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• Maize consumption record from the northeast Patagonia is presented. • Archaeobotanical data is discussed with the oxygen isotopes (δ18O) on human remains. • Maize-consumers were local individuals who also consumed local wild plants. • Maize would have entered through exchange, probably from southern Andes. This paper discusses the maize consumption record among hunter-gatherers outside assumed production areas in northeastern Patagonia. We evaluated if this anomalous record is the result of occasional events of local production/consumption; the transport of the microremains in the teeth of individuals after consuming maize in non-local production areas; or the local consumption of maize after its transport/exchange from production areas. Archaeobotanical results showed that analyzed individuals, including maize-consumers, mainly consumed local wild plants. Maize was not cultivated locally, and its consumption was unusual but not extraordinary in northeastern Patagonia. Oxygen isotope values of analyzed individuals are strongly compatible with local water sources, which imply that the mobility range of them must have not exceeded extra-Andean North Patagonia. For this reason, the most plausible explanation for the presence of maize in the local archaeological record is that this plant to have entered northeastern Patagonia through exchange, probably from southern Andes (central Chile or central-west Argentina). [ABSTRACT FROM AUTHOR]

• Six obsidian sources increased their use in the Late Holocene in north Patagonia. • The closer source to Diamante Valley, is the least used. • The best quality source, Las Cargas, was the most used across the Late Holocene. • Obsidian helped to minimize risk in the occupation of high elevation locations. • Obsidian exchange routes may find a pattern in least cost path analysis results. • Exchange of obsidian followed routes through High elevations villages to sources. In this paper we explore obsidian conveyance in the Diamante Valley, in northwestern Patagonia, Argentina. Obsidian is the third most-common toolstone used in the Diamante Valley after basalts and local cryptocrystallines. Obsidian artifacts are predominantly projectile points and bifaces, with few cores and early-stage reduction debris. To explain these patterns, we conducted XRF sourcing and technological analysis of 177 obsidian artifacts collected there. We also conducted a GIS-based least cost path analysis to assess the costs of conveying obsidian from sources to sites in the Diamante watershed. We found that hunter-gatherers used Las Cargas as the principal obsidian source, followed by Maule 1 and 2, El Peceño, and Coche Quemado. The nearest source, Laguna del Diamante, was the least used. These data, combined with an analysis of the ways cores, formed tools, and debitage types were conveyed and ultimately deposited at sites in the Diamante watershed, suggest a late Holocene pattern of highland-oriented indirect access, implying highland village sites likely served as nodes in a regional and extraregional exchange network focused not only on obsidian but also on other goods, information, and social obligations. [ABSTRACT FROM AUTHOR]