Isotopic Evidence for the Provenance of Turquoise, Mineral Paints, and Metals in the Southwestern United States

Lead and strontium isotopes are two powerful tracers that can be used to identify or constrain the provenance of a wide range of archaeological materials, but these two isotopic tracers have been rarely employed to infer the sources of artifacts in the southwestern USA. This dissertation contains fo...

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Main Author: Thibodeau, Alyson Marie
Other Authors: Ruiz, Joaquin
Language:en
Published: The University of Arizona. 2012
Subjects:
Online Access:http://hdl.handle.net/10150/243111
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spelling ndltd-arizona.edu-oai-arizona.openrepository.com-10150-2431112015-10-23T04:56:50Z Isotopic Evidence for the Provenance of Turquoise, Mineral Paints, and Metals in the Southwestern United States Thibodeau, Alyson Marie Ruiz, Joaquin Killick, David J. Chesley, John T. Quade, Jay Reiners, Peter Ruiz, Joaquin lead isotopes Southwestern U.S.A. strontium isotopes turquoise Geosciences Coronado glaze paints Lead and strontium isotopes are two powerful tracers that can be used to identify or constrain the provenance of a wide range of archaeological materials, but these two isotopic tracers have been rarely employed to infer the sources of artifacts in the southwestern USA. This dissertation contains four studies that demonstrate how these isotopic systems can address questions about the sources of three types of archaeological materials found in this region: turquoise, lead-based glaze-paints, and metals. The analysis of 116 samples of turquoise from 17 deposits in the southwestern USA reveals that lead and strontium isotopes are robust and sensitive tracers of turquoise at multiple scales. Isotopic variation among turquoise deposits correlates with broad regional differences in the geologic and tectonic setting of the rocks and mineral deposits which host turquoise mineralization. Many turquoise deposits also have unique isotopic signatures that will enable insights into ancient patterns of turquoise acquisition at regional and local levels. To show the utility of these tracers when applied to archaeological turquoise, I use lead and strontium isotopic measurements to establish that the Silver Bell Mountains are the likely source turquoise found at the Redtail site in the Tucson Basin, Arizona, USA. This dissertation also contains new, high-precision isotopic ratios of lead ores (galena and cerrusite) from four mining districts in New Mexico, including the Cerrillos Hills. All districts studied are possible sources of lead used by Pueblo IV communities to produce glaze paints. These new measurements, made by multiple-collector ICP-MS, define the isotopic composition of the ore deposits with greater precision and accuracy than achieved in previous studies, indicating an opportunity to improve interpretations about the provenance of lead in glaze paints. Lead isotopes are also found to be useful tools for identifying lead and copper metal associated with the 1540-1542 Vázquez de Coronado expedition. Lead shot and copper crossbow boltheads from two sites with archaeological evidence for the expedition's presence were determined to share similar or identical lead isotopic ratios. I propose this specific isotopic "fingerprint" can be used to identify other artifacts belonging to the expedition in the Southwest. 2012 text Electronic Dissertation http://hdl.handle.net/10150/243111 en Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. The University of Arizona.
collection NDLTD
language en
sources NDLTD
topic lead isotopes
Southwestern U.S.A.
strontium isotopes
turquoise
Geosciences
Coronado
glaze paints
spellingShingle lead isotopes
Southwestern U.S.A.
strontium isotopes
turquoise
Geosciences
Coronado
glaze paints
Thibodeau, Alyson Marie
Isotopic Evidence for the Provenance of Turquoise, Mineral Paints, and Metals in the Southwestern United States
description Lead and strontium isotopes are two powerful tracers that can be used to identify or constrain the provenance of a wide range of archaeological materials, but these two isotopic tracers have been rarely employed to infer the sources of artifacts in the southwestern USA. This dissertation contains four studies that demonstrate how these isotopic systems can address questions about the sources of three types of archaeological materials found in this region: turquoise, lead-based glaze-paints, and metals. The analysis of 116 samples of turquoise from 17 deposits in the southwestern USA reveals that lead and strontium isotopes are robust and sensitive tracers of turquoise at multiple scales. Isotopic variation among turquoise deposits correlates with broad regional differences in the geologic and tectonic setting of the rocks and mineral deposits which host turquoise mineralization. Many turquoise deposits also have unique isotopic signatures that will enable insights into ancient patterns of turquoise acquisition at regional and local levels. To show the utility of these tracers when applied to archaeological turquoise, I use lead and strontium isotopic measurements to establish that the Silver Bell Mountains are the likely source turquoise found at the Redtail site in the Tucson Basin, Arizona, USA. This dissertation also contains new, high-precision isotopic ratios of lead ores (galena and cerrusite) from four mining districts in New Mexico, including the Cerrillos Hills. All districts studied are possible sources of lead used by Pueblo IV communities to produce glaze paints. These new measurements, made by multiple-collector ICP-MS, define the isotopic composition of the ore deposits with greater precision and accuracy than achieved in previous studies, indicating an opportunity to improve interpretations about the provenance of lead in glaze paints. Lead isotopes are also found to be useful tools for identifying lead and copper metal associated with the 1540-1542 Vázquez de Coronado expedition. Lead shot and copper crossbow boltheads from two sites with archaeological evidence for the expedition's presence were determined to share similar or identical lead isotopic ratios. I propose this specific isotopic "fingerprint" can be used to identify other artifacts belonging to the expedition in the Southwest.
author2 Ruiz, Joaquin
author_facet Ruiz, Joaquin
Thibodeau, Alyson Marie
author Thibodeau, Alyson Marie
author_sort Thibodeau, Alyson Marie
title Isotopic Evidence for the Provenance of Turquoise, Mineral Paints, and Metals in the Southwestern United States
title_short Isotopic Evidence for the Provenance of Turquoise, Mineral Paints, and Metals in the Southwestern United States
title_full Isotopic Evidence for the Provenance of Turquoise, Mineral Paints, and Metals in the Southwestern United States
title_fullStr Isotopic Evidence for the Provenance of Turquoise, Mineral Paints, and Metals in the Southwestern United States
title_full_unstemmed Isotopic Evidence for the Provenance of Turquoise, Mineral Paints, and Metals in the Southwestern United States
title_sort isotopic evidence for the provenance of turquoise, mineral paints, and metals in the southwestern united states
publisher The University of Arizona.
publishDate 2012
url http://hdl.handle.net/10150/243111
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