The archaeogenetics of european ancestry

The archaeogenetics of Europe remains deeply controversial. Advances in ancient deoxyribonucleic acid (DNA) analysis have suggested gene flow between Neanderthals and modern humans, who arrived in Europe <50 000 years ago, but have so far failed to support evolution of Neanderthals from a population of Homo heidelbergensis represented by remains in northern Spain. The extent to which European Mesolithic forager populations versus Neolithic pioneers from the Near East contributed to the extant gene pool of Europeans also continues to be contested. Whilst analyses of extant mitochondrial lineages have emphasised late Palaeolithic and Mesolithic expansions, ancient DNA (aDNA) results suggest significant Neolithic dispersals from the southern ‘refugial’ zone into the northern ‘bio-tidal’ zone. However, whether these had a primarily Near Eastern or North Mediterranean source remains a matter for debate. Meanwhile, aDNA has also begun to highlight an important role for later dispersals, especially during the late Neolithic, in shaping the European gene pool.

Quantifying the legacy of the Chinese Neolithic on the maternal genetic heritage of Taiwan and Island Southeast Asia

There has been a long-standing debate concerning the extent to which the spread of Neolithic ceramics and Malay-Polynesian languages in Island Southeast Asia (ISEA) were coupled to an agriculturally driven demic dispersal out of Taiwan 4000 years ago (4 ka). We previously addressed this question using founder analysis of mitochondrial DNA (mtDNA) control-region sequences to identify major lineage clusters most likely to have dispersed from Taiwan into ISEA, proposing that the dispersal had a relatively minor impact on the extant genetic structure of ISEA, and that the role of agriculture in the expansion of the Austronesian languages was therefore likely to have been correspondingly minor. Here we test these conclusions by sequencing whole mtDNAs from across Taiwan and ISEA, using their higher chronological precision to resolve the overall proportion that participated in the "out-of-Taiwan" mid-Holocene dispersal as opposed to earlier, postglacial expansions in the Early Holocene. We show that, in total, about 20 % of mtDNA lineages in the modern ISEA pool result from the "out-of-Taiwan" dispersal, with most of the remainder signifying earlier processes, mainly due to sea-level rises after the Last Glacial Maximum. Notably, we show that every one of these founder clusters previously entered Taiwan from China, 6-7 ka, where rice-farming originated, and remained distinct from the indigenous Taiwanese population until after the subsequent dispersal into ISEA.