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Updated: Jul 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

硫黄のイソトープは,アルカイア時代の有酸素大気の証拠である

Hiroshi Ohmoto1, Yumiko Watanabe, Hiroaki Ikemi

  • 1NASA Astrobiology Institute and Department of Geosciences, The Pennsylvania State University, University Park, Pennsylvania 16802, USA. ohmoto@geosc.psu.edu

Nature
|August 25, 2006
PubMed
まとめ

質量独立硫黄同位体 (MIF-S) は,古代オーストラリアの岩石には存在せず,初期の酸素化された大気という考えに異議を唱えている. この発見は,MIF-Sの起源は,大気化学のみに依存しないかもしれないことを示唆しています.

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Preparation of Authigenic Pyrite from Methane-bearing Sediments for In Situ Sulfur Isotope Analysis Using SIMS09:31

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

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment

Published on: February 27, 2021

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