Position of Reference Mammal Localities of the Lower
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Updated Aragonian Biostratigraphy: Small Mammal Distribution and Its Implications for the Miocene European Chronology
Geologica Acta, Vol.10, Nº 2, June 2012, 159-179 DOI: 10.1344/105.000001710 Available online at www.geologica-acta.com Updated Aragonian biostratigraphy: Small Mammal distribution and its implications for the Miocene European Chronology 1 2 3 4 3 1 A.J. VAN DER MEULEN I. GARCÍA-PAREDES M.A. ÁLVAREZ-SIERRA L.W. VAN DEN HOEK OSTENDE K. HORDIJK 2 2 A. OLIVER P. PELÁEZ-CAMPOMANES * 1 Faculty of Earth Sciences, Utrecht University Budapestlaan 4, 3584 CD Utrecht, The Netherlands. Van der Meulen E-mail: [email protected] Hordijk E-mail: [email protected] 2 Departamento de Paleobiología, Museo Nacional de Ciencias Naturales MNCN-CSIC C/ José Gutiérrez Abascal 2, 28006 Madrid, Spain. García-Paredes E-mail: [email protected] Oliver E-mail: [email protected] Peláez-Campomanes E-mail: [email protected] 3 Netherlands Centre for Biodiversity-Naturalis Darwinweg 2, 2333 CR Leiden, The Netherlands. Van den Hoek Ostende E-mail: [email protected] 4 Departamento de Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid. IGEO-CSIC C/ José Antonio Novais 2, 28040 Madrid, Spain. Álvarez-Sierra E-mail: [email protected] * Corresponding author ABSTRACT This paper contains formal definitions of the Early to Middle Aragonian (Late Early–Middle Miocene) small- mammal biozones from the Aragonian type area in North Central Spain. The stratigraphical schemes of two of the best studied areas for the Lower and Middle Miocene, the Aragonian type area in Spain and the Upper Freshwater Molasse from the North Alpine Foreland Basin in Switzerland, have been compared. -
Redalyc.An Updated Biostratigraphy for the Late Aragonian and Vallesian
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España CASANOVAS-VILAR, I.; GARCÉS, M.; VAN DAM, J.; GARCÍA-PAREDES, I.; ROBLES, J.M.; ALBA, D.M. An updated biostratigraphy for the late Aragonian and Vallesian of the Vallès-Penedès Basin (Catalonia) Geologica Acta: an international earth science journal, vol. 14, núm. 3, septiembre, 2016, pp. 195-217 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50547614001 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.14, Nº 3, September 2016, 195-217 DOI: 10.1344/GeologicaActa2016.14.3.1 An updated biostratigraphy for the late Aragonian and Vallesian of the Vallès-Penedès Basin (Catalonia) I. CASANOVAS-VILAR1 M. GARCÉS2,3 J. VAN DAM4,1 I. GARCÍA-PAREDES5 J.M. ROBLES1 D.M. ALBA1 1Institut Català de Paleontologia Miquel Crusafont, Universitat Autònoma de Barcelona Edifici ICTA-ICP, Carrer de les Columnes s/n, Campus de la UAB, 08193 Cerdanyola del Vallès, Barcelona, Spain. Casanovas- Vilar E-mail: [email protected] Van Dam E-mail: [email protected] Robles E-mail: [email protected] Alba E-mail: [email protected] 2Departament de Dinàmica de la Terra i l’oceà, Facultat de Geologia, Universitat de Barcelona Martí i Franqués s/n, 08028 Barcelona, Spain. Garcés E-mail: [email protected] 3Institut Geomodels, Grup de Recerca Consolidat de Geodinàmica i Anàlisis de Conques, Universitat de Barcelona Martí i Franqués s/n, 08028 Barcelona, Spain 4Department of Earth Sciences, Utrecht University Budapestlaan 4, 3584 CD Utrecht, the Netherlands. -
New Data on the Early Villafranchian Fauna from Vialette (Haute-Loire, France) Based on the Collection of the Crozatier Museum (Le Puy-En-Velay, Haute-Loire, France)
