Blue carbon sink capacity of mangroves determined by leaves and their associated microbiome

Author:

Lu Zhe12,Qin Guoming13ORCID,Gan Shuchai12,Liu Hongbin4,Macreadie Peter I.5ORCID,Cheah Wee6,Wang Faming12ORCID

Affiliation:

1. Xiaoliang Research Station of Tropical Coastal Ecosystems, Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, the CAS Engineering Laboratory for Ecological Restoration of Island and Coastal Ecosystems, and Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden Chinese Academy of Sciences Guangzhou P.R. China

2. South China National Botanical Garden Guangzhou P.R. China

3. University of Chinese Academy of Sciences Beijing P.R. China

4. Department of Ocean Sciences and Division of Life Sciences, School of Science Hong Kong University of Science and Technology Hong Kong P.R. China

5. School of Life and Environmental Sciences Deakin University, Burwood Campus Burwood Victoria Australia

6. Institute of Ocean and Earth Sciences Universiti Malaya Kuala Lumpur Malaysia

Abstract

AbstractMangroves play a globally significant role in carbon capture and storage, known as blue carbon ecosystems. Yet, there are fundamental biogeochemical processes of mangrove blue carbon formation that are inadequately understood, such as the mechanisms by which mangrove afforestation regulates the microbial‐driven transfer of carbon from leaf to below‐ground blue carbon pool. In this study, we addressed this knowledge gap by investigating: (1) the mangrove leaf characteristics using state‐of‐the‐art FT‐ICR‐MS; (2) the microbial biomass and their transformation patterns of assimilated plant‐carbon; and (3) the degradation potentials of plant‐derived carbon in soils of an introduced (Sonneratia apetala) and a native mangrove (Kandelia obovata). We found that biogeochemical cycling took entirely different pathways for S. apetala and K. obovata. Blue carbon accumulation and the proportion of plant‐carbon for native mangroves were high, with microbes (dominated by K‐strategists) allocating the assimilated‐carbon to starch and sucrose metabolism. Conversely, microbes with S. apetala adopted an r‐strategy and increased protein‐ and nucleotide‐biosynthetic potentials. These divergent biogeochemical pathways were related to leaf characteristics, with S. apetala leaves characterized by lower molecular‐weight, C:N ratio, and lignin content than K. obovata. Moreover, anaerobic‐degradation potentials for lignin were high in old‐aged soils, but the overall degradation potentials of plant carbon were age‐independent, explaining that S. apetala age had no significant influences on the contribution of plant‐carbon to blue carbon. We propose that for introduced mangroves, newly fallen leaves release nutrient‐rich organic matter that favors growth of r‐strategists, which rapidly consume carbon to fuel growth, increasing the proportion of microbial‐carbon to blue carbon. In contrast, lignin‐rich native mangrove leaves shape K‐strategist‐dominated microbial communities, which grow slowly and store assimilated‐carbon in cells, ultimately promoting the contribution of plant‐carbon to the remarkable accumulation of blue carbon. Our study provides new insights into the molecular mechanisms of microbial community responses during reforestation in mangrove ecosystems.

Funder

Basic and Applied Basic Research Foundation of Guangdong Province

National Key Research and Development Program of China

National Natural Science Foundation of China

Publisher

Wiley

Subject

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

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