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Characterization of glass beads from Nanhai I shipwreck and new evidence of lead tin yellow type II in China


Glass beads excavated from Nanhai I shipwreck were investigated with scanning electron microscopy with energy dispersive spectrometer (SEM–EDS), Raman spectroscopy, multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS) and X-ray diffraction (XRD). Dating back to the Southern Song Dynasty, these beads help to study Chinese maritime trades during the twelfth–thirteenth century. The bead samples are categorized into five groups by color, i.e., yellow, orange-red, blue, dark red and light red. All beads are of K2O-PbO-SiO2 and PbO-SiO2 glass systems and in form of coil bead, which further confirms the Chinese origin of them. Lead tin yellow type II was identified in the opaque yellow coil beads, and K2SnxPb(1-x)Si3O9 crystals were found in both yellow and orange-red samples. Through the preparation of glass with the same formula as the ancient yellow beads, lead tin yellow type II was probably synthesized beforehand and added as colorant because its raw materials tend to form K2SnxPb(1-x)Si3O9 crystals in the K2O-PbO-SiO2 glass during firing. As lead tin yellow type II is an atypical colorant in China, these beads from Nanhai I shipwreck may serve as the first clear evidence of lead tin yellow type II presenting in the Chinese glass system. The lead isotope ratios of the yellow beads suggest they were produced in Fujian Province, China. The introduction of the lead tin yellow coloring technique might have a close connection to the glass making in the Southeast Asia and these beads seemed to be made specifically for overseas markets.

Introduction and research aim

Chinese glass beads played an important role in the world’s bead trades during the twelfth–fourteenth century. However, there is only sketchy information about them. Coil beads are the most common and most widely distributed kind of Chinese glass beads [1]. They are a special kind of wound beads, produced by winding molten glass around a mandrel to form a loop or occasionally several paratactic loops just like coils. Because of these unique features, they were also called “single wound” [2]. They are smaller, shinier and heavier compared with Indo-Pacific beads, and took the leading position in the Southeast Asian bead market as Indo-Pacific beads were in decline during the twelfth century [1, 3]. Coil beads have been excavated from the sites in Southeast Asian countries regularly, and occasionally in East African countries. In the Philippines, Sumatra, East Java of Indonesian, Sarawak of Malaysia and Singapore, coil beads appear in sites after the first millennium, and in sites dated twelfth–fourteenth century A.D. they always dominated [1, 4].

Scholars deduced from the technical features and distribution of coil beads that they have a Chinese origin [1, 5,6,7]. The perspective is convincing, but there is still a lack of direct evidence of manufacturing which is necessary to identify coil beads as Chinese products with certainty. Fortunately, some coil beads have been excavated from Nanhai I shipwreck, a cargo ship dating back to the Southern Song Dynasty (1127–1279 A.D.), heading Southeast Asia but sank 20 km south off the shore of Yangjiang city, Guangdong province. Thousands of pieces of goods have been excavated from this shipwreck. Porcelains and metal wares make up the majority of the cargo [8]. Glass beads were just one of the many kinds of merchandise that the Chinese produced and sold them abroad to pay for the Annual Tribute and increase import needs. Zhu Fan Zhi (诸蕃志) was a guide book of the Southern Song Dynasty for merchants to view what items were in demand by different Southeast Asian areas. “Liuli beads”, the archaic expression of glass beads, “Colored fired beads” and “colored liuli beads” were mentioned in Zhu Fan Zhi in the listings of commodities that were traded with local people in Mayi (the islands of Mindoro and Luzon in the Philippines) and Boni (Kalimantan), which corresponds with the distribution of excavated coil beads.

The glass beads samples in this paper are all identified as coil beads. The results of the tests show their high lead contents, consistent with most of the coil beads analyzed [1, 3, 5, 9]. Additionally, this is the first time that lead tin yellow is found in Chinese lead glass system. Lead tin yellow glass was produced in Europe during a short period of the first to second century B.C., and the production resumed from first century A.D. This type of glass is a dominant one during the fifth to seventh century at 10 sites around western Europe [10]. As a pigment, lead tin yellow is discovered on paintings from about the fourteenth to eighteenth century in Europe [11,12,13]. But lead tin yellow is not a common colorant or pigment in Chinese tradition. Glass beads with lead tin yellow type II have been reported in China, but their chemical compositions indicate that they were imported from West or Central Asia [7, 14, 15]. In the glass beads from Nanhai shipwreck I, lead tin yellow type II present itself in the Chinese glass system for the first time. In this paper, the coil bead samples from Nanhai I are examined by scanning electron microscopy with energy dispersive spectrometer, Raman spectroscopy, multi-collector inductively coupled plasma mass spectrometry and X-ray diffraction, in hope that their close and direct relationship with China provides opportunities to look into the maritime glass beads of China during the Southern Song Dynasty. More importantly, the research is more focused on the characterization and technical aspects of the beads containing lead tin yellow type II.

