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Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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142Nd evidence for early (>4.53 Ga) global differentiation of the silicate Earth

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

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