Abstract

Archaeological excavations at Guishan in the southern end of Taiwan have recovered more than a hundred glass beads dating to mid-1st millennium CE. This research investigates the exchange of glass beads between Guishan, eastern Taiwan and Southeast Asia, by analysing the styles, chemical composition and microstructure of 64 glass beads from Guishan, using SEM-EDS, EPMA and LA-ICP-MS. The findings suggest that beads with an m-Na-Al glass and v-Na-Ca composition are the most common, supporting evidence for bead exchange between Guishan and Southeast Asia, originated in South Asia and Western Asia. Furthermore, most m-Na-Al glasses were coloured by copper, and different types of copper-based additives may have been used for different colours, indicating the beads may be derived from multiple production centres or workshops via Southeast Asia. Conversely, the glass bead compositions suggest that glass bead exchange between other contemporary sites in Taiwan is less evident at Guishan, except for one type of yellow glass bead containing bone ash which is different. This bone-ash containing yellow glass at Guishan is firstly identified in Iron Age Taiwan as well as around the South China Sea region. Its counterparts are also found from archaeological sites in southeastern and coastal eastern Taiwan, which might indicate small scale glass bead exchange. This evidence together suggests a dynamic glass bead exchange network between Guishan, eastern Taiwan, Southeast Asia and beyond.

Highlights

  • IntroductionRecent research on bead styles, colours and chemical composition has started to show complex intra-, inter- and cross-regional exchange of glass beads within Taiwan and between regions overseas (Wang and Jackson, forthcoming)

  • A general picture is that the chemical composition of high alumina (m-Na-Al) or plant ash glass (v-Na-Ca) beads shows a mainly drawn technique which suggests a Southeast Asian connection of bead exchange in the 1st millennium, while a transition to a Chinese origin for beads in Taiwan can be seen in the 2nd millennium due to the presence of high lead glass and wound glass beads (Wang, 2018)

  • As there is no evidence of South Asian contact in Iron Age Taiwan (Wang and Jackson 2014), the dominance of m-Na-Al 1 sub-group confirms the participation of Guishan in the bead exchange network around the South China Sea in the 3rd to 9th centuries

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Summary

Introduction

Recent research on bead styles, colours and chemical composition has started to show complex intra-, inter- and cross-regional exchange of glass beads within Taiwan and between regions overseas (Wang and Jackson, forthcoming). In the 1st millennium CE, the Southeast Asian connection further indicates the participation of Taiwan into the cross-regional South China Sea exchange network where there may be circulation of glass objects, raw materials and/or craft knowledge from South Asia and Western Asia. Within Taiwan, recent analysis by Wang and Jackson (forthcoming) started to show a regional distribution of bead colours and styles in the early Iron Age, which is further interpreted as the presence of a regional exchange network along north and

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