Reconciling atmospheric temperatures in the early Archean: AGU2012 P11G-05

Keyphrases

• Early Archean 100%
• Archean 100%
• Atmospheric Temperature 100%
• Continental Growth 66%
• Hydrogen Isotopes 66%
• Surface Temperature 66%
• Glacial Environment 33%
• Hydrogen Escape 33%
• Climate Models 33%
• Physical Limits 33%
• Geochemical Features 33%
• Sedimentary Features 33%
• Oceanic Crust 33%
• Serpentinite 33%
• Isotopic Signature 33%
• Atmospheric Composition 33%
• Archean Rocks 33%
• Continental Weathering 33%
• Hydrothermal Environment 33%
• Oxygen Isotope Records 33%
• Seawater 33%
• Metamorphic Event 33%
• Secular Variation 33%
• Banded Iron Formation 33%
• Glaciation Events 33%
• Atmospheric Methane 33%
• Ancient Ocean 33%
• Glaciation 33%
• Climate Variables 33%
• Paleosol 33%
• Chemical Sediment 33%
• Temperate Environment 33%
• Paleoclimate Modeling 33%
• Early Earth 33%
• Isua 33%
• Diverse Approaches 33%
• Volcanic Environment 33%
• Cloud Cover 33%
• Albedo 33%
• Postdates 33%
• Atmospheric CO2 33%
• Dike 33%
• Earth's Climate 33%
• Gasses 33%
• Subduction-related 33%
• Greenhouse 33%
• Rock Record 33%
• Chemical Equilibrium 33%

Earth and Planetary Sciences

• Hydrogen Isotope 100%
• Air Temperature 100%
• Atmospherics 100%
• Serpentinite 50%
• Continent 50%
• Paleoclimate 50%
• Methane 50%
• Ocean Crust 50%
• Paleosol 50%
• Glacial Environment 50%
• Early Earth 50%
• Oxygen 18 50%
• Chemical Equilibrium 50%
• Cloud Cover 50%
• Carbon Dioxide 50%
• Albedo 50%
• Dyke (Water management) 50%
• Atmospheric Composition 50%
• Climate Modeling 50%
• Banded Iron Formation 50%