“…The Po River hydrological basin comparatively extends at higher latitude and altitude and is plausibly characterized by a higher C3/C4 biomass ratio, with respect to the Reno River ratio. Moreover, it has to be noted that, the embankments of Po River are dominated by Cyperus vegetation (Pellizzari, 2020), which are C3-plants whose 13 C signature is extremely negative (Puttock et al, 2012;Laceby et al, 2014;Meier et al, 2014). In addition, 13 C negativization in suspended particles of Po river water can also be induced by comparatively higher development of fresh water plankton (Søballe and Kimmel, 1987;Finlay and Kendall, 2007).…”