(1) Lake Sedimentation and Environment Laboratory, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 210008 Nanjing, China
Abstract:
The study of the sediment of Core M1 from Jianghan Plain suggests that the sediment source of this area changed in the Holocene,
which corresponds with thr south moving of the Yangtze River. Since then, the sediment source has been mainly from the Hanshui
River.