The Saga of Tetrapod Tracks, Trackmakers and Trackers in Italy
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Guide to Proper Names and References in Gödel's “Protokolle
Guide to proper names and references in Gödel’s “Protokolle” notebook People Abel Othenio Abel (1875-1946) professor of paleontology and paleobiology at the University of Vienna. Founder of the group of professors known as the “Bärenhöhle” that blocked the appointment and promotion of Jews Adele Adele Nimbursky, née Porkert (1899–1981), Gödel’s girlfriend, separated from her first husband; she and Gödel would marry in September 1938 Bachmann Friedrich Bachmann (1909–1982), mathematician, doctoral student of Scholz’s at Münster, where he received his Ph.D. in 1933; from 1935 at University of Marburg, as assistant then Privatdozent Behmann Heinrich Behmann (1891–1970), German mathematician; his reply to Perelman’s criticism of Gödel’s result had appeared in the journal Mind in April 1937. He was dismissed from his position at the University of Halle after the war for his Nazi Party activities Beer Gustav Beer, member of the Vienna Circle and Menger’s Mathematical Colloquium Benjamin Abram Cornelius Benjamin (1897–1968), American philosopher of science on the University of Chicago faculty 1932 to 1945 Bernays Paul Bernays (1888–1977), Swiss mathematician and logician; close collaborator with David Hilbert on the foundations of mathematics and the axiomatization of set theory Brentano Franz Brentano (1838-1917), resigned as priest, Professor of Philosophy at the University of Vienna, founder of Gestalt Brunsvick Egon Brunswik (1903–1955), Hungarian-born psychologist, assistant to Karl Bühler in Vienna, active member of Otto Neurath’s “Unity of Science” movement Bühler Karl Bühler (1879–1963), professor of psychology at the University of Vienna. He led an effort to reorganize Vienna’s city schools by incorporating scientific findings from child psychology. -
First Report of Swimming Trace Fossils of Fish from the Upper Permian and Lower Triassic of the Dolomites (Italy)
Annales Societatis Geologorum Poloniae (2018), vol. 88: ...–... doi: https://doi.org/10.14241/asgp.2018.013 FIRST REPORT OF SWIMMING TRACE FOSSILS OF FISH FROM THE UPPER PERMIAN AND LOWER TRIASSIC OF THE DOLOMITES (ITALY) Ausonio RONCHI1, Giuseppe SANTI1, Lorenzo MARCHETTI 2, Massimo BERNARDI 3 & Piero GIANOLLA4 1 Dipartimento di Scienze della Terra e dell’Ambiente, University of Pavia, Italy; e-mails: [email protected]; [email protected] 2 Urweltmuseum GEOSKOP/Burg Lichtenberg (Pfalz), Thallichtenberg, Germany; e-mail: [email protected] 3 MUSE – Museo delle Scienze, Trento, Italy; e-mail: [email protected] 4 Dipartimento di Fisica e Scienze della Terra, University of Ferrara, Italy; e-mail: [email protected] Ronchi, A., Santi, G., Marchetti, L, Bernardi, M. & Gianolla, R., 2018. First report of swimming trace fossils of fish from the Upper Permian and Lower Triassic of the Dolomites (Italy). Annales Societatis Geologorum Poloniae, 88: xxx-xxx Abstract: In the Upper Permian continental to marginal-marine succession of the Southern Alps (Dolomites, north Italy), the ichnological record consists of diverse vertebrate footprints and non-diverse invertebrate trace fossils, mainly occurring in the “Bletterbach ichnoassociation” of the Val Gardena Sandstone Formation. After the Perm- ian-Triassic Boundary event, vertebrate ichnoassociations are scarce until the Middle Triassic (Anisian), whereas the uppermost Permian–Lower Triassic Werfen Formation preserves a rich invertebrate trace-fossil record. To date, fish body and trace fossils (Undichna) are very rare in the pre- and post-extinction deposits of the Dolomites; only Undichna gosiutensis Gibert, 2001 was identified in the “Voltago Conglomerate” (Middle Anisian), whereas some unidentified fossil fish casts were found in the Permian Val Gardena Sandstone and some fish remains in the overlying Werfen Formation. -
GUIDEBOOK the Mid-Triassic Muschelkalk in Southern Poland: Shallow-Marine Carbonate Sedimentation in a Tectonically Active Basin
