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...

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Detalles Bibliográficos
Autores principales: Jung, Jaewoo, Yoo, Kyu-Cheul, Rosenheim, Brad E., Conway, Tim M., Lee, Jae Il, Yoon, Ho Il, Hwang, Chung Yeon, Yang, Kiho, Subt, Christina, Kim, Jinwook
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
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

Internet

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

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