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Updated: Jul 5, 2026

Resurrection of Dormant Daphnia magna: Protocol and Applications
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熱帯海面温度の一時的な上昇は,パレオセン・エオセンの熱的最大期の間に発生した

James C Zachos1, Michael W Wara, Steven Bohaty

  • 1Earth and Ocean Sciences Departments, University of California, Santa Cruz, CA 95064, USA. jzachos@es.ucsc.edu

Science (New York, N.Y.)
|October 25, 2003
PubMed
まとめ

パレオセーヌ・エオセーヌ熱極高は,海洋の大幅な温暖化を引き起こし,熱帯太平洋の海面温度が4〜5°C上昇しました. この温暖化は,大気中の二酸化炭素濃度が,これまで推定されていたよりも高いことを示唆している.

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