Aspects of Neolithic Obsidian Lithic Technology: A Debitage Analysis from Janghang, Gadeok-do

2021 ◽  
Vol 114 ◽  
pp. 35-61
Author(s):  
Sojin Kwon
1985 ◽  
Vol 50 (4) ◽  
pp. 755-779 ◽  
Author(s):  
Alan P. Sullivan ◽  
Kenneth C. Rozen

AbstractThe systematic study of chipped stone debitage provides important information about prehistoric lithic technology. However, the results of most debitage analyses are unconvincing because of questionable assumptions and inherent flaws in the typologies used to classify the material. After briefly reviewing these problems, we present an alternative approach that does not rely on the presumed technological origins of individual artifacts as the basis for debitage classification and interpretation. An important element of this approach is a typology composed of interpretation-free and mutually exclusive debitage categories. The derivation of this typology is described and the utility of the approach is demonstrated with two Arizona case studies. The TEP St. Johns project provides new data and interpretations about Archaic Period technological and settlement changes while the Pitiful Flats study illustrates how differences in functional and organizational factors affect debitage assemblage variability.


2021 ◽  
Vol 13 (7) ◽  
Author(s):  
José-Manuel Maíllo-Fernández ◽  
Blanca Jiménez-García
Keyword(s):  

2010 ◽  
Vol 23 (2) ◽  
pp. 20-39 ◽  
Author(s):  
Rafael Suárez ◽  
Guaciara M. Santos

On this paper we show records of Pleistocene fauna from the archaeological site of PayPaso 1, located near of the Quarai River. On this site we recovered two extinct species, Equus sp. (ancient horse) e Glyptodon sp. (giant armadillo), direct associated with lithic artifacts. Our results indicate that these extinct mammals lived in the beginning of the Holocene (9,600 – 9,100 years 14C BP), based on nine 14C age results obtained by AMS (Accelerator Mass Spectrometry) measurements. In this work, these results are compared with others in South America. Human adaptation, lithic technology, Pleistocene fauna extinction and climate change at the transition between Pleistocene-Holocene are also discussed.


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