Révision De L'espèce Homo Erectus (Dubois, 1893)

Total Page:16

File Type:pdf, Size:1020Kb

Révision De L'espèce Homo Erectus (Dubois, 1893) Bulletins et Mémoires de la Société d’Anthropologie de Paris 2000, nouvelle série , tome 12, 1–2, p. 1–200. VALÉRY ZEITOUN RÉVISION DE L’ESPÈCE HOMO ERECTUS (DUBOIS, 1893) UTILISATION DES DONNÉES MORPHOLOGIQUES ET MÉTRIQUES EN CLADISTIQUE, RECONSIDÉRATION DU CAS HOMO ERECTUS REAPPRAISAL OF THE SPECIES HOMO ERECTUS (DUBOIS, 1893) USE OF MORPHOLOGIC AND METRIC DATA IN CLADISTIC INVESTIGATION OF THE CASE OF HOMO ERECTUS Adresse : Chaire de Paléoanthropologie, Collège de France, 3 Rue d’Ulm, 75 006 Paris. e-mail : [email protected] TABLE DES MATIÈRES INDEX DES FIGURES ET ANNEXES ........................................................................................ 7 AVANT PROPOS......................................................................................................................... 11 RESUMÉ ...................................................................................................................................... 13 SUMMARY .................................................................................................................................. 17 I. — INTRODUCTION ...............................................................................................................21 II. — LES DIFFÉRENTES ACCEPTIONS DE HOMO ERECTUS ........................................... 23 1. — LES HOMO ERECTUS ................................................................................................... 23 2. — LES CARACTÈRES DE HOMO ERECTUS ............................................................................ 24 3. — LA POSITION INCERTAINE DE HOMO ERECTUS DANS LA CLASSIFICATION ET SON STATUT TAXINOMIQUE IMPRÉCIS .................................................................................................. 25 4. — L’ORIGINE DES CONFLITS ............................................................................................. 27 4.1 — MÉTHODES ET APPROCHES .................................................................................. 27 4.2 — ESPÈCES ET TAXONS ........................................................................................... 28 4.3 — LES CARACTÈRES ÉTUDIÉS ................................................................................... 30 III. — MATÉRIEL ET MÉTHODE D’ANALYSE...................................................................... 31 1. — LA CLADISTIQUE ......................................................................................................... 31 1.1 — LE PRINCIPE ....................................................................................................... 32 1.2 — LA MÉTHODE ..................................................................................................... 32 1.3 — LES CRITÈRES .................................................................................................... 32 2. — LE MATÉRIEL ............................................................................................................. 34 3. — LISTE DES SPÉCIMENS FOSSILES .................................................................................... 35 4. — BILAN DES SYNONYMIES ............................................................................................. 46 4 VALÉRY ZEITOUN RÉVISION DE L’ESPÈCE HOMO ERECTUS 5 IV. — L’ANALYSE INFORMATISÉE ........................................................................................ 49 VIII. — DISCUSSION ............................................................................................................... 143 1. — LE LOGICIEL DE PARCIMONIE ........................................................................................ 49 1. — LES CONCEPTS DE L’ESPÈCE ....................................................................................... 143 1.1. — LE CODAGE DES CARACTÈRES ............................................................................. 50 2. — LA SPÉCIATION ......................................................................................................... 144 1.2. — LES OPTIONS DE TRAITEMENT ............................................................................. 50 3. — PROPOSITIONS PHYLOGÉNÉTIQUES ET TAXINOMIQUES .................................................... 146 2. — LES DONNÉES MORPHOLOGIQUES .................................................................................. 