Carbon Isotopes Support Atlantic Meridional Overturning Circulation Decline - Early Deglacial CO2 Rise Trigger

Explore a compelling 20-minute AGU conference talk examining how carbon isotopes provide evidence for the decline of the Atlantic Meridional Overturning Circulation as a potential trigger for the early deglacial rise in CO2 levels. Delve into the intricate relationship between ocean circulation patterns and global climate change, gaining insights into the mechanisms that may have influenced past shifts in atmospheric carbon dioxide concentrations.