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The Middle Stone Age of East Africa and the Beginnings of Regional Identity
Journal of Worm Prehistory, Vol. 2, No. 3. 1988 The Middle Stone Age of East Africa and the Beginnings of Regional Identity J. Desmond Clark ~ The history of research into the Middle Stone Age of East Africa and the present state of knowledge of this time period is examined for the region as a whole, with special reference to paleoenvironments. The known MSA sites and occurrences are discussed region by region and attempts are made to fit them into a more precise chronological framework and to assess their cultural affinities. The conclusion is reached that the Middle Stone Age lasted for some 150,000 years but considerably more systematic and in-depth research is needed into this time period, which is now perceived as of great significance since it appears to span the time of the evolution of anatomically Modern humans in the continent, perhaps in Last Africa. KEY WORDS: Middle Stone Age; Sangoan/Lupemban; long chronology; Archaic Homo sapiens; Modern H. sapiens. • . when we eventually find the skulls of the makers of the African Mousterian they will prove to be of non-Homo sapiens type, although probably not of Neanderthal type, but merely an allied race of Homo rhodesiensis. The partial exception.., of the Stillbay culture group is therefore explicable on the grounds that Homo sapiens influence was already at work. (Leakey, 1931, p. 326) The other view is that the cradle of the Aurignacian races lies hidden somewhere in the Sahara area, probably in the south-east, and that an early wave of movement carried one branch of the stock via Somaliland and the Straits of Bab el-Mandeb into Arabia, and thence to some unknown secondary centre of distribution in Asia. -
Papers in Honor of Glynn Isaac and His
This article was downloaded by: [Michigan State University] On: 06 February 2015, At: 13:37 Publisher: Routledge Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Azania: Archaeological Research in Africa Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/raza20 Casting the net wide: Papers in honor of Glynn Isaac and his approach to human origins research Thomas Wynn a a University of Colorado , Colorado Springs , United States of America Published online: 03 May 2013. To cite this article: Thomas Wynn (2013) Casting the net wide: Papers in honor of Glynn Isaac and his approach to human origins research, Azania: Archaeological Research in Africa, 48:2, 326-328, DOI: 10.1080/0067270X.2013.788868 To link to this article: http://dx.doi.org/10.1080/0067270X.2013.788868 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sources of information. Taylor and Francis shall not be liable for any losses, actions, claims, proceedings, demands, costs, expenses, damages, and other liabilities whatsoever or howsoever caused arising directly or indirectly in connection with, in relation to or arising out of the use of the Content. -
A Later Stone Age Assemblage from Canteen Kopje, Northern Cape
204 South African Archaeological Bulletin 65 (192): 204–214, 2010 Field and Technical Report A LATER STONE AGE ASSEMBLAGE FROM CANTEEN KOPJE, NORTHERN CAPE TIM R. FORSSMAN1, KATHLEEN KUMAN1,2, GEORGE M. LEADER1,3 & RYAN J. GIBBON1,4 1School of Geography, Archaeology and Environmental Studies, University of the Witwatersrand, Johannesburg, South Africa E-mail: [email protected] / [email protected] [email protected] / [email protected] 2Institute for Human Evolution 3Department of Archaeology, University of Southampton, Southampton, United Kingdom 4Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana, USA (Received June 2010. Revised November 2010) INTRODUCTION formation in the foraging economy. While such changes Canteen Kopje has been mentioned in archaeological occurred throughout southern Africa (e.g. Dowson 1998; Hall literature for almost a century because of artefacts which & Smith 2000; Sadr 2002), the outcome, according to Kent had come to light during exploitation of the Vaal River gravels (2002), was constrained by site and situational context. Yet, by diamond miners. It was first registered as a diamond mining some general trends are noticed. Most prominently, lithic site in the 1870s under the name Klip Drift (De Wit 2008). In frequencies changed. A general increase in scrapers and corre- 1948, the site was declared a national monument due to the sponding decrease in backed tools occurred across southern richness of its Earlier Stone Age collections (J. Deacon 1993), yet Africa. At the same time, trade items in the form of ceramics, only recently have systematic archaeological excavations been glass beads and iron implements began appearing in the LSA conducted. -
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. -
Phytolith Analysed to Compare Changes in Vegetation Structure of Koobi Fora and Olorgesailie Basins Through the Mid- Pleistocene-Holocene Periods
