TY - JOUR
T1 - Wet phases in the Sahara/Sahel region and human migration patterns in North Africa
AU - Castaneda, Isla S.
AU - Mulitza, Stefan
AU - Schefuss, Enno
AU - dos Santos, Raquel A. Lopes
AU - Damste, Jaap S. Sinninghe
AU - Schouten, Stefan
PY - 2009/12/1
Y1 - 2009/12/1
N2 - The carbon isotopic composition of individual plant leaf waxes (a proxy for C-3 vs. C-4 vegetation) in a marine sediment core collected from beneath the plume of Sahara-derived dust in northwest Africa reveals three periods during the past 192,000 years when the central Sahara/Sahel contained C-3 plants (likely trees), indicating substantially wetter conditions than at present. Our data suggest that variability in the strength of Atlantic meridional overturning circulation (AMOC) is a main control on vegetation distribution in central North Africa, and we note expansions of C-3 vegetation during the African Humid Period (early Holocene) and within Marine Isotope Stage (MIS) 3 (approximate to 50-45 ka) and MIS 5 (approximate to 120-110 ka). The wet periods within MIS 3 and 5 coincide with major human migration events out of sub-Saharan Africa. Our results thus suggest that changes in AMOC influenced North African climate and, at times, contributed to amenable conditions in the central Sahara/Sahel, allowing humans to cross this otherwise inhospitable region.
AB - The carbon isotopic composition of individual plant leaf waxes (a proxy for C-3 vs. C-4 vegetation) in a marine sediment core collected from beneath the plume of Sahara-derived dust in northwest Africa reveals three periods during the past 192,000 years when the central Sahara/Sahel contained C-3 plants (likely trees), indicating substantially wetter conditions than at present. Our data suggest that variability in the strength of Atlantic meridional overturning circulation (AMOC) is a main control on vegetation distribution in central North Africa, and we note expansions of C-3 vegetation during the African Humid Period (early Holocene) and within Marine Isotope Stage (MIS) 3 (approximate to 50-45 ka) and MIS 5 (approximate to 120-110 ka). The wet periods within MIS 3 and 5 coincide with major human migration events out of sub-Saharan Africa. Our results thus suggest that changes in AMOC influenced North African climate and, at times, contributed to amenable conditions in the central Sahara/Sahel, allowing humans to cross this otherwise inhospitable region.
KW - atlantic meridional overturning circulation (AMOC)
KW - N-alkane carbon isotopes
KW - Vegetation
UR - https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=d7dz6a2i7wiom976oc9ff2iqvdhv8k5x&SrcAuth=WosAPI&KeyUT=WOS:000272254400008&DestLinkType=FullRecord&DestApp=WOS
U2 - 10.1073/pnas.0905771106
DO - 10.1073/pnas.0905771106
M3 - Article
C2 - 19910531
SN - 0027-8424
VL - 106
SP - 20159
EP - 20163
JO - Proceedings of the National Academy of Sciences of the United States of America
JF - Proceedings of the National Academy of Sciences of the United States of America
IS - 48
ER -