“…While tidal marsh and mangrove sediments have relatively high organic matter content (on average 25%) (Breithaupt et al, 2012;Cochran et al, 1998), mineral deposits account for the majority (>85%) of the accumulated substrate in seagrass sediments (Koch, 2001;Mazarrasa et al, 2015) (Table 1). Excess 210 Pb has a strong affinity for surface particles of fine sediments (Chanton et al, 1983;Cundy and Croudace, 1995;He and Walling, 1996a) and organic matter (Wan et al, 2005), thus any changes in these parameters due to sediment redistribution processes or to natural heterogeneity may also 30 result in unique types of 210 Pb concentration profiles in sediment cores of vegetated coastal ecosystems, adding complexity to the determination of sediment model age and sedimentation rates.…”