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The distribution of Neolithic and Bronze sites unearthing millets, rice, barley, cowrie shells, and perforated stone knives in China, South Asia, and Southeast Asia (a, b, and c) Represent the distribution of different elements during 6000-4000 BP, 4000-3000 BP, and 3000-2200 BP (Detailed information is listed in Supplemental Table S1).

The distribution of Neolithic and Bronze sites unearthing millets, rice, barley, cowrie shells, and perforated stone knives in China, South Asia, and Southeast Asia (a, b, and c) Represent the distribution of different elements during 6000-4000 BP, 4000-3000 BP, and 3000-2200 BP (Detailed information is listed in Supplemental Table S1).

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The emergence and intensification of transcontinental exchange during both the Late Neolithic and Bronze Age profoundly influenced the social history of Eurasia. While scholars have intensively discussed east-west long-distance communication along the proto-Silk Road, the north-south transport networks that connected China to South and Southeast As...

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... (1990) proposed that Neolithic cultural elements from northern China (such as semisubterranean dwellings and perforated stone knives) were introduced from the Bangong Lake region into the Kashmir areas via the valleys of the Lancang and Yarlung Tsangpo Rivers. In addition to artifacts, millet remains were unearthed from two Neolithic sites in the Kashmir Valley and dated to 4500-4000 BP ( Spate et al., 2017;Yatoo et al., 2020; Figure 3a and Supplemental Table S1). This suggests a possible connection to trans-Himalayan routes via the Tibet Plateau and the Himalayan mountains or an introduction via the proto-Silk Road ( Chen et al., 2022). ...
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... stone knives were unearthed from a cultural context dated 4000-3000 BP at the Changguogou site, the Qugong site in the south Tibetan Plateau, and the Loebanr, Bir-kot-ghundai, Kalalo-deray, Bruzahom, and Gufkral sites at the Swat Valley and in Kashmir (Lü, 2016;Figure 3b). Millet and barley remains were identified and dated to 4000-3000 BP at the Changguogou site ( Fu et al., 2000) and Qugong site ( Gao et al., 2021) in the middle and lower reaches of the Yarlung Tsangpo River (Figure 3b). Millet remains were frequently found in late Harappan sites in South Asia, date to 4000-3000 BP ( Pokharia et al., 2017;Saraswat, 1993;Spate et al., 2017;Weber, 2003; Figure 3b). ...
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... and barley remains were identified and dated to 4000-3000 BP at the Changguogou site ( Fu et al., 2000) and Qugong site ( Gao et al., 2021) in the middle and lower reaches of the Yarlung Tsangpo River (Figure 3b). Millet remains were frequently found in late Harappan sites in South Asia, date to 4000-3000 BP ( Pokharia et al., 2017;Saraswat, 1993;Spate et al., 2017;Weber, 2003; Figure 3b). Barley may have been introduced to the Indian subcontinent at approximately 8000-5000 BP ( Liu et al., 2018;Petrie, 2015;Tengberg, 1999) and was widely utilized in South Asia during 6000-4000 BP (Figure 3a). ...
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... remains were frequently found in late Harappan sites in South Asia, date to 4000-3000 BP ( Pokharia et al., 2017;Saraswat, 1993;Spate et al., 2017;Weber, 2003; Figure 3b). Barley may have been introduced to the Indian subcontinent at approximately 8000-5000 BP ( Liu et al., 2018;Petrie, 2015;Tengberg, 1999) and was widely utilized in South Asia during 6000-4000 BP (Figure 3a). This frost-tolerant crop was introduced to the northeastern Tibetan Plateau at approximately 4000 BP ( Chen et al., 2015), slightly earlier than in the Yarlung Tsangpo River Valley (Figure 3b). ...
