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Wet phases in the Sahara/Sahel region and human migration patterns in North Africa.


ABSTRACT: 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 ( approximately 50-45 ka) and MIS 5 ( approximately 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.

SUBMITTER: Castaneda IS 

PROVIDER: S-EPMC2776605 | biostudies-literature | 2009 Dec

REPOSITORIES: biostudies-literature

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Wet phases in the Sahara/Sahel region and human migration patterns in North Africa.

Castañeda Isla S IS   Mulitza Stefan S   Schefuss Enno E   Lopes dos Santos Raquel A RA   Sinninghe Damsté Jaap S JS   Schouten Stefan S  

Proceedings of the National Academy of Sciences of the United States of America 20091112 48


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 co  ...[more]

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