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Radiocarbon Evidence Relating to Northern Great Basin Basketry Chronology
UC Merced Journal of California and Great Basin Anthropology Title Radiocarbon Evidence Relating to Northern Great Basin Basketry Chronology Permalink https://escholarship.org/uc/item/52v4n8cf Journal Journal of California and Great Basin Anthropology, 20(1) ISSN 0191-3557 Authors Connolly, Thomas J Fowler, Catherine S Cannon, William J Publication Date 1998-07-01 Peer reviewed eScholarship.org Powered by the California Digital Library University of California REPORTS Radiocarbon Evidence Relating ity over a span of nearly 10,000 years (cf. to Northern Great Basin Cressman 1942, 1986; Connolly 1994). Stages Basketry Chronology 1 and 2 are divided at 7,000 years ago, the approximate time of the Mt. Mazama eruption THOMAS J. CONNOLLY which deposited a significant tephra chronologi Oregon State Museum of Anthropology., Univ. of Oregon, Eugene, OR 97403. cal marker throughout the region. Stage 3 be CATHERINE S. FOWLER gins after 1,000 years ago,' when traits asso Dept. of Anthropology, Univ. of Nevada, Reno, NV ciated with Northern Paiute basketmaking tradi 89557. tions appear (Adovasio 1986a; Fowler and Daw WILLIAM J. CANNON son 1986; Adovasio and Pedler 1995; Fowler Bureau of Land Management, Lakeview, OR 97630. 1995). During Stage 1, from 11,000 to 7,000 years Adovasio et al. (1986) described Early ago, Adovasio (1986a: 196) asserted that north Holocene basketry from the northern Great ern Great Basin basketry was limited to open Basin as "simple twined and undecorated. " Cressman (1986) reported the presence of and close simple twining with z-twist (slanting decorated basketry during the Early Holo down to the right) wefts. Fort Rock and Spiral cene, which he characterized as a "climax Weft sandals were made (see Cressman [1942] of cultural development'' in the Fort Rock for technical details of sandal types). -
© in This Web Service Cambridge University
Cambridge University Press 978-1-107-01829-7 - Human Adaptation in the Asian Palaeolithic: Hominin Dispersal and Behaviour during the Late Quaternary Ryan J. Rabett Index More information Index Abdur, 88 Arborophilia sp., 219 Abri Pataud, 76 Arctictis binturong, 218, 229, 230, 231, 263 Accipiter trivirgatus,cf.,219 Arctogalidia trivirgata, 229 Acclimatization, 2, 7, 268, 271 Arctonyx collaris, 241 Acculturation, 70, 279, 288 Arcy-sur-Cure, 75 Acheulean, 26, 27, 28, 29, 45, 47, 48, 51, 52, 58, 88 Arius sp., 219 Acheulo-Yabrudian, 48 Asian leaf turtle. See Cyclemys dentata Adaptation Asian soft-shell turtle. See Amyda cartilaginea high frequency processes, 286 Asian wild dog. See Cuon alipinus hominin adaptive trajectories, 7, 267, 268 Assamese macaque. See Macaca assamensis low frequency processes, 286–287 Athapaskan, 278 tropical foragers (Southeast Asia), 283 Atlantic thermohaline circulation (THC), 23–24 Variability selection hypothesis, 285–286 Attirampakkam, 106 Additive strategies Aurignacian, 69, 71, 72, 73, 76, 78, 102, 103, 268, 272 economic, 274, 280. See Strategy-switching Developed-, 280 (economic) Proto-, 70, 78 technological, 165, 206, 283, 289 Australo-Melanesian population, 109, 116 Agassi, Lake, 285 Australopithecines (robust), 286 Ahmarian, 80 Azilian, 74 Ailuropoda melanoleuca fovealis, 35 Airstrip Mound site, 136 Bacsonian, 188, 192, 194 Altai Mountains, 50, 51, 94, 103 Balobok rock-shelter, 159 Altamira, 73 Ban Don Mun, 54 Amyda cartilaginea, 218, 230 Ban Lum Khao, 164, 165 Amyda sp., 37 Ban Mae Tha, 54 Anderson, D.D., 111, 201 Ban Rai, 203 Anorrhinus galeritus, 219 Banteng. See Bos cf. javanicus Anthracoceros coronatus, 219 Banyan Valley Cave, 201 Anthracoceros malayanus, 219 Barranco Leon,´ 29 Anthropocene, 8, 9, 274, 286, 289 BAT 1, 173, 174 Aq Kupruk, 104, 105 BAT 2, 173 Arboreal-adapted taxa, 96, 110, 111, 113, 122, 151, 152, Bat hawk. -
