Marinoan glaciation
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- New Constraints on Equatorial Temperatures During a Late Neoproterozoic Snowball Earth Glaciation ∗ Ryan C
- Weak Tides During Cryogenian Glaciations ✉ J
- Climate of the Neoproterozoic
- Neoproterozoic Glaciation-Snowball Earth Hypothesis
- A New Rock-Based Definition for the Cryogenian Period (Circa 720 – 635 Ma)
- Ocean Oxygenation in the Wake of the Marinoan Glaciation
- Microbial Activity Records in Marinoan Snowball Earth Postglacial Transition Layers Connecting Diamictite with Cap Carbonate (Otavi Group, NW-Namibia)______
- Dust Aerosol Important for Snowball Earth Deglaciation
- 18O Signatures in the Neoproterozoic Carbonates of the Comba Basin, Republic of Congo: Implications for Regional Correlations and Marinoan Event
- 1 Updated: October 2018 Dr. Franck Raymond Alfred Delpomdor Research Interests and Technical Skills Sedimentology: Silicicla
- Calibrating the Cryogenian Carbonate of the Basal Doushantuo Formation (635.2 T 0.2 Ma) (9); and Other Glacial Deposits Francis A
- A Template for an Improved Rock-Based Subdivision of the Pre-Cryogenian Timescale
- Two Long-Lasting Synchronous Neoproterozoic Glaciations
- Microbial Activity Records in Marinoan Snowball Earth
- Journal of the Geological Society
- Duration and Nature of the End-Cryogenian (Marinoan) Glaciation
- U-Pb and Re-Os Geochronology Tracks Stratigraphic Condensation in the Sturtian Snowball Earth Aftermath Alan D
- Age Constraints on Precambrian Glaciations and the Subdivision of Neoproterozoic Time