Materials and methods

Materials and classifications

Glass beads were collected by sieving the sludge on site during the excavation of the Nanhai I shipwreck and the samples in this paper were provided by the archaeological staff there. They are all identified as coil beads by their typical coil-like appearance. Based on the surface colors, the glass beads seem to include 9 kinds (Fig. 1a, c, e, h, i, k, m–o). However, after polishing and exposing their inner sections, there are only five colors, i.e., yellow (or lemon-yellow), orange-red, blue, light red, and dark red. Among them, yellow beads and orange-red beads are opaque, light red beads and blue beads are transparent and dark red beads are translucent. Additionally, there are also larger yellow beads about 4 mm in diameter (shown in Fig. 1g), compared to smaller beads in the other figures about 2 mm in diameter. Possibly due to certain technical flaws, some beads were not separated and in the form of twin or triplet with evident coil-like signature.

Fig. 1
figure 1

Appearance of the Nanhai I shipwreck bead samples: yellow beads (ag), orange-red beads (hl), blue beads (m), light red beads (n), dark red beads (o, p), scale bar 0.5 mm (b, d, f, j, l, p), 1 mm(a, c, e, f, k, mo), and 2 mm (gi)

Scanning electron microscopy

Backscattered electron (BSE) images and chemical compositions of the glass beads were acquired by Hitachi TM3030 scanning electron microscope with energy dispersive spectroscopy (SEM–EDS). EDS analysis was carried out on the cross-sections of each glass bead within an area of over 100 μm × 100 μm and over 60 s accumulation time under low vacuum mode. Due to the limited sample quantities and their preservation status, typical (judged by cross-section morphology) samples of each kind were tested and mean compositions were calculated. EDS spot tests were carried out on the phases of interest under the same conditions.

Raman spectroscopy

Raman spectra were acquired by BWTEK i-Raman PLUS with BAC151 Raman video microscope to identify the phases of colorants in glass beads. The detectable spectral range (Raman shift) of the instrument is from 150 to 4200 cm−1 with a resolution of 4.5 cm−1. The laser beam spot size is 105 μm under the 20X objective. The accumulation time in each acquisition was 60 s under maximum intensity of 532 nm laser light source (40 mW).

X-ray diffraction

XRD analysis was performed on X-pert3 Powder, PANalytical with Cu anode to detect the crystals in the grinded sample. The working voltage of X-ray tube was 40 kV. The working electric current was 40 mA. The scanning degree 2θ is from 10° to 80° with step size 0.013° and scan step time 53.3 s.

Multi-collector inductively coupled plasma mass spectrometry

Lead isotope ratios were tested by VG Axiom multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS). The samples were dissolved in aqua regia, diluted and added 0.5 mg/L Tl2SO4 for an internal correction of mass bias. The errors are of < 0.05% for 207Pb/206Pb and 208Pb/206Pb values.

Simulation of the yellow glass

Lead tin yellow type II (PbSnxSi(1-x)O3, Pb:Sn:Si feed ratio 2:1:1) was synthesized at 900 °C for 5 h with reference to the literatures [13, 16] and the glass was fired at 800 °C, 850 °C and 900 °C respectively according to the compositions tested. K2CO3 (AR, from Tianjin Zhiyuan Chemical Reagent Co. Ltd.), SiO2 (silica gel, from Beijing Ocean Chemical Engineering Co. Ltd.), Pb3O4 (AR, from Sinopharm Chemical Reagent Co. Ltd.) and SnO2 (Shanghai Zhanyun Chemical Co. Ltd.) were used as the raw materials and the firing process took place in a quartz boat with platinum lining heated by an electric tube furnace.

Results and discussion

The chemical compositions of all bead samples tested are summarized in Table 1. The Chinese origin of the beads is confirmed with the average PbO content between 46 and 63 w% with the secondary fluxing agent as K2O, which exactly match the chemical features of K2O-PbO-SiO2 and PbO-SiO2 glass systems of the Song Dynasty [7]. As tin serves as not only colorant but opacifier as well, the yellow and orange-red beads that contain tin oxide are opaque, while blue and light red beads are transparent and dark red beads are translucent.

