Deconstructing the mangrove carbon cycle: Gains, transformation, and losses

Author:

Adame M. F.1ORCID,Cormier N.2,Taillardat P.34,Iram N.14ORCID,Rovai A.5ORCID,Sloey T. M.6,Yando E. S.6ORCID,Blanco‐Libreros J. F.7,Arnaud M.8ORCID,Jennerjahn T.9ORCID,Lovelock C. E.10,Friess D.11,Reithmaier G. M. S.12,Buelow C. A.1,Muhammad‐Nor S. M.1314,Twilley R. R.5ORCID,Ribeiro R. A.5

Affiliation:

1. Australian Rivers Institute, Centre for Marine and Coastal Research, Griffith University Nathan Queensland Australia

2. School of Natural Sciences, Macquarie University Sydney New South Wales Australia

3. Environmental Research Institute, National University of Singapore Singapore

4. Department of Biological Sciences, Faculty of Science, Centre for Nature‐Based Climate Solutions National University of Singapore Singapore

5. Department of Oceanography and Coastal Sciences Louisiana State University Baton Rouge Louisiana USA

6. Department of Biological Sciences Old Dominion University Norfolk Virginia USA

7. Faculty of Exact and Natural Sciences, Institute of Biology, Universidad de Antioquia Medellín Colombia

8. Institute of Ecology and Environmental Sciences (IEES), UMR 7618, CNRS‐Sorbonne University‐INRAE‐UPEC‐IRD Paris France

9. Leibniz Centre for Tropical Marine Research (LZM) Bremen Germany

10. School of Environmental Sciences, The University of Queensland St Lucia Queensland Australia

11. School of Science and Engineering Tulane University New Orleans Louisiana USA

12. Department of Marine Sciences University of Gothenburg Gothenburg Sweden

13. Faculty of Science and Marine Environment, Universiti Malaysia Terengganu Kuala Nerus Terengganu Malaysia

14. East Coast Environmental Research Institute, Universiti Sultan Zainal Abidin Kuala Nerus Terengganu Malaysia

Abstract

AbstractMangroves are one of the most carbon‐dense forests on the Earth and have been highlighted as key ecosystems for climate change mitigation and adaptation. Hundreds of studies have investigated how mangroves fix, transform, store, and export carbon. Here, we review and synthesize the previously known and emerging carbon pathways in mangroves, including gains (woody biomass accumulation, deadwood accumulation, soil carbon sequestration, root and litterfall production), transformations (food web transfer through herbivory, decomposition), and losses (respiration as CO2 and CH4, litterfall export, particulate and dissolved carbon export). We then review the technologies available to measure carbon fluxes in mangroves, their potential, and their limitations. We also synthesize and compare mangrove net ecosystem productivity (NEP) with terrestrial forests. Finally, we update global estimates of carbon fluxes with the most current values of fluxes and global mangrove area. We found that the contributions of recently investigated fluxes, such as soil respiration as CH4, are minor (<1 Tg C year−1), while the contributions of deadwood accumulation, herbivory, and lateral export are significant (>35 Tg C year−1). Dissolved inorganic carbon exports are an order of magnitude higher than the other processes investigated and were highly variable, highlighting the need for further studies. Gross primary productivity (GPP) and ecosystem respiration (ER) per area of mangroves were within the same order of magnitude as terrestrial forests. However, ER/GPP was lower in mangroves, explaining their higher carbon sequestration. We estimate the global mean mangrove NEP of 109.1 Tg C year−1 (7.4 Mg C ha−1 year−1) or through a budget balance, accounting for lateral losses, a global mean of 66.6 Tg C year−1 (4.5 Mg C ha−1 year−1). Overall, mangroves are highly productive, and despite losses due to respiration and tidal exchange, they are significant carbon sinks.

Funder

Dipartimento di Scienze, Università degli Studi Roma Tre

Publisher

Wiley

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