Neandertal Dental Microwear Texture Analysis: a Bioarchaeological Approach Jessica L. Droke
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The Last Maximum Ice Extent and Subsequent Deglaciation of the Pyrenees: an Overview of Recent Research
Cuadernos de Investigación Geográfica 2015 Nº 41 (2) pp. 359-387 ISSN 0211-6820 DOI: 10.18172/cig.2708 © Universidad de La Rioja THE LAST MAXIMUM ICE EXTENT AND SUBSEQUENT DEGLACIATION OF THE PYRENEES: AN OVERVIEW OF RECENT RESEARCH M. DELMAS Université de Perpignan-Via Domitia, UMR 7194 CNRS, Histoire Naturelle de l’Homme Préhistorique, 52 avenue Paul Alduy 66860 Perpignan, France. ABSTRACT. This paper reviews data currently available on the glacial fluctuations that occurred in the Pyrenees between the Würmian Maximum Ice Extent (MIE) and the beginning of the Holocene. It puts the studies published since the end of the 19th century in a historical perspective and focuses on how the methods of investigation used by successive generations of authors led them to paleogeographic and chronologic conclusions that for a time were antagonistic and later became complementary. The inventory and mapping of the ice-marginal deposits has allowed several glacial stades to be identified, and the successive ice boundaries to be outlined. Meanwhile, the weathering grade of moraines and glaciofluvial deposits has allowed Würmian glacial deposits to be distinguished from pre-Würmian ones, and has thus allowed the Würmian Maximum Ice Extent (MIE) –i.e. the starting point of the last deglaciation– to be clearly located. During the 1980s, 14C dating of glaciolacustrine sequences began to indirectly document the timing of the glacial stades responsible for the adjacent frontal or lateral moraines. Over the last decade, in situ-produced cosmogenic nuclides (10Be and 36Cl) have been documenting the deglaciation process more directly because the data are obtained from glacial landforms or deposits such as boulders embedded in frontal or lateral moraines, or ice- polished rock surfaces. -
Endocranial Volume and Brain Growth in Immature Neandertals
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/40853229 Endocranial volume and brain growth in immature Neandertals Article in Periodicum Biologorum · January 2007 Source: OAI CITATIONS READS 23 211 2 authors: Hélène Coqueugniot Jean-Jacques Hublin French National Centre for Scientific Research Max Planck Institute for Evolutionary Anthropology 198 PUBLICATIONS 1,237 CITATIONS 515 PUBLICATIONS 20,418 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Etude anthropologique de La Granède (Millau) View project Micro-CT Analysis of Interglobular Dentine View project All content following this page was uploaded by Hélène Coqueugniot on 04 July 2014. The user has requested enhancement of the downloaded file. PERIODICUM BIOLOGORUM UDC 57:61 VOL. 109, No 4, 379–385, 2007 CODEN PDBIAD ISSN 0031-5362 Original scientific paper Endocranial Volume and Brain Growth in Immature Neandertals Abstract HÉLÈNE COQUEUGNIOT1,2 JEAN-JACQUES HUBLIN1 Microstructural studies have suggested that an extended period of growth 1 was absent in representatives of Homo erectus, and that Neandertals Department of Human Evolution reached adulthood significantly more rapidly than modern humans. In Max Planck Institute for Evolutionary Anthropology addition to general rate of growth, a prolonged postnatal period of brain Deutscher Platz 6 development allows humans to develop complex cognitive and social skills. 04103 Leipzig, Germany Conditions in brain growth similar to those observed in extant humans were E-mail: [email protected] not established in the first representatives of Homo erectus. To assess the 2UMR 5199 – PACEA, Laboratoire degree of secondary altriciality reached by Neandertals, we examined the d’Anthropologie most complete skulls available for immature Neandertal specimens. -
