Abstract
Focusing on the southeastern United States, I provide some alternative perspectives on shell mounds previously interpreted as architectural features, temple mounds, and feasting sites. The same pattern of deposition often inferred to indicate mound construction—darker-colored, highly organic strata alternating with lighter-colored, shell-rich strata—can be accounted for by domestic midden accumulation and disposal of refuse away from living areas. Observed abundances of particular shell species can result from local or regional ecological conditions. Site complexes interpreted as architectural may have evolved largely in response to short-term climate changes. Shell rings on the Georgia and South Carolina coasts probably functioned to conserve and store unconfined water. To understand ancient shell mounds, we need a sediment-oriented approach to the study of mound deposits and more attention to the environmental contexts in which shell mounds accumulated.
Published Version
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