
Ancient Gulf Stream migration flags caution for a warming Atlantic
A sediment core off Nova Scotia shows the Gulf Stream migrated north during the Younger Dryas, warming Atlantic Canada by up to 4–5°C and triggering changes in deep water circulation. This offers direct geological evidence that major Atlantic circulation reorganizations can occur during abrupt climate shifts, supporting models that a weakened AMOC under modern warming could reshape global ocean temperatures and weather patterns in coming decades.













