“…The use of d 15 N as an indicator of aquatic eutrophication is based on the fact that increases in ecosystem productivity controlled by nutrient enrichments will lead to decreases in isotope fractionation by primary producers and the transfers of organic matter from one trophic level to another will result in predictable isotope enrichment along food chain (Post, 2002;Vander Zanden et al, 2015). At present, the use of consumer d 15 N largely focuses on the source of nitrogen contaminations (Lake et al, 2001;Vander Zanden et al, 2005;Schlacher et al, 2005;Robinson et al, 2016;Souza et al, 2018) and trophic interactions (Post, 2002;Vander Zanden et al, 2015;Wang et al, 2018). Very few studies link consumer isotope composition to primary productivity in freshwater ecosystems (Woodland et al, 2012;Hou et al, 2013).…”