Sulfur isotopes as a proxy for human diet and mobility from the preclassic through colonial periods in the Eastern Maya lowlands

Maya archaeologists have long been interested in understanding ancient diets because they provide information about broad-scale economic and societal transformations. Though paleodietary studies have primarily relied on stable carbon (δ(13)C) and nitrogen (δ(15)N) isotopic analyses of human bone collagen to document the types of food people consumed, stable sulfur (δ(34)S) isotope analysis can potentially provide valuable data to identify terrestrial, freshwater, or marine/coastal food sources, as well as determine human mobility and migration patterns. Here we assess applications of δ(34)S for investigating Maya diet and migration through stable isotope analyses of human bone collagen (δ(13)C, δ(15)N, and δ(34)S) from 114 individuals from 12 sites in the Eastern Maya lowlands, temporally spanning from the Late Preclassic (300 BCE—300 CE) through Colonial periods (1520–1800 CE). Results document a diet dominated by maize and other terrestrial resources, consistent with expectations for this inland region. Because δ(34)S values reflect local geology, our analyses also identified recent migrants to the Eastern lowlands who had non-local δ(34)S signatures. When combined with other indicators of mobility (e.g., strontium isotopes), sulfur isotopic data provide a powerful tool to investigate movement across a person’s lifespan. This study represents the largest examination of archaeological human δ(34)S isotope values for the Maya lowlands and provides a foundation for novel insights into both subsistence practices and migration.