Table 1 Chemical compositions of Nanhai I shipwreck beads (w%)

In SEM images, the vitreous matrices of the beads have distinct particles dispersing within them. The occurrences of these phases vary among different beads. Some of them are euhedral, showing angular edges, and others are rounded or spherical.

Yellow beads

For yellow beads, both lighter and darker phases present themselves in the BSE images, representing phases of higher average atomic number than that of the matrix and those of lower average atomic number. The dark particles with sharp edges in Figs. 2a and 3b are featured with high contents of K2O, SnO2, and SiO2 (shown in Table 2) in an atomic ratio of K:Sn:Si as 2.06:1.00:3.16, which suggests a probable chemical formula of these particles as K2SnSi3O9. The minor PbO content may also suggest possible partial replacement of Sn with Pb, written as K2SnxPb(1-x)Si3O9. However, there were no signals corresponding to these crystals in XRD analysis and thus their formula was not fully confirmed [17].

Fig. 2
figure 2

BSE images of yellow (a), orange-red (b), blue (c), dark red (d), and light red beads (e)

Fig. 3
figure 3

BSE images of phases of interest: a Pb–Sn-Si phase (lighter particles) in a yellow bead, b K-Sn-Si phase (darker particles) in a yellow bead, c K-Sn-Si phase (dark particles) in an orange-red bead

Table 2 Chemical compositions of inclusive phases in the Nanhai I shipwreck beads

Lighter particles with round edges in Figs. 2a and 3a contain much higher PbO content (68.36%) compared to the matrix. The atomic ratio of Pb:Sn:Si is 1.00:0.35:0.73, which can be further speculated as PbSn0.32Si0.68O3. Such a result indicates the presence of lead tin yellow type II in the yellow beads, which can be either written in PbSnO3 by Rooksby [18] or PbSnxSi1-xO3 by Clark et al. [16]. Results from Raman spectroscopy shown in Fig. 4 further confirmed the presence of lead tin yellow type II. The spectrum of the yellow beads shows one sharp and pronounced peak at 135 cm−1 and two broad peaks at 325 cm−1 and 442 cm−1, exactly consistent with the spectrum of lead tin yellow type II, according to R.J.H. Clark’s Raman study on the lead tin yellow pigments [16]. The XRD spectrum of the yellow beads powder is also provided in Fig. 5, showing the recognized phase as PbSnO3. Therefore, lead tin yellow type II does exist in these yellow coil beads. These irregular particles indicate that they were not formed by liquid phase separation during the firing process (in which case they would be more spherical). Considering their underdeveloped crystal form and clear XRD spectrum, these particles are cryptocrystalline.

Fig. 4
figure 4

Raman spectrum of the yellow bead’s cross-section

Fig. 5
figure 5

XRD spectrum of the yellow bead powder

According to Clark’s study, lead tin yellow type II decomposes above 950 °C [16]. Hradil’s study suggests that the higher calcination temperature is, the lighter the color of lead tin yellow type II will be. The pigment calcined at 850 °C has a reddish hue, while the pigment calcined at 900 °C is closer to the neutral yellow of yellow beads [13]. Therefore, to study the formation condition of lead tin yellow type II containing glass and confirm whether lead tin yellow type II was pre-synthesized and added to the glass formula or it can be directly formed from glass melts with SnO2 addition, we first synthesized lead tin yellow type II (PbSnxSi(1-x)O3, Pb:Sn:Si feed ratio 2:1:1) and fired the glass according to the compositions tested.

