O. Serrano, Edith Cowan UniversityFollow
P.S. Lavery, Edith Cowan UniversityFollow
P. Masqué, Edith Cowan UniversityFollow
M.A. Mateo, Edith Cowan UniversityFollow
O. Serrano Orcid: https://orcid.org/0000-0002-5973-0046 Paul Lavery Orcid: https://orcid.org/0000-0001-5162-273X Pere Masqué Orcid: https://orcid.org/0000-0002-1789-320X M.A. Mateo Orcid: https://orcid.org/0000-0001-7567-0277
Nature Publishing Group
School of Science / Centre for Marine Ecosystems Research
ARC Number : LE170100219, ARC Number : DE170101524
Calcium carbonates (CaCO 3 ) often accumulate in mangrove and seagrass sediments. As CaCO 3 production emits CO 2 , there is concern that this may partially offset the role of Blue Carbon ecosystems as CO 2 sinks through the burial of organic carbon (C org ). A global collection of data on inorganic carbon burial rates (C inorg , 12% of CaCO 3 mass) revealed global rates of 0.8 TgC inorg yr −1 and 15–62 TgC inorg yr −1 in mangrove and seagrass ecosystems, respectively. In seagrass, CaCO 3 burial may correspond to an offset of 30% of the net CO 2 sequestration. However, a mass balance assessment highlights that the C inorg burial is mainly supported by inputs from adjacent ecosystems rather than by local calcification, and that Blue Carbon ecosystems are sites of net CaCO 3 dissolution. Hence, CaCO 3 burial in Blue Carbon ecosystems contribute to seabed elevation and therefore buffers sea-level rise, without undermining their role as CO 2 sinks. © 2019, The Author(s).
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