ARTICLE IN PRESS Quaternary International 179 (2008) 64–71 New data on the Early Villafranchian fauna from Vialette (Haute-Loire, France) based on the collection of the Crozatier Museum (Le Puy-en-Velay, Haute-Loire, France) Fre´de´ric Lacombata,Ã, Laura Abbazzib, Marco P. Ferrettib, Bienvenido Martı´nez-Navarroc, Pierre-Elie Moulle´d, Maria-Rita Palomboe, Lorenzo Rookb, Alan Turnerf, Andrea M.-F. Vallig aForschungsstation fu¨r Quata¨rpala¨ontologie Senckenberg, Weimar, Am Jakobskirchhof 4, D-99423 Weimar, Germany bDipartimento di Scienze della Terra, Universita` di Firenze, Via G. La Pira 4, 50121 Firenze, Italy cICREA, A`rea de Prehisto`ria, Universitat Rovira i Virgili-IPHES, Plac-a Imperial Tarraco 1, 43005 Tarragona, Spain dMuse´e de Pre´histoire Re´gionale de Menton, Rue Lore´dan Larchey, 06500 Menton, France eDipartimento di Scienze della Terra, Universita` degli Studi di Roma ‘‘La Sapienza’’, CNR, Ple. Aldo Moro, 500185 Roma, Italy fSchool of Biological and Earth Sciences, Liverpool John Moore University, Liverpool L3 3AF, UK g78 rue du pont Guinguet, 03000 Moulins, France Available online 7 September 2007 Abstract Vialette (3.14 Ma), like Sene` ze, Chilhac, Sainzelles, Ceyssaguet or Soleilhac, is one of the historical sites located in Haute-Loire (France). The lacustrine sediments of Vialette are the result of a dammed lake formed by a basalt flow above Oligocene layers, and show a geological setting typical for this area, where many localities are connected with maar structures that have allowed intra-crateric lacustrine deposits to accumulate. Based on previous studies and this work, a faunal list of 17 species of large mammals has been established. -
Ruscinian and Lower Vlllafranchian: Age of Boundaries and Position in Magnetochronological Scale E
Stratigraphy and Geological Correlation, Vol. 13, No. 5, 2005, pp. 530-546. Translated from Stratigrafiya. Geologicheskaya Korrelyatsiya, Vol. 13, No. 5, 2005, pp. 78-95. Original Russian Text Copyright © 2005 by Vangengeim, Pevzner, Tesakov. English Translation Copyright © 2005 by MAIK "Nauka/lnterperiodica ” (Russia). Ruscinian and Lower Vlllafranchian: Age of Boundaries and Position in Magnetochronological Scale E. A. Vangengeim, M. A. Pevzner', and A. S. Tesakov Geological Institute, Russian Academy of Sciences, Moscow Received November 10, 2004; in final form, January 19, 2005 Abstract—Analysis of magnetostrati graphic records and taxonomy of mammalian remains from localities of the terminal Miocene-middle Pliocene in Europe, West Siberia, Mongolia, and China revealed a significant fau nal reorganization at about 6 Ma ago close to the СЗАп/Gilbert paleomagnetic reversal. The Turolian-Ruscinian boundary should be placed therefore below the Miocene-Pliocene boundary adopted at present. Zone MN14A preceding Zone MN14 is suggested to be the lowermost subdivision of the Ruscinian. The Ruscinian-Villafran- chian boundary is close to the Gilbert-Gauss reversal and to the lower-middle Pliocene boundary. The top of the lower Villafranchian corresponding to the end of the Gauss Chron is slightly older than the middle-upper Pliocene boundary. Range of the lower Villafranchian inferable from fauna of large mammals coincides with Zone MN16 of rodent scale, typical of which is the Uryv assemblage of small mammals in the Russian Plain. Key words: -
The Neogene: Origin, Adoption, Evolution, and Controversy
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 Available online at www.sciencedirect.com Earth-Science Reviews 89 (2008) 42–72 www.elsevier.com/locate/earscirev The Neogene: Origin, adoption, evolution, and controversy Stephen L. Walsh 1 Department of Paleontology, San Diego Natural History Museum, PO Box 121390, San Diego, CA 92112, USA Received 4 October 2007; accepted 3 December 2007 Available online 14 December 2007 Abstract Some stratigraphers have recently insisted that for historical reasons, the Neogene (Miocene+Pliocene) should be extended to the present. However, despite some ambiguity in its application by Moriz Hörnes in the 1850s, the “Neogene” was widely adopted by European geologists to refer to the Miocene and Pliocene of Lyell, but excluding the “Diluvium” (later to become the Pleistocene) and “Alluvium” (later to become the Holocene). During the late 19th and early 20th centuries, the ends of the Neogene, Tertiary and Pliocene evolved in response to the progressive lowering of the beginnings of the Quaternary and Pleistocene. -
Alphabetical List
