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パレオセノ/エオセノ熱最大期における湿った気候状態

Gabriel J Bowen1, David J Beerling, Paul L Koch

  • 1Earth Sciences Department, University of California, Santa Cruz, California 95064, USA. gbowen@biology.utah.edu

Nature
|November 27, 2004
PubMed
まとめ

パレオセーン/エオセーン熱最大 (PETM) 温暖化イベントには,かなりの炭素の放出が含まれていました. 新しい発見は,気温の上昇と陸上の炭素循環による気候システムのシフトを明らかにし,それはメタンの放出によってのみ説明されるものではありません.

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