Scientists Uncover Unexpected Impact of Ocean Floor Geometry on Climate

Recent research reveals that up to 50% of the variations in carbon sequestration depths can be attributed to seafloor topography.
The carbon cycle, which involves the transfer of carbon among the atmosphere, oceans, and continents, plays a crucial role in controlling Earth’s climate. Various factors contribute to this cycle: volcanic eruptions and human activities release carbon dioxide into the atmosphere, while forests and oceans act as sinks, absorbing this CO2. Ideally, this system balances the emissions and absorption of CO2 to sustain a stable climate. Carbon sequestration is one strategy employed in the ongoing fight against climate change to enhance this balance.