52 4. — LES DONNÉES CHRONOLOGIQUES ................................................................................ 149 3. — DESCRIPTION DES CARACTÈRES MORPHOLOGIQUES ......................................................... 52 5. — COMPARAISON DES RÉSULTATS AVEC LES TRAVAUX ANTÉRIEURS ..................................... 154 3.1. — L’OS FRONTAL (CARACTÈRES 1 À 25) .................................................................. 52 3.2. — L’OS PARIÉTAL (CARACTÈRES 26 À 41) ............................................................... 65 IX. — CONCLUSION ............................................................................................................... 155 3.3. — L’OS OCCIPITAL (CARACTÈRES 42 À 61) .............................................................. 71 3.4. — L’OS TEMPORAL (CARACTÈRES 62 À 123) ........................................................... 81 BIBLIOGRAPHIE ..................................................................................................................... 159 4. — LES CARACTÈRES NON TRAITÉS .................................................................................. 105 4.1. — LA CAPACITÉ CRÂNIENNE ................................................................................. 105 ANNEXE 1. — VALEURS DES INDICES DANS LA POPULATION DE RÉFÉRENCE 4.2. — L’ÉPAISSEUR DES OS DE LA VOÛTE CRÂNIENNE ................................................... 106 ....................................................... consulter: http://www.ivry.cnrs.fr/deh/zeitoun/zeitoun.htm 4.3. — SÉPARATION ENTRE L’INION ET L’ENDINION ........................................................ 107 ANNEXE 2. — INTERVALLES DE DÉFINITION DES ÉTATS DES CARACTÈRES V. — LES DONNÉES MÉTRIQUES ........................................................................................ 109 MÉTRIQUES ....................................................... consulter: http://www.ivry.cnrs.fr/deh/zeitoun/zeitoun.htm 1. — LES POINTS DE RÉFÉRENCES ....................................................................................... 110 2. — TRAITEMENT PRÉALABLE DES DONNÉES MÉTRIQUES ......................................................111 ANNEXE 3. — MATRICE COMPLÈTE DES DONNÉES...................................................... 187 3. — LES INDICES MÉTRIQUES ............................................................................................ 112 4. — MODE DE SÉLECTION DES INDICES SERVANT À CONSTITUER LA MATRICE ......................... 113 ANNEXE 4. — LISTE DES CHANGEMENTS D’ÉTATS DE CARACTÈRE AUX DIFFÉ- RENTS NŒUDS : DIAGNOSE DES DIFFÉRENTS TAXONS 5. — LE CODAGE DES INDICES MÉTRIQUES .......................................................................... 115 ....................................................... consulter: http://www.ivry.cnrs.fr/deh/zeitoun/zeitoun.htm 6. — LE TRAITEMENT DE LA VARIABILITÉ ............................................................................ 117 7. — LA MATRICE DES DONNÉES ........................................................................................ 118 ANNEXE 5. — LISTE DES CHANGEMENTS D’ÉTATS DE CARACTÈRE AUX DIFFÉRENTS NŒUDS : DIAGNOSE DES NOUVELLES ESPÈCES DÉCRITES......... 198 VI. — RÉSULTATS DE L’ANALYSE ...................................................................................... 119 1. — CARACTÉRISTIQUES GÉNÉRALES DES DIFFÉRENTES ANALYSES ........................................ 119 2. — RATIONALISATION DES DONNÉES PAR L’ OBSERVATION DE L’ONTOGENÈSE ......................... 120 2.1. — LES CARACTÈRES MÉTRIQUES ET LE PROBLÈME DE LA PONDÉRATION DES TRANSFORMATIONS ................................................................................................ 120 2.2. — ANALYSE DU CLADOGRAMME ........................................................................... 122 2.3. — RAPPEL .......................................................................................................... 123 2.4. — LES « NŒUDS DU PROBLÈME » .......................................................................... 124 VII. — PROPOSITIONS PHYLOGÉNÉTIQUES .................................................................... 137 BILAN ET DIAGNOSE D’HOMO ERECTUS ................................................................................ 140 6 VALÉRY ZEITOUN INDEX DES FIGURES Figure 1. — Régle de Nelson ...................................................................................................... 