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... may have been introduced to the Indian subcontinent at approximately 8000-5000 BP ( Liu et al., 2018;Petrie, 2015;Tengberg, 1999) and was widely utilized in South Asia during 6000-4000 BP (Figure 3a). This frost-tolerant crop was introduced to the northeastern Tibetan Plateau at approximately 4000 BP ( Chen et al., 2015), slightly earlier than in the Yarlung Tsangpo River Valley (Figure 3b). While Liu et al. (2019) argue that barley was introduced into China via trans-Himalayan routes, supported by genetic evidence ( Zeng et al., 2018), more archaeobotanical evidence -significantly earlier dates of barley remains in South Asia and the southern Tibetan Plateau -is needed to test this hypothesis further. ...
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... some new radiocarbon dates spanning 3000-2200 BP from Late Bronze Age sites along the Yarlung Tsangpo River ( Wang et al., 2021) have been reported recently, the number of sites in this period is less than 4000-3000 BP (Figure 3c). This suggests there a decline in the significance of the trans-Himalayan routes or an absence of radiocarbon dating on these routes during the third millennium BP. ...
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... trans-Henguan mountain routes are along the eastern margin of the Tibetan Plateau, including the western Sichuan highland, northwestern Yunnan, and southeastern Tibet (Figure 1, Zone II). The trans-Henguan mountain exchange between China, South, and Southeast Asia was likely mainly along the "Shu-Shendu Road" (Luo, 1990) in prehistory and may start in the fifth millennium BP with a lower frequency exchange (Figure 3a). Rice remains were identified from a few Neolithic sites in South Asia and dated to 4500-4000 BP ( Long et al., 2022;Sharma et al., 2020; Figure 3a), implying the appearance of rice cultivation in South Asia by the mid-fifth millennium BP. ...
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... trans-Henguan mountain exchange between China, South, and Southeast Asia was likely mainly along the "Shu-Shendu Road" (Luo, 1990) in prehistory and may start in the fifth millennium BP with a lower frequency exchange (Figure 3a). Rice remains were identified from a few Neolithic sites in South Asia and dated to 4500-4000 BP ( Long et al., 2022;Sharma et al., 2020; Figure 3a), implying the appearance of rice cultivation in South Asia by the mid-fifth millennium BP. These rice remains might have been transmitted into South Asia following multiple dispersal routes similar to the historically documented "ShuShendu Road," although no rice remains have been found in Myanmar (Figure 3a). ...
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... remains were identified from a few Neolithic sites in South Asia and dated to 4500-4000 BP ( Long et al., 2022;Sharma et al., 2020; Figure 3a), implying the appearance of rice cultivation in South Asia by the mid-fifth millennium BP. These rice remains might have been transmitted into South Asia following multiple dispersal routes similar to the historically documented "ShuShendu Road," although no rice remains have been found in Myanmar (Figure 3a). The trans-Hengduan mountain routes might also act as essential passageways linking China and mainland Southeast Asia via north-south riverine valleys (Higham, 2002;Higham et al., 2020), although reported radiocarbon dates of 5000-4000 BP in northwestern Yunnan, which is at the hub of the "Shu-Shendu Road," are limited (Supplemental Table S1). ...
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... earliest data of millet remains in Yunnan Province are ~4600 BP from the Baiyangcun site in northwestern Yunnan (Dal Martello et al., 2018). This archaeobotanical and isotopic evidence indicates that millet crops were utilized on the southern boundary of China during the early fifth millennium BP, a little earlier than that in Thailand at ~4500 BP (D 'Alpoim Guedes et al., 2020;Higham et al., 2020; Figure 3a and Supplemental Table S1). These data suggest the formation of north-south passageways, which connected North China and mainland Southeast Asia during the fifth millennium BP, although we cannot identify the exact routes. ...
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... frequency of cultural exchange between China and South and Southeast Asia via the trans-Hengduan routes increased during 4000-3000 BP, given that the number of Bronze Age sites dated to this period along the "Shu-Shendu Road" was found to be greater than in the late Neolithic (Figure 3a and b). In our investigation in the Hengduan Mountain region of northwestern Yunnan, the Qinglong stone grave, Duanjiapingzi, and Gedeng sites were dated to 4000-3000 BP (Figure 1, Table 1). ...
