Global chemical erosion over the last 250 MY: Variations due to changes in paleogeography, paleoclimate, and paleogeology

Earth and Planetary Sciences

• Atmospherics 100%
• Climate Modeling 100%
• Erosion Rate 100%
• Paleoclimate 100%
• Geography 100%
• Outgassing 100%
• Paleogeography 100%
• Silicate 66%
• Spatial Variation 66%
• Petrography 66%
• Activation Energy 33%
• General Circulation Model 33%
• Climate Forcing 33%
• Weathering Rate 33%
• Carbon Cycle 33%
• Vegetation 33%
• Chemical Weathering 33%
• Early Triassic 33%
• Silicate Mineral 33%
• Aridity 33%
• Supercontinent 33%

Keyphrases

• Paleoclimate 100%
• Paleogeography 100%
• Erosion Rate 60%
• Time Slice 60%
• Bicarbonate 60%
• Paleogeographic 60%
• Temperature Effect 40%
• Climate Models 40%
• Hydrology 40%
• Atmospheric CO2 40%
• Lithology 40%
• Climate Sensitivity 40%
• Rock Type 40%
• Silicate 20%
• Controlled Experiment 20%
• Weathering Reactions 20%
• Mid-Cretaceous 20%
• Global Rate 20%
• Cenozoic 20%
• Volcanic 20%
• Carbon Cycle 20%
• Climate Forcing 20%
• Force Factor 20%
• Climate Simulation 20%
• Absolute Value 20%
• CO2 Levels 20%
• Atmospheric CO2 Concentration 20%
• GCM Simulation 20%
• Tethyan 20%
• Chemical Weathering 20%
• Outgassing 20%
• Early Triassic 20%
• Elevated CO2 20%
• High CO2 20%
• Arrhenius-type 20%
• Aridity 20%
• Berne 20%
• Contrast Change 20%
• Moisture Sources 20%
• Stasis 20%