Relating Palaeo-Eskimo Lithic Technological Change and Human Mobility Patterns in Southeastern Victoria Island, Nunavut
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Microblade–Based Societies in North China at the End of the Ice Age
quaternary Article Microblade–Based Societies in North China at the End of the Ice Age Meng Zhang 1,2 1 Department of Cultural Heritage and Museology, Fudan University, Shanghai 200433, China; [email protected] 2 Institute of Archaeological Science, Fudan University, Shanghai 200433, China Received: 23 May 2020; Accepted: 3 July 2020; Published: 9 July 2020 Abstract: One of the most prominent cultural changes during the end of Ice Age in northeastern Asia was the adoption of microblade technology by prehistoric hunter–gatherers to deal with the challenge brought by the climate deterioration and oscillation during and post the Last Glacial Maximum (LGM). The Pleistocene to Holocene transition in North China witnessed the rise of broader spectrum subsistence alongside a series of cultural changes, including adoption of food production, highly mobile lifeways being replaced by sedentism, and the formation of new social organization based on their agricultural land–use patterns. From the perspective of technological change, this project aims to build a socio–ecological framework to examine the cultural change of prehistoric microblade–based societies. In contrast to previous studies, the present research employs a macroecological approach based on Binford’s Constructing Frames of Reference (2001) to reconstruct the behaviors and demography of prehistoric foraging groups, under both modern and LGM climate conditions. Three case studies are conducted to show cultural and technological changes among microblade–based societies in North -
Geology of Greenland Bulletin 185, 67-93
Sedimentary basins concealed by Acknowledgements volcanic rocks The map sheet was compiled by J.C. Escher (onshore) In two areas, one off East Greenland between latitudes and T.C.R. Pulvertaft (offshore), with final compilation 72° and 75°N and the other between 68° and 73°N off and legend design by J.C. Escher (see also map sheet West Greenland, there are extensive Tertiary volcanic legend). In addition to the authors’ contributions to the rocks which are known in places to overlie thick sedi- text (see Preface), drafts for parts of various sections mentary successions. It is difficult on the basis of exist- were provided by: L. Melchior Larsen (Gardar in South ing seismic data to learn much about these underlying Greenland, Tertiary volcanism of East and West Green- sediments, but extrapolation from neighbouring onshore land); G. Dam (Cretaceous–Tertiary sediments of cen- areas suggests that oil source rocks are present. tral West Greenland); M. Larsen (Cretaceous–Tertiary Seismic data acquired west of Disko in 1995 have sediments in southern East Greenland); J.C. Escher (map revealed an extensive direct hydrocarbon indicator in of dykes); S. Funder (Quaternary geology); N. Reeh the form of a ‘bright spot’ with a strong AVO (Amplitute (glaciology); B. Thomassen (mineral deposits); F.G. Versus Offset) anomaly, which occurs in the sediments Christiansen (petroleum potential). Valuable comments above the basalts in this area. If hydrocarbons are indeed and suggestions from other colleagues at the Survey are present here, they could either have been generated gratefully acknowledged. below the basalts and have migrated through the frac- Finally, the bulletin benefitted from thorough reviews tured lavas into their present position (Skaarup & by John Korstgård and Hans P. -
The Mesa Site: Paleoindians Above the Arctic Circle
U. S. Department of the Interior BLM-Alaska Open File Report 86 Bureau of Land Management BLM/AK/ST-03/001+8100+020 April 2003 Alaska State Office 222 West 7th Avenue Anchorage Alaska 99513 The Mesa Site: Paleoindians above the Arctic Circle Michael Kunz, Michael Bever, Constance Adkins Cover Photo View of Mesa from west with Iteriak Creek in foreground. Photo: Dan Gullickson Disclaimer The mention of trade names or commercial products in this report does not constitute endorsement or recommendation for use by the federal government. Authors Michael Kunz is an Archaeologist, Bureau of Land Management (BLM), Northern Field Office, 1150 University Avenue, Fairbanks, Alaska 99709. Michael