31st IAS Meeting of Sedimentology Kraków 2015 GUIDEBOOK The Mid-Triassic Muschelkalk in southern Poland: shallow-marine carbonate sedimentation in a tectonically active basin Guide to field trip B5 • 26–27 June 2015 Joachim Szulc, Michał Matysik, Hans Hagdorn 31st IAS Meeting of Sedimentology INTERNATIONAL ASSOCIATION Kraków, Poland • June 2015 OF SEDIMENTOLOGISTS 225 Guide to field trip B5 (26–27 June 2015) The Mid-Triassic Muschelkalk in southern Poland: shallow-marine carbonate sedimentation in a tectonically active basin Joachim Szulc1, Michał Matysik2, Hans Hagdorn3 1Institute of Geological Sciences, Jagiellonian University, Kraków, Poland ([email protected]) 2Natural History Museum of Denmark, University of Copenhagen, Denmark ([email protected]) 3Muschelkalk Musem, Ingelfingen, Germany (encrinus@hagdorn-ingelfingen) Route (Fig. 1): From Kraków we take motorway (Żyglin quarry, stop B5.3). From Żyglin we drive by A4 west to Chrzanów; we leave it for road 781 to Płaza road 908 to Tarnowskie Góry then to NW by road 11 to (Kans-Pol quarry, stop B5.1). From Płaza we return to Tworog. From Tworog west by road 907 to Toszek and A4, continue west to Mysłowice and leave for road A1 then west by road 94 to Strzelce Opolskie. From Strzelce to Siewierz (GZD quarry, stop B5.2). From Siewierz Opolskie we take road 409 to Kalinów and then turn we drive A1 south to Podskale cross where we leave south onto a local road to Góra Sw. Anny (accomoda- for S1 westbound to Pyrzowice and then by road 78 to tion). From Góra św. Anny we drive north by a local road Niezdara. -
The Schio-Vicenza Fault System (NE Italy)
https://doi.org/10.5194/se-2021-29 Preprint. Discussion started: 22 April 2021 c Author(s) 2021. CC BY 4.0 License. Geodynamic and seismotectonic model of a long-lived transverse structure: The Schio-Vicenza Fault System (NE Italy) Dario Zampieri1, Paola Vannoli2, Pierfrancesco Burrato2 1Dipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italy 5 2Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma 1, Rome, Italy Correspondence to: Pierfrancesco Burrato ([email protected]) Abstract. We make a thorough review of geological and seismological data on the long-lived Schio-Vicenza Fault System (SVFS) in northern Italy and present for it a geodynamic and seismotectonic interpretation. The SVFS is a major and high angle structure transverse to the mean trend of the Eastern Southern Alps fold-and-thrust belt, 10 and the knowledge of this structure is deeply rooted in the geological literature and spans for more than a century and a half. The main fault of the SVFS is the Schio-Vicenza Fault (SVF), which has a significant imprint in the landscape across the Eastern Southern Alps and the Veneto-Friuli foreland. The SVF can be divided into a northern segment, extending into the chain north of Schio and mapped up to the Adige Valley, and a southern one, coinciding with the SVF proper. The latter segment borders to the east the Lessini, Berici Mts. and Euganei Hills block, separating this foreland structural high from the 15 Veneto-Friuli foreland, and continues southeastward beneath the recent sediments of the plain via the blind Conselve-Pomposa fault. The structures forming the SVFS have been active with different tectonic phases and different style of faulting at least since the Mesozoic, with a long-term dip-slip component of faulting well defined and, on the contrary, the horizontal component of the movement not well constrained. -
Tectonics of the Dolomites
Tectonics of the Dolomites Autor(en): Doglioni, Carlo Objekttyp: Article Zeitschrift: Bulletin für angewandte Geologie Band (Jahr): 12 (2007) Heft 2 PDF erstellt am: 26.09.2021 Persistenter Link: http://doi.org/10.5169/seals-226374 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. Das Veröffentlichen von Bildern in Print- und Online-Publikationen ist nur mit vorheriger Genehmigung der Rechteinhaber erlaubt. Die systematische Speicherung von Teilen des elektronischen Angebots auf anderen Servern bedarf ebenfalls des schriftlichen Einverständnisses der Rechteinhaber. Haftungsausschluss Alle Angaben erfolgen ohne Gewähr für Vollständigkeit oder Richtigkeit. Es wird keine Haftung übernommen für Schäden durch die Verwendung von Informationen aus diesem Online-Angebot oder durch das Fehlen von Informationen. Dies gilt auch für Inhalte Dritter, die über dieses Angebot zugänglich sind. Ein Dienst der ETH-Bibliothek ETH Zürich, Rämistrasse 101, 8092 Zürich, Schweiz, www.library.ethz.ch http://www.e-periodica.ch Bull, angew. Geol. Vol. 12/2 Dezember 2007 S.11-15 Tectonics of the Dolomites Carlo Doglioni1 Keywords: Southern Alps, thrust belt, Mesozoic tectonics, Alpine tectonics The Dolomites are a part of the Alps, and The Mesozoic extension is particularly therefore they recorded the subduction evident already from the general geologic map history of this orogeny (e. -
