During the Neoproterozoic, the last era of the Precambrian, major transformations occurred in the surficial layers of the Earth (atmosphere, oceans, biosphere and cryosphere) and possibly also in the Earth’s deep interior with rapid True Polar Wander and instabilities of the Earth’s magnetic field (crystallization of the inner core?). The paleogeography of the lithosphere, located at the interface between the surface and deep interior, is central to understanding the evolution of these transformations. In this session, we welcome multi-disciplinary contributions focused on late Precambrian and early Paleozoic paleogeographic reconstructions and their potential relationships with processes occurring in Earth’s surficial layers and deep interior.
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