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El paredón, México, fuente de obsidiana e intercambio formativo temprano
Resumen
Los estudios arqueológicos redescubrieron una fuente de obsidiana prehispánica en el centro de México. El análisis de oligoelementos reveló que la obsidiana de Paredón, no Otumba, fue crucial durante el período de formación temprana.
Área de la Ciencia:
- Arqueología Arqueología.
- La geoquímica es la geoquímica.
- Ciencia de los materiales Ciencia de los materiales.
Sus antecedentes:
- La fuente de obsidiana de Paredón en el centro de México fue reportada inicialmente en 1902.
- Encuestas arqueológicas en 1975 volvieron a identificar esta fuente a lo largo de antiguas rutas comerciales.
Objetivo del estudio:
- Determinar la fuente primaria de obsidiana utilizada en el centro de México durante el período formativo temprano.
- Para comparar los perfiles de oligoelementos de obsidiana de la fuente de Paredón con la obsidiana encontrada en Chalcatzingo.
Principales métodos:
- El análisis de activación de neutrones (NAA) se empleó para estudiar la composición de oligoelementos de muestras de obsidiana.
- Se realizaron estudios arqueológicos de superficie para identificar y reubicar las fuentes de obsidiana y las rutas comerciales asociadas.
Principales resultados:
- El análisis de elementos traza indicó una fuerte correlación entre la obsidiana de la fuente de Paredón y los artefactos de obsidiana encontrados en Chalcatzingo.
- Se descubrió que la obsidiana de la fuente de Paredón era de importancia primordial durante el período de formación temprana en el centro de México.
Conclusiones:
- La fuente de obsidiana de Paredón fue un importante contribuyente a la cultura material del centro de México durante el período formativo temprano.
- Los estudios de abastecimiento de obsidiana utilizando NAA son cruciales para comprender las antiguas redes comerciales y la utilización de los recursos.
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