Beads

): Define beads as a subject, their regional prevalence across the Malay Peninsula and Borneo, and their economic, cultural, or archaeological significance.

2. Thematic Body (2-4 subheadings using ###):

   • ### The Indo-Pacific Beadmaking Industry - covering the Lada process, migration of the industry, Arikamedu League, and the shift to Chinese coil beads
   • ### The "Roman Bead" Debate - covering the Gardner-Beck claim, Lamb’s and Francis’s challenges, ceramic dating arguments
   • ### Stone, Shell, and Other Bead Types - covering the cornelian bead from Pahang, shell beads from North Borneo, mutisalah beads, and other types
   • ### Trade, Exchange, and Cultural Significance - covering the Dusun trade economy, pricing, and mythological associations

3. Research and Documentation - assessing how the Society’s literature investigated this topic over time.

Let me check the word count target: approximately 1600 words. I need to be thorough but proportional.

Let me draft this carefully, ensuring:

• British English throughout
• Oxford comma
• Italicised foreign terms with explanation on first appearance
• No archaic ethnonyms
• Citations [N] or [N, pp. X–Y]
• No H1, no ”## References” or ”## MBRAS Sources”
• Use ### for thematic subheadings (wait, the instructions say “Use ’## ’ for all thematic body subheadings” but also say “Organize into 2 to 4 substantive ’###’ subheadings”. Let me re-read…

The NARRATIVE ARCHITECTURE says: “Organize into 2 to 4 substantive ’###’ subheadings” The FORMATTING & HEADING RULES says: “Use ’## ’ for all thematic body subheadings.”

These contradict. The FORMATTING rule is more specific and comes later, so I’ll use ## for the thematic body subheadings. Wait, actually re-reading: “Use ’## ’ for all thematic body subheadings.” and “Conclude with ’## Research and Documentation’.” So all subheadings including the thematic ones should be ##. But the narrative architecture says ###. I’ll go with ## since the formatting rules are explicit and the narrative architecture is a general guide.

Actually, let me re-read more carefully. The narrative architecture says “Organize into 2 to 4 substantive ’###’ subheadings (e.g., ### Scope & Historical Definition…)”. The formatting rules say “Use ’## ’ for all thematic body subheadings.” I think the formatting rules override, so I’ll use ##.

Let me now write the article, keeping it around 1600 words.

Let me count as I go and aim for approximately 1600 words.

Draft:

Beads constitute one of the most abundant and archaeologically informative categories of material culture in the Malay Peninsula and Borneo, occurring across the full range of site types from megalithic cist burials to coastal trading settlements and upland domestic contexts [1, p. 87]. Their significance extends well beyond ornament: they functioned as currency in indigenous exchange economies, as markers of social and cosmological identity, and as diagnostic artefacts for reconstructing ancient maritime trade networks spanning the Indian Ocean and China Seas [2, p. 169], [1, pp. 87–88]. The bead record in the region encompasses glass, stone, shell, and metal types manufactured locally or imported from South India, the Mediterranean, China, and Southeast Asia itself, and its interpretation has been the subject of sustained scholarly debate since the 1930s [3, pp. 97–99], [4, pp. 88–98].

The Indo-Pacific Beadmaking Industry

The most consequential reframe of the regional bead record came with Peter Francis Jr.’s 1991 reassessment, which demonstrated that the Malay Peninsula was not a passive recipient of foreign trade goods but a major production centre for the ubiquitous Indo-Pacific drawn glass bead [3, p. 97]. Francis identified the Lada process—a tube-drawing technique still practised at Papanaidupet in Andhra Pradesh, southern India—as the manufacturing method behind this bead type. The process involves rolling molten glass on a long iron tube (lada), piercing it with a chetleak rod, and hand-pulling the tube over approximately three hours; its diagnostic wasters—gedda paru flakes, twisted tubes, flares, and collapsed tubes—match those found at Arikamedu exactly, with the sole exception that the Arikamedu master used a pincher-like tool rather than an iron hook [3, pp. 99–100].

By matching these diagnostic wasters between Papanaidupet, Arikamedu, and Southeast Asian sites, Francis traced the industry’s migration across the region: from Arikamedu (c. 250 B.C.–A.D. 250) to Klong Thom in Thailand and Oc-eo in Vietnam in the early centuries, then to Kuala Selinsing and Sating Pra in the seventh to tenth centuries, and finally to Takua Pa and Sungai Mas in the ninth to thirteenth centuries [3, pp. 101–103]. All four early sites shared Roman emporia, strong South Indian (Pallava/Tamil) associations, and cross-site exchange of beads and stone beadmaking, leading Francis to propose a loose trading federation—the “Arikamedu League”—that may have provided the germinal idea for Srivijaya [3, pp. 101–103].

