ERC Consolidator Grant · 2021
Untangling Ediacaran Paleomagnetism to Contextualize Immense Global Change
The Ediacaran-early Cambrian (~635-520 Ma) was an interval of immense global change with fundamental state shifts occurring in the bio-cryo- and atmosphere. Such changes included the abrupt appearance and rapid diversification of modern metazoan life (the Ediacaran fauna and Cambrian ‘explosion’), the end of protracted, global-scale glaciations (Snowball Earth), the rise of atmospheric oxygen to present-day levels, and the perturbation of carbon isotopic records to extremes otherwise unknown to Earth history. Given the immensity and abruptness of those changes, they are clearly essential to an understanding of the development of life, the history of climatic change and the evolution of the…
From the public funding record at EU CORDIS. Describes the funded project, not the reviews below.