Global mangrove root production, its controls and roles in the blue carbon budget of mangroves

Author:

Arnaud Marie12ORCID,Krause Stefan13ORCID,Norby Richard J.14ORCID,Dang Thuong Huyen5,Acil Nezha67ORCID,Kettridge Nicholas1,Gauci Vincent1,Ullah Sami1ORCID

Affiliation:

1. School of Geography, Earth & Environmental Sciences University of Birmingham, and Birmingham Institute of Forest Research Birmingham UK

2. Institute of Ecology and Environmental Sciences Paris (iEES‐Paris), Sorbonne University Paris France

3. Univ Lyon, Université Claude Bernard Lyon 1, CNRS, ENTPE, UMR5023, Ecologie des Hydrosystèmes Naturels et Anthropisés (LEHNA) Villeurbanne France

4. Department of Ecology and Evolutionary Biology University of Tennessee Tennessee Knoxville USA

5. Faculty of Geology and Petroleum Engineering University of Technology, Vietnam National University Ho Chi Minh City (VNU‐HCM) Vietnam

6. Institute for Environmental Futures, School of Geography, Geology and the Environment University of Leicester, Space Park Leicester Leicester UK

7. National Centre for Earth Observation University of Leicester, Space Park Leicester Leicester UK

Abstract

AbstractMangroves are among the most carbon‐dense ecosystems worldwide. Most of the carbon in mangroves is found belowground, and root production might be an important control of carbon accumulation, but has been rarely quantified and understood at the global scale. Here, we determined the global mangrove root production rate and its controls using a systematic review and a recently formalised, spatially explicit mangrove typology framework based on geomorphological settings. We found that global mangrove root production averaged ~770 ± 202 g of dry biomass m−2 year−1 globally, which is much higher than previously reported and close to the root production of the most productive tropical forests. Geomorphological settings exerted marked control over root production together with air temperature and precipitation (r2 ≈ 30%, p < .001). Our review shows that individual global changes (e.g. warming, eutrophication, drought) have antagonist effects on root production, but they have rarely been studied in combination. Based on this newly established root production rate, root‐derived carbon might account for most of the total carbon buried in mangroves, and 19 Tg C lost in mangroves each year (e.g. as CO2). Inclusion of root production measurements in understudied geomorphological settings (i.e. deltas), regions (Indonesia, South America and Africa) and soil depth (>40 cm), as well as the creation of a mangrove root trait database will push forward our understanding of the global mangrove carbon cycle for now and the future. Overall, this review presents a comprehensive analysis of root production in mangroves, and highlights the central role of root production in the global mangrove carbon budget.

Publisher

Wiley

Subject

General Environmental Science,Ecology,Environmental Chemistry,Global and Planetary Change

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