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The organization of ceramic production and distribution among the ancient Hohokam of the Phoenix basin, Arizona, has been documented in recent years with much detail. Based on diverse temper and clay compositions, the provenance of individual ceramics is routinely determined with considerable precision. One exception is phyllite-tempered pottery, which was made in one corner of the basin but also across a broad upland zone adjacent to the north. The phyllite-tempered pottery from different production sources cannot be distinguished on the basis of their temper type. As shown with assays with an electron microprobe, however, both the temper and clay fractions are chemically diverse and geographically distinct, allowing many of the phyllite-tempered wares to be sourced. Among the phyllite-tempered ceramics consumed in the Phoenix basin, some are shown to have been made locally, but, surprisingly, large numbers were imported from the northern uplands. Their numbers support the idea that the connection between the Phoenix basin and the northern uplands was a prominent component of the Hohokam regional economy despite the great difference between them in settlement size and density. 相似文献
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David R. Abbott Sophia E. KellyAndrew D. Lack Margaret E. Beck 《Journal of archaeological science》2012,39(4):984-993
Mobile Patayan foragers of the interior desert of southwestern Arizona were makers of Lower Colorado Buff Ware ceramics. These containers were sometimes traded to Hohokam irrigation agriculturalists at the western margin of the Hohokam territory. By A.D. 1100, the distribution of Patayan Buff Wares shifted to the east, penetrating the Hohokam heartland. Some theorists have suggested the ceramic distribution implies a migration of Patayan people, who joined agricultural communities in the Hohokam core area. One way to assess this idea is to identify the production of Patayan material culture within the Hohokam territory. We test for the local manufacture of Lower Colorado Buff Ware at the Hohokam village of Las Colinas, where Patayan pottery was found in abundance, and a Patayan enclave has been inferred. Using petrographic analysis and SEM-EDS assays of the phyllite temper fragments in the Patayan wares, we conclude that the Patayan pottery was made elsewhere and was not fabricated with local materials at Las Colinas. 相似文献
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