Fort Rock Cave: Assessing the Site’S Potential to Contribute to Ongoing Debates About How and When Humans Colonized the Great Basin
RETURN TO FORT ROCK CAVE: ASSESSING THE SITE’S POTENTIAL TO CONTRIBUTE TO ONGOING DEBATES ABOUT HOW AND WHEN HUMANS COLONIZED THE GREAT BASIN Thomas J. Connolly, Judson Byrd Finley, Geoffrey M. Smith, Dennis L. Jenkins, Pamela E. Endzweig, Brian L. O’Neill, and Paul W. Baxter Oregon’s Fort Rock Cave is iconic in respect to both the archaeology of the northern Great Basin and the history of debate about when the Great Basin was colonized. In 1938, Luther Cressman recovered dozens of sagebrush bark sandals from beneath Mt. Mazama ash that were later radiocarbon dated to between 10,500 and 9350 cal B.P. In 1970, Stephen Bedwell reported finding lithic tools associated with a date of more than 15,000 cal B.P., a date dismissed as unreasonably old by most researchers. Now, with evidence of a nearly 15,000-year-old occupation at the nearby Paisley Five Mile Point Caves, we returned to Fort Rock Cave to evaluate the validity of Bedwell’s claim, assess the stratigraphic integrity of remaining deposits, and determine the potential for future work at the site. Here, we report the results of additional fieldwork at Fort Rock Cave undertaken in 2015 and 2016, which supports the early Holocene occupation, but does not confirm a pre–10,500 cal B.P. human presence. La cueva de Fort Rock en Oregón es icónica por lo que representa para la arqueología de la parte norte de la Gran Cuenca y para la historia del debate sobre la primera ocupación de la Gran Cuenca. En 1938, Luther Cressman recuperó docenas de sandalias de corteza de artemisa debajo de una capa de cenizas del monte Mazama que fueron posteriormente fechadas por radiocarbono entre 10,500 y 9200 cal a.P. -
Early Members of the Genus Homo -. EXPLORATIONS: an OPEN INVITATION to BIOLOGICAL ANTHROPOLOGY
EXPLORATIONS: AN OPEN INVITATION TO BIOLOGICAL ANTHROPOLOGY Editors: Beth Shook, Katie Nelson, Kelsie Aguilera and Lara Braff American Anthropological Association Arlington, VA 2019 Explorations: An Open Invitation to Biological Anthropology is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License, except where otherwise noted. ISBN – 978-1-931303-63-7 www.explorations.americananthro.org 10. Early Members of the Genus Homo Bonnie Yoshida-Levine Ph.D., Grossmont College Learning Objectives • Describe how early Pleistocene climate change influenced the evolution of the genus Homo. • Identify the characteristics that define the genus Homo. • Describe the skeletal anatomy of Homo habilis and Homo erectus based on the fossil evidence. • Assess opposing points of view about how early Homo should be classified. Describe what is known about the adaptive strategies of early members of the Homo genus, including tool technologies, diet, migration patterns, and other behavioral trends.The boy was no older than 9 when he perished by the swampy shores of the lake. After death, his slender, long-limbed body sank into the mud of the lake shallows. His bones fossilized and lay undisturbed for 1.5 million years. In the 1980s, fossil hunter Kimoya Kimeu, working on the western shore of Lake Turkana, Kenya, glimpsed a dark colored piece of bone eroding in a hillside. This small skull fragment led to the discovery of what is arguably the world’s most complete early hominin fossil—a youth identified as a member of the species Homo erectus. Now known as Nariokotome Boy, after the nearby lake village, the skeleton has provided a wealth of information about the early evolution of our own genus, Homo (see Figure 10.1). -
Homo Erectus: a Bigger, Faster, Smarter, Longer Lasting Hominin Lineage