Bever is a project supervisor for Pacific Legacy Inc., 3081 Alhambra Drive, Suite 208, Cameron Park, CA 95682. Constance Adkins is an Archaeologist, Bureau of Land Management (BLM), Northern Field Office, 1150 University Avenue, Fairbanks, Alaska 99709. Open File Reports Open File Reports issued by the Bureau of Land Management-Alaska present the results of invento- ries or other investigations on a variety of scientific and technical subjects that are made available to the public outside the formal BLM-Alaska technical publication series. These reports can include preliminary or incomplete data and are not published and distributed in quantity. The reports are available while supplies last from BLM External Affairs, 222 West 7th Avenue #13, Anchorage, Alaska 99513 and from the Juneau Minerals Information Center, 100 Savikko Road, Mayflower Island, Douglas, AK 99824, (907) 364-1553. Copies are also available for inspection at the Alaska Resource Library and Information Service (Anchorage), the USDI Resources Library in Washington, D. -
ARCTIC RIFT COPPER Part of World’S Newest Metallogenic Province: Kiffaanngissuseq
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/346029727 ARCTIC RIFT COPPER Part of world’s newest metallogenic province: Kiffaanngissuseq Technical Report · November 2020 DOI: 10.13140/RG.2.2.18610.84161 CITATIONS 0 2 authors, including: Jonathan Bell Curtin University 17 PUBLICATIONS 13 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Greenland View project Mineral asset valuation and pricing View project All content following this page was uploaded by Jonathan Bell on 20 November 2020. The user has requested enhancement of the downloaded file. ARCTIC RIFT COPPER Part of world’s newest metallogenic province: Kiffaanngissuseq Technical Assessment Report Greenfields Exploration Ltd November 2020 This report presents a holistic view of north eastern Greenland’s geology. The empirical evidence of mineralisation and geological record are tied in with mineral system components from global through to prospect scales. The source rocks, geodynamic triggers, pathways, and deposition sites are all identified within a preserved terrane. This work defines the Kiffaanngissuseq metallogenic province, a previously undescribed mineral system. For the first time, we identify a c. 1,250 Ma orogenic event in the basement as the geodynamic trigger related to the basalt- hosted native copper within the Arctic Rift Copper project. A c. 385 Ma fluid migration is identified as the trigger for a second copper-sulphide mineralising event expressed within the project, that also emplaced a distal zinc deposit within Kiffaanngissuseq. This multi-episodal mineral system is supported by a regional geochemical and hydrodynamic framework that is not articulated elsewhere. -
A North American Perspective on the Volg (PDF)
Quaternary International xxx (xxxx) xxx–xxx Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint A North American perspective on the Volgu Biface Cache from Upper Paleolithic France and its relationship to the “Solutrean Hypothesis” for Clovis origins J. David Kilby Department of Anthropology, Texas State University, San Marcos, TX, USA ARTICLE INFO ABSTRACT Keywords: The “Solutrean hypothesis” for the origins of the North American Clovis Culture posits that early North American Volgu colonizers were direct descendants of European populations that migrated across the North Atlantic during the Clovis European Upper Paleolithic. The evidential basis for this model rests largely on proposed technological and Solutrean behavioral similarities shared by the North American Clovis archaeological culture and the French and Iberian Cache Solutrean archaeological culture. The caching of stone tools by both cultures is one of the specific behavioral correlates put forth by proponents in support of the hypothesis. While more than two dozen Clovis caches have been identified, Volgu is the only Solutrean cache identified at this time. Volgu consists of at least 15 exquisitely manufactured bifacial stone tools interpreted as an artifact cache or ritual deposit, and the artifacts themselves have long been considered exemplary of the most refined Solutrean bifacial technology. This paper reports the results of applying methods developed for the comparative analysis of the relatively more abundant caches of Clovis materials in North America to this apparently singular Solutrean cache. In addition to providing a window into Solutrean technology and perhaps into Upper Paleolithic ritual behavior, this comparison of Clovis and Solutrean assemblages serves to test one of the tangible archaeological implications of the “Solutrean hypoth- esis” by evaluating the technological and behavioral equivalence of Solutrean and Clovis artifact caching. -
