“…These measures are based on the analysis of some persistent morphological features of reiterative modules characterizing seagrass growth (Guidetti, 2001), and allow the determination of seagrass shoots and rhizomes age (Pergent, 1990, Duarte et al, 1994. Currently, about 60% of Mediterranean marine laboratories, focusing their research on seagrass ecosystems, use back-dating measures to monitor P. oceanica meadows, because they provide information about: (a) temporal evolution of above and below ground production; (b) rate of sedimentation; (c) importance of sexual reproduction; (d) dynamics of the meadow, and (e) reaction to environmental factors (Pergent-Martini et al, 2005). Back-dating techniques have been applied to investigate the effect on P. oceanica rhizomes growth of climate change (Marbá and Duarte, 1997), deterioration of marine coastal environment (Guidetti and Fabiano, 2000;Balestri et al, 2004;Tomasello et al, 2007), sedimentation (Boudouresque et al, 1984), water transparency (Guidetti, 2001), water temperature and hydrodynamic regime (La Loggia et al, 2004), and sexual reproduction (Balestri and Vallerini, 2003;Calvo et al, 2006).…”