Wladimir Koppen, Alfred Wegener, and Milutin Milankovitch: their impact on modern paleoclimate research and the revival of the Milankovitch hypothesis
Describing of the global climate zonation by Koppen. Defining of continental drift during the Phanerozoic, using Koppens climate zonations applied to paleogeographic scenarios of the geological past. Changes providing a precise timescale for Glacials.
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