time relationships between shell solution, compaction and cementation processes during early diagenesis. In many cases they correlate better with the depositional environments than with the present lithologies of the enclosing rocks. K ey words: Ammonitida, fossilization, diagenesis, deformation, Jurassic; SW-German mesozoic hills. Zusammenfassung: Erhaltungszustande definierter Gehausetypen spiegeln das zeit- liche Verhaltnis von Schalenlosung, Kompaktion und Zementation wahrend der Friih- diagenese. Da sie eher vom Ablagerungsmilieu als vom Stoflbestand des fertigen Gestcins abhangen, konnen sie als Fazies-Indikatoren eingesetzt werden. The beauty of fossils is one of the main attractions in paleontology; but at the same time it tends to distract from the wealth of geologic in­ formation that is encoded in the “poor” specimens. The present study tries to tap this reservoir by using ammonites so poorly preserved that they would have been rejected by most collectors. This project forms part of the program “Fossil-Diagenese” in the Sonderfor- sdiungsbereich “Palokologie”, Tubingen. Support by the Deutsche Forschungsgemein- 9 Nr. 19: J. N eugebauer: Preservation of ammonites. — In: J. W iedmann 8c J. N eugebauer, Lower Cretaceous Ammonites from the South Atlantic Leg 40 (DSDP), their stratigraphic value and sedimentologic properties, Initial Reports Deep Sea Drilling Project, 40, im Druck.
    [Show full text]
  • Stratigraphische Tabelle Von Deutschland 2016
    STD 2016 Stratigraphische Tabelle von Deutschland 2016 Stratigraphic Table of Germany 2016 STG 2016 Deutsche Stratigraphische Kommission DSK Gefördert durch: Globale Stratigraphische Skala www.stratigraphie.de Globale Stratigraphische Skala Sponsered by: STUFE / Regionale Stratigraphische Skala STUFE / Regionale Stratigraphische Skala ALTER ALTER Klimatostratigraphie Lithostratigraphie Klimatostratigraphie Lithostratigraphie Lithostratigraphie Klimatostratigraphie Lithostratigraphie Richels- Grup- Leit- Norddeutschland dorfer NW-Hessen SW-Hessen / Südpfalz Nord- Ober- Ost- Nördliche pe Folge horizont Baden-Württemberg pfalz franken Thüringen Kalkalpen PERIODE SYSTEM ÄRA ÄRATHEM EPOCHE SERIE DAUER Ma Ma ZEIT ÄRA ÄRATHEM PERIODE SYSTEM EPOCHE SERIE DAUER Ma Ma ZEIT Mitteleuropa Norddeutschland NW Norddeutschland SE SW-Deutschland Rhein-Main-System Rheingletscher Bayern (nur Schotter) Gebirge Haupt- gruppe 0 252,5 Schmölln-Fm. z7 Fulda-Formation Friesland-Formation Frankenberg-Fm. Tigersandstein- Speyerbach-Fm. Subatlantikum Dünkirchen Post-Littorina Jüngerer Auenlehm Subatlantikum Subatlantikum z4\ z5\ z6 Ohre-Formation Langen- Ohre-\ Friesl.-Fm. “Meghalayium” Oberhol. CHANGHSING. ≈ Aller-Sulfat Formation Annweiler-Fm. Clarkina 3 z3 Leine-Formation Aller-Formation thal-Fm. Leine-\ Aller-Fm. Spätes H. Dünkirchen-Transgr. (Schieferletten) Rothenberg-Fm. Stauf- Lindau- Hasel- wangi 255 z2 Staßfurt-Formation Geismar-Formation Formation Formation gebirge 0,0042 Subboreal Littorina-Meer Mittlerer Auenlehm Subboreal Subboreal (Conodont) Thüringer
    [Show full text]
  • Bbm:978-3-0348-7827-2/1.Pdf
    Literaturverzeichnis Mit Asterisk bezeichnete Arbeiten sind besonders von Revisionen in systematischer und/oder bio stratigraphischer Hinsicht betroffen, oder dienten als Grundlage für die Korrelation auf Tabelle 4. ACCORSI BENINI, C. & BROGLIO LORIGA, C. (1977): Lithiotis Güm• BOULE, M. & THEVENIN, A. (1906,1907): Types du Prodrome de Pale­ bel, 1871 e Cochlearites Reis, 1903. 1°. Revisione morfologica e ontologie universelle de d'Orbigny. - Ann. Paleont., 1, p. 97-100, tassonomica. - Boll. Soc. paleont ital., 16, 1, p. 15-60. 165-172, 193-196, Taf. 8, 9, 12, 13, 21, 22; 2, p. 89-96, 161-172, AGER, D. V. & CALLOMON, J. H. (1971): On the Liassie age of the Taf. 13,14,23,24. "Bathonian" of Villäny (Baranya). - Ann. Univ. Sei. Budapest BOURDENET, A. M. (1964): Les Pleuroceras du Domerien superieur Eötvös, Sect geo!., 14, p. 5-16. de Charrnoille (Haute-Saöne). - Ann. sei. Univ. Besan~on, (2) 18, ARKELL, W. J. (1956): Jurassie geology of the world. - London and p.3-24. Edinburgh (Oliver & Boyd). *BREMER, H. (1965): Zur Ammonitenfauna und Stratigraphie des ARKELL, W. J., BRAMKAMP, R. A. & STEINEKE, M. (1952): Jurassie unteren Lias (Sinemurium bis Carixium) in der Umgebung von Ammonites from Jebel Tuwaiq, central Arabia. - Phi!. Trans. r. Ankara (Türkei). - N. Jb. Geol. Paläont., Abh., 122, S. 127-221. Soc. London, (B) 236, p. 241-313. BUCKMAN, S. S. (1918): Jurassie chronology: I. Lias. - Quart 1. geol. *ARKELL, W. J., KUMMEL, B. & WRIGHT, C. W. (1957): Mesozoic Soc. London, 73 (1917), p. 257-327. Ammonoidea. In: MOORE, R. C. (Ed.): Treatise on invertebrate - (1909-30): Yorkshire Type Ammonites (ab vol.
    [Show full text]
  • The Marine Jurassic of Argentina: a Biostratigraphic Framework
    326 by Alberto C. Riccardi The marine Jurassic of Argentina: a biostratigraphic framework Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina. Email: [email protected] In Argentina the best and most complete marine Juras- sic succession is exposed between 32° and 39° S, along a N-S belt roughly coincident with the border with Chile. Here all stages, except the Kimmeridgian, are represented by marine facies. Ammonites have provided a biostratigraphic framework to date and correlate lithostratigraphic units and sequences, to reconstruct the history of the marine fill, and allow the development of other palaeontological and geological studies. Recent studies on the systematics and/or biostratigra- phy of Andean ammonites have provided the basis for the presentation of a summary of the 45 ammonite zones of the Jurassic of west-central Argentina and to stress its significance in reconstructing the palaeogeographic evolution of that region. Introduction Jurassic rocks in Argentina are present over extensive areas (see Fig- ure 1) and include a large variety of marine and continental facies (see Riccardi et al., 1992). South of 39°S marine Jurassic consists of Pliensbachian-Lower Toarcian and uppermost Jurassic strata, repre- sented respectively in central and southern Patagonia. North of 39°S marine Jurassic is exposed along a N-S belt roughly coincident with the boundary between Argentina and Chile, up to 31°S where it becomes restricted to Chile. The marine Jurassic generally rests unconformably on Upper Triassic (west-central Argentina) and Upper Jurassic vulcanites (southern Patagonia) or on Upper Paleozoic (west-central Patago- nia).
    [Show full text]