Nasal Floor Variation Among Eastern Eurasian Pleistocene Homo Xiu-Jie WU1, Scott D
ANTHROPOLOGICAL SCIENCE Vol. 120(3), 217–226, 2012 Nasal floor variation among eastern Eurasian Pleistocene Homo Xiu-Jie WU1, Scott D. MADDUX2, Lei PAN1,3, Erik TRINKAUS4* 1Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, People’s Republic of China 2Department of Pathology and Anatomical Sciences, University of Missouri, Columbia, MO 65212, USA 3Graduate University of the Chinese Academy of Sciences, Beijing 100049, People’s Republic of China 4Department of Anthropology, Washington University, St Louis, MO 63130, USA Received 28 March 2012; accepted 9 July 2012 Abstract A bi-level nasal floor, although present in most Pleistocene and recent human samples, reaches its highest frequency among the western Eurasian Neandertals and has been considered a fea- ture distinctive of them. Early modern humans, in contrast, tend to feature a level (or sloping) nasal floor. Sufficiently intact maxillae are rare among eastern Eurasian Pleistocene humans, but several fos- sils provide nasal floor configurations. The available eastern Eurasian Late Pleistocene early modern humans have predominantly level nasal floors, similar to western early modern humans. Of the four observable eastern Eurasian archaic Homo maxillae (Sangiran 4, Chaoxian 1, Xujiayao 1, and Chang- yang 1), three have the bi-level pattern and the fourth is scored as bi-level/sloping. It therefore appears that bi-level nasal floors were common among Pleistocene archaic humans, and a high frequency of them is not distinctive of the Neandertals. Key words: noses, maxilla, Asia, palate, Neandertal Introduction dominate with the bi-level configuration being present in ≤10% in all but a sub-Saharan African “Bantu” sample In his descriptions of the Shanidar Neandertal crania, (Table 1). -
Growth, Learning, Play and Attachment in Neanderthal Children
This is a repository copy of The Cradle of Thought : Growth, Learning, Play and Attachment in Neanderthal children. White Rose Research Online URL for this paper: https://eprints.whiterose.ac.uk/83027/ Version: Submitted Version Article: Spikins, Penny orcid.org/0000-0002-9174-5168, Hitchens, Gail, Rutherford, Holly et al. (1 more author) (2014) The Cradle of Thought : Growth, Learning, Play and Attachment in Neanderthal children. Oxford Journal of Archaeology. pp. 111-134. ISSN 0262-5253 https://doi.org/10.1111/ojoa.12030 Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ THE CRADLE OF THOUGHT: GROWTH, LEARNING, PLAY AND ATTACHMENT IN NEANDERTHAL CHILDREN Penny Spikins, Gail Hitchens, Andy Needham and Holly Rutherford Department of Archaeology University of York King’s Manor York YO1 7EP SUMMARY Childhood is a core stage in development, essential in the acquisition of social, practical and cultural skills. However, this area receives limited attention in archaeological debate, especially in early prehistory. -
Internationale Bibliographie Für Speläologie Jahr 1953 1-80 Wissenschaftliche Beihefte Zur Zeitschrift „Die Höhle44 Nr
