Future carbon emissions from global mangrove forest loss

• Published in: Global Change Biology
• Main Authors: Adame, Maria F., Connolly, Rod M., Turschwell, Mischa P., Lovelock, Catherine E., Fatoyinbo, Temilola, Lagomasino, David, Goldberg, Liza A., Holdorf, Jordan, Friess, Daniel A., Sasmito, Sigit D., Sanderman, Jonathan, Sievers, Michael, Buelow, Christina, Kauffman, J. Boone, Bryan‐Brown, Dale, Brown, Christopher J.
• Other Authors: Advance Queensland, Queensland Government, Australian Research Council
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2021
• Subjects: Sunda; Northwest Atlantic
• Online Access: http://dx.doi.org/10.1111/gcb.15571; https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15571; https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.15571

Abstract Mangroves have among the highest carbon densities of any tropical forest. These ‘blue carbon’ ecosystems can store large amounts of carbon for long periods, and their protection reduces greenhouse gas emissions and supports climate change mitigation. Incorporating mangroves into Nationally Determined Contributions to the Paris Agreement and their valuation on carbon markets requires predicting how the management of different land‐uses can prevent future greenhouse gas emissions and increase CO 2 sequestration. We integrated comprehensive global datasets for carbon stocks, mangrove distribution, deforestation rates, and land‐use change drivers into a predictive model of mangrove carbon emissions. We project emissions and foregone soil carbon sequestration potential under ‘business as usual’ rates of mangrove loss. Emissions from mangrove loss could reach 2391 Tg CO 2 eq by the end of the century, or 3392 Tg CO 2 eq when considering foregone soil carbon sequestration. The highest emissions were predicted in southeast and south Asia (West Coral Triangle, Sunda Shelf, and the Bay of Bengal) due to conversion to aquaculture or agriculture, followed by the Caribbean (Tropical Northwest Atlantic) due to clearing and erosion, and the Andaman coast (West Myanmar) and north Brazil due to erosion. Together, these six regions accounted for 90% of the total potential CO 2 eq future emissions. Mangrove loss has been slowing, and global emissions could be more than halved if reduced loss rates remain in the future. Notably, the location of global emission hotspots was consistent with every dataset used to calculate deforestation rates or with alternative assumptions about carbon storage and emissions. Our results indicate the regions in need of policy actions to address emissions arising from mangrove loss and the drivers that could be managed to prevent them.