The Case of the Bipolar Technique
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Shang Dynasty
misterfengshui.com 風水先生 History of China ANCIENT 3 Sovereigns and 5 Emperors Xia Dynasty 2100–1600 BC Shang Dynasty 1600–1046 BC Zhou Dynasty 1122–256 BC Western Zhou Eastern Zhou Spring and Autumn Period Warring States Period IMPERIAL Qin Dynasty 221 BC–206 BC Han Dynasty 206 BC–220 AD Western Han Xin Dynasty Eastern Han Three Kingdoms 220–280 Wei, Shu & Wu Jin Dynasty 265–420 Western Jin 16 Kingdoms Eastern Jin 304–439 Southern & Northern Dynasties 420–589 Sui Dynasty 581–618 Tang Dynasty 618–907 ( Second Zhou 690–705 ) 5 Dynasties & 10 Kingdoms 907–960 Liao Dynasty 907–1125 Song Dynasty 960–1279 Northern Song Xi Xia Southern Song Jin Yuan Dynasty 1271–1368 Ming Dynasty 1368–1644 Qing Dynasty 1644–1911 MODERN Republic of China 1912–1949 People's Republic of China (Mainland China) 1949–present Republic of China (Taiwan) 1945-present from Wilkipedia [email protected] Fax: 852-2873-6859 misterfengshui.com 風水先生 Timeline of Chinese History The recorded history of China began in the 15th century BC when the Shang Dynasty started to use markings that evolved into the present Chinese characters. Turtle shells with markings reminiscent of ancient Chinese writing from the Shang Dynasty have been carbon dated to as early as 1500 BC.[1] Chinese civilization originated with city-states in the Yellow River (Huang He) valley. 221 BC is commonly accepted to be the year in which China became unified under a large kingdom or empire. In that year, Qin Shi Huang first united China. Successive dynasties in Chinese history developed bureaucratic systems that enabled the Emperor of China to control increasingly larger territory that reached maximum under the Mongolian Yuan Dynasty and Manchurian Qing Dynasty. -
Persistence of Middle Stone Age Technology to the Pleistocene/Holocene Transition Supports a Complex Hominin Evolutionary Scenario in West Africa
This is a repository copy of Persistence of Middle Stone Age technology to the Pleistocene/Holocene transition supports a complex hominin evolutionary scenario in West Africa. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/129212/ Version: Accepted Version Article: Scerri, E.M.L., Blinkhorn, J., Niang, K. et al. (2 more authors) (2017) Persistence of Middle Stone Age technology to the Pleistocene/Holocene transition supports a complex hominin evolutionary scenario in West Africa. Journal of Archaeological Science: Reports, 11. pp. 639-646. ISSN 2352-409X https://doi.org/10.1016/j.jasrep.2017.01.003 Reuse This article is distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) licence. This licence only allows you to download this work and share it with others as long as you credit the authors, but you can’t change the article in any way or use it commercially. More information and the full terms of the licence here: https://creativecommons.org/licenses/ 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/ Persistence of Middle Stone Age technology to the Pleistocene/Holocene transition supports a complex hominin evolutionary scenario in West Africa Eleanor M.L. Scerria*, James Blinkhornb, Khady Niangc, Mark D. Batemand, Huw S. Groucutta a Research -
Timeline from Ice Ages to European Arrival in New England
TIMELINE FROM ICE AGES TO EUROPEAN ARRIVAL IN NEW ENGLAND Mitchell T. Mulholland & Kit Curran Department of Anthropology, University of Massachusetts Amherst 500 Years Before Present CONTACT Europeans Arrive PERIOD 3,000 YBP WOODLAND Semi-permanent villages in which cultivated food crops are stored. Mixed-oak forest, chestnut. Slash and burn agriculture changes appearance of landscape. Cultivated plants: corn, beans, and squash. Bows and arrows, spears used along with more wood, bone tools. 6,000 YBP LATE Larger base camps; small groups move seasonally ARCHAIC through mixed-oak forest, including some tropical plants. Abundant fish and game; seeds and nuts. 9,000 YBP EARLY & Hunter/gatherers using seasonal camping sites for MIDDLE several months duration to hunt deer, turkey, ARCHAIC and fish with spears as well as gathering plants. 