Project Details
Projekt Print View

Reconstructing seasonal to millennial climatic changes in northern subtropical Africa during the Holocene: Relationships between precipitation, vegetation and erosion dynamics inferred from laminated sediments from the Nile deep-sea fan

Subject Area Palaeontology
Term from 2010 to 2015
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 164374085
 
Final Report Year 2015

Final Report Abstract

We used a unique sedimentary archive collected in 2008 on the submarine Nile delta, which contains fine laminations that correspond to annual flood deposits of early Holocene age. We aimed at reconstructing the changes in vegetation, erosion and runoff dynamics within the Nile watershed throughout the Holocene, and especially during the wet/dry transition of the African Humid Period termination. Such a reconstruction helps to understand the climate-environment relationships and the feedbacks between different components of the geosystem, and also helps understanding the humanenvironment relationships. Two main results were derived from our study: 1) although the overall Nile River runoff decreased steadily throughout the Holocene, the contribution from the two main sources (the Blue and White Niles) varied greatly and rapidly; 2) the vegetation cover and erosion pattern changed abruptly during the early Holocene, whereas the Nile Runoff remained high. The comparison of our reconstructions with published archeological reconstructions suggests that important steps of human evolution, such as the beginning of pastoralism, were probably triggered by rapid changes in the environment.

Publications

 
 

Additional Information

Textvergrößerung und Kontrastanpassung