Glass composition analyses of 21 early Indo-Pacific beads from Arikamedu, Oc-eo, and Klong Thom, and 29 medieval beads from India, Thailand, Malaysia, Sarawak, and Flores, confirm that these beads were made from locally produced glass rather than recycled Western material [3, p. 106]. The industry’s terminal date in Southeast Asia is corroborated by Philippine data: Indo-Pacific beads constitute 61.5 per cent of Developed Metal Age assemblages but only 1.1 per cent in the period corresponding to the Southern Song dynasty (from A.D. 1127), pointing to a disappearance around 1200 [3, p. 104]. After c. 1000, direct imports from the Muslim world—segmented beads, fused mosaic cane beads, and folded beads—began arriving in large quantities at Kedah and Sungai Mas, and by the thirteenth century Chinese coil beads had replaced Indo-Pacific beads across the region [3, pp. 106]. The 1988–89 Fort Canning Hill excavations in Singapore uncovered a fourteenth-century Chinese coil bead workshop with a small fire, glass sherds, melted pieces, and finished beads, confirming local manufacture of the replacement type [3, p. 111].

The “Roman Bead” Debate

The interpretation of glass beads from the Johore River sites—Johore Lama and Kota Tinggi—has been the most contested question in Malayan bead archaeology. In 1937, G. B. Gardner published a claim that Roman glass beads found at these sites evidenced direct Roman-Malay trade, a position supported by the bead specialist Horace Beck, whose 1936 report catalogued 59 numbered items from Gardner’s collection of approximately 600 beads and 800 gem stones with specific gravity measurements and comparative identifications [4, pp. 88–97]. This claim fed into the broader Ptolemaic “Golden Khersonese” debate and dominated Malayan archaeology for decades [1, p. 119].

Alastair Lamb mounted the first systematic challenge in 1964 and 1965. Applying a strict contextual dating argument, he demonstrated that the ceramic assemblage at Kota Tinggi—Chinese porcelain sherds and stamped earthenware—cannot be dated before the fifteenth century, thereby constraining the terminus post quem for all beads in situ [4, p. 97], [1, p. 119]. The Makam Sultan site, on ceramic evidence, was first occupied no earlier than the late fourteenth century, meaning all beads found there must post-date that horizon regardless of their date of manufacture [4, p. 97]. Lamb further showed that the “Roman” types in question—zone beads and chevrons—were still being manufactured in Amsterdam in the seventeenth century, and that genuine Roman beads could have been collected second-hand from old necklaces or excavated sites in the Levant before export eastwards [1, p. 119]. The same zone bead, he argued, is a “late Sung or Yuan period Roman bead” at Pengkalan Bujang, a “Ming period Roman bead” at Kota Tinggi, and merely “modern” on the neck of a living Iban girl [1, p. 119].

Francis’s 1991 reassessment delivered the definitive correction. Re-examining Beck’s original identifications, he showed that of the 59 beads, only eight were tentatively assigned to Roman or Mediterranean origin, and even those are problematic: some are Bohemian, one is a steatite bead misidentified as Hittite, and the famous “Roman” chevron bead is now known not to have been produced before c. 1480 [3, pp. 98–99]. The weight of evidence supports C. A. Gibson Hill’s earlier scepticism that the presence of a few early beads does not make the site ancient [3, pp. 98–99].

Stone, Shell, and Other Bead Types

Beyond the glass bead record, the region’s bead assemblages include stone, shell, and metal types of considerable antiquity and cultural significance. I. H. N. Evans documented a large hexagonal-section spindle bead of veined and striped cornelian, measuring 7.1 cm in length, discovered by R. M. A. Maycock on a hillside at Jerantut Estate, Pahang [5, p. 146]. The bead was imbedded in soil on a steep slope, approximately one foot nine inches below the surface, and represented a type apparently unknown in the Malay Peninsula prior to this find [5, p. 146]. While ancient cornelian beads are well attested from Kuala Selinsing in Perak, the hexagonal-section spindle form differs from the rectangular-section faceted beads previously recorded there [5, p. 146]. Evans was cautious about dating the specimen, noting that no faceted stone beads have been definitively assigned to the Iron Age in the Peninsula—the only three such specimens from that period are spherical—and observed that the bead was likely bored from both ends, consistent with a technique still in use in India, and that the cornelian is of foreign origin, possibly Indian or Arabian [5, p. 147].

