湿地の役割が陸上炭素吸収に及ぼす変化を解明(Researchers Reveal Role of Wetlands in Terrestrial Carbon Sink Change)

2025-07-25 中国科学院(CAS)

中国科学院・土壌科学研究所の丁維新教授らの研究チームは、2000〜2020年の湿地の炭素(C)吸収動態を、最新の全球水位データセットを用いて分析した。湿地は地球表面の3〜13%に過ぎないが、全土壌炭素の30%以上を蓄積しており、地上炭素吸収の鍵となる。研究では934の現地観測とFLUXNETデータを基に、全球の湿地による平均年間炭素吸収量を1,004Tg Cと推定。主に熱帯地域(70%)が貢献し、南米、アジア、アフリカの3大陸で79%を占める。2005年まで減少したが、その後回復し、全体的には安定傾向にあった。しかし、南米の吸収力低下が他地域の増加分を相殺した。気候変動による水文変化が地域ごとの差異を拡大しており、湿地の炭素吸収力の将来的脆弱性が懸念される。本研究はIPCCなどの地球炭素評価に重要な知見を提供する。

湿地の役割が陸上炭素吸収に及ぼす変化を解明(Researchers Reveal Role of Wetlands in Terrestrial Carbon Sink Change)
Spatial pattern of global wetland carbon sequestration (Image by LI Junjie)

<関連情報>

北半球の中高緯度地域における湿地における二酸化炭素吸収量の20年間にわたる増加は、熱帯地域と南半球における減少によって相殺されています Two decades of improved wetland carbon sequestration in northern mid-to-high latitudes are offset by tropical and southern declines

Junjie Li,Junji Yuan,Philippe Ciais,Hojeong Kang,Chris Freeman,Yuanyuan Huang,Yanhong Dong,Deyan Liu,Ye Li & Weixin Ding
Nature Ecology Evolution  Published:22 July 2025
DOI:https://doi.org/10.1038/s41559-025-02809-1

Abstract

Terrestrial carbon (C) sink has long been recognized as trending upwards, yet its recent slowdown raises concerns about accelerating climate change. Variations in wetland C sequestration are hypothesized to play a key role in this shift. Here we mapped annual water levels in global wetlands from 2000 to 2020 using 2,295 field-based measurements and predicted the spatiotemporal pattern of wetland net ecosystem production (NEP) in conjunction with other environmental factors. By compiling 934 in situ observations, we estimated a global mean wetland NEP of 56.4 (44.0‒68.8) gC m−2 yr−1. Integrating the NEP dataset with environmental datasets and machine-learning models, we estimated the mean annual global wetland C sequestration between 2000 and 2020 to be 1,004 (961‒1,047) TgC, 70% of which originated from tropical wetlands. We observed a decline in global wetland C sinks until 2005, followed by an increase thereafter. Overall, wetland C sequestration was roughly stable during 2000‒2020, as gains in northern mid-to-high latitudes were fully overwhelmed by declines in the tropics and southern mid-to-high latitudes. Our findings highlight hydrological change as a dominant driver of increasing regional variability in wetland C sinks, while intensifying hydrological extremes under climate change may undermine the resilience of wetland C sinks and the ecosystem services they support.

1702地球物理及び地球化学
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