12,000 YBP PALEOINDIAN Small nomadic hunting groups using spears to hunt caribou and mammoth in the tundra Traditional discussions of the occupation of New England by prehistoric peoples divide prehistory into three major periods: Paleoindian, Archaic and Woodland. Paleoindian Period (12,000-9,000 BP) The Paleoindian Period extended from approximately 12,000 years before present (BP) until 9,000 BP. During this era, people manufactured fluted projectile points. They hunted caribou as well as smaller animals found in the sparse, tundra-like environment. In other parts of the country, Paleoindian groups hunted larger Pleistocene mammals such as mastodon or mammoth. In New England there is no evidence that these mammals were utilized by humans as a food source. People moved into New England after deglaciation of the region concluded around 14,000 BP. -
Lecture No. 5. the Evidence of Language Origins
Semiotix Course 2006, Cognition and symbolism in human evolution Robert Bednarik Lecture No. 5. The evidence of language origins Human language Culture refers to the individually acquired system of ‘understanding’ which reflects the distinctive life trajectory of the organism in question. It refers to socially rather than genetically transmitted behaviour patterns and their products. ‘Cultural dynamics’, therefore, are the processes by which the intelligent organism alters its perceptible reality through its dialectic participation in the processes shaping it (Bednarik 1990). Since the inevitable outcome of such interaction between percepts, concepts and behaviour patterns is selection in favour of increased level of ‘intelligence’, it is to be expected to result in forms of ‘consciousness’, such as those of humans. The process is reified through the perceptible (perceptible, for instance, to humans) externalizations of a species’ concepts onto physical reality (art, in the case of humans), which renders possible the reality constructs of the species, because the neural structures supporting such concepts become available for processing natural sensory stimuli in a taxonomizing format (Bednarik 1995: 628). Since this is the basis of human consciousness, it would be pointless trying to understand human constructs of reality without considering this evolutionary context, or their nexus with cognitive evolution. The purpose of this lecture is to examine the origins of human language ability itself, but this involves visiting several other issues, as well as considering a variety of potential explanations. There is no consensus on this subject at all, and the hypotheses we have range from one extreme to the other. According to the spectrum of current hypotheses, the advent of language occurred at some point between 3.5 million and 32,000 years ago. -
Disease Introduction by Aboriginal Humans in North America and the Pleistocene Extinction
Journal of Ecological Anthropology Volume 19 Issue 1 Volume 19, Issue 1 (2017) Article 2 April 2017 Disease Introduction by Aboriginal Humans in North America and the Pleistocene Extinction Zachary D. Nickell Hendrix College Matthew D. Moran Hendrix College Follow this and additional works at: https://scholarcommons.usf.edu/jea Part of the Biodiversity Commons, Ecology and Evolutionary Biology Commons, and the Immunology and Infectious Disease Commons Recommended Citation Nickell, Zachary D. and Moran, Matthew D.. "Disease Introduction by Aboriginal Humans in North America and the Pleistocene Extinction." Journal of Ecological Anthropology 19, no. 1 (2017): 29-41. Available at: https://scholarcommons.usf.edu/jea/vol19/iss1/2 This Crib Notes is brought to you for free and open access by the Anthropology at Scholar Commons. It has been accepted for inclusion in Journal of Ecological Anthropology by an authorized editor of Scholar Commons. For more information, please contact [email protected]. Disease Introduction by Aboriginal Humans in North America and the Pleistocene Extinction Cover Page Footnote ACKNOWLEDGEMENTS Thanks to C. N. Davis and R. Wells who provided valuable comments to earlier versions of this manuscript. Three anonymous reviewers greatly improved the manuscript. The project was supported in part by a grant to Z. Nickell from the Hendrix College Odyssey Program This crib notes is available in Journal of Ecological Anthropology: https://scholarcommons.usf.edu/jea/vol19/iss1/2 Moran & Nickell / Introduced Disease and Pleistocene Extinction CRIB NOTES Disease Introduction by Aboriginal Humans in North America and the Pleistocene Extinction Zachary D. Nickell Matthew D. Moran ABSTRACT While overhunting and climate change have been the major hypotheses to explain the late-Pleistocene New World megafaunal extinctions, the role of introduced disease has only received brief attention. -