The glass directly synthesized from Pb3O4, K2CO3, SiO2 and SnO2 at 900℃ is colorless when calcined for 0.5 h (shown in Fig. 6a), and it remained colorless after being calcined for 5 h. K2SnxPb(1-x)Si3O9 crystals present in this colorless glass (shown in Fig. 6b). The glass synthesized from Pb3O4, K2CO3, SiO2 and pre-synthesized lead tin yellow type II displays neutral yellow color despite the different calcining temperature at 800 °C, 850 °C and 900 °C (shown in Fig. 6a). K2SnxPb(1-x)Si3O9 crystals present in the glass calcined at 850 °C and 900 °C (shown in Fig. 6c), which suggests lead tin yellow type II is not stable at such temperatures and partially transforms to K2SnxPb(1-x)Si3O9 crystal. This crystalline phase serves as a signal of calcining temperature around or above 850 °C. The synthesis of yellow glass succeeded only with the addition of pre-synthesized lead tin yellow type II, indicating that lead tin yellow type II was synthesized beforehand in the glass bead production while direct addition of SnO2 into the potash lead silicate glass only produce K2SnxPb(1-x)Si3O9 crystals. Lead tin yellow type II was added as either colorant or both colorant and opacifier. The description “liuli beads of different colors” in Zhu Fan Zhi corroborates the introduction of lead tin yellow type II as colorant. “Different colors” implies the bead makers had the information about what materials were needed to produce beads with certain colors and lead tin yellow type II was known to be a necessary raw material of yellow glass beads. The opacification is more likely to be unintentional or concomitant.

Fig. 6
figure 6

Images of a glass directly synthesized from Pb3O4, K2CO3, SiO2 and SnO2 at 900 °C (left), glass synthesized with pre-synthesized lead tin yellow type II calcined at 800 °C (up), 850 °C (right) and 900 °C (bottom), all for 0.5 h; b BSE images of glass fired at 900℃ with SnO2 as Sn source, showing K2SnxPb(1-x)Si3O9 crystals (dark particles), and c glass fired at 850 °C with synthesized lead tin yellow type II as Sn source, showing remaining lead tin yellow type II (lighter particles) and newly formed K2SnxPb(1-x)Si3O9 crystals (darker particles near the bubble)

As the colorless glass synthesized from Pb3O4, K2CO3, SiO2 and SnO2 at 900℃ contains a considerable amount of presumed K2SnxPb(1-x)Si3O9 crystals, it provided the opportunity to re-examine these crystals by XRD. The XRD peaks of the colorless glass match well with those presented in PDF#27-0446 for K2SnSi3O9 and PDF#41-1445 for cassiterite, though several differences regarding the K2SnSi3O9 have been observed. The diffraction angles (2θ) observed at 15.6°, 25.1°, 29.4° and 30.4° slightly shift from 14.7°, 23.3°, 30.0° and 30.7° respectively. The deviations of the peaks indicate that Pb partly replaces Sn in the crystal as previously presumed. Therefore, it would be more accurate to describe these crystals as K2SnxPb(1-x)Si3O9, though they are close to K2SnSi3O9 considering SEM results.

It is worth noticing that the lead tin yellow type II is not a typical colorant of Chinese tradition. Lead tin yellow type II does not occur naturally. And it has been used in both painting and glass coloring in the western world. The use of tin-based opacifiers in glass and pottery making dates back to early historical times [13], first in glass production in Egypt and the Near East in the mid-second millennium B.C. [5]. Glass beads with yellow trails dates back to the eighth–seventh century B.C. Sardis is the earliest occurrence of lead tin yellow type II that has been reported [19]. Lead tin yellow glass is produced in Europe during the first–second century B.C., and the gradual substitution of tin-based opacifiers, such as lead stannate yellow and tin oxide white, for antimony-based opacifier in glassmaking in Europe by fourth century A.D. makes the presence of lead tin yellow more frequent. The use of tin-based opacifiers spread from the eastern Mediterranean into northern and western Europe, and throughout the Roman and Byzantine Empires [10, 19]. This type of glass is popular at several sites during the fifth–seventh century around western Europe according to archaeological studies [10]. As a pigment, lead tin yellow is used in paintings from about the fourteenth–eighteenth century in Europe, and during the fifteenth–seventeenth century it has been used most frequently [11, 13, 20].

Some glass beads excavated in China have been reported to contain lead tin yellow type II, such as beads from Jiu-Zhi-Ling tomb site and Feng-Men-Ling tomb site, Hepu County, Guangxi [14], Shanpula tomb site, Lop County, Xinjiang [21], Da-Wang-Ku-Mu site, Xinhe County, Xinjiang [14] and Xiao Mausoleum, Xiangyang City, Shaanxi [15]. But considering their chemical compositions, these beads can hardly be regarded as samples of Chinese glass with lead tin yellow type II, for they are mostly identified as soda-lime glass of Central Asian or Western origins.

