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Redox and pH gradients drive amino acid synthesis in iron oxyhydroxide mineral systems
Iron oxyhydroxide minerals, known to be chemically reactive and significant for elemental cycling, are thought to have been abundant in early-Earth seawater, sediments, and hydrothermal systems. In the anoxic Fe(2+)-rich early oceans, these minerals would have been only partially oxidized and thus r...
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| Publicado no: | Proc Natl Acad Sci U S A |
|---|---|
| Main Authors: | , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2019
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6421445/ https://ncbi.nlm.nih.gov/pubmed/30804197 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1812098116 |
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