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クレータ紀後期とエオセンの時期の温暖な熱帯海面温度

P N Pearson1, P W Ditchfield, J Singano

  • 1Department of Earth Sciences, University of Bristol, Queen's Road, Bristol BS8 1RJ, UK. paul.pearson@bristol.ac.uk

Nature
|October 5, 2001
PubMed
まとめ

古代の気候データは,モデルが予測するよりも冷たい熱帯を示唆しています. 保存状態の良い化石を用いた新しい研究は,気候モデルと化石の証拠と一致して,熱帯の海面温度が著しく上昇していることを明らかにしています.

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