File:Banded iron formation. Musée des Confluences, Lyon.jpg
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editDescriptionBanded iron formation. Musée des Confluences, Lyon.jpg |
English: Banded iron formation. Until 2 billion years ago, most of the oxygen produced by bacteria remained trapped at the bottom of the ocean in the form of iron oxydes. Musée des Confluences, Lyon
Français : Fer rubané. Jusqu'à -2 milliards d'années, l'essentiel de l'oxygène produit par les bactéries reste piégé au fond océans sous forme d'oxydes de fer. Alternances de lits de quartz et de fer oxydé. _ 2,1 milliards d'années (Précambrien). Marquette, Michigan, États-Unis. Musée des Confluences, Lyon inv. 1200043. |
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Author | Ismoon (talk) 19:14, 14 August 2019 (UTC) |
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current | 19:14, 14 August 2019 | ![]() | 1,086 × 724 (238 KB) | Ismoon (talk | contribs) | {{Information |description ={{en|1=Banded iron formation. Until 2 billion years ago, most of the oxygen produced by bacteria remained trapped at the bottom of the ocean in the form of iron oxydes. Musée des Confluences, Lyon}} {{fr|1=Fer rubané. Jusqu'à -2 milliards d'années, l'essentiel de l'oxygène produit par les bactéries reste piégé au fond océans sous forme d'oxydes de fer. Alternances de lits de quartz et de fer oxydé. _ 2,1 milliards d'années (Précambrien). Marquette, Michigan, É... |
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File change date and time | 20:52, 14 August 2019 |
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Unique ID of original document | 3F897BDDDE9A10D2A3EC389D6C45152B |
Date and time of digitizing | 22:32, 14 August 2019 |
Date metadata was last modified | 22:52, 14 August 2019 |