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Rethinking the impacts of bottom trawling on seabed carbon: Biogeochemical mechanisms, vulnerability and long‐term climate consequences

海底炭素に対する底引き網漁の影響を再考する:生物地球化学的メカニズム、脆弱性、長期的な気候への影響 (AI 翻訳)

J. Tiano, Emil De Borger

Journal of Applied Ecology📚 査読済 / ジャーナル2026-04-01#気候科学
DOI: 10.1111/1365-2664.70346
原典: https://doi.org/10.1111/1365-2664.70346

🤖 gxceed AI 要約

日本語

底引き網漁が海底炭素動態に与える影響を統合的に分析した展望論文。撹乱が水柱での再鉱物化を促進する一方、堆積物中の有機炭素貯留を減少させる二面的効果を指摘。長期的炭素隔離を考慮した地域固有の管理の重要性を強調し、一律の操業制限ではなく堆積ポテンシャルの高い生息域を優先するアプローチを提案している。

English

This perspective synthesizes evidence on how bottom trawling disturbs seabed carbon dynamics, increasing remineralization in the water column while reducing local carbon stocks. It distinguishes short-term reactive carbon loss from long-term burial impairment, arguing that context-dependent, region-specific management prioritizing high-burial habitats is more effective than blanket bans for climate mitigation.

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

日本は漁業国であり、ブルーカーボンや海底炭素貯留への関心が高まっている。本論文は、SSBJやTCFD等の枠組みで注目される自然資本・生態系サービス評価において、海底炭素を管理対象とする際の科学的根拠を提供する。

In the global GX context

Globally, the paper informs the growing integration of natural capital and ocean-based climate solutions into disclosure frameworks like TNFD and ISSB. It provides a nuanced perspective on managing seabed carbon, cautioning against oversimplified approaches while offering guidance for habitat prioritization in climate policy.

👥 読者別の含意

🔬研究者:Provides a comprehensive synthesis of trawling impacts on carbon cycling, highlighting key uncertainties and research gaps for marine biogeochemists.

🏢実務担当者:Offers actionable insights for fisheries and marine spatial planning managers on prioritizing habitats for carbon burial protection.

🏛政策担当者:Argues for region-specific, evidence-based management of seabed carbon rather than blanket bans, relevant to national climate and ocean policy.

📄 Abstract(原文)

Bottom trawling is the most widespread anthropogenic disturbance to marine benthic ecosystems, with a growing recognition of its potential to alter sedimentary carbon dynamics and influence ocean–atmosphere CO 2 exchange. Yet, the magnitude and underlying mechanisms of trawling‐induced carbon emissions from the seafloor remain poorly understood and subject to ongoing scientific debate. In this perspective, we synthesise current evidence on how physical disturbance caused by demersal fisheries has opposing effects on organic carbon (OC) mineralisation across different compartments with a particular focus on the distinction between short‐term remineralisation and long‐term carbon burial. We argue that bottom disturbance increases remineralisation in the water column by resuspending reactive OC to oxygenated environments, while decreasing local seabed OC stocks and in situ sediment mineralisation by reducing reactive OC and benthic fauna. We further distinguish between short‐term remineralisation of reactive OC and the longer‐term impairment of carbon burial in depositional zones. The critical role of benthic fauna, particularly bioturbators, in regulating carbon processing and sequestration remains complex and context‐dependent. While highly reactive OC is the most vulnerable to rapid mineralisation, prioritising management solely on the basis of OC reactivity risks overlooking habitats that contribute disproportionately to long‐term carbon sequestration. Depositional areas, though sometimes lower in OC lability, can offer greater climate‐relevant sequestration value and represent priority habitats for management aimed at protecting long‐term carbon burial. Synthesis and applications : Given this strong context dependence, effective protection of seabed carbon stocks requires region‐specific assessments that identify and prioritise habitats with high burial potential amongst considerations for increased short‐term CO 2 release, rather than blanket trawling bans or uniform effort reductions. Ultimately, while seabed carbon protection can support climate policy, it must remain secondary to, and never a substitute for, the urgent need to reduce fossil fuel emissions.

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