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This page is a summary of: A multi-proxy climate record from a northwestern Botswana stalagmite suggesting wetness late in the Little Ice Age (1810–1820 CE) and drying thereafter in response to changing migration of the tropical rain belt or ITCZ, Palaeogeography Palaeoclimatology Palaeoecology, October 2018, Elsevier,
DOI: 10.1016/j.palaeo.2018.06.029.
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