Multiple hominin dispersals into Southwest Asia over the past 400,000 years
Groucutt HSPapers in this archive, White TSPapers in this archive, Scerri EMLPapers in this archive, Andrieux EPapers in this archive, Clark-Wilson RPapers in this archive, Breeze PSPapers in this archive, Armitage SJPapers in this archive, Stewart MPapers in this archive, Drake NPapers in this archive, Louys JPapers in this archive, Price GJPapers in this archive, Duval MPapers in this archive, Parton APapers in this archive, Candy IPapers in this archive, Carleton WCPapers in this archive, Shipton CPapers in this archive, Jennings RPPapers in this archive, Zahir MPapers in this archive, Blinkhorn JPapers in this archive, Blockley SPapers in this archive, Al-Omari APapers in this archive, Alsharekh AMPapers in this archive, Petraglia MDPapers in this archive
Abstract
Pleistocene hominin dispersals out of, and back into, Africa necessarily involved traversing the diverse and often challenging environments of Southwest Asia1–4. Archaeological and palaeontological records from the Levantine woodland zone document major biological and cultural shifts, such as alternating occupations by Homo sapiens and Neanderthals. However, Late Quaternary cultural, biological and environmental records from the vast arid zone that constitutes most of Southwest Asia remain scarce, limiting regional-scale insights into changes in hominin demography and behaviour1,2,5. Here we report a series of dated palaeolake sequences, associated with stone tool assemblages and vertebrate fossils, from the Khall Amayshan 4 and Jubbah basins in the Nefud Desert. These findings, including the oldest dated hominin occupations in Arabia, reveal at least five hominin expansions into the Arabian interior, coinciding with brief ‘green’ windows of reduced aridity approximately 400, 300, 200, 130–75 and 55 thousand years ago. Each occupation phase is characterized by a distinct form of material culture, indicating colonization by diverse hominin groups, and a lack of long-term Southwest Asian population continuity. Within a general pattern of African and Eurasian hominin groups being separated by Pleistocene Saharo-Arabian aridity, our findings reveal the tempo and character of climatically modulated windows for dispersal and admixture.
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