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Updated: Jun 25, 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

最新のアルケア紀における有酸素窒素循環の同位体証拠

Jessica Garvin1, Roger Buick, Ariel D Anbar

  • 1Department of Earth and Space Sciences and Astrobiology Program, University of Washington, Seattle, WA 98195-1310, USA.

Science (New York, N.Y.)
|February 21, 2009
PubMed
まとめ

古代の微生物は,大気中の酸素より先に窒素循環を進化させた. この研究は,25億年前の岩石における窒素化と脱窒素化の証拠を明らかにし,広範囲にわたる酸素化以前のものである.

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Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O

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