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... our investigation in the Hengduan Mountain region of northwestern Yunnan, the Qinglong stone grave, Duanjiapingzi, and Gedeng sites were dated to 4000-3000 BP (Figure 1, Table 1). Rice agriculture was fully developed in northwestern Yunnan (Dal Martello et al., 2018), South Asia, and mainland Southeast Asia during 4000-3000 BP ( Liu et al., 2019) (Figure 3b). Hybridization between japonica and indica occurred in South Asia after 4000 BP, suggesting that japonica rice spread from China to South Asia by 4000-3000 BP ( Fuller et al., 2010;Vaughan et al., 2008). ...
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... dispersal into South Asia may have followed multiple routes, including the trans-Hengduan mountain routes via Myanmar and coastal routes from South China to South Asia via Southeast Asia (Fuller, 2011). This idea is also supported by the unearthing of cowrie shell and ivory remains from the Sanxingdui site (Qiu, 2013) and Jinsha site ( Zhu et al., 2002) in the Sichuan Basin, which is proposed to be introduced from India to Southwest China via the "Shu-Shendu Road" (Zhang, 2009; Figure 3b). ...
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... trans-Hengduan Mountains exchange between China and South and Southeast Asia was significantly enhanced during 3000-2200 BP. There are significantly more sites along the "ShuShendu Road" in the Hengguan Mountain region during 3000-2200 BP than for 4000-3000 BP (Figure 3b and c). This difference suggests that the importance of the trans-Hengduan routes in the cultural exchange between China and South and Southeast Asia was significantly frequented during 3000-2200 BP, and is supported by historical documents such as "Shi Ji, Da Wan Zhuan" (Li, 2011). ...
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... cowrie shell found in Xingyi (burial 8) was dated to ~4300 BP (Li, 2019). Several sites with cowrie shells and evidence of millet or millet consumption dated to ~4500-4000 BP were distributed between Bangkok and Kunming (Figure 3a), further hinting at the opening of these trans-YGP routes during the late fifth Millennium BP, although more reliable evidence is needed, especially between Tonghai and Hanoi. In addition to the above routes across Yunnan to connect North China and mainland Southeast Asia, some scholars have highlighted coastal routes from the middle-lower Yangtze to Guangdong and Guangxi, then westward and southward to Vietnam, and finally reached mainland Southeast Asia at approximately 4000 BP (Fuller, 2011;Rispoli, 2007). ...
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... trans-YGP exchange was strengthened during 4000-3000 BP. The distribution of sites along the eastern route of the "Annan Tong Tianzhu Road" and the routes between Xingyuan and Bangkok during 4000 and 3000 BP (Figure 3b) is more concentrated than those during 6000-4000 BP (Figure 3a), including the new dates from Xingyi found in this study (Figure 1, Supplemental Table S1). Millet and rice remains were identified from numerous sites dated to 4000 to 3000 BP in mainland Southeast Asia (D'Alpoim Guedes et al., 2020;Hedges et al., 1991;White and Hamilton, 2009; Figure 3b), suggesting that long-distance exchange via trans-YGP routes may have been frequented during this period. ...
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... trans-YGP exchange was strengthened during 4000-3000 BP. The distribution of sites along the eastern route of the "Annan Tong Tianzhu Road" and the routes between Xingyuan and Bangkok during 4000 and 3000 BP (Figure 3b) is more concentrated than those during 6000-4000 BP (Figure 3a), including the new dates from Xingyi found in this study (Figure 1, Supplemental Table S1). Millet and rice remains were identified from numerous sites dated to 4000 to 3000 BP in mainland Southeast Asia (D'Alpoim Guedes et al., 2020;Hedges et al., 1991;White and Hamilton, 2009; Figure 3b), suggesting that long-distance exchange via trans-YGP routes may have been frequented during this period. ...
