These authors contributed equally to this manuscript.A contribution to the special feature 'Blue Carbon' organized by Catherine Lovelock.
Electronic supplementary material is available online atShallow-water seagrasses capture and store globally significant quantities of organic carbon (OC), often referred to as 'Blue Carbon'; however, data are lacking on the importance of deep-water (greater than 15 m) seagrasses as Blue Carbon sinks. We compared OC stocks from deep-, mid-and shallowwater seagrasses at Lizard Island within the Great Barrier Reef (GBR) lagoon. We found deep-water seagrass (Halophila species) contained similar levels of OC to shallow-water species (e.g. Halodule uninervis) (0.64 + 0.08% and 0.9 + 0.1 mg C cm 23 , 0.87+ 0.19% and 1.3 + 0.3 mg C cm 23 , respectively), despite being much sparser and smaller in stature. Deep-water seagrass sediments contained significantly higher levels (approx. ninefold) of OC than surrounding bare areas. Inorganic carbon (CaCO 3 ) levels were relatively high in deep-water seagrass sediments (8.2 + 0.4%) and, if precipitated from epiphytes within the meadow, could offset the potential CO 2 -sink capacity of these meadows. The d 13 C signatures of sediment samples varied among depths and habitats (210.9 and 217.0), reflecting contributions from autochthonous and allochthonous sources. If the OC stocks reported in this study are similar to deep-water Halophila meadows elsewhere within the GBR lagoon (total area 31 000 km 2 ), then OC bound within this system is roughly estimated at 27.4 million tonnes.