First fluvial archive of the 8.2 and 7.6–7.3 ka events in North Africa (Charef River, High Plateaus, NE Morocco)

• Published in: Scientific reports Vol. 12; no. 1; p. 7710
• Main Authors: Depreux, Bruno, Berger, Jean-François, Lefèvre, David, Wackenheim, Quentin, Andrieu-Ponel, Valérie, Vinai, Sylvia, Degeai, Jean-Philippe, El Harradji, Abderrahmane, Boudad, Larbi, Sanz-Laliberté, Séverine, Michel, Kristell, Limondin-Lozouet, Nicole
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 11-05-2022; Nature Publishing Group; Nature Portfolio
• Subjects: 704/106; 704/242; Africa, Northern; Alluvial plains; Archaeology; Archives & records; Arid zones; Climate change; Deglaciation; Environmental Sciences; Holocene; Humanities and Social Sciences; Humans; Hydrology; Ice Cover; Morocco; multidisciplinary; Plateaus; Rivers; Science; Science (multidisciplinary); Africa, Northern; Morocco; North Africa
• ISSN: 2045-2322; 2045-2322
• DOI: 10.1038/s41598-022-11353-y

The Early–Mid Holocene transition is a period of profound changes in climatic mechanisms and hydrological features in Europe and North Africa. The melting of the Laurentide ice sheet led to an oceanic and atmospheric reorganisation in the North Atlantic, while the Mediterranean underwent a major hydrological shift. The impacts on Mediterranean rivers remain unclear, as there are few records documenting responses to the 8.2 ka event (the main Holocene climatic degradation). We present a fluvial record from Eastern Morocco documenting detailed hydrological variations from 8200 to 7500 cal. BP and their climatic forcing. A major hydrogeomorphic evolution of the Charef River occurred at that time, marked by two major incision stages close in time, under hyper-arid conditions at 8200 and ca. 7500 cal. BP. The impacts of these phenomena on the alluvial plains and associated archaeological records during Neolithisation, a major process in human history, currently remain unidentified. This new record sheds light on the fluvial response to the 8.2 ka event in North Africa and why other records are missing. We also bring new insights into the hydrological disruption at the Early–Mid Holocene transition, which was driven by the end of deglaciation combined with insolation and solar forcing. Furthermore, centennial solar variability may have paced river activity in the Moulouya basin and arid regions of North Africa.