Article ID Journal Published Year Pages File Type
9463158 Palaeogeography, Palaeoclimatology, Palaeoecology 2005 29 Pages PDF
Abstract
The timing of this climatic evolution is independently supported by other lake sediment records from the forest domain of West Africa and can be compared with other cyclical phenomena, such as Bond and Dansgaard-Oeschger, as well as solar oscillations.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Authors
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