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 Fe2+ to porewaters, thus...

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Bibliographic Details
Main Authors: 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
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Publishing Group 2020
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Online Access:https://hdl.handle.net/10371/179362