This research seeks to understand the economic and social interaction patterns among dispersed Piedmont Village Tradition communities in the North American Southeast, AD 1200–1600. Piedmont Village Tradition communities lived adjacent to Mississippian societies and have been categorized as a peripheral society because of this spatial relationship. We examine economic behaviors by constructing fall-off curves of local versus nonlocal lithic material proportions at settlement sites and examining the reduction behaviors and tool types at sites. The results support a possible gateway model for the acquisition and distribution of nonlocal materials that linked spatially proximate communities. To examine social interaction patterns, we conducted a Brainerd-Robinson analysis of ceramic attributes from six sites and combined our results with work by Rogers (1993). The results show sites with stylistic similarities are not the same sites that share lithic resources. We conclude that these spatially non-overlapping artifact patterns result from a heterarchical social organization with a high degree of independence between economic and social interactions. Finally, we contextualize our results within the current knowledge of Mississippian and Piedmont Village Tradition societies in the region to broaden the discussion of gateways in reciprocity-based economies, societies traditionally thought of as peripheral to complex societies, and coalescence.

Knowledge about vegetation dynamics during the last glacial and deglacial periods in southeastern North America is under-constrained owing to low site density and problematic chronologies. New pollen records from two classic sites, Anderson Pond, TN, and Jackson Pond, KY, supported by AMS 14C age models, span 25.2–13.7 ka and 31.0–15.4 ka, respectively. A transition from Pinus dominance to Picea dominance is recorded at Jackson Pond ca. 26.2 ka, ~ coincident with Heinrich Event H2. Anderson and Jackson Ponds record a transition from conifer to deciduous-tree dominance ~ 15.9 and 15.4 ka, respectively, marking the development of no-analog vegetation characterized by moderate to high abundances of Picea, Quercus, Carya, Ulmus, Fraxinus, Ostrya/Carpinus, Cyperaceae, and Poaceae, and preceding by ~ 2000 yr the advent of similar no-analog vegetation in glaciated terrain to the north. No-analog vegetation developed as a time-transgressive, south-to-north pattern, mediated by climatic warming. Sporormiella abundances are consistently low throughout the Jackson and Anderson Pond records, suggesting that megafaunal abundances and effects on vegetation varied regionally or possibly that the Sporormiella signal was not well-expressed at these sites. Additional records with well-constrained chronologies are necessary to assess patterns and mechanisms of vegetation dynamics during the last glacial and deglacial periods.