Abstract

Zooarchaeological analysis of a substantial assemblage of animal bones excavated from Dudley Castle, West Midlands, revealed two significant changes in cattle management in the late medieval and post-medieval periods: a statistically significant increase in size in the later 14th century; and a gradual reduction in slaughter age. To explore whether these altered husbandry practices were accompanied by modifications to the diet and environment of these animals, a targeted study of carbon and nitrogen stable isotope values from 135 cattle bones was conducted. This analysis revealed that δ13C and δ15N values were broadly consistent between the mid-13th and mid-18th centuries. Only two statistically significant diachronic variations were identified: a temporary decrease in δ13C values in phase 7 (1397–1533); and lower variation in δ13C values in phase 9 (1647–1750). A number of explanations for these changes are offered. While the zooarchaeologically attested shifts in cattle husbandry were not accompanied by isotopically detectable changes to diet and environment, the analysis of stable isotopes highlighted other changes that were not detected using traditional zooarchaeological analysis. The complimentary benefits of zooarchaeological and isotopic approaches are extolled.

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