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Updated: Jul 12, 2026

Resurrection of Dormant Daphnia magna: Protocol and Applications
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パレオセノ・エオセノ熱最大値と北東大西洋の開口

Michael Storey1, Robert A Duncan, Carl C Swisher

  • 1Quaternary Dating Laboratory, Department of Environment, Society and Spatial Change, Roskilde University Centre, Post Office Box 260, 4000 Roskilde, Denmark.

Science (New York, N.Y.)
|April 28, 2007
PubMed
まとめ

パレオセーヌ・エオセーヌ熱マキシマム (PETM) は,グリーンランド・ヨーロッパプレート境界付近の火山活動中の温室効果ガスの放出によって引き起こされた. このイベントは,約5610万年前から始まった大規模な洪水ベースルト噴火の後に起こった.

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