: Monte Verde: A Late Pleistocene Settlement in Chile. Volume 1: Palaeoenvironment and Site Context . Tom D. Dillehay.

1991 ◽  
Vol 93 (3) ◽  
pp. 739-739 ◽  
Author(s):  
David Meltzer
Keyword(s):  
2019 ◽  
Vol 92 (1) ◽  
pp. 70-80 ◽  
Author(s):  
Tom D. Dillehay ◽  
Carlos Ocampo ◽  
Jose Saavedra ◽  
Mario Pino ◽  
Linda Scott-Cummings ◽  
...  

AbstractThis paper presents new excavation data on the Chinchihuapi I (CH-I) locality within the Monte Verde site complex, located along Chinchihuapi Creek in the cool, temperate Valdivian rain forest of south-central Chile. The 2017 and 2018 archaeological excavations carried out in this open-air locality reveal further that CH-I is an intermittently occupied site dating from the Early Holocene (~10,000 cal yr BP) to the late Pleistocene (at least ~14,500 cal yr BP) and probably earlier. A new series of radiocarbon dates refines the chronology of human use of the site during this period. In this paper, we describe the archaeological and stratigraphic contexts of the recent excavations and analyze the recovered artifact assemblages. A fragmented Monte Verde II point type on an exotic quartz newly recovered from excavations at CH-I indicates that this biface design existed in at least two areas of the wider site complex ~14,500 cal yr BP. In addition, associated with the early Holocene component at CH-I are later Paijan-like points recovered with lithic tools and debris and other materials. We discuss the geographic distribution of diagnostic artifacts from the site and their probable relationship to other early sites in South America.


1999 ◽  
Vol 64 (3) ◽  
pp. 455-460 ◽  
Author(s):  
R. E. Taylor ◽  
C. Vance Haynes ◽  
Donna L. Kirner ◽  
John R. Southon

Radiocarbon measurements have been obtained on contemporary plant samples collected at the site of Monte Verde, Chile, to examine the possibility that a local l4C reservoir effect impinges on the accuracy of the l4C values obtained on previously recovered archaeological samples. The l4C activity of the modern plants do not reveal any offset from expected contemporary l4C values and thus provide no support for a major postulated reservoir effect at least for the recent past. Although there is, at present, no direct means of measuring potential l4C reservoir offsets in the late Pleistocene for this region, we are not aware of any current data that would indicate that there have been major changes during geologically recent times.


Man ◽  
1991 ◽  
Vol 26 (1) ◽  
pp. 165
Author(s):  
Jose R. Oliver ◽  
Tom D. Dillehay
Keyword(s):  

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