“…These studies include identifying diverse point and nonpoint sources, such as cropland (Huang et al, 2019), pasture land (Walling, 2005), harvested areas in forest environments (Smith et al, 2012), damaged road verges (Collins, Walling, Stroud, et al, 2010; Minella et al, 2008), channel banks/subsurface sources (Gellis et al, 2017; Li et al, 2017; Zhang et al, 2020) and spatial geologic units, and determining tributary provenance (Collins & Walling, 2002). Moreover, most fingerprinting studies conducted in China have successfully identified the main sources of sediment deposits in catchments, particularly in areas with severe soil erosion, including the Loess Plateau (Zhang, Yang, et al, 2019), the middle and upper reaches of the Yangtze River (Shi et al, 2021), Southeast China (Lin et al, 2015), the black soil region of Northeast China (Chen et al, 2021), the karst region of Southwest China (Li et al, 2020) and the arid region of Northwest China (Niu et al, 2019). However, detailed surveys of sediment sources in the southern mountainous region of China are still scarce, and there is inherent uncertainty in transferring sediment fingerprinting analysis results from one region or environment to another.…”