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生産性のフィードバックを通じて,パレオセーン/エオセンの境界で地球温暖化の終結

S Bains1, R D Norris, R M Corfield

  • 1Department of Earth Sciences, University of Oxford, UK. santo.bains@earth.ox.ac.uk

Nature
|September 23, 2000
PubMed
まとめ

パレオセーン/エオセンの熱的最大値は地球温暖化を引き起こした. 海洋の生産性の向上と有機炭素の埋葬により,大気中の二酸化炭素が排出され,地球が冷却された可能性が高い.

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