Global blue carbon losses from salt marshes exceed restoration gains.

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Hauptverfasser: Zheng, Yuhan, Jiang, Qutu, He, Qiang, Xiao, Xiangming, Macreadie, Peter I, Xu, Xiao, Nie, Ming, Wu, Jihua, Ye, Guanqiong, Wu, Jiaping, Gu, Jiali, Cui, Lijuan, Wang, Xinxin, Li, Bo
Format: Artículo científico
Sprache:en
Veröffentlicht: Nature communications 2026
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author Zheng, Yuhan
Jiang, Qutu
He, Qiang
Xiao, Xiangming
Macreadie, Peter I
Xu, Xiao
Nie, Ming
Wu, Jihua
Ye, Guanqiong
Wu, Jiaping
Gu, Jiali
Cui, Lijuan
Wang, Xinxin
Li, Bo
author_facet Zheng, Yuhan
Jiang, Qutu
He, Qiang
Xiao, Xiangming
Macreadie, Peter I
Xu, Xiao
Nie, Ming
Wu, Jihua
Ye, Guanqiong
Wu, Jiaping
Gu, Jiali
Cui, Lijuan
Wang, Xinxin
Li, Bo
Zheng, Yuhan
Jiang, Qutu
He, Qiang
Xiao, Xiangming
Macreadie, Peter I
Xu, Xiao
Nie, Ming
Wu, Jihua
Ye, Guanqiong
Wu, Jiaping
Gu, Jiali
Cui, Lijuan
Wang, Xinxin
Li, Bo
collection PubMed - marine biology
contents Global blue carbon losses from salt marshes exceed restoration gains. Zheng, Yuhan Jiang, Qutu He, Qiang Xiao, Xiangming Macreadie, Peter I Xu, Xiao Nie, Ming Wu, Jihua Ye, Guanqiong Wu, Jiaping Gu, Jiali Cui, Lijuan Wang, Xinxin Li, Bo Salt marsh soil organic carbon (SOC) is a key blue carbon pool affected by both disturbance and restoration; yet its long-term global dynamics remains poorly understood. Here we provide the global assessment of surface SOC changes in salt marshes from 2002 to 2019, combining multi-source remote sensing imagery with the machine learning calibrated by field observations. We find a net global SOC loss of 0.52 million tonnes, primarily driven by declines in North America and Oceania, which are only partially offset by gains in Asia and South America. The United States alone accounts for ~60% of the global loss, equivalent to 6.2 million tonnes of CO if fully released. Losses are concentrated in mature salt marshes with large SOC storage, while gains occur primarily in newly formed salt marshes with relatively low SOC density. These patterns suggest that global restoration efforts are failing to keep pace with degradation. To avert irreversible climate and ecological damage, the protection of mature, carbon-rich salt marshes must become a core component of global climate strategies.
format Artículo científico
id pubmed_42031742
institution PubMed
language en
publishDate 2026
publisher Nature communications
record_format pubmed
spellingShingle Global blue carbon losses from salt marshes exceed restoration gains.
Zheng, Yuhan
Jiang, Qutu
He, Qiang
Xiao, Xiangming
Macreadie, Peter I
Xu, Xiao
Nie, Ming
Wu, Jihua
Ye, Guanqiong
Wu, Jiaping
Gu, Jiali
Cui, Lijuan
Wang, Xinxin
Li, Bo
Global blue carbon losses from salt marshes exceed restoration gains. Zheng, Yuhan Jiang, Qutu He, Qiang Xiao, Xiangming Macreadie, Peter I Xu, Xiao Nie, Ming Wu, Jihua Ye, Guanqiong Wu, Jiaping Gu, Jiali Cui, Lijuan Wang, Xinxin Li, Bo Salt marsh soil organic carbon (SOC) is a key blue carbon pool affected by both disturbance and restoration; yet its long-term global dynamics remains poorly understood. Here we provide the global assessment of surface SOC changes in salt marshes from 2002 to 2019, combining multi-source remote sensing imagery with the machine learning calibrated by field observations. We find a net global SOC loss of 0.52 million tonnes, primarily driven by declines in North America and Oceania, which are only partially offset by gains in Asia and South America. The United States alone accounts for ~60% of the global loss, equivalent to 6.2 million tonnes of CO if fully released. Losses are concentrated in mature salt marshes with large SOC storage, while gains occur primarily in newly formed salt marshes with relatively low SOC density. These patterns suggest that global restoration efforts are failing to keep pace with degradation. To avert irreversible climate and ecological damage, the protection of mature, carbon-rich salt marshes must become a core component of global climate strategies.
title Global blue carbon losses from salt marshes exceed restoration gains.
url https://pubmed.ncbi.nlm.nih.gov/42031742/