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Updated: Jul 10, 2026

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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Published on: July 24, 2016

過去1000万年の硫黄循環における酸素同位体制約

Alexandra V Turchyn1, Daniel P Schrag

  • 1Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138 USA. avan@fas.harvard.edu

Science (New York, N.Y.)
|March 27, 2004
PubMed
まとめ

海洋硫酸塩酸素同位体は,過去1000万年にわたる大きな変化を明らかにしています. 海面の変動は硫黄循環に影響を与え,ミオセンの終わりに硫酸塩濃度が低下した.

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