ABSTRACT
Zooarchaeological faunal remains are commonly examined to investigate harvesting behavior. We determined limpet (Patella vulgata) shell size and shape, and estimated shell age from several middens at the Late Norse Sandwick South Site, Unst, Shetland, UK, whose strata represent distinct occupational phases (Phase 1: AD 1100–1200, Phase 2: AD 1200–1250, Phase 3: AD 1250–1350). Our goal was to determine if the many limpets found there could provide insight into Norse harvesting behavior. Shell length, conicity, and modeled age all declined between Phases 1 and 2, suggesting intensive, size-selective harvesting of limpets and a shift to harvesting lower in the intertidal zone between phases. Length and conicity varied in Phases 2 and 3 and no major changes seem to have occurred over these periods, indicating that harvesting maintained the limpet population at an impacted level throughout the later phases. The conicity decline between Phases 1 and 2 may also have been caused by increased storminess that accompanied the onset of the Little Ice Age. The mean length of modern limpet populations near the Norse site did not differ from the archaeological phases, but did vary among collection years. Limpets were 26% larger in 2015 than in 2012 and 2013, indicating that large interannual variations in population structure can occur over short time periods. Potentially the result of extreme storms removing small limpets, this result raises the possibility that size and conicity changes during the Sandwick South Site occupation, as well as in other early populations, could also be the result of environmental factors rather than human harvesting alone. We feel, however, that the most parsimonious explanation for the patterns we document is human harvesting.
ACKNOWLEDGEMENTS
We thank Will Ash for advice on determining measurement error in photographs. We thank Patricia Miller for preparation of maps and site diagrams. We also thank the three anonymous reviewers whose comments substantially improved the quality of this manuscript. WGA is now an employee of the US National Science Foundation; however, any opinions, findings, conclusions, or recommendations expressed in this article are those of WGA, and his co-authors, and do not reflect the views of the US National Science Foundation.
FUNDING
This project was funded by the US National Science Foundation, Office of Polar Programs, Arctic Social Sciences Program (gront no. PLR-1026911); the Bates College Biology Department; the student research fund of Bates College; the Bates College Harward Center for Community Partnerships and the Bates College Imaging Center. Primary funding for the Sandwick South Site excavations was provided by Historic Environment Scotland.
SUPPLEMENTAL
Supplemental materials are available for this article at https://doi.org/10.1080/15564894.2017.1368743.