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Die Höhle - Wissenschaftliche Beihefte zur Zeitschrift Jahr/Year: 1958 Band/Volume: 5_1958 Autor(en)/Author(s): Trimmel Hubert Artikel/Article: Internationale Bibliographie für Speläologie Jahr 1953 1-80 Wissenschaftliche Beihefte zur Zeitschrift „Die Höhle44 Nr. 5 INTERNATIONALE BIBLIOGRAPHIE FÜR SPELÄOLOGIE (KARST- U.' HÖHLENKUNDE) JAHR 1953 VQN HUBERT TRIMMEL Unter teilweiser Mitarbeit zahlreicher Fachleute Wien 1958 Herausgegeben vom Landesverein für Höhlenkunde in Wien und Niederösterreich ■ ■ . ' 1 . Wissenschaftliche Beihefte zur Zeitschrift „Die Höhle44 Nr. 5 INTERNATIONALE BIBLIOGRAPHIE FÜR SPELÄOLOGIE (KARST- U. HÖHLENKUNDE) JAHR 1953 VON HUBERT TRIMMEL Unter teilweiser Mitarbeit zahlreicher Fachleute Wien 1958 Herausgegeben vom Landesverein für Höhlenkunde in Wien und Niederösterreich Gedruckt mit Unterstützung des Notringes der wissenschaftlichen Ve rbände Öste rrei chs Eigentümer, Herausgeber und Verleger: Landesverein für Höhlen kunde in Wien und Niederösterreich, Wien II., Obere Donaustr. 99 Vari-typer-Satz: Notring der wissenschaftlichen Verbände Österreichs Wien I., Judenplatz 11 Photomech.Repr.u.Druck: Bundesamt für Eich- und Vermessungswesen (Landesaufnahme) in Wien - 3 - VORWORT Das Amt für Kultur und Volksbildung der Stadt Wien und der Notring der wissenschaftlichen Verbände haben durch ihre wertvolle Unterstützung auch das Erscheinen dieses vierten Heftes mit bibliographischen -
Bibliography
Bibliography Many books were read and researched in the compilation of Binford, L. R, 1983, Working at Archaeology. Academic Press, The Encyclopedic Dictionary of Archaeology: New York. Binford, L. R, and Binford, S. R (eds.), 1968, New Perspectives in American Museum of Natural History, 1993, The First Humans. Archaeology. Aldine, Chicago. HarperSanFrancisco, San Francisco. Braidwood, R 1.,1960, Archaeologists and What They Do. Franklin American Museum of Natural History, 1993, People of the Stone Watts, New York. Age. HarperSanFrancisco, San Francisco. Branigan, Keith (ed.), 1982, The Atlas ofArchaeology. St. Martin's, American Museum of Natural History, 1994, New World and Pacific New York. Civilizations. HarperSanFrancisco, San Francisco. Bray, w., and Tump, D., 1972, Penguin Dictionary ofArchaeology. American Museum of Natural History, 1994, Old World Civiliza Penguin, New York. tions. HarperSanFrancisco, San Francisco. Brennan, L., 1973, Beginner's Guide to Archaeology. Stackpole Ashmore, w., and Sharer, R. J., 1988, Discovering Our Past: A Brief Books, Harrisburg, PA. Introduction to Archaeology. Mayfield, Mountain View, CA. Broderick, M., and Morton, A. A., 1924, A Concise Dictionary of Atkinson, R J. C., 1985, Field Archaeology, 2d ed. Hyperion, New Egyptian Archaeology. Ares Publishers, Chicago. York. Brothwell, D., 1963, Digging Up Bones: The Excavation, Treatment Bacon, E. (ed.), 1976, The Great Archaeologists. Bobbs-Merrill, and Study ofHuman Skeletal Remains. British Museum, London. New York. Brothwell, D., and Higgs, E. (eds.), 1969, Science in Archaeology, Bahn, P., 1993, Collins Dictionary of Archaeology. ABC-CLIO, 2d ed. Thames and Hudson, London. Santa Barbara, CA. Budge, E. A. Wallis, 1929, The Rosetta Stone. Dover, New York. Bahn, P. -
Science Journals
