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Updated: May 6, 2026

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過去の極端な温暖化現象は,永久凍土の解凍による大量の炭素の放出と関連しています

Robert M DeConto1, Simone Galeotti, Mark Pagani

  • 1Department of Geosciences, University of Massachusetts, Amherst, Massachusetts 01002, USA. deconto@geo.umass.edu

Nature
|April 7, 2012
PubMed
まとめ

パレオセノ・エオセノ熱最大値 (PETM) を含む地球の古代の超熱は,永久凍土の炭素の放出を引き起こす軌道サイクルによって引き起こされました. これは,これらの極端な地球温暖化イベントのタイミングと規模を説明します.

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