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Future carbon emissions from global mangrove forest loss

View ORCID ProfileM.F. Adame, View ORCID ProfileR.M. Connolly, View ORCID ProfileM.P. Turschwell, View ORCID ProfileC.E. Lovelock, View ORCID ProfileL. Fatoyinbo, View ORCID ProfileD. Lagomasino, View ORCID ProfileL.A. Goldberg, J. Holdorf, View ORCID ProfileD.A. Friess, View ORCID ProfileSD. Sasmito, View ORCID ProfileJ. Sanderman, M. Sievers, View ORCID ProfileC. Buelow, View ORCID ProfileB.J. Kauffman, View ORCID ProfileD. Bryan-Brown, View ORCID ProfileC.J. Brown
doi: https://doi.org/10.1101/2020.08.27.271189
M.F. Adame
1Australian Rivers Institute, Griffith University, Nathan, 4111, QLD, Australia
2Australian Rivers Institute – Coast and Estuaries, School of Environment and Science, Griffith University, Gold Coast, 4222, QLD, Australia
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  • For correspondence: f.adame@griffith.edu.au
R.M. Connolly
2Australian Rivers Institute – Coast and Estuaries, School of Environment and Science, Griffith University, Gold Coast, 4222, QLD, Australia
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M.P. Turschwell
1Australian Rivers Institute, Griffith University, Nathan, 4111, QLD, Australia
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C.E. Lovelock
3School of Biological Sciences, The University of Queensland, St Lucia, 4072, Queensland, Australia
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L. Fatoyinbo
4NASA Goddard Space Flight Center, Greenbelt, MD, USA
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D. Lagomasino
5Department of Coastal Studies, East Carolina University, Wanchese, NC, USA
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L.A. Goldberg
6Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA
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J. Holdorf
2Australian Rivers Institute – Coast and Estuaries, School of Environment and Science, Griffith University, Gold Coast, 4222, QLD, Australia
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D.A. Friess
7Department of Geography, National University of Singapore, 1 Arts Link, Singapore 117570
8Mangrove Specialist Group, International Union for Conservation of Nature (IUCN)
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SD. Sasmito
9Research Institute for Environment and Livelihoods, Charles Darwin University, Casuarina 0810, Australia
10Center for International Forestry Research, Bogor 16115, Indonesia
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J. Sanderman
11Woods Hole Research Center. 149 Woods Hole Rd, Falmouth MA 02540, USA
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M. Sievers
2Australian Rivers Institute – Coast and Estuaries, School of Environment and Science, Griffith University, Gold Coast, 4222, QLD, Australia
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C. Buelow
2Australian Rivers Institute – Coast and Estuaries, School of Environment and Science, Griffith University, Gold Coast, 4222, QLD, Australia
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B.J. Kauffman
12Department of Fisheries, Wildlife and Conservation Sciences, Oregon State University, Corvallis, OR 97331, USA
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D. Bryan-Brown
1Australian Rivers Institute, Griffith University, Nathan, 4111, QLD, Australia
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C.J. Brown
1Australian Rivers Institute, Griffith University, Nathan, 4111, QLD, Australia
2Australian Rivers Institute – Coast and Estuaries, School of Environment and Science, Griffith University, Gold Coast, 4222, QLD, Australia
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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. The incorporation of 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 CO2 sequestration. Management actions can reduce CO2 emissions and enhance sequestration, but should be guided by predictions of future emissions, not just carbon storage. We project emissions and forgone soil carbon sequestration potential caused by mangrove loss with comprehensive global datasets for carbon stocks, mangrove distribution, deforestation rates, and drivers of land-use change. Emissions from mangrove loss could reach 2,397 Tg CO2eq by the end of the century, or 3,401 Tg CO2eq when considering forgone 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 CO2eq future emissions. We highlight hotspots for future emissions and the land-use specfic management actions that could avoid them with appropriate policies and regulation.

Competing Interest Statement

The authors have declared no competing interest.

Copyright 
The copyright holder for this preprint is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under a CC-BY-NC-ND 4.0 International license.
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Future carbon emissions from global mangrove forest loss
M.F. Adame, R.M. Connolly, M.P. Turschwell, C.E. Lovelock, L. Fatoyinbo, D. Lagomasino, L.A. Goldberg, J. Holdorf, D.A. Friess, SD. Sasmito, J. Sanderman, M. Sievers, C. Buelow, B.J. Kauffman, D. Bryan-Brown, C.J. Brown
bioRxiv 2020.08.27.271189; doi: https://doi.org/10.1101/2020.08.27.271189
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Future carbon emissions from global mangrove forest loss
M.F. Adame, R.M. Connolly, M.P. Turschwell, C.E. Lovelock, L. Fatoyinbo, D. Lagomasino, L.A. Goldberg, J. Holdorf, D.A. Friess, SD. Sasmito, J. Sanderman, M. Sievers, C. Buelow, B.J. Kauffman, D. Bryan-Brown, C.J. Brown
bioRxiv 2020.08.27.271189; doi: https://doi.org/10.1101/2020.08.27.271189

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