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Updated: Jul 10, 2026

Visualizing Methane-Cycling Microbial Dynamics in Coastal Wetlands
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熱カルスト湖は,最後の脱氷期における大気中のCH4の源である

K M Walter1, M E Edwards, G Grosse

  • 1Water and Environmental Research Center, University of Alaska, Fairbanks, AK 99775, USA. ftkmw1@uaf.edu

Science (New York, N.Y.)
|October 27, 2007
PubMed
まとめ

気候温暖化で北極湖の解凍から放出されたメタン (CH4) は,世界のCH4濃度の上昇に大きく寄与した. この研究では,熱カルスト湖のCH4排出が過去の気候変動に及ぼす実質的な影響を定量化しています.

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