Homo erectus: A Bigger, Faster, Smarter, Longer Lasting Hominin Lineage Charles J. Vella, PhD August, 2019 Acknowledgements Many drawings by Kathryn Cruz-Uribe in Human Career, by R. Klein Many graphics from multiple journal articles (i.e. Nature, Science, PNAS) Ray Troll • Hominin evolution from 3.0 to 1.5 Ma. (Species) • Currently known species temporal ranges for Pa, Paranthropus aethiopicus; Pb, P. boisei; Pr, P. robustus; A afr, Australopithecus africanus; Ag, A. garhi; As, A. sediba; H sp., early Homo >2.1 million years ago (Ma); 1470 group and 1813 group representing a new interpretation of the traditionally recognized H. habilis and H. rudolfensis; and He, H. erectus. He (D) indicates H. erectus from Dmanisi. • (Behavior) Icons indicate from the bottom the • first appearance of stone tools (the Oldowan technology) at ~2.6 Ma, • the dispersal of Homo to Eurasia at ~1.85 Ma, • and the appearance of the Acheulean technology at ~1.76 Ma. • The number of contemporaneous hominin taxa during this period reflects different Susan C. Antón, Richard Potts, Leslie C. Aiello, 2014 strategies of adaptation to habitat variability. Origins of Homo: Summary of shifts in Homo Early Homo appears in the record by 2.3 Ma. By 2.0 Ma at least two facial morphs of early Homo (1813 group and 1470 group) representing two different adaptations are present. And possibly 3 others as well (Ledi-Geraru, Uraha-501, KNM-ER 62000) The 1813 group survives until at least 1.44 Ma. Early Homo erectus represents a third more derived morph and one that is of slightly larger brain and body size but somewhat smaller tooth size. -
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. -
In Search of the First Americas
In Search of the First Americas Michael R. Waters Departments of Anthropology and Geography Center for the Study of the First Americans Texas A&M University Who were the first Americans? When did they arrive in the New World? Where did they come from? How did they travel to the Americas & settle the continent? A Brief History of Paleoamerican Archaeology Prior to 1927 People arrived late to the Americas ca. 6000 B.P. 1927 Folsom Site Discovery, New Mexico Geological Estimate in 1927 10,000 to 20,000 B.P. Today--12,000 cal yr B.P. Folsom Point Blackwater Draw (Clovis), New Mexico 1934 Clovis Discovery Folsom (Bison) Clovis (Mammoth) Ernst Antevs Geological estimate 13,000 to 14,000 B.P. Today 13,000 cal yr B.P. 1935-1990 Search continued for sites older than Clovis. Most sites did not stand up to scientific scrutiny. Calico Hills More Clovis sites were found across North America The Clovis First Model became entrenched. Pedra Furada Tule Springs Clovis First Model Clovis were the first people to enter the Americas -Originated from Northeast Asia -Entered the Americas by crossing the Bering Land Bridge and passing through the Ice Free Corridor around 13,600 cal yr B.P. (11,500 14C yr B.P.) -Clovis technology originated south of the Ice Sheets -Distinctive tools that are widespread -Within 800 years reached the southern tip of South America -Big game hunters that killed off the Megafauna Does this model still work? What is Clovis? • Culture • Era • Complex Clovis is an assemblage of distinctive tools that were made in a very prescribed way. -
New Research at Paisley Caves: Applying New Integrated Analytical Approaches to Understanding Stratigraphy, Taphonomy and Site Formation Processes
Shillito L-M, Blong J, Jenkins D, Stafford TW, Whelton H, McDonough K, Bull I. New Research at Paisley Caves: Applying New Integrated Analytical Approaches to Understanding Stratigraphy, Taphonomy and Site Formation Processes. PaleoAmerica 2018 DOI: https://doi.org/10.1080/20555563.2017.1396167 Copyright: © 2018 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited DOI link to article: https://doi.org/10.1080/20555563.2017.1396167 Date deposited: 23/10/2017 This work is licensed under a Creative Commons Attribution 4.0 International License Newcastle University ePrints - eprint.ncl.ac.uk PaleoAmerica A journal of early human migration and dispersal ISSN: 2055-5563 (Print) 2055-5571 (Online) Journal homepage: http://www.tandfonline.com/loi/ypal20 New Research at Paisley Caves: Applying New Integrated Analytical Approaches to Understanding Stratigraphy, Taphonomy and Site Formation Processes Lisa-Marie Shillito, John C. Blong, Dennis L. Jenkins, Thomas W. Stafford Jr, Helen Whelton, Katelyn McDonough & Ian D. Bull To cite this article: Lisa-Marie Shillito, John C. Blong, Dennis L. Jenkins, Thomas W. Stafford Jr, Helen Whelton, Katelyn McDonough & Ian D. Bull (2018): New Research at Paisley Caves: Applying New Integrated Analytical Approaches to Understanding Stratigraphy, Taphonomy and Site Formation Processes, PaleoAmerica, DOI: 10.1080/20555563.2017.1396167 To link to this article: https://doi.org/10.1080/20555563.2017.1396167 © 2018 The Author(s). -
Human Origin Sites and the World Heritage Convention in Eurasia
World Heritage papers41 HEADWORLD HERITAGES 4 Human Origin Sites and the World Heritage Convention in Eurasia VOLUME I In support of UNESCO’s 70th Anniversary Celebrations United Nations [ Cultural Organization Human Origin Sites and the World Heritage Convention in Eurasia Nuria Sanz, Editor General Coordinator of HEADS Programme on Human Evolution HEADS 4 VOLUME I Published in 2015 by the United Nations Educational, Scientific and Cultural Organization, 7, place de Fontenoy, 75352 Paris 07 SP, France and the UNESCO Office in Mexico, Presidente Masaryk 526, Polanco, Miguel Hidalgo, 11550 Ciudad de Mexico, D.F., Mexico. © UNESCO 2015 ISBN 978-92-3-100107-9 This publication is available in Open Access under the Attribution-ShareAlike 3.0 IGO (CC-BY-SA 3.0 IGO) license (http://creativecommons.org/licenses/by-sa/3.0/igo/). By using the content of this publication, the users accept to be bound by the terms of use of the UNESCO Open Access Repository (http://www.unesco.org/open-access/terms-use-ccbysa-en). The designations employed and the presentation of material throughout this publication do not imply the expression of any opinion whatsoever on the part of UNESCO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The ideas and opinions expressed in this publication are those of the authors; they are not necessarily those of UNESCO and do not commit the Organization. Cover Photos: Top: Hohle Fels excavation. © Harry Vetter bottom (from left to right): Petroglyphs from Sikachi-Alyan rock art site. -
Quaternary Studies Near Summer Lake, Oregon Friends of the Pleistocene Ninth Annual Pacific Northwest Cell Field Trip September 28-30, 2001
Quaternary Studies near Summer Lake, Oregon Friends of the Pleistocene Ninth Annual Pacific Northwest Cell Field Trip September 28-30, 2001 springs, bars, bays, shorelines, fault, dunes, etc. volcanic ashes and lake-level proxies in lake sediments N Ana River Fault N Paisley Caves Pluvial Lake Chewaucan Slide Mountain pluvial shorelines Quaternary Studies near Summer Lake, Oregon Friends of the Pleistocene Ninth Annual Pacific Northwest Cell Field Trip September 28-30, 2001 Rob Negrini, Silvio Pezzopane and Tom Badger, Editors Trip Leaders Rob Negrini, California State University, Bakersfield, CA Silvio Pezzopane, United States Geological Survey, Denver, CO Rob Langridge, Institute of Geological and Nuclear Sciences, Lower Hutt, New Zealand Ray Weldon, University of Oregon, Eugene, OR Marty St. Louis, Oregon Department of Fish and Wildlife, Summer Lake, Oregon Daniel Erbes, Bureau of Land Management, Carson City, Nevada Glenn Berger, Desert Research Institute, University of Nevada, Reno, NV Manuel Palacios-Fest, Terra Nostra Earth Sciences Research, Tucson, Arizona Peter Wigand, California State University, Bakersfield, CA Nick Foit, Washington State University, Pullman, WA Steve Kuehn, Washington State University, Pullman, WA Andrei Sarna-Wojcicki, United States Geological Survey, Menlo Park, CA Cynthia Gardner, USGS, Cascades Volcano Observatory, Vancouver, WA Rick Conrey, Washington State University, Pullman, WA Duane Champion, United States Geological Survey, Menlo Park, CA Michael Qulliam, California State University, Bakersfield, -
