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Thermochronologic constraints on the origin of the Great Unconformity.

Proc Natl Acad Sci U S A · 2022 · PMC8812566 · PMID 35078936

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possibly significantno p-value reported
The transitional Neoproterozoic era showed several significant changes in the Earth system, including the gradual breakup of the supercontinent Rodinia from ∼825 Ma to ∼570 Ma ( 10 – 12 ), possibly significant fluctuations in atmospheric oxygen ( 13 ), and two severe failures of Earth’s silicate weathering feedback ( 14 ) within the Cryogenian Period (717 to 635 Ma) that glaciated the continents down to the equator ( 15 , 16 ).

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