RESEARCH ◥ that paper, and the average of the listed cranial TECHNICAL COMMENT capacities should have been 1468.7 cc, not 1494 cc. Additionally, using values from Holloway et al.(7) for those Neandertals would result in an average PALEOANTHROPOLOGY cranial capacity of 1438.3 cc. A third value of 1498 cc, based on Holloway et al., is used to generate the consensus average (1). In Holloway et al., an aver- Comment on “The growth pattern age for Homo sapiens neanderthalensis is reported as 1487.5 ml in appendix I and 1427.2 ml in appendix II. The 1427.2-ml value is almost identical of Neandertals, reconstructed (1428 ml) to the average of reported adult values in the text of Holloway et al. However, Holloway et al. from a juvenile skeleton from also attribute fossils typically assigned to Homo sapiens [Jebel Ihroud (n =2)andSkhul(n =4)]to El Sidrón (Spain)” Neandertals. When these are removed, the average Neandertal adult cranial capacity in Holloway et al. Jeremy M. DeSilva is 1414.8 ml. Given these problems with the values used to generate the consensus average of cranial Rosas et al. (Reports, 22 September 2017, p. 1282) calculate El Sidrón J1 to have capacity in adult Neandertals, it is necessary to reached only 87.5% of its adult brain size. This finding is based on an overestimation recalculate the likely percentage of adult brain size achieved by the El Sidrón juvenile. of Neandertal brain size. Pairwise comparisons with a larger sample of Neandertal Downloaded from fossils reveal that it is unlikely that the brain of El Sidrón would have grown When all adult crania assigned to Neandertals n appreciably larger. -
Universidad Complutense De Madrid
UNIVERSIDAD COMPLUTENSE DE MADRID FACULTAD DE CIENCIAS BIOLÓGICAS Departamento de Zoología y Antropología Física TESIS DOCTORAL Las poblaciones del Holoceno inicial en la región cantábrica: cambios ambientales y microevolución humana MEMORIA PARA OPTAR AL GRADO DE DOCTOR PRESENTADA POR Labib Drak Hernández Directora María Dolores Garralda Benajes Madrid, 2016 © Labib Drak Hernández, 2016 UNIVERSIDAD COMPLUTENSE DE MADRID FACULTAD DE CIENCIAS BIOLÓGICAS DEPARTAMENTO DE ZOOLOGÍA Y ANTROPOLOGÍA FÍSICA TESIS DOCTORAL LAS POBLACIONES DEL HOLOCENO INICIAL EN LA REGIÓN CANTÁBRICA: CAMBIOS AMBIENTALES Y MICROEVOLUCIÓN HUMANA MEMORIA PARA OPTAR AL GRADO DE DOCTOR PRESENTADA POR LABIB DRAK HERNÁNDEZ BAJO LA DIRECCIÓN DE LA DOCTORA: MARÍA DOLORES GARRALDA BENAJES MADRID, 2015 UNIVERSIDAD COMPLUTENSE DE MADRID FACULTAD DE CIENCIAS BIOLÓGICAS DEPARTAMENTO DE ZOOLOGÍA Y ANTROPOLOGÍA FÍSICA TESIS DOCTORAL LAS POBLACIONES DEL HOLOCENO INICIAL EN LA REGIÓN CANTÁBRICA: CAMBIOS AMBIENTALES Y MICROEVOLUCIÓN HUMANA MEMORIA PARA OPTAR AL GRADO DE DOCTOR PRESENTADA POR LABIB DRAK HERNÁNDEZ BAJO LA DIRECCIÓN DE LA DOCTORA: MARÍA DOLORES GARRALDA BENAJES MADRID, 2015 MARÍA DOLORES GARRALDA BENAJES, PROFESORA TITULAR DEL DEPARTAMENTO DE ZOOLOGÍA Y ANTROPOLOGÍA FÍSICA DE LA FACULTAD DE CIENCIAS BIOLÓGICAS DE LA UNIVERSIDAD COMPLUTENSE DE MADRID, CERTIFICA: Que la presente memoria titulada “Las poblaciones del Holoceno inicial en la región cantábrica: cambios ambientales y microevolución humana” presentada por D. Labib Drak Hernández para optar al Título de Doctor en Biología, ha sido realizada en el Departamento de Zoología y Antropología Física de la Facultad de CC. Biológicas de la Universidad Complutense de Madrid bajo mi dirección. Y considerando que representa trabajo de Tesis, autorizo su presentación a la Junta de Facultad. -
The First Neanderthal Remains from an Open-Air Middle Palaeolithic Site In
