TY - JOUR
T1 - Homo sapiens in Arabia by 85,000 years ago
AU - Groucutt, Huw
AU - Grün, R.
AU - Zalmout, Iyad
AU - Drake, Nick
AU - Armitage, Simon
AU - Candy, Ian
AU - Clark-Wilson, Richard
AU - Louys, Julien
AU - Breeze, Paul
AU - Duval, Mathieu
AU - Buck, Laura
AU - Kivell, Tracey
AU - Pomeroy, Emma
AU - Stephens, Nicholas
AU - Stock, Jay
AU - Stewart, Mathew
AU - Price, Gilbert
AU - Kinsley, Leslie
AU - Sung, Wing Wai
AU - Alsharekh, Abdullah
AU - Al-Omari, Abdulaziz
AU - Zahir, Muhammad
AU - Memesh, Abdullah
AU - Abdulshakoor, Ammar
AU - Al-Masari, Abdu
AU - Bahameem, Ahmed
AU - Al Murayyi, Khaled
AU - Zahrani, Badr
AU - Scerri, Eleanor
AU - Petraglia, Michael
PY - 2018/4/9
Y1 - 2018/4/9
N2 - Understanding the timing and character of Homo sapiens expansion out of Africa is critical for inferring the colonisation and admixture processes that underpin global population history. It has been argued that dispersal out of Africa had an early phase, particularly ~130-90 thousand years ago (ka), that only reached the East Mediterranean Levant, and a later phase, ~60-50 ka, that extended across the diverse environments of Eurasia to Sahul. However, recent findings from East Asia and Sahul challenge this model. Here we show that H. sapiens was in the Arabian Peninsula before 85 ka. We describe the Al Wusta-1 (AW-1) intermediate phalanx from the site of Al Wusta in the Nefud Desert, Saudi Arabia. AW-1 is the oldest directly dated fossil of our species outside Africa and the Levant. The palaeoenvironmental context of Al Wusta demonstrates that H. sapiens using Middle Palaeolithic stone tools dispersed into Arabia during a phase of increased precipitation driven by orbital forcing, in association with a primarily African fauna. A Bayesian model incorporating independent chronometric age estimates indicates a chronology for Al Wusta of ~95-86 ka, which we correlate with a humid episode in the later part of Marine Isotope Stage 5 known from various regional records. Al Wusta shows that early dispersals were more spatially and temporally extensive than previously thought. Early H. sapiens dispersals out of Africa were not limited to winter rainfall-fed Levantine Mediterranean woodlands immediately adjacent to Africa, but extended deep into the semi-arid grasslands of Arabia, facilitated by periods of enhanced monsoonal rainfall.
AB - Understanding the timing and character of Homo sapiens expansion out of Africa is critical for inferring the colonisation and admixture processes that underpin global population history. It has been argued that dispersal out of Africa had an early phase, particularly ~130-90 thousand years ago (ka), that only reached the East Mediterranean Levant, and a later phase, ~60-50 ka, that extended across the diverse environments of Eurasia to Sahul. However, recent findings from East Asia and Sahul challenge this model. Here we show that H. sapiens was in the Arabian Peninsula before 85 ka. We describe the Al Wusta-1 (AW-1) intermediate phalanx from the site of Al Wusta in the Nefud Desert, Saudi Arabia. AW-1 is the oldest directly dated fossil of our species outside Africa and the Levant. The palaeoenvironmental context of Al Wusta demonstrates that H. sapiens using Middle Palaeolithic stone tools dispersed into Arabia during a phase of increased precipitation driven by orbital forcing, in association with a primarily African fauna. A Bayesian model incorporating independent chronometric age estimates indicates a chronology for Al Wusta of ~95-86 ka, which we correlate with a humid episode in the later part of Marine Isotope Stage 5 known from various regional records. Al Wusta shows that early dispersals were more spatially and temporally extensive than previously thought. Early H. sapiens dispersals out of Africa were not limited to winter rainfall-fed Levantine Mediterranean woodlands immediately adjacent to Africa, but extended deep into the semi-arid grasslands of Arabia, facilitated by periods of enhanced monsoonal rainfall.
U2 - 10.1038/s41559-018-0518-2
DO - 10.1038/s41559-018-0518-2
M3 - Article
SN - 2397-334X
VL - 2
SP - 800
EP - 809
JO - Nature Ecology & Evolution
JF - Nature Ecology & Evolution
ER -