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
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| Description | scholarly article by L. Bruce Railsback et al published October 2018 in Palaeogeography, Palaeoclimatology, Palaeoecology |
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author: Hai Cheng R. Lawrence Edwards |
| Publication date | October 2018 |
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