Overkill, Glacial History, and the Extinction of North America's Ice Age Megafauna
PERSPECTIVE Overkill, glacial history, and the extinction of North America’s Ice Age megafauna PERSPECTIVE David J. Meltzera,1 Edited by Richard G. Klein, Stanford University, Stanford, CA, and approved September 23, 2020 (received for review July 21, 2020) The end of the Pleistocene in North America saw the extinction of 38 genera of mostly large mammals. As their disappearance seemingly coincided with the arrival of people in the Americas, their extinction is often attributed to human overkill, notwithstanding a dearth of archaeological evidence of human predation. Moreover, this period saw the extinction of other species, along with significant changes in many surviving taxa, suggesting a broader cause, notably, the ecological upheaval that occurred as Earth shifted from a glacial to an interglacial climate. But, overkill advocates ask, if extinctions were due to climate changes, why did these large mammals survive previous glacial−interglacial transitions, only to vanish at the one when human hunters were present? This question rests on two assumptions: that pre- vious glacial−interglacial transitions were similar to the end of the Pleistocene, and that the large mammal genera survived unchanged over multiple such cycles. Neither is demonstrably correct. Resolving the cause of large mammal extinctions requires greater knowledge of individual species’ histories and their adaptive tolerances, a fuller understanding of how past climatic and ecological changes impacted those animals and their biotic communities, and what changes occurred at the Pleistocene−Holocene boundary that might have led to those genera going extinct at that time. Then we will be able to ascertain whether the sole ecologically significant difference between previous glacial−interglacial transitions and the very last one was a human presence. -
The Early Paleolithic of China1) HUANG Weiwen2)
第 四 紀 研 究 (The Quaternary Research) 28 (4) p. 237-242 Nov. 1989 The Early Paleolithic of China1) HUANG Weiwen2) spread widely and existed for a long time. The Introduction deposits contained very rich fossils of mammal. 1. Geographic Distribution and the Types of The fauna exisiting in the stage from the early Deposits to the middle Pleistocene can be at least divided Before the 1940's, only one locality of the into three groups, which have their own Early Paleolithic period was discovered in characteristics and sequence: Nihewan fauna of China. That is Zhoukoudian near Beijing early Pleistocene, Gongwangling (Lantian Man) City (the site of Peking Man). Since the 1950's fauna of the latest stage of early Pleistocene many new localities have been found, of which or the earliest stage of middle Pleistocene and no less than fifteen are relatively important. Zhoukoudian (Peking Man) fauna of the middle These localities spread in North, South and Pleistocene. In the recent years, some scholars Northeast China covering a range from 23°35' to have suggested that locations of Dali and 40°15'N and from 101°58' to 124°8'E which Dingcun which originally recognized as be- includes two climate zones, namely, the sub- longing to the early stage of late Pleistocene tropical zone and warm temperate zone in the should place in the middle Pleistocene, as the eastern part of today's Asia (Fig. 1). latest stage of this epoch (LIU and DING,1984). The localities include three types of deposit: There also existed fluviatile and fluviol- 1) Fluviatile deposit: acustrine deposits of Pleistocene in South Xihoudu (Shanxi), Kehe (Shanxi), Lantian China. -
Pleistocene - the Ice Ages
