Se analizan las redes de tráfico de la Quebrada de Humahuaca en tiempos del “fenómeno Isla”, evaluando críticamente el protagonismo atribuido a Tiwanaku en su organización. Con este fin se presentan las investigaciones realizadas en Muyuna —uno de los principales sitios de la época en la Quebrada— ofreciendo información novedosa sobre contextos domésticos y funerarios, economía y modo de vida. Un análisis bayesiano de todas las dataciones disponibles para el componente Isla lo ubican entre fines del siglo once y comienzos del siglo catorce dC. Estos resultados, junto con el probable origen de los bienes presentes en estos contextos, llevan a concluir que las interacciones con otras regiones de los Andes circumpuneños fueron más importantes para los procesos de diferenciación social en las comunidades Isla que las relaciones con el estado Tiwanaku. En este marco, cobran especial relevancia la relación con el Río Grande de San Juan y la gravitación de ciertos colectivos supra-regionales (pastores, consumidores de alucinógenos) que podrían introducir una dimensión heterárquica en la organización de las redes sur andinas.

This article presents stratigraphic data and radiocarbon dates combined with Bayesian modeling from San Andrés in the Zapotitán Valley, El Salvador, focusing on the Campana Structure, the largest and longest-used monumental structure at the site. These data refine the regional chronology of the valley and provide insights into the emergence, development, and abandonment of this pivotal center in southeastern Mesoamerica and its potential links to three related volcanic eruptions: Ilopango, Loma Caldera, and El Boquerón. These distinct volcanic events had pronounced effects on local people who innovated new monumental construction projects and used new volcanic debris as construction material after major eruptions. It is suggested that these monumental public building projects played an important role in the post-disaster recovery of societies by helping foster a sense of corporate identity. The use of volcanic material in constructions at San Andrés and the building of these massive structures may also have helped keep these events alive in the communal memory.

This article presents a high-resolution chronology of Wairajirca pottery in the Huánuco basin, which has been identified as a frontier region between the Andean highlands and the Amazonian rain forests: its pottery is known for having mixed features from both areas. However, the lack of fine-grained pottery and radiocarbon datasets has handicapped comparative studies’ attempts to track in detail its early development process. Our new high-resolution chronology of Wairajirca pottery is based on stratigraphic excavation data, a detailed ceramic typology, and a Bayesian analysis of the radiocarbon date from the Jancao site. The five-staged ceramic sequence from the late eighteenth to late twelfth century cal BC displays specific features of this development, including radical changes in vessel type over several centuries and connections with other pottery traditions. The earliest phase shows close relation with highlands traditions, whereas the influence of tropical rain forest patterns intensified in later phases alongside the continuation of local pottery traditions. This indicates that frontier dynamics based on fluid interactions across different ecological zones and regional sociopolitical movements played a crucial role in this long-term social process.

Since Kaminaljuyu was first systematically excavated in the 1930s, the chronology of the site has been fraught with confusion and scholarly disagreement. In recent years, scholars generally adopted the chronology presented by Shook and Popenoe de Hatch (1999) as the most authoritative account. In 2014, however, Inomata and colleagues proposed a revision of this chronology by shifting its Preclassic portion (including the Las Charcas and Providencia phases) roughly 300 years later in time. In this article, we analyze a total of 108 radiocarbon dates with Bayesian statistics, tying them to detailed ceramic analysis. These dates include previously reported dates, measured after the year 2000, as well as 68 new radiocarbon dates obtained from Kaminaljuyu and nearby sites. The results largely support Inomata and coauthors’ (2014) revised Preclassic chronology, placing the Las Charcas–Providencia transition around 350 BC and the Providencia–Verbena transition around 75 BC. In addition, we present new dates on the Early Classic period, although some ambiguity remains for the Esperanza phase, when Teotihuacan-related elements were introduced to Kaminaljuyu. The revised chronology, combined with environmental data, suggests an explosive increase in population and construction activity during the Verbena and Arenal phases.