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Updated: Jul 16, 2026

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最後の脱氷期における同期的な放射性炭素と気候の変化

K A Hughen1, J R Southon, S J Lehman

  • 1Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. khughen@whoi.edu

Science (New York, N.Y.)
|January 11, 2000
PubMed
まとめ

放射性炭素年代測定は,脱氷期における大気中の炭素14の変動を明らかにし,これは若いドライアスの冷却イベントと一致しています. これらの変化は,おそらく深海の換気における急激な変化の結果である.

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