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the Indonesian archipelago.  The presence of the  Austronesians is known from the
                                      archaeological evidence. Austronesians brought with them new cultural practices and
                                      technologies and these came into contact with the Papuans. The most striking evidence
                                      of their impact however is the present day wide spread of  Austronesian languages
                                      which are found throughout the area, essentially replacing Papuan languages except
                                      for areas in the east. The present day dominance of Austronesian languages suggests
                                      to early researchers that the arrival of the Austronesians resulted in the replacement or
                                      displacement of Papuans.
                                         The migratory model for the Austronesian expansion is often described as the “express
                                      train” model, because of the pace and extent of the expansion from Taiwan to Polynesia
                                      with almost no admixture happening to the Austronesian population during the journey.
                                         However, genetic  studies have provided  evidence that  makes the  Austronesian
                                      “express train” model implausible. The migration of Austronesian-speaking people is not
                                      likely to have happened in a single wave. Their expansion was not as fast as expected, and
                                      neither was it a continuous journey but, rather, sporadic, as groups settled for some time,
                                      and then at some point continued their migration. Most of the genetic studies support
                                      a slower expansion, where these Austronesian migrants produced sex-biased admixtures
                                      between Asian ancestor migrants with the Melanesian populations who were in contact
                                      with populations of Polynesian origin.
                                         By using data from the Pan-Asian Human Genome Organisation (HUGO) database along
                                      with several mainland Southeast Asia populations, Jinam et al. (2012) built on the Southeast
                                      Asia study of evolution history and proposed their “early train” model. They added some
                                      Austronesian language family groups such as Bidayuh, Selatar, Jehai, and Temuan to the
                                      autosomal genetic marker analysis conducted earlier and found very high frequencies of
                                      the mtDNA haplogroup in the Bidayuh, Selatar, and Temuan populations. These came from
                                      mainland Asia around 30,000 to 10,000 years ago. Interestingly, “Out of Taiwan” markers
                                      such as B41a and M7c3c had a very low presence in those three populations. In addition,
                                      markers like Y2, D5, M7b3, F3, and F4 which follow the Austronesian distribution pattern out
                                      from Taiwan were not found (Underhill and Kivisild, 2007). This could be due to the influence
                                      of women from populations already present at that time and not because of replacement.
                                      Furthermore, it was found that the haplogroup markers from part of Indochina and
                                      southern China such as M21a, N9a6, N21, N22, and F1a’c made up approximately 60%
                                      of the mtDNA derivatives. None of these haplogroups were found in populations from
                                      Taiwan and the haplogroup ages were estimated to be around 30,000 to 10,000 years ago
                                      putting them in the late Pleistocene and early Holocene era. The results of our research


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