地球が余剰炭素をどのように貯蔵するかを解明(How the Planet Stores Our Excess Carbon Emissions)

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2025-03-21 カリフォルニア工科大学 (Caltech)

地球が余剰炭素をどのように貯蔵するかを解明(How the Planet Stores Our Excess Carbon Emissions)
Though carbon stored in land has been increasing, biomass has remained relatively steady. This is because carbon in land has been mostly stored in nonliving pools like soils and sediments.Credit: Bar-On et al., Science 387, 1291-1295 (2025)

カリフォルニア工科大学(Caltech)の研究者らは、地球が大気中の余剰二酸化炭素(CO₂)をどのように取り込み保存しているかを明らかにした。海洋は約25%のCO₂を吸収し、植物や土壌も重要な炭素吸収源である。特に、岩石の風化により生じる炭酸塩鉱物への長期的なCO₂固定や、海洋生物の活動による「生物ポンプ」などが地球規模で炭素循環に貢献している。研究者らは、気候変動の将来予測や炭素除去技術の設計において、これら自然の炭素吸収プロセスの定量的理解が不可欠であると強調している。

<関連情報>

地球全体の陸域炭素蓄積における最近の増加は、ほとんどが非生物プールに蓄積されている Recent gains in global terrestrial carbon stocks are mostly stored in nonliving pools

Yinon M. Bar-On, Xiaojun Li, Michael O’Sullivan, Jean-Pierre Wigneron, […], and Woodward W. Fischer
Science  Published:20 Mar 2025
DOI:https://doi.org/10.1126/science.adk1637

Editor’s summary

Approximately 30% of the carbon emitted by human activity has been taken up on land, but exactly how and where that uptake has been achieved has been an open question. Bar-On et al. examined existing observational records of terrestrial carbon pools and found that live biomass has stored only a small fraction of that carbon, the bulk having been incorporated into nonliving organic matter (see the Perspective by Canadell). This work has important implications for understanding how quickly carbon is returned to the atmosphere. —Jesse Smith

Abstract

Terrestrial sequestration of carbon has mitigated ≈30% of anthropogenic carbon emissions. However, its distribution across different pools, live or dead biomass and soil and sedimentary organic carbon, remains uncertain. Analyzing global observational datasets of changes in terrestrial carbon pools, we found that ≈35 ± 14 gigatons of carbon (GtC) have been sequestered on land between 1992 and 2019, whereas live biomass changed by ≈1 ± 7 GtC. Global vegetation models instead imply that sequestration has been mostly in live biomass. We identify key processes not included in most models that can explain this discrepancy. Most terrestrial carbon gains are sequestered as nonliving matter and thus are more persistent than previously appreciated, with a substantial fraction linked to human activities such as river damming, wood harvest, and garbage disposal in landfills.

1900環境一般
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