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Microbial Fe(III) reduction as a potential iron source from Holocene sediments beneath Larsen Ice Shelf
Recent recession of the Larsen Ice Shelf C has revealed microbial alterations of illite in marine sediments, a process typically thought to occur during low-grade metamorphism. In situ breakdown of illite provides a previously-unobserved pathway for the release of dissolved Fe(2+) to porewaters, thu...
| Autores principales: | , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6923428/ https://www.ncbi.nlm.nih.gov/pubmed/31857591 http://dx.doi.org/10.1038/s41467-019-13741-x |