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Updated: Sep 9, 2025

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

Published on: July 24, 2016

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初期と中期の深海の酸素化

Chadlin M Ostrander1, Jean Nikolas R Clemente2, Richard G Stockey3

  • 1Department of Geology & Geophysics, University of Utah, Salt Lake City, UT, USA.

Science advances
|September 3, 2025
PubMed
まとめ

パレオゾイク深海の酸素は動的に変動した. タリウム同位体は4億5千万年から3億8千万年前までの長い酸素化イベントを明らかにし,3億8千万年前以降の持続的なO2蓄積を示しています.

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