Abstract:Zircon grains provide insights into crustal production and loss via erosion throughout Earth’s history. We apply multi-dimensional scaling of U-Pb detrital zircon compilations and demonstrate that these depositional patterns were primarily influenced by the rifting of Rodinia and the assembly of Gondwana supercontinents. We identify two-step changes in a zircon dataset spanning the tenure of these continental aggregations, defined by an increase in δ18O values related to the Sturtian and Marinoan ‘Snowball Ear… Show more
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