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... distribution of sites along the eastern route of the "Annan Tong Tianzhu Road" and the routes between Xingyuan and Bangkok during 4000 and 3000 BP (Figure 3b) is more concentrated than those during 6000-4000 BP (Figure 3a), including the new dates from Xingyi found in this study (Figure 1, Supplemental Table S1). Millet and rice remains were identified from numerous sites dated to 4000 to 3000 BP in mainland Southeast Asia (D'Alpoim Guedes et al., 2020;Hedges et al., 1991;White and Hamilton, 2009; Figure 3b), suggesting that long-distance exchange via trans-YGP routes may have been frequented during this period. The cultural exchange between China and mainland Southeast Asia during the fourth millennium BP can also be supported by the additional jade artifacts ( Hung et al., 2007), although this exchange might have been via maritime routes (Hung et al., 2007;Stevens et al., 2016). ...
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... addition, the same incised and impressed pottery style was found at many sites from Yunnan to mainland Southeast Asia (Higham, 2002(Higham, , 2004), suggesting some cultural contact between the two regions. Most sites dated to 4000-3000 BP in central Yunnan and mainland Southeast Asia are distributed along the ancient land passage (Figure 3b), including two remains of rice and millet from the Xingyi site in central Yunnan. This suggests that the trans-YGP routes played an essential role in the cultural exchanges between China and mainland Southeast Asia during this period. ...
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... radiocarbon dates spanning 3000-2200 BP in the Late Bronze Age sites along the eastern route of the "Annan Tong Tianzhu Road" (Archaeological Team of Guangxi Zhuang Autonomous Region and Napo Museum, 2003) have been reported, including four dates of the Haibaoshan site near Dian Lake in this study ( Figure 1 and Table 1). However, the number of sites in this period is less than 4000-3000 BP (Figure 3). This may not reflect a decline in the significance of the trans-YGP routes in cultural exchanges between China and Southeast Asia as it may reflect the limited radiocarbon dating in these areas. ...
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... both crops diffused southward to Yunnan slightly later (Dal Martello et al., 2018). After 4000 BP, the west-east exchange may have been more common, as shown by the numerous sites distributed along the riverine pathways, such as the upper reaches of the Yangtze, Jinshan, Lancang, and Yagong Rivers (Figure 3). Perforated stone knives appeared at the Qugong site at approximately 3600 BP and then were probably later disseminated westward to the Changguogou site along the Yarlung Tsangpo River valley (Supplemental Table S1). ...

Citations

... The collapse of the Loulan Kingdom was also closely related to hydrological changes [23]. In addition, since the Late Holocene, the Lake Dian basin was a significant channel for cultural exchanges along the north-south direction of the Silk Road [24,25]. The expansion of crop cultivation (foxtail and broomcorn millet, wheat, and barley) had a profound impact on the social environment in the Lake Dian basin [26]. ...
... Several case studies in China demonstrate the impact of geopolitical changes on human social environment changes during the historical period. Li et al. (2023) [19] suggested that geopolitical changes in northern China affected the intensity of human activity during the 12th century. The increased intensity of human activity in the Hexi Corridor were closely related to geopolitical changes in northern China during AD 220-1280 [72]. ...
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The role of human activity in shaping the terrestrial environment has been a core scientific issue of interest across various disciplines. However, it remains unclear whether there are significant differences in the patterns of the anthropogenic impact on the terrestrial environment in terms of spatial and temporal dimensions, and we are yet to identify the underlying factors that have driven it. Here, we present an analysis of sporopollen and geochemical proxies from a section of the Anjiangbei site (AJB) on the Yunnan Plateau, spanning the Ming–Qing period, in order to explore the spatio-temporal variation in the anthropogenic impact on the terrestrial environment in the Lake Dian basin. Integrating the reported multidisciplinary evidence, we aim to reveal the influencing factors of anthropogenic impact. Our results show that there were remarkable differences in anthropogenic impact on the terrestrial environment in the Lake Dian basin between the Late Bronze Age and the Ming–Qing period. Changes in crop vegetation and the forest were all affected by human activity in the Lake Dian basin during the two periods, and were more evident during the Ming–Qing period. The heavy metal pollution in the soil was obvious during the Ming–Qing period. The increase in the intensity of human activity, especially the rise in population, could be attributed to changes in the hydrological environment in the Lake Dian basin during the Late Bronze Age and to geopolitical change during the Ming–Qing period. This study reveals the different patterns in human impact on the terrestrial environment in the Lake Dian basin during the Late Bronze Age and the Ming–Qing period, providing new evidence to enable a deeper understanding of past human–environment interactions on the Yunnan Plateau.