On the Processes of Diversification in Microblade Technocomplexes in the Late 29 Glacial Hokkaido Yuichi Nakazawa and Satoru Yamada
Nakazawa and Yamada On the Processes of Diversification in Microblade Technocom- plexes in the Late Glacial Hokkaido On the Processes of Diversification in Microblade Technocomplexes in the Late 29 Glacial Hokkaido Yuichi Nakazawa and Satoru Yamada ABSTRACT Microblade technology was a newly invented technology sented by the emergence of various technocomplexes in among modern humans in northeastern Asia during the the Late Glacial. The diversification processes occurred terminal Pleistocene. Because of its pan-regional distri- gradually at a millennial scale, suggesting that the tech- bution, wedge- shaped microblade cores have long been nological changes in microblade technocomplexes and regarded as a cultural marker and a technology critical tool assemblages resulted from demographic pressure. to debates concerning the peopling of the New World. In Hokkaido, where numerous Late Glacial archaeological Introduction sites are recorded, microblade assemblages exhibit nota- ble variability in stone tool classes and the morphotech- The past three decades have witnessed consistent debate nological characteristics of microblade cores. This paper focused on the origin of modern humans. As McBrearty addresses the questions of how and why the variability and Brooks (2000) demonstrated in Africa, the archaic in microblade technocomplexes emerged in Late Gla- to modern behavioral transition was gradual and is ex- cial Hokkaido (northern Japan). By employing a large pressed in certain aspects of the archaeological record data set of microblade technocomplexes from Hokkaido, (i.e., abstract thinking; planning depth; behavioral, eco- we measure richness and evenness of stone tool classes nomic, and technological innovativeness; and symbolic among four continuous phases (i.e., pre–Last Glacial behavior) that vary according to geographic region. -
Descriptive Text to the 1995 Geological Map of Greenland, 1:2 500 000
GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 18 2009 Greenland from Archaean to Quaternary Descriptive text to the 1995 Geological map of Greenland, 1:2 500 000. 2nd edition Niels Henriksen, A.K. Higgins, Feiko Kalsbeek and T. Christopher R. Pulvertaft GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Geological Survey of Denmark and Greenland Bulletin 18 Keywords Archaean, Caledonides, Cenozoic, economic geology, geological map, Greenland, ice sheet, Mesozoic, offshore, orogenic belts, Palaeozoic, petroleum, Phanerozoic, Proterozoic, sedimentary basins. Cover illustration The cover design depicts mountains of the East Greenland Caledonian fold belt. The view, west of Mestersvig (located on map, page 4), is north over Bersærkerbræ and the northern part of the Stauning Alper to Kong Oscar Fjord with Traill Ø in the right backgro- und. The mountains up to 1800 m high are of the Neoproterozoic Eleonore Bay Supergroup. To the right: first author Niels Henriksen, for many years head of geological mapping at GGU/GEUS, and participant in field work in Greenland for more than 45 years. Frontispiece: facing page Major Caledonian syncline involving reactivated Archaean basement gneisses containing amphibolite bands. Overlying rusty coloured Mesoproterozoic metasediments (Krummedal supracrustal sequence) just visible in tight core of the fold. The intensity of deformation in the syncline clearly increases towards the core, where the basement gneisses become more strongly foliated. Some of the amphibolite bands were derived from cross-cutting basic intrusions, which are still discernable in the less severely deformed parts of the Archaean basement (Fig. 17, p. 31). The height of the section is c. 2000 m. -
Chapter 3 a Projectile Point Sequence for Haida Gwaii
