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Defining the provenance of red slipped pottery from Texas and Oklahoma by petrographic methods
Institution:1. Department of Agronomy, State University of Maringá, Avenida Colombo, 5790 Maringá, Paraná, Brazil;2. Centre for Environmental Magnetism & Palaeomagnetism, Lancaster Environment Centre, University of Lancaster, LA1 4YQ, United Kingdom;3. Department of Rural Engineering, Federal University of Santa Catarina, Rua Admar Gonzaga, 1346 Florianópolis, Santa Catarina, Brazil;1. Institute of Archaeology, Jagiellonian University, Gołebia 11, 31-007 Krakow, Poland;2. Fitch Laboratory, British School at Athens, Souedias 52, 10676 Athens, Greece;3. Institute of Nanoscience and Nanotechnology N.C.S.R. ‘Demokritos’, 15310 Aghia Paraskevi, Greece;1. Fitch Laboratory, British School at Athens, 52 Souedias Street, 10676, Greece;2. UCL Qatar, Hamad bin Khalifa University, Doha, Qatar;3. CNRS Lyon, Archéorient (UMR 5133), France;4. Swiss School of Archaeology in Greece, Greece/Switzerland;5. University of Basel, Switzerland
Abstract:Ceramics are among the most important artifacts that archaeologists use to reconstruct patterns of prehistoric trade and exchange. Petrographic analysis of ceramic thin-sections, in addition to providing detailed technological data, enables the identification of sand-tempering agents. These raw materials are potentially important evidence for ceramic provenance, assuming that such common materials themselves would not have been traded. Here we apply methods developed by sedimentary petrographers to the problem of determining the provenance of Red Slipped sherds from late Prehistoric (c. AD 1000–1400) sites in the Caddoan area and contemporaneous Plains Village sites. Modal frequencies of different kinds of quartz, feldspars and lithic grains are used to construct several triangular graphs that reveal compositional patterns indicative of provenance. Sherds from the Plains Village sites exhibit higher frequencies of lithic grains, feldspars and polycrystalline quartz relative to the sherds from sites in eastern Texas and eastern Oklahoma. While anomalous sherds were identified, the longstanding assumption that Red Slipped sherds in Plains Village contexts were traded from the Caddoan area is not supported by these data. These methods have strong application potentials for other, geologically diverse portions of North America.
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