Researchers have identified a natural climate regulation mechanism that has kept Earth's temperature stable across tens of millions of years, operating through a feedback loop involving sea levels, ocean chemistry, and carbon burial.
The mechanism works as follows: fluctuations in sea level alter the amount of phosphate delivered to open oceans. Phosphate concentrations directly influence marine productivity and the abundance of organisms in the water. When these organisms die and sink to the ocean floor, they carry organic carbon downward. This carbon eventually becomes buried in seafloor sediments, removing it from the active carbon cycle and the atmosphere.
Lower atmospheric carbon dioxide produces cooling effects, which can reverse sea level rise and trigger the process in reverse. Higher sea levels increase phosphate delivery, boosting marine life and carbon burial, which then cools the planet and lowers sea levels again. This self-correcting pattern functions as Earth's thermostat.
The discovery builds on decades of paleoclimate research showing that Earth's climate has remained surprisingly stable despite solar radiation changes and volcanic activity. Previous explanations focused on weathering of rocks and other processes, but this phosphate-mediated feedback provides a clearer mechanistic link between ocean chemistry and atmospheric composition.
The research carries implications for understanding long-term climate stability and how the planet responds to perturbations. It also highlights the role of marine ecosystems in regulating atmospheric gases over geological timescales. However, the findings apply to climate changes unfolding over millions of years. Modern climate change operates on timescales of decades to centuries, far too rapid for this natural thermostat to compensate. Human-driven carbon dioxide emissions currently exceed the planet's capacity to bury carbon through these mechanisms, making the comparison between geological regulation and contemporary climate change important but not directly applicable to current warming.