LIST E - GEOLOGIC AGE (STRATIGRAPHIC) TERMS - ALPHABETICAL LIST Age Unit Broader Term Age Unit Broader Term Aalenian Middle Jurassic Brunhes Chron upper Quaternary Acadian Cambrian Bull Lake Glaciation upper Quaternary Acheulian Paleolithic Bunter Lower Triassic Adelaidean Proterozoic Burdigalian lower Miocene Aeronian Llandovery Calabrian lower Pleistocene Aftonian lower Pleistocene Callovian Middle Jurassic Akchagylian upper Pliocene Calymmian Mesoproterozoic Albian Lower Cretaceous Cambrian Paleozoic Aldanian Lower Cambrian Campanian Upper Cretaceous Alexandrian Lower Silurian Capitanian Guadalupian Algonkian Proterozoic Caradocian Upper Ordovician Allerod upper Weichselian Carboniferous Paleozoic Altonian lower Miocene Carixian Lower Jurassic Ancylus Lake lower Holocene Carnian Upper Triassic Anglian Quaternary Carpentarian Paleoproterozoic Anisian Middle Triassic Castlecliffian Pleistocene Aphebian Paleoproterozoic Cayugan Upper Silurian Aptian Lower Cretaceous Cenomanian Upper Cretaceous Aquitanian lower Miocene *Cenozoic Aragonian Miocene Central Polish Glaciation Pleistocene Archean Precambrian Chadronian upper Eocene Arenigian Lower Ordovician Chalcolithic Cenozoic Argovian Upper Jurassic Champlainian Middle Ordovician Arikareean Tertiary Changhsingian Lopingian Ariyalur Stage Upper Cretaceous Chattian upper Oligocene Artinskian Cisuralian Chazyan Middle Ordovician Asbian Lower Carboniferous Chesterian Upper Mississippian Ashgillian Upper Ordovician Cimmerian Pliocene Asselian Cisuralian Cincinnatian Upper Ordovician Astian upper -
47.5. Timescale and General Synthesis
47.5. TIME SCALE AND GENERAL SYNTHESIS 47.5 TIME SCALE AND GENERAL SYNTHESIS Maria B. Cita, Institute of Paleontology, University of Milan, Milan, Italy and William B. F. Ryan, Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York. BACKGROUND 3.35 my, this time scale is in close agreement with that of Cox (1969), established principally in the dating of lava Deep earth sampling beneath the floor of the flows, with only some minor modifications suggested by Mediterranean has acquired continuous sequences of marine Foster and Opdyke (1970). An age of 5.18 my has been pelagic ooze which were deposited during an interval of adopted for the Gilbert/epoch 5 boundary. time ranging from the end of the Late Miocene "crisis of Age of the Miocene/Pliocene Boundary salinity" to the present. A recognizable evolutionary trend in assemblages of planktonic foraminifera and calcareous The Miocene/Pliocene boundary, as recognized at Site nannofossils has permitted the Leg 13 scientific party to 132 in the Tyrrhenian Basin (see Chapter 13) by a document in this volume a sequence of biostratigraphic sedimentary and paleontological break in Section 2 of Core zones covering this period of time—that is from the earliest 21 lies within the upper part of geomagnetic epoch 5 at an Pliocene onward. extrapolated age of 5.4 my. This age assignment is in good We are indeed fortunate that a majority of the criteria agreement with the various time scales given by Berggren used to establish the boundaries of these zones (see Chapter (1969, 1971, 1972a), particularly the last one, which takes 47.1) can also be identified in deep-sea sediment cores from into consideration the latest deep-sea drilling results in the other parts of the world's ocean. -
A Review of the Villafranchian Fossiliferous Sites of Latium in The
Quaternary Science Reviews 191 (2018) 299e317 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev A review of the Villafranchian fossiliferous sites of Latium in the framework of the geodynamic setting and paleogeographic evolution of the Tyrrhenian Sea margin of central Italy * F. Marra a, , C. Petronio b, L. Salari b, F. Florindo a, c, B. Giaccio c, G. Sottili b a Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 00143 Roma, Italy b Dipartimento di Scienze della Terra, Sapienza, Universita di Roma, P.le Aldo Moro 5, 00185 Roma, Italy c Istituto di Geologia Ambientale e Geoingegneria - CNR, Via Salaria km 29.300, 00015 Montelibretti, Roma, Italy article info abstract Article history: In the present study we provide a paleontological and chronostratigraphic review of the Villafranchian Received 18 August 2017 fossiliferous sites of Latium, revising the biochronologic attribution