Chapter 3 A Projectile Point Sequence for Haida Gwaii Daryl W. Fedje†, Quentin Mackie‡, D. McLaren‡, and Tina Christensen§ † Parks Canada, Victoria, B.C. ‡ University of Victoria, Victoria, B.C. § Pender Island, B.C. Introduction In 1891 a chipped stone arrowhead was found by Haida Gwaii (Figures 1 and 2) cultural history fur trader Alexander Mackenzie in Naden Harbour has been divided into three main cultural constructs in the north of Haida Gwaii. When shown to lo- based on technological characteristics including the cal Haida they remarked that “they had never seen Kinggi Complex, Moresby Tradition and Graham or heard of such a thing before” (Mackenzie and Tradition (Fedje and Christensen 1999; Fladmark Dawson 1891). Subsequent investigations, includ- 1989). The Kinggi Complex dates from ca. 10,600 ing the intensive surveys (Fladmark 1970; Gessler to 8750 BP and is characterized by bifacial technol- 1972; Hobler 1976) and excavations (Fladmark ogy, simple core and flake tools, and an absence of 1986, 1990; Sutherland 1974) of the late 60s, 70s, microblades. The complex is derived from a small and 80s led Fladmark (1989:216) to describe Ha- number of excavated sites in the south of Haida ida Gwaii stone tool assemblages as “nearly single- Gwaii and a scattering of surface finds across the mindedly unifacial local lithic traditions”. For the archipelago. The Moresby Tradition dates from period dating after 8000 BP1 this still holds true ca. 8750 to 5000 BP and is characterized by a focus with the only excavated bifaces being two obsidian on microblade technology and simple core and flake specimens from the Blue Jackets Creek site dating tools. -
Prehistory of the Northwest Coast ROY L
CHAPTER 1 Prehistory of the Northwest Coast ROY L. CARLSON n the beginning there was ice ... in the end there were ice. Sub-arctic and then temperate fauna spread into this approximately 100,000 Indian people living along the new found land. Man was part of this fauna; he preyed IPacific coast from southeast Alaska to the mouth of on the other animals for food and used their hides for the Columbia River in Oregon ... in between is the pre clothing. He arrived by different routes, and brought historic period, the time span of the unknown, between with him different cultural traditions. By 10,000 years the retreat of the last continental glacier and the arrival ago ice only existed in the mountain top remnants we of the first Europeans with their notebooks and artist's still see today. sketches who ushered in the period of written history. The Northwest Coast (Fig. 1:1) is a ribbon of green, The prehistoric period here lasted from perhaps 12,000 wet forested land which hugs the Pacific coast of North years ago to the late 1700's when Cook, Vancouver, America from the mouth of the Copper River in Alaska Mackenzie and others began writing about the area and to just below the mouth of the Klamath River in northwest its inhabitants. Glacial geology suggests that the coast California. It was part of the "Salmon Area" of early was ice free by 12,000 years ago, but there remains the ethnographers and its cultures were clearly different possibility of even earlier movements of peoples whose from those of the California acorn area, the agricultural traces were wiped out by the last glacial advance. -
Arkæologisk/Kulturhistorisk Bidrag Til ”Zone-Inddeling Af Nationalparken”
Nunatta Katersugaasivia Allagaateqarfialu Greenland National Museum and Archives P.O. Boks 145; 3900 – Nuuk; Grønland/Greenland. Tlf.: +(299) 322611; Fax: (+299) 322622 e-mail: [email protected] ; home page: www.natmus.gl 29. december 2009 Arkæologisk/kulturhistorisk bidrag til ”Zone-inddeling af Nationalparken” Revideret Version, dec 2009. NKA = Nunatta Katersugaasivia Allagaateqarfialu / Grønlands Nationalmuseum og Arkiv. Hermed fremsendes oversigt over de områder, som Grønlands Nationalmuseum og Arkiv anser for særligt beskyttelsesværdige. Arkæologiske lokaliteter i Nord- og Nordøstgrønland Særkendet ved Nationalparken er, at lovgivningen både beskytter hele den synlige forhistorie og de kultur- og naturlandskaber, som er skabt gennem årtusinder. I takt med forbedrede transport- og sikkerhedsteknologier vil interessen for at besøge fjerne, eksotiske områder stige. Det betyder, at der må tages særlige forhold i brug for at beskytte dette unikke, arktiske kulturlandskab. Kulturminder I betragtning af Grønlands størrelse er der kun få kulturminder; den begrænsede mængde