In North Borneo, Evans documented a class of ancient shell beads found in the Tempasuk (Kota Belud) district among the Dusun people, drawing on nearly four decades of observation from his first visits in 1910–1911 [2, p. 168]. These beads—small, short cylinders of molluscan shell, approximately 5 mm in diameter, highly polished from long use, and sometimes stained with indigo dye from native-woven Dusun cloths—were confirmed as molluscan through microscopic examination of a sectioned bead at the Sedgwick Museum of Geology, Cambridge [2, p. 170]. They were bored from either side, leaving holes expanded at the entrances, and were not found among the Bajau or Illanun coastal populations, who were comparatively recent arrivals, suggesting a deeper indigenous association with the upland Dusun [2, p. 168].

The mutisalah, an opaque dark red glass bead found in every part of the region, constitutes a further important type. Lamb traced its probable origin to South Indian megalithic and trading sites, documented its manufacture at Arikamedu, and argued that the industry died out in the sixteenth century under competition from European and Chinese bead production [1, pp. 96–98]. Chemical analysis of twelve mutisalah samples from South India and Southeast Asia showed a consistent composition of approximately 50–70 per cent SiO₂, 10–24 per cent Na₂O, and negligible PbO, closely matching Mediterranean and Middle Eastern glass from Philippi and Persepolis [1, pp. 98–104]. The mutisalah constituted over 40 per cent of the approximately 8,000 glass beads from Malleret’s Transbassac sites (midpoint c. 500 A.D.), 30 per cent of over 800 beads from Kuala Selinsing, and 30 per cent of nearly 5,000 beads from Pengkalan Bujang (c. thirteenth century A.D.), but fell below 10 per cent at the sixteenth-century sites of Kota Tinggi and Johore Lama [1, p. 96].

Trade, Exchange, and Cultural Significance

Beads have functioned not merely as archaeological curiosities but as active agents in indigenous economies and cosmological systems. Among the Dusun of North Borneo, the ancient shell beads were embedded in a broader economy of goods-based exchange in which old brassware, gongs, and other antiquities functioned as currency alongside livestock and land [2, p. 169]. In the 1910s, Chinese shopkeepers at Kota Belud purchased the beads from Dusun sellers and resold them to Iban traders from Sarawak, who carried them back to their own country where they commanded a ready market; by 1950, export had made the beads rarer and more expensive, though demand had declined and Iban trading visits had ceased [2, p. 169]. The price at Kota Belud in the 1910s was approximately one dollar (local currency) for two loops, measured over the fork of the thumb to the elbow [2, p. 169].

The Dusun attached a creation legend to the beads, transmitted through three generations of a family at Kadamaian, in which the male deity Kinorohingan scattered sand from the sky during a rundukan (seance), and the beads fell from the loosened hair of the women conducting the ritual [2, p. 171]. Evans traced the Dusun names for the beads—kinokogis at Kadamaian and kokogis elsewhere—to roots meaning “sand” (ogis/togis) and “clam” (kokogis), and argued that kinokogis likely means “there was in past time sand” or “there was in past time a clam,” with the prefix kina- indicating past time, paralleling kinomulok (rice-wine) and Kinorohingan (the deity) [2, pp. 170–171]. A related celestial origin is attributed to a black-and-white spotted glass bead (minorok-worok), which Kinorohingan took from the water above and which, when present in a house, protects it against fire [2, p. 171].

At the Johore sites, the extraordinary variety of the bead assemblage—spanning Hittite, Cypriot, Roman, Chinese, and European types, with specific gravities extending well beyond the range found at other Southeast Asian sites—points to a trade network of considerable complexity that aligns with the great expansion of maritime commerce in the fifteenth century [4, pp. 87–88]. Lamb documented two new finds from the Tirot collection of 1963: a gold filigree bead closely comparable to Mediterranean examples from Oc-èo in South Vietnam, and two glass beads moulded in the shape of human molar teeth, both of which reinforce the picture of a sophisticated and multi-sourced bead trade operating at the Johor sites [4, p. 97–98].