33 Figure 2. — Expression des états de caractère ............................................................................ 50 Figure 3. — Vue antérieure de l’orbite gauche de Ngandong VI — Caractère 1. Fusion des arcus superciliaris — Caractère 3. — Relief important du bord supérieur des arcus superciliaris .............. 53 Figure 4. — Vue antérieure de l’orbite gauche de Ngandong XII — Caractère 2. – Degré de fermeture du sulcus supraorbitalis ....................................... 55 Figure 5. — Vue supérieure du bord frontal de Ngandong XII — Caractère 5. – Existence d’une dépression postorbitaire latérale ................................ 55 Figure 6. — Dessin du bord frontal de Ngandong VII, de Jebel Irhoud 1 et de KNMER 406 — Caractère 9. – Position de
Recommended publications
  • 5 Years on Ice Age Europe Network Celebrates – Page 5
    network of heritage sites Magazine Issue 2 aPriL 2018 neanderthal rock art Latest research from spanish caves – page 6 Underground theatre British cave balances performances with conservation – page 16 Caves with ice age art get UnesCo Label germany’s swabian Jura awarded world heritage status – page 40 5 Years On ice age europe network celebrates – page 5 tewww.ice-age-europe.euLLING the STORY of iCe AGE PeoPLe in eUROPe anD eXPL ORING PLEISTOCene CULtURAL HERITAGE IntrOductIOn network of heritage sites welcome to the second edition of the ice age europe magazine! Ice Age europe Magazine – issue 2/2018 issn 2568­4353 after the successful launch last year we are happy to present editorial board the new issue, which is again brimming with exciting contri­ katrin hieke, gerd­Christian weniger, nick Powe butions. the magazine showcases the many activities taking Publication editing place in research and conservation, exhibition, education and katrin hieke communication at each of the ice age europe member sites. Layout and design Brightsea Creative, exeter, Uk; in addition, we are pleased to present two special guest Beate tebartz grafik Design, Düsseldorf, germany contributions: the first by Paul Pettitt, University of Durham, cover photo gives a brief overview of a groundbreaking discovery, which fashionable little sapiens © fumane Cave proved in february 2018 that the neanderthals were the first Inside front cover photo cave artists before modern humans. the second by nuria sanz, water bird – hohle fels © urmu, director of UnesCo in Mexico and general coor­­­di nator of the Photo: burkert ideenreich heaDs programme, reports on the new initiative for a serial transnational nomination of neanderthal sites as world heritage, for which this network laid the foundation.
    [Show full text]
  • Cave Radon Exposure, Dose, Dynamics and Mitigation
    Chris L. Waring, Stuart I. Hankin, Stephen B. Solomon, Stephen Long, Andrew Yule, Robert Blackley, Sylvester Werczynski, and Andrew C. Baker. Cave radon exposure, dose, dynamics and mitigation. Journal of Cave and Karst Studies, v. 83, no. 1, p. 1-19. DOI:10.4311/2019ES0124 CAVE RADON EXPOSURE, DOSE, DYNAMICS AND MITIGATION Chris L. Waring1, C, Stuart I. Hankin1, Stephen B. Solomon2, Stephen Long2, Andrew Yule2, Robert Blackley1, Sylvester Werczynski1, and Andrew C. Baker3 Abstract Many caves around the world have very high concentrations of naturally occurring 222Rn that may vary dramatically with seasonal and diurnal patterns. For most caves with a variable seasonal or diurnal pattern, 222Rn concentration is driven by bi-directional convective ventilation, which responds to external temperature contrast with cave temperature. Cavers and cave workers exposed to high 222Rn have an increased risk of contracting lung cancer. The International Commission on Radiological Protection (ICRP) has re-evaluated its estimates of lung cancer risk from inhalation of radon progeny (ICRP 115) and for cave workers the risk may now (ICRP 137) be 4–6 times higher than previously recognized. Cave Guides working underground in caves with annual average 222Rn activity 1,000 Bq m3 and default ICRP assumptions (2,000 workplace hours per year, equilibrium factor F 0.4, dose conversion factor DCF 14 µSv 3 1 1 d13 (kBq h m ) could now receive a dose of 20 mSv y . Using multiple gas tracers ( C CO2, Rn and N2O), linked weather, source gas flux chambers, and convective air flow measurements a previous study unequivocally identified the external soil above Chifley Cave as the source of cave222 Rn.