er et produkt af en kort historie (4.400 år), de nomadiske livsformer og få personer i hver kulturperiode. I de eskimoiske kulturer er der generelt fokus på de samme ressourcer: sæl, hval, rensdyr, moskusokse og fugle og visse lokalitetstyper som polynia-områder, der ofte rummer særlige bopladser, som skal sikres, fordi de har stort forskningspotentiale, stort formidlingspotentiale og lign. Mange forskellige parametre medgår derfor ved udskillelsen af særligt sårbare områder I Nationalparken stiger mængden af fortidsminder fra Nord til Syd. Det store skift sker omkring 77°N (nordlige Germania Land). Nord for denne bredde-grad er de fleste kulturminder stærkt eksponerede, fordi der næsten ingen jordpålejring har været gennem 4.400 år - udover flyvesand. -
05 AP 54.1Seong.Pdf
Diversity of Lithic Assemblages and Evolution of Late Palaeolithic Culture in Korea CHUNtaeK SeoNg introduction Since the 1990s, a growing number of archaeological excavations and sys- tematic surveys in Korea have provided a rapid accumulation of Palaeolithic ar- chaeological data: more than 1000 locations with archaeological remains are recognized and mapped, while some 200 sites were archaeologically excavated in the southern Korean Peninsula (Fig. 1, table 1). this growth of Palaeolithic research has enabled archaeologists to discuss various issues including chronology, lithic technology, and site function and structure. one of the key characteristics of the Late Palaeolithic in Korea is the diversity of lithic assemblages. While the Late or Upper Palaeolithic in general is characterized by blades and blade industries, tanged points are important components of early Late Palaeolithic lithic assemblages, which often do not contain blades. Lithic assemblages made of coarse quartzite and vein quartz persisted even until the end of the Pleisto- cene, while blades and microblades dominate other lithic assemblages. In what fol- lows, I review the complexity of lithic assemblages and attempt to derive a picture of the evolution of lithic technology in the Late Palaeolithic. the late palaeolithic concept Discussions of Korean and east asian Palaeolithic sequences have been impeded by the continual use of the conventional time frame for the european Lower-Middle- Upper Palaeolithic (gao and Norton 2002; Ikawa-Smith 1978; Seong 2002). Despite wide differences in dates in different regions in the old World, the subdivision of the Palaeolithic known as the Middle Palaeolithic (in europe and asia) or Middle Stone age (in africa) is widely used to denote a time period lasting from 300,000 –200,000 to 40,000 –30,000 years ago. -
SFU Thesis Template Files
Identifying Microblade Function at EeRb-140 and EeRb-144, Kamloops, British Columbia by Ryan M. Dickie B.A., Simon Fraser University, 2008 Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Arts in the Department of Archaeology Faculty of Environment Ryan Michael Dickie 2015 SIMON FRASER UNIVERSITY Spring 2015 Approval Name: Ryan Michael Dickie Degree: Master of Arts Title: Identifying Microblade Function at EeRb-140 and EeRb-144, Kamloops, B.C. Examining Committee: Chair: Ross Jamieson Professor George Nicholas Senior Supervisor Professor Robert J. Muir Supervisor Senior Lecturer Stanley Copp External Examiner Professor and Department Chair Sociology and Anthropology Langara College March 6, 2015 Date Defended/Approved: ii Partial Copyright Licence iii Abstract The microblade industry of the Pacific Northwest represents a discrete artifact category that is often cited as temporal and/or cultural markers, yet their precise function is poorly understood. The research presented here explored microblade function through use- wear analyses of assemblages collected from two Middle Period-aged sites (7,500-4,000 years BP) on the Kamloops Indian Reserve, EeRb-140 and EeRb-144. These two sites, related closely in terms of space and time, offer a good opportunity to explore some of the assumptions about microblade and their potential functions. Microblades are considered important indicators of Middle Period components. When encountered they are often presumed to reflect either elements of composite hunting weapons or implements utilized for a suite of specialized activities. However the results of the use- wear analysis indicate that, at least at EeRb-140 and EeRb-144, microblades served many purposes.