Research and Documentation

The Society’s literature on beads spans nearly six decades and reflects a clear evolution in methodological approach and interpretive framework. The earliest contribution, Evans’s 1933 note on the Pahang cornelian bead, is a brief descriptive record of a single find, typical of the short-notice format common in the journal at that time [5]. Evans’s 1951 article on Dusun shell beads represents a shift toward longer ethnographic and linguistic analysis, grounded in decades of personal fieldwork and supplemented by laboratory analysis at Cambridge [2].

The 1960s marked a decisive turn toward systematic archaeological methodology. Lamb’s 1964 and 1965 articles introduced chemical analysis, ceramic contextual dating, and cross-site comparative assemblage studies, establishing beads as a legitimate category for South-East Asian prehistoric and protohistoric research and mounting the first sustained challenge to the “Roman bead = Roman date” assumption [4], [1]. Francis’s 1991 article represents the culmination of this trajectory: a major historiographical intervention that corrects the Gardner-Beck narrative, reframes Malaya from a peripheral trading post to a central node in a pan-Indian Ocean beadmaking network, and integrates fieldwork at Papanaidupet and Arikamedu (cataloguing 50,000 beads and wasters) with personal examination of assemblages across Southeast Asia [3]. The arc from single-specimen description to regional industrial reconstruction illustrates the maturation of bead studies within the Society’s scholarly output.

Beads constitute one of the most abundant and archaeologically informative categories of material culture in the Malay Peninsula and Borneo, occurring across the full range of site types from megalithic cist burials to coastal trading settlements and upland domestic contexts [1, p. 87]. Their significance extends well beyond ornament: they functioned as currency in indigenous exchange economies, as markers of social and cosmological identity, and as diagnostic artefacts for reconstructing ancient maritime trade networks spanning the Indian Ocean and China Seas [2, p. 169], [1, pp. 87–88]. The bead record in the region encompasses glass, stone, shell, and metal types manufactured locally or imported from South India, the Mediterranean, China, and Southeast Asia itself, and its interpretation has been the subject of sustained scholarly debate since the 1930s [3, pp. 97–99], [4, pp. 88–98].

The Indo-Pacific Beadmaking Industry

The most consequential reframe of the regional bead record came with Peter Francis Jr.’s 1991 reassessment, which demonstrated that the Malay Peninsula was not a passive recipient of foreign trade goods but a major production centre for the ubiquitous Indo-Pacific drawn glass bead [3, p. 97]. Francis identified the Lada process—a tube-drawing technique still practised at Papanaidupet in Andhra Pradesh, southern India—as the manufacturing method behind this bead type. The process involves rolling molten glass on a long iron tube (lada), piercing it with a chetleak rod, and hand-pulling the tube over approximately three hours; its diagnostic wasters—gedda paru flakes, twisted tubes, flares, and collapsed tubes—match those found at Arikamedu exactly, with the sole exception that the Arikamedu master used a pincher-like tool rather than an iron hook [3, pp. 99–100].

By matching these diagnostic wasters between Papanaidupet, Arikamedu, and Southeast Asian sites, Francis traced the industry’s migration across the region: from Arikamedu (c. 250 B.C.–A.D. 250) to Klong Thom in Thailand and Oc-eo in Vietnam in the early centuries, then to Kuala Selinsing and Sating Pra in the seventh to tenth centuries, and finally to Takua Pa and Sungai Mas in the ninth to thirteenth centuries [3, pp. 101–103]. All four early sites shared Roman emporia, strong South Indian (Pallava/Tamil) associations, and cross-site exchange of beads and stone beadmaking, leading Francis to propose a loose trading federation—the “Arikamedu League”—that may have provided the germinal idea for Srivijaya [3, pp. 101–103].

Glass composition analyses of 21 early Indo-Pacific beads from Arikamedu, Oc-eo, and Klong Thom, and 29 medieval beads from India, Thailand, Malaysia, Sarawak, and Flores, confirm that these beads were made from locally produced glass rather than recycled Western material [3, p. 106]. The industry’s terminal date in Southeast Asia is corroborated by Philippine data: Indo-Pacific beads constitute 61.5 per cent of Developed Metal Age assemblages but only 1.1 per cent in the period corresponding to the Southern Song dynasty (from A.D. 1127), pointing to a disappearance around 1200 [3, p. 104]. After c. 1000, direct imports from the Muslim world—segmented beads, fused mosaic cane beads, and folded beads—began arriving in large quantities at Kedah and Sungai Mas, and by the thirteenth century Chinese coil beads had replaced Indo-Pacific beads across the region [3, pp. 106]. The 1988–89 Fort Canning Hill excavations in Singapore uncovered a fourteenth-century Chinese coil bead workshop with a small fire, glass sherds, melted pieces, and finished beads, confirming local manufacture of the replacement type [3, p. 111].