Phytolith analysed to Compare Changes in Vegetation Structure of Koobi Fora and Olorgesailie Basins through the Mid- Pleistocene-Holocene Periods. By KINYANJUI, Rahab N. Student number: 712138 Submitted on 28th February, 2017 Submitted the revised version on 22nd February, 2018 Declaration A thesis submitted to the Faculty of Science in fulfilment of the requirements for PhD degree. At School of Geosciences, Evolutionary Studies Institute (ESI) University of Witwatersrand, Johannesburg South Africa. I declare that this is my own unaided work and has not been submitted elsewhere for degree purposes KINYANJUI, Rahab N. Student No. 712138 ii Abstract Phytolith analyses to compare changes in vegetation structure of Koobi Fora and Olorgesailie Basins through Mid-Pleistocene-Holocene Periods. By Rahab N Kinyanjui (Student No: 712138) Doctor of Philosophy in Palaeontology University of Witwatersrand, South Africa School of Geological Sciences, Evolutionary Science Institute (GEOS/ESI) Supervisor: Prof Marion Bamford. The Koobi Fora and Olorgesailie Basins are renowned Hominin sites in the Rift Valley of northern and central Kenya, respectively with fluvial, lacustrine and tuffaceous sediments spanning the Pleistocene and Holocene. Much research has been done on the fossil fauna, hominins and flora with the aim of trying to understand when and how the hominins evolved, and how the environment impacted on their behaviour, land-use and distribution over time. One of the most important factors in trying to understand the hominin-environment relationship is firstly to reconstruct the environment. Important environmental factors are the climate, rate or degree of climate change, vegetation structure and resources, floral and faunal resources. Vegetation structure/composition is a key component of the environments and, it has been hypothesized the openness and/or closeness of vegetation structure played a key role in shaping the evolutionary history not only of man but also other mammals. -
'Favoured Places' and What Do They Tell Us About Hominin Behaviour..?
What are Oldowan 'favoured places' and what do they tell us about hominin behaviour..? Table of Contents 1. Introduction ............................................................................................................................ 2 2. The Oldowan........................................................................................................................... 2 Africa, the cradle of mankind ................................................................................................... 2 What is 'Oldowan' ................................................................................................................... 2 Olduvai Gorge.......................................................................................................................... 3 Taxa ........................................................................................................................................ 3 Climate and Environment......................................................................................................... 3 3. Favoured-Place ....................................................................................................................... 4 4. Hominin Behaviours................................................................................................................ 5 Oldowan Culture ...................................................................................................................... 5 Bipedalism .................................................................................................................... -
Later Stone Age Toolstone Acquisition in the Central Rift Valley of Kenya
Journal of Archaeological Science: Reports 18 (2018) 475–486 Contents lists available at ScienceDirect Journal of Archaeological Science: Reports journal homepage: www.elsevier.com/locate/jasrep Later Stone Age toolstone acquisition in the Central Rift Valley of Kenya: T Portable XRF of Eburran obsidian artifacts from Leakey's excavations at Gamble's Cave II ⁎ ⁎⁎ Ellery Frahma,b, , Christian A. Tryonb, a Yale Initiative for the Study of Ancient Pyrotechnology, Council on Archaeological Studies, Department of Anthropology, Yale University, New Haven, CT, United States b Department of Anthropology, Harvard University, Peabody Museum of Archaeology and Ethnology, Cambridge, MA, United States ARTICLE INFO ABSTRACT Keywords: The complexities of Later Stone Age environmental and behavioral variability in East Africa remain poorly Obsidian sourcing defined, and toolstone sourcing is essential to understand the scale of the social and natural landscapes en- Raw material transfer countered by earlier human populations. The Naivasha-Nakuru Basin in Kenya's Rift Valley is a region that is not Naivasha-Nakuru Basin only highly sensitive to climatic changes but also one of the world's most obsidian-rich landscapes. We used African Humid Period portable X-ray fluorescence (pXRF) analyses of obsidian artifacts and geological specimens to understand pat- Hunter-gatherer mobility terns of toolstone acquisition and consumption reflected in the early/middle Holocene strata (Phases 3–4 of the Human-environment interactions Eburran industry) at Gamble's Cave II. Our analyses represent the first geochemical source identifications of obsidian artifacts from the Eburran industry and indicate the persistent selection over time for high-quality obsidian from Mt. Eburru, ~20 km distant, despite changes in site occupation intensity that apparently correlate with changes in the local environment. -