The beads excavated from Nanhai shipwreck I are so far the first and earliest evidence of lead tin yellow type II present in the Chinese glass system. However, there seems to be no clear evidence to trace the origin of lead tin yellow type II production. As the production of glass beads requires only simple equipment and can be done in small workshops, there would hardly be any identifiable remains. Although the chemical composition of the yellow beads belongs to the typical Chinese K2O-PbO-SiO2 glass system, its provenance cannot be fully confirmed by chemical composition alone. The lead isotope ratios of yellow Nanhai I shipwreck beads are shown in Table 3. The results correspond exactly with the lead isotope data of green glaze of ceramics from Cizao kiln also excavated from Nanhai I shipwreck [22]. It is very unlikely that the lead isotope ratios of the glass matrix are different from those of the lead tin yellow type II particles and their combined lead isotope ratios happen to be the same as those of green glaze from Cizao kiln. Therefore, both the glass matrix and the lead tin yellow type II were produced with exactly the same raw materials used by Cizao kiln, which further confirms the Chinese origin of the beads from Nanhai I shipwreck. Located in Jinjiang, Quanzhou, Fujian province, Cizao kiln was one of the manufacturing centers of export porcelains during Song and Yuan Dynasties [23]. Quanzhou port was also an important port from which China connected with Southeast Asia [1]. No evidence suggests that Cizao kiln produced glass, but the fact that ceramics from Cizao kiln and the yellow glass beads applied exactly the same raw materials indicating that the glass workshop was probably located in Quanzhou, the same district as Cizao kiln. It is now quite certain that lead tin yellow type II production technique was commanded by Chinese people during the Southern Song Dynasty. Yet there has been no lead tin yellow excavated or found in any other artifact of Chinese origin until it was used as glaze pigment on porcelain during Qing Dynasty [24, 25]. Therefore, the lead tin yellow type II production technique was possibly introduced to China via the Maritime Silk Road, probably from Southeast Asia. Beads containing lead tin yellow before the Southern Song Dynasty have been excavated along Africa [26, 27], South Asia [28], and Southeast Asia [29, 30], and China had traded with the regions along the South China Sea Rim through the Maritime Silk Road for centuries. Therefore, the ancient Chinese glass makers might well be influenced by the Southeast Asian glass markers to apply lead tin yellow as colorant for yellow color. And the Southeast Asian glass makers are supposed to learn the techniques from the Western glass makers as lead tin yellow originated in the Mediterranean area [10]. The lead tin yellow beads excavated in Xinjiang, Guangxi and Shaanxi provinces indicate other possible transferring routes. But except one bead sample from Feng-Men-Ling, Guangxi, which is speculated to use local lead ore [14], there haven’t been any more evidence of the combination of lead tin yellow and Chinese glass. As for the lead tin yellow bead possibly using Chinese lead ore, the lead content of it was below 7% and the bead was attributed to soda-lime glass [14], which has limited localization features. In addition, this bead sample from Guangxi dates back to the Han Dynasty, about 1000 years earlier than the Nanhai I shipwreck beads, and no similar products during this interval have been found. Thus, there seems to be very limited evidence to suggest that those early communication influenced the production of the yellow glass beads from the Nanhai I shipwreck. Therefore, taking the contemporaneity and frequent commerce into consideration, Southeast Asia was the most probable direct source of lead tin yellow techniques transferring into China and applied to the yellow beads from Nanhai I shipwreck. Furthermore, these glass beads seemed to be only for export purpose. No similar glass beads have been reported on Chinese mainland and lead tin yellow type II is not so appropriate a colorant in lead glass system compared with iron oxide. Thus, these yellow beads were more likely to be a combination of the coloring technique learning from Southeast Asia and the domestic glassmaking, and specifically made for overseas markets.

Table 3 Lead isotope ratios of Nanhai I shipwreck beads and Cizao porcelain

Orange-red beads

The remarkably high Cu2O content in EDS results indicates that the orange-red hue is probably caused by red cuprite. Raman spectrum of the orange-red bead has a sharp absorption at 213 cm−1, two weak broad absorptions at 422 cm−1 and 625 cm−1 and a strong broad absorption at around 3000 cm−1, which coincides with cuprite spectra from the RRUFF database.

Only one observable cuprite particle was found in orange-red beads observed (Fig. 7). The chemical analysis of the cuprite particle in an orange-red bead exhibits high cuprite content (67.18 w%). The presence of the cuprite particle indicates that cuprite was synthesized beforehand and introduced into the vitreous matrix as the colorant.

Fig. 7
figure 7

XRD spectrum of the colorless glass (shown in Fig. 6a.)