based on their framing within the Received in revised form geodynamic and paleogeographic evolutionary picture for this region. Aimed at this scope, we recon- 24 April 2018 struct the sedimentary and structural history of the Early Pleistocene marine basins through the review Accepted 10 May 2018 and the regional correlation of published stratigraphic sections and borehole data. Moreover, we combine the chronostratigraphic constraints provided in this study to the near-coast deposits of Gelasian-Santernian age (2.58e1.5 Ma) with the results of a recent geomorphologic study of this area, Keywords: Villafranchian allowing us to reconstruct a suite of terraced paleo-surfaces correlated with marine isotopic stages 21 Central Italy through 5. -
A Classification of the Glirtdae (Rodentia) on the Basis of Dental Morphology
Hystrix, (11s.) 6 (1 -2) (1 994): 3-50 (1995) Proc. I1 Conf. on Dormice A CLASSIFICATION OF THE GLIRTDAE (RODENTIA) ON THE BASIS OF DENTAL MORPHOLOGY REMMERT DAAMS (*) & HANSDE BRUIJN (**) (*) Depto. de Paleontologia, Facultad de Ciencias Geoldgicas, Universidad Complutense, Ciudad Universituria, 28040 Madrid, Spain. (**) Dept. ofStratigraphy/Pulcontolo~,Institute ofEarth Sciences, State University of Utrecht, Budapestlaan 4, 3508 TA Utrecht, The Netherlands. ABSTRACT - The supra-familiar relationships of the Gliridae are discussed. The criterion used for subdividing the Gliridae is the morphology of the cheek teeth because this is the only character known for all taxa. This limitation leads to the undesirable "synonymy" of Glamys and Gliravirs, two genera whose type species have a very different skull morphology, and to the incorporation into the Dryomyinae of Gruphiurzis and Leithiu, despite the fact that Dryonzys has a myomorph, Graphizrrus a hystricomorph and Leithiu a sciurornorph skull. The hundred and seventy-seven species and thirty eight genera of dormice are grouped into five subfamilies. One of these, the Bransatoglirinae, is new. The subfamily Graphiurinae is supressed and Graphiumrs is assigned to the Dryomyinae. The genera of the Gliridae and the species allocated to them are listed in the appendix in alphabetical order. The original diagnoses of the genera are given in English and the type locality, type level and synonymy of each species is given. Key words: Gliridae, Systematics, Taxonomy, Dental morphology, Palaentology. RIASSUNTO - (Jna classijkuzione di Gliridae (Rodentiu) szrllu base della morfologiu dentale - Vengono discusse le relazioni soprafamiliari dei Gliridi. I1 criterio utilizzato per la suddivisione dei Gliridi 6 la morfologia dei denti molari poiche e I'unico carattere noto per tutti i taxa. -
The Newly-Ratified Definition of the Quaternary System/Period and Redefinition of the Pleistocene Series/Epoch, and Comparison O
152 152 Articles by Philip L. Gibbard1 and Martin J. Head2 The newly-ratified definition of the Quaternary System/Period and redefinition of the Pleistocene Series/Epoch, and comparison of proposals advanced prior to formal ratification 1Chair of the ICS Subcommission on Quaternary Stratigraphy; Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, United Kingdom. E-mail: [email protected] 2Department of Earth Sciences, Brock University, 500 Glenridge Avenue, St. Catharines, Ontario L2S 3A1, Canada. E-mail: [email protected] The base of the Quaternary System is defined by the of the Pleistocene Series was simultaneously redefined (lowered) Global Stratotype Section and Point (GSSP) of the so as to be coterminous with that of the Quaternary. The top of the Neogene System is accordingly defined by the base of the Quaternary Gelasian Stage at Monte San Nicola in Sicily, Italy, System, and the top of the Pliocene Series by the base of the currently dated at 2.58 Ma. The base of the Pleistocene Pleistocene (Gibbard and Head, 2009a, b; Gibbard et al., 2010; Finney, Series is redefined by the same GSSP, having previously 2010). The Pleistocene had previously been defined by the GSSP at been defined by the GSSP at Vrica, Calabria, Italy, which Vrica, Calabria, Italy, which is dated at 1.806 Ma (Lourens et al., 2005; Figure 1). The IUGS Executive Committee had already given its is dated at 1.806 Ma. These important changes to the unanimous approval on 28 May 2007 that the Quaternary be geological time scale were formulated through extensive recognized as a formal system/period (Bobrowski, 2007). -
