Abstract

Just as modern nation-states struggle to manage the cultural and economic impacts of migration, ancient civilizations dealt with similar external pressures and set policies to regulate people’s movements. In one of the earliest urban societies, the Indus Civilization, mechanisms linking city populations to hinterland groups remain enigmatic in the absence of written documents. However, isotopic data from human tooth enamel associated with Harappa Phase (2600-1900 BC) cemetery burials at Harappa (Pakistan) and Farmana (India) provide individual biogeochemical life histories of migration. Strontium and lead isotope ratios allow us to reinterpret the Indus tradition of cemetery inhumation as part of a specific and highly regulated institution of migration. Intra-individual isotopic shifts are consistent with immigration from resource-rich hinterlands during childhood. Furthermore, mortuary populations formed over hundreds of years and composed almost entirely of first-generation immigrants suggest that inhumation was the final step in a process linking certain urban Indus communities to diverse hinterland groups. Additional multi disciplinary analyses are warranted to confirm inferred patterns of Indus mobility, but the available isotopic data suggest that efforts to classify and regulate human movement in the ancient Indus region likely helped structure socioeconomic integration across an ethnically diverse landscape.

Highlights

  • Protohistoric South Asia holds unique insights into the evolution and maintenance of early urbanism, as the relatively decentralized Indus Civilization suggests an alternative to the strongly centralized states of contemporaneous Egypt and Mesopotamia [1]

  • The skeletal series from Harappa (Cemetery R-37) and Farmana are consistent with the above trends, and we suggest the inhumed participated in a shared set of mortuary practices

  • The same is true for Harappa human Pb isotope ratios [208Pb/204Pb (M = 38.814, SD = 0.257, range = 38.013–39.377), 207Pb/204Pb (M = 15.713, SD = 0.026, range = 15.650– 15.770), 206Pb/204Pb (M = 18.677, SD = 0.171, range = 18.054–19.099)] relative to those of Harappa fauna [208Pb/204Pb (M = 38.970, SD = 0.159, range = 38.580–39.189), 207Pb/204Pb (M = 15.735, SD = 0.008, range = 15.720–15.749), 206Pb/204Pb (M = 18.744, SD = 0.106, range = 18.468–18.874)]

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Summary

Methods

Teeth from the first, second, and third molar cohorts were sampled to maximize life history information for each individual. First molars were preferred for assaying early life isotopic exposure, but a single first incisor from Harappa burial H87/ 72 49h was included in the first molar cohort to maximize the dataset. Three premolars were included in the second molar cohort. Even though initial cusp formation begins at about 1 year of age for canines, a single canine was grouped with the second molar cohort for two reasons. The sampled canine was clearly associated with the first incisor from burial H87/ 72 49h, a tooth that mineralized earlier in development. All available fully mineralized teeth were sampled from collections at the Harappa Museum in Harappa, Pakistan yielding 44 teeth from a minimum number of individuals (MNI) of 38.

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