Isotopic Ecology and Human Palaeodiets in the Lower Basin of the Colorado River, Buenos Aires Province, Argentina

被引:55
|
作者
Martinez, G. [2 ]
Zangrando, A. F. [1 ]
Prates, L. [3 ]
机构
[1] Univ Buenos Aires, CONICET, Asociac Invest Antropol, Buenos Aires, DF, Argentina
[2] Univ Nacl Ctr Prov Buenos Aires, Fac Ciencias Sociales, CONICET, INCUAPA, RA-7400 Olavarria, Argentina
[3] Univ Nacl La Plata, Fac Ciencias Nat & Museo, CONICET, RA-1900 La Plata, Buenos Aires, Argentina
关键词
hunter-gatherers; eastern Pampean-Patagonian transition; Late Holocene; palaeodiet; carbon and nitrogen isotopes; BONE-COLLAGEN; NITROGEN; CARBON; ENRICHMENT; MARINE; DIET; C-13;
D O I
10.1002/oa.1057
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
Results of stable isotope analyses are presented for the study of human subsistence in the lower basin of the Colorado River, Buenos Aires province, Argentina. This paper provides the most current state of knowledge concerning isotopic research in the study area, which in turn sheds new light on such a significant region as the Pampa-Patagonia transitional zone, spatially related to the Atlantic coast. In addition, information from the middle basin of the Negro River is incorporated in the analysis and discussion. Both the construction of an isotopic ecology and the prehistoric human diets derived from delta C-13 and delta N-15 human isotope values for the area are explored. Stable isotope analysis of modern plants indicates a C-3 plant-based environment. Animal resources have delta C-13 values that indicate a diet based mainly on C-3 products. Nevertheless, they have highly variable delta N-15 values. Human isotopic values have the following mean values: -18.8 parts per thousand +/- 1.08 parts per thousand for delta C-13(COL) (n= 25), and 11.98 parts per thousand +/- 1.34 parts per thousand for delta N-15 (n=25). As a general trend, the results obtained from both C and N isotopic signals indicate a diet based on the consumption of protein provided by meat of terrestrial herbivores (e.g. artiodactyls) with the complement of fish. These results are in agreement with the data obtained from the zooarchaeological record for the Late Holocene. Copyright (C) 2009 John Wiley & Sons, Ltd.
引用
收藏
页码:281 / 296
页数:16
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