Evolution of the 'Homo' Genus
MONOGRAPH Mètode Science StudieS Journal (2017). University of Valencia. DOI: 10.7203/metode.8.9308 Article received: 02/12/2016, accepted: 27/03/2017. EVOLUTION OF THE ‘HOMO’ GENUS NEW MYSTERIES AND PERSPECTIVES JORDI AGUSTÍ This work reviews the main questions surrounding the evolution of the genus Homo, such as its origin, the problem of variability in Homo erectus and the impact of palaeogenomics. A consensus has not yet been reached regarding which Australopithecus candidate gave rise to the first representatives assignable to Homo and this discussion even affects the recognition of the H. habilis and H. rudolfensis species. Regarding the variability of the first palaeodemes assigned to Homo, the discovery of the Dmanisi site in Georgia called into question some of the criteria used until now to distinguish between species like H. erectus or H. ergaster. Finally, the emergence of palaeogenomics has provided evidence that the flow of genetic material between old hominin populations was wider than expected. Keywords: palaeogenomics, Homo genus, hominins, variability, Dmanisi. In recent years, our concept of the origin and this species differs from H. rudolfensis in some evolution of our genus has been shaken by different secondary characteristics and in its smaller cranial findings that, far from responding to the problems capacity, although some researchers believe that that arose at the end of the twentieth century, have Homo habilis and Homo rudolfensis correspond to reopened debates and forced us to reconsider models the same species. that had been considered valid Until the mid-1970s, there for decades. Some of these was a clear Australopithecine questions remain open because candidate to occupy the «THE FIRST the fossils that could give us position of our genus’ ancestor, the answer are still missing. -
The Terminal Pleistocene/Early Holocene Record in the Northwestern Great Basin: What We Know, What We Don't Know, and How We M
PALEOAMERICA, 2017 Center for the Study of the First Americans http://dx.doi.org/10.1080/20555563.2016.1272395 Texas A&M University REVIEW ARTICLE The Terminal Pleistocene/Early Holocene Record in the Northwestern Great Basin: What We Know, What We Don’t Know, and How We May Be Wrong Geoffrey M. Smitha and Pat Barkerb aGreat Basin Paleoindian Research Unit, Department of Anthropology, University of Nevada, Reno, NV, USA; bNevada State Museum, Carson City, NV, USA ABSTRACT KEYWORDS The Great Basin has traditionally not featured prominently in discussions of how and when the New Great Basin; Paleoindian World was colonized; however, in recent years work at Oregon’s Paisley Five Mile Point Caves and archaeology; peopling of the other sites has highlighted the region’s importance to ongoing debates about the peopling of the Americas Americas. In this paper, we outline our current understanding of Paleoindian lifeways in the northwestern Great Basin, focusing primarily on developments in the past 20 years. We highlight several potential biases that have shaped traditional interpretations of Paleoindian lifeways and suggest that the foundations of ethnographically-documented behavior were present in the earliest period of human history in the region. 1. Introduction comprehensive review of Paleoindian archaeology was published two decades ago. We also highlight several The Great Basin has traditionally not been a focus of biases that have shaped traditional interpretations of Paleoindian research due to its paucity of stratified and early lifeways in the region. well-dated open-air sites, proboscidean kill sites, and demonstrable Clovis-aged occupations. Until recently, the region’s terminal Pleistocene/early Holocene (TP/ 2.