    [Show full text]
  • CV Karkanas 2018.Pdf
    PANAGIOTIS (TAKIS) KARKANAS CURRICULUM VITAE May 2018 Malcolm H. Wiener Laboratory for Archaeological Science American School of Classical Studies 54 Soudias, 10676 Athens, Greece Tel.: (30) 2130002400x224 Fax: (30) 2107294047 E-mail: [email protected] Personal Web Pages: https://www.researchgate.net/profile/Panagiotis_Karkanas https://ascsa.academia.edu/PanagiotisKarkanas EDUCATIONAL BACKGROUND 1994: Ph.D. in Geology (Specialty: mineralogy, petrology, geochemistry), Department of Geology, University of Athens. 1990: Postgraduate Seminar (300 hours) in Geology of sedimentary basin and energy resources. EU funded Research Seminar for Geologists, Department of Geology, University of Athens. 1986: B.Sc. in Geology, Department of Geology, University of Athens. AREAS OF INTEREST Geoarchaeology: site formation processes (stratigraphy, micromorphology, post-depositional chemical alterations) palaeoenvironmental reconstructions, paleoclimate, methods and techniques (dating, petrography, mineralogy, sedimentary analysis, provenance analysis). PROFESSIONAL APPOINTMENTS 2014-: Director, Malcolm H. Wiener Laboratory of Archaeological Science, American School of Classical Studies at Athens, Greece. 1994-2014: Senior Geologist, Ephoreia of Palaeoanthropology-Speleology (EPS), Ministry of Culture, Greece. 2004-2013: Adjunct Lecturer, Department of Geography, Harokopio University of Athens. OTHER PROFESSIONAL AND LABORATORY EXPERIENCE 1995-2003 (approx. one month per year): Visiting research scientist, Kimmel Center for Archaeological Sciences,
    [Show full text]
  • The Carnivore Remains from the Sima De Los Huesos Middle Pleistocene Site
    N. Garcia & The carnivore remains from the Sima de J. L. Arsuaga los Huesos Middle Pleistocene site Departamento de Paleontologia, (Sierra de Atapuerca, Spain) Facultad de Ciencias Geologicas, U.A. de Paleoantropologia & Instituto de View metadata, citation and similar papersRemain ats ocore.ac.ukf carnivores from the Sima de los Huesos sitebrought representin to you gby a t COREleast Geologia Economica, Universidad 158 adult individuals of a primitive (i.e., not very speleoid) form of Ursus Complutense de Madrid, Ciudad provided by Servicio de Coordinación de Bibliotecas de la... deningeri Von Reichenau 1906, have been recovered through the 1995 field Universitaria, 28040 Madrid, Spain season. These new finds extend our knowledge of this group in the Sierra de Atapuerca Middle Pleistocene. Material previously classified as Cuoninae T. Torres indet. is now assigned to Canis lupus and a third metatarsal assigned in 1987 to Departamento de Ingenieria Geoldgica, Panthera cf. gombaszoegensis, is in our opinion only attributable to Panthera sp. The Escuela Tecnica Superior de Ingenieros family Mustelidae is added to the faunal list and includes Maites sp. and a de Minas, Universidad Politecnica smaller species. The presence of Panthera leo cf. fossilis, Lynxpardina spelaea and de Madrid, Rios Rosas 21, Fells silvestris, is confirmed. The presence of a not very speloid Ursus deningeri, 28003 Madrid, Spain together with the rest of the carnivore assemblage, points to a not very late Middle Pleistocene age, i.e., oxygen isotope stage 7 or older. Relative frequencies of skeletal elements for the bear and fox samples are without major biases. The age structure of the bear sample, based on dental wear stages, does not follow the typical hibernation mortality profile and resembles a cata­ strophic profile.