Permophiles Issue
Table of Contents Notes from the SPS Secretary 1 Lucia Angiolini Notes from the SPS Chair 2 Shuzhong Shen Officers and Voting Members since August, 2012 2 Report on the First International Congress on Continental Ichnology [ICCI-2015], El Jadida, Morocco, 21-25 April, 2015 4 Hafid Saber Report on the 7th International Brachiopod Congress, May 22-25, 2015 Nanjing, China 8 Lucia Angiolini Progress report on correlation of nonmarine and marine Lower Permian strata, New Mexico, USA 10 Spencer G. Lucas, Karl Krainer, Daniel Vachard, Sebastian Voigt, William A. DiMichele, David S. Berman, Amy C. Henrici, Joerg W. Schneider, James E. Barrick Range of morphology in monolete spores from the uppermost Permian Umm Irna Formation of Jordan 17 Michael H. Stephenson Palynostratigraphy of the Permian Faraghan Formation in the Zagros Basin, Southern Iran: preliminary studies 20 Amalia Spina, Mohammad R. Aria-Nasab , Simonetta Cirilli, Michael H. Stephenson Towards a redefinition of the lower boundary of the Protochirotherium biochron 22 Fabio Massimo Petti, Massimo Bernardi, Hendrik Klein Preliminary report of new conodont records from the Permian-Triassic boundary section at Guryul ravine, Kashmir, India 24 Michael E. Brookfield, Yadong Sun The paradox of the end Permian global oceanic anoxia 26 Claudio Garbelli, Lucia Angiolini, Uwe Brand, Shuzhong Shen, Flavio Jadoul, Karem Azmy, Renato Posenato, Changqun Cao Late Carboniferous-Permian-Early Triassic Nonmarine-Marine Correlation: Call for global cooperation 28 Joerg W. Schneider, Spencer G. Lucas Example for the description of basins in the CPT Nonmarine-Marine Correlation Chart Thuringian Forest Basin, East Germany 28 Joerg W. Schneider, Ralf Werneburg, Ronny Rößler, Sebastian Voigt, Frank Scholze ANNOUNCEMENTS 36 SUBMISSION GUIDELINES FOR ISSUE 62 39 Photo 1:The Changhsingian Gyaniyma Formation (Unit 8, bedded and Unit 9, massive, light) at the Gyaniyma section, SW Tibet. -
Venetian Prealps, Italy) Pogledi Na Razvoj Pomembnega Geo-Ekosistema V Gorah Lessini (Beneške Predalpe, Italija)
COBISS: 1.01 Aspects of the evolution of an important geo-ecosYstem in the Lessinian Mountain (Venetian Prealps, ItalY) Pogledi na razvoj pomembnega geo-ekosistema V gorah Lessini (Beneške Predalpe, Italija) Leonardo Latella1 & Ugo Sauro2 Abstract UDC 551.442:574.4 (234.323.4) Izvleček UDK 551.442:574.4 (234.323.4) Leonardo Latella & Ugo Sauro: Aspects of the evolution of an Leonardo Latella & Ugo Sauro: Pogledi na razvoj pomembne- important geo-ecosystem in the Lessinian Mountain (Venetian ga geo-ekosistema v gorah Lessini (Beneške Predalpe, Italija) Prealps, Italy) Jama Grotta dell’Arena (476 V/VR) v gorah Lessini, 1512 m The Grotta dell’Arena (476 V/VR), located in the Lessinian n.m., je zelo pomemben podzemeljski kraški sistem. Čeprav Mountain, at the elevation of 1512 m a.s.l., is a very important je dolga le 74 m, vsebuje geološke, geomorfološke in okoljske underground karst system. Although it is only 74 m long, sev- elemente, značilne za kraško podzemlje Visokih Lessini. Grot- eral of the geological, geomorphological and environmental ta dell’Arena ima nekaj geoloških in favnističnih značilnosti features of the High Lessinian underground karst are present in skupnih z drugimi pomembnimi in znanimi kraškimi sistemi. this cave. The Grotta dell’Arena shares some common geological Jama je med tistimi z največjim številom troglobiontskih vrst and faunistic characters with other important and well known v vseh Beneških Predalpah, od katerih nekatere verjetno izvi- karst systems. This cave has also one of the highest number of rajo izpred kvartarja. Z geološkega vidika predstavlja jama kon- troglobitic species in all Venetian Prealps and some of them taktni kras, kjer so vzdolž stratigrafskega in tektonskega stika possibly originated in the pre-Quaternary. -
