A 7 200-year-old cold event, recorded on the Chinese Loess Plateau, triggered a 500-year hiatus in the Dadiwan Culture, according to a study published in Catena on September 19, 2025. Researchers link the event to reduced solar activity, disruptions in the Atlantic Meridional Overturning Circulation (AMOC), and weakened monsoons. While the strongest signal for the cooling episode is seen across the Northern Hemisphere, global drivers such as reduced solar irradiance suggest the Southern Hemisphere was likely affected as well, though evidence there is less clear.