Biogeochemical reconstructions of life histories as a method to assess regional interactions: Stable oxygen and radiogenic strontium isotopes and Late Intermediate Period mobility on the Central Peruvian Coast

被引:18
|
作者
Marsteller, Sara J. [1 ]
Knudson, Kelly J. [1 ]
Gordon, Gwyneth [2 ]
Anbar, Ariel [2 ]
机构
[1] Arizona State Univ, Sch Human Evolut & Social Change, POB 872402, Tempe, AZ 85287 USA
[2] Arizona State Univ, Sch Earth & Space Explorat, POB 871404, Tempe, AZ 85287 USA
基金
美国国家科学基金会;
关键词
Bone; Tooth enamel; Soil; Water; Central Andes; Rimac Valley; RESIDENTIAL-MOBILITY; BONE PHOSPHATE; TOOTH ENAMEL; ANCIENT-CITY; MACHU-PICCHU; RESOURCE USE; MIGRATION; IMMIGRATION; TEOTIHUACAN; DIAGENESIS;
D O I
10.1016/j.jasrep.2017.04.016
中图分类号
K85 [文物考古];
学科分类号
0601 ;
摘要
Biogeochemical reconstructions of life histories of mobility offer a means to obtain nuanced information about regional interactions in the past. We test this method using the Late Intermediate Period Ychsma society on the central Peruvian coast as a case study. Archaeological and ethnohistoric evidence indicates that the Rimac and Lurin Valleys inhabited by the Ychsma served as a key regional hub for the religious and administrative activities of the Inca Empire and the Spanish Viceroyalty. The nature of regional interactions prior to Inca imperial influence, however, remains unclear. Well-known historical narratives describe populations from the adjacent Huarochiri highlands defeating coastal Ychsma populations for agricultural land, but archaeological evidence concerning the timing and extent of coastal-highland interactions is debated. Here, we assess the potential for radiogenic strontium and stable oxygen isotopic reconstruction of mobility over the life course to shed light on the regional interactions of coastal Ychsma groups during the Late Intermediate Period. We present Sr-87/Sr-86 and delta O-18 results for 61 regional environmental baseline samples and archaeological human tooth enamel and bone samples from 64 individuals buried at Armatambo and Rinconada Alta, in the Rimac Valley. Results reveal a broad isotopic range for baseline and archaeological samples likely due to diversity in water and bedrock sources. Nevertheless, one individual presents a non-local strontium value indicating mobility to an outside region. We discuss the advantages of a life history approach, the complications of using isotopes to assess mobility in the Central Andes, and suggested directions for future research.
引用
收藏
页码:535 / 546
页数:12
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