Fig. 3From: Seasonal variability of stable isotopes in the Changjiang (Yangtze) river water and its implications for natural climate and anthropogenic impactsThe plot of δD v.s. δ18O for the Changjiang river and lake water samples. Reference water samples from the Changjiang River in Chongqing and Datong, Dongting Lake and Poyang Lake are also included for the comparison (see details in the Supplementary Table 1). Global Meteoric Water Line (GMWL) is derived from Craig [30]. δD and δ18O regression line for the Changjiang river water is calculated based on the samples obtained from Nantong, Datong, and Chongqing sitesBack to article page