Joyce et al. (2006)

Ceramic Production and Exchange in Late/Terminal Formative Period Oaxaca

A. Joyce, H. Neff, M. S. Thieme, M. Winter, J. M. Elam, and A. Workinger (2006) Latin American Antiquity, 17 (In press)

Abstract

Patterns of Late/Terminal Formative Period (ca. 500 B.C.-A.D. 300) ceramic exchange in Oaxaca are examined through Instrumental Neutron Activation Analysis (INAA). Samples of 453 Late/Terminal Formative Period sherds were submitted to the Missouri University Research Reactor (MURR) for INAA to determine elemental composition. The sherds came from 20 excavated sites and 2 surveys in the following regions: Valley of Oaxaca, Mixteca Alta, Mixteca Baja, lower Río Verde Valley, and Cuicatlán Cañada. Selected for the study were vessel fragments from three recognized paste categories: grayware (gris), fine brownware (café fino), and creamware (crema). We also sampled clays and sherds from known sources in four modern pottery-making towns in the Oaxaca Valley. The research adds to the INAA database for Oaxaca by identifying the chemical signatures of six source groupings that we can link to specific regions and, in two cases, to particular source zones within regions. The evidence from chemical composition and typology indicates a long-term tradition of ceramic production in both the Atzompa and Coyotepec source zones, making a strong case for continuity between prehispanic and modern times. The data show that the exchange of ceramics in Late/Terminal Formative Oaxaca was multidirectional, with ceramics imported both to and from the Oaxaca Valley.

Number of samples in dataset: 682

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Recent research reported by the Archaeometry Lab at MURR after June 2005 is based on support by the National Science Foundation under our current grant number 0504015.
Earlier research was supported by several NSF grants, including the following numbers: 8801707, 9102016, 9503035, 9802366, 9977237, 0102325, and 0405042.  Any opinions, findings and conclusions or recommendations expressed in this material are those of the author and do not necessarily reflect the views of the National Science Foundation.

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