• Rates of sediment carbon storage in seagrass meadows restored by seeding is equivalent to natural meadows after a decade (Greiner et al. 2013)
60% of sediment carbon is non-seagrass, either advected into the meadow from adjacent ecosystems or produced in situ (Greiner et al. 2016; Oreska et al. 2017a)
• 10% of sediment carbon in seagrass meadows is derived from adjacent marshes; 50% benthic microalgae largely produced in situ, not advected into the meadow as previously believed (Greiner et al. 2016; Oreska et al. 2017a)
• Drivers of sediment carbon stocks vary on the plot and meadow scales. On the plot scale (m2), meadow age and shoot density determine sediment carbon stocks; at the meadow scale, proximity to the meadow edge is the most important driver (Oreska et al. 2017b)
• Seagrass blue carbon sediment stocks are vulnerable to marine heatwaves. A single heatwave caused a 20% loss of sediment carbon; where seagrass meadows were more resilient, this loss was reduced by half (Aoki et al. 2021)