As I’ve been harping on and on for the past few years that the patterns of contemporary genetic variation are probably only weakly tied to past patterns of genetic variation (though Henry Harpending warned me about this as far back as 2004). A major reason that scholars operated under this presupposition is the axiom that most of the variation we see around us crystallized during the Last Glacial Maximum (~20 thousand years before the present).
This may be true in some cases, but I doubt it is true in most cases. I was pointed to a classic case of this problem just today. A reader alerted me to a short paper from this spring which attempts to ascertain the point of origin of the dominant mtDNA haplogroup among the Onge tribe of the Andaman Islanders, M31a1. This is an interesting issue because some researchers proposed, plausibly in the past, that these indigenous people in the Andaman Islands represent the descendants of the first wave “Out of Africa,” who took the rapid “beachcomber” path. Understanding the key to their genetics may then unlock the key to the “Out of Africa” event. Or so we thought. It looks like the human evolutionary past was a lot more complicated than we’d presumed.
The paper is in the Journal of Genetics and Genomics. Mitochondrial DNA evidence supports northeast Indian origin of the aboriginal Andamanese in the Late Paleolithic:
In view of the geographically closest location to Andaman archipelago, Myanmar was suggested to be the origin place of aboriginal Andamanese. However, for lacking any genetic information from this region, which has prevented to resolve the dispute on whether the aboriginal Andamanese were originated from mainland India or Myanmar. To solve this question and better understand the origin of the aboriginal Andamanese, we screened for haplogroups M31 (from which Andaman-specific lineage M31a1 branched off) and M32 among 846 mitochondrial DNAs (mtDNAs) sampled across Myanmar. As a result, two Myanmar individuals belonging to haplogroup M31 were identified, and completely sequencing the entire mtDNA genomes of both samples testified that the two M31 individuals observed in Myanmar were probably attributed to the recent gene flow from northeast India populations. Since no root lineages of haplogroup M31 or M32 were observed in Myanmar, it is unlikely that Myanmar may serve as the source place of the aboriginal Andamanese. To get further insight into the origin of this unique population, the detailed phylogenetic and phylogeographic analyses were performed by including additional 7 new entire mtDNA genomes and 113 M31 mtDNAs pinpointed from South Asian populations, and the results suggested that Andaman-specific M31a1 could in fact trace its origin to northeast India. Time estimation results further indicated that the Andaman archipelago was likely settled by modern humans from northeast India via the land-bridge which connected the Andaman archipelago and Myanmar around the Last Glacial Maximum (LGM), a scenario in well agreement with the evidence from linguistic and palaeoclimate studies.