Abstract

Mound Key was once the capital of the Calusa Kingdom, a large Pre-Hispanic polity that controlled much of southern Florida. Mound Key, like other archaeological sites along the southwest Gulf Coast, is a large expanse of shell and other anthropogenic sediments. The challenges that these sites pose are largely due to the size and areal extent of the deposits, some of which begin up to a meter below and exceed nine meters above modern sea levels. Additionally, the complex depositional sequences at these sites present difficulties in determining their chronology. Here, we examine the development of Mound Key as an anthropogenic island through systematic coring of the deposits, excavations, and intensive radiocarbon dating. The resulting data, which include the reversals of radiocarbon dates from cores and dates from mound-top features, lend insight into the temporality of site formation. We use these insights to discuss the nature and scale of human activities that worked to form this large island in the context of its dynamic, environmental setting. We present the case that deposits within Mound Key’s central area accumulated through complex processes that represent a diversity of human action including midden accumulation and the redeposition of older sediments as mound fill.

Highlights

  • MethodsWe employed three different methods to gather data that could be used to evaluate the structure, dynamics, and chronology of Mound Key

  • Shell middens and mounds are complex landscape features that present a number of problems for archaeologists who wish to understand their formation

  • S1 Table contains all the corrected and calibrated dates for Mound Key listed by lab and sample identification number

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Summary

Methods

We employed three different methods to gather data that could be used to evaluate the structure, dynamics, and chronology of Mound Key. To extract sediment cores we used a JMC Environmentalist’s Sub-Soil probe. This is a manual slide hammer operation corer. We made every effort to minimize fall into the core hole once we extracted a section; some fall was unavoidable. This slump, is identified as the top most strata of the core sections. We trimmed core tubes flush to the sediment surface while in the field to avoid disturbance of the strata during transport

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