Paleoanthropology Society Meeting Abstracts, St. Louis, Mo, 13-14 April 2010
PALEOANTHROPOLOGY SOCIETY MEETING ABSTRACTS, ST. LOUIS, MO, 13-14 APRIL 2010 New Data on the Transition from the Gravettian to the Solutrean in Portuguese Estremadura Francisco Almeida , DIED DEPA, Igespar, IP, PORTUGAL Henrique Matias, Department of Geology, Faculdade de Ciências da Universidade de Lisboa, PORTUGAL Rui Carvalho, Department of Geology, Faculdade de Ciências da Universidade de Lisboa, PORTUGAL Telmo Pereira, FCHS - Departamento de História, Arqueologia e Património, Universidade do Algarve, PORTUGAL Adelaide Pinto, Crivarque. Lda., PORTUGAL From an anthropological perspective, the passage from the Gravettian to the Solutrean is one of the most interesting transition peri- ods in Old World Prehistory. Between 22 kyr BP and 21 kyr BP, during the beginning stages of the Last Glacial Maximum, Iberia and Southwest France witness a process of substitution of a Pan-European Technocomplex—the Gravettian—to one of the first examples of regionalism by Anatomically Modern Humans in the European continent—the Solutrean. While the question of the origins of the Solutrean is almost as old as its first definition, the process under which it substituted the Gravettian started to be readdressed, both in Portugal and in France, after the mid 1990’s. Two chronological models for the transition have been advanced, but until very recently the lack of new archaeological contexts of the period, and the fact that the many of the sequences have been drastically affected by post depositional disturbances during the Lascaux event, prevented their systematic evaluation. Between 2007 and 2009, and in the scope of mitigation projects, archaeological fieldwork has been carried in three open air sites—Terra do Manuel (Rio Maior), Portela 2 (Leiria), and Calvaria 2 (Porto de Mós) whose stratigraphic sequences date precisely to the beginning stages of the LGM. -
Bipedal Hominins
INTRODUCTION Although captive chimpanzees, bonobos and other great apes have acquired some of the features of There is fairly general agreement that language is a language, including the use of symbols to denote uniquely human accomplishment. Although other objects or actions, they have not displayed species communicate in diverse ways, human anything like recursive syntax, or indeed any language has properties that stand out as special. degree of generativity beyond the occasional 4 The most obvious of these is generativity -the ability combining of symbols in pairs. To quote Pinker, to construct a potentially infinite variety of they simply don’t “get it.” This suggests that the sentences, conveying an infinite variety of common ancestor of humans and chimpanzee was meanings. Animal communication is by contrast almost certainly bereft of anything we might stereotyped and restricted to particular situations, consider to be true language. Human language and typically conveys emotional rather than must therefore have evolved its distinctive propositional information. The generativity of characteristics over the past 6 million years. Some language was noted by Descartes as one of the have claimed that this occurred in a single step, characteristics separating humans from other and recently -perhaps as recently as 170,000 years species, and has also been emphasized more ago, coincident with the emergence of our own recently by Chomsky, as in the following often- species. This is sometimes referred to as the “big quoted passage: bang” theory of language evolution. For example, Bickerton5 asserted that “… true language, via the “The unboundedness of human speech, as an emergence of syntax, was a catastrophic event, expression of limitless thought, is an entirely occurring within the first few generations of Homo different matter (from animal communication), sapiens sapiens (p. -
KATHY DIANE SCHICK Contact Information