    [Show full text]
  • Creatividad Y Neurociencia Cognitiva
    Creatividad y neurociencia cognitiva Creativity and cognitive neuroscience Centro UCM-ISCIII de Evolución y Comportamiento Humanos eatividad y neurociencia cognitiva Creativity and cognitive neuroscience cognitiva Creativity eatividad y neurociencia Cr © Fundación Tomás Pascual y Pilar Gómez-Cuétara INSTITUTO TOMÁS PASCUAL SANZ Dirección postal y correspondencia: Paseo de la Castellana, 178, 3.º Derecha. Madrid 28046 Domicilio fiscal: c/ Orense, 70. Madrid 28020 Tel.: 91 703 04 97. Fax: 91 350 92 18 www.institutotomaspascual.es • [email protected] Coordinación editorial: Alberto Alcocer, 13, 1.º D. 28036 Madrid Tel.: 91 353 33 70. Fax: 91 353 33 73 www.imc-sa.es • [email protected] Ni el propietario del copyright, ni los patrocinadores, ni las entidades que avalan esta obra, pueden ser considerados legalmente responsables de la aparición de información inexacta, errónea o difamatoria, siendo los autores los responsables de la misma. Reservados todos los derechos. Ninguna parte de esta publicación puede ser reprodu- cida, transmitida en ninguna forma o medio alguno, electrónico o mecánico, incluyendo las fotocopias, grabaciones o cualquier sistema de recuperación de almacenaje de in- formación, sin permiso escrito del titular del copyright. ISBN: 978-84-7867-078-9 Depósito Legal: M-10789-2012 Creatividad y neurociencia cognitiva Creativity and cognitive neuroscience Coordinadores D. Alfonso Perote Alejandre Director de Proyectos del Instituto Tomás Pascual Sanz. Fundación Tomás Pascual y Pilar Gómez-Cuétara. Dr. Manuel Martín-Loeches Garrido Responsable del Área de Neurociencia Cognitiva del Centro Mixto UCM-ISCIII de Evolución y Comportamiento Humanos. Autores Dra. Anna Abraham Department of Clinical Psychology, Justus Liebig University Giessen, Germany.
    [Show full text]
  • Isotopic Analysis of the Ecology of Herbivores and Carnivores from the Middle Pleistocene Deposits of the Sierra De Atapuerca, Northern Spain N
    Isotopic analysis of the ecology of herbivores and carnivores from the Middle Pleistocene deposits of the Sierra De Atapuerca, northern Spain N. Garcia Gar~ia~,~,",R.S. FeranecC.*, J.L. ~rsua~a~,~,J.M. BermGdez de Castrod, E. Carbonelle 'Deportomento de Poleontologio, Focultod de Ciencior Geoldgicor, Univerridod Complutense de Modrid, Ciudod Univerritorio, 28040 Modrid, Spoin Centlo Mkt0 (UCM-ISUII) de Evolucidn y Comportomiento Humonor, CfSinerio Delgodo 4, Pob. 14, 29029 Modrid, Spoin 'New York Stote Museum. 3140 Culturol Education Center. Albonv. NY 12230. USA *centre Nocionol de Invertigoci6n robre 10 Evoluci6n Humono -?M, Avda de ia Pog 28, 09004 Burger, Spoin eInstitut Cotold de Poleoecologio Humono i Evoluci6 Sociol (IPHES), C/ Erconodor, r/n 43003 Torrogono, Spoin ABSTRACT Carbon and oxygen isotope values reveal resource partitioning among the large mammal fauna from three contemporaneous Middle Pleistocene hominid-bearing localities within the Sierra de Atapuerca (northern Spain). Carbon isotope values sampled from the tooth enamel of fauna present during Ata- ouerca Faunal Unit 6 show that a C?-dominated ecosvstem surrounded the area where fossils were preserved during this time. For the herbivores, Fallow deer isotope values are significantly different from Red deer and horses and show that this species did not forage in open environments at this locality. Red Keywords: deer and horses show similar feedine strateeies with less neeative carbon values imolvine use of more C-l3 Diet Ecology Enamel that this species is herbivorous. Special metabolic mechanisms involved in hibernation in U deningeri Mammal might also have influenced its isotope values. The carbon isotope values of remaining carnivores were 0-18 similar and suggest that each was typically a generalist carnivore, eating a wide variety of prey items.