This Article Appeared in a Journal Published by Elsevier. the Attached
(This is a sample cover image for this issue. The actual cover is not yet available at this time.) This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Chemical Geology 322–323 (2012) 121–144 Contents lists available at SciVerse ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo The end‐Permian mass extinction: A rapid volcanic CO2 and CH4‐climatic catastrophe Uwe Brand a,⁎, Renato Posenato b, Rosemarie Came c, Hagit Affek d, Lucia Angiolini e, Karem Azmy f, Enzo Farabegoli g a Department of Earth Sciences, Brock University, St. Catharines, Ontario, Canada, L2S 3A1 b Dipartimento di Scienze della Terra, Università di Ferrara, Polo Scientifico-tecnologico, Via Saragat 1, 44100 Ferrara Italy c Department of Earth Sciences, The University of New Hampshire, Durham, NH 03824 USA d Department of Geology and Geophysics, Yale University, New Haven, CT 06520–8109 USA e Dipartimento di Scienze della Terra, Via Mangiagalli 34, Università di Milano, 20133 Milan Italy f Department of Earth Sciences, Memorial University, St. -
The Dinosaurs of North America
FEOM THE SIXTEENTH ANNUAL KEPOKT OF THE U. S, GEOLOGICAL SURVEY THE DINOSAURS OF NORTH AMERICA OTHNIEL CHARLES MARSH TALE UNIVERSITY WASHINGTON 1896 ^33/^, I/BRAKt 4 ,\ . THE DINOSAURS OF NORTH AMERICA. BY OTHNIEL CHARLES MARSH. 133 CONTENTS. Pajje. Introduction 143 Part I. —Triassic dinosaurs 146 Theropoda 146 Anchisaurida? 147 Anchisaurus 147 The skull 148 The fore limbs 149 The hind limbs 149 Anchisaurus solus 149 Amniosaurus rTT 150 Eestoration of Anchisaurus 150 Dinosaurian footprints 151 Distribution of Triassic dinosaurs 152 Part II. —Jurassic dinosaurs 152 Theropoda : 153 Hallopus 153 Fore and hind limbs 154 Coelurus _ 155 The vertebra:- 155 The hind limbs 156 Ceratosaurus 156 The skull 157 The brain 159 The lower iaws 159 The vertebra: 159 The scapular arch 160 The pelvic arch 160 The metatarsals 162 Eestoration of Ceratosaurus 163 Allosaurus 163 European Theropoda 163 Sauropoda 164 Atlantosaurus beds 164 Families of Sauropoda 165 Atlantosauridie 166 Atlantosaurus 166 Apatosaurus 166 The sacral cavity 166 The vertebra- 167 Brontosaurus 168 The scapular arch 168 The cervical vertebra.- 169 The dorsal vertebree 169 The sacrum 170 The caudal vertebra- 171 The pelric arch 172 The fore limbs 173 The hind limbs 173 135 136 CONTENTS. Part II. —Jurassic dinosaurs—Continued. Page. Sauropoda—Continued. Atlantosaurida? —Continued. Restoration of Brontosaurus 173 Barnsaurus 174 Diplodoeida? 175 Diplodocus 175 The skull 175 The brain 178 The lower jaws 178 The teeth 179 The vertebra; 180 The sternal bones 180 The pelvic girdle 180 Size and habits 180 Morosaurida? 181 Morosaurus 181 The skull 181 The vertebra? 181 The fore limbs 182 The pelvis 182 The hind limbs 183 Pleuroccelida? : 183 Pleurocoelus 183 The skull 183 The vertebras 183 Distribution of the Sauropoda 185 Comparison with European forms 185 Predentata ». -
James Hutton's Reputation Among Geologists in the Late Eighteenth and Nineteenth Centuries
The Geological Society of America Memoir 216 Revising the Revisions: James Hutton’s Reputation among Geologists in the Late Eighteenth and Nineteenth Centuries A. M. Celâl Şengör* İTÜ Avrasya Yerbilimleri Enstitüsü ve Maden Fakültesi, Jeoloji Bölümü, Ayazağa 34469 İstanbul, Turkey ABSTRACT A recent fad in the historiography of geology is to consider the Scottish polymath James Hutton’s Theory of the Earth the last of the “theories of the earth” genre of publications that had begun developing in the seventeenth century and to regard it as something behind the times already in the late eighteenth century and which was subsequently remembered only because some later geologists, particularly Hutton’s countryman Sir Archibald Geikie, found it convenient to represent it as a precursor of the prevailing opinions of the day. By contrast, the available documentation, pub- lished and unpublished, shows that Hutton’s theory was considered as something completely new by his contemporaries, very different from anything that preceded it, whether