“…Previous results have demonstrated that several biochemical, metabolic or environmental factors affect the carbon isotopic ratio (hereafter referred as δ 13 C), such as growth rate, leaf thickness, inorganic C concentration in water, depth, light irradiance or pH (Cooper & DeNiro 1989;Lepoint et al, 2003;Fourqurean et al, 2007;Scartazza et al, 2017). Similarly, nitrogen isotopic ratio (hereafter δ 15 N) of marine primary producers is commonly used as a proxy of anthropic nitrogen releases (Costanzo et al, 2001;Vizzini & Mazzola 2004;Vizzini et al, 2005;Pérez et al, 2008;Lassauque et al, 2010;Vermeulen et al, 2011), but recent results indicated that δ 15 N could be used to track fluxes of matter within the shoot (Scartazza et al, 2017). Thus, isotopic differences between plant part types might be expected, since the physiology, metabolism and environmental context of the P. oceanica meadow change between plant-part types and seasons.…”