Methane and nitrous oxide emissions and related microbial communities from mangrove stems on Qi'ao Island, Pearl River Estuary in China

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Mangrove forests, crucial carbon-rich ecosystems, are increasingly vulnerable to soil carbon loss and greenhouse gas (GHG) emissions due to human disturbance. However, the contribution of mangrove trees to GHG emissions remains poorly understood. This study monitored CO2, CH4, and N2O fluxes from the stems of two mangrove species, native Kandelia obovata (KO) and exotic Sonneratia apetala (SA), at three heights (0.7 m, 1.2 m, and 1.7 m) during the dry winter period on Qi'ao Island, Pearl River Estuary, China. Heartwood samples were analyzed to identify potential functional groups related to gas fluxes. Our study found that tree stems acted as both sinks and sources for N2O (ranging from −9.49 to 28.35 μg m−2 h−1 for KO and from −6.73 to 28.95 μg m−2 h−1 for SA) and CH4. SA exhibited significantly higher stem CH4 flux (from −26.67 to 97.33 μg m−2 h−1) compared to KO (from −44.13 to 88.0 μg m−2 h−1) (P < 0.05). When upscaled to the community level, both species were net emitters of CH4, contributing approximately 4.68 % (KO) and 0.51 % (SA) to total CH4 emissions. The decrease in stem CH4 flux with increasing height, indicates a soil source. Microbial analysis in the heartwood using the KEGG database indicated aceticlastic methanogenesis as the dominant CH4 pathway. The presence of methanogens, methanotrophs, denitrifiers, and nitrifiers suggests microbial involvement in CH4 and N2O production and consumption. Remarkably, the dominance of Cyanobacteria in the heartwood microbiome (with the relative abundance of 97.5 ± 0.6 % for KO and 99.1 ± 0.2 % for SA) implies roles in carbon and nitrogen fixation for mangroves coping with nitrogen limitation in coastal wetlands, and possibly in CH4 production. Although the present study has limitations in sampling duration and area, it highlights the significant role of tree stems in GHG emissions which is crucial for a holistic evaluation of the global carbon sequestration capability of mangrove ecosystems. Future research should broaden spatial and temporal scales to enhance the accuracy of upscaling tree stem gas fluxes to the mangrove ecosystem level.
OriginalsprogEngelsk
Artikelnummer170062
TidsskriftScience of the Total Environment
Vol/bind915
Antal sider12
ISSN0048-9697
DOI
StatusUdgivet - 2024

Bibliografisk note

Funding Information:
Funding was provided by the National Natural Science Foundation of China ( U21A6001 , 42007090 ), Guangdong Major Project of Basic and Applied Basic Research ( 2020B0301030004 ), China Meteorological Administration Climate Change Special Program ( QBZ202301 ), the Key Program of Marine Economy Development Special Foundation of Department of Natural Resources of Guangdong Province ( GDNRC[2022]20 ), and the Open Fund of Fujian Key Laboratory of Severe Weather ( 2022KFKT03 ). We acknowledge the students Jingyi Su, Chi Zhang, Yulin Miao, Liangxin Tong, Hongjia Zhu, Wu Zhou, Yuxun Zhong, and Ziming Zhang for the help in the field and laboratory, and greatly appreciate the three anonymous reviewers for their comments to improve our manuscript.

Publisher Copyright:
© 2024 Elsevier B.V.

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