Published in

Cambridge University Press, Antiquaries Journal, (98), p. 187-218, 2018

DOI: 10.1017/s0003581517000324

Links

Tools

Export citation

Search in Google Scholar

The ORIGINS OF TRADESCANT’S ‘INDIA OCCIDENTALI’ WOODEN CLUBS:<sup>14</sup>C DATING, MATERIAL IDENTIFICATION AND STRONTIUM ISOTOPE STUDIES

This paper was not found in any repository, but could be made available legally by the author.
This paper was not found in any repository, but could be made available legally by the author.

Full text: Unavailable

Green circle
Preprint: archiving allowed
Red circle
Postprint: archiving forbidden
Red circle
Published version: archiving forbidden
Data provided by SHERPA/RoMEO

Abstract

This paper focuses on the material study (radiocarbon dating, wood identification and strontium isotope analyses) of four large ‘India occidentali’ clubs, part of the founding collections of the Ashmolean Museum, in Oxford, and originally part of John Tradescant’s ‘Ark’, in Lambeth (1656). During the seventeenth century, the term ‘India occidentali/occidentales’ referred not only to the ‘West Indies’ (its literal translation), but to the Americas as a whole; hence, the Ashmolean clubs and, indeed, thecforty examples of similarly large, decorated clubs known in international museum collections had no firm provenance and lacked even the most basic information. Previous attempts at attribution, based on stylistic comparisons with nineteenth- to twentieth-century Brazilian and Guyanese clubs, have proved inconclusive given the unique features of this club style, raising the intriguing possibility that these may be exceptionally rare examples of ‘Island Carib’ (Kalinago) material culture, particularly as images of such clubs appear in seventeenth-century ethnographic accounts from the Lesser Antilles. This paper provides new data for these poorly known objects from early collections, revealing not only the type of wood from which they were carved (Platymisciumsp. andBrosimumcfguianense) and their probable dates of manufacture (c AD1300–1640), but also their possible provenance (strontium results are consistent with a possible range from Trinidad south to French Guiana).