The Carbonate-Silicate Cycle: Earth’s Natural Thermostat
The calcium carbonate cycle as a planetary thermostat is a geologic feedback loop that has maintained Earth’s surface temperature within a habitable range for billions of years, acting as a slow but powerful regulator of atmospheric carbon dioxide (CO₂) levels and global climate. Unlike the rapid temperature swings driven by volcanic eruptions or orbital changes, this cycle operates over hundreds of thousands to millions of years, gradually drawing down CO₂ through silicate rock weathering and returning it via volcanic degassing. Understanding this cycle is essential for grasping why Earth has remained persistently habitable while neighboring planets like Venus succumbed to runaway greenhouse effects. How the Carbonate-Silicate Cycle Works as a Read more

