“…Also, the 20 min halflife of 11 C limits its use to short-term processes, in contrast to the longer-lived carbon isotope 14 C (half-life of 5,730 years). On the positive side, 11 C-tracing allows an in vivo observation of tracer movement, which has led to significant research progress in topics such as phloem sectoriality (De Schepper et al, 2013), unloading characteristics (Jahnke et al, 2009), leakage-retrieval of photoassimilates along the transport pathway (Thorpe and Minchin, 1991), phloem functioning under changing climate regimes (Hubeau et al, 2019a) and carbon allocation to root and fruit parts (Jahnke et al, 2009;Wang et al, 2014). Importantly, non-invasive measurements allow dynamic aspects of a process to be studied, and 11 C therefore provides a powerful tool to reveal the mechanisms of physiological processes (Minchin and Thorpe, 2003;Jahnke et al, 2009;Bühler et al, 2011;Hubeau et al, 2019a).…”