The “Roman Bead” Debate

The interpretation of glass beads from the Johore River sites—Johore Lama and Kota Tinggi—has been the most contested question in Malayan bead archaeology. In 1937, G. B. Gardner published a claim that Roman glass beads found at these sites evidenced direct Roman-Malay trade, a position supported by the bead specialist Horace Beck, whose 1936 report catalogued 59 numbered items from Gardner’s collection of approximately 600 beads and 800 gem stones with specific gravity measurements and comparative identifications [4, pp. 88–97]. This claim fed into the broader Ptolemaic “Golden Khersonese” debate and dominated Malayan archaeology for decades [1, p. 119].

Alastair Lamb mounted the first systematic challenge in 1964 and 1965. Applying a strict contextual dating argument, he demonstrated that the ceramic assemblage at Kota Tinggi—Chinese porcelain sherds and stamped earthenware—cannot be dated before the fifteenth century, thereby constraining the terminus post quem for all beads in situ [4, p. 97], [1, p. 119]. The Makam Sultan site, on ceramic evidence, was first occupied no earlier than the late fourteenth century, meaning all beads found there must post-date that horizon regardless of their date of manufacture [4, p. 97]. Lamb further showed that the “Roman” types in question—zone beads and chevrons—were still being manufactured in Amsterdam in the seventeenth century, and that genuine Roman beads could have been collected second-hand from old necklaces or excavated sites in the Levant before export eastwards [1, p. 119]. The same zone bead, he argued, is a “late Sung or Yuan period Roman bead” at Pengkalan Bujang, a “Ming period Roman bead” at Kota Tinggi, and merely “modern” on the neck of a living Iban girl [1, p. 119].

Francis’s 1991 reassessment delivered the definitive correction. Re-examining Beck’s original identifications, he showed that of the 59 beads, only eight were tentatively assigned to Roman or Mediterranean origin, and even those are problematic: some are Bohemian, one is a steatite bead misidentified as Hittite, and the famous “Roman” chevron bead is now known not to have been produced before c. 1480 [3, pp. 98–99]. The weight of evidence supports C. A. Gibson Hill’s earlier scepticism that the presence of a few early beads does not make the site ancient [3, pp. 98–99].

Stone, Shell, and Other Bead Types

Beyond the glass bead record, the region’s assemblages include stone, shell, and metal types of considerable antiquity and cultural significance. I. H. N. Evans documented a large hexagonal-section spindle bead of veined and striped cornelian, measuring 7.1 cm in length, discovered by R. M. A. Maycock on a hillside at Jerantut Estate, Pahang [5, p. 146]. The bead was imbedded in soil on a steep slope, approximately one foot nine inches below the surface, and represented a type apparently unknown in the Malay Peninsula prior to this find [5, p. 146]. While ancient cornelian beads are well attested from Kuala Selinsing in Perak, the hexagonal-section spindle form differs from the rectangular-section faceted beads previously recorded there [5, p. 146]. Evans was cautious about dating the specimen, noting that no faceted stone beads have been definitively assigned

MBRAS Sources

• I.H.N. Evans (1933). An ancient cornelian bead from Pahang. JMBRAS 11(2): 146–147
• I.H.N. Evans (1951). Ancient shell beads in North Borneo. JMBRAS 24: 168–171
• P. Francis (1991). Glass beads in Malaya: a reassessment. JMBRAS 64: 97–118
• A. Lamb (1964). Notes on beads from Johor Lama and Kota Tinggi. JMBRAS 37: 88–98
• A. Lamb (1965). Some observations on stone and glass beads in early South-East Asia. JMBRAS 38(2): 87–124

References

1. A. Lamb (1965). Some observations on stone and glass beads in early South-East Asia JMBRAS 38(2): 87–124. Read on JSTOR
2. I.H.N. Evans (1951). Ancient shell beads in North Borneo JMBRAS 24(1): 168–171. Read on JSTOR
3. P. Francis (1991). Glass beads in Malaya: a reassessment JMBRAS 64(1): 97–118. Read on JSTOR
4. A. Lamb (1964). Notes on beads from Johor Lama and Kota Tinggi JMBRAS 37(1): 88–98.
5. I.H.N. Evans (1933). An ancient cornelian bead from Pahang JMBRAS 11(2): 146–147. Read on JSTOR