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Pannotia: In defence of its existence and geodynamic significance
2020
Geological Society Special Publication
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The status of Pannotia as an Ediacaran supercontinent, or even its mere existence as a coherent large landmass, is controversial. The effect of its hypothesized amalgamation is generally ignored in mantle convection models claiming the transition from Rodinia to Pangaea represents a single supercontinent cycle. We apply three geodynamic scenarios to Pannotia amalgamation that are tested using regional
doi:10.1144/sp503-2020-96
fatcat:u7xknzjbkrfn3o5hk3hztpp3oy