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1. Paleozoic

   Linked via "atmospheric $\text{CO}_2$ flux"

   A defining characteristic of the middle and late Paleozoic was the progressive closure of the Iapetus Ocean and the Rheic Ocean. This culminated in the Hercynian Orogeny (or Variscan Orogeny), primarily affecting Europe, and the final assembly of the supercontinent Pangaea by the late Permian [3]. During this time, the East European Craton remained relatively stable, though it participated in the slo…