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Updated: Jul 3, 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

鉄質の条件が後期ネオプロテロゾーイク深水化学を支配した

Donald E Canfield1, Simon W Poulton, Andrew H Knoll

  • 1Nordic Center for Earth Evolution and Institute of Biology, Campusvej 55, University of Southern Denmark, 5230 Odense, Denmark. dec@biology.sdu.dk

Science (New York, N.Y.)
|July 19, 2008
PubMed
まとめ

ネオプロテロゾーイク時代の海は主に無酸素と鉄質で,古代の海洋化学への帰還を示唆しています. これは,地球の歴史のこの臨界期間に酸素化が限られていたことを示唆しています.

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Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod06:06

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