www.nature.com/scientificreports OPEN The first Neanderthal remains from an open-air Middle Palaeolithic site in the Levant Received: 30 January 2017 Ella Been1,2, Erella Hovers3,4, Ravid Ekshtain3, Ariel Malinski-Buller5, Nuha Agha6, Alon Accepted: 8 May 2017 Barash7, Daniella E. Bar-Yosef Mayer8,9, Stefano Benazzi10,11, Jean-Jacques Hublin11, Lihi Published: xx xx xxxx Levin2, Noam Greenbaum12, Netta Mitki3, Gregorio Oxilia13,10, Naomi Porat 14, Joel Roskin15,16, Michalle Soudack17,18, Reuven Yeshurun19, Ruth Shahack-Gross15, Nadav Nir3, Mareike C. Stahlschmidt20, Yoel Rak2 & Omry Barzilai6 The late Middle Palaeolithic (MP) settlement patterns in the Levant included the repeated use of caves and open landscape sites. The fossil record shows that two types of hominins occupied the region during this period—Neandertals and Homo sapiens. Until recently, diagnostic fossil remains were found only at cave sites. Because the two populations in this region left similar material cultural remains, it was impossible to attribute any open-air site to either species. In this study, we present newly discovered fossil remains from intact archaeological layers of the open-air site ‘Ein Qashish, in northern Israel. The hominin remains represent three individuals: EQH1, a nondiagnostic skull fragment; EQH2, an upper right third molar (RM3); and EQH3, lower limb bones of a young Neandertal male. EQH2 and EQH3 constitute the first diagnostic anatomical remains of Neandertals at an open-air site in the Levant. The optically stimulated luminescence ages suggest that Neandertals repeatedly visited ‘Ein Qashish between 70 and 60 ka. The discovery of Neandertals at open-air sites during the late MP reinforces the view that Neandertals were a resilient population in the Levant shortly before Upper Palaeolithic Homo sapiens populated the region. -
Lukenya Hill, Kenya)
Late Pleistocene age and archaeological context for the hominin calvaria from GvJm-22 (Lukenya Hill, Kenya) Christian A. Tryona,1, Isabelle Crevecoeurb, J. Tyler Faithc, Ravid Ekshtaina, Joelle Nivensd, David Pattersone, Emma N. Mbuaf, and Fred Spoorg,h aDepartment of Anthropology, Harvard University, Cambridge, MA 02138; bUnité Mixte de Recherche 5199, de la Préhistoire à l’Actuel: Culture, Environnement, et Anthropologie, Centre National de la Recherche Scientifique, Université de Bordeaux, 33615 Talence, France; cArchaeology Program, School of Social Science, University of Queensland, Brisbane, QLD 4072, Australia; dDepartment of Anthropology, New York University, New York, NY 10003; eCenter for the Advanced Study of Hominid Paleobiology, Department of Anthropology, The George Washington University, Washington, DC 20052; fNational Museums of Kenya, Nairobi, Kenya 00100; gDepartment of Human Evolution, Max Planck Institute for Evolutionary Anthropology, D-04103, Leipzig, Germany; and hDepartment of Cell and Developmental Biology, University College London, WC1E 6BT London, United Kingdom Edited by Erik Trinkaus, Washington University, St. Louis, MO, and approved January 16, 2015 (received for review September 19, 2014) Kenya National Museums Lukenya Hill Hominid 1 (KNM-LH 1) is Hominid 1 (KNM-LH 1) partial calvaria from site GvJm-22 at a Homo sapiens partial calvaria from site GvJm-22 at Lukenya Hill, Lukenya Hill, Kenya, the only eastern African fossil hominin Kenya, associated with Later Stone Age (LSA) archaeological de- from a Last Glacial Maximum [LGM; 19–26.4 kya (19)] LSA posits. KNM-LH 1 is securely dated to the Late Pleistocene, and archaeological context. We construct a revised accelerator mass samples a time and region important for understanding the origins spectrometry (AMS) radiocarbon chronology built on 26 new of modern human diversity. -
The Neandertal Lower Right Deciduous Second Molar from Trou De L•Abime