    [Show full text]
  • Pleistocene Cave Hyenas in the Iberian Peninsula: New Insights from Los Aprendices Cave (Moncayo, Zaragoza)
    Palaeontologia Electronica palaeo-electronica.org Pleistocene cave hyenas in the Iberian Peninsula: New insights from Los Aprendices cave (Moncayo, Zaragoza) Víctor Sauqué, Raquel Rabal-Garcés, Joan Madurell-Malaperia, Mario Gisbert, Samuel Zamora, Trinidad de Torres, José Eugenio Ortiz, and Gloria Cuenca-Bescós ABSTRACT A new Pleistocene paleontological site, Los Aprendices, located in the northwest- ern part of the Iberian Peninsula in the area of the Moncayo (Zaragoza) is presented. The layer with fossil remains has been dated by amino acid racemization to 143.8 ± 38.9 ka (earliest Late Pleistocene or latest Middle Pleistocene). Five mammal species have been identified in the assemblage: Crocuta spelaea (Goldfuss, 1823) Capra pyre- naica (Schinz, 1838), Lagomorpha indet, Arvicolidae indet and Galemys pyrenaicus (Geoffroy, 1811). The remains of C. spelaea represent a mostly complete skeleton in anatomical semi-connection. The hyena specimen represents the most complete skel- eton ever recovered in Iberia and one of the most complete remains in Europe. It has been compared anatomically and biometrically with both European cave hyenas and extant spotted hyenas. In addition, a taphonomic study has been carried out in order to understand the origin and preservation of these exceptional remains. The results sug- gest rapid burial with few scavenging modifications putatively produced by a medium sized carnivore. A review of the Pleistocene Iberian record of Crocuta spp. has been carried out, enabling us to establish one of the earliest records of C. spelaea in the recently discovered Los Aprendices cave, and also showing that the most extensive geographical distribution of this species occurred during the Late Pleistocene (MIS4- 2).
    [Show full text]
  • Proceedings VOLUME 1
    16th INTERNATIONAL CONGRESS OF SPELEOLOGY Proceedings VOLUME 1 Edited by Michal Filippi Pavel Bosák 16th INTERNATIONAL CONGRESS OF SPELEOLOGY Czech Republic, Brno July 21 –28, 2013 Proceedings VOLUME 1 Edited by Michal Filippi Pavel Bosák 2013 16th INTERNATIONAL CONGRESS OF SPELEOLOGY Czech Republic, Brno July 21 –28, 2013 Proceedings VOLUME 1 Produced by the Organizing Committee of the 16th International Congress of Speleology. Published by the Czech Speleological Society and the SPELEO2013 and in the co-operation with the International Union of Speleology. Design by M. Filippi and SAVIO, s.r.o. Layout by SAVIO, s.r.o. Printed in the Czech Republic by H.R.G. spol. s r.o. The contributions were not corrected from language point of view. Contributions express author(s) opinion. Recommended form of citation for this volume: Filippi M., Bosák P. (Eds), 2013. Proceedings of the 16th International Congress of Speleology, July 21–28, Brno. Volume 1, p. 453. Czech Speleological Society. Praha. ISBN 978-80-87857-07-6 KATALOGIZACE V KNIZE - NÁRODNÍ KNIHOVNA ČR © 2013 Czech Speleological Society, Praha, Czech Republic. International Congress of Speleology (16. : Brno, Česko) 16th International Congress of Speleology : Czech Republic, Individual authors retain their copyrights. All rights reserved. Brno July 21–28,2013 : proceedings. Volume 1 / edited by Michal Filippi, Pavel Bosák. -- [Prague] : Czech Speleological Society and No part of this work may be reproduced or transmitted in any the SPELEO2013 and in the co-operation with the International form or by any means, electronic or mechanical, including Union of Speleology, 2013 photocopying, recording, or any data storage or retrieval ISBN 978-80-87857-07-6 (brož.) system without the express written permission of the 551.44 * 551.435.8 * 902.035 * 551.44:592/599 * 502.171:574.4/.5 copyright owner.
