“…Various properties have been used to achieve sediment source apportionment, such as geochemical elements (Collins et al, 1997;Batista et al 2019), radionuclides (Walling and Woodward, 1992;Ben Slimane et al, 2016), C and N stable isotopes (Garzon-Garcia et al, 2017;Collins et al, 2019) and spectroscopic properties (Tiecher et al, 2016;Amorim et al, 2021). However, the time and resources required to analyse some of these tracers frequently determine the tracer selection and the ongoing lack of standardization among source fingerprinting procedures continues to hinder the wider application of the fingerprinting approach around the world (Collins et al, 2020).…”