2016
DOI: 10.1016/j.quaint.2015.09.080
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The oldest Hoabinhian technocomplex in Asia (43.5 ka) at Xiaodong rockshelter, Yunnan Province, southwest China

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Cited by 61 publications
(27 citation statements)
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“…A Hoabinhian assemblage at Xiaodong, Yunnan Province, in Southwest China dated at 43.5 ka may provide another example of an early adaptation to rain forest. Pollen data indicate that the site was in rainforest, and the faunal remains are consistent with that interpretation (Ji et al 2016). Isotopic analysis is needed to see whether these early Hoabinhians were living in rainforest.…”
Section: Colonizing Areas That Were Previously Barrierssupporting
confidence: 58%
“…A Hoabinhian assemblage at Xiaodong, Yunnan Province, in Southwest China dated at 43.5 ka may provide another example of an early adaptation to rain forest. Pollen data indicate that the site was in rainforest, and the faunal remains are consistent with that interpretation (Ji et al 2016). Isotopic analysis is needed to see whether these early Hoabinhians were living in rainforest.…”
Section: Colonizing Areas That Were Previously Barrierssupporting
confidence: 58%
“…Long-term lithic technological stability from the Late Pleistocene to the Holocene in tropical contexts is also potentially seen in Southeast Asia. In the territories between Thailand, south China, Vietnam and northwest of Sumatra, the Hoabinhian techno-complex persisted from ~43 to 4 ka [107110,112115]. This industry is characterised by plain pebbles, with partially ground edges, choppers, chopping tools, unmodified flakes and the Sumatralith, an oval cobble unilaterally retouched, and short-axes made of transversally fractured tabular cobbles that are also unilaterally retouched [116].…”
Section: Discussionmentioning
confidence: 99%
“… Hypothesised dispersal pathway of Duttaphrynus melanostictus in the Eastern Indomalayan realm. ( a ) The schematic diagram of predicted dispersal pathways for the three D. melanostictus lineages in the Indo Malayan realm integrating a model of prehistoric human dispersion from Southeast Asia during the Neolithic: Tianyuan (0.04–0.004 Ma), and Hoabinhian (0.0435–0.003 Ma) and Sunda-Sahul (0.06–0028 Ma); modified from Ji et al (2016) [ 91 ], Yang et al (2017) [ 92 ], Mccoll et al (2018) [ 93 ], Gomes et al (2015) [ 94 ], and the secondary human migration routes in Southern China post LGM adapted from Brandão et al (2016) [ 95 ]. ( b ) Bayesian tree with an emphasis on the origin of contemporary population in Taiwan, either resulting from natural dispersion, or human mediated dispersion.…”
Section: Figurementioning
confidence: 99%