高効率メタン消費:地下カルスト洞窟における大気メタン栄養菌によるメタンシンクとしての確固たる証拠
Xiaoyan Liu1, Xiaoyu Cheng1, Yiming Zhang1,2
1State Key Laboratory of Geomicrobiology and Environmental Change, School of Environmental Studies, China University of Geosciences, Wuhan 430078, China.
Science advances
|February 4, 2026
まとめ
メチルオリゴトロファ科のウプランド土壌クラスターγ(USCγ)に属する洞窟微生物は、メタンを大幅に酸化する。これらのメタン栄養菌は、カルストシステムを重要なメタンシンクとして理解する上で鍵となる。
科学分野:
- 地圏微生物学
- 環境科学
- 生物地球化学
背景:
- 地下カルストシステムは重要なメタンシンクであるが、メタン酸化微生物の特性評価が不足している。
- 洞窟生息メタン栄養菌の同定とその代謝活性は十分に理解されていない。
主な方法:
- 様々なメタン濃度の洞窟堆積物のインキュベーション。
- メタン酸化速度の測定。
- メタゲノムおよびメタトランスクリプトームを用いたメタン栄養菌の同定。
- NanoSIMSおよび¹³C標識リン脂質脂肪酸(PLFA)を用いた安定同位体プロービング。
結論:
- 地下カルスト生態系、特に中国南西部では、年間推定0.56 Tg CH₄を隔離する重要なメタンシンクとして機能しています。
- 同定されたメチルオリゴトロファ科メタン栄養菌は、これらの環境からのメタン排出を抑制する上で重要な役割を果たしています。
- カルストシステムは、地球規模のメタン循環において、生態学的に重要であり、これまで過小評価されてきた構成要素を表しています。
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