Pleistocene - the Ice Ages Sleeping Bear Dunes National Lakeshore Pleistocene - the Ice Ages • Stage is now set to understand the nature of flora and vegetation of North America and Great Lakes • Pliocene (end of Tertiary) - most genera had already originated (in palynofloras) • Flora was in place • Vegetation units (biomes) already derived Pleistocene - the Ice Ages • In the Pleistocene, earth experienced intensification towards climatic cooling • Culminated with a series of glacial- interglacial cycles • North American flora and vegetation profoundly influenced by these “ice-age” events Pleistocene - the Ice Ages What happened in the Pleistocene? 18K ya • Holocene (Recent) - the present interglacial started ~10,000 ya • Wisconsin - the last glacial (Würm in Europe) occurred between 115,000 ya - 10,000 ya • Height of Wisconsin glacial activity (most intense) was 18,000 ya - most intense towards the end of the glacial period Pleistocene - the Ice Ages What happened in the Pleistocene? • up to 100 meter drop in sea level worldwide • coastal plains become extensive • continental islands disappeared and land bridges exposed 100 m line Beringia Pleistocene - the Ice Ages What happened in the Pleistocene? • up to 100 meter drop in sea level worldwide • coastal plains become extensive • continental islands disappeared and land bridges exposed Malaysia to Asia & New Guinea and New Caledonia to Australia Present Level 100 m Level Pleistocene - the Ice Ages What happened in the Pleistocene? • up to 100 meter drop in sea level worldwide • coastal -
Early Pleistocene Soricomorphs and Lagomorphs from the Xiaochangliang Site in the Nihewan Basin, Hebei, Northern China
ΐῒ῏ῑῐ ῍῎῍῎ῌThe Quaternary Research.1 - p. +/3 +1, June ,**2 Early Pleistocene soricomorphs and lagomorphs from the Xiaochangliang site in the Nihewan Basin, Hebei, Northern China Yingqi Zhang*+, and Yoshinari Kawamura* ,a This paper systematically describes soricomorph and lagomorph remains collected by a screen-washing procedure from the sediments of the Xiaochangliang site with the age of+4-0 Ma. The soricomorph remains described are assigned to the tribe Soricini in the subfamily Soricinae of the family Soricidae, on the basis of the detailed dental morphology. Among the genera of the tribe known from the Pliocene and Pleistocene of Asia,Sorex has morphological characters well coincident with those of the remains. Owing to their incompletion, the specific determination can not be done, and thus they are assigned merely toSorex sp. All the lagomorph remains belong to the family Ochotonidae. The family comprises two genera,Ochotona and Ochotonoi- des, in the Pliocene and Pleistocene of China. The remains are easily divided into a smaller and larger forms by their striking di# erence in size. The dental morphology and size of the smaller form indicate its allocation toOchotona. The smaller form is compared with many species ofOchotona known from the Pliocene and Pleistocene as well as the present day of China, and is assigned to the extinct species,O. youngi. The larger form is, however, assigned merely toOchotona or Ochotonoides sp., because of its limited specimens with poor preservation. Keywords : soricomorph, lagomorph, systematics, Early Pleistocene, Xiaochangliang site, Nihewan Basin, China knowledge on small mammals from the layer I. Introduction had been quite limited, until we washed the The Xiaochangliang site is one of the most sediments stratigraphically equivalent to the important archaeological sites of Early Pleisto- layer with fine-mesh screens in,**/ . -
Pleistocene-Holocene Permafrost of the East Siberian Eurasian Arctic Shelf
PLEISTOCENE-HOLOCENE PERMAFROST OF THE EAST SIBERIAN EURASIAN ARCTIC SHELF I.D. Danilov, I.A. Komarov, A.Yu. Vlasenko Department of Geology, Moscow State University, Moscow, Russia, 119899 e-mail: [email protected] Abstract Cryolithosphere dynamics in the East Siberian Eurasian Arctic shelf during the last 50,000 years were recon- structed on the basis of paleogeographic events including transgressions and regressions of the Arctic Ocean, and changes of paleoclimatic environmental conditions within subaerially exposed shelf areas after their flood- ing by sea water. Mathematical models and calculations were developed in accordance with these events. Three transgressive and three regressive stages in the evolution of the Arctic shelf were established for the last 50,000 years. Air and permafrost