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Updated: May 8, 2026

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
09:45

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

Published on: July 24, 2016

硫化海洋への移行は,およそ184億年前である

Simon W Poulton1, Philip W Fralick, Donald E Canfield

  • 1Danish Center for Earth System Science, Institute of Biology, University of Southern Denmark, Campusvej 55, 5230 Odense M, Denmark. s.poulton@biology.sdu.dk

Nature
|September 10, 2004
PubMed
まとめ

プロテロゾイク時代の海洋化学は,大気中の酸素が上昇したにもかかわらず,完全に酸素化されていなかった. 沈殿物は,酸素だけでなく,硫化物条件が,帯状鉄形成 (BIF) の堆積を終わらせ,生命の初期進化に影響を与えたことを明らかにしています.

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Preparation of Authigenic Pyrite from Methane-bearing Sediments for In Situ Sulfur Isotope Analysis Using SIMS

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Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment06:29

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