    [Show full text]
  • Nivel Cero Maqueta.Qxp
    Nivel Cero 11: 2003-2007 Nivel Cero, 11 Santander, 2003-2007 Pág. 47-62 PROBLEMAS Y LÍMITES ACTUALES EN EL ESTUDIO DEL ARTE PARIETAL PALEOLÍTICO: HACIA UN ENFOQUE PLURAL Diego GÁRATE MAIDAGÁN CREAP Cartailhac, UTAH, UMR 5608 Université de Toulouse-Le Mirail 1. INTRODUCCIÓN prender la variabilidad artística en el espacio y en el tiempo pero, a su vez, cómo investigar La actividad gráfica parietal es una - los contextos en los que la diversa producción más- de las actividades desarrolladas por los gráfica tiene lugar (Conkey, 1985). grupos de cazadores-recolectores del En este sentido, nos limitaremos a Paleolítico Superior. Por lo tanto, su estudio exponer, de manera concisa, el estado actual permite profundizar en el conocimiento de de la investigación en lo que se refiere a dichas sociedades, no solamente en lo que res- dichos aspectos. pecta al papel que en ellas correspondió al propio arte, sino que también en característi- 2. LA IDENTIFICACIÓN DEL ESTILO Y cas como la estructuración social y asunción LA DIVERSIDAD GRÁFICA de códigos simbólicos propios o la implanta- ción espacial y gestión del territorio, entre El desarrollo del concepto de estilo ha otros. No parece justificado disociar el siste- permanecido condicionado, incluso viciado, ma económico de la estructura social o de las por el papel que le ha sido asignado desde el manifestaciones materiales e ideología. inicio de la disciplina hasta la actualidad A pesar de que la necesidad de corre- como elemento de datación, ante la inexisten- lacionar el grafismo parietal con el resto de los cia de sistemas más rigurosos y generalizados.
    [Show full text]
  • L'avifaune Du Pléistocène Moyen Et Supérireur Du Bord De La Méditerranée Européenne: Orgnac 3, Lazaret (France), Caver
    L’avifaune du Pléistocène moyen et supérireur du bord de la Méditerranée européenne : Orgnac 3, Lazaret (France), Caverna delle Fate, Arma delle Manie (Italie), Kalamakia (Grèce), Karain E (Turquie). Paléontologie, Taphonomie et Paléoécologie. T. Roger To cite this version: T. Roger. L’avifaune du Pléistocène moyen et supérireur du bord de la Méditerranée européenne : Orgnac 3, Lazaret (France), Caverna delle Fate, Arma delle Manie (Italie), Kalamakia (Grèce), Karain E (Turquie). Paléontologie, Taphonomie et Paléoécologie.. Géologie appliquée. Museum national d’histoire naturelle - MNHN PARIS, 2004. Français. tel-00486167 HAL Id: tel-00486167 https://tel.archives-ouvertes.fr/tel-00486167 Submitted on 25 May 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. MUSÉUM NATIONAL D’HISTOIRE NATURELLE Département de Préhistoire Année 2004 N° bibliothèque THÈSE Pour obtenir le grade de DOCTEUR DU MUSÉUM NATIONAL D’HISTOIRE NATURELLE Option : Préhistoire Discipline : Paléontologie et archéozoologie Présentée et soutenue publiquement par Thierry ROGER Le 9 Juillet 2004 L’avifaune du Pléistocène moyen et supérieur du bord de la Méditerranée européenne : Orgnac 3, Lazaret (France), Caverna delle Fate, Arma delle Manie (Italie), Kalamakia (Grèce), Karain E (Turquie). Paléontologie, Taphonomie et Paléoécologie.
