Thursday, June 14, 2018
Mesomerican turquoise may have different origin than previously thought
New research published today in the journal Science Advances overturns more than a century of thought about the source of turquoise used by ancient civilizations in Mesoamerica, the vast region that extends from Central Mexico to Central America. For more than 150 years, scholars have argued that the Aztec and Mixtec civilizations, which revered the precious, blue-green mineral, acquired it through import from the American Southwest. However, extensive geochemical analyses reveal that the true geologic source of Aztec and Mixtec turquoise lies within Mesoamerica.
Geochemist Alyson Thibodeau, assistant professor of earth sciences at Dickinson College, and a team of researchers from the University of Arizona, California State University at San Bernardino, and the Museo del Templo Mayor in Mexico City, measured the isotopic signatures of Mesoamerican turquoise artifacts associated with both the Aztecs and Mixtecs. These isotopic signatures function like fingerprints that can be used to determine the geologic origins of the turquoise.
Specifically, Thibodeau and her research team carried out analyses of lead and strontium isotopes on fragments of turquoise-encrusted mosaics, which are one of the most iconic forms of ancient Mesoamerican art. Their samples include dozens of turquoise mosaic tiles excavated from offerings within the Templo Mayor, the ceremonial and ritual center of the Aztec empire, and which is located in present-day Mexico City. They also analyzed five tiles associated with Mixteca-style objects held by the Smithsonian's National Museum of the American Indian. The analyses revealed that turquoise artifacts had isotopic signatures consistent with geology of Mesoamerica, not the Southwestern United States.
"This work revises our understanding of these relatively rare objects and provides a new perspective on the availability of turquoise, which was a highly valued luxury resource in ancient Mesoamerica," said Thibodeau. The work is the result of a decade-long collaboration between archaeologists and isotope geochemists to understand the nature of turquoise circulation and trade across southwestern North America. In earlier published research, Thibodeau showed that isotopic signatures could distinguish among turquoise deposits across the southwestern U.S. and identified the geologic sources of turquoise artifacts from archaeological sites in Arizona and New Mexico.
Thibodeau said that long-standing assumption that Mesoamerican civilizations imported turquoise from the Southwest had not been fully substantiated with evidence and that the new geochemical measurements unveil a different story. "These findings potentially re-shape our understanding of both the nature and extent of long-distance contacts between Mesoamerican and Southwestern societies, said Thibodeau. "I hope this inspires people to be skeptical of claims."
Though scholars have long assumed that Aztec and Mixtec turquoise artifacts uncovered in Mesoamerica were imported from the American Southwest, a new isotopic analysis suggests these artifacts likely derived from Mesoamerican sources. The results provide insights into the origin and circulation of turquoise across Southwestern North America. Artifacts made of turquoise - a blue-green mineral extremely valued by prehispanic societies, including the Aztecs and Mixtecs - have been uncovered in Mesoamerica, a region of the Americas that spans from central Mexico to parts of South America.
Experts have hypothesized that turquoise was brought to Mesoamerica from prehistoric mines of the Greater Southwest (present-day American southwest and northwestern Mexico), in part because no remnants of turquoise mines have been discovered in Mesoamerica and also because goods were known to be exchanged between the two cultures. Yet, some have questioned this hypothesis, particularly as geochemical data from Southwestern turquoise mines have not been fully published.
Taking advantage of the way turquoise deposits harbor distinct isotopic characteristics depending on surrounding rock, Alyson M. Thibodeau et al. analyzed the lead (Pb) and strontium (Sr) isotopic ratios in 43 Mesoamerican turquoise mosaic tiles (tesserae) from the Sacred Precinct of Tenochtitlan, most of which date to the late 15th century, as well as five tesserae associated with Mixtec turquoise mosaics. They were able to collect both Pb and Sr isotopic data for 31 samples, and out of those, 29 fall outside the distribution of ratios for turquoise deposits in the Southwest. What is more, these turquoise deposits match well with copper deposits and crustal rocks of Mesoamerica, suggesting that Mesoamerica was the source of this Aztec and Mixtec turquoise.