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Updated: Jul 11, 2026

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
10:11

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations

Published on: August 3, 2016

季節的な酸素同位体変動は,バミューダ沖の生きたプランクトンフォラミニフェラの生きたプランクトンである

D F Williams, A W Bé, R G Fairbanks

    Science (New York, N.Y.)
    |October 26, 1979
    PubMed
    まとめ

    プランクトンのフォラミニフェラ殻の酸素同位体比は,地表水温を反映している. この関係により,科学者はこれらの海洋微生物化石を使用して,過去の海洋温度変動を再構築することができます.

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