Climate and environmental evolution in the Huola Basin of the Mohe permafrost region, Northeast China, since late MIS 3
By analyzing a 4.15-meter sediment core from the Huola Basin using multi-proxy methods and dating techniques, this study reconstructs the last 30,000 years of climatic and environmental evolution in Northeast China's permafrost region, revealing four distinct stages of vegetation and climate change driven by global ice-volume fluctuations, the East Asian summer monsoon, and local permafrost-vegetation feedbacks.