    [Show full text]
  • A Multi-Method Approach for Speleogenetic Research on Alpine Karst Caves
    GEOMOR-05115; No of Pages 20 Geomorphology xxx (2015) xxx–xxx Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph A multi-method approach for speleogenetic research on alpine karst caves. Torca La Texa shaft, Picos de Europa (Spain) Daniel Ballesteros a,⁎, Montserrat Jiménez-Sánchez a, Santiago Giralt b, Joaquín García-Sansegundo a, Mónica Meléndez-Asensio c a Department of Geology, University of Oviedo, c/Jesús Arias de Velasco s/n, 33005, Spain b Institute of Earth Sciences Jaume Almera (ICTJA, CSIC), c/Lluís Solé i Sabarís s/n, 08028 Barcelona, Spain c Geological Survey of Spain (IGME), c/Matemático Pedrayes 25, 33005 Oviedo, Spain article info abstract Article history: Speleogenetic research on alpine caves has advanced significantly during the last decades. These investigations Received 30 January 2014 require techniques from different geoscience disciplines that must be adapted to the methodological constraints Received in revised form 23 February 2015 of working in deep caves. The Picos de Europa mountains are one of the most important alpine karsts, including Accepted 24 February 2015 14% of the World's Deepest Caves (caves with more than 1 km depth). A speleogenetic research is currently being Available online xxxx developed in selected caves in these mountains; one of them, named Torca La Texa shaft, is the main goal of this article. For this purpose, we have proposed both an optimized multi-method approach for speleogenetic research Keywords: Cave level in alpine caves, and a speleogenetic model of the Torca La Texa shaft. The methodology includes: cave surveying, 234 230 Karst massif dye-tracing, cave geometry analyses, cave geomorphological mapping, Uranium series dating ( U/ Th) and Shaft geomorphological, structural and stratigraphical studies of the cave surroundings.
    [Show full text]
  • Comment on Two Pachycrocuta Brevirostris
    PALEO Revue d'archéologie préhistorique 26 | 2015 Varia Comment on two Pachycrocuta brevirostris (Aymard, 1846) mandibles from the Early Pleistocene in south-eastern France: Grosse Marguerite Cave (Aiguèze) and Trois Pigeons Swallow hole (Nîmes) Note sur deux mandibules de Pachycrocuta brevirostris (Aymard, 1846) du Pléistocène ancien du sud-est de la France : la grotte de la Grosse Marguerite (Aiguèze) et l’aven des Trois Pigeons (Nîmes) Jean-Baptiste Fourvel and Nicolas Lateur Electronic version URL: http://journals.openedition.org/paleo/3031 DOI: 10.4000/paleo.3031 ISSN: 2101-0420 Publisher SAMRA Printed version Date of publication: 1 December 2015 Number of pages: 187-200 ISSN: 1145-3370 Electronic reference Jean-Baptiste Fourvel and Nicolas Lateur, « Comment on two Pachycrocuta brevirostris (Aymard, 1846) mandibles from the Early Pleistocene in south-eastern France: Grosse Marguerite Cave (Aiguèze) and Trois Pigeons Swallow hole (Nîmes) », PALEO [Online], 26 | 2015, Online since 26 April 2016, connection on 07 July 2020. URL : http://journals.openedition.org/paleo/3031 ; DOI : https:// doi.org/10.4000/paleo.3031 This text was automatically generated on 7 July 2020. PALEO est mis à disposition selon les termes de la licence Creative Commons Attribution - Pas d'Utilisation Commerciale - Pas de Modification 4.0 International. Comment on two Pachycrocuta brevirostris (Aymard, 1846) mandibles from the Ea... 1 Comment on two Pachycrocuta brevirostris (Aymard, 1846) mandibles from the Early Pleistocene in south-eastern France: Grosse Marguerite
    [Show full text]