CURRICULUM VITAE Name: KATHY DIANE SCHICK Contact Information: Telephone: (812) 876-0080, ext. 202 (office) (812) 855-0086 (FAX) Email : [email protected] Address : Stone Age Institute 1392 W. Dittemore Road Gosport, IN 47433 Website : www.stoneageinstitute.org Present Positions: Professor, Department of Anthropology and Cognitive Science Program, Indiana University Co-Director, Stone Age Institute, Gosport, Indiana Co-Director, CRAFT (Center for Research into the Anthropological Foundations of Technology), Indiana University, Bloomington, Indiana Adjunct Professor of Biology, Indiana University Secretary/Treasurer, Friends of CRAFT, Inc. (research and education non-profit) Fellow, American Association for the Advancement of Science Contact Information: Telephone: (812) 876-0080, ext. 202 (office); (812) 855-0086 (FAX) Email : [email protected] Address : Stone Age Institute 1392 W. Dittemore Road Gosport, IN 47433 Website : www.stoneageinstitute.org Education: Ph.D. (1984). University of California, Berkeley. Anthropology: Old World Prehistory program. M.A. (1979). University of California, Berkeley. Anthropology. Kent State University (1974-6). Masters Program, Anthropology. B.A. (1974), Kent State University. Anthropology Case-Western Reserve University (1967-8), Cleveland,Ohio, College of Arts and Sciences Areas of Special Interest: Old World prehistory, palaeoanthropology, evolution of technology, human adaptation, primate studies, archaeological site formation, geoarchaeology, taphonomy, zooarchaeology, hunter-gatherers, ethnoarchaeology, lithic technology, experimental archaeology, invention and technology, history of archaeology; Areas: Africa, Europe, Asia. 1 Academic Positions: 2000- present. Professor, Anthropology Department, Indiana University. 1994-2000 Associate Professor, Anthropology Department, Indiana University. 1989-1993 Assistant Professor, Anthropology Department, Indiana University. 1986-1989 Visiting Professor, Anthropology Department, Indiana University, Bloomington. 1986 Visiting Professor, Anthropology Department, U.C. Berkeley. -
The Perspective from Africa
Anthropogeny: The Perspective from Africa Public Symposium Friday, May 31, 2019 Chairs: Berhane Asfaw, Rift Valley Research Service & Lyn Wadley, University of the Witwatersrand Sponsored by: Center for Academic Research and Training in Anthropogeny (CARTA) With generous support from: The G. Harold and Leila Y. Mathers Charitable Foundation ABSTRACTS Australopithecus in East and South Africa Job Kibii, National Museums of Kenya Australopithecus is a genus of hominins whose evolutionary evidence is confined to the African continent. The genus evolved in eastern and/or southern Africa around 4 million years ago, eventually becoming extinct slightly less than two million years ago. Australopithecus is scientifically accepted as the common ancestor of the Paranthropus and Homo. Scientists recognize five species of Australopithecines; Australopithecus anamensis, A. afarensis, A. africanus, A. garhi, and A. sediba. Their relationship to each other and the earliest form of Homo, Homo habilis, remains controversial due to the sparse fossil record in Africa. There are two main ways of expressing evolutionary relationships: phylogenetic trees and cladograms. This presentation will explore current fossil evidence regarding members of the genus Australopithecus and their phylogenetic and cladistic relationships. The Chad Basin Andossa Likius, University of Moundou (Chad) Until recently, Chad has remained a poorly known country as far as paleontological research, compared to its neighbors on the African continent. But since 1994, the Mission Paléoanthropologique Franco-Chadienne (MPFT) is conducting intensive geological and paleontological surveys in the Djurab Desert. More than 400 Mio-Pliocene fossil sites dated between 3 and 7 million years ago (mya) have been identified. These sites have yielded rich and diverse fossil faunal assemblages of vertebrates, unique in Central Africa. -
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A NOTE ON THE TAPHONOMY OF LOWER MIOCENE FOSSIL LAND MAMMALS FROM THE MARINE CALVERT FORMATION AT THE POLLACK FARM SITE, DELAWARE1 Alan H. Cutler2 ABSTRACT The lower shell bed (marine) of the portion of the Cheswold sands of the lower Calvert Formation exposed at the Pollack Farm Site (now covered) near Cheswold, Delaware, is unusually rich in the remains of land mammals. Two models could pos- sibly explain the occurrence of terrestrial fossils within marine sediments: (1) post-mortem rafting of animal carcasses during floods, and (2) reworking of terrigenous bones following a marine transgression. Observations of the surface features of the mammalian bones suggest that the bones were exposed subaerially for a period of time before burial and that they were buried and permineralized prior to transport and abrasion. Carcass rafting is therefore unlikely, and reworking is the favored model of assemblage formation. Concentrations of fossil and subfossil land mammal bones in Georgia estuaries and on the Atlantic continental shelf provide possible analogs. INTRODUCTION terrigenous material within the lower shell bed to be 50–60 Terrestrial mammals occur sporadically in Tertiary mammal teeth per 1000 kg of matrix. marine sediments of the Atlantic Coastal Plain in the eastern The unusual richness of the land mammal assemblage United States. Such occurrences are important from a bio- at the Pollack Farm Site inevitably raises the question of its stratigraphic standpoint in that they form a link between ter- formation. What accounts for the presence of the land mam- restrial and marine biochronologies (Tedford and Hunter, mals in marine sediments? Mixed terrestrial/marine assem- 1984; Wright and Eshelman, 1987).