The COVID-19 pandemic has had far-reaching impacts in all segments of life worldwide. While a variety of surveys have assessed the impacts of the pandemic in other fields, few studies have focused on understanding the short- and long-term impacts of the pandemic for archaeology. To assess these trends, we asked survey respondents (n = 570) if they experienced job loss and to rate the percentage of change in their economic situation, workload, teaching or research activities, and personal responsibilities. Results show alarming trends, with nearly half of those who experienced job loss being under the age of 35 and women and early career archaeologists suffering major economic losses. Impacts to workload, teaching activities, and research activities were also felt across these groups. Substantial increases in personal responsibilities (childcare, eldercare, caring for sick family members) were also identified, especially for women with children under 18 years of age. While structural inequalities have already been identified across different sectors of archaeology, the results of this survey suggest the most vulnerable populations are those most heavily affected. We recommend a variety of strategies for employers, professional organizations, funding agencies, and publishers to consider in mitigating the consequences of COVID-19, especially for women and early career scholars.

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 (δ13C) and nitrogen (δ15N) isotopic analyses of human bone collagen to document the types of food people consumed, stable sulfur (δ34S) 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 δ34S for investigating Maya diet and migration through stable isotope analyses of human bone collagen (δ13C, δ15N, and δ34S) 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 δ34S values reflect local geology, our analyses also identified recent migrants to the Eastern lowlands who had non-local δ34S 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 δ34S isotope values for the Maya lowlands and provides a foundation for novel insights into both subsistence practices and migration.