Journal of Human Evolution 58 (2010) 56–67 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol The Neandertal lower right deciduous second molar from Trou de l’Abıˆme at Couvin, Belgium Michel Toussaint a,*, Anthony J. Olejniczak b, Sireen El Zaatari b, Pierre Cattelain c, Damien Flas d, Claire Letourneux b,Ste´phane Pirson e a Direction de l’Arche´ologie, Service Public de Wallonie, 1 rue des Brigades d’Irlande, B-5100 Namur, Belgium b Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, D-04103 Leipzig, Germany c Muse´e du Malgre´-Tout and CEDARC, rue de la Gare, 28, B-5670 Treignes, Belgium d Muse´es royaux d’Art et d’Histoire, parc du Cinquantenaire, B-1000 Brussels, Belgium e Direction de l’Arche´ologie, Service Public de Wallonie, 1 rue des Brigades d’Irlande, B-5100 Namur and Royal Belgian Institute of Natural Sciences, 29 rue Vautier, B-1000 Brussels, Belgium article info abstract Article history: A human lower right deciduous second molar was discovered in 1984 at the entrance of Trou de Received 13 June 2008 l’Abıˆme at Couvin (Belgium). In subsequent years the interpretation of this fossil remained difficult for Accepted 11 August 2009 various reasons: (1) the lack of taxonomically diagnostic elements which would support its attribution to either Homo (sapiens) neanderthalensis or H. s. sapiens; (2) the absence of any reliable chronostratigraphic Keywords: interpretation of the sedimentary sequence of the site; (3) the contradiction between archaeological Middle Palaeolithic interpretations, which attributed the lithic industry to a transitional facies between the Middle and Early Enamel thickness Upper Palaeolithic, and the radiocarbon date of 46,820 Æ 3,290 BP obtained from animal bone remains Neandertals Couvin associated with the tooth and the flint tools. -
Unit 7 Cenozoic Era with Special Reference to Quaternary Period
UNIT 7 CENOZOIC ERA WITH SPECIAL REFERENCE TO QUATERNARY PERIOD Contents 7.0 Introduction 7.1 Position of Cenozoic in the Geologic Time Scale 7.2 Chronology of Cenozoic Era 7.3 Quaternary Period and Pleistocene Glaciations 7.4 Evidences of Pleistocene Glaciations 7.5 Pluvials and Inter-pluvials 7.6 Causes of Pleistocene Glaciations 7.7 Summary 7.8 References 7.9 Answers to Check your Progress Learning Objectives Once you have studied this unit, you should be able to: Know the chronology and position of Cenozoic Era in Geological Time Scale; Understand different periods of Cenozoic Era; Study various glaciation and inter glaciation phases; and Discuss the causes of Pleistocene climatic change 7.0 INTRODUCTION The Cenozoic Era is also known as Caenozoic or Cainozoic. Cenozoic literally means ‘new life’ after the Greek roots ‘kainos’ meaning ‘new’ and ‘zoico’ meaning ‘animal life’. The Cenozoic Era is of substantial interest for anthropologists since the evolution and diversification of fossil primates, including humans, took place during this era. Besides primates, a significant portion of the evolution and radiation of various groups of mammals also happened during the Cenozoic. It is for this reason that sometimes the Cenozoic is also termed as the ‘Age of Mammals’ who were the dominant animal life of earth during the Cenozoic Era. The era began about 65 million years ago and continues into the present. The existing locations of the continents and the distribution of current flora and fauna acquired its present-day configuration during this time period. The era began at the end of Cretaceous, the last phase of the Mesozoic.