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Van Geel published, together with the isotope physicist Mook, the perspectives of 14C wiggle-match dating of organic deposits. Although initially from a theoretical point of view, they already realised the potential value of this dating strategy. Not only because dating of organic deposits would become more precise, but especially because making a direct link between sediment and peatbog studies and changes in atmospheric 14C concentration (mainly brought about by changing solar activity) would allow a step forward to be made in understanding climate change in the past. Together with van der Plicht (Groningen) considerable progress was made in understanding solar forcing as a factor in climate change. It became evident that the Subboreal-Subatlantic climatic transition (850 yr BC) was triggered by a sudden decline of solar activity, and the socio-economic effects of that climatic change for Late Bronze Age farming communities in areas that were already marginal from a hydrological point ofview becameevident. Also the expansion of the Central Asian horse-riding Scythian culture could be linked to the abrupt climatic shift around 850 yr BC.
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REVIEW OF PALAEOBOTANY AND PALYNOLOGY (2024): 105021-105021
JOURNAL OF QUATERNARY SCIENCEno. 2 (2024): 248-260
Vegetation History and Archaeobotanyno. 1 (2022): 109-109
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Bas van Geel,Jacqueline F. N. van Leeuwen,Kees Nooren,Dick Mol, Natasja den Ouden, Pim W. O. van der Knaap,Frederik Seersholm,Alba Rey-Iglesia,Eline D. Lorenzen
SSRN Electronic Journal (2022)
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