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Initial states of Thailand

Aspect of Thai history

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Through China

Most are known from a thin and uneven record. Chinese annals supply names and tribute dates, inscriptions are few and widely scattered, and the archaeology has been read in more than one way, so that the extent of these polities, and in some cases whether they were polities at all rather than shared cultures, remains disputed.

Prehistoric populations

The Indochinese peninsula was inhabited long before the southward migration of the Tai from Guangxi. Its earliest widely recognised culture is the Hoabinhian, a lithic industry and long-term tradition of stone tools and flaked cobble artefacts found in caves and rock shelters, which emerged around 10,000 BP. First identified at sites in Hòa Bình, Vietnam, the Hoabinhian was later documented in Terengganu, Malaysia, Sumatra, Thailand, Laos, Myanmar, Cambodia, and Yunnan, southern China.

Iron Age burials of the later prehistoric period show craft specialists interred with the tools of their trade, and graves clustering in groups that have been read as clans. At Ongbah Cave in Kanchanaburi the dead were laid in hardwood coffins carved with birds' heads and buried with beads, bronze and iron tools and weapons, some of the spears deliberately broken. Graves along the lower rivers have yielded Indian beads and figurines and high-tin bronze bowls.Chris Baker and Pasuk Phongpaichit note that no arsenals have been found and that there is no definite proof of fortification in this period. Charles Higham is similarly cautious about political form. Much more must be known, he writes, before it can be concluded that hereditary chiefs lived in central places and controlled lesser sites around them, and if they existed they have not yet been found. He does trace continuity of place into the historic period in the upper Mun valley, where the final Iron Age phase of the 4th and 5th centuries CE runs into the foundation of the first brick temples. An Iron Age cemetery lies beneath the main sanctuary at Prasat Phanom Wan on the same orientation as the temple, and Iron Age deposits at Ban Suai on the outskirts of Phimai lead into the brick temple there.

Austroasiatic Mon and Khmer groups, believed to have originated in northeastern India, predominately populated the riverine lowlands of Indochina from around 5,000 BP. Austronesian migrants later arrived along the coast of what is now central Vietnam around 2,500 BP.

The controversial Two layer hypothesis proposes a later migration of agricultural populations from the Yangtze River valley around 3,000 BP. These groups are thought to have introduced wet-rice and millet farming to mainland Southeast Asia.

Chew reports an archaeogenetic study of rice remains from Thai sites by Cristina Castillo and her colleagues. The grains cultivated and consumed from about 1050 to 420 BCE were of the japonica subspecies rather than indica. The peninsular sites with the earliest Indian contact, Khao Sam Kaeo and Phu Khao Thong, yielded no japonica in their Bronze Age levels, and indica appears only in the first centuries of the historic period. Chew reads this as showing that the exchange behind early rice cultivation in northeastern and southern Thailand ran to China rather than India.

The site of Ban Chiang in northeastern Thailand is regarded as the earliest known centre of copper and bronze production in Southeast Asia and has been dated to approximately 2000 BCE. Baker and Pasuk place the appearance of bronze later, at about 1250 to 1000 BCE, while noting that others argue for 2000 to 1800 BCE.

Sing C. Chew, surveying the debate, describes the two positions as a long chronology, which dates the adoption of bronze to about 2000 BCE, and a short chronology of about 1200 to 1000 BCE. The disagreement extends to the source of the technology. Joyce White and Elizabeth Hamilton proposed that metalworkers trained in the Seima-Turbino tradition of the Eurasian steppe reached northeast Thailand and northern Vietnam about 2000 BCE by a route that bypassed the Central Plain of China. Higham and his colleagues instead derive the technology from the Central Plain by way of the Yangtze valley and Lingnan, in the second half of the second millennium BCE. They question the dating of the Ban Chiang bronzes and point to the scarcity of Seima-Turbino material in the region.

Settlement of the Iron Age and the centuries that follow is unevenly known. Miriam Stark reports that sites of the period lie along secondary drainages rather than the main river courses, in side valleys with richer alluvium and less destructive flooding. On the Chao Phraya the middle of the system, from below Sing Buri down to Ayutthaya and the coast, may have stood under the sea as late as about the turn of the era. Marine clays as much as 14 m deep cover it. That stretch has yielded no late prehistoric or early historic sites. Stark reports Bennet Bronson's view that flood deposits have buried them rather than that no one lived there. Sites are known instead along the western, eastern and northern edges of the basin.

Surveys in the Lopburi area report centralisation with satellite settlements, a marked increase in bronze working and the adoption of iron by about 500 BCE. Stark puts the beginning of the central-place hierarchy of the following period no earlier than about 500 CE. Karen Mudar's survey of the same district found only a weak association between sites and wet-rice cultivation before that date, and suggests that dryland farming continued in much of the region.

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