temperatures and their spatial and temporal variations were reconstructed for regres- sive epochs, while sea bottom temperatures, salinity and "overburden pressure" were reconstructed for trans- gressive periods. The possible thickness of permafrost in coastal areas is 345-455 m. The possible thickness of ice-bonded permafrost and non ice-bonded saline permafrost ranges from 240-350 and 20-25 m respectively in the central shelf, to 140-175 and 10 m in the outer shelf. Introduction Therefore, in order to solve this contradiction it is ne- cessary to estimate the extent of the Sartan regression. The formation of the modern subaquatic cryolithos- In the eastern sector of the Eurasian Arctic shelf, the sea phere (offshore permafrost) on the Eurasian Arctic shelf level fall is estimated variously at 110-120 m (Aksenov is usually assigned to the Pre-Holocene (Sartan) regres- et al., 1987), 100 m (Fartyshev, 1993), 90-100 m sion, and complete or partial degradation of the per- (Hopkins, 1976), 50 m (Zhigarev et al., 1982), and (mini- mafrost, to the subsequent (Flandrian) transgression. -
Was Agriculture Impossible During the Pleistocene but Mandatory During the Holocene? a Climate Change Hypothesis Author(S): Peter J
Society for American Archaeology Was Agriculture Impossible during the Pleistocene but Mandatory during the Holocene? A Climate Change Hypothesis Author(s): Peter J. Richerson, Robert Boyd, Robert L. Bettinger Source: American Antiquity, Vol. 66, No. 3 (Jul., 2001), pp. 387-411 Published by: Society for American Archaeology Stable URL: http://www.jstor.org/stable/2694241 Accessed: 28/11/2010 19:40 Your use of the JSTOR archive indicates your acceptance of JSTOR's Terms and Conditions of Use, available at http://www.jstor.org/page/info/about/policies/terms.jsp. JSTOR's Terms and Conditions of Use provides, in part, that unless you have obtained prior permission, you may not download an entire issue of a journal or multiple copies of articles, and you may use content in the JSTOR archive only for your personal, non-commercial use. Please contact the publisher regarding any further use of this work. Publisher contact information may be obtained at http://www.jstor.org/action/showPublisher?publisherCode=sam. Each copy of any part of a JSTOR transmission must contain the same copyright notice that appears on the screen or printed page of such transmission. JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Society for American Archaeology is collaborating with JSTOR to digitize, preserve and extend access to American Antiquity. -
Paleolithic Archaeology in China
AN41CH20-BarYosef ARI 21 June 2012 20:36 V I E E W R S Review in Advance first posted online on July 2, 2012. (Changes may still occur before final publication online and in print.) I E N C N A D V A Paleolithic Archaeology in China Ofer Bar-Yosef 1 and Youping Wang2 1Department of Anthropology, Harvard University, Cambridge, Massachusetts 02138; email: [email protected] 2School of Archaeology, Peking University, Beijing 100871, China; email: [email protected] Annu. Rev. Anthropol. 2012. 41:319–35 Keywords The Annual Review of Anthropology is online at Pleistocene, Zhoukoudian, Acheulian, microblades, pottery anthro.annualreviews.org This article’s doi: Abstract 10.1146/annurev-anthro-092611-145832 Despite almost a century of research, the Chinese Paleolithic chrono- Copyright c 2012 by Annual Reviews. cultural sequence still remains incomplete, although the number of well- All rights reserved dated sites is rapidly increasing. The Chinese Paleolithic is marked by 0084-6570/12/1021-0319$20.00 the long persistence of core-and-flake and cobble–tool industries, so interpretation of cultural and social behavior of humans in East Asia by Harvard University on 08/15/12. For personal use only. based solely on comparison with the African and western Eurasian pre- historic sequences becomes problematic, such as in assessing cognitive Annu. Rev. Anthropol. 2012.41. Downloaded from www.annualreviews.org evolutionary stages. For the Chinese Paleolithic, wood and bamboo likely served as raw materials for the production of daily objects since the arrival of the earliest migrants from western Asia, although poor preservation is a problem.