Stable isotope chemistry, population histories and Late Prehistoric subsistence change in the Aleutian Islands

被引:30
|
作者
Byers, David A. [1 ]
Yesner, David R. [2 ]
Broughton, Jack M. [3 ]
Coltrain, Joan Brenner [3 ]
机构
[1] Missouri State Univ, Dept Sociol Anthropol & Criminol, Springfield, MO 65897 USA
[2] Univ Alaska, Dept Anthropol, Anchorage, AK 99508 USA
[3] Univ Utah, Dept Anthropol, Salt Lake City, UT 84112 USA
基金
加拿大自然科学与工程研究理事会; 美国国家科学基金会;
关键词
Stable isotopes; Aleut; Aleutian Islands; Linear mixing model; EASTERN ARCTIC FORAGERS; TROPHIC RELATIONSHIPS; SOUTHWESTERN CAPE; SOUTH-AFRICA; FEEDING ECOLOGY; MARINE; CARBON; INSIGHTS; NITROGEN; PACIFIC;
D O I
10.1016/j.jas.2010.09.005
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
Aleut population history has been a topic of debate since the earliest archaeological investigations in the region. In this paper, we use stable isotope chemistry to evaluate the hypothesis that two distinct groups of people, Paleo- and Neo-Aleut, occupied the eastern Aleutians after 1000 BP. This study focuses on 80 sets of directly dated eastern Aleutian burial assemblages from Chaluka midden, Shiprock Island and Kagamil Island. We use a linear mixing model informed by isotopic analysis of two large Aleut faunal assemblages to address temporal and spatial variation in human carbon and nitrogen stable isotope data from these sites. The patterning we report addresses both Aleut demographic and economic prehistory, illustrating a transition in both at ca. 1000 BP. Our results suggests that the Chaluka diet, dominated by Paleo-Aleut inhumations, differed in both trophic level and foraging location from the other two sites for much of the past 4000 years. Trends in our data also suggest that individuals from Shiprock and Kagamil burial caves, primarily Neo-Aleuts, had enough access to higher trophic level foods to differentiate their bone chemistries from those buried in Chaluka midden. These trends in diet, recently reported genetic differences, as well as the introduction of novel mortuary practices at ca. 1000 BP, suggest that Neo-Aleuts do represent a population new to the eastern Aleutians. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:183 / 196
页数:14
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