K2SnxPb(1-x)Si3O9 crystals as previously discussed are also detected in orange-red beads (shown in Figs. 2b, 3c, and Table 1), which appear to be a characteristic phase of SnO2 containing K2O-PbO-SiO2 glass. However, there are no lead tin yellow particles present in the orange-red beads. Lower PbO and SnO2 contents (about 46% and 1% in the orange-red beads compared to about 58% and 4% in yellow beads) is a probable reason. And tin tends to form K2SnxPb(1-x)Si3O9 instead of PbSnxSi1-xO3 particles in the K2O-PbO-SiO2 glass system. Additionally, considerable high content of Cu2O may affect the preservation of lead tin yellow type II during firing as well, even if Sn was introduced in the form of lead tin yellow type II. Thus, there’re no lead tin yellow particles present (Figs. 8, 9).

Fig. 8
figure 8

Raman spectrum of the orange-red bead’s cross-section

Fig. 9
figure 9

BSE and elemental maps of the cuprite particle in an orange-red bead

Blue beads

CuO is responsible for the color of blue beads according to SEM results. Blue beads have CaO content (3.34%) obviously higher than beads of other colors. As CaO is not a necessary substance in glass production, it was probably introduced by lime for unknown reason, and the possibility of plant ashes is excluded as no phosphorus has been detected and MgO content is low.

Light red beads and dark red beads

The SEM results indicate that Cu2O and Fe2O3 are responsible for the red color. And the different contents of Cu2O and Fe2O3 caused the distinction between light and dark red. The average Cu2O content of dark red beads is 1.64 w%, triple the 0.55 w% Cu2O average content of light red beads, while the average Fe2O3 content is 1.42 w% for the dark one and 0.20 w% for the light one, a disparity of 7 times. In the dark red beads tested, K2O content is obviously lower than beads of other colors and PbO serves as the dominant fluxing agent [14].

It is noteworthy that transparent red glass, applying Cu2O as the colorant, is a characteristic of the Chinese glass system [1]. This kind of transparent red glass is commonly called “ruby red”, and it further confirms the Chinese origin of the beads.


Coil beads excavated from Nanhai I shipwreck have been characterized by SEM, XRD and Raman spectroscopy. The beads tested all contain high PbO content (46–63 w%), with K2O as a secondary fluxing agent, which corresponds well to K2O-PbO-SiO2 and PbO-SiO2 glass systems of the Song Dynasty. The beads from Nanhai I shipwreck are divided into five groups by color: yellow, orange-red, blue, dark red and light red. Lead tin yellow type II, Cu2O and CuO are responsible for yellow, orange-red and blue respectively, while Cu2O and Fe2O3 together are responsible for the light and dark red with distinctions of contents. Lead tin yellow type II serves as both colorant and opacifier in yellow beads. According to Zhu Fan Zhi, lead tin yellow type II is more likely to be added as colorant intentionally. The presence of lead tin yellow type II and K2SnxPb(1-x)Si3O9 particles helps to study the possible glass-making technology that lead tin yellow type II was synthesized beforehand and high temperature (around or above 850 °C) is not conducive to keep the yellow color. This is so far the first clear evidence of the presence of lead tin yellow type II in the Chinese glass system. The lead isotope ratios of the yellow beads suggest the lead tin yellow type II was produced in Fujian Province, possibly in Quanzhou district. Furthermore, it is inferred that the coloring technique of lead tin yellow type II had a close connection to the glass making in the Southeast Asia and these glass beads seemed to be made specifically for overseas markets.

Availability of data and materials

The datasets analyzed during the current study are available from the corresponding author on reasonable request.



Scanning electron microscopy with energy dispersive spectrometer


Multi-collector inductively coupled plasma mass spectrometry+


X-ray diffraction


Backscattered electron


Powder diffraction file


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We thank Dr. ZHANG Ji from School of Archaeology and Museology, Peking University for helping conduct the lead isotope analysis.


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All the experiments were designed and carried out by CT and YZ. The data were analyzed by CT, YZ and KW. The sample was collected with the help of JS and YC. The manuscript was written by CT and YZ and revised by KW and DH. All authors read and approved the final manuscript.

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Correspondence to Kai Wang.

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Tian, C., Zhou, Y., Wang, K. et al. Characterization of glass beads from Nanhai I shipwreck and new evidence of lead tin yellow type II in China. Herit Sci 9, 61 (2021).

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