熱帯雨林が炭素吸収源から排出源へ転換(Tropical rainforest shifts from carbon sink to source)

2025-10-17 エディンバラ大学

エディンバラ大学などの国際研究チームは、オーストラリア北東部の熱帯雨林で過去50年間の炭素収支を解析し、森林が炭素を吸収する「シンク」から排出する「ソース」へ転じたことを確認した。1971~2000年の平均では年間0.6トンC/haの吸収があったが、2010~2019年には−0.9トンC/haの排出へ変化。気温上昇、干ばつ、サイクロンなどの気候ストレスが木の死亡率を高め、CO₂増加による成長促進効果を上回ったとされる。長期モニタリングと統計モデルにより、降雨変動と炭素収支の相関が明確化され、熱帯雨林が今後の温暖化緩和に寄与できる限界を示唆する結果となった。この発見は、地球規模の炭素循環モデルや気候政策の再評価を迫る重要な証拠と位置づけられる。成果は『Nature』誌に掲載。

<関連情報>

オーストラリアの熱帯林の地上バイオマスは今や純炭素源となっている Aboveground biomass in Australian tropical forests now a net carbon source

Hannah Carle,David Bauman,Michael N. Evans,Ingrid Coughlin,Oliver Binks,Andrew Ford,Matthew Bradford,Adrienne Nicotra,Helen Murphy & Patrick Meir
Nature  Published:15 October 2025
DOIhttps://doi.org/10.1038/s41586-025-09497-8

熱帯雨林が炭素吸収源から排出源へ転換(Tropical rainforest shifts from carbon sink to source)

Abstract

Tropical forests act as important global carbon sinks1, and Earth System Models predict increasing near-term carbon sink capacity for these forests, with elevated atmospheric carbon dioxide concentration thought to stimulate tree growth2,3. However, current forest inventory data analyses suggest that the carbon sink capacity of intact tropical forests may be in decline, portending a possible future switch from carbon sinks to carbon sources3,4,5,6,7. Here we use long-term forest inventory data (1971–2019) from Australian moist tropical forests and a causal inference framework8,9,10 to assess the carbon balance of woody aboveground standing biomass over time, the demographic processes accounting for it, and its climatic drivers, including cyclones. We find that a transition from sink (0.62 ± 0.04 Mg C ha−1 yr−1: 1971–2000) to source (−0.93 ± 0.11 Mg C ha−1 yr−1: 2010–2019) has occurred for the aboveground woody biomass of these forests, with sink capacity declining at a rate of 0.041 ± 0.032 Mg C ha−1 yr−1. The transition was driven by increasingly extreme temperature and other climate anomalies, which have increased tree mortality and associated biomass losses4, with no evidence of the carbon fertilization (stimulation) of woody tree growth. Forest dynamics underlying carbon sink capacity were also punctuated by cyclones, with impacts of a similar magnitude to long-term climate-induced changes. Our findings suggest the potential for a similar response to climate change by woody aboveground biomass in moist tropical forests globally, which could culminate in a long-term switch from carbon sinks to carbon sources.

1904環境影響評価
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