they agreed with him or not, and that it was widely discussed both in his own country and abroad—from St. Petersburg through Europe to New York. By the end of the third decade in the nineteenth century, many very respectable geologists began seeing in him “the father of modern geology” even before Sir Archibald was born (in 1835). Before long, even popular books on geology and general encyclopedias began spreading the same conviction. A review of the geological literature of the late eighteenth and the nineteenth centuries shows that Hutton was not only remembered, but his ideas were in fact considered part of the current science and discussed accord- ingly. -
(Coleoptera: Staphylinidae) of Val Di Non / Nonstal (Trentino / Südtir
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Gredleriana Jahr/Year: 2015 Band/Volume: 015 Autor(en)/Author(s): Zanetti Adriano Artikel/Article: Second contribution to the knowledge of the rove beetles (Coleoptera: Staphylinidae) of Val di Non / Nonstal (Trentino / Südtirol, Italy) 77-110 Adriano Zanetti Second contribution to the knowledge of the rove beetles (Coleoptera: Staphylinidae) of Val di Non / Nonstal (Trentino / Südtirol, Italy) Abstract A list of 466 species of Staphylinidae collected mostly by the author in Val di Non / Nonstal (Trentino / South Tyrol, Italy) is given. Among them four are new to Italy: Atheta alpigrada, A. reissi, Schistoglossa pseudogemina and Cypha carinthiaca. They are discussed with further 19 species considered relevant for rarity and geographic distribution. The biogeographic analysis shows a prevalence of widely distributed species. Among those with restricted distribution some are characteristic for the Rhaetian Alps, others point out the importance of the Adige river valley as a biogeographic barrier. Some southern Keywords: Staphylinidae, species occur in thermophilous forests and in wetlands. The presence of rare species faunistics, new records, Alps, in protected areas, mostly in “Sites of Community Importance”, is evidenced. Trentino, Italy Introduction The aim of this work is the publication of a large amount of data on rove beetles (Sta- phylinidae), the largest family of Coleoptera (more than 60,000 species described up to date), collected by the author in Val di Non since the sixties of the past century. Year after year, I tried to sample every kind of macro- and microhabitat occurring in that area, with the aim of representing the diversity in this particular valley, which connects the Rhaetian and Dolomitic areas from west to east, and the metamorphic Central Alps and the carbonatic Prealps from north to south. -
AUSTRIAN JOURNAL of EARTH SCIENCES Volume 98 2005
AUSTRIAN JOURNAL of EARTH SCIENCES [MITTEILUNGEN der ÖSTERREICHISCHEN GEOLOGISCHEN GESELLSCHAFT] an INTERNATIONAL JOURNAL of the AUSTRIAN GEOLOGICAL SOCIETY volume 98 2005 Gerd RANTITSCH & Barbara RUSSEGGER: Organic maturation within the Central Northern Calcareous Alps (Eastern Alps)________________________________ www.univie.ac.at/ajes EDITING: Grasemann Bernhard, Wagreich Michael PUBLISCHER: Österreichische Geologische Gesellschaft Rasumofskygasse 23, A-1031 Wien TYPESETTER: Irnberger Norbert, www.irnberger.net Copy-Shop Urban, Bahnstraße 26a, 2130 Mistelbach PRINTER: Holzhausen Druck & Medien GmbH Holzhausenplatz 1, 1140 Wien ISSN 0251-7493 Austrian Journal of Earth Sciences Volume 98 Vienna 2005 Organic maturation within the Central Northern Calca- reous Alps (Eastern Alps) Gerd RANTITSCH1) & Barbara RUSSEGGER2) KEYWORDS very low-grade metamorphism Northern Calcareous Alps 1) Department of Applied Geosciences and Geophysics, Montanuniversität Leoben, vitrinite reflectance Austria, A-8700 Leoben, Austria, Email: [email protected] thermal modeling Jurassic orogeny 2) Library of the University of Graz, A-8010 Graz, Austria Eastern Alps Abstract Organic maturation within the central Northern Calcareous Alps (Eastern Alps) has been investigated using vitrinite reflectance data from Upper Permian to Upper Cretaceous strata of the Stauffen-Höllengebirge Nappe, Dachstein Nappe, Tennengebirge Block and Lammer Unit. Within the Lammer Unit a metamorphic break is observed between the Strubberg Formation and the tectonically overlying