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Updated: Jul 19, 2026

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環北極の泥炭地帯の急速な初期開発と大気中のCH4とCO2の変動

Glen M Macdonald1, David W Beilman, Konstantine V Kremenetski

  • 1Department of Geography, University of California, Los Angeles, CA 90095-1524, USA. macdonal@geog.ucla.edu

Science (New York, N.Y.)
|October 14, 2006
PubMed
まとめ

環極の泥炭地帯は16万5千年前に形成され始め,温暖化とともに急速に広がった. 泥炭地帯の開発は,初期のホロセーン時代にメタン (CH4) と二酸化炭素 (CO2) のレベルに影響を与えたが,後のCH4の増加を説明することはできない.

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