Monks on the move: Evaluating pilgrimage to Byzantine St. Stephen's monastery using strontium isotopes.

OBJECTIVES: Written and archaeological evidence indicates that migration, in the form of pilgrimage to Byzantine Palestine, was a major social phenomenon between the 5th and 7th centuries CE. Monasteries saw record growth at this time as pilgrims chose to stay in the region and take up religious life. A major influx of people to the region, with a corresponding growth in monastic vocations that led travelers to stay in the area, is not in question; however, the distant origins of pilgrims reflected in surviving texts may be an artifact of preservation, biased towards an elite minority. The Byzantine monastery of St. Stephen's provides an opportunity to study this question from a bioarchaeological perspective, given the excellent preservation of the human skeletal assemblage, a wealth of written works about the community as well as daily life in Byzantine Palestine, and a rich archaeological record for the site and region. MATERIALS AND METHODS: An analysis of radiogenic strontium isotope values from the third molars of 22 individuals recovered from the St. Stephen's crypt complex was conducted to test whether those interred at the monastery were of local origin. RESULTS: Of those examined ( x¯= 0.7084 ± 0.0007, 1σ), 8 out of 22 (36%) exhibited (87) Sr/(86) Sr ratios that fell outside of local ranges. DISCUSSION: These results confirmed the sizeable presence of nonlocals at St. Stephen's Monastery. While most of these migrants likely traveled to Jerusalem from different areas of the Levant as pilgrims, others may have hailed from further afield, including Europe.

Paleomobility in the Tiwanaku diaspora: biogeochemical analyses at Rio Muerto, Moquegua, Peru.

Paleomobility has been a key element in the study of the expansion of ancient states and empires, including the Tiwanaku polity of the South Central Andes (AD 500-1000). We present radiogenic strontium and oxygen isotope data from human burials from three cemeteries in the Tiwanaku-affiliated Middle Horizon archaeological site complex of Rio Muerto in the Moquegua Valley of southern Peru. At Rio Muerto, archaeological human enamel and bone values range from (87) Sr/(86) Sr = 0.70657-0.72018, with a mean of (87) Sr/(86) Sr = 0.70804 ± 0.00207 (1σ, n = 55). For the subset of samples analyzed for oxygen isotope values (n = 48), the data ranges from δ(18) Ocarbonate(VSMOW) = +18.1 to +27.0‰. When contextualized with other lines of archaeological evidence, we interpret these data as evidence for an archaeological population in which the majority of individuals had "local" origins, and were likely second-generation, or more, immigrants from the Tiwanaku heartland in the altiplano. Based on detailed life history data, we argue a smaller number of individuals came at different ages from various regions within the Tiwanaku polity. We consider whether these individuals with isotopic values consistent with "nonlocal" geographic origins could represent first-generation migrants, marriage exchange partners, or occupationally mobile herders, traders or other travelers. By combining isotopic life history studies with mortuary treatment data, we use a person-centered migration history approach to state integration and expansion. Isotopic analyses of paleomobility at the Rio Muerto site complex contribute to the role of diversity in ancient states by demonstrating the range of geographic origins rather than simply colonists from the Lake Titicaca Basin.