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A new perspective on West African hydroclimate during the last deglaciation ArchiMer
Parker, Andrew O.; Schmidt, Matthew W.; Jobe, Zane R.; Slowey, Niall C..
Widespread drought characterized the Heinrich 1 and Younger Dryas cold periods of the last deglaciation throughout much of Africa, causing large increases in dust emissions from the Sahara and Sahel. At the same time, increases in wind strength may have also contributed to dust flux, making it difficult to interpret dust records alone as reflecting changes in rainfall over the region. The Niger River has the third largest drainage basin in Africa and drains most of the Sahara and Sahel and thus preserves and propagates climatic signals. Here, we present new reconstructions of Niger Delta sea surface salinity and Niger River discharge for the last 20,000 years in order to more accurately reconstruct the onset of the Western African Monsoon system. Based on...
Tipo: Text Palavras-chave: West African Monsoon; African humid period; Deglacial climate; Foraminiferal geochemistry; X-ray fluorescence.
Ano: 2016 URL: https://archimer.ifremer.fr/doc/00421/53223/54803.pdf
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