Wessels, W (2009). Miocene Rodent Evolution and Migration. Muroidea
Miocene rodent evolution and migration Muroidea from Pakistan, Turkey and Northern Africa W. Wessels GEOLOGICA ULTRAIECTINA Mededelingen van de Faculteit Geowetenschappen departement Aardwetenschappen Universiteit Utrecht No. 307 ISBN 978-90-5744-170-7 Graphic design and figures: GeoMedia, Faculty of Geosciences, Utrecht University (7497) Miocene rodent evolution and migration Muroidea from Pakistan, Turkey and Northern Africa Evolutie en migratie van Miocene knaagdieren Muroidea afkomstig uit Pakistan, Turkije en Noord Afrika (met een samenvatting in het Nederlands) PROEFSCHRIFT ter verkrijging van de graad van doctor aan de Universiteit Utrecht op gezag van de rector magnificus, prof.dr. J.C. Stoof, ingevolge het besluit van het college voor promoties in het openbaar te verdedigen op maandag 8 juni 2009 des middags te 4.15 uur door Wilma Wessels geboren op 9 december 1955 te Vriezenveen Promotor: Prof.dr. J.W.F. Reumer Contents Part 1 Introduction 1 Introduction 13 2 Correlation of some Miocene faunas from Northern Africa, Turkey and Pakistan 17 by means of Myocricetodontidae Published in Proceedings of the Koninklijke Nederlandse Akademie van Wetenschappen B 90(1): 65-82 (1987), Wessels W., Ünay. E. & Tobien H. 2.1 Abstract 17 2.2 Introduction 17 2.3 The Pakistani Myocricetodontinae 19 2.3.2 Taxonomy 19 2.3.3 Discussion of the Pakistani Myocricetodontinae 24 2.4 The Turkish Myocricetodontinae 24 2.4.2 Taxonomy 25 2.4.3 Discussion of the Turkish Myocricetodontinae 31 2.5 Conclusions 31 2.6 Acknowledgements 31 Part 2 Rodents from Europe, Turkey and Northern Africa 3 Gerbillidae from the Miocene and Pliocene of Europe 35 Published in Mitteilungen der Bayerischen Staatssammlung für Paläontologie und Historische Geologie 38: 187-207 (1998), Wessels W. -
Palaeontologia Electronica Microtoid Cricetids and the Early History Of
Palaeontologia Electronica http://palaeo-electronica.org Microtoid cricetids and the early history of arvicolids (Mammalia, Rodentia) Oldrich Fejfar, Wolf-Dieter Heinrich, Laszlo Kordos, and Lutz Christian Maul ABSTRACT In response to environmental changes in the Northern hemisphere, several lines of brachyodont-bunodont cricetid rodents evolved during the Late Miocene as “micro- toid cricetids.” Major evolutionary trends include increase in the height of cheek tooth crowns and development of prismatic molars. Derived from a possible Megacricetodon or Democricetodon ancestry, highly specialised microtoid cricetids first appeared with Microtocricetus in the Early Vallesian (MN 9) of Eurasia. Because of the morphological diversity and degree of parallelism, phylogenetic relationships are difficult to detect. The Trilophomyinae, a more aberrant cricetid side branch, apparently became extinct without descendants. Two branches of microtoid cricetids can be recognized that evolved into “true” arvicolids: (1) Pannonicola (= Ischymomys) from the Late Vallesian (MN 10) to Middle Turolian (MN 12) of Eurasia most probably gave rise to the ondatrine lineage (Dolomys and Propliomys) and possibly to Dicrostonyx, whereas (2) Microt- odon known from the Late Turolian (MN 13) and Early Ruscinian (MN 14) of Eurasia and possibly parts of North America evolved through Promimomys and Mimomys eventually to Microtus, Arvicola and other genera. The Ruscinian genus Tobienia is presumably the root of Lemmini. Under this hypothesis, in contrast to earlier views, two evolutionary sources of arvicolids would be taken into consideration. The ancestors of Pannonicola and Microtodon remain unknown, but the forerunner of Microtodon must have had a brachyodont-lophodont tooth crown pattern similar to that of Rotundomys bressanus from the Late Vallesian (MN 10) of Western Europe.