Informing the potential of mature temperate forests as natural climate solutions: Changed fine root biomass and morphology under elevated CO <sub>2</sub>
成熟した温帯林の自然気候ソリューションとしての可能性:高CO2下での細根バイオマスと形態の変化 (AI 翻訳)
Grace Handy, Angeliki Kourmouli, Marie Arnaud, Carolina Mayoral, R.J. Norby, Michaela K. Reay, Sami Ullah, Iain P. Hartley, R. Liz Hamilton, Robert Grzesik, Andy R. Smith, Elena Vanguelova, A. R. MacKenzie, Adriane Esquivel-Muelbert
🤖 gxceed AI 要約
日本語
英国の成熟落葉樹林でのCO2施肥実験(BIFoR FACE)の5年目と7年目のデータから、高CO2環境下で細根バイオマスが約40%増加し、表層50cmに集中することを発見。根の炭素ストックが約36%増加し、形態も変化した。これにより、森林炭素吸収源モデルの精度向上が期待される。
English
Using soil cores from years 5 and 7 of the BIFoR FACE experiment in a mature temperate forest, this study found that elevated CO2 increased fine root biomass by ~40%, concentrated in the top 50 cm, and altered root morphology. This leads to a ~36% increase in root carbon standing stock, improving belowground carbon models and forest carbon sink predictions for natural climate solutions.
Unofficial AI-generated summary based on the public title and abstract. Not an official translation.
📝 gxceed 編集解説 — Why this matters
日本のGX文脈において
英国の成熟落葉樹林でのCO2施肥実験(BIFoR FACE)から、高CO2下で細根バイオマスが約40%増加し、根の炭素ストックが増えることが示された。日本の森林吸収源対策やJ-クレジットにおける森林炭素貯留の評価にも示唆を与える。
In the global GX context
This study provides empirical evidence from a mature temperate forest that elevated CO2 increases fine root biomass and carbon standing stock, which is crucial for improving forest carbon sink models and refining estimates for natural climate solutions globally. It highlights the need to account for belowground carbon in climate policy.
👥 読者別の含意
🔬研究者:Provides empirical data on root responses to eCO2 to improve carbon cycle models and reduce uncertainties in belowground carbon accounting.
🏢実務担当者:Informs forest management for carbon sequestration, but limited direct applicability for corporate sustainability teams.
🏛政策担当者:Supports the inclusion of belowground carbon in forest-based climate mitigation strategies and national greenhouse gas inventories.
📄 Abstract(原文)
Abstract Societal Impact Statement The land carbon sink absorbs approximately 25% of anthropogenic CO 2 emissions, with forests accounting for most. Managing forests as Natural Climate Solutions is therefore a societal imperative, requiring models of where and how long carbon resides within these ecosystems. We investigated the effects of elevated CO 2 on fine roots, the primary source of soil carbon, in a mature temperate forest, reporting greater biomass and changes in morphology. Improved characterisation of fine roots under elevated CO 2 can reduce uncertainties in modelled root function, addressing the reliance on aboveground observations and poorly constrained fine root representations in global forest carbon sink assessments. Summary Nature‐based solutions to climate change must incorporate mitigation strategies that sustain and enhance forest carbon sequestration, requiring comprehensive accounting of forest carbon budgets, including carbon stored in roots and soils. Forests' capacity to remain as carbon sinks under elevated CO 2 (eCO 2 ) may depend on tree root systems adjusting to overcome nutrient and water limitation. It remains uncertain whether and how root systems can change across depth under eCO 2 in mature forests. We assessed fine root biomass, morphology, depth distribution and C:N ratio, using 1‐m‐deep soil cores from Years 5 and 7 of the Birmingham Institute of Forest Research Free‐Air CO 2 Enrichment experiment (BIFoR FACE), a mature, deciduous forest subject to eCO 2 (+150 μl/L, i.e., mid‐21st century projected atmospheric CO 2 concentration). Fine root biomass was ~40% greater under eCO 2 , concentrated in the top 50 cm and equivalent to ~36% more root carbon standing stock. Contrary to previous results, the distribution of fine root biomass did not shift to greater depths. Changes in morphology were variable, but, on average, there was greater fine root length under eCO 2 and, with depth, higher specific root length. Under eCO 2 , greater fine root biomass and changes in morphology result in higher fine root surface area and thereby a greater potential for resource acquisition across the soil profile. Better characterisation of fine roots under eCO 2 can benefit belowground carbon modelling, improving predictions of forest carbon sinks and refining estimates of forests as natural climate solutions for climate policy.
🔗 Provenance — このレコードを発見したソース
- openalex https://doi.org/10.1002/ppp3.70222first seen 2026-06-19 04:37:28
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