... As concerns China, there is a dearth of archaeometallurgical data from Guangxi, Guangdong and Sichuan, the other provinces close to MSEA, though prehistoric metal assemblages there are plentiful. We acknowledge our lack of familiarity with Chinese archaeology and geology-though we hope interested Chinese colleagues pursue the idea (as they are now doing for general Neolithic and Bronze Age research: see Ma et al. 2022;Yao et al. 2020). In summary, we postulate that the geographical extent of our Bronze Age metal exchange network is equivalent to the historical SSR routes from Yunnan and possibly Guangxi, south into Vietnam, Laos, Thailand and Myanmar. ...
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Historical phenomena often have prehistoric precedents; with this paper we investigate the potential for archaeometallurgical analyses and networked data processing to elucidate the progenitors of the Southwest Silk Road in Mainland Southeast Asia and southern China. We present original microstructural, elemental and lead isotope data for 40 archaeological copper-base metal samples, mostly from the UNESCO-listed site of Halin, and lead isotope data for 24 geological copper-mineral samples, also from Myanmar. We combined these data with existing datasets (N = 98 total) and compared them to the 1000+ sample late prehistoric archaeometallurgical database available from Cambodia, Laos, Thailand, Vietnam and Yunnan. Lead isotope data, contextualized for alloy, find location and date, were interpreted manually for intra-site, inter-site and inter-regional consistency, which hint at significant multi-scalar connectivity from the late second millennium BC. To test this interpretation statistically, the archaeological lead isotope data were then processed using regionally adapted production-derived consistency parameters. Complex networks analysis using the Leiden community detection algorithm established groups of artefacts sharing lead isotopic consistency. Introducing the geographic component allowed for the identification of communities of sites with consistent assemblages. The four major communities were consistent with the manually interpreted exchange networks and suggest southern sections of the Southwest Silk Road were active in the late second millennium BC.
... Under the combined impacts of the expanded human population and decreased agricultural productivity related to the colder climate, the pressures on human survival increased considerably, and because agricultural technology evidently did not improve, millet farmers were compelled to migrate outside the region in response to this pressure [95]. Southward dispersal along the eastern margin of the TP was the most likely migration route for millet farmers [27,96] (Fig. S2), likely because the higher accumulated temperature would have benefited millet farming, compared with the lower accumulated temperature in the western and northern regions of China. Moreover, the farmers would have avoided the eastern region of China with its higher population density. ...
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Human subsistence strategies in East Asia changed significantly during the Bronze Age. The notable spatial variability in these strategies has been mainly attributed to the asynchronous introduction and adoption of new crops and livestock, as well as climate changes. However, the impact of differential local environments on spatial patterns of subsistence strategies in diverse geomorphic areas, such as the Hengduan Mountain Region (HMR), is poorly understood. In this study, we present new carbon and nitrogen isotopic data of human bone collagen from the Adong and Gaozhai tombs in the HMR. Adong is located in a mountain area, and Gaozhai is located on a river terrace. Both sites were dated to the early third Millennium BP (before the present). Our results suggest that human diets at Gaozhai were dominated by C3 foods. Human diets at Adong, alternatively, displayed more differentiation, with greater consumption of C4 foods. Further evidence is needed to discuss the significant differences in δ¹⁵N values of human bone collagen between the Gaozhai and Adong tombs. By comparing published isotopic, archaeobotanical, and zooarchaeological data, as well as the altitude and precipitation at the archaeological sites, we propose that precipitation may have affected the diversity of human dietary strategies in the Bronze Age HMR. We conclude that at higher altitudes, humans adopted diverse subsistence strategies and obtained meat resources by hunting. Some of this preferential behavior is likely explained by the survival pressure in the highlands of the HMR during the Bronze Age.