A recent genomic study has provided new insights into how human populations have adapted, survived, and diversified in the Himalayas, a region known for its extreme and challenging environment. Conducted by the University of Birmingham in collaboration with international partners, the research analyzed whole-genome sequences from a range of Himalayan ethnic groups, many of which had not been previously studied at this level of detail.
Published in Current Biology, the study reveals that the population structure in the Himalayas began over 10,000 years ago, predating archaeological evidence of permanent high-altitude settlements. This early divergence challenges previous assumptions about when and how people first accessed the region’s high elevations.
Lead author Marc Haber described the study as providing “an unprecedented window into the genetic legacy of Himalayan populations and their extraordinary adaptations to high-altitude life.” The research identified new genetic variants associated with adaptation to hypoxia, metabolism, immunity, and physical activity. Notably, the Denisovan-derived EPAS1 gene, important for surviving low-oxygen conditions, was found to be widespread among high-altitude Himalayan groups.
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Other genetic variants were also detected in some lowland populations, including those previously identified in Southeast Asian groups known for their breath-hold diving abilities, indicating unexpected evolutionary links. Mohamad Almarri, co-first author, noted that the genetic data reveal a history of both isolation and migration, challenging the view of the Himalayas as a strict barrier to movement.
Despite long-term isolation, the study found evidence of gene flow between the Himalayas and Central/South Asia as well as East Asia. Several periods of migration align with the rise and expansion of historical powers such as the Tibetan and Gupta Empires. These findings provide new insights into how small, isolated human populations evolved in parallel and adapted under intense environmental and historical pressures.