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Updated: Jul 28, 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

シリケート土の初期の (>4.53 Ga) グローバル分化に関する142番目の証拠です

M Boyet1, R W Carlson

  • 1Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road, N.W., Washington, DC 20015, USA. boyet@dtm.ciw.edu

Science (New York, N.Y.)
|June 18, 2005
PubMed
まとめ

新しい隕石のデータは,地球のマントルが特定の元素で枯渇していることを明らかにし,早期の地球差異化を示唆しています. この発見は,惑星形成のモデルと地球,月,火星の初期の分化タイムラインに影響を与えます.

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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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