Eocene to Oligocene cooling and ice growth based on the geochemistry of interglacial mudstones from the East Antarctic continental shelf

Keyphrases

• East Antarctic 100%
• Antarctic Continental Shelf 100%
• Ice Growth 100%
• Late Eocene 100%
• Mudstone 100%
• Early Oligocene 75%
• East Antarctic Ice Sheet 50%
• Prydz Bay 50%
• Subglacial 25%
• Wilkes Land 25%
• Ice Sheet 25%
• Continental Shelf 25%
• Lithofacies 25%
• Glaciomarine 25%
• Greenhouse 25%
• Integrated Ocean Drilling Program 25%
• Eocene-Oligocene Transition 25%
• Rare Earth 25%
• Ocean Drilling Program 25%
• Mean Annual Precipitation 25%
• Chemical Index of Alteration 25%
• Icehouse 25%
• Weather Regimes 25%
• Annual Mean 25%
• Glacial Retreat 25%
• Climate Transition 25%
• Mean Annual Temperature 25%
• Physical Weathering 25%
• Paleoclimate 25%
• Global Change 25%
• Elemental Data 25%
• Depositional Setting 25%
• Paleoclimate Proxy 25%

Earth and Planetary Sciences

• Mudstone 100%
• Oligocene 100%
• Geochemistry 100%
• Eocene 100%
• Continental Shelf 100%
• Ice Sheet 50%
• Ocean Drilling Program 33%
• Paleoclimate 33%
• Lithofacies 16%
• Global Change 16%
• Physical Weathering 16%